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Tadeusz Górecki Ionic Equilibria
Page 1
Chemical Equilibria
OHAcOHHAc 32
Tadeusz Górecki Ionic Equilibria
Page 2
Addition of HAc to a mixture of NaOH and ammonia:
AcHHAc
34 NHHNH
OHOHH 2
Reaction of copper sulphate with ammonia:
Overall: 2
4332 )(4 NHCuNHCu
233
2 CuNHNHCu
2233
23 )()( NHCuNHNHCu
2333
223 )()( NHCuNHNHCu
2433
233 )()( NHCuNHNHCu
2533
243 )()( NHCuNHNHCu
More accurately:
....))(()( 225233
262 OHOHNHCuNHOHCu
Other possible species and reactions:
CuOH 2
22 )(OHCu
43 NHHNH
OHHOH2
Tadeusz Górecki Ionic Equilibria
Page 3
Equilibrium constant
Chemical potential:
Total free energy:
At equilibrium
)()(
)( 1
,,
molkJmoln
kJGi
nPTiij
i
iii nnnnTPG ),...,,,,( 21
0 Gdn
dG
r
Tadeusz Górecki Ionic Equilibria
Page 4
Most common REFERENCE STATES:
• pure liquid state
• infinite dilution state
• elements in their naturally occurring state
STANDARD CONDITIONS:
temperature, pressure and concentration
Reference state and standard conditions together define the
STANDARD STATE
Chemical potential of i in a liquid solution:
xRTf
fRT iliquidpurei
liquidpurei
iliquidpurei lnln 00
iii
ref
i axf
f (activity of the compound)
Activities are relative measures (they depend on the choice of the
reference state)
DCBA
Equilibrium constant:
BA
DC
BA
DC
BA
DC
aa
aaK
][][
][][
Tadeusz Górecki Ionic Equilibria
Page 5
Assuming that activity coefficients are equal to one:
]][[
]][[
BA
DCK
For acetic acid: AcHHAc
][
]][[
HA
AcHKa
When activity coefficients are not neglected:
0
0
][
][][
HAc
AcHKa
0
AK is independent of the composition of the solution
Tadeusz Górecki Ionic Equilibria
Page 6
Activity coefficients
extended Debye-Hueckel theory:
IBa
IzzA
1log
- geometric mean activity coefficient of the two ions forming the
electrolyte. For simple 1:1 salts (e.g. NaCl) 2/1
A - constant dependent on temperature and the dielectric constant of
the solvent
in water C25at 51.010825.12/36
TA
z - charge of the ion
I - ionic strength
i
ii zCI 2
2
1
Ci - concentration of every ion present in the solution
zi - charge of ion i
a - adjustable parameter, measured in Å, corresponding to the
effective size of the hydrated ion
B - function of temperature and dielectric constant:
in water C25at 33.03.502/1
TB
Activity coefficient for a single ion:
IBa
IAzz
1log 2
Tadeusz Górecki Ionic Equilibria
Page 7
Tadeusz Górecki Ionic Equilibria
Page 8
How well does it work?
Davies equation:
I
I
IzzA 2.0
1log
for single ion:
I
I
IAzz 2.0
1log 2
Tadeusz Górecki Ionic Equilibria
Page 9
General interpretation of activity:
1. Ions in dilute solutions: activity is equal to the product of the
concentration (M or m) and the activity coefficient:
AAA ][
2. Uncharged molecules (e.g. CO2, H2S, NH3):
bI0log
b depends on the molecule and temperature (typically between 0 and
0.2).
3. Solvent in a dilute solution: activity is approximately equal to the
mole fraction of the solvent (e.g. for 0.1 M NaCl x = 55.5/55.6 =
0.9982).
4. Pure solids and liquids: activity is exactly 1.
5. Gases in equilibrium with the solution: activity is partial pressure of
the gas in atm. At high pressures, a fugacity coefficient is required.
6. Mixtures of liquids: activity of a given compound is approximately
equal to its mole fraction.
