Dissolution, Solubility, and Stability of the Basic Ferric Sulfate-Arsenates [Fe(SO4)x(AsO4)y(OH)z·nH2O] at 25–45°C and pH 2–10
Dissolution, Solubility, and Stability of the Basic Ferric Sulfate-Arsenates [Fe(SO4)x(AsO4)y(OH)z·nH2O] at 25–45°C and pH 2–10
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碱式硫酸铁砷酸盐 [Fe(SO4)x(AsO4)y(OH)z·nH2O] 在 25–45°C 和 pH 2–10 下的溶解度、溶解度和稳定性
DOI:
10.1155/2021/5556295
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发表时间:
2021-06
影响因子:
3
通讯作者:
Xingxing Wang
中科院分区:
文献类型:
--
作者:
Zongqiang Zhu;Hongqu Yang;Jie Liu;Yinian Zhu;Shen Tang;Lihao Zhang;Xingxing Wang
Basic ferric sulfate-arsenates [FeSAsOH, Fe(SO4)x(AsO4)y(OH)z·nH2O] were prepared and characterized to study their potential fixation of arsenic in the oxidizing and acidic environment through a dissolution for 330d. The synthetic solids were well-shaped monoclinic prismatic crystals. For the dissolution of the sample FeSAsOH–1 [Fe(SO4)0.27(AsO4)0.73 (OH)0.27·0.26H2O] at 25–45°C and initial pH 2, all constituents preferred to be dissolved in the order of AsO43− SO42− Fe3+ in 1–3 h, in the order of SO42− AsO43− Fe3+ from 1–3 h to 12–24 h, and finally in the order of SO42− Fe3+ AsO43−. The released iron, sulfate, and arsenate existed dominantly as Fe3+/Fe(OH)2+/FeSO4+, HSO4−/SO42−/FeSO4+, and H3AsO40/H2AsO4−, respectively. The higher initial pHs (6 and 10) could obviously inhibit the release of Fe3+ from solid into solution, and the solid components were released in the order of SO42− AsO43− Fe3+. The crystal tops were first dissolved, and the crystal surfaces were gradually smoothed/rounded until all edges and corners disappeared. The dissociations were restricted by the Fe-O(H) breakdown in the FeO6 octahedra and obstructed by the OH− and AsO4 tetrahedra outliers; the lowest concentration of the dissolved arsenic was 0.045 mg/L. Based on the dissolution experiment at 25°C and pH 2, the solubility products (Ksp) for the basic ferric sulfate-arsenate [Fe(SO4)0.27(AsO4)0.73 (OH)0.27·0.26H2O], which are equal to the ion activity products (logˍIAP) at equilibrium, were calculated to be -23.04 ± 0.01 with the resulting Gibbs free energies of formation (ΔGfo) of −914.06 ± 0.03 kJ/mol.
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DOI:
10.1007/978-94-011-1214-7_10
发表时间:
1994
期刊:
--
影响因子:
--
作者:
Pm Swash-;A. Monhemius
通讯作者:
Pm Swash-;A. Monhemius
DOI:
10.1007/s11144-016-1065-y
发表时间:
2016-08
期刊:
Reaction Kinetics, Mechanisms and Catalysis
影响因子:
--
作者:
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通讯作者:
F. Patiño;Mizraim U. Flores;I. Reyes;S. Ordóñez;J. Eliecer Méndez;Víctor H. Flores;Hernán Islas;Martín Reyes
DOI:
10.5860/choice.33-6312
发表时间:
1970
期刊:
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影响因子:
--
作者:
W. Stumm;J. J. Morgan-J.
通讯作者:
W. Stumm;J. J. Morgan-J.
DOI:
10.1017/cbo9781139207249.009
发表时间:
2012
期刊:
--
影响因子:
--
作者:
W. Marsden
通讯作者:
W. Marsden
影响因子:
2.5
作者:
Gomez, M. A.;Assaaoudi, H.;Demopoulos, G. P.
通讯作者:
Demopoulos, G. P.