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1.
15 p, 669.8 KB Reductive degradation of p,p'-DDT by Fe(II) in nontronite NAu-2 / Fialips, Claire I. (Newcastle University. School of Civil Engineering and Geosciences) ; Cooper, Nicola G. A. (Newcastle University. School of Civil Engineering and Geosciences) ; Jones, D. Martin (Newcastle University. School of Civil Engineering and Geosciences) ; White, Maggie L. (Newcastle University. School of Civil Engineering and Geosciences) ; Gray, Neil D. (Newcastle University. School of Civil Engineering and Geosciences)
Clay minerals are abundant in soils and sediments and often contain Fe. Some varieties, such as nontronites, contain as much as 40 wt. % FeO within their molecular structure. Several studies have shown that various Fe-reducing micro-organisms can use ferric iron in Fe-bearing clay minerals as their terminal electron acceptor, thereby reducing it to ferrous iron. [...]
2010 - 10.1346/CCMN.2010.0580610
Clays and Clay Minerals, Vol. 58, Núm. 6 (2010) , p. 821-836  
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2.
12 p, 504.0 KB Differences in the dehydration-rehydration behavior of halloysites : New evidence and interpretations / Joussein, Emmanuel (CNRS UMR 6532 HydrASA. Faculté des Sciences) ; Petit, Sabine (CNRS UMR 6532 HydrASA. Faculté des Sciences) ; Fialips, Claire-Isabelle (School of Civil Engineering and Geosciences. University of Newcastle upon Tyne) ; Vieillard, Philippe (CNRS UMR 6532 HydrASA. Faculté des Sciences) ; Righi, Dominique (CNRS UMR 6532 HydrASA. Faculté des Sciences)
Two reference halloysites from New Zealand (Te Puke and Opotiki) were studied by X-ray diffraction under (1) various levels of relative humidity (RH) from 95 to 0% (dehydration), and (2) various temperatures increasing from 25 to 120°C (dehydration). [...]
2006 - 10.1346/CCMN.2006.0540408
Clays and Clay Minerals, Vol. 54, Núm. 4 (2006) , p. 473-484  
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1 Fialips, Claire-Isabelle
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