Tadeusz Górecki Ionic Equilibria
Page 10
Examples of equilibrium constants
Autodissociation of water: OHHOH2
Thermodynamic equilibrium constant:
}{
}}{{
2
0
OH
OHHK
{H2O} is 1 for pure water, but 0.98 for 1 M NaCl
In general:
0
0 ][][
OHH
Kw
0 - activity coefficient of water
Concentration constant:
]][[ OHHKw
00
ww KK
Dissociation constant of a weak acid
polyprotic acid (e.g. H3PO4):
HPOHPOH 4243 ][
]][[
43
421
POH
POHHKa
HHPOPOH 2
442 ][
]][[
42
24
2
POH
HPOHKa
HPOHPO 3
4
2
4 ][
]][[24
34
3
HPO
POHKa
Tadeusz Górecki Ionic Equilibria
Page 11
Weak base:
OHNHOHNH 423
][
]][[
3
4
NH
OHNHKb
we can also write
HNHNH 34
][
]][[
4
3
NH
NHHKa
bwa KKK /
Stepwise formation constant for complexes:
CdClClCd 2
]][[
][21
ClCd
CdClK
2CdClClCdCl
]][[
][ 2
2
ClCdCl
CdClK
32 CdClClCdCl ]][[
][
2
3
3
ClCdCl
CdClK
2
43 CdClClCdCl ]][[
][
3
24
4
ClCdCl
CdClK
Activities can be easily introduced, e.g.:
Tadeusz Górecki Ionic Equilibria
Page 12
][][
][
2
21ClCd
CdClK
Overall formation constant:
CdClClCd 2
]][[
][21
ClCd
CdCl
11 K
2
2 2 CdClClCd
22
2
2]][[
][
ClCd
CdCl
212 KK
3
2 3 CdClClCd 32
3
3]][[
][
ClCd
CdCl
3213 KKK
2
4
2 4 CdClClCd 42
2
4
4]][[
][
ClCd
CdCl
43214 KKKK
Instability constant:
ClCdCdCl 422
4
][
]][[2
4
42
CdCl
ClCdK inst 4/1 instK
Tadeusz Górecki Ionic Equilibria
Page 13
Solubility product
ClAgsAgCl )(
}}{{0
ClAgK s
In terms of concentration:
]][[0
ClAgK s
For a divalent cation:
OHMgsOHMg 2)()( 2
2
22
0 ]][[ OHMgK s
AgCl equilibria in the presence of excess Cl-:
ClAgsAgCl )( ]][[0
ClAgK s
.)()( aqAgClsAgCl .)]([1 aqAgClK s
we can also write complex formation reaction:
.)(aqAgClClAg
]][[
.)]([1
ClAg
aqAgCl
hence 011 .)]([ ss KaqAgClK
Tadeusz Górecki Ionic Equilibria
Page 14
2)( AgClClsAgCl ][
][ 22
Cl
AgClK s
or
22 AgClClAg 2
22
]][[
][
ClAg
AgCl
hence 02
2
2][
][ss K
Cl
AgClK
2
32)( AgClClsAgCl 032
2
3
3][
][ss K
Cl
AgClK
3
43)( AgClClsAgCl 043
3
4
4][
][ss K
Cl
AgClK
.)(aqAgCl - dissolved (but not dissociated) AgCl
Tadeusz Górecki Ionic Equilibria
Page 15
Temperature dependence of K
000 ln STHKRTG
R - gas constant (8.314 kJ/mol) 0 denotes standard state
015
2
00
)1006.4(303.2
logHJ
RT
H
dT
Kd
Assumption when estimating K at a different temperature: 0H is
constant
Tadeusz Górecki Ionic Equilibria
Page 16
Mass balance
For acid HA:
][][ AHACHA
When more sources of A- are present (e.g. HA, NaA and CaA2):
...][][][2][2
CaAAHACCCA CaANaAHAT
Poorly soluble salts in water at saturation (e.g. BaSO4):
Mass balance on barium:
SBa ][ 2 (S – molar solubility)
Mass balance on sulphate:
SHSOSO ][][ 4
2
4
hence:
][][][ 4
2
4
2 HSOSOBa
Formation of precipitate (AgCl):
...][.)]([][)]([][ 2 AgClaqAgClAgsAgClAg T
...][2.)]([][)]([][ 2 AgClaqAgClClsAgClCl T
To eliminate [AgCl(s)] (unknown):
...][][][][][ 2 AgClClAgClAg TT
Charge balance
For HAc:
][][][ OHAcH
If a species has more than one charge, its concentration is multiplied by the
number of charges:
Tadeusz Górecki Ionic Equilibria
Page 17
][][3][2][][ 3
4
2
442
OHPOHPOPOHH
Proton condition (proton balance equation, PBE)
# protons consumed = # protons released
Water can consume a proton to form H3O+ or release a proton to form OH
-,
thus PBE for water is:
][][ OHH
PBE for water is involved in all PBEs for aqueous solutions.
PBE for a monoprotic acid:
][][][ OHAcH
PBE for a strong base:
][][][ OHKH
PBE for a weak base:
][][][ 4 OHNHH
PBE for strong electrolytes:
NaCl:
][][ OHH
NH4Cl:
][][][ 3 OHNHH
Tadeusz Górecki Ionic Equilibria
Page 18
NaAc:
][][][ OHHAcH
NH4Ac:
][][][][ 3 OHNHHAcH
Polyprotic acids and bases: the concentration terms in PBE must be multiplied
by the number of protons consumed or released in the formation of the species
from the starting material.
Examples:
H2S
][][2][][ 2 OHSHSH
NaHS:
][][][][ 22
OHSSHH
Na2S:
][][][2][ 2 OHHSSHH
Mixtures of electrolytes: the contributions of all the components are added.
Examples:
solution of HAc and HCOOH:
][][][][ COOHAcOHH
mixture of HOBz and NaOBz:
][][][][ OBzOHHOBzH
_____________________________________________________
Tadeusz Górecki Ionic Equilibria
Page 19
PBE for NaAc:
][][][ OHHAcH
Charge balance:
][][][][ OHAcNaH
Mass balance:
][][][ HAcAcNa
Substitution of mass balance into charge balance:
][][][][][ OHAcHAcAcH
Which is equivalent to PBE.
PBE can always be obtained by combining mass and charge balances.
========================================================
Solving an equilibrium problem
1. Establish the nature of all the species present in the solution.
2. Find the equilibrium constants relating the concentrations of the various
species.
3. Find enough other relations so that there are as many independent equations
as variables.
4. Solve the equations, using approximations where possible.
5. Check the provisional answer by substitution in the full original set of exact
equations. If the discrepancies are too high (> 5%), try more complicated
approximations.
6. Calculate the ionic strength and adjust the equation constants to correspond.
Repeat until the answers do not change.
7. Check all the final answers by substitution in the full set of exact equations.