Suspended Transformation.--Although it is possible for the anhydrous salt

to make its appearance at the temperature of the quadruple point, it will

not necessarily do so; and it is therefore possible to follow the

solubility curve of sodium sulphate decahydrate to a higher temperature.

Since, however, the solubility of the decahydrate at temperatures above the

quadruple point is greater than that of the anhydrous salt, the solution

which is _saturated_ with respect to the former will be _supersaturated_

with respect to the latter. On bringing a small quantity of the anhydrous

salt in contact with the solution, therefore, anhydrous salt will be

deposited; and all the hydrated salt present will ultimately undergo

conversion into the anhydrous salt, through the medium of the solution. In

this case, as in all cases, the solid phase, which is the most stable at

the temperature of the experiment, has at that temperature the least

solubility.

Similarly, the solubility curve of anhydrous sodium sulphate has been

followed to temperatures below 32.5deg. Below this temperature, however,

the solubility of this salt is greater than that of the decahydrate, and

the saturated solution of the anhydrous salt will therefore be

supersaturated for the decahydrate, and will deposit this salt if a

"nucleus" is added to the solution. From this we see that at temperatures

above 32.5deg the anhydrous salt is the stable form, while the decahydrate

is unstable (or metastable); at temperatures below 32.5deg the decahydrate

is stable. This temperature, therefore, is the _transition temperature_ for

decahydrate and anhydrous salt.

From Fig. 33 we see further that the solubility curve of the anhydrous salt

(which at all temperatures below 32.5deg is metastable) is cut by the

solubility curve of the heptahydrate; and this point of intersection (at a

temperature of 24.2deg) must be the _transition point_ for heptahydrate and

anhydrous salt. Since at all temperatures the solubility of the

heptahydrate is greater than that of the decahydrate, the former hydrate

must be metastable with respect to the latter; so that throughout its whole

course the solubility curve of the heptahydrate {138} represents only

metastable equilibria. Sodium sulphate, therefore, forms only one stable

hydrate, the decahydrate.

The solubility relations of sodium sulphate illustrate very clearly the

importance of the solid phase for the definition of saturation and

supersaturation. Since the solubility curve of the anhydrous salt has been

followed backwards to a temperature of about 18deg, it is readily seen,

from Fig. 33, that at a temperature of, say, 20deg three different

_saturated_ solutions of sodium sulphate are possible, according as the

anhydrous salt, the heptahydrate or the decahydrate, is present as the

solid phase. Two of these solutions, however, would be metastable and

_supersaturated with respect to the decahydrate_.

Further, the behaviour of sodium sulphate and water furnishes a very good

example of the fact that a "break" in the solubility curve occurs when, and

only when, the solid phase undergoes change. So long as the decahydrate,

for example, remained unaltered in contact with the solution, the

solubility curve was continuous; but when the anhydrous salt appeared in

the solid phase, a distinct change in the direction of the solubility curve

was observed.

Dehydration by Means of Anhydrous Sodium Sulphate.--The change in the

relative stability of sodium sulphate decahydrate and anhydrous salt in

presence of water at a temperature of 32.5deg explains why the latter salt

cannot be employed for dehydration purposes at temperatures above the

transition point. The dehydrating action of the anhydrous salt depends on

the formation of the decahydrate; but since at temperatures above 33deg the

latter is unstable, and cannot be formed in presence of the anhydrous salt,

this salt cannot, of course, effect a dehydration above that temperature.

Pressure-Temperature Diagram.--The consideration of the

pressure-temperature relations of the two components, sodium sulphate and

water, must include not only the vapour pressure of the saturated

solutions, but also that of the crystalline hydrates. The vapour pressures

of salt hydrates have already been treated in a general manner (Chap. V.),

so that it is only necessary here to point out the connection between the

two classes of systems. {139}

In most cases the vapour pressure of a salt hydrate, _i.e._ the vapour

pressure of the system hydrate--anhydrous salt (or lower hydrate)--vapour,

is at all temperatures lower than that of the system anhydrous salt (or

lower hydrate)--solution--vapour. This, however, is not a necessity; and

cases are known where the vapour pressure of the former system is, under

certain circumstances, equal to or higher than that of the latter. An

example of this is found in sodium sulphate decahydrate.

On heating Na_{2}SO_{4},10H_{2}O, a point is reached at which the

dissociation pressure into anhydrous salt and water vapour becomes equal to

the vapour pressure of the saturated solution of the anhydrous salt, as is

apparent from the following measurements;[212] the differences in pressure

being expressed in millimetres of a particular oil.

Temperature: 29.0deg 30.83deg 31.79deg 32.09deg 32.35deg 32.6deg

Difference of

pressure: 23.8 10.8 5.6 3.6 1.6 0

At 32.6deg, therefore, the vapour pressures of the two systems

Na_{2}SO_{4},10H_{2}O--Na_{2}SO_{4}--vapour

Na_{2}SO_{4}--solution--vapour

are equal; at this temperature the four phases, Na_{2}SO_{4},10H_{2}O;

Na_{2}SO_{4}; solution; vapour, can coexist. From this it is evident that

when sodium sulphate decahydrate is heated to 32.6deg, the two new phases

anhydrous salt and solution will be formed (suspended transformation being

supposed excluded), and the hydrate will appear to undergo _partial

fusion_; and during the process of "melting" the vapour pressure and

temperature will remain constant.[213] This is, however, not a true but a

so-called _incongruent_ melting point; for the composition of the liquid

phase is not the same as that of the solid. As has already been pointed out

(p. 137), we are dealing here with the _transition point_ of the

decahydrate and anhydrous salt, _i.e._ with the reaction

Na_{2}SO_{4},10H_{2}O <--> Na_{2}SO_{4} + 10H_{2}O.

Since at the point of partial fusion of the decahydrate four {140} phases

can coexist, the point is a quadruple point in a two-component system, and

the system at this point is therefore invariant. The temperature of this

point is therefore perfectly definite, and on this account the proposal has

been made to adopt this as a fixed point in thermometry.[214] The

temperature is, of course, practically the same as that at which the two

solubility curves intersect (p. 112). If, however, the vapour phase

disappears, the system becomes univariant, and the equilibrium temperature

undergoes change with change of pressure. The transition curve has been

determined by Tammann,[215] and shown to pass through a point of maximum

temperature.

[Illustration: FIG. 34.]

The vapour pressure of the different systems of sodium sulphate and water

can best be studied with the help of the diagram in Fig. 34.[216] The curve

ABCD represents the vapour-pressure curve of the saturated solution of

anhydrous sodium sulphate. GC is the pressure curve of decahydrate +

anhydrous salt, which, as we have seen, cuts the curve ABCD at the

transition temperature, 32.6deg. Since at this point the solution is

saturated with respect to both the anhydrous salt and the decahydrate, the

vapour-pressure curve of the saturated solution of the latter must also

pass through the point C.[217] As at temperatures below this point the

solubility of the decahydrate is less than that of the anhydrous salt, the

vapour pressure of the solution will, in accordance with Babo's law

(p. 126), be higher than that of the solution of the anhydrous salt; which

was also found experimentally to be the case (curve HC).

{141}

In connection with the vapour pressure of the saturated solutions of the

anhydrous salt and the decahydrate, attention must be drawn to a

conspicuous deviation from what was found to hold in the case of

one-component systems in which a vapour phase was present (p. 31). There,

it was seen that the vapour pressure of the more stable system was always

_lower_ than that of the less stable; in the present case, however, we find

that this is no longer so. We have already learned that at temperatures

below 32.5deg the system decahydrate--solution--vapour is more stable than

the system anhydrous salt--solution--vapour; but the vapour pressure of the

latter system is, as has just been stated, lower than that of the former.

At temperatures above the transition point the vapour pressure of the

saturated solution of the decahydrate will be lower than that of the

saturated solution of the anhydrous salt.

This behaviour depends on the fact that the less stable form is the more

soluble, and that the diminution of the vapour pressure increases with the

amount of salt dissolved.

With regard to sodium sulphate heptahydrate the same considerations will

hold as in the case of the decahydrate. Since at 24deg the four phases

heptahydrate, anhydrous salt, solution, vapour can coexist, the

vapour-pressure curves of the systems hydrate--anhydrous salt--vapour

(curve EB) and hydrate--solution--vapour (curve FB) must cut the pressure

curve of the saturated solution of the anhydrous salt at the above

temperature, as represented in Fig. 34 by the point B. This constitutes,

therefore, a second quadruple point, which is, however, metastable.

From the diagram it is also evident that the dissociation pressure of the

heptahydrate is higher than that of the decahydrate, although it contains

less water of crystallization. The system heptahydrate--anhydrous

salt--vapour must be metastable with respect to the system

decahydrate--anhydrous salt--vapour, and will pass into the latter.[218]

Whether or not there is a temperature at which the vapour-pressure curves

of the two systems intersect, and below which the heptahydrate becomes the

more stable form, is not known.

{142}

In the case of sodium sulphate there is only one stable hydrate. Other

salts are known which exhibit a similar behaviour; and we shall therefore

expect that the solubility relationships will be represented by a diagram

similar to that for sodium sulphate. A considerable number of such cases

have, indeed, been found,[219] and in some cases there is more than one

metastable hydrate. This is found, for example, in the case of nickel

iodate,[220] the solubility curves for which are given in Fig. 35. As can

be seen from the figure, suspended transformation occurs, the solubility

curves having in some cases been followed to a considerable distance beyond

the transition point. One of the most brilliant examples, however, of

suspended transformation in the case of salt hydrates, and the sluggish

transition from the less stable to the more stable form, is found in the

case of the hydrates of calcium chromate.[221]

[Illustration: FIG. 35.]

In the preceding cases, the dissociation-pressure curve of the hydrated

salt cuts the vapour-pressure curve of the saturated {143} solution of the

anhydrous salt. It can, however, happen that the dissociation-pressure

curve of one hydrate cuts the solubility curve, not of the anhydrous salt,

but of a lower hydrate; in this case there will be more than one stable

hydrate, each having a stable solubility curve; and these curves will

intersect at the temperature of the transition point. Various examples of

this behaviour are known, and we choose for illustration the solubility

relationships of barium acetate and its hydrates[222] (Fig. 36).

[Illustration: FIG. 36.]

At temperatures above 0deg, barium acetate can form two stable hydrates, a

trihydrate and a monohydrate. The solubility of the trihydrate increases

very rapidly with rise of temperature, and has been determined up to

26.1deg. At temperatures above 24.7deg, however, the trihydrate is

metastable with respect to the monohydrate; for at this temperature the

solubility curve of the latter hydrate cuts that of the former. This is,

therefore, the transition temperature for the trihydrate and monohydrate.

The solubility curve of the monohydrate succeeds that of the trihydrate,

and exhibits a conspicuous point of minimum solubility at about 30deg.

Below 24.7deg the {144} monohydrate is the less stable hydrate, but its

solubility has been determined to a temperature of 22deg. At 41deg the

solubility curve of the monohydrate intersects that of the anhydrous salt,

and this is therefore the transition temperature for the monohydrate and

anhydrous salt. Above this temperature the anhydrous salt is the stable

solid phase. Its solubility curve also passes through a minimum.

The diagram of solubilities of barium acetate not only illustrates the way

in which the solubility curves of the different stable hydrates of a salt

succeed one another, but it has also an interest and importance from

another point of view. In Fig. 36 there is also shown a faintly drawn curve

which is continuous throughout its whole course. This curve represents the

solubility of barium acetate as determined by Krasnicki.[223] Since,

however, three different solid phases can exist under the conditions of

experiment, it is evident, from what has already been stated (p. 111), that

the different equilibria between barium acetate and water could not be

represented by one _continuous_ curve.

Another point which these experiments illustrate and which it is of the

highest importance to bear in mind is, that in making determinations of the

solubility of salts which are capable of forming hydrates, it is not only

necessary to determine the composition of the solution, but _it is of equal

importance to determine the composition of the solid phase in contact with

it_. In view of the fact, also, that the solution equilibrium is in many

cases established with comparative slowness, it is necessary to confirm the

point of equilibrium, either by approaching it from higher as well as from

lower temperatures, or by actually determining the rate with which the

condition of equilibrium is attained. This can be accomplished by actual

weighing of the dissolved salt or by determinations of the density of the

solution, as well as by other methods.

