Approximate prediction of mixed-electrolyte activity coefficients

Approximate prediction of mixed-electrolyte activity coefficients

PRELIMINARY Apfiroximate NOTE prediction D-R. ROSSEINSKY activity coefficients and R.J. HILL of Chemistry. Department of mixed-electrolyte T...

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PRELIMINARY

Apfiroximate

NOTE

prediction

D-R. ROSSEINSKY

activity coefficients

and R.J. HILL

of Chemistry.

Department

of mixed-electrolyte

The

University,Exeter (England)

(Received 2nd March 1971)

Lakshmanan and Rangarajan ’ have recently suggested a useful approximate estimate of activity coefficients y in mixed electrolytes, based on the use of Gu~mheim’s specific interaction parameters2p obtained from the expression for the log 7’ of single-electrolyte solutions. For log 7’, the p are coefficients of a term in molality 112which is additional to the Debye-Htickel (DH) term, taken here’a2 to be --oz.+ lz_ i I %/( 1 + 1%) at ionic strength I (oris the Debye-Htickel constant, z + and z _ are cation and anion charge numbers, and zero superscriptsdenote single-electrolyte solutions). The innovation’ was to allow p to be molality-dependent. However, most of this dependence is due to the particularchoice of DH term, which can be made to cancel if assumed to be identical for electrolytes of similar charge type. Hence we can arriveat a much simpler method which holds with identical accuracy (the cancellation of unspecified DH terms led Guggenheim3 to favour the Akerlof-Thomas relation4

bhf~/702), = J&m

(1)

for obtaining only differences B 12 in the specific interaction coefficients). We follow the procedure of ref_ 1 exactly; but wherever u p occurs we substitute the expeninental single-electrolyte activity coefficcient 7’ (at the I of the mixture) divided by I and the appropriate stoichiometry factor, the 7’ is that which would have been used’ to calculate p_ The DH terms by assumption cancel. This then gives for the mixed 1: 1 electrolytes Rx (electrolyte 1) and NY (electrolyte 2) log(7R&

- log(rOR&

=

m2/mc~o~~“Ry)I

+

log(7°Nyl;

-

=g(Y”R& G3

*

withI=m, a21 F-

dog

+m, 7~

= m For constant I the Hamed coefficients (~~2= /dnz 1 are, from (2),

J. EZecrrti

:

dlog7&dmZ

Chem,, 30

and

(1971j.~~~7_-U) -._, “I:.’ .-_.

:

,.,/

PRELIMINARY

App.8 a21

=

c20-’

{2logboNy)J

-

log(~“NJ&

‘-

‘lo&‘Ry

NOTE

(4)

)I]

For a 1: 1 in a 2: 1 or 1.2 electrolyte the DH terms do not ali cancel, and one (but only one) f3 is still required- Thus, for RX in NY, we get (for cy12=-dIog rl IdIs)

and ~irnilarly -12 for RX in N2Y (but with replacement of suffuc. RX by NX; RY by RX, RX remaining, NX2 by RzY, NX by RY). Our 4~~~in these cases thus still depend in part on an arbitrary choice of DH term for p. Applied to the experimental data, the simple expressions (2) to (5) reproduce Tables 2 and 3 of ref. 1 so closely as to make unnecessary their repetition here. A major-part of the discrepancies, exptl, - calcd., in ref. 1, arise from the consequence of the specific-interaction assumption best shown for “common-ion” systems (R = N or X = Y), from (3) and (4), as

This is not necessarily general (Table l), and it is instructive to establish the relationship between calcd- and exptl, To distinguish, we put +,Fd

aed Now ifBlz

=o

(6a)

in (1) is truly a constant it is readily establishedr’

B12

=

exptl

Ql2

that, exactly,

exptl

-

(7)

%I

but if(as we know it sometimes to be) it is a function of m. Bzz (m), exptl

-

a12

exptl

a21

=B12

we may still write

(W

(ml

since observed departures from constancy are never gross. and the approximation satisfactory. From (6a) and (7a) we have calca.

a12

-

cakd

a21

For constant Br2, a cakd

=

&gcd

‘Bl2

(59

(ml

is thus predicted to be exactly the mean %(cr~~pu -

w3.$le for B12. (m), it is to be obtained. Table ,I,shows the -Few measurements ion @‘able 2) For these our

is

exptl. Ql2l

h

approximately so. Where &Gpti and azfp’ have both been average of the exptl. values to be closely predicted. ha&been made on 1: 1 electrolyte mixtures without a common treatment gives (9)

PRELIMINARY

TABLE

NOTE

App-9

1

System

I/m01 kg-’

HCI-LiC15

0.5

exptl WI

_&P”

0.010 0.009 0.009 0.067

0.006 0.005 0.005 0.062

0.011 0.012 0.012 0.074

calcd

>:

.

