W = Vw0; or w0 = W/V. Also

W = (V + lA)w1; or w1 = W/(V + lA),

w_p = W/(V + plA), and

w_n= W/(V + nlA),

or the densities of the several liquids vary inversely as the

respective volumes of the instrument immersed in them; and, since the

divisions of the scale correspond to equal increments of volume

immersed, it follows that the densities of the several liquids in

which the instrument sinks to the successive divisions form a harmonic

series.

If V = NlA then N expresses the ratio of the volume of the instrument

up to the zero of the scale to that of one of the scale-divisions. If

we suppose the lower part of the instrument replaced by a uniform bar

of the same sectional area as the stem and of volume V, the

indications of the instrument will be in no respect altered, and the

bottom of the bar will be at a distance of N scale-divisions below the

zero of the scale.

In this case we have w_p = W/(N + p)lA; or the density of the liquid

varies inversely as N + p, that is, as the whole number of

scale-divisions between the bottom of the tube and the plane of

flotation.

If we wish the successive divisions of the scale to correspond to

equal increments in the density of the corresponding liquids, then the

volumes of the instrument, measured up to the successive divisions of

the scale, must form a series in harmonical progression, the lengths

of the divisions increasing as we go up the stem.

The greatest density of the liquid for which the instrument described

above can be employed is W/V, while the least density is W/(V + nlA),

or W/(V + v), where v represents the volume of the stem between the

extreme divisions of the scale. Now, by increasing v, leaving W and V

unchanged, we may increase the range of the instrument indefinitely.

But it is clear that if we increase A, the sectional area of the stem,

we shall diminish l, the length of a scale-division corresponding to a

given variation of density, and thereby proportionately diminish the

sensibility of the instrument, while diminishing the section A will

increase l and proportionately increase the sensibility, but will

diminish the range over which the instrument can be employed, unless

we increase the length of the stem in the inverse ratio of the

sectional area. Hence, to obtain great sensibility along with a

considerable range, we require very long slender stems, and to these

two objections apply in addition to the question of portability; for,

in the first place, an instrument with a very long stem requires a

very deep vessel of liquid for its complete immersion, and, in the

second place, when most of the stem is above the plane of flotation,

the stability of the instrument when floating will be diminished or

destroyed. The various devices which have been adopted to overcome

this difficulty will be described in the account given of the several

hydrometers which have been hitherto generally employed.

The plan commonly adopted to obviate the necessity of inconveniently

long stems is to construct a number of hydrometers as nearly alike as

may be, but to load them differently, so that the scale-divisions at

the bottom of the stem of one hydrometer just overlap those at the top

of the stem of the preceding. By this means a set of six hydrometers,

each having a stem rather more than 5 in. long, will be equivalent to

a single hydrometer with a stem of 30 in. But, instead of employing a

number of instruments differing only in the weights with which they

are loaded, we may employ the same instrument, and alter its weight

either by adding mercury or shot to the interior (if it can be opened)

or by attaching weights to the exterior. These two operations are not

quite equivalent, since a weight added to the interior does not affect

the volume of liquid displaced when the instrument is immersed up to a

given division of the scale, while the addition of weights to the

exterior increases the displacement. This difficulty may be met, as in

Keene's hydrometer, by having all the weights of precisely the same

volume but of different masses, and never using the instrument except

with one of these weights attached.

[Illustration: FIG. 2.--Clarke's Hydrometer.]

The first hydrometer intended for the determination of the densities of

liquids, and furnished with a set of weights to be attached when

necessary, was that constructed by Mr Clarke (instrument-maker) and

described by J. T. Desaguliers in the _Philosophical Transactions_ for

March and April 1730, No. 413, p. 278. The following is Desaguliers's

account of the instrument (fig. 2):--

"After having made several fruitless trials with ivory, because it

imbibes spirituous liquors, and thereby alters its gravity, he (Mr

Clarke) at last made a copper hydrometer, represented in fig. 2,

having a brass wire of about 1 in. thick going through, and soldered

into the copper ball Bb. The upper part of this wire is filed flat on

one side, for the stem of the hydrometer, with a mark at m, to which

it sinks exactly in proof spirits. There are two other marks, A and B,

at top and bottom of the stem, to show whether the liquor be (1/10)th

above proof (as when it sinks to A), or (1/10)th under proof (as when

it emerges to B), when a brass weight such as C has been screwed on to

the bottom at c. There are a great many such weights, of different

sizes, and marked to be screwed on instead of C, for liquors that

differ more than (1/10)th from proof, so as to serve for the specific

gravities in all such proportions as relate to the mixture of

spirituous liquors, in all the variety made use of in trade. There are

also other balls for showing the specific gravities quite to common

water, which make the instrument perfect in its kind."

Clarke's hydrometer, as afterwards constructed for the purposes of the

excise, was provided with thirty-two weights to adapt it to spirits of

different specific gravities, and eleven smaller weights, or "weather

weights" as they were called, which were attached to the instrument in

order to correct for variations of temperature. The weights were

adjusted for successive intervals of 5° F., but for degrees intermediate

between these no additional correction was applied. The correction for

temperature thus afforded was not sufficiently accurate for excise

purposes, and William Speer in his essay on the hydrometer (Tilloch's

_Phil. Mag._, 1802, vol. xiv.) mentions cases in which this imperfect

compensation led to the extra duty payable upon spirits which were more

than 10% over proof being demanded on spirits which were purposely

diluted to below 10% over proof in order to avoid the charge. Clarke's

hydrometer, however, remained the standard instrument for excise

purposes from 1787 until it was displaced by that of Sikes.

