Natural attenuation of TCE, As, Hg linked to the heterogeneous oxidation of Fe(II): an AFM study

被引:91
作者
Charlet, L
Bosbach, D
Peretyashko, T
机构
[1] Univ Grenoble 1, CNRS, OSUG, Observ Earth & Planetary Sci,Environm Geochem Grp, F-38041 Grenoble, France
[2] Univ Munster, Inst Mineral, D-48149 Munster, Germany
关键词
ferrous iron; natural attenuation; clay edges; mercury; AFM;
D O I
10.1016/S0009-2541(02)00122-5
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Hydrous ferric oxide (HFO) colloids formed, in strictly anoxic conditions upon oxidation of Fe2+ ions adsorbed on mineral surface, were investigated under in situ conditions by contact mode atomic force microscopy (AFM). Freshly cleaved and acid-etched large single crystals of near endmember phlogopite were pre-equilibrated with dissolved Fe(II) and then reacted with Hg(II), As(V) and trichlorethene (TCE)-bearing solutions at 25 degreesC and 1 atm. HFO structures are found to be of nanometer scale. The As(V)-Fe(II) and Hg(II)-Fe(II) reaction products are round (25 nm) microcrystallites located predominantly on the layer edges and are indicative of an accelerated Fe(II) oxidation rate upon formation of Fe(II) inner sphere surface complexes with the phyllosilicate edge surface sites. On the other hand, TCE-Fe(II)-phlogopite reaction products are needle-shaped (45 nm long) particles located on the basal plane along the Periodic Bond Chains (PCBs) directions. Experiments with additions of sodium chloride confirm the importance of the Fe(II) adsorption step in the control of the overall heterogeneous Fe(II)-TCE electron transfer reaction. Kinetic measurements at the nanomolar level of Hg-degrees formed upon reduction of Hg(II) by Fe(II) in presence of phlogopite particles provide further convincing evidence for reduction of Hg(II)(aq) coupled to the oxidation of Fe(II) adsorbed at the phlogopite-fluid interface, and indicate that sorption of Fe(II) to mineral surfaces enhances the reduction rate of Hg(II) species. The Hg(II) reduction reaction follows a first-order kinetic law. Under our experimental conditions, which were representative of many natural systems, 80% of the mercury is transferred to the atmosphere as Hgdegrees in less than 2 h. The reduction of a heavy metal (Hg), a toxic oxyanion (arsenate ion) and a chlorinated solvent (TCE) thus appear to be driven by the high reactivity of adsorbed Fe(II). This is of environmental relevance since these three priority pollutants are that way reductively transformed to a volatile, an immobilizable and a biodegradable species, respectively. Such kinetic data and reaction pathways are important in the evaluation of natural evaluation scenarios, in the optimization of Fe(II)/mineral mixtures as reductants in technical systems, and in general, in predicting the fate and transport of pollutants in natural systems. (C) 2002 Published by Elsevier Science B.V.
引用
收藏
页码:303 / 319
页数:17
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