Fukushi Keisuke, Sato Tsutomu, Yanase Nobuyuki
Division of Global Environmental Science and Engineering, Graduate School of Natural Science and Technology, and Institute of Nature and Environmental Technology, Kanazawa University, Kakuma, Kanazawa, Ishikawa 920-1192, Japan.
Environ Sci Technol. 2003 Aug 15;37(16):3581-6. doi: 10.1021/es026427i.
Sorption behavior of As(V) by synthesized schwertmannite was examined under pH 3.3 as a function of As(V) concentration in the initial solution and interpreted in term of solid-solution reactions. Results showed that schwertmannite released 0.62 mmol of SO4(2-) for every 1 mmol of H2AsO4- and 0.24 mmol of OH- that has been sorbed. As(V) replaced SO4 up to half of the total SO4 in schwertmannite. The quantitative relationship among the three chemical compositions indicated that As(V)-sorbed schwertmannite would behave as a solid solution between the As(V) free schwertmannite and schwertmannite containing the maximum level of As(V). The equilibrium constant for the anion exchange in the solid-solution reaction estimated from the reacted solution chemistry depicts the As(V) content found in precipitates formed in acid mine drainage and laboratory experiments. Although schwertmannite is metastable with respect to goethite, the transformation is significantly inhibited by sorption of As(V). The solid-solution reactions also explain the stabilization of schwertmannite by sorption of As(V).
在pH值为3.3的条件下,研究了合成施氏矿物对五价砷(As(V))的吸附行为,考察了其与初始溶液中As(V)浓度的关系,并从固液反应的角度进行了解释。结果表明,每吸附1 mmol的H2AsO4-,施氏矿物会释放0.62 mmol的SO4(2-),同时吸附0.24 mmol的OH-。As(V)取代了施氏矿物中高达一半的总SO4。这三种化学成分之间的定量关系表明,吸附了As(V)的施氏矿物将表现为不含As(V)的施氏矿物与含最大量As(V)的施氏矿物之间的固溶体。根据反应溶液化学估算的固溶体反应中阴离子交换的平衡常数,描述了在酸性矿山排水和实验室实验中形成的沉淀物中发现的As(V)含量。尽管相对于针铁矿而言,施氏矿物是亚稳的,但As(V)的吸附显著抑制了其转变。固溶体反应也解释了As(V)的吸附对施氏矿物的稳定作用。