19 Heterogeneous & complex equilibria 1 19 Heterogeneous and complex equilibria CaCO 3 exists as...
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19 Heterogeneous & complex equilibria 1
19 Heterogeneous and complex equilibria
CaCO3 exists as aragonite calcite
Formation of crystals such as AgCl in a solution is a heterogeneous equilibrium, because there are more than one phase,
AgCl (s) = Ag+ (aq) + Cl– (aq)
Species such as Ag(NH3)2+ & Ag(CN)2
– are complexes (or complex ions).
Ag+ (aq) + 2 NH3 (aq) = Ag(NH3)2+ (aq)
19 Heterogeneous & complex equilibria 2
Beauty due to heterogeneous equilibria
There are many natural heterogeneous equilibria.
Please think of some!
19 Heterogeneous & complex equilibria 3
The solubility productFor the dissolution,
CaCO3 (s) = Ca2+ (aq) + CO32- (aq)
Ksp = [Ca2+] [CO32-] = 3.8e-9 (a constant) solubility product
Substance Formula Ksp
Aluminum hydroxide Al(OH)3 4.6e-35
Barium chromate BaCrO3 1.2e-10
Calcium phosphate Ca3(PO4)2 1e-26
Iron sulfite FeS 6e-18
Lead sulfite PbS 2.5e-27
Mercury sulfite HgS 1.6e-52
Ksp = [Al3+] [OH-]3
Ksp = [Ca2+]3 [PO4]2
Which is the most and least soluble?
19 Heterogeneous & complex equilibria 4
Solubility product
constants
Compound Ksp Compound Ksp
AgBr 5.0 x 10-13 Fe(OH)3 4.0 x 10-38
AgCl 1.8 x 10-10 FeS 6.3 x 10-18
AgI 8.3 x 10-17 HgS 1.6 x 10-52
AgIO3 3.1 x 10-8 Mg(OH)2 1.8 x 10-11
Ag3PO4 1.3 x 10-20 MgC2O4 8.6 x 10-5
Al(OH)3 2.0 x 10-32 Mn(OH)2 1.9 x 10-13
Ba(OH)2 5.0 x 10-3 MnS 2.5 x 10-13
BaSO4 1.1 x 10-10 NiS 1.0 x 10-24
Bi2S3 1.0 x 10-97 PbCl2 1.6 x 10-5
CaCO3 4.8 x 10-9 PbSO4 1.6 x 10-8
CaC2O4 4.0 x 10-9 PbS 8.0 x 10-28
CaSO4 1.2 x 10-6 SrSO4 3.2 x 10-7
CdS 8.0 x 10-27 Zn(OH)2 3.3 x 10-17
CoS 2.0 x 10-25 ZnS 1.6 x 10-23
CuS 6.3 x 10-36
Table like this is available in handbooks or data bases. Know where to find them when you need them. Write Ksp expressions.
19 Heterogeneous & complex equilibria 5
Ksp and solubilityThe Ksp = 1.0e-6 for BaF2, what are [Ba2+] and [F¯]?
Solution:BaF2 = Ba2+ + 2 F¯
assume x 2 x
Ksp = x (2x)2 = 1.0e-6x = 3 (1.0e-6 / 4) = 6.3e-3 M
[Ba2+] = x = 6.3e-3 M molar solubility = 6.3e-3 *175 = 1.1g/L[F¯] = 2 x = 0.013 M
Checking:6.3e-3 *0.0132 = 1e-6 = Ksp
Calculate solubility of BaCrO3, Ksp = 1.2e-10
Molar mass of BaF2=175 g/mol
19-2
19 Heterogeneous & complex equilibria 6
Concentrations of ions in solution
CaF2(s) = Ca2+(aq) + 2 F- (aq), Ksp know where to find
Ksp = 5.3e-9
19 Heterogeneous & complex equilibria 7
Perception of a saturate solution
Ag2S = 2 Ag+ + S2–
Ksp = [Ag+]2[ S2–]
19 Heterogeneous & complex equilibria 8
Calculate Ksp from Solubility
When 0.50 L saturated CaC2O4 solution was dried, 0.0030 g dry salt was obtained. Evaluate the Ksp.
