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西部黄土丘陵区降雨特征及其对坡地土壤侵蚀的影响
引用本文:周子渊,王立,王小平,马海龙,李梦茹. 西部黄土丘陵区降雨特征及其对坡地土壤侵蚀的影响[J]. 水土保持通报, 2014, 0(3): 24-27
作者姓名:周子渊  王立  王小平  马海龙  李梦茹
作者单位:甘肃农业大学林学院, 甘肃兰州 730070;甘肃农业大学林学院, 甘肃兰州 730070;甘肃省定西市水土保持科学研究所, 甘肃定西 743000;甘肃省定西市水土保持科学研究所, 甘肃定西 743000;甘肃农业大学林学院, 甘肃兰州 730070
基金项目:甘肃省教育厅研究生导师项目"保护性耕作措施下坡耕地水土流失研究"(1102-08)
摘    要:
以甘肃省定西市安家沟流域的大型径流观测场为依托,以2009—2011年天然降雨在不同土地利用条件下产流产沙特征数据为依据,研究了黄土高原西部黄土丘陵区降雨特征及其对坡地土壤侵蚀的影响。结果表明,在次降雨条件下不同处理径流过程分别经历了产流、峰值、稳定、消减4个表征时刻,土壤侵蚀过程分别经历了发生、峰值、消减3个表征时刻。次降雨条件下,不同处理其径流总量、侵蚀总量排序均为:15°春小麦10°春小麦10°油松林15°荒地15°沙棘林10°荒地15°油松林10°沙棘林。通过层次聚类分析得出,在10°,15°的坡度下,灌木林沙棘、乔木林油松分别具有明显的水土保持效应。所以结合试验地的气候和环境特点,10°坡面适宜种植沙棘林,15°坡面适宜退耕还林。

关 键 词:天然降雨  坡地侵蚀  径流量  侵蚀量
收稿时间:2013-07-11
修稿时间:2013-08-08

Rainfall Characteristics and Their Effects on Slope Erosion in Western Loess Hilly Region
ZHOU Zi-yuan,WANG Li,WANG Xiao-ping,MA Hai-long and LI Meng-ru. Rainfall Characteristics and Their Effects on Slope Erosion in Western Loess Hilly Region[J]. Bulletin of Soil and Water Conservation, 2014, 0(3): 24-27
Authors:ZHOU Zi-yuan  WANG Li  WANG Xiao-ping  MA Hai-long  LI Meng-ru
Affiliation:College of Forestry, Gansu Agricultural University, Lanzhou, Gansu 730070, China;College of Forestry, Gansu Agricultural University, Lanzhou, Gansu 730070, China;Dingxi Institute of Soil and Water Conservation, Dingxi, Gansu 743000, China;Dingxi Institute of Soil and Water Conservation, Dingxi, Gansu 743000, China;College of Forestry, Gansu Agricultural University, Lanzhou, Gansu 730070, China
Abstract:
Rainfall characteristics and their effects on loess slope erosion in the loess hilly region of the western Loess Plateau were studied using the runoff plots located in the Anjiagou watershed, Dingxi City, Gansu Province and the data observed from 2009 to 2011. Results showed that in the condition of natural rainfall, runoff process under different treatments could be divided into runoff producing, maximum runoff, stability of runoff and disappearance of runoff and soil erosion, into erosion producing, maximum erosion amount and curtailment erosion. The eight treatments, in order of the decreasing total amounts of runoff and soil loss, were 15° spring wheat, 10° spring wheat, 10° Pinus tabulaeformis arboreal forest, 15° waste land, 15° Hippophae rhamnoides shrub forest, 10° waste land, 15° Pinus tabulaeformis arboreal forest and 10° Hippophae rhamnoides shrub forest. From the hierarchical clustering, on the 10° slope, Hippophae rhamnoides shrub forest had an obvious effect of soil and water conservation, while on the 15° slope, Pinus tabulaeformis arboreal forest had an obvious effect of soil and water conservation. Therefore, combined with the climate and environment of test site, 10° slope is suitable for planting Hippophae rhamnoides and 15° slope, for returning farmland to forest.
Keywords:natural rainfall  slope erosion  runoff  erosion amount
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