Literature DB >> 10536285

The stabilities of calcium arsenates at 23+/-1 degrees C.

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Abstract

The stabilities of calcium arsenate compounds were established by analysis of suspensions made with varying molar Ca/As ratios. Solution chemistry analyses determined the concentrations of calcium and arsenic and pH. The phases that were shown to form in order of descending pH were Ca(4)(OH)(2)(AsO(4))(2).4H(2)O, Ca(5)(AsO(4))(3)OH (arsenate-apatite), Ca(3)(AsO(4))(2).3 23H(2)O, Ca(3)(AsO(4))(2).4 14H(2)O, Ca(5)H(2)(AsO(4))(4).9H(2)O - ferrarisite, Ca(5)H(2)(AsO(4))(4).9H(2)O - guerinite and CaHAsO(4).H(2)O. The analytical concentrations of calcium and arsenic and pH were used in estimating solubility products. The estimated values were then refined through the comparison of the analytical data with calculated K(sp) values using the computer program PhreeqC. From the refined solubility products, the free energies of formation of the calcium arsenate hydrates were calculated as follows: Ca(4)(OH)(2)(AsO(4))(2).4H(2)O (-4941 kJ/mol), Ca(5)(AsO(4))(3)OH (-5087 kJ/mol), Ca(3)(AsO(4))(2).3 23H(2)O (-3945 kJ/mol), Ca(3)(AsO(4))(2).4 14H(2)O (-4085 kJ/mol), Ca(5)H(2)(AsO(4))(4).9H(2)O - ferrarisite (-7808 kJ/mol), Ca(5)H(2)(AsO(4))(4).9H(2)O - guerinite (-7803 kJ/mol), and CaHAsO(4).H(2)O (-1533 kJ/mol). Unlike other solubility studies on arsenate immobilization, this study was the first to consider the complete array of calcium arsenate hydrates that can form and to use the associated ions, CaAsO(4)(-), CaHAsO(4)(0) and CaH(2)AsO(4)(+) in determining their solubility products.

Entities:  

Year:  1999        PMID: 10536285     DOI: 10.1016/s0304-3894(99)00105-3

Source DB:  PubMed          Journal:  J Hazard Mater        ISSN: 0304-3894            Impact factor:   10.588


  6 in total

1.  Effect of grain size and heavy metals on As immobilization by marble particles.

Authors:  M Simón; I García; V González; A Romero; F Martín
Journal:  Environ Sci Pollut Res Int       Date:  2014-11-30       Impact factor: 4.223

2.  Effect of simulated acid rain on stability of arsenic calcium residue in residue field.

Authors:  Jiangchi Fei; Jingjing Ma; Jinqin Yang; Yanjie Liang; Yong Ke; Liwei Yao; Yuancheng Li; Degang Liu; Xiaobo Min
Journal:  Environ Geochem Health       Date:  2019-03-09       Impact factor: 4.609

3.  Groundwater chemistry and arsenic mobilization in the Holocene flood plains in south-central Bangladesh.

Authors:  Prosun Bhattacharya; M Aziz Hasan; Ondra Sracek; Euan Smith; K Matin Ahmed; Mattias von Brömssen; S M Imamul Huq; Ravi Naidu
Journal:  Environ Geochem Health       Date:  2009-01-03       Impact factor: 4.609

4.  Geochemistry of mine tailings and behavior of arsenic at Kombat, northeastern Namibia.

Authors:  O Sracek; M Mihaljevič; B Kříbek; V Majer; J Filip; A Vaněk; V Penížek; V Ettler; B Mapani
Journal:  Environ Monit Assess       Date:  2014-04-02       Impact factor: 2.513

5.  Synthesis and thermodynamic properties of arsenate and sulfate-arsenate ettringite structure phases.

Authors:  Weixing Wang; Yan Shao; Haobo Hou; Min Zhou
Journal:  PLoS One       Date:  2017-07-31       Impact factor: 3.240

6.  Alternative Method for the Treatment of Hydrometallurgical Arsenic-Calcium Residues: The Immobilization of Arsenic as Scorodite.

Authors:  Xu Ma; Zidan Yuan; Guoqing Zhang; Jiaxi Zhang; Xin Wang; Shaofeng Wang; Yongfeng Jia
Journal:  ACS Omega       Date:  2020-05-28
  6 in total

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