[1]陈国建,张晓萍,张平仓,等.基于RS和GIS的六道沟流域土地利用动态变化研究[J].水土保持研究,2009,16(02):95-100.
　CHEN Guo-jian,ZHANG Xiao-ping,ZHANG Ping-cang,et al.Dynamic Changes of Land Use in Liudaogou Watershed Based on RS and GIS[J].Research of Soil and Water Conservation,2009,16(02):95-100.
点击复制

基于RS和GIS的六道沟流域土地利用动态变化研究

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 16 期数: 2009年02期 页码: 95-100 栏目: 出版日期: 2009-04-20
Title:
Dynamic Changes of Land Use in Liudaogou Watershed Based on RS and GIS
作者:
陈国建1, 张晓萍2, 张平仓3, 李锐2, 杨勤科2
1. 重庆师范大学地理科学学院, 重庆, 400047;
2. 中国科学院水利部水土保持研究所, 陕西, 杨陵, 712100;
3. 长江水利委员会长江科学院, 武汉, 430010
Author(s):
CHEN Guo-jian1, ZHANG Xiao-ping2, ZHANG Ping-cang3, LI Rui2, YANG Qin-ke2
1. School of Geographical Sciences, Chongqing Normal University, Chongqing, 400047, China;
2. Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shanxi, 712100, China;
3. Changjiang River Science Research Institute, Changjiang Water Resources Committee, Wuhan, 430010, China
关键词:
黄土高原; 水蚀风蚀交错带; 土地利用; 退耕还林
Keywords:
the Loess Plateau; the water wind erosion crisscross region; land use; converting farmland into forestry land and grass land
分类号:
F301.24
摘要:
以位于水蚀风蚀交错带的六道沟流域为研究区,应用遥感和GIS相结合的方法,提取不同年份的土地利用信息进行动态分析,并且计算了六道沟的退耕影响系数.结果表明:与1990年相比,2002年水浇地、林地类、草地类面积分别增加了43.45%、28.43%、5.83%,坡旱地减少了60.81%,土地利用结构不断优化.土地利用转换主要以耕地、林地、草地和工矿用地为主,“八五”期间土地利用变化受退耕还林影响的程度大于1995年后的影响.科技试点研究促进了当地的土地利用结构调整,1995年后采煤业的兴起,则进一步促进了土地利用结构的优化.
Abstract:
Taking Liudaogou watershed in water-wind erosion crisscross region as the study site,based on the monochrome aerial photo,the color aerial photo and the local surveying,the paper draws information on land use in different years from them by the integration of RS and GIS to analyze the dynamic changes of land use,and calculates the de-farming influencing coefficient in Liudaogou watershed from 1990 to 2002.The results showed that compared with the identical land use in 1990,the irrigable land increased by 43.45%,forestry land by 28.43% and grass land by 5.83%,while slope dry farmland decreased by 60.81% in 2002.The land use structure has been optimized gradually.During two different period from 1990 to 2002,the land use conversion has mostly happened among farmland,forestry land,grass land and mine land.The change of land use suffer more influence from the project of converting slope farmland into forestry land and grass land in the Eighth Five-year Program than after 1995;the pilot study of the Eighth Five-year Program has optimized the structure of land use,since 1995,coal mining industry has become more active gradually,which has promoted the structure of land use to optimize further.

参考文献/References:

[1] 李秀彬.全球环境变化研究的核心领域:土地利用/土地覆被变化的国际研究动向[J].地理学报,1996,51(6):553-558.
[2] Lambin E F,Baulies X,Bockstael N,et al.Land-use and land-cover change(LUCC) implementation strategy.IGBP Report No.48 and HDP Report No.10[R].sttockholm:IGBP,1999.
[3] 朱会义,李秀彬,何书金.环渤海地区土地利用的时空变化分析[J].地理学报,2001,56(3):253-260.
[4] 赵庚星,李玉环,徐春达.遥感和GIS支持的土地利用动态监测研究:以黄河三角洲垦利县为例[J].应用生态学报,2000,11(4):573-576.
[5] 查书平,丁裕国,于红博,等.基于RS与GIS的长江三角洲土地利用变化分析[J].南京气象学院学报,2003,26(6):815-820.
[6] 张晓萍,李谭宝,杨勤科,等.基于RS和GIS的陕北丘陵沟壑区土地利用格局特征研究[J].水土保持学报,2002,16(1):39-43.
[7] Tan G X,Ryosuke S,Kanichiro M.Development of a GIS-based decision support system for assessing land use status[J].Geo-spatial information science,2004,7(1):72-78.
[8] 张咏梅,包维楷,庞学勇.天保、退耕工程与环境可持续发展的关系[J].长江流域资源与环境,2004,13(3):296-300.
[9] 常庆瑞,刘京,杨勤科,等.基于RS与GIS的黄土丘陵沟壑区土地覆盖动态研究[J].应用生态学报,2003,14(12):2187-2190.
[10] 刘盛和,何书金.土地利用动态变化的空间分析测算模型[J].自然资源学报,2002,17(5):533-540.
[11] 延军平,严艳.陕甘宁边区生态购买设计与操作途径[J].地理学报,2002,57(3):343-353.

