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

黄土高原南部土地利用/覆被变化的土壤侵蚀效应
引用本文:卞鸿雁,庞奖励,任志远,赵艳雷,毛沛妮,郑树伟.黄土高原南部土地利用/覆被变化的土壤侵蚀效应[J].水土保持通报,2013,33(2):11-16.
作者姓名:卞鸿雁  庞奖励  任志远  赵艳雷  毛沛妮  郑树伟
作者单位:陕西师范大学旅游与环境学院,陕西西安,710062
基金项目:国家自然科学重点基金项目"汉江上游(南水北调水源区)万年尺度古洪水水文学研究","汉江上游河谷风成黄土堆积及成壤改造对全新世气候变化的响应规律"
摘    要:基于3S技术对黄土高原南部地区土地利用/覆被变化及空间分布格局进行了综合测评,同时应用通用土壤流失方程(USLE)定量研究了不同土地利用方式下的土壤侵蚀效应.研究表明,研究区1980-2005年共有1 123.80 km2耕地被用为城镇建设用地,建设用地面积净增了1 238.29 km2,林地、草地面积总量变化小,但局部地区流转特征显著;与此同时,该区土壤侵蚀模数从11.54 t/(hm2·a)增至13.81t/(hm2·a),1980和2005年黄土沟壑区侵蚀模数的峰值分别为1 708.52和1 584.69 t/(hm2·a).该区域土壤侵蚀效应与土地利用空间格局耦合性较强,林地、草地由于分布区域海拔高,坡度陡,侵蚀强烈,而地势低洼、平坦地区(建设用地、耕地、未利用地)的土壤侵蚀强度小.林地、草地的土壤侵蚀效应由于受到地形因素的影响,对降雨侵蚀因子增强的响应尤其明显.2005年该区林地和草地的平均侵蚀模数分别增加了2.34和7.32 t/(hm2·a),并且微度以上侵蚀等级的面积有所增加.

关 键 词:土壤侵蚀  土地利用变化  黄土高原南部
收稿时间:4/9/2012 12:00:00 AM
修稿时间:2012/4/27 0:00:00

Effects of Soil Erosion on Land Use and Land Cover Change in Southern Loess Plateau
BIAN Hong-yan,PANG Jiang-li,REN Zhi-yuan,ZHAO Yan-lei,MAO Pei-ni and ZHENG SHu-wei.Effects of Soil Erosion on Land Use and Land Cover Change in Southern Loess Plateau[J].Bulletin of Soil and Water Conservation,2013,33(2):11-16.
Authors:BIAN Hong-yan  PANG Jiang-li  REN Zhi-yuan  ZHAO Yan-lei  MAO Pei-ni and ZHENG SHu-wei
Institution:College of Tourism and Environment Science, Shaanxi Normal University, Xi'an, Shaanxi 710062, China;College of Tourism and Environment Science, Shaanxi Normal University, Xi'an, Shaanxi 710062, China;College of Tourism and Environment Science, Shaanxi Normal University, Xi'an, Shaanxi 710062, China;College of Tourism and Environment Science, Shaanxi Normal University, Xi'an, Shaanxi 710062, China;College of Tourism and Environment Science, Shaanxi Normal University, Xi'an, Shaanxi 710062, China;College of Tourism and Environment Science, Shaanxi Normal University, Xi'an, Shaanxi 710062, China
Abstract:Land use change influences vegetation distribution on the earth surface.Vegetation coverage,tinyterrain,physical properties and chemical properties of soil,as well as erosion resistance,lead to an increasingly complex system for mutual responses to land use/cover changes.The research of soil erosion with regard to different land use types is therefore of great importance.In this study,we implemented the universalsoil loss equation to simulate the soil erosion of Southern Loess Plateau based on different land use type withthe technologies of 3S.The results showed that the cultivated land and construction land changed significantly,and 1 123.80km2 cultivated land has turned to construction land in the past 25years at southern loessplateau;the construction land has increased 1 238.29km2.On the whole,forest and meadow changed little,but they changed significantly in the part of the study area.At he same time,the average soil erosion modulus of southern loess plateau has increased from 11.54t/(hm2·a)to 13.81t/(hm2·a),the peak value ofSouthern Loess Plateau were Gully region of Loess Plateau which were 1 708.52t/(hm2·a),1 584.69t/(hm2·a)in 1980and 2005.the research also shows that the soil erosion is closely related to the spatialdistribution pattern of land cover.In the study area,forest and meadow's were steeper and higher than construction land,cultivated land and unused land,so the latter(construction land,cultivated land and unusedland)'s soil erosion modulus was lower than the former(forest and meadow).The meadow land and forestwere infected by the terrain,which infected the rainfall factors severely.Forest and meadow's average soil erosion modulus were increased 2.34t/(hm2·a)and 7.32t/(hm2·a)respectively.Among all the erosiongrade,above the grade of micro-erosion's area has increased.
Keywords:soil erosion  land use change  Southern Loess Plateau
本文献已被 万方数据 等数据库收录!
点击此处可从《水土保持通报》浏览原始摘要信息
点击此处可从《水土保持通报》下载免费的PDF全文
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