{145}

2. _The Compounds formed have a Definite Melting Point._

In the cases which have just been considered we saw that the salt hydrates

on being heated did not undergo complete fusion, but that a solid was

deposited consisting of a lower hydrate or of the anhydrous salt. It has,

however, been long known that certain crystalline salt hydrates (_e.g._

sodium thiosulphate, Na_{2}S_{2}O_{3},5H_{2}O, sodium acetate,

NaC_{2}H_{3}O_{2},3H_{2}O) melt completely in their water of

crystallization, and yield a liquid of the _same composition_ as the

crystalline salt. In the case of sodium thiosulphate pentahydrate the

temperature of liquefaction is 56deg; in the case of sodium acetate

trihydrate, 58deg. These two salts, therefore, have a definite melting

point. For the purpose of studying the behaviour of such salt hydrates, we

shall choose not the cases which have just been mentioned, but two others

which have been more fully studied, viz. the hydrates of calcium chloride

and of ferric chloride.

Solubility Curve of Calcium Chloride Hexahydrate.[224]--Although calcium

chloride forms several hydrates, each of which possesses its own

solubility, it is nevertheless the solubility curve of the hexahydrate

which will chiefly interest us at present, and we shall therefore first

discuss that curve by itself.

[Illustration: FIG. 37.]

The solubility of this salt has been determined from the cryohydric point,

which lies at about -55deg, up to the melting point of the salt.[225] The

solubility increases with rise of temperature, as is shown by the figures

in the following table, and by the (diagrammatic) curve AB in Fig. 37. In

the table, the numbers under the heading "solubility" denote the number of

grams of CaCl_{2} dissolved in 100 grams {146} of water; those under the

heading "composition," the number of gram-molecules of water in the

solution to one gram-molecule of CaCl_{2}.

SOLUBILITY OF CALCIUM CHLORIDE HEXAHYDRATE.

-----------------------------------------

Temperature. | Solubility. | Composition.

-----------------------------------------

-55deg | 42.5 | 14.5

-25deg | 50.0 | 12.3

-10deg | 55.0 | 11.2

0deg | 59.5 | 10.37

10deg | 65.0 | 9.49

20deg | 74.5 | 8.28

25deg | 82.0 | 7.52

28.5deg | 90.5 | 6.81

29.5deg | 95.5 | 6.46

30.2deg | 102.7 | 6.00

29.6deg | 109.0 | 5.70

29.2deg | 112.8 | 5.41

-----------------------------------------

So far as the first portion of the curve is concerned, it resembles the

most general type of solubility curve. In the present case the solubility

is so great and increases so rapidly with rise of temperature, that a point

is reached at which the water of crystallization of the salt is sufficient

for its complete solution. This temperature is 30.2deg; and since the

composition of the solution is the same as that of the solid salt, viz. 1

mol. of CaCl_{2} to 6 mols. of water, this temperature must be the melting

point of the hexahydrate. At this point the hydrate will fuse or the

solution will solidify without change of temperature and without change of

composition. Such a melting point is called a _congruent_ melting point.

But the solubility curve of calcium chloride hexahydrate differs markedly

from the other solubility curves hitherto considered in that it possesses a

_retroflex portion_, represented in the figure by BC. As is evident from

the figure, therefore, calcium chloride hexahydrate exhibits the peculiar

and, as it was at first thought, impossible behaviour that it can be in

equilibrium at one and the same temperature with two different solutions,

one of which contains more, the other less, water than the solid hydrate;

for it must be remembered that {147} throughout the whole course of the

curve ABC the solid phase present in equilibrium with the solution is the

hexahydrate.

Such a behaviour, however, on the part of calcium chloride hexahydrate will

appear less strange if one reflects that the melting point of the hydrate

will, like the melting point of other substances, be lowered by the

addition of a second substance. If, therefore, water is added to the

hydrate at its melting point, the temperature at which the solid hydrate

will be in equilibrium with the liquid phase (solution) will be lowered; or

if, on the other hand, anhydrous calcium chloride is added to the hydrate

at its melting point (or what is the same thing, if water is removed from

the solution), the temperature at which the hydrate will be in equilibrium

with the liquid will also be lowered; _i.e._ the hydrate will melt at a

lower temperature. In the former case we have the hydrate in equilibrium

with a solution containing more water, in the latter case with a solution

containing less water than is contained in the hydrate itself.

It has already been stated (p. 109) that the solubility curve (in general,

the equilibrium curve) is continuous so long as the solid phase remains

unchanged; and we shall therefore expect that the curve ABC will be

continuous. Formerly, however, it was considered by some that the curve was

not continuous, but that the melting point is the point of intersection of

two curves, a solubility curve and a fusion curve. Although the earlier

solubility determinations were insufficient to decide this point

conclusively, more recent investigation has proved beyond doubt that the

curve is continuous and exhibits no break.[226]

{148}

Although in taking up the discussion of the equilibria between calcium

chloride and water, it was desired especially to call attention to the form

of the solubility curve in the case of salt hydrates possessing a definite

melting point, nevertheless, for the sake of completeness, brief mention

may be made of the other systems which these two components can form.

[Illustration: FIG. 38.]

Besides the hexahydrate, the solubility curve of which has already been

described, calcium chloride can also crystallize in two different forms,

each of which contains four molecules {149} of water of crystallization;

these are distinguished as [alpha]-tetrahydrate, and [beta]-tetrahydrate.

Two other hydrates are also known, viz. a dihydrate and a monohydrate. The

solubility curves of these different hydrates are given in Fig. 38.

On following the solubility curve of the hexahydrate from the ordinary

temperature upwards, it is seen that at a temperature of 29.8deg

represented by the point H, it cuts the solubility curve of the

[alpha]-tetrahydrate. This point is therefore a quadruple point at which

the four phases hexahydrate, [alpha]-tetrahydrate, solution, and vapour can

coexist. It is also the transition point for these two hydrates. Since, at

temperatures above 29.8deg, the [alpha]-tetrahydrate is the stable form, it

is evident from the data given before (p. 146), as also from Fig. 38, that

the portion of the solubility curve of the hexahydrate lying above this

temperature represents _metastable_ equilibria. The realization of the

metastable melting point of the hexahydrate is, therefore, due to suspended

transformation. At the transition point, 29.8deg, the solubility of the

hexahydrate and [alpha]-tetrahydrate is 100.6 parts of CaCl_{2} in 100

parts of water.

The retroflex portion of the solubility curve of the hexahydrate extends to

only 1deg below the melting point of the hydrate. At 29.2deg crystals of a

new hydrate, [beta]-tetrahydrate, separate out, and the solution, which now

contains 112.8 parts of CaCl_{2} to 100 parts of water, is saturated with

respect to the two hydrates. Throughout its whole extent the solubility

curve EDF of the [beta]-tetrahydrate represents metastable equilibria. The

upper limit of the solubility curve of [beta]-tetrahydrate is reached at

38.4deg (F), the point of intersection with the curve for the dihydrate.

Above 29.8deg the stable hydrate is the [alpha]-tetrahydrate; and its

solubility curve extends to 45.3deg (K), at which temperature it cuts the

solubility curve of the dihydrate. The curve of the latter hydrate extends

to 175.5deg (L), and is then succeeded by the curve for the monohydrate.

The solubility curve of the anhydrous salt does not begin until a

temperature of about 260deg. The whole diagram, therefore, shows a

succession of stable hydrates, a metastable hydrate, a metastable melting

point and retroflex solubility curve. {150}

Pressure-Temperature Diagram.--The complete study of the equilibria between

the two components calcium chloride and water would require the discussion

of the vapour pressure of the different systems, and its variation with the

temperature. For our present purpose, however, such a discussion would not

be of great value, and will therefore be omitted here; in general, the same

relationships would be found as in the case of sodium sulphate (p. 138),

except that the rounded portion of the solubility curve of the hexahydrate

would be represented by a similar rounded portion in the pressure

curve.[227] As in the case of sodium sulphate, the transition points of the

different hydrates would be indicated by breaks in the curve of pressures.

Finally, mention may again be made of the difference of the pressure of

dissociation of the hexahydrate according as it becomes dehydrated to the

[alpha]- or the [beta]-tetrahydrate (p. 88).

The Indifferent Point.--We have already seen that at 30.2deg calcium

chloride hexahydrate melts congruently, and that, provided the pressure is

maintained constant, addition or withdrawal of heat will cause the complete

liquefaction or solidification, without the temperature of the system

undergoing change. This behaviour, therefore, is similar to, but is not

quite the same as the fusion of a simple substance such as ice; and the

difference is due to the fact that in the case of the hexahydrate the

emission of vapour by the liquid phase causes an alteration in the

composition of the latter, owing to the non-volatility of the calcium

chloride; whereas in the case of ice this is, of course, not so.

Consider, however, for the present that the vapour phase is absent, and

that we are dealing with the two-phase system solid--solution. Then, since

there are two components, the system is bivariant. For any given value of

the pressure, therefore, we should expect that the system could exist at

different temperatures; which, indeed, is the case. It has, however,

already been noted that when the composition of the liquid phase becomes

the same as that of the solid, the system then behaves as a _univariant_

system; for, at a given pressure, the system solid--solution can exist only

at _one_ temperature, change of temperature producing complete

transformation in {151} one or other direction. _The variability of the

system has therefore been diminished._

This behaviour will perhaps be more clearly understood when one reflects

that since the composition of the two phases is the same, the system may be

regarded as being formed of _one component_, just as the system NH_{4}Cl

<--> NH_{3} + HCl was regarded as being composed of one component when the

vapour had the same total composition as the solid (p. 13). One component

in two phases, however, constitutes a univariant system, and we can

therefore see that calcium chloride hexahydrate in contact with solution of

the same composition will constitute a univariant system. The temperature

of equilibrium will, however, vary with the pressure;[228] if the latter is

constant, the temperature will also be constant.

A point such as has just been referred to, which represents the special

behaviour of a system of two (or more) components, in which the composition

of two phases becomes identical, is known as an _indifferent point_,[229]

and it has been shown[230] that at a given pressure the temperature in the

indifferent point is the _maximum_ or _minimum_ temperature possible at the

particular pressure[231] (cf. critical solution temperature). At such a

point a system loses one degree of freedom, or behaves like a system of the

next lower order.

The Hydrates of Ferric Chloride.--A better illustration of the formation of

compounds possessing a definite melting point, and of the existence of

retroflex solubility curves, is afforded by the hydrates of ferric

chloride, which not only possess definite points of fusion, but these

melting points are stable. A very brief description of the relations met

with will suffice.[232]

{152}

Ferric chloride can form no less than four stable hydrates, viz.

Fe_{2}Cl_{6},12H_{2}O, Fe_{2}Cl_{6},7H_{2}O, Fe_{2}Cl_{6},5H_{2}O, and

Fe_{2}Cl_{6},4H_{2}O, and each of these hydrates possesses a definite,

stable melting point. On analogy with the behaviour of calcium chloride,

therefore, we shall expect that the solubility curves of these different

hydrates will exhibit a series of _temperature maxima_; the points of

maximum temperature representing systems in which the composition of the

solid and liquid phases is the same. A graphical representation of the

solubility relations is given in Fig. 39, and the composition of the

different saturated solutions which can be formed is given in the following

tables, the composition being expressed in molecules of Fe_{2}Cl_{6} to 100

molecules of water. The figures printed in thick type refer to transition

and melting points.

[Illustration: FIG. 39.]

{153}

COMPOSITION OF THE SATURATED SOLUTIONS OF FERRIC CHLORIDE AND ITS

HYDRATES.

(_The name placed at the head of each table is the solid phase._)

ICE.

---------------------------

Temperature. | Composition.

---------------------------

+/--55deg | +/-2.75

-40deg | 2.37

-27.5deg | 1.90

-20.5deg | 1.64

-10deg | 1.00

0deg | 0

---------------------------

Fe_{2}Cl_{6},12H_{2}O.

---------------------------

Temperature. | Composition.

---------------------------

-55deg | +/-2.75

-41deg | 2.81

-27deg | 2.98

0deg | 4.13

10deg | 4.54

20deg | 5.10

30deg | 5.93

35deg | 6.78

36.5deg | 7.93

37deg | 8.33

36deg | 9.29

33deg | 10.45

30deg | 11.20

27.4deg | 12.15

20deg | 12.83

10deg | 13.20

8deg | 13.70

---------------------------

Fe_{2}Cl_{6},7H_{2}O.

---------------------------

Temperature. | Composition.

---------------------------

20deg | 11.35

27.4deg | 12.15

32deg | 13.55

32.5deg | 14.29

30deg | 15.12

25deg | 15.54

---------------------------

Fe_{2}Cl_{6},5H_{2}O.

---------------------------

Temperature. | Composition.

---------------------------

20deg | 11.35

12deg | 12.87

20deg | 13.95

27deg | 14.85

30deg | 15.12

35deg | 15.64

50deg | 17.50

55deg | 19.15

56deg | 20.00

55deg | 20.32

---------------------------

Fe_{2}Cl_{6},4H_{2}O

---------------------------

Temperature. | Composition.

