CHAPTER II

SOLUTIONS

We have seen that living beings are transformers of energy and of matter,

evolutionary in form and liquid in consistency; that they are solutions of

colloids and crystalloids separated by osmotic membranes to form

microscopic cells, or consisting merely of a gelatinous mass of protoplasm,

with a nucleus of slightly differentiated material. The elementary

phenomenon of life is the contact of two different solutions. This is the

initial physical phenomenon from which proceed all the other phenomena of

life in accordance with the ordinary chemical and physical laws. Thus the

basis of biological science is the study of solution and of the phenomena

which occur between two different solutions, either in immediate contact or

when separated by a membrane.

A solution is a homogeneous mixture of one or more solutes in a liquid

solvent. Before solution the solute or dissolved substance may be solid,

liquid, or gaseous.

Solutes, or substances capable of solution, may be divided into two

classes--substances which are capable of crystallization, or crystalloids;

and those which are incapable of crystallization, the colloids.

Crystalloids may be divided again into two classes, those whose solutions

are ionizable and therefore conduct electricity, chiefly salts, acids, and

bases; and those whose solutions are non-ionizable and are therefore

non-conductors. These latter are for the most part crystallizable

substances of organic origin, such as sugars, urea, etc.

Avogadro's law asserts that under similar conditions of temperature and

pressure, equal volumes of various gases {15} contain an equal number of

molecules. Under similar conditions, the molecular weights of different

substances have therefore the same ratio as the weights of equal volumes of

their vapours. Hence if we fix arbitrarily the molecular weight of any one

substance, the molecular weight of all other substances is thereby

determined. The molecular weight of hydrogen has been arbitrarily fixed as

two, and hence the molecular weight of any substance will be double its

gaseous density when compared with that of hydrogen.

_Gramme-Molecule._--A gramme-molecule is the molecular weight of a body

expressed in grammes. Occasionally for brevity a gramme-molecule is spoken

of as a "molecule." Thus we may say that the molecular weight of oxygen is

16 grammes, meaning thereby that there are the same number of molecules in

16 grammes of oxygen as there are atoms in 1 gramme of hydrogen.

_Concentration._--The concentration of a solution is the ratio between the

quantity of the solute and the quantity of the solvent. The concentration

of a solution is expressed in various ways. (_a_) The weight of solute

dissolved in 100 grammes of the solvent. (_b_) The weight of solute present

in 100 grammes of the solution. (_c_) The weight of solute dissolved in a

litre of the solvent. (_d_) The weight of solute in a litre of the

solution. The most usual method is to give the concentration as the weight

of solute dissolved in 100 grammes or in one litre of the solvent.

_Molecular Concentration._--Many of the physical and biological properties

of a solution are proportional, not to its mass or weight concentration,

but to its molecular concentration, _i.e_. to the number of

gramme-molecules of the solute contained in a litre of the solution. Many

physical properties are quite independent of the nature of the solute,

depending only on its degree of molecular concentration.

_Normal Solution._--A normal solution is one which contains one

gramme-molecule of the solute per litre. A decinormal solution contains

one-tenth of a gramme-molecule of the solute per litre, and a centinormal

solution one-hundredth of a gramme-molecule. A normal solution of urea, for

example, {16} contains 60 grammes of urea per litre, while a normal

solution of sugar contains 342 grammes of sugar per litre.

_The Dissolved Substance is a Gas._--Van t' Hoff, using the data obtained

by the botanist Pfeffer, showed that the dissolved matter in a solution

behaved exactly as if it were a gas. The analogy is complete in every

respect. Like the gaseous molecules, the molecules of a solute are mobile

with respect to one another. Like those of a gas, the molecules of a solute

tend to spread themselves equally, and to fill the whole space at their

disposal, _i.e._ the whole volume of the solution. The surface of the

solution represents the vessel containing the gas, which confines it within

definite limits and prevents further expansion.

_Osmotic Pressure._--Like the molecules of a gas, the molecules of a solute

exercise pressure on the boundaries of the space containing it. This

osmotic pressure follows exactly the same laws as gaseous pressure. It has

the same constants, and all the notions acquired by the study of gaseous

pressure are applicable to osmotic pressure. Osmotic pressure is in fact

the gaseous pressure of the molecules of the solute.

When a gas dilates and increases in volume, its temperature falls, and cold

is produced. Similarly, when a soluble substance is dissolved, it increases

in volume, and the temperature of the liquid falls. This phenomenon is well

known as a means of producing cold by a refrigerating mixture.

