Influence of Sedimentary Bedding on Reactive Transport Parameters under Unsaturated Conditions

Moisture and contaminant transport in partially saturated, heterogeneous, layered sediments is typically anisotropic. Solute transport parameters, including dispersivity and the adsorption coefficient, and the modeled concentration of reactive minerals may depend on the direction of flow with respec...

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Veröffentlicht in:	Soil Science Society of America journal 2009-11, Vol.73 (6), p.1938-1946
Hauptverfasser:	Mayes, Melanie A, Tang, Guoping, Jardine, Philip M, McKay, Larry D, Yin, Xiangping L, Pace, Molly N, Parker, Jack C, Zhang, Fan, Mehlhorn, Tonia L, Dansby-Sparks, Royce
Format:	Artikel
Sprache:	eng
Schlagworte:	ADSORPTION Agronomy. Soil science and plant productions Biological and medical sciences chemical reactions Cobalt COBALT COMPLEXES Colleges & universities Contaminants Cores dispersivity Earth sciences Earth, ocean, space EDTA EDTA (chelating agent) Environmental restoration ENVIRONMENTAL SCIENCES ENVIRONMENTAL TRANSPORT Exact sciences and technology Flow Fundamental and applied biological sciences. Psychology HYDRAULIC CONDUCTIVITY KINETICS layered soils MATHEMATICAL MODELS Minerals Moisture content pollutants saturated conditions SATURATION sedimentary soils SEDIMENTS soil hydraulic properties soil pollution Soil science soil transport processes soil water movement Soils Solute transport SOLUTES spatial variation Surficial geology TRACER TECHNIQUES unsaturated conditions
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