|本期目录/Table of Contents|

[1]于海洋,张振德,张佩民,等.西藏土地荒漠化遥感监测[J].地球科学与环境学报,2007,29(03):316-320.
　YU Hai-yang,ZHANG Zhen-de,ZHANG Pei-min,et al.Monitoring of Land Desertification in Tibet Based on RS[J].Journal of Earth Sciences and Environment,2007,29(03):316-320.
点击复制

西藏土地荒漠化遥感监测(PDF)
分享到：

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第29卷
期数:
2007年第03期
页码:
316-320
栏目:
环境地学
出版日期:
2007-09-15

文章信息/Info

Title:
Monitoring of Land Desertification in Tibet Based on RS
作者:
于海洋1; 张振德2; 张佩民2; 余江宽2
1.中国地质大学地球科学与资源学院,北京100083;2.中国国土资源航空物探遥感中心,北京100083
Author(s):
YU Hai-yang1; ZHANG Zhen-de2; ZHANG Pei-min2; YU Jiang-kuan2
1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; 2. China Center of Aerogeophysical Survey and Remote Sensing for Land and Resources, Beijing 100083, China
关键词:
西藏; 土地荒漠化; 遥感; 地理信息系统
Keywords:
Tibet;  land desertification;  RS;  GIS
分类号:
P941.71
DOI:
-
文献标志码:
A
摘要:
应用RS与GIS技术,利用1976年的MSS数据和2000年TM遥感数据,对西藏境内的荒漠化土地现状 与动态变化进行监测研究,并对其时空演变特征进行了分析。结果表明,西藏荒漠化土地面积2000年为29.08 ×104km2,占总面积的24.28%,其中沙质荒漠化土地面积为24.99×104km2,占20.86%。1976年荒漠化总面 积为27×104km2。由1976～2000年间,荒漠化土地总面积增加了20764.67km2,共增长7.69%,年增长率为 0.32%。同时,土地荒漠化程度明显加重,重度沙质荒漠化土地面积增加了315.87%。
Abstract:
Based on remote sensing and GIS technology, this paper monitored and analyzed the spatial-temporal characteristics of the land desertification in Tibet by using MSS and TM data acquired in 1976 and 2000 respectively. According to the monitoring result, the land area of desertification in Tibet is 2.908× 105 km2, which occupies 24.28% of Tibet whole land. The sandy desertification in Tibet is 2.499× 105 km2, which occupies 20. 86% of Tibet whole land. The area of land desertification in 1976 is 2.7× 105 km2. The analytical result of remote sensing also shows that the gross land area of desertification in Tibet has increased 20 764.67 km2, the increase rate of each year is 0.32%. Obviously, the degree of desertification becomes severer. The area of the severest sandy desertification and desert has increased 315.87%.

参考文献/References:

[1] 中国荒漠 化(土地退化)防治研究课 题组. 中国荒漠 化(土地 退化)防治研究[M] . 北京 :中国环境科学出版社,1998.
[2] 李 虎,高雅琪,王晓峰,等. 新疆土 地荒漠 化监测 分析[J] . 地理学报,2004,59(2):197-202.
[3] 齐雁冰,常庆瑞. 高寒地区 荒漠化动 态监测 技术构 想[J] . 水 土保持通报,2004,24(4):44-46.
[4] 韩 玲,徐惠莲. 利用遥感技术和地理信息系统技术对土地资 源分类的研究[J] . 西安工程学院学报,2000,22(3):56-58.
[5] Yan ga X, Zhangb K,Ji aa B,et al. Deserti ficat ion As sessment in Chin a:Anoverview [J] . J ou rnal of A rid Environment s,2005,5(63):517-531.
[6] 张克斌. 荒漠化评价与监测研究 ———以盐池荒漠 化定位监测 为例[D] . 北京 :北京林业大学,2002.
[7] 曾永年,冯兆东. 沙质荒漠 化遥感监 测与环境 影响研究 进展 [J] . 山地学报,2005,24(2):218-227.
[8] 白爱娟,刘晓东. 从气候标 准的改变 分析西北 地区的气 候变 化[J] . 干旱区研究,2005,22(4):458-464.
[9] 易 秀,李 侠. 西北地 区土壤资源特 征及其开发利 用与保 护[J] . 地球科学与环境学报,2004,26(4):85-89.
[10] 陈梦熊. 西北干旱区水文系统的演变与荒 漠化[J] . 地球科学 与环境学报,2005,27(1):1-4.

相似文献/References:

[1]周羽漩,赵兵,严亮,等.西藏改则地区昂拉仁错中—下二叠统昂杰组—下拉组地层古生物[J].地球科学与环境学报,2014,36(04):107.
　ZHOU Yu-xuan,ZHAO Bing,YAN Liang,et al.Lithostratigraphy and Biostratigraphy of Angjie Formation-Xiala Formation of Middle-Lower Permian in Anglaren Co of Gaize Area, Tibet[J].Journal of Earth Sciences and Environment,2014,36(03):107.
[2]李壮,王立强,张忠,等.西藏邦铺斑岩钼(铜)多金属矿床侵入岩锆石微量元素特征及其地质意义[J].地球科学与环境学报,2015,37(06):59.
　LI Zhuang,WANG Li-qiang,ZHANG Zhong,et al.Zircon Trace Element Characteristics of Intrusions in Bangpu Porphyry Mo(Cu) Polymetallic Deposit of Tibet and Their Geological Significance[J].Journal of Earth Sciences and Environment,2015,37(03):59.
[3]李鹏,张聪,刘晓瑜,等.西藏多巴地区片麻岩变质演化过程及其地质意义[J].地球科学与环境学报,2016,38(05):601.
　LI Peng,ZHANG Cong,LIU Xiao-yu,et al.Metamorphic Evolution Processes and Their Geological Implications of Gneisses from Duoba Area of Tibet[J].Journal of Earth Sciences and Environment,2016,38(03):601.
[4]张继承,姜琦刚,李远华,等.基于RS/GIS的西藏地区湖泊 变化动态监测及气候背景[J].地球科学与环境学报,2008,30(01):87.
　ZHANG Ji-cheng,JIANG Qi-gang,LI Yuan-hua,et al.Dynamic Monitoring and Climatic Background of Lake Changes in Tibet Based on RS/GIS[J].Journal of Earth Sciences and Environment,2008,30(03):87.
[5]杨俊峰,卢书炜,赵虹,等.西藏结则茶卡湖岸沉积物中铀系年龄及意义[J].地球科学与环境学报,2006,28(03):6.
　YANG Jun-feng,LU Shu-w ei,ZHAO Hong,et al.Lacustrine Sediments’ U-seires Age and Its Significance in Jiezechaka Lake of Tibet[J].Journal of Earth Sciences and Environment,2006,28(03):6.

备注/Memo

备注/Memo:
收稿日期:2006-10-20 基金项目:中国地质调查局项目(200315100002) 作者简介:于海洋(1978-),男,山东沂南人,博士研究生,从事RS与GIS地学应用研究。E-mail:yuhyang@sohu.Com
更新日期/Last Update: 1900-01-01