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晋西黄土区坡面水土保持林地产流产沙的观测分析
引用本文:张建军,朱金兆.晋西黄土区坡面水土保持林地产流产沙的观测分析[J].北京林业大学学报,1996,18(3):14-20.
作者姓名:张建军  朱金兆
作者单位:北京林业大学水土保持学院
摘    要:以径流小区的观测资料为依据,对晋西黄土区坡面水土保持林地降雨、径流、泥沙进行了分析,该地区产生地表径流的基本降雨条件为最大雨强在10mm/h以上,降雨量在10mm以上;该地区能够造成土壤侵蚀的主要降雨形式为降雨量在30mm以上的降雨。该文还建立了计算地表径流量的回归模型。

关 键 词:地表径流,土壤侵蚀,水土保持林,晋西黄土区

Analysis on the Runoff and Sediment Yields of Soil and Water Conservation Forests on Loess Slope in the West of Shanxi Province
Zhang Jianjun,Zhu Jinzhao, Wei Tianxing.Analysis on the Runoff and Sediment Yields of Soil and Water Conservation Forests on Loess Slope in the West of Shanxi Province[J].Journal of Beijing Forestry University,1996,18(3):14-20.
Authors:Zhang Jianjun  Zhu Jinzhao  Wei Tianxing
Abstract:Based on the data of runoff plots, runoff and sediment yiekls were analyzed in theforests of soil and water conservation in the Loess region, west of Shanxi province,It was sug-gested that surface runoff was caused only under the condition that the maximum rainfall intensi-ty was more than 10mm per hour with precipitation over 10mm. Soil erosion was preduced underthe condition of precipitation more than 30mm. A regressive medel was also put forward in thispaper.
Keywords:surface runoff  soil ercosion  forest of soil and water conservation  Loess region
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