黄土高原土壤入渗速率的研究
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STUDY ON THE FILTRATION RATE OF SOILS ON THE LOESS PLATEAU OF CHINA
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    摘要:

    根据黄土高原土壤入渗速率的明显地域差异,绘制了黄土高原土壤入渗速率分区图;文中对比了用双圈法测得的土壤稳定入渗速率与用水文资料推出的小流域土壤稳定入渗速率.

    Abstract:

    The filtration rate of soils on Loess Plateau is different in varrious regions.In accordance with the steady infilatrition rate of the soils, Loess Plateau is divided into five regions of grade-Ⅰ and four regions of grade-Ⅱ.The regions of the highest filtration rate are located in Ziwuling, Liaoshan, Huanglongshan and the southern sector of Luliangshan Mt.on the central of the Plateau generally covered by secondary broadleaf forests of abores or brushes, the soil surface is commonly covered by a thick layer of litters;with good structure and greater porosity, the soils are the highest in filitritation rate.The regions of higher filtration rate include Hujialing, Dongzhiyuan of Gansu, Yijun, Zhouzhi, Meiaian and Changan of Shaanai, and Yicheng, Quwo of Shangi.

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蒋定生,黄国俊.黄土高原土壤入渗速率的研究[J].土壤学报,1986,23(4):299-305. Jiang Dingsheng, Huang Guojun. STUDY ON THE FILTRATION RATE OF SOILS ON THE LOESS PLATEAU OF CHINA[J]. Acta Pedologica Sinica,1986,23(4):299-305.

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  • 在线发布日期: 2013-02-25
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