Core |
Atom |
R/Å |
N |
σ2/Å2
|
ΔE0/eV |
|
|
Sediments |
SC4-12 |
Cd–Sa
|
2.50e
|
4.0 |
0.0044e
|
-1.0e
|
|
34.5 cm |
|
|
|
|
|
|
192 ppm |
|
|
|
|
|
|
Cl-2 |
Cd–Sa
|
2.51e
|
4.0 |
0.005 le
|
-1.4e
|
|
55.0 cm |
|
|
|
|
|
|
1222 ppm |
|
|
|
|
|
|
SC4-11 |
Cd–Sb
|
2.51 |
1.9e
|
0.0050 |
-4.1e
|
|
31.5 cm |
Cd–Ob
|
2.31e
|
3.2e
|
0.01 20e
|
|
|
Leached |
|
|
|
|
|
|
|
|
|
|
|
|
|
Reference precipitatesc
|
Cd1.0S |
Cd–S |
2.51e
|
4.0 |
0.0056e
|
-1.7e
|
|
Cd0.25S |
Cd–S |
2.51e
|
4.0 |
0.0048e
|
-2.6e
|
|
|
|
|
|
|
|
|
Reference compound: greenockite (CdS)d
|
|
Cd–S |
2.52 |
1 |
|
|
|
|
Cd–S |
2.53 |
3 |
|
|
|
|
Cd–Cd |
4.12 |
6 |
|
|
|
|
Cd–Cd |
4.13 |
6 |
|
|
|
|
|
|
|
|
|
|
Scale factor (S02) = 1.5. aFirst-shell Cd–S coordination fixed at 4; R and σ2 were varied. b For the sulfide component, R and σ2 were fixed on the average of values determined from fits to reference precipitates; N was varied. If NCd–S = 4 and Ncd–O = 6 are assumed, then the sulfide component is 47% and the oxide component is 53% of the total absorption spectrum. c Cadmium sulfide was precipitated by adapting an FeS method.10 XAS spectra collected on wet samples immediately after precipitation. d Crystallographic values for greenockite from ref. 58. e Parameter varied in least-squares fits. |
|
|
|
|
|
|
|
|
Zinc EXAFS analysis |
|
Core |
Rel. % |
Atom |
R/Å |
N |
σ2/Å2
|
ΔE0/eV |
|
Sulfide componentf
|
SC4-1 |
75 |
Zn–S |
2.33 |
3.0l
|
0.0065 |
-5.2l
|
2.5 cm |
|
Zn–Zn |
3.83 |
8.9 |
0.0231l
|
|
287 ppm |
|
Zn–S |
4.49 |
8.9 |
0.0267l
|
|
SC4-12 |
78 |
Zn–S |
2.33 |
3.1l
|
0.0065 |
-6.3l
|
34.5 cm |
|
Zn–Zn |
3.83 |
9.3 |
0.0221l
|
|
515 ppm |
|
Zn–S |
4.49 |
9.3 |
0.0297l
|
|
C3-9 |
90 |
Zn–S |
2.33 |
3.6l
|
0.0065 |
-5.2l
|
55.0 cm |
|
Zn–Zn |
3.83 |
10.8 |
0.0259l
|
|
486 ppm |
|
Zn–S |
4.49 |
10.8 |
0.0257l
|
|
SC4-11 |
25 |
Zn–S |
2.33 |
0.9l
|
0.0065 |
-5.9l
|
31.5 cm |
|
Zn–Zn |
3.82 |
2.6 |
0.0225l
|
|
Leached |
|
Zn–S |
4.49 |
2.6 |
0.0139l
|
|
|
|
|
|
|
|
|
Oxide componentg
|
SC4-1 |
25 |
Zn–O |
2.04l
|
1.7l
|
0.0065 |
-5.2l
|
2.5 cm |
|
Zn–Meh
|
3.13l
|
1.0l
|
0.0080 |
|
287 ppm |
|
Zn–Mei
|
3.13l
|
0.8l
|
0.0100 |
|
SC4-12 |
22 |
Zn–O |
1.99l
|
1.4l
|
0.0065 |
-6.3l
|
34.5 cm |
|
Zn–Meh
|
3.06l
|
0.9l
|
0.0080 |
|
515 ppm |
|
Zn–Mei
|
3.13l
|
0.8l
|
0.0080 |
|
|
|
Zn–Mej
|
3.21l
|
1.7l
|
0.0080 |
|
C3-9 |
10 |
Zn–O |
2.09l
|
1.4l
|
0.0065 |
-5.2l
|
55.0 cm |
|
Zn–Mef
|
3.10l
|
0.4l
|
0.0080 |
|
486 ppm |
