Correlating Solubility and Distribution Coefficient Data

of Brooklyn, Brooklyn 2, V, Y. PREVIOUSLY, many physical properties of systems contain- ing solids, liquids, and gases have been correlated by a simpl...
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Correlating Solubility a istribution Coe DONALD F. OTHhlER AND MAHESH S. THAKAR Polytechnic I n s t i t u t e of Brooklyn, Brooklyn 2 , -1'.Y .

REVIOUSLY, many physical properties of systems containing solids, liquids, and gases have been correlated by a simple method of logarithmic plotting and correspondingly simple algebraic equations. For vapor pressures and latent heate the tollowing equation applies ( S ) , log 'I

=

A log P' L'

+c

(1)

cated in the regular way from the corresponding vapor pressure of water as the reference substance. All data were taken from ( 2 ) . In most cases correlation is good and straight lines are obtainod over wide temperature ranges. In gome cases the straight line shows a sharp break with a consequent change in slope. This break is obviously due to the change of a physical or a chemical nature of the subst.ance at, t h a t particular temperature. Thus, in the case of sodium sulfate, a sharp break in the straight line occurs a t 36" C. where the sodium sulfate decahydrate, NazSOc.lOHzO, changes to its anhydrous form, SaeSOr. One advantage of this method of plotting is that it helps t o locate the transition point wherc such a physical or chemical change occurs more precisely than is possible by intersection of curved lines of empirical shape. The equat,ion may be expressed for these lines representing solubilities, x, expressed as mole per cents.

where at the %me tempei ature P and P' are vapor pressures and L and L' are molal latent heats, respectively, of two compounds a n d C is a constant Log P' actually serves as a temperature scale which can be obtained directly from vapor pressure data of standard substances. LIL' 16 nearly independent of temperature and a logarithmic plot of P versus P' gives substantially a straight line whose slope L / L ' provides latent heat data a t any temperature for the compound in question from that of the reference substance. This method of plotting has been applied t o correlate as straight linea othei properties, such as gas solubilities and partial log z = L 7 f log P' c (2) I, pressures, adsorption pressure, vapor compositions, equilibrium constants, activity coefficients, relative volatility, electromotive If z,/L', where tfis equal to (6,- h,) and L' is the molal latent force, and viscosities (4-8). The slopes of these lines have been heat of vaporization of the wfercnce liquid, is assumed to remain identified in each case with the heat effects accompanying nearly constant, it is obthe chemical or physical vious that a plot of solubilichange. TEMPE R A T U RE,OC. ties versus the vapor presIn most cases an algesures of the reference liquid braic equation is not needed at the same temperatures .and the property can be M-ill give a straight line on p l o t t e d d i r e c t l y on a standard logarithmic paper. logarithmic paper by the For some solutes, such following steps: as sucrose in water, the 1. Plot vapor pressure plot gives a slight curve of t,he reference substance because of the very major on the X axis and calideviations from Raoult's brate it by indicating ('orreor Henry's l a w s . T h e s e sponding temperatures from a standard table a t respecirregular cases are probat,ive vapor pressures. bly due to high solubility, 2. Plot the values of the high molecular weight, and property in question on the possible varying hydration appropriate t e m e r a t u r e lines against t i e correof the solute molecules. sponding Y axis scale. 3. Connect t,he points so APPLICATION TO DISTRIobtained by a, straight line. BUTION COEFFICIENTS

+

APPLICATION T O SOLUBILITY DATA

Solubility data of solidh in Liquids can be plotted by t h e method indicated. Figure 1 indicates such a plot for s e v e r a l s u b s t a n c e e , w h e r e s o l u b i l i t i e s expressed in mole fraction (or per cent) of different solids in water are plotted versus temperature, indi-

VAPOR Figure 1. 1. 2. 3.

4.

L

P R E S S U R E OF mm. H g

WATER

Logarithmic Plot of Solubility i n Water against Vapor Pressure of Water

Urea Sucrose Ammonium sulfate Copper sulfate (a) Copper sulfate (PI

fi. Sodium sulfate (anhydrous)

7.

Sodium sulfate (decahydrate) Potassium permanganate 9. Calcium hydrodde 8.

46.34

Distribution coefficients of a solute between two solvent layers are closely related t o the solubility of the solute in either of the solvents. T h e r e f o r e , i t should be possible to correlate the variation of distribution coefficients with t e m p e r a t u r e as straight lines b y following t h e method of plotting indicated previously.

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cases of the van’t Hoff equation and can be found in standard textbooks on physical chemistry and chemical thermodynamics.