Solution:3.0e-3 g————0.50 L
1 mol———128 g
= 4.7e-5 mol / L = [Ca2+]
CaC2O4 = Ca2+ + C2O42-
4.7e-5 4.7e-5
Ksp = 4.7e-5 * 4.7e-5 = 2.2e-9
Figure out how to calculate solubility from Ksp .
How many grams of HgS will dissolve in 1 L?
19 Heterogeneous & complex equilibria 9
Precipitation of AgCl
Goto URL:
http:// dl.clackamas.cc.or.us/ch105-05/solubili.htm
for a demonstration if you have not seen the experiment
Ag+ (aq) + Cl- (aq) = AgCl(s)
19 Heterogeneous & complex equilibria 10
Common-ion effect on solubilityLike acid-base equilibria, presence of common ions from more than one electrolyte affects the solubility, since Ksp remains constant.
For example, the Ksp = 1.8e-10 for AgCl. The maximum [Ag+] is governed by the condition,
NaCl = Na+ + Cl-0.10 0.10
AgCl = Ag+ + Cl-[Ag+] 0.10
Thus [Ag+] * 0.10 = 1.8e-10 [Ag+] = 1.8e-9 M
Solubility of AgCl = 1.8e-10 = 1.3e-5 M in pure water is 7,454 times more.
? Should we considerAgCl = Ag+ + Cl-
x 0.10+x
19-3
19 Heterogeneous & complex equilibria 11
Graph the common ion effect
AgCl = Ag+ + Cl-
NaCl = Na+ + Cl-
19 Heterogeneous & complex equilibria 12
Condition for precipitationRecall: Predicting reaction directions by comparing Qc and Kc.
Same principle applies to precipitation (ppt)
Q < Ksp, unsaturated (solution)Q = Ksp, saturated (usually two phases are present)Q > Ksp, super-saturated
(unstable, often needs a seed to start the ppt)
19-5
19 Heterogeneous & complex equilibria 13
Separation by precipitationA 10-mL solution contains 0.10 M each of Cl–, Br–, and I– ions. Micro amounts of 0.10 M AgNO3 solution is added to the system. What are the Ag+ concentrations before AgI, AgBr, and AgCl precipitate?Solution: Data sheet Ksp:AgCl 1.8e-10, AgBr 5.0e-13, and AgI 8.3e-17.
[Ag+] for AgI, AgBr, & AgCl solids to form:[I–] = 0.10 M [Ag+] = 8.3e-17/ 0.10 = 8.3e-16 AgI(s) appears
[Br–] = 0.10 M [Ag+] = 5.0e-13/ 0.10 = 5.0e-12 AgBr(s) appears [Cl–] = 0.10 M [Ag+] = 1.8e-10 / 0.10 = 1.8e-9 AgCl(s) appears
As [Ag+] increases, how do [Cl-], [Br-] and [I-] vary ? [Ag+] [Cl–] [Br–] [I–]
0 8.3e-16 0.1 0.1 0.10 AgI(s) 5.0e-12 0.1 0.10 AgBr(s) 1.7e-5 1.8e-9 0.10 AgCl(s) 2.8e-4 4.6e-8 1e-7 1.8e-3 5.0e-6 8.3e-10 0.1 ____? ____? ____?
