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祁连山不同林地类型对土壤理化性质和水源涵养功能的影响 被引量:52

Influence of Different Type of Forest Land on Soil Physico-chemical Property and Function of Water Conservation
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摘要 以祁连山灌木林、针叶林、阔叶林3种林地为研究材料,探讨不同林地类型对土壤理化性质和水源涵养功能的影响,结果表明:土壤孔隙度、团粒结构、物理性粘粒含量均为灌木林>针叶林>阔叶林,土壤容重、物理性砂粒含量均为灌木林<针叶林<阔叶林;土壤有机质、全N、速效N、速效P、速效K、CEC均为灌木林>针叶林>阔叶林,而CaCO3、pH、全盐含量均为灌木林<针叶林<阔叶林;土壤水层厚度、自然含水量、饱和蓄水量、毛管蓄水量、非毛管蓄水量、贮水量均为灌木林>针叶林>阔叶林;枯落物积累厚度、枯落物积累干质量、持水量、最大持水率均为灌木林>针叶林>阔叶林。灌木林植物种类丰富,郁闭度大,枯落物积累数量多,水源涵养功能强。 This paper with the bush forest, needle leaf forest and rich leaf forest of Qilian mountains 3 kinds of forest land is research material, discuss the different type of forest land as soil reason melts, the influence of nature and the self-control function of source of water, show as a result: Soil porosity, granule structure and physicalness glue grain content is bush forest 〉 needle leaf forest 〉 rich leaf forest, soil unit weight and physicalness sand grain content are bush forest 〈 needle leaf forest 〈 rich leaf forest; Soil organic matter, whole N, N of quick result, P of quick result, K of quick result and CEC is bush forest 〉 needle leaf forest 〉 rich leaf forest, and CaCO3, pH, completely salt content is bush forest 〈 needle leaf forest 〈 rich leaf forest; Soil water layer thickness, natural water content, saturation reservoir storage and woollen pipe reservoir storage, not woollen pipe reservoir storage, store water quantity is bush forest 〉 needle leaf forest 〉 rich leaf forest; Withered fall thing accumulation thickness, withered fall thing accumulation dry quality, hold water quantity, biggest hold water rate is bush forest 〉 needle leaf forest 〉 rich leaf forest. Bush forest plant kind is rich, closing degree big, withered fall thing accumulation quantity much, the self-control function of source of water is strong.
出处 《水土保持学报》 CSCD 北大核心 2007年第1期92-94,139,共4页 Journal of Soil and Water Conservation
基金 国家自然科学基金重点项目子课题"黑河流域生态恢复问题的研究"(40235053)
关键词 祁连山 林地类型 理化性质 水源涵养 Qilian mountains type of forest land physical and chemical property self-control of source of water
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