侵蚀土壤地表径流和土壤渗透的研究
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STUDY ON RUNOFF AND PERMEABILITY OF ERODED SOILS
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    摘要:

    我国南方水土流失区属水蚀区,地表径流是引起土壤侵蚀的主要动力.研究不同土壤在特定降雨条件下,降雨持续时间与地表径流的关系、土壤渗透时间与渗透速度的关系、渗透时间与渗透总量的关系,掌握地表径流和土壤渗透规律,揭示地表径流、土壤渗透与土壤环境、土壤性质的内在联系,可为保护、改良土壤,防治土壤侵蚀,以及进行侵蚀预报提供理论依据.为此,我们在采用渗透筒法进行土壤渗透性研究[6]的基础上,进一步采用人工降雨方法,对侵蚀土壤地表径流和土壤渗透进行研究.

    Abstract:

    Based on the data of artificial rain obtained from 42 experimental plots on the different eroded soils including red earths derved from quaternary red clay and granite and puple soils in Xingguo County of Jiangxi Province,the equations,W=aTb,V =aTb and M=(a+b/T)-1, were established by curve-fitting method to give expression to the relationship between raining duration and runoff coefficient,infiltration time and its rate,and infiltration time and its capacity.These equations are of practical significance for revealing the characteristics of runoff and permeability,estimating the amount of runoff and loss of soil by erosion and evalusting the beneficial effect of soil conservation.

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杨艳生,史德明,姚宗虞.侵蚀土壤地表径流和土壤渗透的研究[J].土壤学报,1984,21(2):203-210. Yang Yansheng, Shi Deming, Yao Zongyu. STUDY ON RUNOFF AND PERMEABILITY OF ERODED SOILS[J]. Acta Pedologica Sinica,1984,21(2):203-210.

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  • 在线发布日期: 2013-02-25
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