相似文献/References:

[1]白桦,穆兴民,王双银.水土保持措施对秃尾河径流的影响[J].水土保持研究,2010,17(01):40.
　BAI Hua,MU Xing-min,WANG Shuang-yin.Impact of Soil and Water Conservation on River Flow of Tuwei River[J].Research of Soil and Water Conservation,2010,17(02):40.
[2]杨国安,徐勇,郭腾云.基于脆弱性和可持续生计视角的黄土高原生态环境治理研究[J].水土保持研究,2010,17(02):64.
　YANG Guo-an,XU Yong,GUO Teng-yun.Eco-environmental Construction on the Loess Plateau Based on the Perspective of the Vulnerability and Sustainable Livelihoods Approaches[J].Research of Soil and Water Conservation,2010,17(02):64.
[3]肖培青,姚文艺,张海峰.黄土高原植被固土减蚀作用研究进展[J].水土保持研究,2012,19(06):282.
　XIAO Pei-qing,YAO Wen-yi,ZHANG Hai-feng.Research Progress of the Role of Vegetation in Soil Conservtion and Soil Erosion Reduction on the Loess Plateau[J].Research of Soil and Water Conservation,2012,19(02):282.
[4]马芹,张晓萍,万龙,等.黄土高原河龙区间最大日雨量(PMP)极值拟合及时空演变特征[J].水土保持研究,2012,19(02):71.
　MA Qin,ZHANG Xiao-ping,WAN Long,et al.Fitting of the PMP Values and Identifying Its Spatiotemporal Characteristics in the Helong Section on the Loess Plateau[J].Research of Soil and Water Conservation,2012,19(02):71.
[5]卓玛兰草,刘普幸,张亚宁,等.甘肃黄土高原区潜在蒸散量时空变化与成因研究[J].水土保持研究,2012,19(01):70.
　ZHUO Malancao,LIU Pu-xing,ZHANG Ya-ning,et al.Study on Temporal and Spatial Changes of the Potential Evapotranspiration and Its Impact Factors in Loess Plateau of Gansu Province[J].Research of Soil and Water Conservation,2012,19(02):70.
[6]施宇,温仲明,龚时慧,等.黄土丘陵区植物功能性状沿气候梯度的变化规律[J].水土保持研究,2012,19(01):107.
　SHI Yu,WEN Zhong-ming,GONG Shi-hui,et al.Trait Variations along a Climatic Gradient in Hilly Area of Loess Plateau[J].Research of Soil and Water Conservation,2012,19(02):107.
[7]穆兴民,陈国良,徐学选.黄土高原降水量与地理因素关系分析[J].水土保持研究,1992,(02):80.
　Mu Xingmin,Chen Guoliang,Xu Xuexuan.ANALYSIS OF THE RELATIONSHIP BETWEEN PRECIPITATION AND GEOGRAPICAL FACTORS IN LOESS PLATEAU[J].Research of Soil and Water Conservation,1992,(02):80.
[8]刘静.数字化地形模型（DTM）在水土保持中的应用[J].水土保持研究,1992,(02):96.
　Liu Jeng.ESTABLSHING AND APPLICATION OF DTM FOR SOIL AND WATER CONSERVATION[J].Research of Soil and Water Conservation,1992,(02):96.
[9]侯庆春.神木试区自然条件及环境整治综合分析[J].水土保持研究,1993,(02):136.
　Hou Qingchun.Comprehensive Analysis on Natural Conditions and Environmental Harnessing in the Experimental Area[J].Research of Soil and Water Conservation,1993,(02):136.
[10]赵安成.陇东黄土高原沟壑区典型小流域治理模式剖析[J].水土保持研究,1994,1(01):45.
　Zhao Ancheng.Analysis of Control Models of Typical Small Watershedin Gully Area of Loess Plateau, the East Part of Gansu Province[J].Research of Soil and Water Conservation,1994,1(02):45.
[11]唐克丽,侯庆春,王斌科,等.黄土高原水蚀风蚀交错带和神木试区的环境背景及整治方向[J].水土保持研究,1993,(02):2.
　Tang Keli,Hou Qingchun,Wang Binke,et al.The Environment Background and Administration Way of Wind-water Erosion Crisscross Region and Shenmu Experimental Area on the Loess Plateau[J].Research of Soil and Water Conservation,1993,(02):2.
[12]唐克丽.黄土高原水蚀风蚀交错带小流域治理模式探讨[J].水土保持研究,1996,3(04):46.
　Tang Keli.Discussion on Comprehensive Control of Small Watershed in Water and Wind Crisscrossed Erosion Region on The Loess Plateau[J].Research of Soil and Water Conservation,1996,3(02):46.

备注/Memo

收稿日期:2008-10-4;改回日期:。
基金项目:中科院知识创新项目“西部生态环境演变规律与水土资源可持续利用研究”(KZCX1-10-04);中科院知识创新重要项目“黄土高原水土保持的区域环境效应研究”(KZCX3-SW-421)
作者简介:陈国建(1975- ),男,汉族,四川达县人,博士,副教授,主要从事区域水土保持研究.E-mail:chengj@cqnu.edu.cn

更新日期/Last Update: 1900-01-01