期刊
COMPTES RENDUS GEOSCIENCE
卷 335, 期 16, 页码 1199-1206出版社
ELSEVIER FRANCE-EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER
DOI: 10.1016/j.crte.2003.07.007
关键词
biogeochemical cycle of silicon; biogenic silica; phytoliths; silicate weathering; soil-plants interactions
Silicon is the most abundant element after oxygen in the lithosphere (27 wt%). Plants and soil microorganisms are important contributors to the weathering of silicates. Plants are able to accumulate several percent of Si in the biomass. The importance of plants in the rates of Si output to surface waters is discussed in this paper. (C) 2003 Academie des sciences. Publie par Elsevier SAS. Tous droits reserves.
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