毛乌素沙地中部地表水体1999-2015时空动态变化特征及驱动分析

干旱区地理 ›› 2017, Vol. 40 ›› Issue (3): 633-639.

毛乌素沙地中部地表水体1999-2015时空动态变化特征及驱动分析

张佩云¹, 王凯², 王戈飞¹, 梁枥文¹, 张世强¹

1 西北大学城市与环境学院, 陕西西安 710127;
2 西北师范大学地理与环境科学学院, 甘肃兰州 730070

收稿日期:2016-10-24 修回日期:2017-02-13 出版日期:2017-05-25
通讯作者: 张世强,教授,研究方向为流域系统中各要素及水循环的观测、遥感反演与模拟等.Email:zhangsq@lzb.ac.cn
作者简介:张佩云(1993-),女,硕士研究生,研究方向为遥感与地理信息科学.Email:13152035260@163.com
基金资助:
水利部公益性行业科研专项”云南高原湖泊水资源地面－遥感监测技术研究”（201401026）

Spatial-temporal changes and factor analysis of surface water in the middle Mu Us Sandy Land areas from 1999 to 2015

ZHANG Pei-yun¹, WANG Kai², WANG Ge-fei¹, LIANG Li-wen¹, ZHANG Shi-qiang¹

1 Northwest University, Xi'An 710127, Shaanxi, China;
2 Northwest Normal University, Lanzhou 730070, Gansu, China

Received:2016-10-24 Revised:2017-02-13 Online:2017-05-25

摘要/Abstract

摘要： 地表水体对于毛乌素沙地的经济发展和生态保护具有重要作用。利用1999、2006、2013、2015 年Landsat TM/ETM+遥感影像，获取了毛乌素沙地中部近16 a 来地表水体面积的时空变化特征。结果表明：水体面积以2006年为界呈先萎缩后回升的变化特征，1999-2006年地表水体总面积从368.52 km²缩减到了242.81 km²，缩减了129.53 km²（34.1%）。2013 年和2015 年水体面积回升，但2015年仍比1999年减少18.6%。研究区地表水体的变化在北部主要受煤炭开采大幅增加（2 252.2%）的影响，而南部主要受灌溉面积增加（92.4%）和畜牧量大幅增加（24 614.7%）的影响。以伊旗查干淖尔为代表的天然水体尽管受采矿用水增加等的影响，但在严格的水资源保护制度下面积变化不大，而以伊和日淖尔为代表的天然水体面积缩减显著，表明地表水体需要积极调控和适应才能维持稳定。

关键词: 毛乌素沙地, 地表水体变化, 遥感, 人类活动, 调控

Abstract: The surface water is very important to local economic development and ecological protection in Mu Us Sandy Land among Inner Mongolia,Ningxia and Shaanxi Province,China. The spatial-temporal changes of surface water in the middle areas of Mu Us Sandy Land were analyzed by using Landsat TM/ETM+ images of 1999,2006,2013,2015. The surface water shrunk about 125.71 km²(35.2%)from 1999(368.51 km²)to 2006 (242.81 km²),and then recovered in 2013(299.59 km²)and 2015(299.82 km²). The area of water body in 2015 was still about 18.64% less than that in 1999,the long-term change trends of annual precipitation and yearly average air temperature are not significant(at ɑ =0.05). The water consumption with effective irrigation area,livestock, raw coal production from 1999 to 2014 suggest that water body decrease mainly caused by increased coal mining(2 252.2%)in north part while by increased agricultural irrigation(92.4%)and grazing(24 614.7%)in South part. We found that Chagan Lake is nearly stable with small fluctuation under the increased coal mining and the strictest water protect policy,while the area of natural water body of Yiheri Lake has continued to decline by 1 km²(29.9%)over the past 16 years. These results indicate that the water protection measures are very important to maintain the stability of the lakes.

Key words: Mu Us Sandy Land, surface water changes, remote sensing, human activity, regulate and control

中图分类号:

TP79

张佩云, 王凯, 王戈飞, 梁枥文, 张世强. 毛乌素沙地中部地表水体1999-2015时空动态变化特征及驱动分析[J]. 干旱区地理, 2017, 40(3): 633-639.

