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基于RUSLE的贵州省红枫湖流域土壤侵蚀时空变化特征

曾凌云 汪美华 李春梅

水文地质工程地质2011,Vol.38Issue(2):113-118,6.
水文地质工程地质2011,Vol.38Issue(2):113-118,6.

基于RUSLE的贵州省红枫湖流域土壤侵蚀时空变化特征

Study on soil erosion and its spatio-temporal change at Hongfeng Lake watershed based on RUSLE Model

曾凌云 1汪美华 2李春梅3

作者信息

  • 1. 中国国土资源经济研究院,廊坊,065201
  • 2. 中国地质环境监测院,北京,100081
  • 3. 北京大学城市与环境学院,北京,100871
  • 折叠

摘要

Abstract

Based on the data of RS、rainfall、DEM and soil, a study of soil erosion of the Catchment of Lake Hongfenghu located in karst ecological fragile area in Guizhou Province during the past 40 years ( 1960 ~ 2004) is taken by using GIS and RUSLE Model. The main contents of the research include: computing the annual amount of soil erosion, assessing the soil erosion intensity in the catchment of Lake Hongfeng during the periods of 1960 ~ 1986、1987 ~ 1997 and 1998 ~ 2004, and discussing the relation between soil erosion and spatio - temporal changes of land use in the past 40 years. Soil erosion in the drainage basin has experienced a process of getting more intense and then weakening. Soil erosion in the west of drainage basin is more serious than in the east. In the three periods, the special change of soil erosion intensity in the west has the character of getting more intense and then getting slight, but the relevant change is slight in the east of the drainage basin.

关键词

RUSLE/喀斯特地区/土壤侵蚀/时空格局/红枫湖流域

分类

农业科技

引用本文复制引用

曾凌云,汪美华,李春梅..基于RUSLE的贵州省红枫湖流域土壤侵蚀时空变化特征[J].水文地质工程地质,2011,38(2):113-118,6.

基金项目

国家自然科学基金重点项目(40335036) (40335036)

水文地质工程地质

OA北大核心CSCDCSTPCD

1000-3665

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