---------------------------

20deg | 11.35

50deg | 19.96

55deg | 20.32

60deg | 20.70

69deg | 21.53

72.5deg | 23.35

73.5deg | 25.00

72.5deg | 26.15

70deg | 27.90

66deg | 29.20

---------------------------

Fe_{2}Cl_{6} (ANHYDROUS).

---------------------------

Temperature. | Composition.

---------------------------

20deg | 11.35

66deg | 29.20

70deg | 29.42

75deg | 28.92

80deg | 29.20

100deg | 29.75

---------------------------

The lowest portion of the curve, AB, represents the equilibria between ice

and solutions containing ferric chloride. It represents, in other words,

the lowering of the fusion point of ice by addition of ferric chloride. At

the point B (-55deg), the cryohydric point (p. 117) is reached, at which

the solution is in equilibrium with ice and ferric chloride dodecahydrate.

As {154} has already been shown, such a point represents an invariant

system; and the liquid phase will, therefore, solidify to a mixture of ice

and hydrate without change of temperature. If heat is added, ice will melt

and the system will pass to the curve BCDN, which is the solubility curve

of the dodecahydrate. At C (37deg), the point of maximum temperature, the

hydrate melts completely. The retroflex portion of this curve can be

followed backwards to a temperature of 8deg, but below 27.4deg (D), the

solutions are supersaturated with respect to the heptahydrate; point D is

the eutectic point for dodecahydrate and heptahydrate. The curve DEF is the

solubility curve of the heptahydrate, E being the melting point, 32.5deg.

On further increasing the quantity of ferric chloride, the temperature of

equilibrium is lowered until at F (30deg) another eutectic point is

reached, at which the heptahydrate and pentahydrate can co-exist with

solution. Then follow the solubility curves for the pentahydrate, the

tetrahydrate, and the anhydrous salt; G (56deg) is the melting point of the

former hydrate, J (73.5deg) the melting point of the latter. H and K, the

points at which the curves intersect, represent eutectic points; the

temperature of the former is 55deg, that of the latter 66deg. The dotted

portions of the curves represent metastable equilibria.

As is seen from the diagram, a remarkable series of solubility curves is

obtained, each passing through a point of maximum temperature, the whole

series of curves forming an undulating "festoon." To the right of the

series of curves the diagram represents unsaturated solutions; to the left,

supersaturated.

If an unsaturated solution, the composition of which is represented by a

point in the field to the right of the solubility curves, is cooled down,

the result obtained will differ according as the composition of the

solution is the same as that of a cryohydric point, or of a melting point,

or has an intermediate value. Thus, if a solution represented by _x__{1} is

cooled down, the composition will remain unchanged as indicated by the

horizontal dotted line, until the point D is reached. At this point,

dodecahydrate and heptahydrate will separate out, and the liquid will

ultimately solidify completely to a mixture or "conglomerate" of these two

hydrates; the temperature of {155} the system remaining constant until

complete solidification has taken place. If, on the other hand, a solution

of the composition _x__{3} is cooled down, ferric chloride dodecahydrate

will be formed when the temperature has fallen to that represented by C,

and the solution will completely solidify, without alteration of

temperature, with formation of this hydrate. In both these cases,

therefore, a point is reached at which complete solidification occurs

without change of temperature.

Somewhat different, however, is the result when the solution has an

intermediate composition, as represented by _x__{2} or _x__{4}. In the

former case the dodecahydrate will first of all separate out, but on

further withdrawal of heat the temperature will fall, the solution will

become relatively richer in ferric chloride, owing to separation of the

hydrate, and ultimately the eutectic point D will be reached, at which

complete solidification will occur. Similarly with the second solution.

Ferric chloride dodecahydrate will first be formed, and the temperature

will gradually fall, the composition of the solution following the curve CB

until the cryohydric point B is reached, when the whole will solidify to a

conglomerate of ice and dodecahydrate.

Suspended Transformation.--Not only can the upper branch of the solubility

curve of the dodecahydrate be followed backwards to a temperature of 8deg,

or about 19deg below the temperature of transition to the heptahydrate; but

suspended transformation has also been observed in the case of the

heptahydrate and the pentahydrate. To such an extent is this the case that

the solubility curve of the latter hydrate has been followed downwards to

its point of intersection with the curve for the dodecahydrate. This point

of intersection, represented in Fig. 39 by M, lies at a temperature of

about 15deg; and at this temperature, therefore, it is possible for the two

solid phases dodecahydrate and pentahydrate to coexist, so that M is a

eutectic point for the dodecahydrate and the pentahydrate. It is, however,

a metastable eutectic point, for it lies in the region of supersaturation

with respect to the heptahydrate; and it can be realized only because of

the fact that the latter hydrate is not readily formed.

Evaporation of Solutions at Constant Temperature.--On {156} evaporating

dilute solutions of ferric chloride at constant temperature, a remarkable

series of changes is observed, which, however, will be understood with the

help of Fig. 40. Suppose an unsaturated solution, the composition of which

is represented by the point _x__{1}, is evaporated at a temperature of

about 17deg - 18deg. As water passes off, the composition of the solution

will follow the dotted line of constant temperature, until at the point

where it cuts the curve BC the solid hydrate Fe_{2}Cl_{6},12H_{2}O

separates out. As water continues to be removed, the hydrate must be

deposited (in order that the solution shall remain saturated), until

finally the solution dries up to the hydrate. As dehydration proceeds, the

heptahydrate can be formed, and the dodecahydrate will finally pass into

the heptahydrate; and this, in turn, into the pentahydrate.

[Illustration: FIG. 40.]

But the heptahydrate is not always formed by the dehydration of the

dodecahydrate, and the behaviour on evaporation is therefore somewhat

perplexing at first sight. After the solution has dried to the

dodecahydrate, as explained above, further removal of water causes

liquefaction, and the system is now represented by the point of

intersection at _a_; at this point the solid hydrate is in equilibrium with

a solution containing relatively more ferric chloride. If, therefore,

evaporation is continued, the solid hydrate must _pass into solution_ in

order that the composition of the latter may remain unchanged, so that

ultimately a liquid will again be obtained. A very slight further

dehydration will bring the solution into the state represented by _b_, at

which the pentahydrate is formed, and the solution will at last disappear

and leave this hydrate alone.

Without the information to be obtained from the curves in Figs. 39 and 40,

the phenomena which would be observed on carrying out the evaporation at a

temperature of about 31 - 32deg {157} would be still more bewildering. The

composition of the different solutions formed will be represented by the

perpendicular line _x__{2}12345. Evaporation will first cause the

separation of the dodecahydrate, and then total disappearance of the liquid

phase. Then liquefaction will occur, and the system will now be represented

by the point 2, in which condition it will remain until the solid hydrate

has disappeared. Following this there will be deposition of the

heptahydrate (point 3), with subsequent disappearance of the liquid phase.

Further dehydration will again cause liquefaction, when the concentration

of the solution will be represented by the point 4; the heptahydrate will

ultimately disappear, and then will ensue the deposition of the

pentahydrate, and complete solidification will result. On evaporating a

solution, therefore, of the composition _x__{2}, the following series of

phenomena will be observed: solidification to dodecahydrate; liquefaction;

solidification to heptahydrate; liquefaction; solidification to

pentahydrate.[233]

Although ferric chloride and water form the largest and best-studied series

of hydrates possessing definite melting points, examples of similar

hydrates are not few in number; and more careful investigation is

constantly adding to the list.[234] In all these cases the solubility curve

will show a point of maximum temperature, at which the hydrate melts, and

will end, above and below, in a cryohydric point. Conversely, if such a

curve is found in a system of two components, we can argue that a definite

compound of the components possessing a definite melting point is formed.

Inevaporable Solutions.--If a saturated solution in contact with two

hydrates, or with a hydrate and anhydrous salt is heated, the temperature

and composition of the solution will, of course, remain unchanged so long

as the two solid phases are present, for such a system is invariant. In

addition to this, however, the _quantity_ of the solution will also remain

unchanged, the water which evaporates being supplied by the higher hydrate.

The same phenomenon is also observed in the case of cryohydric points when

ice is a solid phase; so long as the latter is present, evaporation will be

accompanied {158} by fusion of the ice, and the quantity of solution will

remain constant. Such solutions are called _inevaporable_.[235]

[Illustration: FIG. 41.]

Illustration.--In order to illustrate the application of the principles of

the Phase Rule to the study of systems formed by a volatile and a

non-volatile component, a brief description may be given of the behaviour

of sulphur dioxide and potassium iodide, which has formed the subject of a

recent investigation. After it had been found[236] that liquid sulphur

dioxide has the property of dissolving potassium iodide, and that the

solutions thus obtained present certain peculiarities of behaviour, the

question arose as to whether or not compounds are formed between the

sulphur dioxide and the potassium iodide, and if so, what these compounds

are. To find an answer to this question, Walden and Centnerszwer[237] made

a complete investigation of the solubility curves (equilibrium curves) of

these two components, the investigation extending from the freezing point

to the critical point of sulphur dioxide. For convenience of reference, the

results which they obtained are represented diagrammatically in Fig. 41.

The freezing point (A) of pure sulphur dioxide was found to be -72.7deg.

Addition of potassium iodide lowered the freezing point, but the maximum

depression obtained was very small, and was reached when the concentration

of the potassium iodide in the solution was only 0.336 mols. per cent.

Beyond this point, an increase in the concentration of the iodide was

accompanied by an elevation of the freezing point, the change of the

freezing point with the concentration being represented by the curve BC.

The solid {159} which separated from the solutions represented by BC was a

bright _yellow_ crystalline substance. At the point C (-23.4deg) a

temperature-maximum was reached; and as the concentration of the potassium

iodide was continuously increased, the temperature of equilibrium first

fell and then slowly rose, until at +0.26deg (E) a second

temperature-maximum was registered. On passing the point D, the solid which

was deposited from the solution was a _red_ crystalline substance. On

withdrawing sulphur dioxide from the system, the solution became turbid,

and the temperature remained constant. The investigation was not pursued

farther at this point, the attention being then directed to the equilibria

at higher temperatures.

When a solution of potassium iodide in liquid sulphur dioxide containing

1.49 per cent. of potassium iodide was heated, solid (potassium iodide) was

deposited at a temperature of 96.4deg. Solutions containing more than about

3 per cent. of the iodide separated, on being heated, into two layers, and

the temperature at which the liquid became heterogeneous fell as the

concentration was increased; a temperature-minimum being obtained with

solutions containing 12 per cent. of potassium iodide. On the other hand,

solutions containing 30.9 per cent. of the iodide, on being heated,

deposited potassium iodide; while a solution containing 24.5 per cent. of

the salt first separated into two layers at 89.3deg, and then, on cooling,

solid was deposited and one of the liquid layers disappeared.

Such are, in brief, the results of experiment; their interpretation in the

light of the Phase Rule is the following:--

The curve AB is the freezing-point curve of solid sulphur dioxide in

contact with solutions of potassium iodide. BCD is the solubility curve of

the yellow crystalline solid which is deposited from the solutions. C, the

temperature-maximum, is the melting point of this _yellow_ solid, and the

composition of the latter must be the same as that of the solution at this

point (p. 145), which was found to be that represented by the formula

KI,14SO_{2}. B is therefore the eutectic point, at which solid sulphur

dioxide and the compound KI,14SO_{2} can exist together in equilibrium with

solution and vapour. The curve DE is the solubility curve of the _red_

crystalline solid, and the {160} point E, at which the composition of

solution and solid is the same, is the melting point of the solid. The

composition of this substance was found to be KI,4SO_{2}.[238] D is,

therefore, the eutectic point at which the compounds KI,14SO_{2} and

KI,4SO_{2} can coexist in equilibrium with solution and vapour. The curve

DE does not exhibit a retroflex portion; on the contrary, on attempting to

obtain more concentrated solutions in equilibrium with the compound

KI,4SO_{2}, a new solid phase (probably potassium iodide) was formed. Since

at this point there are four phases in equilibrium, viz. the compound

KI,4SO_{2}, potassium iodide, solution, and vapour, the system is

invariant. E is, therefore, the _transition point_ for KI,4SO_{2} and KI.

Passing to higher temperatures, FG is the solubility curve of potassium

iodide in sulphur dioxide; at G two liquid phases are formed, and the

system therefore becomes invariant (cf. p. 121). The curve GHK is the

solubility curve for two partially miscible liquids; and since complete

miscibility occurs on _lowering_ the temperature, the curve is similar to

that obtained with triethylamine and water (p. 101). K is also an invariant

point at which potassium iodide is in equilibrium with two liquid phases

and vapour.