19-6
19 Heterogeneous & complex equilibria 14
pH H2S and solubility of metal ionsThe pH affects the equilibrium of many species, for example:
H2S = H+ + HS– Ka1 = 1e-9HS– = H+ + S2– Ka2 = 1e-14 (doubtful but adopt)H2S = 2 H+ + S2– Koverall = 1e-23
[S2–] = [H2S] *1e-23 / [H+]2 = [H2S] *1e(2*pH-23), strongly affected by pH
If [H2S] = 1.0 MpH [S2–] Ksp of MS [S2–] for [M2+] = 0.0011 1e-21 1.6e-52 HgS 1.6e-49 (ppt)2 1e-19 2.5e-27 PbS 2.5e-24 (ppt)2.52 1.1e-18 1.1e-21 ZnS 1.1e-18 (no ppt pH < 2.5) 4.39 6e-15 6e-18 FeS 6e-15 (no ppt pH < 4.4)7 1e-9 2.5e-13 MnS _____ (no ppt pH < ____)10 1e-3
11 0.1
19-7
Recalculate [s2-] at various pH if [H2S] = 0.10 M
19 Heterogeneous & complex equilibria 15
pH, and CO2 on CaCO3 solubilityThe [CO3
2–] in a 0.0010 M H2CO3 solution is determined by,H2CO3 = H+ + HCO3
– Ka1 = 4.3e-7HCO3
– = H+ + CO32– Ka2 = 5.6e-11
H2CO3 = 2 H+ + CO32– Koverall = Ka1*Ka2 = 2.4e-17
= [H+]2 [CO32–] / [H2CO3]
[CO32–] = (0.0010*2.4e-17) [H+]–2
= 2.4e-20 * 1e(2*pH) = 2.4e(2*pH-20)
[CO32–] affects [Ca2+] due to equilibrium
CaCO3 = Ca2+ + CO32– Ksp = 8.7e–9
[Ca2+] = 8.7e–9 [CO32–]–1
= 8.7e–9 / 2.4e(2*pH–20)
= 3.6e(20 – 9–2*pH) = 3.6e(11-2*pH)
Decrease pH by 1 increases [Ca2+] by 2 order of magnitude
pH [Ca2+]8 3.6e-57 3.6e-36 0.36
19 Heterogeneous & complex equilibria 16
Stalactites and stalagmites
stalactites
stalagmites
Rain dissolves limestone and when water drops form stalactites and stalagmites in caves. They grew about 2 cm per 1000 years.
The slightly acidic rain dissolves lime stone:CaCO3 (s) + H+ = Ca2+ (aq) + HCO3
- (aq)
When acidity is reduced, solid forms:Ca2+ (aq) + HCO3
- (aq) + OH- (aq) = CaCO3 (s) + H2O
19 Heterogeneous & complex equilibria 17
Stalactites hanging down from the ceiling formed over hundreds of years in Mercer Cavern
19 Heterogeneous & complex equilibria 18
Aragonite formations found at Mercer Caverns, California
The "Angel Wings" are two delicate and translucent crystalline formations, over 9 feet long and 2.5 feet wide in Mercer Caverns
19 Heterogeneous & complex equilibria 19
Equilibrium of complexesMetal ions tend to attract Lewis bases forming coordinated complexes, or complex ions. These formation is governed by equilibrium,
metal ion ligand Step-wise formation constantAg+ (aq) + NH3 (aq) = Ag(NH3)+ (aq) K1
Ag(NH3)+ (aq) + NH3 (aq) = Ag(NH3)2+ (aq) K2
formation constantAg+ (aq) + 2 NH3 (aq) = Ag(NH3)2
+ (aq) Kf = K1 K2 = 1.7e7Ag+ (aq) + 2 S2O3
2– (aq) = Ag(S2O3)23– (aq) Kf = 2.9e13
Ag+ (aq) + 2 CN– (aq) = Ag(CN)2– (aq) Kf = 5.6e18
Dissociation constant Ag(NH3)2
+ (aq) = Ag+ (aq) + 2 NH3 (aq) Kd = 1 / Kf = 5.9e-8 Ag(S2O3)2
3– (aq) = Ag+ (aq) + 2 S2O32– (aq) Kd = 1/2.9e13 = 3.4e-14
19-8
19 Heterogeneous & complex equilibria 20
Logical, but impractical method!!!
Evaluate [Ag+] in a solution containing 1.0 M NH3 and 0.10 M AgNO3.
