遥感科学与应用技术

塔里木河流域综合治理生态要素变化的遥感分析

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  • 1. 中国煤炭地质总局航测遥感局, 西安 710054;
    2. 长安大学地球科学与资源学院, 西安 710054;
    3. 中国科学院地理科学与资源研究所 资源与环境信息系统国家重点实验室, 北京 100101
谭克龙(1964- ),男,博士,教授级高工,主要从事生态环境及遥感地质等方面的研究。E-mail:Tan-kl@163.com

收稿日期: 2012-10-01

  修回日期: 2013-04-05

  网络出版日期: 2013-08-08

基金资助

国家自然科学基金专项项目“生态导向的陕北能源工矿区主体功能区划及可持续发展模式研究”(41040011);国家发改委[发改投资(2003)1124号、发改投资(2004)1491号]和世界银行贷款[3093-CHA/4341-CHA]项目。

Analysis of Ecological Elements of Comprehensive Harnessing in Tarim River Basin Using Remote Sensing

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  • 1. Aerial Photogrammetry and Remote Sensing Bureau, China National Administration of Coal Geology, Xi'an 710054, China;
    2. College of Earth Science Resources, Chang'an University, Xi'an 710054, China;
    3. State Key Laboratory of Resources and Environmental Information System, Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China

Received date: 2012-10-01

  Revised date: 2013-04-05

  Online published: 2013-08-08

摘要

采用多种类、多时相遥感数据对塔里木河流域综合治理后的耕地变化和干流绿色走廊带的植被、沙质荒漠化和盐碱质荒漠化等主要生态要素进行了动态监测,结果表明:(1)1999-2008年间,流域耕地面积逐步扩大,从167.17万hm2增长到207.51万hm2。其中,塔里木河干流区耕地面积增加最快,叶尔羌河、开都河-孔雀河与和田河三流域稳步增加,而阿克苏河流域耕地面积先增加,后减少。除阿克苏河流域外,塔里木河流域等其他三流域和塔里木河干流,在2004-2008年间的面积增长速度明显大于1999-2002年和2002-2004年两个时段。(2)2002-2004年间,塔里木河干流绿色走廊带生态环境明显改善,主要表现为植被覆盖度的提高、沙质荒漠化土地面积的减小和强度减弱、盐碱质荒漠化土地的强度减弱等。耕地面积的大幅度增加引起的灌溉用水量的增大,对长期采用输水实现塔里木河的生态功能恢复具有长期性制约作用。

本文引用格式

谭克龙, 王晓峰, 高会军, 程维明 . 塔里木河流域综合治理生态要素变化的遥感分析[J]. 地球信息科学学报, 2013 , 15(4) : 604 -610 . DOI: 10.3724/SP.J.1047.2013.00604

Abstract

The Tarim River Basin, especially the downstream area of it is one of the ecologically fragile areasin China. Based on technologies of multi-type, multi-temporal remote sensing imagery, key ecological elements, that is, cultivated land changes in whole Tarim River Basin, the vegetation, sandy and salinized desertification in the green corridor zone of Tarim River mainstream were monitored from 1999 to 2008, after the implementation of comprehensive harnessing engineering for the whole Tarim River Basin. The investigation results show that the ecological environment in the green corridor zone of Tarim mainstream was conspicuously improved, mainly appearing as the rise of vegetation cover rate, the reduction of sandy desertification land area and the weakening of intensity of sandy and salinized land. On the other hand, the cultivated area in the Tarim River Basin significantly increased from 1999 to 2008, which reached 40.34×104 hm2, for 24.13%. Among the whole basin, the cultivated area of the mainstream area increased most quickly. The growth rate of cultivated area of whole basin from 2004 to 2008 is significantly higher than those of the two periods from 1999 to 2002 and from 2002 to 2004. Moreover, the characteristics of sandy and salinized land in upstream of the main channel showed an increase in area of 2.69×104 hm2 and a reduction in increase rate from 2002 to 2004. And sandy desertification land area decreased 1.20×104 hm2 in the same period in lower reach of the basin. Vegetation cover rate of the whole basin apparently increased, especially the surrounding area of the Taitema Lake.Although the ecological environment presented an somewhat improvement after the implementation of comprehensive harnessing in the whole basin, the ecologically fragile environment need long-term supply of water resource and continuous concern from the whole society. The increase of irrigation water resulting from the substantial increase of cultivated area could undertake a long-term potential restraining effect on the harnessing of ecological functions of the Tarim River.