The complete investigation of the equilibria between sulphur dioxide and

potassium iodide, therefore, shows that these two components form the

compounds KI,14SO_{2} and KI,4SO_{2}; and that when solutions having a

concentration between those represented by the points G and K are heated,

separation into two layers occurs. The temperatures and concentrations of

the different characteristic points are as follows:--

-------------------------------------------------------------

| | Composition of

Point. | Temperature. | the solution

| | per cent. KI.

-------------------------------------------------------------

A (m.p. of SO_{2}) | -72.7deg | --

B (eutectic point) | -- | 0.86

C (m.p. of KI,14SO_{2}) | -23.4deg | 17.63

E (m.p. of KI,4SO_{2}) | +0.26deg| 39.33

G (KI + two liquid phases) |(about) 88deg | 24.0

H (critical solution point) | 77.3deg | 12

K (KI + two liquid phases) |(about) 88deg | 2.7

-------------------------------------------------------------

* * * * *

{161}

CHAPTER IX

EQUILIBRIA BETWEEN TWO VOLATILE COMPONENTS

General.--In the two preceding chapters certain restrictions were imposed

on the discussion of the equilibria between two components; but in the

present chapter the restriction that only one of the components is volatile

will be allowed to fall, and the general behaviour of two volatile[239]

components, each of which is capable of forming a liquid solution with the

other, will be studied. As we shall see, however, the removal of the

previous restriction produces no alteration in the general aspect of the

equilibrium curves for concentration and temperature, but changes to some

extent the appearance of the pressure-temperature diagram. The latter would

become still more complicated if account were taken not only of the total

pressure but also of the partial pressures of the two components in the

vapour phase; this complication, however, will not be introduced in the

present discussion.[240] In this chapter we shall consider the systems

formed by the two components iodine and chlorine, and sulphur dioxide and

water.

Iodine and Chlorine.--The different systems furnished by iodine and

chlorine, rendered classical by the studies of Stortenbeker,[241] form a

very complete example of equilibria in a two-component system. We shall

first of all consider the {162} relations between concentration and

temperature, with the help of the accompanying diagram, Fig. 42.

[Illustration: FIG. 42.]

Concentration-Temperature Diagram.--In this diagram the temperatures are

taken as the abscissae, and the composition of the solution, expressed in

atoms of chlorine to one atom of iodine,[242] is represented by the

ordinates. In the diagram, A represents the melting point of pure iodine,

114deg. If chlorine is added to the system, a solution of chlorine in

liquid iodine is obtained, and the temperature at which solid iodine is in

equilibrium with the liquid solution will be all the lower the greater the

concentration of the chlorine. We therefore obtain the curve ABF, which

represents the composition of the solution {163} with which solid iodine is

in equilibrium at different temperatures. This curve can be followed down

to 0deg, but at temperatures below 7.9deg (B) it represents metastable

equilibria. At B iodine monochloride can be formed, and if present the

system becomes invariant; B is therefore a quadruple point at which the

four phases, iodine, iodine monochloride, solution, and vapour, can

coexist. Continued withdrawal of heat at this point will therefore lead to

the complete solidification of the solution to a mixture or conglomerate of

iodine and iodine monochloride, while the temperature remains constant

during the process. B is the eutectic point for iodine and iodine

monochloride.

Just as we found in the case of aqueous salt solutions that at temperatures

above the cryohydric or eutectic point, two different solutions could

exist, one in equilibrium with ice, the other in equilibrium with the salt

(or salt hydrate), so in the case of iodine and chlorine there can be two

solutions above the eutectic point B, one containing a lower proportion of

chlorine in equilibrium with iodine, the other containing a higher

proportion of chlorine in equilibrium with iodine monochloride. The

composition of the latter solution is represented by the curve BCD. As the

concentration of chlorine is increased, the temperature at which there is

equilibrium between iodine monochloride and solution rises until a point is

reached at which the composition of the solution is the same as that of the

solid. At this point (C), iodine monochloride melts. Addition of one of the

components will lower the temperature of fusion, and a continuous

curve,[243] exhibiting a retroflex portion as in the case of

CaCl_{2},6H_{2}O, will be obtained. At temperatures below its melting

point, therefore, iodine monochloride can be in equilibrium with two

different solutions.

The upper portion of this curve, CD, can be followed downwards to a

temperature of 22.7deg. At this temperature iodine trichloride can separate

out, and a second quadruple {164} point (D) is obtained. This is the

eutectic point for iodine monochloride and iodine trichloride.

By addition of heat and increase in the amount of chlorine, the iodine

monochloride disappears, and the system passes along the curve DE, which

represents the composition of the solutions in equilibrium with solid

iodine trichloride. The concentration of chlorine in the solution increases

as the temperature is raised, until at the point E, where the solution has

the same composition as the solid, the maximum temperature is reached; the

iodine trichloride melts. On increasing still further the concentration of

chlorine in the solution, the temperature of equilibrium falls, and a

continuous curve, similar to that for the monochloride, is obtained. The

upper branch of this curve has been followed down to a temperature of

30deg, the solution at this point containing 99.6 per cent. of

chlorine.[244] The very rounded form of the curve is due to the trichloride

being largely dissociated in the liquid state.

One curve still remains to be considered. As has already been mentioned,

iodine monochloride can exist in two crystalline forms, only one of which,

however, is stable at temperatures below the melting point; the two forms

are _monotropic_ (p. 44). The stable form which melts at 27.2deg, is called

the [alpha]-form, while the less stable variety, melting at 13.9deg, is

known as the [beta]-form. If, now, the presence of [alpha]-ICl is excluded,

it is possible to obtain the [beta]-form, and to study the conditions of

equilibrium between it and solutions of iodine and chlorine, from the

eutectic point F to the melting point G. As the [beta]-ICl becomes less

stable in presence of excess of chlorine, it has not been possible to study

the retroflex portion of the curve represented by the dotted continuation

of FG.

The following table gives some of the numerical data from which Fig. 42 was

constructed.[245]

{165}

IODINE AND CHLORINE.

I. _Invariant systems._

-------------------------------------------------------------------------

| | Phases present.

Temper-| Pressure.+--------------------+-----------------+--------------

ature. | | Solid. | Liquid. | Vapour.

--------+----------+--------------------+-----------------+--------------

7.9deg | 11 mm. | I_{2},[alpha]-ICl | I[wavy]Cl_{0.66}| I + Cl_{0.92}

0.9deg | -- | I_{2},[beta]-ICl | I[wavy]Cl_{0.72}| --

22.7deg | 42 mm. | [alpha]-ICl,ICl_{3}| I[wavy]Cl_{1.19}| I + Cl_{1.75}

[-102deg| <1 atm. | ICl_{3},Cl_{2} | I[wavy]Cl_{m} | I + Cl_{n}]

--------+----------+--------------------+-----------------+--------------

II. _Melting points._

A. Iodine,[246] 114.15deg (pressure 89.8 mm.).

C. [alpha]-Iodine monochloride, 27.2deg (pressure 37 mm.).

E. Iodine trichloride, 101deg (pressure 16 atm.).

G. [beta]-Iodine monochloride, 13.9deg.

Since the vapour pressure at the melting point of iodine trichloride

amounts to 16 atm., the experiments must of course be carried out

in closed vessels. At 63.7deg the vapour pressure of the system

trichloride--solution--vapour is equal to 1 atm.

Pressure-Temperature Diagram.--In this diagram there are represented the

values of the vapour pressure of the saturated solutions of chlorine and

iodine. To give a complete picture of the relations between pressure,

temperature, and concentration, a solid model would be required, with three

axes at right angles to one another along which could be measured the

values of pressure, temperature, and concentration of the components in the

solution. Instead of this, however, there may be employed the accompanying

projection figure[247] (Fig. 43), the lower portion of which shows the

projection of the equilibrium curve on the surface containing the

concentration and temperature axes, while the upper portion is the

projection on the plane containing the pressure and temperature axes. The

lower portion is therefore a concentration-temperature diagram; {166} the

upper portion, a pressure-temperature diagram. The corresponding points of

the two diagrams are joined by dotted lines.

[Illustration: FIG. 43.]

Corresponding to the point C, the melting point of pure iodine, there is

the point C_{1}, which represents the vapour pressure of iodine at its

melting point. At this point three curves cut: 1, the sublimation curve of

iodine; 2, the vaporization curve of fused iodine; 3, C_{1}B_{1}, the

vapour-pressure curve of the saturated solutions in equilibrium with solid

iodine. Starting, therefore, with the system solid iodine--liquid iodine,

addition of chlorine will cause the temperature of equilibrium to fall

continuously, while the vapour pressure will first increase, pass through a

maximum and then fall continuously {167} until the eutectic point, B

(B_{1}), is reached.[248] At this point the system is invariant, and the

pressure will therefore remain constant until all the iodine has

disappeared. As the concentration of the chlorine increases in the manner

represented by the curve B_f_H, the pressure of the vapour also increases

as represented by the curve B_{1}_f__{1}H_{1}. At H_{1}, the eutectic point

for iodine monochloride and iodine trichloride, the pressure again remains

constant until all the monochloride has disappeared. As the concentration

of the solution passes along the curve HF, the pressure of the vapour

increases as represented by the curve H_{1}F_{1}; F_{1} represents the

pressure of the vapour at the melting point of iodine trichloride. If the

concentration of the chlorine in the solution is continuously increased

from this point, the vapour pressure first increases and then decreases,

until the eutectic point for iodine trichloride and solid chlorine is

reached (D_{1}). Curves Cl_{2} solid and Cl_{2} liquid represent the

sublimation and vaporization curves of chlorine, the melting point of

chlorine being -102deg.

Although complete measurements of the vapour pressure of the different

systems of pure iodine to pure chlorine have not been made, the

experimental data are nevertheless sufficient to allow of the general form

of the curves being indicated with certainty.

Bivariant Systems.--To these, only a brief reference need be made. Since

there are two components, two phases will form a bivariant system. The

fields in which these systems can exist are shown in Fig. 43 and Fig. 44,

which is a more diagrammatic representation of a portion of Fig. 43.

I. Iodine--vapour.

II. Solution--vapour.

III. Iodine trichloride--vapour.

IV. Iodine monochloride--vapour.

[Illustration: FIG. 44.]

The conditions for the existence of these systems will probably be best

understood from Fig. 44. Since the curve B'A' {168} represents the

pressures under which the system iodine--solution--vapour can exist,

increase of volume (diminution of pressure) will cause the volatilization

of the solution, and the system iodine--vapour will remain. If, therefore,

we start with a system represented by _a_, diminution of pressure at

constant temperature will lead to the condition represented by _x_. On the

other hand, increase of pressure at _a_ will lead to the condensation of a

portion of the vapour phase. Since, now, the concentration of chlorine in

the vapour is greater than in the solution, condensation of vapour would

increase the concentration of chlorine in the solution; a certain amount of

iodine must therefore pass into solution in order that the composition of

the latter shall remain unchanged.[249] If, therefore, the volume of vapour

be sufficiently great, continued diminution of volume will ultimately lead

to the disappearance of all the iodine, and there will remain only solution

and vapour (field II.). As the diminution of volume is continued, the

vapour pressure and the concentration of the chlorine in the solution will

increase, until when the pressure has reached the value _b_, iodine

monochloride can separate out. The system, therefore, again becomes

univariant, and at constant temperature the pressure and composition of the

phases must remain unchanged. Diminution of volume will therefore not

effect an increase of pressure, but a condensation of the vapour; and since

this is richer in chlorine than the {169} solution, solid iodine

monochloride must separate out in order that the concentration of the

solution remain unchanged.[250] As the result, therefore, we obtain the

bivariant system iodine monochloride--vapour.

A detailed discussion of the effect of a continued increase of pressure

will not be necessary. From what has already been said and with the help of

Fig. 44, it will readily be understood that this will lead successively to

the univariant system (_c_), iodine monochloride--solution--vapour; the

bivariant system solution--vapour (field II.); the univariant system (_d_),

iodine trichloride--solution--vapour; and the bivariant system _x'_, iodine

trichloride--vapour. If the temperature of the experiment is above the

melting point of the monochloride, then the systems in which this compound

occurs will not be formed.

Sulphur Dioxide and Water.--In the case just studied we have seen that the

components can combine to form definite compounds possessing stable melting

points. The curves of equilibrium, therefore, resemble in their general

aspect those of calcium chloride and water, or of ferric chloride and

water. In the case of sulphur dioxide and water, however, the melting point

of the compound formed cannot be realized, because transition to another

system occurs; retroflex concentration-temperature curves are therefore not

found here, but the curves exhibit breaks or sudden changes in direction at

the transition points, as in the case of the systems formed by sodium

sulphate and water. The case of sulphur dioxide and water is also of

interest from the fact that two liquid phases can be formed.