Desaguliers himself constructed a hydrometer of the ordinary type for

comparing the specific gravities of different kinds of water

(Desaguliers's _Experimental Philosophy_, ii. 234). In order to give

great sensibility to the instrument, the large glass ball was made

nearly 3 in. in diameter, while the stem consisted of a wire 10 in. in

length and only (1/40)in. in diameter. The instrument weighed 4000

grains, and the addition of a grain caused it to sink through an inch.

By altering the quantity of shot in the small balls the instrument could

be adapted for liquids other than water.

To an instrument constructed for the same purpose, but on a still larger

scale than that of Desaguliers, A. Deparcieux added a small dish on the

top of the stem for the reception of the weights necessary to sink the

instrument to a convenient depth. The effect of weights placed in such a

dish or pan is of course the same as if they were placed within the bulb

of the instrument, since they do not alter the volume of that part which

is immersed.

[Illustration: FIG. 3.--Nicholson's Hydrometer.]

The first important improvement in the hydrometer after its reinvention

by Boyle was introduced by G. D. Fahrenheit, who adopted the second mode

of construction above referred to, arranging his instrument so as always

to displace the same volume of liquid, its weight being varied

accordingly. Instead of a scale, only a single mark is placed upon the

stem, which is very slender, and bears at the top a small scale pan into

which weights are placed until the instrument sinks to the mark upon its

stem. The volume of the displaced liquid being then always the same, its

density will be proportional to the whole weight supported, that is, to

the weight of the instrument together with the weights required to be

placed in the scale pan.

Nicholson's hydrometer (fig. 3) combines the characteristics of

Fahrenheit's hydrometer and of Boyle's essay instrument.[2] The

following is the description given of it by W. Nicholson in the

_Manchester Memoirs_, ii. 374:--

"AA represents a small scale. It may be taken off at D. Diameter 1½

in., weight 44 grains.

"B a stem of hardened steel wire. Diameter 1/100 in.

"E a hollow copper globe. Diameter 2(8/10) in. Weight with stem 369

grains.

"FF a stirrup of wire screwed to the globe at C.

"G a small scale, serving likewise as a counterpoise. Diameter 1½ in.

Weight with stirrup 1634 grains.

"The other dimensions may be had from the drawing, which is one-sixth

of the linear magnitude of the instrument itself.

"In the construction it is assumed that the upper scale shall

constantly carry 1000 grains when the lower scale is empty, and the

instrument sunk in distilled water at the temperature of 60° Fahr. to

the middle of the wire or stem. The length of the stem is arbitrary,

as is likewise the distance of the lower scale from the surface of the

globe. But, the length of the stem being settled, the lower scale may

be made lighter, and, consequently, the globe less, the greater its

distance is taken from the surface of the globe; and the contrary."

In comparing the densities of different liquids, it is clear that this

instrument is precisely equivalent to that of Fahrenheit, and must be

employed in the same manner, weights being placed in the top scale only

until the hydrometer sinks to the mark on the wire, when the specific

gravity of the liquid will be proportional to the weight of the

instrument together with the weights in the scale.

In the subsequent portion of the paper above referred to, Nicholson

explains how the instrument may be employed as a thermometer, since,

fluids generally expanding more than the solids of which the instrument

is constructed, the instrument will sink as the temperature rises.

To determine the density of solids heavier than water with this

instrument, let the solid be placed in the upper scale pan, and let

the weight now required to cause the instrument to sink in distilled

water at standard temperature to the mark B be denoted by w, while W

denotes the weight required when the solid is not present. Then W - w

is the weight of the solid. Now let the solid be placed in the lower

pan, care being taken that no bubbles of air remain attached to it,

and let w1 be the weight now required in the scale pan. This weight

will exceed w in consequence of the water displaced by the solid, and

the weight of the water thus displaced will be W1 - w, which is

therefore the weight of a volume of water equal to that of the solid.

Hence, since the weight of the solid itself is W - w, its density must

be (W - w)/(w1 - w).

The above example illustrates how Nicholson's or Fahrenheit's hydrometer

may be employed as a weighing machine for small weights.

In all hydrometers in which a part only of the instrument is immersed,

there is a liability to error in consequence of the surface tension, or

capillary action, as it is frequently called, along the line of contact

of the instrument and the surface of the liquid (see CAPILLARY ACTION).

This error diminishes as the diameter of the stem is reduced, but is

sensible in the case of the thinnest stem which can be employed, and is

the chief source of error in the employment of Nicholson's hydrometer,

which otherwise would be an instrument of extreme delicacy and

precision. The following is Nicholson's statement on this point:--

"One of the greatest difficulties which attends hydrostatical

experiments arises from the attraction or repulsion that obtains at

the surface of the water. After trying many experiments to obviate the

irregularities arising from this cause, I find reason to prefer the

simple one of carefully wiping the whole instrument, and especially

the stem, with a clean cloth. The weights in the dish must not be

esteemed accurate while there is either a cumulus or a cavity in the

water round the stem."

