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国家自然科学基金(41071141)

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亚热带典型花岗岩小流域径流化学特征与化学风化被引量:3
2012年
为了解小流域尺度下生物地球化学过程对径流水体的影响及花岗岩化学风化对CO2的吸收,对亚热带典型花岗岩区不同利用条件下的2个相邻小流域(F-森林、FA-森林/农田)的地表径流及其常量离子和溶解Si含量进行了连续3年的定期观测和分析.结果表明,溶解Si,Na+和HCO3-构成地表径流的主要化学成分,FA流域离子总量高于F流域,反映了流域内农业活动对其化学径流的贡献.皖南典型花岗岩小流域(F、FA)径流中Sidiss/Na+和NO3-/SO24-比值均远高于同一生物气候带内富含碳酸盐岩的太湖流域径流中的相应值,揭示了区域岩性差异和人类活动导致的大气酸沉降组成差异是决定径流化学组成的主要因素.皖南花岗岩小流域(F、FA)径流化学组分约43%和38%来源于大气降水,57%和50%来源于岩石风化,FA流域内农业活动对其化学径流的贡献约为12%.皖南小流域(F、FA)花岗岩化学风化过程对CO2的消耗通量分别为(0.67—0.96)×105 mol.km-.2a-1和(0.64—1.05)×105 mol.km-.2a-1,远低于同一生物气候带内石灰岩母质流域.
黄来明张甘霖杨金玲
关键词:流域花岗岩化学风化
Nitrogen sink in a small forested watershed of subtropical China被引量:4
2011年
Global nitrogen (N) emission and deposition have been increased rapidly due to massive mobilization of N which may have longreaching impacts on ecosystems.Many agricultural and forest ecosystems have been identified as secondary N sources.In the present study,the input-output budget of inorganic N in a small forested watershed of subtropical China was investigated.Inorganic N wet deposition and discharge by stream water were monitored from March,2007 to February,2009.The concentrations and fluxes of inorganic N in wet precipitation and stream water and net retention of N were calculated.Global N input by dry deposition and biological fixation and N output by denitrification for forested watersheds elsewhere were reported as references to evaluate whether the studied forested watershed is a source or a sink for N.The results show that the inorganic N output by the stream water is mainly caused by NO 3-N even though the input is dominated by NH 4 +-N.The mean flux of inorganic N input by wet precipitation and output by stream water is 1.672 and 0.537 g N/(m 2 ·yr),respectively,which indicates that most of inorganic N input is retained in the forested watershed.Net retention of inorganic N reaches 1.135 g N/(m 2 ·yr) considering wet precipitation as the main input and stream water as the main output.If N input by dry deposition and biological fixation and output by denitrification are taken into account,this subtropical forested watershed currently acts as a considerable sink for N,with a net sink ranging from 1.309 to 1.913 g N/(m 2 ·yr) which may enhance carbon sequestration of the terrestrial ecosystem.
Laiming Huang
关键词:森林流域小氮肥森林生态系统大气降水
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