|
|
|
|
|
|
SC4-11 |
75 |
Zn–O |
2.02l
|
3.2l
|
0.0065 |
-5.9l
|
31.5 cm |
|
Zn–Meh
|
3.13l
|
1.3l
|
0.0080 |
|
Leached |
|
Zn–Mej
|
3.39l
|
0.6l
|
0.0080 |
|
|
|
|
|
|
|
|
Reference compound: sphalerite (ZnS)k
|
|
|
Zn–S |
2.33 |
4 |
|
|
|
|
Zn–Zn |
3.83 |
12 |
|
|
|
|
Zn–S |
4.49 |
12 |
|
|
|
|
|
|
|
|
|
Scale factor (So2) = 1.0. f Sulfide component: Interatomic distances (R) for Zn–S and Zn–Zn fixed on Crystallographic values in sphalerite; first-shell σ2 for Zn–S was fixed on an empirical value determined from fits to sulfide reference compounds. For higher Zn–Zn and Zn–S shells, N was fixed on the value calculated from the proportion of sphalerite component determined in fits to filtered first-shell spectra and σ2 was varied. g Oxide component: Values for σ2 were fixed for all shells based on empirical fits to reference compounds; R and N were varied. h Backscatterer is Fe or similar transition metal cation; edge-sharing octahedra. i Backscatterer is Mg or Al; edge-sharing octahedra. jBackscatterer is Fe or Si; corner-sharing octahedra or tetrahedra. k Crystallographic values for sphalerite from ref. 28. lParameter varied in least-squares fit. |
|
|
|
|
|
|
|
|
Chromium EXAFS analysis |
|
Core |
Atom |
R/Å |
N |
σ2/Å2
|
ΔE0/eV |
|
|
Oxide componentm
|
SC2-7 |
Cr–O |
1.97s
|
6.0 |
0.0035s
|
-8.5s
|
|
19.5 cm |
Cr–Men
|
3.01s
|
1.9s
|
0.0100 |
|
|
<2 μm |
Cr–Meo
|
3.00s
|
1.7s
|
0.0100 |
|
|
392 ppm |
Cr–Fe |
3.42s
|
1.8s
|
0.0080 |
|
|
SC4-1 |
Cr–O |
1.98s
|
6.0 |
0.0041s
|
-8.9s
|
|
1.5 cm |
Cr–Mep
|
2.97s
|
1.6s
|
0.0080 |
|
|
243 ppm |
Cr–Fe |
3.44s
|
1.9s
|
0.0080 |
|
|
SC4-12 |
Cr–O |
1.97s
|
6.0 |
0.0041s
|
-6.0s
|
|
34.5 cm |
Cr–Mep
|
3.02s
|
1.1s
|
0.0100 |
|
|
766 ppm |
Cr–Fe |
3.44s
|
2.2s
|
0.0080 |
|
|
SC4-11 |
Cr–O |
1.98s
|
6.0 |
0.0037s
|
-8.8s
|
|
31.5 cm |
Cr–Op
|
3.00s
|
1.8s
|
0.0100 |
|
|
Leached |
Cr–Fe |
3.42s
|
1.2s
|
0.0080 |
|
|
|
|
|
|
|
|
|
Reference compounds |
|
|
|
|
|
|
Cr2S3q
|
Cr-S |
2.42 |
6 |
|
|
|
|
Cr–Cr |
2.79 |
2 |
|
|
|
|
Cr-S |
4.20 |
6 |
|
|
|
K2Cr2O7r
|
Cr–O |
1.52, 1.54, |
4 |
|
|
|
|
|
1.73, 1.85 |
|
|
|
|
|
Cr–Cr |
3.13 |
1 |
|
|
|
|
Cr–K |
3.26 |
1 |
|
|
|
|
|
|
|
|
|
|
