摘要 : The coprecipitation of dissolved organic matter (DOM) and phosphate with Fe(III) at the sediment-water interface plays an important role in the biogeochemical cycle of organic carbon (OC) and phosphorus (P) in aquatic ecosystems. ... 展开
作者 | Luo~ ChunYan Wen~ ShuaiLong Lu~ YueHan Dai~ JiaRu Du~ YingXun |
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作者单位 | |
期刊名称 | 《Chemical geology》 |
总页数 | 9 |
语种/中图分类号 | 英语 / P59 |
关键词 | Humic acids Phosphate Coprecipitation Fractionation Sequestration Adsorption Eutrophication Carbon burial Phosphorus burial Lake sediment DISSOLVED ORGANIC-MATTER MOLECULAR-WEIGHT IRON FERRIHYDRITE FRACTIONATION FE ADSORPTION REACTIVITY LAKES ASSOCIATIONS |
馆藏号 | N2008EPST0000621 |