The phenomena of life are governed by the laws of gaseous pressure, since

all these phenomena take place in solutions. The fundamental laws of

biology are those of the distribution of substances in solution, which is

regulated by the laws of gaseous pressure, since all these laws are

applicable also to osmotic pressure.

_Boyle's Law_.--When a gas is compressed its volume is diminished. If the

pressure is doubled, the volume is reduced to one-half. The quantity V x P,

that is the volume multiplied by the pressure, is constant.

_Gay-Lussac's Law._--For a difference of temperature of a degree Centigrade

all gases dilate or contract by 1 / 273 of their volume at 0deg Centigrade.

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_Dalton's Law._--In a gaseous mixture, the total pressure is equal to the

sum of the pressures which each gas would exert if it alone filled the

whole of the receptacle.

_Pressure proportional to Molecular Concentration._--The above laws are

completely independent of the chemical nature of the gas, they depend only

on the number of gaseous molecules in a given space, _i.e._ on the

molecular concentration. If we double the mass of the gas in a given space,

we double the number of molecules, and we also double the pressure,

whatever the nature of the molecules. We may also double the pressure by

compressing the molecules of a gas, or of several gases, into a space half

the original size. The molecular concentration of a gas, or of a mixture of

gases, is the ratio of the number of molecules to the volume they occupy.

The pressure of a gas or of a mixture of gases is proportional to its

molecular concentration. This is a better and a shorter way of expressing

both Boyle's law and Dalton's law.

One gramme-molecule of a gas, whatever its nature, condensed into the

volume of 1 litre, has a pressure of 22.35 atmospheres. Similarly one

gramme-molecule of a solute, whatever its nature, when dissolved in a litre

of water, has the same pressure, viz. 22.35 atmospheres.

_Absolute Zero._--According to Gay-Lussac's law, the volume of a gas

diminishes by 1 / 273 of its volume at 0deg C. for each degree fall of

temperature. Thus if the contraction is the same for all temperatures, the

volume would be reduced to zero at -273deg C. This is the absolute zero of

temperature. Temperatures measured from this point are called absolute

temperatures, and are designated by the symbol T. If _tdeg_ indicates the

Centigrade temperature above the freezing point of water, then the absolute

temperature is equal to _tdeg_ + 273deg.

_The Gaseous Constant._--Consider a mass of gas at 0deg C. under a pressure

P_o, with volume V_o. At the absolute temperature T, if the pressure be

unaltered, the volume of this gas will be V_oT / 273. Therefore the

constant PV, the product of the pressure by the volume, will be represented

by P_oV_oT / 273. {18}

At the same temperature, but under another pressure P' the gas will have a

different volume V'. Since, according to Boyle's law, PV is constant (P'V'

= P_oV_o), it will still equal P_oV_oT / 273. Therefore P_oV_o / 273 is

also constant. This quantity is called "the gaseous constant," and if we

represent it by the symbol R, we obtain the general formula PV = RT for all

gases, or PV / T = R.

Suppose, for instance, we have a gramme-molecule of a gas at 0deg C. in a

space of 1 litre. It has a pressure of 22.35 atmospheres at 0deg C., or

273deg absolute temperature. Since PV = RT, R = PV / T = 1 x 22.35 / 273 =

.0819. This number .0819 is the numerical value of the constant R for all

gases, volume being measured in litres and pressure in atmospheres.

Substances in solution behave exactly like gases, they follow the same laws

and have the same constants. All the conceptions which have been acquired

by the study of gases are applicable to solutions, and therefore to the

phenomena of life. The osmotic pressure of a solution is the force with

which the molecules of the solute, like gaseous molecules, strive to

diffuse into space, and press on the limits which confine them, the

containing vessel being represented by the surfaces of the solution.

Osmotic pressure is measured in exactly the same way as gaseous pressure.

To measure steam pressure we insert a manometer in the walls of the boiler.

In the same way we may use a manometer to measure osmotic pressure. We

attach the tube to the walls of the porous vessel, allow the solvent to

increase in volume under the pressure of the solute, and measure the rise

of the liquid in the manometer tube.