It is possible by applying a little oil to the upper part of the bulb of

a common or of a Sikes's hydrometer, and carefully placing it in pure

water, to cause it to float with the upper part of the bulb and the

whole of the stem emerging as indicated in fig. 4, when it ought

properly to sink almost to the top of the stem, the surface tension of

the water around the circumference of the circle of contact, AA',

providing the additional support required.

[Illustration: FIG. 4.]

The universal hydrometer of G. Atkins, described in the _Phil. Mag._

for 1808, xxxi. 254, is merely Nicholson's hydrometer with the screw

at C projecting through the collar into which it is screwed, and

terminating in a sharp point above the cup G. To this point soft

bodies lighter than water (which would float if placed in the cup)

could be attached, and thus completely immersed. Atkins's instrument

was constructed so as to weigh 700 grains, and when immersed to the

mark on the stem in distilled water at 60° F. it carried 300 grains in

the upper dish. The hydrometer therefore displaced 1000 grains of

distilled water at 60° F. and hence the specific gravity of any other

liquid was at once indicated by adding 700 to the number of grains in

the pan required to make the instrument sink to the mark on the stem.

The small divisions on the scale corresponded to differences of

(1/10)th of a grain in the weight of the instrument.

The "Gravimeter," constructed by Citizen Guyton and described in

_Nicholson's Journal_, 4to, i. 110, differs from Nicholson's

instrument in being constructed of glass, and having a cylindrical

bulb about 21 centimetres in length and 22 millimetres in diameter.

Its weight is so adjusted that an additional weight of 5 grammes must

be placed in the upper pan to cause the instrument to sink to the mark

on the stem in distilled water at the standard temperature. The

instrument is provided with an additional piece, or "plongeur," the

weight of which exceeds 5 grammes by the weight of water which it

displaces; that is to say, it is so constructed as to weigh 5 grammes

in water, and consists of a glass envelope filled with mercury. It is

clear that the effect of this "plongeur," when placed in the lower

pan, is exactly the same as that of the 5 gramme weight in the upper

pan. Without the extra 5 grammes the instrument weighs about 20

grammes, and therefore floats in a liquid of specific gravity .8. Thus

deprived of its additional weight it may be used for spirits. To use

the instrument for liquids of much greater density than water

additional weights must be placed in the upper pan, and the "plongeur"

is then placed in the lower pan for the purpose of giving to the

instrument the requisite stability.

Charles's balance areometer is similar to Nicholson's hydrometer,

except that the lower basin admits of inversion, thus enabling the

instrument to be employed for solids lighter than water, the inverted

basin serving the same purpose as the pointed screw in Atkins's

modification of the instrument.

Adie's sliding hydrometer is of the ordinary form, but can be adjusted

for liquids of widely differing specific gravities by drawing out a

sliding tube, thus changing the volume of the hydrometer while its

weight remains constant.

The hydrometer of A. Baumé, which has been extensively used in France,

consists of a common hydrometer graduated in the following manner.

Certain fixed points were first determined upon the stem of the

instrument. The first of these was found by immersing the hydrometer

in pure water, and marking the stem at the level of the surface. This

formed the zero of the scale. Fifteen standard solutions of pure

common salt in water were then prepared, containing respectively 1, 2,

3, ... 15% (by weight) of dry salt. The hydrometer was plunged in

these solutions in order, and the stem having been marked at the

several surfaces, the degrees so obtained were numbered 1, 2, 3, ...

15. These degrees were, when necessary, repeated along the stem by the

employment of a pair of compasses till 80 degrees were marked off. The

instrument thus adapted to the determination of densities exceeding

that of water was called the hydrometer for salts.

The hydrometer intended for densities less than that of water, or the

hydrometer for spirits, is constructed on a similar principle. The

instrument is so arranged that it floats in pure water with most of

the stem above the surface. A solution containing 10% of pure salt is

used to indicate the zero of the scale, and the point at which the

instrument floats when immersed in distilled water at 10° R. (54½° F.)

is numbered 10. Equal divisions are then marked off upwards along the

stem as far as the 50th degree.

