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Table 4 Selected thermodynamic data for the Fe–S, Zn–S, Cu–S, and Cd–S systems

From: Fate and transport of metals in H2S-rich waters at a treatment wetland

Source

Solid

T/°C

Reactions

Log K

65

Amorphous Fes

20

FeS + H+ = Fe2+ + HS-

-3.00

   

FeS + H+ + HS = Fe(HS)2°

+ 3.45

51

Crystalline sphalerite

25

ZnS + H2S°= Zn2+ + 2HS-

-18.47

   

ZnS + H2S°= Zn(HS)2°

-5.65

   

ZnS + 2HS- = ZnS(HS)22-

-5.33

   

ZnS+H2S °+2HS- = Zn(HS)42-

-3.83

   

ZnS + HS-ZnS(HS)-

-4.64

52

Crystalline sphalerite

25

ZnS + H2S°= Zn(HS)2°

-5.3

   

ZnS + H2S°+ HS- = Zn(HS)3-

-3.3

   

ZnS +H2S °+ 2HS- = Zn(HS)42-

-3.4

   

ZnS + H2O+HS- = Zn(OH)(HS)2-

-4.4

   

ZnS +H2O+2HS- = Zn(OH)(HS)32-

4.9

53

Amorphous ZnS

25

ZnS + H+ = Zn2+ + HS-

-10.89a

   

ZnS + H2O = Zn(OH)(HS)°

-5.87

54

Crystalline covellite, CuS

25

CuS + H+ = Cu2+ + HS-

-20.95

   

CuS + 2HS- = CuS(HS)22-

-4.97

   

CuS + 3HS- = CuS(HS)33-

-4.04

   

CuS + 4S(s) + HS- = CuS(S5)2- + H+

-12.19b

   

CuS + 6.5S(s) + 1.5HS- = CuS4S53- + 1.5H+

-15.71c

   

CuS + 7.5S(s) 1.5HS- = Cu(S5)23- + 1.5H+

-16.06c

55

Crystalline chalcocite, Cu2S

22

Cu2S + H+ = 2Cu+ + HS-

-34.62

   

0.5Cu2S + 1.5HS- + 0.5H+ = Cu(HS)2-

-0.13

   

Cu2S + 2HS- = Cu2S(HS)22-

-4.75

10

Crystalline greenockite (gr) and two amorphous precipitates (al and a2)

25

CdS(gr) + H+ = Cd2+ + HS-

-14.82

   

CdS(al) + H+ = Cd2+ + HS-

-14.40

   

CdS(a2)+H+ = Cd2++HS-

-14.15

   

Cd2++HS- = Cd(HS)+

+7.38

   

Cd2+2HS- = Cd(HS)2°

+14.43

   

Cd2+3HS- = Cd(HS)3

+16.28

   

Cd2+4HS- = Cd(HS)42-

+18.43

63

Crystalline greenockite

25

CdS + H+ = Cd2+ + HS-

-14.36

   

Cd2+ + 3HS- = Cd(HS)3-

+16.44

   

Cd2+ + 4HS- = Cd(HS)42-

+17.89

   

Cd2++HS-+H2O = CdOHS-+2H+

-2.47

62

Amorphous CdS

25

CdS + H+ = Cd2+ + HS-

-12.28d

   

Cd2++HS- = Cd(HS)+

+7.55

   

Cd2++2HS- = Cd(HS)2°

+14.61

   

Cd2++3HS- = Cd(HS)3-

+16.49

   

Cd2++4HS- = Cd(HS)42-

+19.35

  1. aAdjusted from S2- using Gubeli's[53] dissociation constant: HS- = H++ S2-, log K = -13.48.
  2. bAdjusted using the reaction from Shea and Helz:[58] 4S(s) + HS- = S52- + H+, log K = -9.44.
  3. cAdjusted using the reaction from Shea and Helz:[58] 3S(s) + HS- = S42- + H+, log K = -9.56.
  4. dAdjusted from S2- using Ste. Marie's[62] dissociation constant: HS- = H+ + S2-, log K = -13.48.