揭示濕地土壤碳對(duì)水位下降響應(yīng)機(jī)制
發(fā)布時(shí)間:2019-05-12 03:25
【摘要】:正近日,中國(guó)科學(xué)院植物研究所馮曉娟研究組與北京大學(xué)教授賀金生團(tuán)隊(duì)合作,利用海北站高寒濕地中宇宙水位控制實(shí)驗(yàn),結(jié)合分子有機(jī)地球化學(xué)手段,對(duì)濕地水位下降過(guò)程中鐵氧化還原轉(zhuǎn)化過(guò)程對(duì)土壤有機(jī)碳動(dòng)態(tài)的調(diào)控機(jī)理展開研究。
[Abstract]:Recently, Feng Xiaojuan, a research team from the Institute of Botany of the Chinese Academy of Sciences, worked with he Jinsheng, a professor at Peking University, to use the cosmic water level control experiment in the alpine wetlands of Haibei Station, combined with molecular organic geochemistry. The regulation mechanism of iron redox conversion process on soil organic carbon dynamics during the decline of wetland water level was studied.
【分類號(hào)】:S153.6
,
本文編號(hào):2475068
[Abstract]:Recently, Feng Xiaojuan, a research team from the Institute of Botany of the Chinese Academy of Sciences, worked with he Jinsheng, a professor at Peking University, to use the cosmic water level control experiment in the alpine wetlands of Haibei Station, combined with molecular organic geochemistry. The regulation mechanism of iron redox conversion process on soil organic carbon dynamics during the decline of wetland water level was studied.
【分類號(hào)】:S153.6
,
本文編號(hào):2475068
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