TEMPERATURE. O C .

d l o g x = - Lf dT RT2

(4))

or integrating logx =

A

+B

If Equation 4 is divided by the Clausius-Clapeyron equation, always a t bhe same temperature

L‘

d log P’ = - d7’

RT2

there follou7s d log2 ___

d log P’

-

=LL’r

This,on integrating, assuming zf/L‘ to remain constant, yields approximately log

VAPOR

PRESSURE OF WATER

mm. Hg Figure 2. Legarithmic Plot of Distribution Coefficients of Various SubBtances between Various Solvents and Water Data multiplied by 10 1. Succinic acid between ether and water 2. Dimethylamine between ether and water 3. Bromine between carbon tetrachloride and water 4. Trimethylamine between ether and water 5. Trimethylamine between toluene and water 6. 2.3.4-Trimethylpyridine between toluene and water

In Figure 2, such a plot of distribution coefficients of various distributed solutes in two solvent layers is given, where the distribution coefficients are plotted versus the vapor pressures of water at the same temperature. Straight-line correlation again is obtained. All data were taken from ( 2 ) . The equation of this line representing KD,the distribution coefficient, is log KO

=

AL, log P‘ L

+C

El

5 = 7 log

L

P‘

THERMODYNAMIC DERIVATIONS

Thermodynamic derivations are given here t o indicate briefly t h e basis for the correlations. SOLUBILITY. For the solubility of a pure solid in a solvent, when the solution obeys Raoult’s law or Henry’s law, an equation has been derived previously by numerous authors as special

(8)

which is the equation used in the correlation above. i p defined a5 ( E l - h,) or the difference between the partial molal enthalpy of the solute in saturated solution and the molal enthalpy of solute in pure solid state. For solutions obeying Raoult’s ideal law, this quantity becomes equal t o the latent heat of fusion of the solid from the pure liquid state t o the solid state. However, for real solutions which obey Henry’s law, this quantity depends on the differential heat of solution of the solute in saturated Holution and can be plus values as well as minus values. DISTRIBUTION COEFFICIENTS.Following similar procedure of derivation, it can be shown t h a t for distributed s y s t e m in which the solute obeys Raoult’s law or Henry’s law, Equation 9 can be derived

Dividing this relation by the Clausius-Clapeyron equation, and integrating as before, there is obtained the relation used for correlating distribution coefficients

(3)

The slope of the line A L , / L ’ represents the ratio of the molal heat of transfer for the solute from one solvent layer t o the other t o the molal latent heat of vaporization of the reference substance. This slope, ALJL‘, is nearly constant over the usual temperature ranges for many systems and therefore a straight line is obtained when the distribution coefficient is plotted versus the vapor pressure of a reference substance on a logarithmic paper. The distribution law is rigorously applicable only t o dilute solutions where Henry’s law applies and a straight line plot will be obtained in such cases. Where the concentration of the solute in solvent becomes so appreciable as t o affect the distribution coefficient, a better correlation will be obtained if the distribution coefficients at various temperatures are selected in the concentration range of the same order of magnitude.

+C

log KO = $log

P‘

+C

(10)

RELATION OF REFERENCE SUBSTANCE PLOT (LOG P) TO RECIPROCAL TEMPERATURE PLOT ( 1 / T )

In other papers of this series, particularly those relating t o vapor pressure, reference has been made t o the corresponding integration of the simple Clausius-Clapeyron equation (or related equations for other functions). Thus, there is the common B. This equation is sometimes expression log P = A / T plotted directly on specid graph paper, ruled with logarithmic scale on the Y axis and a reciprocal temperature scale (or negative reciprocal temperature scale) on the X axis. Attention has been called to the greater eaae of using standard logarithmic paper on which t h e X axis is then calibrated directly in temperature values from the corresponding points of vapor pressure of a reference substance, usually water. Because of t h e ease of using different range of both temperatures and pressures which can be done readily with logarithmic paper of different numbers of cycles, and the several inherent advantages of logarithmic paper and its ready availability, the present plot has muck practical advantage. Furthermore, it has ~ f t e nkeen noted that the liaes SQ ob-

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tained are more nearly straight on the logarithmic plot than on the reciprocal temperature plot for reasons which have been developed. I n the present case, working with solubility and distribution coefficients, this is also noted in numerous cases. It follows directly t h a t L//L‘ and particularly AL,/L’ are more nearly constant with a variation of temperature than are z j and AL, alone, since the numerator and the denominator of the fractions are both decreasing with increase in temperature. As the straightnesa of the line depends on the approach t o constancy of its slope, the better correlation is obtained using the method of this paper. This is more particularly true for distribution coefficients since, in all cases tested, the decrease of AL, with temperature is notable. The breaks in the lines caused by transition points in the chemical compositions has been noted with the reciprocal temperature plot by Davidson ( 1 ) who relates the changes in slopes to the heats of transition. Obviously in the case of the logarithmic plot, the heats of transition may be developed even more readily by reference t o the latent heats of the reference substance and the different slopes of the lines in question. NOBIENCLATURE