The phases which occur are--Solid: ice, sulphur dioxide hydrate,

SO_{2},7H_{2}O. Liquid: two solutions, the one containing excess of sulphur

dioxide, the other excess of water, and represented by the symbols SO_{2}

[wavy] _x_H_{2}O (solution I.), and H_{2}O [wavy] _y_SO_{2} (solution II.).

Vapour: a mixture of sulphur dioxide and water vapour in varying

proportions. Since there are two components, sulphur dioxide and water, the

number of {170} possible systems is considerable. Only the following,

however, have been studied:--

I. _Invariant Systems: Four co-existing phases._

(_a_) Ice, hydrate, solution, vapour.

(_b_) Hydrate, solution I., solution II., vapour.

II. _Univariant Systems: Three co-existing phases._

(_a_) Hydrate, solution I., vapour.

(_b_) Hydrate, solution II., vapour.

(_c_) Solution I., solution II., vapour.

(_d_) Hydrate, solution I., solution II.

(_e_) Hydrate, ice, vapour.

(_f_) Ice, solution II., vapour.

(_g_) Ice, hydrate, solution II.

III. _Bivariant Systems: Two co-existing phases._

(_a_) Hydrate, solution I.

(_b_) Hydrate, solution II.

(_c_) Hydrate, vapour.

(_d_) Hydrate, ice.

(_e_) Solution I., solution II.

(_f_) Solution I., vapour.

(_g_) Solution I., ice.

(_h_) Solution II., vapour.

(_i_) Solution II., ice.

(_j_) Ice, vapour.

[Illustration: FIG. 45.]

Pressure-Temperature Diagram.[251]--If sulphur dioxide is passed into water

at 0deg, a solution will be formed and the temperature at which ice can

exist in equilibrium with this solution will fall more and more as the

concentration of the sulphur dioxide increases. At -2.6deg, however, a

cryohydric point is reached at which solid hydrate separates out,

and the system becomes invariant. The curve AB (Fig. 45) therefore

represents the pressure of the system ice--solution II.--vapour, and B

represents the temperature and pressure at which the invariant system

ice--hydrate--solution II.--vapour can exist. At this point the temperature

is -2.6deg, and the pressure 21.1 cm. If heat is withdrawn from this

system, the solution will ultimately {171} solidify to a mixture of

ice and hydrate, and there will be obtained the univariant system

ice--hydrate--vapour. The vapour pressure of this system has been

determined down to a temperature of -9.5deg, at which temperature the

pressure amounts to 15 cm. The pressures for this system are represented by

the curve BC. If at the point B the volume is diminished, the pressure must

remain constant, but the relative amounts of the different phases will

undergo change. If suitable quantities of these are present, diminution of

volume will ultimately lead to the total condensation of the vapour phase,

and there will remain the univariant system ice--hydrate--solution. The

temperature of equilibrium of this system will alter with the pressure,

but, as in the case of the melting point of a simple substance, great

differences of pressure will cause only comparatively small changes in the

temperature of equilibrium. The change of the cryohydric point with the

pressure is represented by the line BE; the actual values have not been

determined, but the curve must slope towards the pressure axis because

fusion is accompanied by diminution of volume, as in the case of pure ice.

{172}

A fourth univariant system can be formed at B. This is the system

hydrate--solution II.--vapour. The conditions for the existence of

this system are represented by the curve BF, which may therefore be

regarded as the vapour-pressure curve of the saturated solution of

sulphur dioxide heptahydrate in water. Unlike the curve for iodine

trichloride--solution--vapour, this curve cannot be followed to the melting

point of the hydrate. Before this point is reached, a second liquid phase

appears, and an invariant system consisting of hydrate--solution

I.--solution II.--vapour is formed. We have here, therefore, the phenomenon

of melting under the solution as in the case of succinic nitrile and water

(p. 122). This point is represented in the diagram by F; the temperature at

this point is 12.1deg, and the pressure 177.3 cm. The range of stable

existence of the hydrate is therefore from -2.6deg to 12.1deg;

nevertheless, the curve FB has been followed down to a temperature of

-6deg, at which point ice formed spontaneously.

So long as the four phases hydrate, two liquid phases, and vapour are

present, the condition of the system is perfectly defined. By altering the

conditions, however, one of the phases can be made to disappear, and a

univariant system will then be obtained. Thus, if the vapour phase is made

to disappear, the univariant system solution I.--solution II.--hydrate,

will be left, and the temperature at which this system is in equilibrium

will vary with the pressure. This is represented by the curve FI; under a

pressure of 225 atm. the temperature of equilibrium is 17.1deg. Increase of

pressure, therefore, raises the temperature at which the three phases can

coexist.

Again, addition of heat to the invariant system at F will cause the

disappearance of the solid phase, and there will be formed the univariant

system solution I.--solution II.--vapour. In the case of this system the

vapour pressure increases as the temperature rises, as represented by the

curve FG. Such a system is analogous to the case of ether and water, or

other two partially miscible liquids (p. 103). As the temperature changes,

the composition of the two liquid phases will undergo change; but this

system has not been studied fully.

The fourth curve, which ends at the quadruple point F, is {173} that

representing the vapour pressure of the system hydrate--solution I.--vapour

(FH). This curve has been followed to a temperature of 0deg, the pressure

at this point being 113 cm. The metastable prolongation of GF has also been

determined. Although, theoretically, this curve must lie below FH, it was

found that the difference in the pressure for the two curves was within the

error of experiment.

Bivariant Systems.--The different bivariant systems, consisting of two

phases, which can exist within the range of temperature and pressure

included in Fig. 45, were given on p. 170. The conditions under which these

systems can exist are represented by the areas in the diagram, and the

fields of the different bivariant systems are indicated by letters,

corresponding to the letters on p. 170. Just as in the case of

one-component systems (p. 29), we found that the field lying between any

two curves gave the conditions of existence of that phase which was common

to the two curves, so also in the case of two-component systems, a

bivariant two-phase system occurs in the field enclosed[252] by the two

curves to which the two phases are common. As can be seen, the same

bivariant system can occur in more than one field.

As is evident from Fig. 45, three different bivariant systems are capable

of existing in the area HFI; which of these will be obtained will depend on

the relative masses of the different phases in the univariant or invariant

system. Thus, starting with a system represented by a point on the curve

HF, diminution of volume at constant temperature will cause the

condensation of a portion of the vapour, which is rich in sulphur dioxide;

since this would increase the concentration of sulphur dioxide in the

solution, it must be counteracted by the passage of a portion of the

hydrate (which is relatively poor in sulphur dioxide) into the solution.

If, therefore, the amount of hydrate present is relatively very small, the

final result of the compression will be the production of the system _f_,

solution I.--vapour. On the other hand, if the vapour is present in

relatively small amount, it will be the first phase to disappear, {174} and

the bivariant system _a_, hydrate--solution I., will be obtained. Finally,

if we start with the invariant system at F, compression will cause the

condensation of vapour, while the composition of the two solutions will

remain unchanged. When all the vapour has disappeared, the univariant

system hydrate--solution I.--solution II. will be left. If, now, the

pressure is still further increased, while the temperature is kept below

12deg, more and more hydrate must be formed at the expense of the two

liquid phases (because 12deg is the lower limit for the coexistence of the

two liquid phases), and if the amount of the solution I. (containing excess

of sulphur dioxide) is relatively small, it will disappear before solution

II., and there will be obtained the bivariant system hydrate--solution II.

(bivariant system _b_).

In a similar manner, account can be taken of the formation of the other

bivariant systems.

A behaviour similar to that of sulphur dioxide and water is shown by

chlorine and water and by bromine and water, although these have not been

so fully studied.[253] In the case of hydrogen bromide and water, and of

hydrogen chloride and water, a hydrate, viz. HBr,2H_{2}O and HCl,2H_{2}O,

is formed which possesses a definite melting point, as in the case of

iodine trichloride. In these cases, therefore, a retroflex curve is

obtained. Further, just as in the case of the chlorides of iodine the upper

branch of the retroflex curve ended in a eutectic point, so also in the

case of the hydrate HBr,2H_{2}O the upper branch of the curve ends in a

eutectic point at which the system dihydrate--monohydrate--solution--vapour

can exist. Before the melting point of the monohydrate is reached, two

liquid phases are formed, as in the case of sulphur dioxide and water.

* * * * *

{175}

CHAPTER X

SOLID SOLUTIONS. MIXED CRYSTALS

General.--With the conception of gaseous and liquid solutions, every one is

familiar. Gases can mix in all proportions to form homogeneous solutions.

Gases can dissolve in or be "absorbed" by liquids; and solids, also, when

brought in contact with liquids, "pass into solution" and yield a

homogeneous liquid phase. On the other hand, the conception of a _solid

solution_ is one which in many cases is found more difficult to appreciate;

and the existence and behaviour of solid solutions, in spite of their not

uncommon occurrence and importance, are in general comparatively little

known.

The reason of this is to be found, to some extent, no doubt, in the fact

that the term "solid solution" was introduced at a comparatively recent

date,[254] but it is probably also due in some measure to a somewhat hazy

comprehension of the definition of the term "solution" itself. As has

already been said (p. 92), a solution is a homogeneous phase, the

composition of which can vary continuously within certain limits; the

definition involves, therefore, no condition as to the physical state of

the substances. Accordingly, solid solutions are homogeneous solid phases,

the composition of which can undergo continuous variation within certain

limits. Just as we saw that the range of variation of composition is more

limited in the case of liquids than in the case of gases, so also we find

that the limits of miscibility are in general still more restricted in the

case of solids. Examples of complete miscibility are, however, not unknown

even in the case of solid substances.

Solid solutions have long been known, although, of course, {176} they were

not defined as such. Thus, the phenomena of "occlusion" of gases by metals

and other substances (occlusion of hydrogen by palladium; occlusion of

hydrogen by iron) are due to the formation of solid solutions. The same is

probably also true of the phenomena of "adsorption," as in the removal of

organic colouring matter by charcoal, although, in this case, surface

tension no doubt plays a considerable part.[255]

As examples of the solution of gases in solids there may be cited (in

addition to the phenomena of occlusion already mentioned), the hydrated

silicates and the zeolites. During dehydration these crystalline substances

remain clear and transparent, and the pressure of the water vapour which

they emit varies with the degree of hydration or the concentration of water

in the mineral.[256] As examples of the solution of solids in solids we

have the cementation of iron by charcoal, the formation of glass, and the

crystallization together of isomorphous substances.

Although we have here spoken of the glasses as "solid solutions," it should

be mentioned that the term "solid" is used in its popular sense. Strictly

speaking, the glasses are to be regarded as supercooled liquids (see also

p. 53, footnote).

In discussing the equilibria in systems containing a solid solution, it is

of essential importance to remember that a solid solution constitutes only

_one_ phase, a phase of varying composition, as in the case of liquid

solutions.

Solution of Gases in Solids.--Comparatively little work has been done in

this connection, the investigations being limited chiefly to the phenomena

of occlusion or adsorption of gases by charcoal.[257] We shall, therefore,

indicate only briefly {177} and in a general manner, the behaviour which

the Phase Rule enables us to foresee.[258]

In dealing with the systems formed by the two phases gas--solid, three

chief cases call for mention:--

I. _The gas is not absorbed by the solid, but when the pressure reaches a

certain value, combination of the two components can result._

[Illustration: Fig. 46.]

The graphic representation of such a system is shown in Fig. 46, the

ordinates being the pressures of the gas, and the abscissae the

concentrations of the gaseous component in the solid phase. Since there is

no formation of a solid solution, the concentration of gas in the solid

phase remains zero until the pressure has increased to the point A. At this

point combination can take place. There will now be three phases present,

viz. solid component, compound, and vapour. The system is therefore

univariant, and if the temperature is maintained constant, the vapour

pressure will be constant, irrespective of the amount of compound formed,

_i.e._ irrespective of the relative amounts of gas and solid. This is

indicated by the line AB. When the solid component has entirely

disappeared, the system ceases to be univariant, and if no absorption

occurs, the pressure will increase again, as shown by BC. If a second

compound can be formed, then a second _pc_-line will be obtained, similar

to the preceding. To this group belong the salt hydrates (Chap. VII.).

II. _The gas may be absorbed and may also form a compound._

If absorption of gas occurs with formation of a solid solution, then, as

the system consists of two phases, solution--vapour, it is bivariant. At

constant temperature, therefore, the pressure will still vary with the

concentration of the gaseous component in the solid phase. This is

represented by the curve AB in Fig. 47. When, however, the pressure has

reached a certain value, combination can take place; and since there are

now three phases present, the system is {178} univariant, and at constant

temperature the pressure is constant, as shown by the line BC.

