首页 | 本学科首页   官方微博 | 高级检索  
     检索      

三峡库区土壤侵蚀空间分布特征
引用本文:吴昌广,吕华丽,周志翔,肖文发,王鹏程,汪涛.三峡库区土壤侵蚀空间分布特征[J].中国水土保持科学,2012,10(3):15-21.
作者姓名:吴昌广  吕华丽  周志翔  肖文发  王鹏程  汪涛
作者单位:1. 华中农业大学园艺林学学院,430070,武汉;中国林业科学研究院亚热带林业研究所,311400,浙江富阳
2. 华中农业大学园艺林学学院,430070,武汉
3. 中国林业科学研究院森林生态环境与保护研究所,100091,北京
4. 华中农业大学园艺林学学院,430070,武汉;中国林业科学研究院森林生态环境与保护研究所,100091,北京
基金项目:国家“十二五”科技支撑项目“长江流域防护林体系整体优化及调控技术研究”(2011BAD38B04);林业公益性行业科研专项经费项目“生态经济型石漠化植被恢复模式构建技术研究”(201004033);农业科技成果转化资金项目“石漠化植被恢复技术应用示范”(2009GB24320475);中国林科院中央级公益性科研院所基本科研业务费专项资金“石漠化土地地表水土流失规律研究”(CAFYBB2007033)
摘    要:结合三峡库区的区位特征和数据获取条件,对RUSLE模型的因子算法进行相应修正,最后基于GIS评估库区土壤侵蚀风险及其空间分布特征。结果表明:1)库区年均土壤侵蚀量为1亿8 359.43万t/a,平均土壤侵蚀模数为31.85 t/(hm2.a),水土流失面积占库区土地总面积的66.97%;2)库区土壤侵蚀强度与高程梯度间无直接线性关系,中度以上侵蚀主要分布在500~1 500 m高程带上,其中极强烈、剧烈侵蚀在500~1 000 m间出现频率最高,这应该与该区域强烈的人类活动有关;3)库区土壤侵蚀强度与坡度呈显著正相关,中度以上侵蚀在15°以上坡度带的发生频率急剧增加,其53.74%的面积比例贡献了89.06%土壤侵蚀量;4)库区土壤侵蚀强度在不同坡向上表现为半阴坡>正阴坡>半阳坡>正阳坡,阴坡的侵蚀量稍大于阳坡,占库区总侵蚀量的56.63%。说明500~1 500 m高程带、>15°坡度带以及阴坡是库区发生土壤侵蚀的主要区域,也是水土流失防治及治理的重点区域。

关 键 词:RUSLE  土壤侵蚀  空间分布特征  三峡库区

Spatial distribution analysis of soil erosion in the Three Gorges Reservoir Area
Wu Changguang , Lü Huali , Zhou Zhixiang , Xiao Wenfa , Wang Pengcheng , Wang Tao.Spatial distribution analysis of soil erosion in the Three Gorges Reservoir Area[J].Science of Soil and Water Conservation,2012,10(3):15-21.
Authors:Wu Changguang  Lü Huali  Zhou Zhixiang  Xiao Wenfa  Wang Pengcheng  Wang Tao
Institution:1(1.College of Horticulture and Forestry,Huazhong Agricultural University,430070,Wuhan;2.Research Institute of Subtropical Forestry,Chinese Academy of Forestry Sciences,311400,Fuyang,Zhejiang;3.Research Institute of Forest Ecology Environment and Protection,Chinese Academy of Forestry Sciences,100091,Beijing: China)
Abstract:In this paper,RUSLE factors algorithms were improved based on environmental characteristics and data availability in the Three Gorges Reservoir Area.Based on GIS technology the improved algorithms were used to evaluate the risk and spatial distribution of soil erosion.The results showed that the annual soil erosion amount and the mean soil erosion modulus in the Three Gorges Reservoir Area were 18 359.43×104 t/a and 31.85 t/(hm2·a),respectively.The area suffering soil erosion accounted for 66.97% of the reservoir area.There was no direct linear relationship between soil erosion intensity and the altitudinal gradient in Three Gorges Reservoir Area.The area with from moderate to severe erosion intensity mainly distributed in 500-1 500 m elevation zone,which may resulted from the impact of intensive human activities in last decades.The soil erosion intensity was significantly positively correlated with slop gradient.When slope gradient was larger than 15 degree,the frequency of more than moderate erosion increased significantly,The slope area of larger than 15 degree accounted for 53.74% of the reservoir area,but contributed 89.06% of the total soil loss.Soil erosion intensity varied with slope aspects in a trend of semi-shady slopes〉shady slopes〉semi-sunny slopes〉sunny slopes.The amount of soil erosion on shady slopes was slightly higher than that on sunny slopes,accounted for 56.50% of total erosion amount.The results indicated that soil erosion mainly occurred in 500 to 1 500 m elevation zone,slope gradient larger than 15 degree,and shady slopes,which are also the key regions of soil and water loss prevention in Three Gorges Reservoir Area.
Keywords:RUSLE  Soil erosion  Spatial distribution characteristics  Three Gorges Reservoir Area
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号