The densities corresponding to the several degrees of Baumé's

hydrometer are given by Nicholson (_Journal of Philosophy_, i. 89) as

follows:--

_Baumé's Hydrometer for Spirits. Temperature 10° R._

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

|Degrees.|Density.|Degrees.|Density.|Degrees.|Density.|

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

| 10 | 1.000 | 21 | .922 | 31 | .861 |

| 11 | .990 | 22 | .915 | 32 | .856 |

| 12 | .985 | 23 | .909 | 33 | .852 |

| 13 | .977 | 24 | .903 | 34 | .847 |

| 14 | .970 | 25 | .897 | 35 | .842 |

| 15 | .963 | 26 | .892 | 36 | .837 |

| 16 | .955 | 27 | .886 | 37 | .832 |

| 17 | .949 | 28 | .880 | 38 | .827 |

| 18 | .943 | 29 | .874 | 39 | .822 |

| 19 | .935 | 30 | .867 | 40 | .817 |

| 20 | .928 | | | | |

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

_Baume's Hydrometer for Salts._

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

|Degrees.|Density.|Degrees.|Density.|Degrees.|Density.|

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

| 0 | 1.000 | 27 | 1.230 | 51 | 1.547 |

| 3 | 1.020 | 30 | 1.261 | 54 | 1.594 |

| 6 | 1.040 | 33 | 1.295 | 57 | 1.659 |

| 9 | 1.064 | 36 | 1.333 | 60 | 1.717 |

| 12 | 1.089 | 39 | 1.373 | 63 | 1.779 |

| 15 | 1.114 | 42 | 1.414 | 66 | 1.848 |

| 18 | 1.140 | 45 | 1.455 | 69 | 1.920 |

| 21 | 1.170 | 48 | 1.500 | 72 | 2.000 |

| 24 | 1.200 | | | | |

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

Carrier's hydrometer was very similar to that of Baumé, Cartier having

been employed by the latter to construct his instruments for the

French revenue. The point at which the instrument floated in distilled

water was marked 10° by Cartier, and 30° on Carrier's scale

corresponded to 32° on Baumé's.

Perhaps the main object for which hydrometers have been constructed is

the determination of the value of spirituous liquors, chiefly for

revenue purposes. To this end an immense variety of hydrometers have

been devised, differing mainly in the character of their scales.

In Speer's hydrometer the stem has the form of an octagonal prism, and

upon each of the eight faces a scale is engraved, indicating the

percentage strength of the spirit corresponding to the several

divisions of the scale, the eight scales being adapted respectively to

the temperature 35°, 40°, 45°, 50°, 55°, 60°, 65° and 70° F. Four

small pins, which can be inserted into the counterpoise of the

instrument, serve to adapt the instrument to the temperatures

intermediate between those for which the scales are constructed.

William Speer was supervisor and chief assayer of spirits in the port

of Dublin. For a more complete account of this instrument see

Tilloch's _Phil. Mag._, xiv. 151.

[Illustration: FIG. 5.--Jones's Hydrometer.]

The hydrometer constructed by Jones, of Holborn, consists of a

spheroidal bulb with a rectangular stem (fig. 5). Between the bulb and

counterpoise is placed a thermometer, which serves to indicate the

temperature of the liquid, and the instrument is provided with three

weights which can be attached to the top of the stem. On the four

sides of the stem AD are engraved four scales corresponding

respectively to the unloaded instrument, and to the instrument loaded

with the respective weights. The instrument when unloaded serves for

the range from 74 to 47 over proof; when loaded with the first weight

it indicates from 46 to 13 over proof, with the second weight from 13

over proof to 29 under proof, and with the third from 29 under proof

to pure water, the graduation corresponding to which is marked W at

the bottom of the fourth scale. One side of the stem AD is shown in

fig. 5, the other three in fig. 6. The thermometer is also provided

with four scales corresponding to the scales above mentioned. Each

scale has its zero in the middle corresponding to 60° F. If the

mercury in the thermometer stand above this zero the spirit must be

reckoned weaker than the hydrometer indicates by the number on the

thermometer scale level with the top of the mercury, while if the

thermometer indicate a temperature lower than the zero of the scale

(60° F.) the spirit must be reckoned stronger by the scale reading. At

the side of each of the four scales on the stem of the hydrometer is

engraved a set of small numbers indicating the contraction in volume

which would be experienced if the requisite amount of water (or

spirit) were added to bring the sample tested to the proof strength.

[Illustration: FIG. 6.]

The hydrometer constructed by Dicas of Liverpool is provided with a

sliding scale which can be adjusted for different temperatures, and

which also indicates the contraction in volume incident on bringing

the spirit to proof strength. It is provided with thirty-six different

weights which, with the ten divisions on the stem, form a scale from 0

to 370. The employment of so many weights renders the instrument

ill-adapted for practical work where speed is an object.

[Illustration: FIG. 7.--Atkins's Hydrometer.]

This instrument was adopted by the United States in 1790, but was

subsequently discarded by the Internal Revenue Service for another

type. In this latter form the observations have to be made at the

standard temperature of 60° F., at which the graduation 100

corresponds to proof spirit and 200 to absolute alcohol. The need of

adjustable weights is avoided by employing a set of five instruments,

graduated respectively 0°-100°, 80°-120°, 100°-140°, 130°-170°,

160°-200°. The reading gives the volume of proof spirit equivalent to

the volume of liquor; thus the readings 80° and 120° mean that 100

volumes of the test liquors contain the same amount of absolute

alcohol as 80 and 120 volumes of proof spirit respectively. Proof

spirit is defined in the United States as a mixture of alcohol and

water which contains equal volumes of alcohol and water at 60° F., the

alcohol having a specific gravity of 0.7939 at 60° as compared with

water at its maximum density. The specific gravity of proof spirit is

0.93353 at 60°; and 100 volumes of the mixture is made from 50 volumes

of absolute alcohol and 53.71 volumes of water.

Quin's universal hydrometer is described in the _Transactions of the

Society of Arts_, viii. 98. It is provided with a sliding rule to

adapt it to different temperatures, and has four scales, one of which

is graduated for spirits and the other three serve to show the

strengths of worts. The peculiarity of the instrument consists in the

pyramidal form given to the stem, which renders the scale-divisions

more nearly equal in length than they would be on a prismatic stem.