III. _Absorption of gas occurs, but at a certain concentration the solid

solution can separate into two immiscible solid solutions._

We have seen, in Chapter VI., that two liquids can form two immiscible

solutions, and the same has also been found true of solid solutions, as we

shall presently learn more fully. If, now, two immiscible solutions are

formed, then the system will become univariant, and at constant temperature

the _pc_-curve will be a straight line, as in the case of the formation of

a compound (cf. p. 86). The behaviour of this system will, therefore, also

be represented diagrammatically by Fig. 47.

[Illustration: FIG. 47.]

_Palladium and Hydrogen._--The phenomenon of the absorption of hydrogen by

palladium, to which Graham gave the name "occlusion," is one that has

claimed the attention of several investigators. Although Graham was not of

opinion that a compound is formed, but rather that the gas undergoes very

great condensation, acts as a quasi-metal (to which he gave the name

hydrogenium), and forms a homogeneous alloy with the palladium, later

investigations, especially those of Troost and Hautefeuille,[259] pointed

to the formation of a definite chemical compound, having the formula

Pd_{2}H. This conclusion has, however, not been confirmed by subsequent

investigation.[260]

Roozeboom and Hoitsema[261] sought to arrive at a final decision as to the

nature of the phenomenon by an investigation of the equilibrium between

hydrogen and palladium on the basis of the Phase Rule classification given

above. If a compound is formed, diminution of volume would cause no

increase of pressure, but only an increase in the amount of the compound.

As this is the only case of gas absorption which has been {179} accurately

studied from this point of view, a brief account of the results obtained

will be given here, although these are not so clear and free from ambiguity

as one would desire.

The scientists just mentioned investigated the variation of the pressure of

hydrogen with the amount absorbed by the metal at different temperatures,

and a few of their results, typical of all, are represented graphically in

Fig. 48; the curves indicating the variation of the gas pressure with the

concentration of the hydrogen in the palladium at the temperatures 120deg,

170deg, and 200deg. As can be seen, the curve consists of three parts, an

ascending portion which passes gradually and continuously into an almost

horizontal but slightly ascending middle part, which in turn passes without

break into a second rapidly ascending curve. This, as Fig. 48 indicates, is

the general form of the curve; but the length of the middle portion varies

with the temperature, being shorter at higher than at lower temperatures.

[Illustration: FIG. 48.]

What is the interpretation to be put on these curves? With regard to the

two end portions, these represent bivariant, two-phase systems, consisting

of a solid solution and gas. They correspond, therefore, to curve AB in

Fig. 47. If the middle portion were horizontal, it would indicate either

the formation of a compound or of two immiscible solid solutions. If a

compound Pd_{2}H were formed, then the middle portion would at all

temperatures end at the same value of the concentration, viz. that

corresponding to 0.5 atoms of hydrogen to 1 atom of palladium. As the

figure shows, however, this is not the case; the higher the temperature,

the lower is the concentration at which the middle passes into the terminal

portion of the curve. {180} Such a behaviour would, however, agree with the

assumption of the formation of two solid solutions, the "miscibility" of

which increases with the temperature, as in the case of the liquid

solutions of phenol and water (p. 97). Nevertheless, although the

assumption of the formation of two solid solutions is more satisfactory

than that of the formation of a compound, it does not entirely explain the

facts. If two solid solutions are formed, the pressure curve should be

horizontal, but this is not the case; and the deviation from the horizontal

does not appear to be due to impurities either in the gas or in the metal,

but is apparently a peculiarity of the system. Further, the gradual instead

of abrupt passage of the three portions of the curve into one another

remains unexplained. Hoitsema has expressed the opinion that the occlusion

of hydrogen by palladium is a process of continuous absorption, the

peculiar form of the curve--the flat middle portion--being possibly due to

a condensation of the gas, even at temperatures far above the critical

temperature of liquid hydrogen.

While, therefore, the occlusion of hydrogen by palladium still presents

some unexplained phenomena, the behaviour found by Hoitsema would appear to

disprove conclusively the formation of a definite chemical compound.[262]

SOLUTION OF SOLIDS IN SOLIDS. MIXED CRYSTALS.

The introduction by van't Hoff of the term "solid solution" resulted from

the discovery of a number of deviations from the Raoult-van't Hoff law for

the depression of the freezing point by dissolved substances. In all cases,

the depression was too small; in some instances, indeed, the freezing point

may be raised. To explain these irregularities, van't Hoff assumed that the

dissolved substance crystallized out along with the solid solvent; and he

showed how this would account for the {181} deviations from the law of the

depression of the freezing point, which had been developed on the

assumption that only the pure solvent crystallized out from the

solution.[263]

The "mixed crystals" which were thus obtained, and which van't Hoff called

dilute solid solutions, showed great resemblance in their behaviour to

ordinary liquid solutions, and obeyed the laws applicable to these. These

laws, however, can no longer be applied in the case of the concentrated

solid solutions formed by the crystallization together of isomorphous

substances, and known as isomorphous mixtures. Indeed, it has been

contended[264] that these isomorphous mixtures should not be considered as

solid solutions at all, although no sharp line of demarcation can be drawn

between the two classes. The differences, however, in the behaviour of the

two groups are of a quantitative rather than a qualitative nature; and

since we are concerned at present only with the qualitative behaviour, we

shall make no distinction between the crystalline solid solutions and the

isomorphous mixtures, but shall study the behaviour of the two classes

under the head of "mixed crystals."

Mixed crystals can be formed either by sublimation[265] or from a liquid

phase; and in the latter case the mixed crystals can be deposited either

from solution in a common solvent or from a mixture of the fused

components. In this method of formation, which alone will be discussed in

the present chapter, we are dealing with the fusion curves of two

substances, where, however, the liquid solution is in equilibrium not with

one of the pure components, but with a solid solution or mixed crystal. The

simple scheme (Fig. 29, p. 117) which was obtained in the case of two

components which crystallize out in the pure state, is no longer sufficient

in the case of the formation of mixed crystals. With the help of the Phase

Rule, however, the different possible systems can be classified; and

examples of the different cases predicted by the Phase Rule have also been

obtained by experiment.

{182}

We shall now consider briefly the formation of mixed crystals by

isomorphous substances; the consideration of the formation of mixed

crystals of isodimorphous substances will, on account of the complexity of

the relationships, not be undertaken here.[266]

_Formation of Mixed Crystals of Isomorphous Substances._

For the purpose of representing the relationships found here we shall

employ a temperature-concentration diagram,[267] in which the ordinates

represent the temperature and the abscissae the concentration of the

components. Since there are two solutions, the liquid and the solid, and

since the concentration of the components in these two phases is not, in

general, the same, two curves will be required for each system, one

relating to the liquid phase, the other relating to the solid. The

temperature at which solid begins to be deposited from the liquid solution

will be called the _freezing point_ of the mixture, and the temperature at

which the solid solution just begins to liquefy will be called the _melting

point_ of the solid solution. The temperature-concentration curve for the

liquid phase will therefore be the freezing-point curve; that for the solid

solution, the melting-point curve. The latter will be represented by a

dotted line.[268]

{183}

I.--THE TWO COMPONENTS CAN FORM AN UNBROKEN SERIES OF MIXED CRYSTALS.

Since, as has already been pointed out (p. 176), a mixed crystal (solid

solution) constitutes only one phase, it is evident that if the two

components are miscible with one another in all proportions in the solid

state, there can never be more than one solid phase present, viz. the solid

solution or mixed crystal. If the components are completely miscible in the

solid state, they will also be completely miscible in the liquid state, and

there can therefore be only one liquid phase. The system can at no point

become invariant, because there can never be more than three phases

present. When, therefore, the two components form a continuous series of

mixed crystals, the equilibrium curve must also be continuous. Of these

systems three types are found.

[Illustration: FIG. 49.]

(_a_) _The freezing points of all mixtures lie between the freezing points

of the pure components_ (Curve I., Fig. 49).

Examples.--This type of curve is represented by the mixed crystals of

naphthalene and [beta]-naphthol.[269] The addition of [beta]-naphthol to

naphthalene raises the freezing point of the latter, and the rise is

directly proportional to the amount of naphthol added. The freezing point

curve is therefore a straight line joining the melting points of the two

components. This behaviour, however, is rather exceptional, the

freezing-point curve lying generally above, sometimes also below, the

straight line joining the melting points of the pure components. Thus the

freezing-point curve of mixtures of [alpha]-monochlorocinnamic aldehyde and

[alpha]-monobromocinnamic aldehyde[270] lies above the {184} straight line

joining the melting points of the pure components (31.22deg and 69.56deg),

as is evident from the following table:--

----------------------------------------------------------------------

Molecules of bromo- | |

cinnamic aldehyde in | Freezing point. | Deviation from straight

100 mols. of mixture. | | line.

----------------------------------------------------------------------

0.00 | 31.22deg | --

10.48 | 37.28deg | 2.04deg

21.91 | 43.12deg | 3.50deg

30.07 | 46.80deg | 4.05deg

45.04 | 52.94deg | 4.45deg

62.16 | 58.82deg | 3.77deg

82.98 | 65.07deg | 2.03deg

93.50 | 67.91deg | 0.84deg

100.00 | 69.56deg | --

----------------------------------------------------------------------

Melting-point Curve.--This curve, like the freezing-point curve, must also

be continuous, and the melting points of the different solid solutions will

lie between the melting points of the pure components. This is represented

by the dotted line in Fig. 49, I. The relative position of the two curves,

which can be deduced with the help of thermodynamics and also by

experimental determination, is found in all cases to be in accordance with

the following rule: At any given temperature, _the concentration of that

component by the addition of which the freezing point is depressed, is

greater in the liquid than in the solid phase_; or, conversely, _the

concentration of that component by the addition of which the freezing point

is raised, is greater in the solid than in the liquid phase_. An

illustration of this rule is afforded by the two substances chloro- and

bromo-cinnamic aldehyde already mentioned. As can be seen from the above

table, the addition of chlorocinnamic aldehyde lowers the melting point of

the bromo-compound. In accordance with the rule, therefore, the

concentration of the chloro-compound in the liquid phase must be greater

than in the solid phase; and this was found experimentally. At a

temperature of 49.44deg, the liquid contained 58.52 per cent., the solid

only 52.57 per cent. of the chlorocinnamic aldehyde.

From this it will also be clear that on cooling a fused mixture of two

substances capable of forming mixed crystals, {185} the temperature of

solidification will not remain constant during the separation of the solid;

nor, on the other hand, will the temperature of liquefaction of the solid

solution be constant. Thus, for example, if a liquid solution of two

components, A and B, having the composition represented by the point _x_

(Fig. 50), is allowed to cool, the system will pass along the line _xx'_.

At the temperature of the point _a_, mixed crystals will be deposited, the

composition of which will be that represented by b. As the temperature

continues to fall, more and more solid will be deposited; and since the

solid phase is relatively rich in the component B, the liquid will become

relatively poorer in this. The composition of the liquid solution will

therefore pass along the curve _ad_, the composition of the solid solution

at the same time passing along the curve _bc_; at the point _c_ the liquid

will solidify completely.[271]

[Illustration: FIG. 50.]

Conversely, if mixed crystals of the composition and at the temperature

_x'_ are heated, liquefaction will begin at the temperature _c_, yielding a

liquid of the composition d. On continuing to add heat, the temperature of

the mass will rise, more of the solid will melt, and the composition of the

two phases will change as represented by the curves _da_ and _cb_. When the

temperature has risen to _a_, complete liquefaction will have occurred. The

process of solidification or of liquefaction is therefore extended over a

temperature interval _ac_.

Even when the freezing-point curve is a straight line joining {186} the

melting points of the pure components, the melting-point curve will not

necessarily coincide with the freezing-point curve, although it may

approach very near to it; complete coincidence can take place only when the

melting points of the two components are identical. An example of this will

be given later (Chap. XII.).

(_b_) _The freezing-point curve passes through a maximum_ (Curve II., Fig.

49).

[Illustration: FIG. 51.]

This curve exhibits the greatest degree of contrast to the freezing-point

curve which is obtained when the pure components crystallize out. For,

since the curve passes through a maximum, it is evident that the freezing

point of each of the components must be _raised_ by the addition of the

other component.

Example.--Very few cases belonging to this type are known. The best example

is found in the freezing-point curve of mixtures of _d_- and

_l_-carvoxime[272] (C_{10}H_{14}N.OH). The freezing points and melting

points of the different mixtures of _d_- and _l_-carvoxime are given in the

following table, and represented graphically in Fig. 51:--

---------------+----------------+-----------------+-----------------

Per cent. of | Per cent. of | Freezing point. | Melting point.