A, B , C hr

= constants = partial molal heat content

of the solute in its saturated solution h, = molal heat content of pure solid phase K D = distribution coefficient of solute between two solvent layers

L L’

1,

= molal latent heat of Vaporization of liquid = molal latent heat of vaporization of reference liquid = difference between partial molal heat content of the

A L =

P P’

R T x

Vol. 44, No. 7

= = = = =

solute in its saturated e l u t i o n and the molal heat content of pure solid, or (hi - h,) [heat of solution for 1 mole in dissolving in ( 0 1 negative of 1 mole crystallizing from) its saturated solution], molal heat of transfer of solute between two solvent layers vapor pressure of liqid vapor pressure of reference liquid gas constant temperature, OK. solubility in mole fraction of solid in solution LITERATURE CITED

(1) Davidson, J . Chem. Education, 10, 234 (1933). (2) “International Critical Tables,” Vol. 4, New York, RIcGraw-Hill Book Co., 1928. (3) Othmer, D. F., IND.ENG.CmaI., 32, 841 (1940). (4)Ibid.,36, 669 (1944). (5) Othmer, D. F., and Conwell, J. W., Ibid., 37, 1112 (1945). (6) Othmer, D. F., and Gilmont, R., Ibid.,36, 858 (1944). (7) Othmer, D. F., and Sawyer, F. G., Ibid.,35, 1269 (1943). (8) Othmer, D. F., and White, R. E., Ibid.,34, 952 (1942). RECEIVED for review September 26, 1951. ACCEPTED March 13, 1952. Previous articles in this series have appeared in IKDUSTRIAL A K D ENGINEDRI N G CHEMISTRY during 1940, 1942, 1943, 1944, 1945, 1946, 1948, 1949, and 1950: Chem. & Met. Eno., 1940; Chimze et IndzLstrze (Parzs), 1948; Euclzdes ( M a d i a d ) , 1948; Sugar, 1948; Petroleum Refiner, 1951 a n d 1952

Alkali Lignin to Stabilize SlowBreak Asphalt Emulsions W.A. McINTOSH Development Department, West Virginia Pulp & Paper Co., Charleston, S. C .

T

HE recent development of commercial grades of alhali

lignin could hardly come a t a more appropriate time for the good of streets and highways. This abundant raw material is very useful as a stabilizer for soap emulsified slow-break asphalt emulsion. Shortages, caused by the national emergency, of the light petroleum fractions required for application of asphalt as cut-back need not interfere with proper maintenance of roadway systems. Lignin even can extend the emulsifying soap, even though it is not itself an emulsifier. LIGNIN

Pine wood alkali lignin is available in three forms under the general trade name Indulin. It is isolated from the waste liquors resulting from pulping pine wood by the kraft or sulfate process. One of the three commercial grades, designated Indulin A, is lignin in its acidic or phenolic form. As such, it is insoluble in water or acids, but can be easily dissolved in aqueous alkalies such aa caustic soda, which forms a water-soluble sodium salt. I n Indulin C, the sodium salt is already present, and this product dissolves readily in water without the addition of other chemicals. Indulin B is a very recent addition to commercially available pine wood lignins. Like Indulin C i t is a sodium salt of lignin and is water soluble. Because of its very recent development, Indulin B has not yet been investigated for asphalt emulsion stabilization. All three of these materials are free-flowing brown t o black powders of spherical particles. Shipped in dry form, no freight is paid for water of solution. The dry powders are virtually nonhygroscopic. They may be stored indefinitely without deterioration

or creation of a nuisance. Solutions up t o 18 weight % ’ have low viscosity and are easily handled. Increases in concentration above this figure cause disproportionate increases in viscosity, which can be controlled within limits, however, by using additional alkali. Alkali lignin should be distinguished from the so-called sulfite lignin derived from the acid, or sulfite, process for pulping Rood. The latter is comprised chiefly of lignin sulfonates formed by the action of sulfite liquor, which adds sulfonate groups to the lignin occurring in the wood. iilkali lignin, on the other hand, resembles more closely the lignin as it is present in the wood. The sodium compounds of alkali lignin are used in the stabilization of slow-break asphalt emulsions. Because of solubility in water and insolubility in hydrocarbons, they are applied with the sodium soaps in the aqueous phase. These sodium compounds of pine wood lignin are compatible with all of the widely used soap emulsifier solutions in all normal proportions. Concentrated solutions of the lignins should be maintained a t p H 9.5 or higher to prevent precipitation, but at the low concentrations used for mixing with asphalt, considerably lower p H values could he tolerated if desired. V4TERIALS

The purpose of the present study was to verify the application of pine wood alkali lignin as a stabilizer for a wide variety of asphalts from different crude sources. It was also hoped that some conclusions could be drawn from the effect of source on the quantities of chemicals required. Unfortunately for the latter