Solution:Ag+ (aq) + 2 NH3 (aq) = Ag(NH3)2
+ (aq) Kf = 1.7e7 (find data)
0.1-y 1-2y y (think way)
y——————— = 1.7e7(1-2y)2(0.10-y)
y ——— = (1-2y)2 (0.1-y) By trial an error, y = 0.101.7e7
[Ag+] = 0.10 – y ~ 0 (cannot evaluate [Ag+])
0.10-y = 6e-9, too small, impractical!
5.9e-8y = 0.1 –0.8y –2y2
19 Heterogeneous & complex equilibria 21
Concentration of ions in presence of ligands
Evaluate [Ag+] in a solution containing 1.0 M NH3 and 0.1 M AgNO3.
Solution:Ag+ (aq) + 2 NH3 (aq) = Ag(NH3)2
+ (aq) Kf = 1.7e7 (find data)
x 0.8+2x 0.1-x (think way)
0.1-x (treated as dissociation)————— = 1.7e7(0.8+2x)2 x
0.1 - x ~ 0.1; 0.8+2x ~ 0.8 (x is very small) then
0.1 0.1——— = 1.7e7 x = ————— = 9.2e-9 = [Ag+] 0.82 x 0.82 *1.7e7
3.4e7 x2 + 1.7e7 x – 0.1 = 0x =[ -1.7e7+{(1.7e7)2 + 4*0.1}] / 2 = 0 (cannot solve)
Small indeed
19 Heterogeneous & complex equilibria 22
Complex and precipitate formation-1
What is the maximum [Cl-] before AgCl(s) forms in a solution containing 1.0 M NH3 and 0.1 M AgNO3?
Solution: Previous slide showed [Ag+] = 9.2e-9 M in a solution when [NH3] = 1.0 MKsp = 1.8e-10 for AgCl (know where to look up)
Thus, the max. [Cl-] = 1.8e-10 / 9.2e-9 = 0.02 MWhen no NH3 is present, max. [Cl-] = 1.8e-10/0.1 = 1.8e-9
What is the maximum [Br-] before AgBr(s) forms in a solution containing 1.0 M NH3 and 0.1 M AgNO3?
Ksp = 5e-13 for AgBr,Thus, the max. [Br-] = 5e-13 / 9.2e-9 = 5.4e-5 M.
0.02-------- = 368 times5.4e-5
19 Heterogeneous & complex equilibria 23
Complex and precipitate formation-2What is the maximum [Br-] in a solution suppose to containing 0.10 M AgNO3 and 0.20 M Na2S2O3 before AgBr(s) (Ksp = 5e-13) forms?
Solution: Kf = 2.9e13 for Ag(S2O3)23–;
Ag(S2O3)23– = Ag+ + 2 S2O3
2– , K = 1/2.9e13 = 3.4e-140.1-x x 2x
4x3 ——— = 3.4e-14; x = (3.4e-14*0.1)1 / 3 = 1.5e-5 = [Ag+] (0.1–x) small
max [Br–] = Ksp/[Ag+] = 5e-13/1.5e-5 = 3.3e-8 (very low)
What is [Br–] = ? If [Na2S2O3] is increased to 1.0 M? See next page
19 Heterogeneous & complex equilibria 24
Complex and precipitate formation-3What is the maximum [Br-] in a solution suppose to containing 0.10 M AgNO3 and 1.0 M Na2S2O3 before AgBr(s) (Ksp = 5e-13) forms?
Solution: Kf = 2.9e13 for Ag(S2O3)23– K = 1/2.9e13 = 3.4e-14
Ag(S2O3)23– = Ag+ + 2 S2O3
2–
0.1-x x 2x+0.8
(0.8+2x)2x ———— = 3.4e-14, x = 3.4e-14*0.1/0.82 = 5.3e-14 = [Ag+] (0.1-x) small
max [Br –] = 5e-13/5.3e-14 = 94 M, unrealistically large
What is the maximum [I – ] in a solution containing 0.10 M AgNO3 and 1.0 M Na2S2O3 before AgI(s) (Ksp = 8e-17) forms?