Atkins's hydrometer, as originally constructed, is described in

_Nicholson's Journal_, 8vo, ii. 276. It is made of brass, and is

provided with a spheroidal bulb the axis of which is 2 in. in length,

the conjugate diameter being 1½ in. The whole length of the instrument

is 8 in., the stem square of about 1/8-in. side, and the weight about

400 grains. It is provided with four weights, marked 1, 2, 3, 4, and

weighing respectively 20, 40, 61 and 84 grains, which can be attached

to the shank of the instrument at C (fig. 7) and retained there by the

fixed weight B. The scale engraved upon one face of the stem contains

fifty-five divisions, the top and bottom being marked 0 or zero and

the alternate intermediate divisions (of which there are twenty-six)

being marked with the letters of the alphabet in order. The four

weights are so adjusted that, if the instrument floats with the stem

emerging as far as the lower division 0 with one of the weights

attached, then replacing the weight by the next heavier causes the

instrument to sink through the whole length of the scale to the upper

division 0, and the first weight produces the same effect when applied

to the naked instrument. The stem is thus virtually extended to five

times its length, and the number of divisions increased practically to

272. When no weight is attached the instrument indicates densities

from .806 to .843; with No. 1 it registers from .843 to .880, with No.

2 from .880 to .918, with No. 3 from .918 to .958, and with No. 4 from

.958 to 1.000, the temperature being 55° F. It will thus be seen that

the whole length of the stem corresponds to a difference of density of

about .04, and one division to about .00074, indicating a difference

of little more than 1/3% in the strength of any sample of spirits.

The instrument is provided with a sliding rule, with scales

corresponding to the several weights, which indicate the specific

gravity corresponding to the several divisions of the hydrometer scale

compared with water at 55° F. The slider upon the rule serves to

adjust the scale for different temperatures, and then indicates the

strength of the spirit in percentages over or under proof. The slider

is also provided with scales, marked respectively Dicas and Clarke,

which serve to show the readings which would have been obtained had

the instruments of those makers been employed. The line on the scale

marked "concentration" indicates the diminution in volume consequent

upon reducing the sample to proof strength (if it is _over proof_,

O.P.) or upon reducing proof spirit to the strength of the sample (if

it is _under proof_, U.P.). By applying the several weights in

succession in addition to No. 4 the instrument can be employed for

liquids heavier than water; and graduations on the other three sides

of the stem, together with an additional slide rule, adapt the

instrument for the determination of the strength of worts.

Atkins subsequently modified the instrument (_Nicholson's Journal_,

8vo, iii. 50) by constructing the different weights of different

shapes, viz. circular, square, triangular and pentagonal, instead of

numbering them 1, 2, 3 and 4 respectively, a figure of the weight

being stamped on the sliding rule opposite to every letter in the

series to which it belongs, thus diminishing the probability of

mistakes. He also replaced the letters on the stem by the

corresponding specific gravities referred to water as unity. Further

information concerning these instruments and the state of hydrometry

in 1803 will be found in Atkins's pamphlet _On the Relation between

the Specific Gravities and the Strength of Spirituous Liquors_ (1803);

or _Phil. Mag._ xvi. 26-33, 205-212, 305-312; xvii. 204-210 and

329-341.

In Gay-Lussac's alcoholometer the scale is divided into 100 parts

corresponding to the presence of 1, 2, ... % by volume of alcohol at

15° C., the highest division of the scale corresponding to the purest

alcohol he could obtain (density .7947) and the lowest division

corresponding to pure water. A table provides the necessary

corrections for other temperatures.

Tralles's hydrometer differs from Gay-Lussac's only in being graduated

at 4° C. instead of 15° C., and taking alcohol of density .7939 at

15.5° C. for pure alcohol instead of .7947 as taken by Gay-Lussac

(Keene's _Handbook of Hydrometry_).

In Beck's hydrometer the zero of the scale corresponds to density

1.000 and the division 30 to density .850, and equal divisions on the

scale are continued as far as is required in both directions.

[Illustration: FIG. 8.--Sike's Hydrometer.]

In the centesimal hydrometer of Francoeur the volume of the stem

between successive divisions of the scale is always (1/100)th of the

whole volume immersed when the instrument floats in water at 4° C. In

order to graduate the stem the instrument is first weighed, then

immersed in distilled water at 4° C., and the line of flotation marked

zero. The first degree is then found by placing on the top of the stem

a weight equal to (1/100)th of the weight of the instrument, which

increases the volume immersed by (1/100)th of the original volume. The

addition to the top of the stem of successive weights, each (1/100)th

of the weight of the instrument itself, serves to determine the

successive degrees. The length of 100 divisions of the scale, or the

length of the uniform stem the volume of which would be equal to that

of the hydrometer up to the zero graduation, Francoeur called the

"modulus" of the hydrometer. He constructed his instruments of glass,

using different instruments for different portions of the scale

(Francoeur, _Traité d'aréométrie_, Paris, 1842).

