Oasis land use change and its hydrological response to Tarim River Basin
Received date: 2010-07-29
Revised date: 2010-09-28
Online published: 2010-12-20
In recent years, the study on hydrological effect of land use change has become a focus. In the Tarim River Basin, land use change has exerted great effect on hydrological process of a river, so it is necessary to study the hydrological effect of land use change in the river basin. As cultivated land dominates the land use type in the Tarim River Basin, based on the statistical data of cultivated land of each prefecture and tested data of each main water station in Tarim River Basin, this paper analyzes the total variation trend, variation speed, regional difference and hydrological effect on water quantity of the river. The results are shown as follows. (1) The cultivated land area in the Tarim River Basin shows a fluctuating increasing trend with an annual rate of 2.37%, but per capita cultivated land area saw a gradual decrease with an annual rate of 0.44%. There is a significant spatial disparity in the cultivated land changes. The change of cultivated land area in Bayingolin Mongol Autonomous Prefecture where the reserved land and water resources are plentiful is large, and that in Hotan Prefecture located at the northern foot of Kunlun Mountains is small. (2) As a result of the expansion of cultivated land area in the Tarim River Basin, the hydrological effect such as river process, river discharge, flood, water quality and silt are more remarkable than before, and the spatial effect on river discharge is striking. As a result of cultivated land expansion, cultivated land and consuming water rise by 34.80% and 21.78% from 1957 to 2006, respectively. At the same time, water pollution and the decreasing of the water quality have become the confinement of social development in the Tarim River Basin. At present, the project of water saving has taken effect, and the trend of the venting water quantity from streams to the Tarim River has been under control. In order to keep the sustainable development in this region, it is urgent to harness the Tarim River in a long term, set up coherent management system of water resources, and use water resources reasonably.
MANSUR Sabit, NURKAMIL Yusuf . Oasis land use change and its hydrological response to Tarim River Basin[J]. GEOGRAPHICAL RESEARCH, 2010 , 29(12) : 2251 -2260 . DOI: 10.11821/yj2010120014
[1] TurnerⅡB L,David Skole,Steven Sanderson.Land use and Iand conver change:Science/research planning.IGBP Report No.35,Stockholm,1995.125~137.
[2] NASA.Modeling land-use and land-cover changes in Europe and Northem Asia.NASA ,1999 Research Plan.USA:Houston,1998.56~68.
[3] Reid R S,Kurska R L,et al.Land-use and land-cover dynamics in response to changes in climatic,biological and socio-political forces:The case of southwestern Ethiopia.Landscape Ecology,2000,15:339~355.
[4] 高前兆,王润,Ernst Giese.气候变化对塔里木河来自天山的地表径流影响.冰川冻土,2008,30(1):1~11.
[5] 李昌峰,高俊峰,曹慧.土地利用变化对水资源影响研究的现状和趋势.土壤,2002,(4):191~205.
[6] 陈军锋,张明.梭磨河流域气候波动和土地覆被变化对径流影响的模拟.地理研究,2003,22 (1):73~78.
[7] 姜德娟,李丽娟,侯西勇,等.洮儿河流域中上游水循环要素变化及其原因.地理研究,2009,28(1):55~64.
[8] 李丽娟,姜德娟,李九一,等.土地利用/ 覆被变化的水文效应研究进展.自然资源学报,2007,22(2):211~224.
[9] 邓慧平.气候与土地利用变化对水文水资源的影响研究.地球科学进展,2001,16(3):436~441.
[10] 李丽娟,姜德娟,杨俊伟,等.陕西大理河流域土地利用/覆被变化的水文效应.地理研究,2010,29(7):1233~1244.
[11] 贡璐,王宏卫,鲍平勇,等.塔里木河上游典型绿洲景观变化及其生态效应分析.中国沙漠,2006,26(3):421~425.
[12] 郝兴明,陈亚宁,李卫红.塔里木河流域近50年来生态环境变化的驱动力分析.地理学报,2006,61(3):262~272.
[13] 张一驰,李宝林,程维明,等.开都河流域径流对气候变化的响应研究.资源科学,2004,26(6):69~76.
[14] 新疆维吾尔自治区统计局.新疆50年(1955~2005),北京:中国统计出版社,2005.255~256.
[15] 中共新疆维吾尔自治区委员会办公厅和新疆维吾尔自治区人民政府办公厅. 新疆辉煌50年(1949~1999)下卷. 乌鲁木齐:新疆人民出版社,1999. 172~191.
[16] 新疆维吾尔自治区统计局. 新疆统计年鉴. 北京:中国统计出版社,2006~2009.
[17] 李忠锋,王一谋,冯毓荪,等.基于RS与GIS的榆林地区土地利用变化分析.水土保持学报,2003,17(2):97~99.
[18] 陈曦主编.中国干旱区土地利用与土地覆被变化.北京:科学出版社,2008.169~180.
[19] 毛德华主编.塔里木河流域水资源、环境与管理.北京:中国环境科学出版社,1998.41~97.
[20] 海米提·依米提,潘晓玲,塔西甫拉提·特依拜,等.塔里木盆地水土资源开发及其生态环境效应.资源科学,2002,24(6):48~55.
[21] 新疆维吾尔自治区水利厅和新疆水利学会.新疆河流水文水资源.乌鲁木齐:新疆科技卫生出版社,1999.370~441.
[22] 樊自立,马英杰,季方,等.塔里木河生态环境演变及整治途径.干旱区资源与环境,2001,15(1):11~17.
[23] 徐海量,陈亚宁,雷加强.塔里木河下游生态输水堆沙漠化逆转的影响.中国沙漠,2004,24(2):173~176.
/
| 〈 |
|
〉 |