_Pfeffer's Apparatus._--Pfeffer has designed an apparatus for the

measurement of osmotic pressure. It consists of a vessel of porous

porcelain, the pores of which are filled with a colloidal solution of

ferrocyanide of copper. This forms a semi-permeable membrane which permits

the passage of water into the vessel, but prevents the passage of sugar or

of any {19} colloid. The stopper which hermetically closes the vessel is

pierced for the reception of a mercury manometer. The vessel is filled with

a solution of sugar and plunged in a bath of water. The volume of the

solution in the interior of the vessel can vary, since water passes easily

in either direction through the pores of the vessel. The boundary of the

solvent has become extensible, and its volume can increase or diminish in

accordance with the osmotic pressure of the solute. Under the pressure of

the sugar water is sucked into the vessel like air into a bellows, the

solution passes into the tube of the manometer, and raises the column of

mercury until its pressure balances the osmotic pressure of the sugar

molecules.

_Osmotic Pressure follows the Laws of Gaseous Pressure._--This osmotic

pressure is in fact gaseous pressure, and may be measured in millimetres of

mercury in just the same way. We may thus show that osmotic pressure

follows the laws of gaseous pressure as defined by Boyle, Dalton, and

Gay-Lussac. The coefficient of pressure variation for change of temperature

is the same for a solute as for a gas. The formula PV = RT is applicable to

both. The numerical value of the constant R is also the same for a solute

as for a gas. being .0819 for one gramme-molecule of either, when the

volume is expressed in litres and the pressure in atmospheres. The formula

PV = RT shows that for a given mass, with the same volume, the pressure

increases in proportion to the absolute temperature.

_Osmotic Pressure of Sugar._--A normal solution of sugar, containing 342

grammes of sugar per litre, has a pressure of 22.35 atmospheres, and it may

well be asked why such an enormous pressure is not more evident. The reason

will be found in the immense frictional resistance to diffusion. Frictional

resistance is proportional to the area of the surfaces in contact, and this

area increases rapidly with each division of the substance. When a solute

is resolved into its component molecules, its surface is enormously

increased, and therefore the friction between the molecules of the solute

and those of the solvent.

_Isotonic Solutions._--Two solutions which have the same {20} osmotic

pressure are said to be iso-osmotic or isotonic. When comparing two

solutions of different concentration, the solution with the higher osmotic

pressure is said to be hypertonic, and that with the lower osmotic pressure

hypotonic.

_Lowering of the Freezing Point._--Pure water freezes at 0deg C. Raoult

showed that the introduction of a non-ionizable substance, such as sugar or

alcohol, lowers the freezing point of a solution in proportion to the

molecular concentration of the solute. One gramme-molecule of the solute

introduced into one litre of the solution lowers its temperature of

congelation by 1.85deg C. Thus a normal solution of any non-ionizable

substance in water freezes at -1.85deg C. The measurement of this lowering

of the freezing point is called Cryoscopy, a method which is becoming of

great utility in medicine.

_Cryoscopy of Blood._--In order to determine the osmotic pressure of the

blood at 37deg C., _i.e._ 98.6deg F., the normal temperature, we proceed as

follows. On freezing the blood, we find that it congeals at -.56deg. Its

molecular concentration is therefore .56 / 1.85 = .30, or about one-third

of a gramme-molecule per litre. Its osmotic pressure at 0deg C. is

therefore .3 x 22.35 = 6.7 atmospheres. The increase of pressure with

temperature is the same as for a gas, viz. 1/273, or .00367 of its pressure

at 0deg for every degree rise of temperature. The increase of pressure at

37deg is therefore .00367 x 37 x 6.7 = .9 atmospheres. The total osmotic

pressure at 37deg is therefore 6.7 + .9 = 7.6 atmospheres.

_Rise of Boiling Point._--Water under atmospheric pressure boils at a

temperature of 100deg C. The addition of a solute whose solution does not

conduct electricity, such as sugar, causes a rise in the boiling point

proportional to the molecular concentration of that solute.

_Lowering of the Vapour Tension._--The vapour tension of a liquid is

lowered by the addition of a solute. A liquid boils at the temperature at

which its vapour tension equals that of the atmosphere. Since an aqueous

solution of sugar at atmospheric pressure does not begin to boil at 100deg

C., it is manifest that its vapour tension is then less than that of the

{21} atmosphere. The addition of a solute such as sugar, whose solution is

not ionizable, and therefore does not conduct electricity, lowers the

vapour tension of the solution in proportion to the molecular concentration

of the solute.

