| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 7000912 | Journal of Colloid and Interface Science | 2011 | 11 Pages |
Abstract
⺠Scorodite was found to form at T >138 C and >90min independent of the presence or absence of copper sulfate in the solution. ⺠At <96 min and 138 C an intermediate copper containing ferric arsenate sulfate phase was observed for the first time. ⺠Excess ferric sulfate was found to slow down the full development of H-bond structure in scorodite. ⺠Analysis of an industrial residue found the arsenate environment to be similar to that of intermediate basic ferric arsenate sulfate (BFAS).
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Authors
M.A. Gomez, L. Becze, M. Celikin, G.P. Demopoulos,