Dr Boriés of Montpellier constructed a hydrometer which was based upon

the results of his experiments on mixtures of alcohol and water. The

interval between the points corresponding to pure alcohol and to pure

water Boriés divided into 100 equal parts, though the stem was

prolonged so as to contain only 10 of these divisions, the other 90

being provided for by the addition of 9 weights to the bottom of the

instrument as in Clarke's hydrometer.

The instrument which has now been exclusively used for revenue

purposes for nearly a century is that associated with the name of

Bartholomew Sikes, who was correspondent to the Board of Excise from

1774 to 1783, and for some time collector of excise for Hertfordshire.

Sikes's hydrometer, on account of its similarity to that of Boriés,

appears to have been borrowed from that instrument. It is made of

gilded brass or silver, and consists of a spherical ball A (fig. 8),

1.5 in. in diameter, below which is a weight B connected with the ball

by a short conical stem C. The stem D is rectangular in section and

about 3½ in. in length. This is divided into ten equal parts, each of

which is subdivided into five. As in Boriés's instrument, a series of

9 weights, each of the form shown at E, serves to extend the scale to

100 principal divisions. In the centre of each weight is a hole

capable of admitting the lowest and thickest end of the conical stem

C, and a slot is cut into it just wide enough to allow the upper part

of the cone to pass. Each weight can thus be dropped on to the lower

stem so as to rest on the counterpoise B. The weights are marked 10,

20, ... 90; and in using the instrument that weight must be selected

which will allow it to float in the liquid with a portion only of the

stem submerged. Then the reading of the scale at the line of

flotation, added to the number on the weight, gives the reading

required. A small supernumerary weight F is added, which can be placed

upon the top of the stem. F is so adjusted that when the 60 weight is

placed on the lower stem the instrument sinks to the same point in

distilled water when F is attached as in proof spirit when F is

removed. The best instruments are now constructed for revenue purposes

of silver, heavily gilded, because it was found that saccharic acid

contained in some spirits attacked brass behind the gilding.

The following table gives the specific gravities corresponding to the

principal graduations on Sikes's hydrometer at 60° F. and 62° F.,

together with the corresponding strengths of spirits. The latter are

based upon the tables of Charles Gilpin, clerk to the Royal Society,

for which the reader is referred to the _Phil. Trans._ for 1794.

Gilpin's work is a model for its accuracy and thoroughness of detail,

and his results have scarcely been improved upon by more recent

workers. The merit of Sikes's system lies not so much in the

hydrometer as in the complete system of tables by which the readings

of the instrument are at once converted into percentage of

proof-spirit.

