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Infiltration Characteristics Under Different Land Uses in Yuanmou Dry-Hot Valley Area

机译:元谋干热河谷地区不同土地利用方式下的入渗特征

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On the basis of soil physical index determination of four land use types (arbor forest, shrub land, grassland, and bare wasteland) of Yuanmou dry-hot valley, the soil infiltration characteristics were studied. The results showed that there were differences on soil bulk density, soil porosity, initial soil water infiltration rate, and stable soil water infiltration rate. The steady infiltration rate and soil bulk density are exponential, Greater the soil bulk density, the lower the infiltration rate; smaller soil bulk density, the greater the porosity and porosity ratio, as well as the infiltration rate. Among different stands, It is observed from the research that from the average infiltration rate and steady infiltration rate, its order from high to low was arbor forest, shrub land, grass land, and bare wasteland.
机译:在确定元谋干热河谷四种土地利用类型(乔木林,灌木林地,草地和裸露荒地)的土壤物理指标的基础上,研究了土壤入渗特征。结果表明,土壤容重,孔隙度,初始土壤水分入渗速率和稳定土壤水分入渗速率存在差异。稳定的入渗速率与土壤容重呈指数关系,土壤容重越大,入渗率越低;土壤容重越小,孔隙率和孔隙率以及渗透率越大。在不同林分之间,从研究中可以观察到,从平均入渗率和稳定入渗率来看,从高到低的顺序是乔木林,灌木地,草地和裸露的荒地。

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