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Physicochemical factors controlling the release of dissolved organic carbon from columns of forest subsoils
Author(s) -
Münch J.M.,
Totsche K. U.,
Kaiser K.
Publication year - 2002
Publication title -
european journal of soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.244
H-Index - 111
eISSN - 1365-2389
pISSN - 1351-0754
DOI - 10.1046/j.1365-2389.2002.00439.x
Subject(s) - dissolved organic carbon , ionic strength , distilled water , chemistry , total organic carbon , subsoil , organic matter , effluent , soil water , irrigation , flow velocity , environmental chemistry , water flow , soil science , flow (mathematics) , aqueous solution , environmental engineering , environmental science , chromatography , agronomy , organic chemistry , geometry , mathematics , biology
Summary Retention of dissolved organic carbon in soil depends on the chemical and physical environment. We studied the release of organic carbon from three carbonate‐free forest subsoil materials (Bs1, Bs2, Bg) in unsaturated column experiments as influenced by (i) variations of the flow regime and (ii) varied chemical properties of the irrigation solution. We investigated the effect of flow initiation, constant irrigation, interruptions to flow, and variation in the effective pore water velocity on the release of organic C. The influence of ionic strength and cation valence in the irrigation solution was studied by stepped pulses of NaCl and CaCl 2 . The release of C from all materials was characterized by an initial large output and a decline to constant concentrations under long‐term irrigation. Interrupting the flow increased its release when flow was resumed. The release from the Bs1 material was not related to the duration of the interruption. The Bs2 material, in contrast, released organic carbon in a way that was successfully described by a kinetic first‐order model. Increased pore water velocity decreased the concentrations of C in the effluent from it. The pH of the irrigation solution had negligible effects on the mobilization of C. Increased ionic strength reduced the release, whereas rinsing with distilled water increased the concentrations of C in the effluent. The response of dissolved C to pulses of weak solutions, however, was sensitive to the type of cation in the previous step with strong solutions. The results suggest that the release of organic matter in the soils depends on its colloidal properties.