_d_-carvoxime. | _l_-carvoxime. | |

---------------+----------------+-----------------+-----------------

100 | 0 | 72.0deg | 72.0deg

99 | 1 | 72.4deg | --

98 | 2 | 73.0deg | --

95 | 5 | 75.4deg | 73.0deg

90 | 10 | 79.0deg | 75.0deg

80 | 20 | 84.6deg | 80.0deg

70 | 30 | 88.2deg | 85.0deg

60 | 40 | 90.4deg | --

50 | 50 | 91.4deg | 91.4deg

25 | 75 | 86.4deg | 82.0deg

8 | 92 | 77.4deg | --

1 | 99 | 72.4deg | --

0 | 100 | 72.0deg | 72.0deg

---------------+----------------+-----------------+-----------------

{187}

In this figure, the melting-point curve, _i.e._ the

temperature-concentration curve for the mixed crystals, is represented by

the lower curve. Since the addition of the laevo-form to the dextro-form

raises the melting point of the latter, the concentration of the laevo-form

(on the right-hand branch of the curve) must, in accordance with the rule

given, be greater in the solid phase than in the liquid. Similarly, since

addition of the dextro-form raises the melting point of the laevo-form, the

solid phase (on the left-hand branch of the curve) must be richer in

dextro- than in laevo-carvoxime. At the maximum point, the melting-point

and freezing-point curves touch; at this point, therefore, the composition

of the solid and liquid phases must be identical. It is evident, therefore,

that at the maximum point the liquid will solidify, or the solid will

liquefy completely without change of temperature; and, accordingly, mixed

crystals of the composition represented by the maximum point will exhibit a

definite melting point, and will in this respect behave like a simple

substance.

(_c_) _The freezing-point curve passes through a minimum_ (Curve III., Fig.

49).

In this case, as in the case of those systems where the pure components are

deposited, a minimum freezing point is obtained. In the latter case,

however, there are two freezing-point curves which intersect at a eutectic

point; in the case where mixed crystals are formed there is only one

continuous curve. On one side of the minimum point the liquid phase

contains relatively more, on the other side relatively less, of the one

component than does the solid phase; while at the minimum point the

composition of the two phases is the same. At this point, therefore,

complete solidification or complete liquefaction will occur without change

of temperature, and the mixed crystals will accordingly exhibit a definite

melting point.

[Illustration: FIG. 52.]

{188}

Example.--As an example of this there may be taken the mixed crystals of

mercuric bromide and iodide.[273] Mercuric bromide melts at 236.5deg, and

mercuric iodide at 255.4deg. The mixed crystal of definite constant melting

point (minimum point) contains 59 mols. per cent. of mercuric bromide, the

melting point being 216.1deg.

The numerical data are contained in the following table, and represented

graphically in Fig. 52:--

-----------------------------------------------------

Mols. per cent. of | |

HgBr_{2}. | Freezing point. | Melting point.

-----------------------------------------------------

100 | 236.5deg | 236deg

90 | 228.8deg | 226deg

80 | 222.2deg | 219deg

70 | 217.8deg | 217deg

65 | 216.6deg | 216deg

60 | 216.1deg | 215.5deg

55 | 216.3deg | 216deg

50 | 217.3deg | 216deg

40 | 221.1deg | 218deg

30 | 227.8deg | 223deg

20 | 236.2deg | 231deg

10 | 245.5deg | 242deg

0 | 255.4deg | 254deg

-----------------------------------------------------

[Illustration: FIG. 53.]

Fractional Crystallization of Mixed Crystals.--With the help of the

diagrams already given it will be possible to predict what will be the

result of the fractional crystallization of a fused mixture of two

substances which can form mixed crystals. Suppose, for example, a fused

mixture of the composition _x_ (Fig. 53) is cooled down; then, as we have

already seen, when the temperature has fallen to _a_, mixed crystals of

composition, _b_, are deposited. If the temperature is allowed to fall

{189} to _x'_, and the solid then separated from the liquid, the mixed

crystals so obtained will have the composition represented by e. If, now,

the mixed crystals _e_ are completely fused and the fused mass allowed to

cool, separation of solid will occur when the temperature has fallen to the

point _f_. The mixed crystals which are deposited have now the composition

represented by _g_, i.e. _they are richer in B than the original mixed

crystals_. By repeating this process, the composition of the successive

crops of mixed crystals which are obtained approximates more and more to

that of the pure component B, while, on the other hand, the composition of

the liquid phase produced tends to that of pure A. By a systematic and

methodical repetition of the process of fractional crystallization,

therefore, a _practically_ complete separation of the components can be

effected; a perfect separation is theoretically impossible.

From this it will be readily understood that in the case of substances the

freezing point of which passes through a maximum, fractional

crystallization will ultimately lead to mixed crystals having the

composition of the maximum point, while the liquid phase will more and more

assume the composition of either pure A or pure B, according as the initial

composition was on the A side or the B side of the maximum point. In those

cases, however, where the curves exhibit a minimum, the solid phase which

separates out will ultimately be one of the pure components, while a liquid

phase will finally be obtained which has the composition of the minimum

point.

II.--THE TWO COMPONENTS DO NOT FORM A CONTINUOUS SERIES OF MIXED CRYSTALS.

This case corresponds to that of the partial miscibility of liquids. The

solid component A can "dissolve" the component B until the concentration of

the latter in the mixed crystal has reached a certain value. Addition of a

further amount of B will not alter the composition of the mixed crystal,

but there will be formed a second solid phase consisting {190} of a

solution of A in B. At this point the four phases, mixed crystals

containing excess of A, mixed crystals containing excess of B, liquid

solution, vapour, can coexist; this will therefore be an invariant point.

The temperature-concentration curves will therefore no longer be

continuous, but will exhibit a break or discontinuity at the point at which

the invariant system is formed.

(_a_) _The freezing-point curve exhibits a transition point_ (Curve I.,

Fig. 54).

As is evident from the figure, addition of B raises the melting point of A,

and, in accordance with the rule previously given, the concentration of B

in the mixed crystals will be greater than in the solution. This is

represented in the figure by the dotted curve AD. On the other hand,

addition of A lowers the melting point of B, and the two curves BC and BE

are obtained for the liquid and solid phases respectively. At the

temperature of the line CDE the liquid solution of the composition

represented by C is in equilibrium with the two different mixed crystals

represented by D and E. At this temperature, therefore, the _tc_-curve for

the solid phase exhibits a discontinuity; and, since the solid phase

undergoes change at this point, the freezing-point curve must show a break

(p. 111).

[Illustration: FIG. 54.]

Example.--Curves of the form given in Fig. 54 I. have been found

experimentally in the case of silver nitrate and sodium nitrate.[274] The

following table contains the numerical data, which are also represented

graphically in Fig. 55:--

{191}

-----------------------------------------------------

Molecules NaNO_{3} | Freezing point. | Melting point.

per cent. | |

-----------------------------------------------------

0 | 208.6deg | 208.6deg

8 | 211.4deg | 210deg

15.06 | 215deg | 212deg

19.46 | 217.2deg | 214.8deg

21.9 | 222deg | 215deg

26 | 228.4deg | 216.5deg

29.7 | 234.8deg | 217.5deg

36.2 | 244.4deg | 217.5deg

47.3 | 259.4deg | 237.6deg

58.9 | 272deg | 257deg

72 | 284deg | 274deg

100 | 308deg | 308deg

-----------------------------------------------------

The temperature of the transition point is 217.5deg; at this point the

liquid contains 19.5, and the two conjugate solid solutions 26 and 38

molecules of sodium nitrate per cent. respectively.

[Illustration: FIG. 55.]

[Illustration: FIG. 56.]

(_b_) _The freezing-point curve exhibits a eutectic point_ (Curve II., Fig.

54). {192}

In this case the freezing point of each of the components is lowered by the

addition of the other, until at last a point is reached at which the liquid

solution solidifies to a mixture or conglomerate of two mixed crystals.

Examples.--Curves belonging to this class have been obtained in the case of

potassium and thallium nitrates[275] and of naphthalene and monochloracetic

acid.[276] The data for the latter are given in the following table and

represented in Fig. 56:--

-------------------------------------------------------------------------

| Liquid solution. | Solid solution.

------------------------------------------------------------

Temperature. | | | |

| Per cent. | Per cent. | Per cent. | Per cent.

| naphthalene. | acid. | naphthalene. | acid.

-------------------------------------------------------------------------

62deg | -- | 100 | -- | 100

60deg | 4.0 | 96.0 | 1.7 | 98.3

55deg | 21.0 | 79.0 | 2.1 | 97.9

53.5deg | 29.4 | 70.0 | -- | --

55deg | 31.3 | 68.7 | 59.6 | 40.4

60deg | 42.4 | 57.6 | 80.3 | 19.7

65deg | 53.3 | 46.7 | 89.2 | 10.8

70deg | 69.7 | 2.3 | 95.4 | 4.6

75deg | 84.4 | 15.6 | 96.6 | 3.4

79.9deg | 100 | -- | 100 | --

-------------------------------------------------------------------------

At the eutectic point the liquid solution is in equilibrium with two

different mixed crystals the composition of which is represented by D and E

respectively. If, therefore, a fused mixture containing the two components

A and B in the proportions represented by C is cooled down, it will, when

the temperature has reached the point C, solidify completely to a

_conglomerate_ of mixed crystals, D and E.

[Illustration: FIG. 57.]

[Illustration: FIG. 58.]

Changes in Mixed Crystals with the Temperature.--In the case of the

different types of systems represented in Fig. 49, a homogeneous liquid

solution of the two components will exist at temperatures above the

freezing-point curve, a homogeneous mixed crystal at temperatures below the

melting-point curve, while at any point between the freezing-point and

melting-point {193} curves the mixture will separate into a solid phase and

a liquid phase. In the case, however, of the two types shown in Fig. 54 the

relationships are somewhat more complicated. As before, the area above the

freezing-point curve gives the conditions under which homogeneous liquid

solutions can exist; but below the melting-point curve two different mixed

crystals can coexist. This will be best understood from Figs. 57 and 58. D

and E represent, as we have seen, the composition of two mixed crystals

which are in equilibrium with the liquid solution at the temperature of the

point C. These two mixed crystals represent, in the one case, a saturated

solution of B in A (point D), and the other a saturated solution of A in B

(point E). Just as we saw that the mutual solubility of two liquids varied

with the temperature, so also in the case of two solids; as the temperature

alters, the solubility of the two solid components in one another will

change. This alteration is indicated diagrammatically in Figs. 57 and 58 by

the dotted curve similar to the solubility curves for two mutually soluble

liquids (p. 101).

Suppose, now, that a mixed crystal of the composition _x_ is cooled down,

it will remain unchanged until, when the temperature has fallen to _t'_,

the homogeneous mixed crystal breaks up into a conglomerate of two mixed

crystals the composition of {194} which is represented by _x'_ and _x"_

respectively. From this, then, it can be seen that in the case of

substances which form two solid solutions, the mixed crystals which are

desposited from the liquid fused mass need not remain unchanged in the

solid state, but may at some lower temperature lose their homogeneity. This

fact is of considerable importance for the formation of alloys.[277]

A good example of this will soon be met with in the case of the iron and

carbon alloys. The alloys of copper and tin also furnish examples of the

great changes which may take place in the alloy between the temperature at

which it separates out from the fused mass and the ordinary temperature.

Thus, for example, one of the alloys of copper and tin which separates out

from the liquid as a solid solution breaks up, on cooling, into the

compound Cu_{3}Sn and liquid:[278] a striking example of a solid substance

partially liquefying on being cooled.

* * * * *

{195}

CHAPTER XI

EQUILIBRIUM BETWEEN DYNAMIC ISOMERIDES

It has long been known that certain substances, _e.g._ acetoacetic ester,

are capable when in solution or in the fused state, of reacting as if they

possessed two different constitutions; and in order to explain this

behaviour the view was advanced (by Laar) that in such cases a hydrogen

atom oscillated between two positions in the molecule, being at one time

attached to oxygen, at another time to carbon, as represented by the

formula--

CH_{3}.C--CH.CO_{2}C_{2}H_{5}

. ^

. |

O<-H

When the hydrogen is in one position, the substance will act as an

hydroxy-compound; with hydrogen in the other position, as a ketone.

Substances possessing this double function are called _tautomeric_.

Doubt, however, arose as to the validity of the above explanation, and this

doubt was confirmed by the isolation of the two isomerides in the solid

state, and also by the fact that the velocity of change of the one

isomeride into the other could in some cases be quantitatively measured.

These and other observations then led to the view, in harmony with the laws

of chemical dynamics, that tautomeric substances in the dissolved or fused

state represent a _mixture_ of two isomeric forms, and that equilibrium is

established not by _intra_- but by _inter_-molecular change, as expressed

by the equation--

CH_{3}.CO.CH_{2}.CO_{2}C_{2}H_{5} <--> CH_{3}.C(OH):CH.CO_{2}C_{2}H_{5}

{196} In the solid state, the one or other of the isomerides represents the

stable form; but in the liquid state (solution or fusion) the stable

condition is an equilibrium between the two forms.