参考文献

[1] 刘新华,徐海量,凌红波,等.塔里木河干流河道生态需水量研究[J].干旱区研究,2012,29(6):984-991.

[2] 牛新泉,李于洁.从外流域调水以解决塔里木盆地生态环境危机[J].河南水利与南水北调,2010(9):47-49.

[3] 张天曾.中国干旱区水资源利用与生态环境[J].自然资源,1981(1):62-67.

[4] 马金珠,高前兆.西北干旱区内陆河流域水资源系统与生态环境问题[J].干旱区资源与环境,1997,11(4):15-21.

[5] 汤奇成,张捷斌.西北干旱地区水资源与生态环境保护[J].地理科学进展,2001,20(3):227-233.

[6] 朱震达.塔克拉玛干沙漠地区沙漠化过程及其发展趋势[J].中国沙漠,1987,7(3):16-28.

[7] 王涛.塔里木河下游阿拉干地区沙漠化过程及其预测[J].中国沙漠,1986,6(2):16-26.

[8] 樊自立.塔里木河流域资源环境及可持续发展[M].北京:科学出版社,1998.

[9] 李新,周宏飞,樊自立.塔里木河水资源利用与土地荒漠化效应分析[J].中国沙漠,1998,18(Z1):46-54.

[10] 宋郁东,樊自立,雷志栋,等.中国塔里木河水资源与生态环境问题[M].乌鲁木齐:新疆人民出版社,2000.

[11] 艾尔肯·艾白不拉,刘桂林,艾里西尔·库尔班,等.基于CBERS/CCD遥感影像的塔里木河下游生态输水监测[J].长江流域资源与环境,2012,21(Z2):157-162.

[12] 刘加珍,陈亚宁.新疆塔里木河下游植物群落逆向演替分析[J].干旱区地理,2002,25(3):231-236.

[13] 陈亚宁,李卫红,徐海量,等.塔里木河下游地下水位对植被的影响[J].地理学报,2003,58(4):542-549.

[14] 杨戈,郭文平.塔里木河下游末端实施生态输水后植被变化与展望[J].中国沙漠,2004,24(2):167-173.

[15] 徐海量,陈亚宁,雷加强.塔里木河生态输水对沙化逆转影响[J].中国沙漠,2004,24(2):173-177.

[16] 李霞,侯平,朱小虎,等.塔里木河下游应急输水植被响应效果调查与分析[J].干旱区资源与环境,2004,18(3):68-73.

[17] 李卫红,陈亚鹏,张宏峰,等.塔里木河下游断流河道应急输水与地表植被响应[J].中国沙漠,2004,24(3):301-305.

[18] 阮晓,王强,陈亚宁,等.塔里木河流域荒漠河岸植物对应急输水的生理响应[J]生态学报,2005,25(8):1966-1973.

[19] 高前兆,屈建军,王润,等.塔里木河下游绿色走廊生态输水对沙漠化逆转的影响[J].中国沙漠,2007,27(1):52-58.

[20] 陈亚宁,张小雷,祝向民,等.新疆塔里木河下游断流河道输水的生态效应分析[J].中国科学D辑,2004,34(5):475-482.

[21] 谭克龙,高会君,卢中正,等.中国半干旱生态脆弱带遥感理论与实践[M].北京:科学出版社,2007.

[22] 程维明,柴慧霞,方月,等.基于水资源分区和地貌特征的新疆耕地资源变化分析[J].自然资源学报,2012,27(11): 1809-1822.

[23] 孙美琴,赵成义,施枫芝,等.近20a塔里木河干流区土地利用变化特征[J].干旱区研究,2013,30(1):16-21.

[24] 赵锐锋,姜朋辉,陈亚宁,等.塔里木河干流区土地利用/覆被变化及其生态环境效益[J].地理科学,2012,32(2):244-250.

[25] 刘英.浅谈阿克苏河流域水资源利用现状与节水途径[J].硅谷,2001(5):131-131.

[26] 阿依先木·司马义,吐尔逊·哈斯木,祖木拉提·伊布拉音,等.人类活动对土地沙漠化的影响研究——以塔里木河下游为例[J].水土保持研究,2011,18(1):56-60.

[27] 刘桂林,艾里西尔·库尔班,艾尔肯·艾白不拉,等.塔里木河下游生态输水后植被景观格局动态变化研究[J].冰川冻土,2012,34(1):161-168.

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