_Table showing the Densities corresponding to the Indications of

Sike's Hydrometer._

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

| | 60° F. | 62° F. |

| +---------+--------+---------+--------+

| Sike's | Proof | | Proof | |

|Indications.| Spirit |Density.| Spirit |Density.|

| |per cent.| |per cent.| |

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

| 0 | .815297 | 167.0 | .815400 | 166.5 |

| 1 | .816956 | 166.1 | .817059 | 165.6 |

| 2 | .818621 | 165.3 | .818725 | 164.8 |

| 3 | .820294 | 164.5 | .820397 | 163.9 |

| 4 | .821973 | 163.6 | .822077 | 163.1 |

| 5 | .823659 | 162.7 | .823763 | 162.3 |

| 6 | .825352 | 161.8 | .825457 | 161.4 |

| 7 | .827052 | 160.9 | .827157 | 160.5 |

| 8 | .828759 | 160.0 | .828864 | 159.6 |

| 9 | .830473 | 159.1 | .830578 | 158.7 |

| 10 | .832195 | 158.2 | .832300 | 157.8 |

| 11 | .833888 | 157.3 | .833993 | 156.8 |

| 12 | .835587 | 156.4 | .835692 | 155.9 |

| 13 | .837294 | 155.5 | .837400 | 155.0 |

| 14 | .839008 | 154.6 | .839114 | 154.0 |

| 15 | .840729 | 153.7 | .840835 | 153.1 |

| 16 | .842458 | 152.7 | .842564 | 152.1 |

| 17 | .844193 | 151.7 | .844299 | 151.1 |

| 18 | .845936 | 150.7 | .846042 | 150.1 |

| 19 | .847685 | 149.7 | .847792 | 149.1 |

| 20 | .849442 | 148.7 | .849549 | 148.1 |

| 20B | .849393 | 148.7 | .849500 | 148.1 |

| 21 | .851122 | 147.6 | .851229 | 147.1 |

| 22 | .852857 | 146.6 | .852964 | 146.1 |

| 23 | .854599 | 145.6 | .854707 | 145.1 |

| 24 | .856348 | 144.6 | .856456 | 144.0 |

| 25 | .858105 | 143.5 | .858213 | 142.9 |

| 26 | .859869 | 142.4 | .859978 | 141.8 |

| 27 | .861640 | 141.3 | .861749 | 140.8 |

| 28 | .863419 | 140.2 | .863528 | 139.7 |

| 29 | .865204 | 139.1 | .865313 | 138.5 |

| 30 | .866998 | 138.0 | .867107 | 137.4 |

| 30B | .866991 | 138.0 | .867100 | 137.4 |

| 31 | .868755 | 136.9 | .868865 | 136.2 |

| 32 | .870526 | 135.7 | .870636 | 135.1 |

| 33 | .872305 | 134.5 | .872415 | 133.9 |

| 34 | .874090 | 133.4 | .874200 | 132.8 |

| 35 | .875883 | 132.2 | .873994 | 131.6 |

| 36 | .877684 | 131.0 | .877995 | 130.4 |

| 37 | .879492 | 129.8 | .879603 | 129.1 |

| 38 | .881307 | 128.5 | .881419 | 127.9 |

| 39 | .883129 | 127.3 | .883241 | 126.7 |

| 40 | .884960 | 126.0 | .885072 | 125.4 |

| 40B | .884888 | 126.0 | .885000 | 125.4 |

| 41 | .886689 | 124.8 | .886801 | 124.2 |

| 42 | .888497 | 123.5 | .888609 | 122.9 |

| 43 | .890312 | 122.2 | .890425 | 121.6 |

| 44 | .892135 | 120.9 | .892248 | 120.3 |

| 45 | .893965 | 119.6 | .894078 | 119.0 |

| 46 | .895803 | 118.3 | .895916 | 117.6 |

| 47 | .897647 | 116.9 | .897761 | 116.3 |

| 48 | .899509 | 115.6 | .899614 | 114.9 |

| 49 | .901360 | 114.2 | .901417 | 113.5 |

| 50 | .903229 | 112.8 | .903343 | 112.1 |

| 50B | .903186 | 112.8 | .903300 | 112.1 |

| 51 | .905024 | 111.4 | .905138 | 110.7 |

| 52 | .906869 | 110.0 | .906983 | 109.3 |

| 53 | .908722 | 108.6 | .908837 | 107.9 |

| 54 | .910582 | 107.1 | .910697 | 106.5 |

| 55 | .912450 | 105.6 | .912565 | 105.0 |

| 56 | .914326 | 104.2 | .914441 | 103.5 |

| 57 | .916209 | 102.7 | .916323 | 102.0 |

| 58 | .918100 | 101.3 | .918216 | 100.5 |

| 59 | .919999 | 99.7 | .820115 | 98.9 |

| 60 | .921906 | 98.1 | .922022 | 97.4 |

| 60B | .921884 | 98.1 | .922000 | 97.4 |

| 61 | .923760 | 96.6 | .923877 | 95.9 |

| 62 | .925643 | 95.0 | .925760 | 94.2 |

| 63 | .927534 | 93.3 | .927652 | 92.6 |

| 64 | .929433 | 91.7 | .929550 | 90.9 |

| 65 | .931339 | 90.0 | .931457 | 89.2 |

| 66 | .933254 | 88.3 | .933372 | 87.5 |

| 67 | .935176 | 86.5 | .935294 | 85.8 |

| 68 | .937107 | 84.7 | .937225 | 84.0 |

| 69 | .939045 | 82.9 | .939163 | 82.2 |

| 70 | .940991 | 81.1 | .941110 | 80.3 |

| 70B | .940981 | 81.1 | .941100 | 80.3 |

| 71 | .942897 | 79.2 | .943016 | 78.4 |

| 72 | .944819 | 77.3 | .944938 | 76.5 |

| 73 | .946749 | 75.3 | .946869 | 74.5 |

| 74 | .948687 | 73.3 | .948807 | 72.5 |

| 75 | .950634 | 71.2 | .950753 | 70.4 |

| 76 | .952588 | 69.0 | .952708 | 68.2 |

| 77 | .954550 | 66.8 | .954670 | 66.0 |

| 78 | .956520 | 64.4 | .956641 | 63.5 |

| 79 | .958498 | 61.9 | .958619 | 61.1 |

| 80 | .960485 | 59.4 | .960606 | 58.5 |

| 80B | .960479 | 59.4 | .960600 | 58.5 |

| 81 | .962433 | 56.7 | .962555 | 55.8 |

| 82 | .964395 | 53.9 | .964517 | 53.0 |

| 83 | .966366 | 50.9 | .966488 | 50.0 |

| 84 | .968344 | 47.8 | .968466 | 47.0 |

| 85 | .970331 | 44.5 | .970453 | 43.8 |

| 86 | .972325 | 41.0 | .972448 | 40.4 |

| 87 | .974328 | 37.5 | .974451 | 36.9 |

| 88 | .976340 | 34.0 | .976463 | 33.5 |

| 89 | .978359 | 30.6 | .978482 | 30.1 |

| 90 | .980386 | 27.2 | .980510 | 26.7 |

| 90B | .980376 | 27.2 | .980500 | 26.7 |

| 91 | .982371 | 23.9 | .982496 | 23.6 |

| 92 | .984374 | 20.8 | .984498 | 20.5 |

| 93 | .986385 | 17.7 | .986510 | 17.4 |

| 94 | .988404 | 14.8 | .988529 | 14.5 |

| 95 | .990431 | 12.0 | .990557 | 11.7 |

| 96 | .992468 | 9.3 | .992593 | 9.0 |

| 97 | .994512 | 6.7 | .994637 | 6.5 |

| 98 | .996565 | 4.1 | .996691 | 4.0 |

| 99 | .998626 | 1.8 | .998752 | 1.6 |

| 100 |1.000696 | 0.0 |1.000822 | 0.0 |

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

In the above table for Sikes's hydrometer two densities are given

corresponding to each of the degrees 20, 30, 40, 50, 60, 70, 80 and

90, indicating that the successive weights belonging to the particular

instrument for which the table has been calculated do not quite agree.

