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黄土丘陵沟壑区典型流域径流输沙对土地利用/覆被变化的响应
引用本文:张晓明,曹文洪,余新晓,张满良,王向东,朱毕生.黄土丘陵沟壑区典型流域径流输沙对土地利用/覆被变化的响应[J].应用生态学报,2009,20(1):121-127.
作者姓名:张晓明  曹文洪  余新晓  张满良  王向东  朱毕生
作者单位:1. 中国水利水电科学研究院,北京,100044
2. 北京林业大学水土保持与荒漠化防治重点实验室,北京,100083
3. 水利部黄河水利委员会天水水土保持试验站,甘肃天水,741000
基金项目:国家科技支撑计划,中国水利水电科学研究院科研专项资助项目 
摘    要:基于动力水文过程测定技术和景观生态学测度方法,对位于黄土丘陵沟壑区第三副区的甘肃天水罗玉沟流域1986—2004年土地利用/覆被变化对流域径流输沙的影响进行了研究.结果表明:研究期间,罗玉沟流域土地利用/覆被变化对年径流输沙有显著影响,1995—2004年的输沙量比1986—1994年减少约63.0%,且随着年降水量的增多,其减沙效应明显;土地利用/覆被变化对流域径流输沙的影响具有季节性特征,相对于1986—1994年而言,研究区1995—2004年的减沙效应主要集中在5—10月,且月降水越多,后期的月均输沙量较前期减少得越多.降雨和洪峰流量频率分析表明,若具有相同频率分布的雨强,则任一重现期下罗玉沟流域1995—2004年的洪水平均含沙量小于1986—1994年.

关 键 词:土地利用/覆被变化  输沙  频率分布  黄土丘陵沟壑区
收稿时间:2008-6-16

Effects of land use/cover change on runoff sediment discharge in typical watershed in Loess gullied-hilly region of China.
ZHANG Xiao-ming,CAO Wen-hong,YU Xin-xiao,ZHANG Man-liang,WANG Xiang-dong,ZHU Bi-sheng.Effects of land use/cover change on runoff sediment discharge in typical watershed in Loess gullied-hilly region of China.[J].Chinese Journal of Applied Ecology,2009,20(1):121-127.
Authors:ZHANG Xiao-ming  CAO Wen-hong  YU Xin-xiao  ZHANG Man-liang  WANG Xiang-dong  ZHU Bi-sheng
Institution:China Institute of Water Resources and Hydropower Research, Beijing 100044, China; Ministry of Education Key Laboratory of Soil & Water Conservation and Desertification Combating, Beijing Forestry University, Beijing 100083, China;Tianshui Soil and Water Conservation Experiment Station, the Yellow River Water Conservancy Committee, Ministry of Water Resources, Tianshui 741000, Gansu, China
Abstract:By using the measurement technique of dynamic hydrological process and the estim ation method of landscape ecology, this paper studied the effects of 1986〖KG-*2 〗-〖KG-*7〗2004 land use/cover change (LUCC) on the runoff sediment discharge i n the Luoyugou watershed in Tianshui of Gansu Province in third sub-region of L oess Plateau. The results showed that the LUCC in Luoyugou watershed had signifi cant effects on the annual sediment yield. In 1995〖KG-*2〗-〖KG-*7〗2004, the s ediment discharge was reduced by approximately 630%, compared with that in 198 6〖KG-*2〗-〖KG-*7〗1994, and the reduction effect was more significant with inc reasing annual precipitation. The effects of LUCC on sediment discharge demonstr ated seasonal fluctuation characteristic. Relative to that in 1986〖KG-*2〗-〖KG -*7〗1994, the reduction effect of sediment discharge in 1995〖KG-*2〗-〖KG-*7〗 2004 was more concentrated in the period from May to October, and, the more the monthly precipitation, the more the reduction of monthly average sediment discha rge in 1995〖KG-*2〗-〖KG-*7〗2004 than in 1986〖KG-*2〗-〖KG-*7〗1994. The anal ysis on precipitation and flood peak discharge frequency indicated that under th e same frequency distribution of precipitation intensity, the average sediment c oncentration in any recurrence period in Luoyugou watershed was smaller in 1995 〖KG-*2〗-〖KG-*7〗2004 than in 1986〖KG-*2〗-〖KG-*7〗1994.
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