_Corresponding Values._--We have thus found five properties of a solution

which vary proportionally, so that from the measurement of any one of them

we can determine the corresponding values of all the others. These are--

1. The Molecular Concentration.

2. The Osmotic Pressure.

3. The Diminution of Vapour Tension.

4. The Raising of the Boiling Point.

5. The Lowering of the Freezing Point.

_Cryoscopy._--The usual method employed for the determination of the

molecular concentration and osmotic pressure of a solution is by

cryoscopy--the measurement of its temperature of congelation. A very

sensitive thermometer is used, the scale of which extends over only 5deg

and is divided into hundredths of a degree. The liquid under examination is

placed in a test tube, in which the bulb of the thermometer is plunged, and

this is supported in a second tube with an air space all round it. The

whole is then suspended to the under side of the cover of the refrigerating

vessel, which may be cooled either by filling it with a freezing mixture,

or by the evaporation of ether. During the whole of the operation the

liquid is agitated by a mechanical stirrer. The first step is to determine

the freezing point of distilled water. As the water cools the mercury

gradually descends in the stem of the thermometer till it reaches a point

below the zero mark at 0deg C. As soon as ice begins to form the mercury

rises, at first rapidly and then more slowly, reaches a maximum, and

finally descends again. This maximum reading is the true point of

congelation. The inner tube is then emptied, care being taken to leave a

few small ice crystals to serve as centres of congelation for the

subsequent experiment, thus avoiding supercooling of the solution. The

process is then repeated with the solution under examination. The

difference between {22} the two freezing points is the required "lowering

of the freezing point."

Cryoscopy is the method most used in biological research to determine

molecular concentration. It has, however, some grave defects. It

necessitates several cubic centimetres of the liquid under examination. It

gives us the constants of the solution at the temperature of freezing,

which is far below that of life. Organic liquids are easily altered and are

extremely sensible to minute differences of temperature, cryoscopy

therefore gives us no information as to the constitution of solutions under

normal conditions. It is desirable to have some other method of determining

molecular concentration and the other interdependent constants at the

normal temperature of life. A much better method, were it possible, would

be the direct determination of the vapour tension of the solutions under

normal conditions of temperature and pressure.

_Molecular Lowering of the Freezing Point._--For every substance whose

solution is not ionized and therefore does not conduct electricity, the

lowering of the freezing point is the same, viz. 1.85deg C. for each

gramme-molecule of the solute per litre of the solution.

_Determination of the Molecular Concentration._--In order to obtain the

molecular concentration of a non-ionizable substance, we have only to

determine the lowering of the freezing point. Let A be the lowering of the

freezing point of any solution. On dividing it by 1.85 (the lowering of the

freezing point for a normal solution), we obtain the number of

gramme-molecules in a litre of the solution. If n be the number of

gramme-molecules per litre, then n = A / 1.85.

_Determination of the Osmotic Pressure._--The osmotic pressure P of a

solution may be obtained by multiplying its molecular concentration n by

22.35 atmospheres. P = n x 22.35 = A / 1.85 x 22.35.

_Determination of Molecular Weight._--The lowering of the freezing point

also enables us to calculate the molecular {23} weight of any non-ionizable

solute. Thus Bouchard has been able to determine by means of cryoscopy the

mean molecular weight of the substances eliminated by the urine. A weight

_x_ of the substance is dissolved in a litre of water, and the lowering of

the freezing point is observed. The value thus found divided by 1.85 gives

us n, the number of gramme-molecules per litre. The molecular weight M may

be determined by dividing the original weight x by n.

The study of osmotic pressure was begun by the Abbe Nollet; and one of his

disciples, Parrot, at an early date thus described its importance: "It is a

force analogous in all respects to the mechanical forces, a force able to

set matter in motion, or to act as a static force in producing pressure. It

is this force which causes the circulation of heterogeneous matter in the

liquids which serve as its vehicle. It is this force which produces those

actions which escape our notice by their minuteness and bewilder us by

their results. It is for the infinitely small particles of matter what

gravitation is for heavy masses. It can displace matter in solution upwards

against gravity as easily as downwards or in a horizontal direction."

Thus the recognition of the fact that a substance in solution is really a

gas, has at a single stroke put us in possession of the laws of osmotic

pressure--laws slowly and laboriously discovered by the long series of

investigations on the pressure of gases.

Osmotic pressure plays a most important role in the arena of life. It is

found at work in all the phenomena of life. When osmotic pressure fails,

life itself ceases.

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The Mechanism of Life · 第 2 / 13 章