Preparation and Eh-pH diagrams of Fe(II)-Fe(III) green rust compounds;: hyperfine interaction characteristics and stoichiometry of hydroxy-chloride, -sulphate and -carbonate

被引:51
作者
Genin, JMR [1 ]
Refait, P [1 ]
Simon, L [1 ]
Drissi, SH [1 ]
机构
[1] Univ Nancy 1, Lab Chim Phys Environm, UMR 9992 CNRS, F-54600 Villers Les Nancy, France
来源
HYPERFINE INTERACTIONS | 1998年 / 111卷 / 1-4期
关键词
D O I
10.1023/A:1012638724990
中图分类号
O64 [物理化学(理论化学)、化学物理学]; O56 [分子物理学、原子物理学];
学科分类号
070203 ; 070304 ; 081704 ; 1406 ;
摘要
Fe(II)-Fe(III) hydroxy-chloride, -sulphate and -carbonate were prepared by oxidation of a ferrous hydroxide precipitate in anion-containing aqueous solutions. The compounds are characterized by monitoring the redox potential E-h and the pH of stoichiometric suspension vs time with the appropriate concentration ratios. X-ray diffraction allows us to characterize the crystal structure by distinguishing "green rust one" (GR1) from "green rust two" (GR2). Since green rusts (GRs) are of a pyroaurite-sjogrenite-like structure, i.e., consisting of intercalated foreign anions and water molecules in the interlayers between the brucite-like layers of Fe(OH)(2), their chemical formulae can be determined from the Mossbauer spectra. Three quadrupole doublets are observed: D-1 and D-2 correspond to a ferrous state with isomershift IS of about 1.27 mm s(-1) and quadrupole splittings QS of about 2.85 and 2.60 mm s(-1), respectively, whereas D-3 corresponds to a ferric state with IS and QS of about 0.4 mm s(-1). The hyperfine parameters of these doublets are similar from one green rust to another but their intensity ratios vary considerably. Finally, E-h and pH equilibrium diagrams of the Fe species in the presence of chloride, sulphate and carbonate anions contained within the water solution are drawn and the thermodynamic conditions of existence and degrees of oxidation of green rusts are discussed.
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页码:313 / 318
页数:6
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