The discrepancy, however, does not produce any sensible error in the

strength of the corresponding spirit.

A table which indicates the weight per gallon of spirituous liquors

for every degree of Sikes's hydrometer is printed in 23 and 24 Vict.

c. 114, schedule B. This table differs slightly from that given above,

which has been abridged from the table given in Keene's _Handbook of

Hydrometry_, apparently on account of the equal divisions on Sikes's

scale having been taken as corresponding to equal increments of

density.

Sikes's hydrometer was established for the purpose of collecting the

revenue of the United Kingdom by Act of Parliament, 56 Geo. III. c.

140, by which it was enacted that "all spirits shall be deemed and

taken to be of the degree of strength which the said hydrometers

called Sikes's hydrometers shall, upon trial by any officer or

officers of the customs or excise, denote such spirits to be." This

act came into force on January 5, 1817, and was to have remained in

force until August 1, 1818, but was repealed by 58 Geo. III. c. 28,

which established Sikes's hydrometer on a permanent footing. By 3 and

4 Will. IV. c. 52, § 123, it was further enacted that the same

instruments and methods should be employed in determining the duty

upon imported spirits as should in virtue of any Act of Parliament be

employed in the determination of the duty upon spirits distilled at

home. It is the practice of the officers of the inland revenue to

adjust Sikes's hydrometer at 62° F., that being the temperature at

which the imperial gallon is defined as containing 10 lb. avoirdupois

of distilled water. The specific gravity of any sample of spirits thus

determined, when multiplied by ten, gives the weight in pounds per

imperial gallon, and the weight of any bulk of spirits divided by this

number gives its volume at once in imperial gallons.

Mr (afterwards Colonel) J. B. Keene, of the Hydrometer Office, London,

has constructed an instrument after the model of Sikes's, but provided

with twelve weights of different masses but equal volumes, and the

instrument is never used without having one of these attached. When

loaded with either of the lightest two weights the instrument is

specifically lighter than Sikes's hydrometer when unloaded, and it may

thus be used for specific gravities as low as that of absolute

alcohol. The volume of each weight being the same, the whole volume

immersed is always the same when it floats at the same mark whatever

weight may be attached.

Besides the above, many hydrometers have been employed for special

purposes. Twaddell's hydrometer is adapted for densities greater than

that of water. The scale is so arranged that the reading multiplied by

5 and added to 1000 gives the specific gravity with reference to water

as 1000. To avoid an inconveniently long stem, different instruments

are employed for different parts of the scale as mentioned above.

The lactometer constructed by Dicas of Liverpool is adapted for the

determination of the quality of milk. It resembles Sikes's hydrometer

in other respects, but is provided with eight weights. It is also

provided with a thermometer and slide rule, to reduce the readings to

the standard temperature of 55° F. Any determination of density can be

taken only as affording prima facie evidence of the quality of milk,

as the removal of cream and the addition of water are operations which

tend to compensate each other in their influence on the density of the

liquid, so that the lactometer cannot be regarded as a reliable

instrument.

The marine hydrometers, as supplied by the British government to the

royal navy and the merchant marine, are glass instruments with slender

stems, and generally serve to indicate specific gravities from 1.000

to 1.040. Before being issued they are compared with a standard

instrument, and their errors determined. They are employed for taking

observations of the density of sea-water.

The salinometer is a hydrometer originally intended to indicate the

strength of the brine in marine boilers in which sea-water is

employed. Saunders's salinometer consists of a hydrometer which floats

in a chamber through which the water from the boiler is allowed to

flow in a gentle stream, at a temperature of 200° F. The peculiarity

of the instrument consists in the stream of water, as it enters the

hydrometer chamber, being made to impinge against a disk of metal, by

which it is broken into drops, thus liberating the steam, which would

otherwise disturb the instrument.

The use of Sikes's hydrometer necessitates the employment of a

considerable quantity of spirit. For the testing of spirits in bulk no

more convenient instrument has been devised, but where very small

quantities are available more suitable laboratory methods must be

adopted.

In England, the Finance Act 1907 (7 Ed. VII. c. 13), section 4,

provides as follows: (1) The Commissioners of Customs and the

Commissioners of Inland Revenue may jointly make regulations

authorizing the use of any means described in the regulations for

ascertaining for any purpose the strength or weight of spirits. (2)

Where under any enactment Sykes's (sic) Hydrometer is directed to be

used or may be used for the purpose of ascertaining the strength or

weight of spirits, any means so authorized by regulations may be used

instead of Sykes's Hydrometer and references to Sykes's Hydrometer in

any enactment shall be construed accordingly. (3) Any regulations made

under this section shall be published in the London, Edinburgh and

Dublin Gazette, and shall take effect from the date of publication, or

such later date as may be mentioned in the regulations for the

purpose. (4) The expression "spirits" in this section has the same

meaning as in the Spirits Act 1880. (W. G.)

Encyclopaedia Britannica, 11th Edition, "Hydromechanics" to "Ichnography" Volume 14, Slice 2 · 第 102 / 120 题