A similar behaviour is also found in the case of other isomeric substances

where the isomerism is due to difference of structure, _i.e._ structure

isomerism (_e.g._ in the case of the oximes

C_{6}H_{5}.C.H C_{6}H_{5}.C.H

|| and || ),

N.OH HO.N

or to difference in configuration, _i.e._ stereoisomerism (_e.g._ optically

active substances), or to polymerism (_e.g._ acetaldehyde and paraldehyde).

In all such cases, although the different solid forms correspond to a

single definite constitution, in the liquid state a condition of

equilibrium between the two modifications is established. As a general name

for these different classes of substances, the term "dynamic isomerides"

has been introduced; and the different kinds of isomerism are classed

together under the title "dynamic isomerism."[279]

By reason of the importance of these phenomena in the study more especially

of Organic Chemistry, a brief account of the equilibrium relations

exhibited by systems composed of dynamic isomerides may be given here.[280]

In studying the fusion and solidification of those substances which exhibit

the relationships of dynamic isomerism, the phenomena observed will vary

somewhat according as the reversible transformation of the one form into

the other takes place with measurable velocity at temperatures in the

neighbourhood of the melting points, or only at some higher temperature. If

the transformation is very rapid, the system will behave like a

one-component system, but if the isomeric change is comparatively slow, the

behaviour will be that of a two-component system.

Temperature-Concentration Diagram.--The relationships which are met with

here will be most readily understood with {197} the help of Fig. 59.

Suppose, in the first instance, that isomeric transformation does not take

place at the temperature of the melting point, then the freezing point

curve will have the simple form ACB; the formation of compounds being for

the present excluded. This is the simplest type of curve, and gives the

composition of the solutions in equilibrium with the one modification

([alpha] modification) at different temperatures (curve AC); and of the

solutions in equilibrium with the other modification ([beta] modification)

at different temperatures (curve BC). C is the eutectic point at which the

two solid isomerides can exist side by side in contact with the solution.

[Illustration: FIG. 59.]

Now, suppose that isomeric transformation takes place with measurable

velocity. If the pure [alpha]-modification is heated to a temperature _t'_

above its melting point, and the liquid maintained at that temperature

until equilibrium has been established, a certain amount of the [beta]-form

will be present in the liquid, the composition of which will be represented

by the point _x'_. The same condition of equilibrium will also be reached

by starting with pure [beta]. Similarly, if the temperature of the liquid

is maintained at the temperature _t"_, equilibrium will be reached, we

shall suppose, when the solution has the composition _x"_. The curve DE,

therefore, which passes through all the different values of _x_

corresponding to different values of _t_, will represent the change of

equilibrium with the temperature. It will slope to the right (as in the

figure) if the transformation of [alpha] into [beta] is accompanied by

absorption of heat; to the left if the transformation is accompanied by

evolution of heat, in accordance with van't Hoff's Law of movable

equilibrium. If transformation occurs without heat effect, the equilibrium

will be independent of the {198} temperature, and the equilibrium curve DE

will therefore be perpendicular and parallel to the temperature axis.

We must now find the meaning of the point D. Suppose the pure [alpha]- or

pure [beta]-form heated to the temperature _t'_, and the temperature

maintained constant until the liquid has the composition _x'_ corresponding

to the equilibrium at that temperature. If the temperature is now allowed

to fall sufficiently slowly so that the condition of equilibrium is

continually readjusted as the temperature changes, the composition of the

solution will gradually alter as represented by the curve _x'_D. Since D is

on the freezing point curve of pure [alpha], this form will be deposited on

cooling; and since D is also on the equilibrium curve of the liquid, D is

the only point at which solid can exist in stable equilibrium with the

liquid phase. (The vapour phase may be omitted from consideration, as we

shall suppose the experiments carried out in open vessels.) All systems

consisting of the two hylotropic[281] isomeric substances [alpha] and

[beta] will, therefore, ultimately freeze at the point D, which is called

the "natural" freezing point[282] of the system; provided, of course, that

sufficient time is allowed for equilibrium to be established. From this it

is apparent that _the stable modification at temperatures in the

neighbourhood of the melting point is that which is in equilibrium with the

liquid phase at the natural freezing point_.

From what has been said, it will be easy to predict what will be the

behaviour of the system under different conditions. If pure [alpha] is

heated, a temperature will be reached at which it will melt, but this

melting point will be sharp only if the velocity of isomeric transformation

is comparatively slow; _i.e._ slow in comparison with the determination of

the melting point. If the substance be maintained in the fused condition

for some time, a certain amount of the [beta] modification will be formed,

and on lowering the temperature the pure [alpha] form will be deposited,

not at the temperature of the melting point, but at some lower temperature

depending on the concentration of the [beta] modification in the liquid

phase. If isomeric transformation {199} takes place slowly in comparison

with the rate at which deposition of the solid occurs, the liquid will

become increasingly rich in the [beta] modification, and the freezing point

will, therefore, sink continuously. At the eutectic point, however, the

[beta] modification will also be deposited, and the temperature will remain

constant until all has become solid. If, on the other hand, the velocity of

transformation is sufficiently rapid, then as quickly as the [alpha]

modification is deposited, the equilibrium between the two isomeric forms

in the liquid phase will continuously readjust itself, and the end-point of

solidification will be the natural freezing point.

Similarly, starting with the pure [beta] modification, the freezing point

after fusion will gradually fall owing to the formation of the [alpha]

modification; and the composition of the liquid phase will pass along the

curve BC. If, now, the rate of cooling is not too great, or if the velocity

of isomeric transformation is sufficiently rapid, complete solidification

will not occur at the eutectic point; for at this temperature solid and

liquid are not in stable equilibrium with one another. On the contrary, a

further quantity of the [beta] modification will undergo isomeric change,

the liquid phase will become richer in the [alpha] form, and the freezing

point will _rise_; the solid phase in contact with the liquid being now the

[alpha] modification. The freezing point will continue to rise until the

point D is reached, at which complete solidification will take place

without further change of temperature.

The diagram also allows us to predict what will be the result of rapidly

cooling a fused mixture of the two isomerides. Suppose that either the

[alpha] or the [beta] modification has been maintained in the fused state

at the temperature _t'_ sufficiently long for equilibrium to be

established. The composition of the liquid phase will be represented by

_x'_. If the liquid is now _rapidly_ cooled, the composition will remain

unchanged as represented by the dotted line _x'_G. At the temperature of

the point G solid [alpha] modification will be deposited. If the cooling is

not carried below the point G, so as to cause complete solidification, the

freezing point will be found to rise with time, owing to the conversion of

some of the [beta] form into the [alpha] form {200} in the liquid phase;

and this will continue until the composition of the liquid has reached the

point D. From what has just been said, it can also be seen that if the

freezing point curves can be obtained by actual determination of the

freezing points of different synthetic mixtures of the two isomerides, it

will be possible to determine the condition of equilibrium in the fused

state at any given temperature without having recourse to analysis. All

that is necessary is to rapidly cool the fused mass, after equilibrium has

been established, and find the freezing point at which solid is deposited;

that is, find the point at which the line of constant temperature cuts the

freezing point curve. The composition corresponding to this temperature

gives the composition of the equilibrium mixture at the given temperature.

It will be evident, from what has gone before, that the degree of

completeness with which the different curves can be realised will depend on

the velocity with which isomeric change takes place, and on the rapidity

with which the determinations of the freezing point can be carried out. As

the two extremes we have, on the one hand, practically instantaneous

transformation, and on the other, practically infinite slowness of

transformation. In the former case, only one melting and freezing point

will be found, viz. the natural freezing point; in the latter case, the two

isomerides will behave as two perfectly independent components, and the

equilibrium curve DE will not be realised.

The diagram which is obtained when isomeric transformation does not occur

within measurable time at the temperature of the melting point is somewhat

different from that already given in Fig. 59. In this case, the two

freezing point curves AC and BC (Fig. 60) can be readily realized, as no

isomeric change occurs in the liquid phase. Suppose, however, that at a

higher temperature, _t'_, reversible isomeric transformation can take

place, the composition of the liquid phase will alter until at the point

_x'_ a condition of equilibrium is reached; and the composition of the

liquid at higher temperatures will be represented by the curve _x'_F. Below

the temperature _t'_ the position of the equilibrium curve is hypothetical;

but as the temperature {201} falls the velocity of transformation

diminishes, and at last becomes _practically_ zero. The equilibrium curve

can therefore be regarded as dividing into two branches _x'_G and _x'_H. At

temperatures between G and _t'_ the [alpha] modification can undergo

isomeric change leading to a point on the curve G_x'_; and the [beta]

modification can undergo change leading to a point on the curve H_x'_. The

same condition of equilibrium is therefore not reached from each side, and

we are therefore dealing not with true but with false equilibrium (p. 5).

Below the temperatures G and H, isomeric transformation does not occur in

measurable time. We shall not, however, enter into a detailed discussion of

the equilibria in such systems, more especially as they are not systems in

true equilibrium, and as the temperature at which true equilibrium can be

established with appreciable velocity alters under the influence of

catalytic agents.[283] Examples of such systems will no doubt be found in

the case of optically active substances, where both isomerides are

apparently quite stable at the melting point. In the case of such

substances, also, the action of catalytic agents in producing isomeric

transformation (racemisation) is well known.

[Illustration: FIG. 60.]

Transformation of the Unstable into the Stable Form.--As has already been

stated, the stable modification in the neighbourhood of the melting point

is that one which is in equilibrium with the liquid phase at the natural

freezing point. In the case of polymorphic substances, we have seen (p. 39)

that that form which is stable in the neighbourhood of the melting point

melts at the higher temperature. That was a {202} consequence of the fact

that the two polymorphic forms on melting gave identical liquid phases. In

the present case, however, the above rule does not apply, for the simple

reason that the liquid phase obtained by the fusion of the one modification

is not identical with that obtained by the fusion of the other. In the case

of isomeric substances, therefore, the form of lower melting point _may_ be

the more stable; and where this behaviour is found it is a sign that the

two forms are isomeric (or polymeric) and not polymorphic.[284] An example

of this is found in the case of the isomeric benzaldoximes (p. 203).

Since in Fig. 59 the [alpha] modification has been represented as the

stable form, the transformation of the [beta] into the [alpha] form will be

possible at all temperatures down to the transition point. At temperatures

below the eutectic point, transformation will occur without formation of a

liquid phase; but at temperatures above the eutectic point liquefaction can

take place. This will be more readily understood by drawing a line of

constant temperature, HK, at some point between C and B. Then if the [beta]

modification is maintained for a sufficiently long time at that

temperature, a certain amount of the [alpha] modification will be formed;

and when the composition of the mixture has reached the point H, fusion

will occur. If the temperature is maintained constant, isomeric

transformation will continue to take place in the liquid phase until the

equilibrium point for that temperature is reached. If this temperature is

higher than the natural melting point, the mixture will remain liquid all

the time; but if it is below the natural melting point, then the [alpha]

modification will be deposited when the system reaches the condition

represented by the point on the curve AC corresponding to the particular

temperature. As isomeric transformation continues, the freezing point of

the system will rise until it reaches the natural freezing point D.

Similarly, if the [alpha] modification is maintained at a temperature above

that of the point D, liquefaction will ultimately occur, and the system

will again reach the final state represented by D.[285]

{203}

Examples.--_Benzaldoximes._ The relationships which have just been

discussed from the theoretical point of view will be rendered clearer by a

brief description of cases which have been experimentally investigated. The

first we shall consider is that of the two isomeric benzaldoximes:[286]--

C_{6}H_{5}.C.H C_{6}H_{5}.C.H

|| ||

HO.N N.OH

Benzantialdoxime Benzsynaldoxime

([alpha]-modification). ([beta]-modification).

Fig. 61 gives a graphic representation of the results obtained.

The melting point of the [alpha] modification is 34-35deg; the melting

point of the unstable [beta]-modification being 130deg. The freezing curves

AC and BC were obtained by determining the freezing points of different

mixtures of known composition, and the numbers so obtained are given in the

following table.

{204}

----------------------------------------------------

Grams of the [alpha] modification |

in 100 gm. of mixture. | Freezing point.

----------------------------------+-----------------

26.2 | 101deg

49.2 | 79deg

73.7 | 46deg

91.7 | 26.2deg

95.0 | 28.6deg

96.0 | 30.0deg

----------------------------------------------------

[Illustration: FIG. 61.]

The Phase Rule and Its Applications · 第 20 / 23 章