Scale factor (So2) = 0.90. m Oxide component: First-shell Cr–O coordination fixed at 6; σ2 was varied. For higher shells, values for σ2were fixed based on empirical fits to reference compounds; R and N were varied. n Backscatterer is Mg or Al; edge-sharing octahedra. o Backscatterer is Fe or similar transition metal cation; edge-sharing octahedra. p Fit with single shell of Fe atoms; probably a disordered shell of Al, Mg, and Fe atoms. q Crystallographic values from ref. 59. r Crystallographic values from ref. 60. s Parameter varied in least-squares fits. |
|
|
|
|
|
|
|
|
Iron EXAFS analysis |
|
Core |
Rel. % |
Atom |
R/Å |
N
w
|
σ2/Å2
|
Δ E0/eV |
|
Pyrite componentt
|
SC4-1 |
35.6 |
Fe–S |
2.25 |
0.80 |
0.0011 |
-7.2w
|
2.5 cm |
|
Fe–S |
3.44 |
0.80 |
0.0066 |
|
|
|
Fe–Fe |
3.82 |
1.60 |
0.0066 |
|
|
|
|
|
|
|
|
SC4-12 |
38.5 |
Fe–S |
2.25 |
0.92 |
0.0011 |
-6.7w
|
34.5 cm |
|
Fe–S |
3.44 |
0.92 |
0.0066 |
|
|
|
Fe–Fe |
3.82 |
1.84 |
0.0066 |
|
SC4-11 |
21.4 |
Fe–S |
2.25 |
0.66 |
0.0011 |
-8.3w
|
31.5 cm |
|
Fe–S |
3.44 |
0.66 |
0.0066 |
|
Leached |
|
Fe–Fe |
3.82 |
1.32 |
0.0066 |
|
|
|
|
|
|
|
|
Oxide component |
SC4-1 |
64.4 |
Fe–O |
2.00w
|
2.64 |
0.0048 |
-3.4w
|
2.5 cm |
|
Fe–Fe |
3.10w
|
0.53 |
0.0050 |
|
|
|
Fe–Si |
3.26 |
1.43 |
0.0057 |
|
|
|
Fe–Fe |
3.39w
|
0.29 |
0.0057 |
|
SC4-12 |
61.5 |
Fe–O |
2.00w
|
2.79 |
0.0048 |
-3.2w
|
34.5 cm |
|
Fe–Fe |
3.09w
|
0.62 |
0.0050 |
|
|
|
Fe–Si |
3.26 |
1.15 |
0.0057 |
|
|
|
Fe–Fe |
3.43w
|
0.41 |
0.0057 |
|
SC4-11 |
78.6 |
Fe–O |
2.00w
|
3.12 |
0.0048 |
-0.5w
|
31.5 cm |
|
Fe–Fe |
3.09w
|
0.92 |
0.0050 |
|
Leached |
|
Fe–Si |
3.26 |
0.82 |
0.0057 |
|
|
|
Fe–Fe |
3.39w
|
0.41 |
0.0057 |
|
|
|
|
|
|
|
|
Reference compound: pyrite (FeS2)v
|
|
|
Fe–S |
2.25 |
6 |
|
|
|
|
Fe–S |
3.44 |
6 |
|
|
|
|
Fe–Fe |
3.82 |
12 |
|
|
|
|
|
|
|
|
|
t Pyrite component: Interatomic distances (R) were fixed on crystallo-graphic values from pyrite and σ2 was fixed on values determined from fits to reference sulfide compounds. N for each shell was floated as a linked variable in proportions based on the known coordination in pyrite. Relative percent (Rel. %) for pyrite or oxide components is calculated from the integrated fit areas of all atomic shells comprising each component (normalized to 100%). uOxide component: Values for σ2 were fixed for all shells based on empirical fits to reference compounds of similar composition and structure; R and N were varied, except for the Fe–Si shell, which will co-vary with Fe shells if floated independently. This shell was fixed on a typical crystallo-graphic distance for Fe–Si in phyllosilicates. v Crystallographic values from ref. 61. w Parameter varied in least-squares fit. |