a2

HCl-KC1

0:5

0.064 0.061 0.061

0.057 0.056

0.064 0.072

0.066

0.050

HCl-CsQ

2: 4.0 1.0

0.086

0.100

0.060

ZI: 1.0 2.0 4.0 6.0 2.0 3.0 4.0

0.077 0.073 0.04 1 0.032 0.027 0.027 0.05 1 0.05 1 0.05 2

3.0 4.0 1.0

0.016 0.014 0.028

0.099 0.073 0.021 0.008 0.003 0.003 0.032 0.025 0.024 0.013 0.013 0.013 0.027

0.046 0.041 0.047 0.044 0.044 0.044 0.067 0.075 0.080 0.013 0.011 0.014 0.029

C&l-NaCl

KCl-Lick

6



RI-RbI 8

2.0

NaCl-NaF



0.019

TABLE 2 HARNED

COEFFLClENTS”*n

0.1 0.25 0.50 0.70

* Using osmotic

FOR

SYSTEM

HCl-NaClOa

0.030 0.034

0.085 0.077

0.050 0.025

0.038

0.070

0.025

0.040 0.040 0.038

0.060 0.068 0.073

0.025 0.027 0.039

coefficients from ref. 13.

0.060 0.085 0.085 0.085 0.083 0.073

..

Expression (9) will again in general be in error, (10) again much less so, as illustrated in Table 2_ Invocation of further interaction coefficients for particular pairs of like charges appears to be the only way in which the failure of (9) can be circumvented in theories of this typCW6 _ Moving from constant -I data, we note that for trace amounts of electrolyte (mr e m2. m2 = m), eqn. (1) becomes

lo&~

)m =.% l”d~oRy)

m

+

!o&o&m

Prediction of logy, , for ml .(constant) = 0.01 mol kg-’ and m2 up to 10 mol kg-‘, is sometimes poor, but prediction of dlog rr /dm, is promising_ While for a third of the _systems estimates do lie near or vvithin the bounds of experimental error, in the former .very severe test, log rl for HBr+.NaClO, at I +_9 mol kg’! .thus is 0.78 calcd., and :

._

L’iT@&haL

Chem

..

:

.'30 (l??l~).Ap47-10_.~

Amilo 959

PRELIMINARY

expti,

1 the &rst

reproduced

discrepancy,

(Table 3)),tlioughvarying

ranges noted.

by our prediktions.

(approximately consttit sevenfold, are quite closely

The slopes, however by as much as

This agreement

compares

Skhwabe’? for the somewhat related quantity Am/Am, premises avoiding the need for singI&ion quantities.

satisfactorily

and is obtained

NOTE

in the

with that of from

simpler

TABLE 3 System

(25OCI

tiCl--NaC104

HBr-NaCl04 NaCl-NaCl04 NaBrTNaC104 HCI-Liao, HBr-Liclo4 HCI-HCi04 HBr-HQo&& HCl-KCl = HCl-NaQ HQ-LiCL HBr-KBr HBr-NaBr HBr-L%Br

l4

2-6 3-9 2-6 .2-10 2-6 2-6 3-10 3-10

1.5-4

1-3 1.5-4 IS-3 1.5-3 L-3

ExptL

G7ICd

0.08 0.09 0.03 0.03 0.12 0.13 0.18 0.20

o-10 O-12 0.03 0.04 0.14 0.15 0.17 0.18 0.05 0.07 0.09 0.07 0.09 0.12

Ez 0.11 0.06 0.09 0.14

REFEFiENCES

1 S. Lakshmanan and S.K. Rangamjan, J. Electruanal. C&em., 27 (1970) 170. 2 E.A. Gu~nheim,PhiL Mag, 19 <1935) 588. E.A. Guggenheim, Appt+ztions of Statistical Mechanics. Clarendon Press, Oxford, 1966, p. 177. : G. AkerlWand H.C. Thomas,J. Amer. Cirem Sot., 56 (1934) 594. _5 H.S. Ham&d and B.B. Owen, The Physical Chemistry of Electrolytic Solutions, Reinhold, New York, : 6 3rd edxi., 1958. p. 608. ILA; Robinson,J,‘Amer.. Chem Sot, 74 (1952) 6036. F2.k Robinson and C.L. Lim, nuns. FMf~day So&.49 (1953) 1144. and D.Yu. Stupin, Russ. J. Phys Chem, 35 (1961) 295_ .z L&:Makarov 9 J.N; Butler, Ama& Ctze@z, 42 <1970) 1308, 10 HS. Harr;red&nd B.B. Owen, ZXe Physical Chemistry of Electrolytic Solutions. Reinhold, New York, 3rd..edn., 1958, p_ 606. : zi. SJ. Bates arid 3-W. Urmston,J, Amer. Chem Sock, 55 (1933) 4071. 12 I.E. Me and A.J. Read,JI. ChemSoc A, (1966) 1812. 13 RA. Robinson and R.H. Stokes, Electrolyte Solutions, Butterworths, London, 2nd edn., 1965, p. 483 14 k Fe&&and K. Schwahe, Z. Phys Chem, 230 (1965) 20. Reinhold. New York. 15 H.S. Harned and B.Bi Owen, i?TzePhysicai Chemistry of Etecrrotytic Soluti& 3rd edi,.1958, p:748. .’ 18 HS. Hamed and R_A_ Robinson. &Sulticomponenr Electrolyte Solutions, Pergamon. London, 1968, p.’ 22 !&h&&e. Elec~him slctrf.. 12 (1967) 88. -17 IL . .. .. ~-_