[I-] = 8e-17 / 5.3e-14 = 0.0015 M; small compare to 0.1 M
19 Heterogeneous & complex equilibria 25
Chemical casseroleExperiment
AgNO3 solution | Cl –
AgCl (s) | 6.0 M NH3
Ag(NH3)2+ + Cl –
| Br–
AgBr (s) + NH3, Cl –
| S2O32–
Ag(S2O3)23– + Br – + NH3, Cl–
| I–
AgI (s)
Data
Solid Ksp
AgCl 1.8e-10AgBr 5.0e-13
AgI 8.0e-17
Complex Kf
Ag(NH3)2+ 1.7e7
Ag(S2O3 ) 23–
2.9e13
white
ivory
brown
June 29
19-9
19 Heterogeneous & complex equilibria 26
Some complexes
Ligands (Lewis bases):
Negative ions, F-, Cl-, Br-, I-, OH-, CN-, SO42-, RCOO-, …
Neutral molecules: H2O, NH3, NR3, ROR, CO, C5H5, PR3, C5H5N, …Multidentate ligands: H2NCH2CH2NH2, H2NCH2CH2NHCH2CH2NH2,
Ag(NH3)2+,
Cu(CN)32- (Cu(I)), Cu(PPh3)2Br,
(NH3)2PtCl2 (cis & trans), Ni(CN)5
3-,
19 Heterogeneous & complex equilibria 27
The heme and hemoglobin
(a) The structure of heme is a planar porphoryin ring with iron at the center. (b) Four heme units and four coiled polypeptide chains are bonded together in a molecule of hemoglobin.
19 Heterogeneous & complex equilibria 28
Amphoteric hydroxidesAmphoteric metal hydroxides react with both acids and bases.
Examples: (M = Fe, Zn)M(H2O)4(OH)2 + H+ = M(H2O)5(OH)+
M(H2O)5(OH)+ + H+ = M(H2O)62+
M(H2O)4(OH)2 + OH– = M(H2O)3(OH)3 –
M(H2O)3(OH)3 – + OH– = M(H2O)2(OH)4
2 –
Aluminum hydroxide behave similarly:Al(H2O)3(OH)3 + H+ = Al(H2O)4(OH)2
+
Al(H2O)4(OH)2+ + H+ = Al(H2O)5(OH)2+
Al(H2O)5(OH)2+ + H+ = Al(H2O)63+
Al(H2O)3(OH)3 + OH – = Al(H2O)2(OH)4 –
Al(H2O)2(OH)4– + OH – = Al(H2O)(OH)5
2–
Al(H2O)(OH)52– + OH – = Al(OH)6
3 –
19 Heterogeneous & complex equilibria 29
Qualitative analysis of metal ions
Mixture of metal ions add HCl
group I Ag+, Hg22+, Pb2+
filtrate of soluble chloride chloride | add 0.3 M H+ & H2S
group II Cu2+, Cd2+, Hg2+, Pb2+ filtrate of soluble metal sulfide As3+, Sb3+, Bi3+, Sn4+ | | add OH- & H2S
acid insoluble sulfide | (NH4OH) group III Mn2+, Fe2+, Co2+, Ni2+, Zn2+ filtrate of soluble metal ions base insoluble sulfide | | add CO3
2- or PO43-
Al(OH)3, Cr (OH)3 | |hydroxide |
group IV Mg2+, Ca2+, Sr2+, Ba2+ filtrate of soluble metal ions ppt as carbonates or phosphates | K+, Na+ group V
19 Heterogeneous & complex equilibria 30
Heterogeneous and complex ion equilibria Summary
Calculate Ksp
Evaluate molar solubility (or in other units) from Ksp
Discuss concentrations of species in solution with two or more electrolytes (common ion effect, pH effect, separation by ppt)
Predicts ppt (heterogeneous equilibria)
Describe ligands, metal ions, complexes (ions), and formation constants, and dissociation constant
Apply complex formation to explain solubility
Be able to get out of traps (think in both directions)