ZHANG Pei-yun, WANG Kai, WANG Ge-fei, LIANG Li-wen, ZHANG Shi-qiang. Spatial-temporal changes and factor analysis of surface water in the middle Mu Us Sandy Land areas from 1999 to 2015[J]. , 2017, 40(3): 633-639.

参考文献

[1] 闫峰,吴波. 近40 a 毛乌素沙地荒漠化过程研究[J]. 干旱区地理,2013,36(6):987-996.[YAN Feng,WU Bo. Desertification progress in Mu Us Sandy Land over the past 40 years[J]. Arid Land Geography,2013,36(6):987-996.]

[2] 徐小玲,延军平. 毛乌素沙地的脆弱性与可持续发展研究[J]. 干旱区研究,2004,21(3):286-289.[XU Xiaoling,YAN Junping. Study on the vulnerability and the sustainable development in the Mu Us Sandy land[J]. Arid Zone Research,2004,21(3): 286-289.]

[3] 岳耀杰,王静爱,邹学勇,等. 中国北方沙区湖泊(水库)风沙灾害危险度评价与安全对策——以内蒙古沙区为例[J]. 干旱区研究,2008,25(4):574-582.[YUE Yaojie,WANG Jingai. ZOU Yueyong,et al. Assessment on the risk of aeolian sand disasters around the lake sand reservoirs in sandy Lands in North China and some security measures:a case study in a sandy land in Inner Mongolia[J]. Arid Zone Research,2008,25(4):574-582.]

[4] 中国工程院”西北水资源”项目组. 西北地区水资源配置生态环境建设和可持续发展战略研究[J]. 中国工程科学,2003,5 (4):1-26.[Water-resources-in-northwest-region Task Group of Chinese Academy of Engineering. Strategic study on allocation of water resources,conservation and upgrading of eco-environment and sustainable development in north-west China[J]. Engineering Sciences,2003,5(4):1-26.]

[5] 王兮之. 防沙治沙专家建议调研沙区水资源[N]. 中国绿色时报,2015-08-25(A01).[WANG Xizhi. Experts suggest of water resources research in the prevention and control of desertification[N]. Greentimes,2015-08-25(A01).]

[6] 牛沂芳,李才兴,习晓环,等. 卫星遥感检测高原湖泊水面变化及与气候变化分析[J]. 干旱区地理,2008,31(2):284-290.[NIU Yifang,LI Caixing,XI Xiaohuan,et al. Plateau lake variation monitored by satellite remote sensing and the relation to climate change[J]. Arid Land Geography,2008,31(2):284-290.]

[7] 付颖,徐新良,通拉嘎,等. 近百年来北京市地表水体时空变化特征及驱动力分析[J]. 资源科学,2014,36(1):75-83.[FU Ying,XU Xingliang,TONG Laga,et al. Spatial-temporal variation and driving forces of surface water in Beijing over one hundred years[J]. Resources Science,2014,36(1):75-83.]

[8] 张学雷,段金龙. 河南省地表水时空分布特征研究[J]. 河南农业科学,2013,42(11):64-67.[ZHANG Xeulei,DUAN Jinlong. Characteristics of surface water tempor land spatial distribution in Henan Province[J]. Journal of Henan Agricultural Sciences, 2013,42(11):64-67.]

[9] 郭坚,王涛,韩邦帅,等. 近30 a 来毛乌素沙地及其周边地区沙漠化动态变化过程研究[J]. 中国沙漠,2008,28(6):1017- 1021.[GUO Jian,WANG Tao,HAN Bangshuai,et al. Dynamic process of aeolian desertification land variation in Mu Us Sandy Land and its surrounding area in recent 30 years[J]. Journal of Desert Reaearch,2008,28(6):1017-1021.]

[10] 孙芳蒂,赵圆圆,宫鹏,等. 动态地表覆盖类型遥感监测:中国主要湖泊面积2000-2010 年间逐旬时间尺度消长[J]. 科学通报,2014,59(2):397-411.[SUN Fangdi,ZHAO Yuanyuan, GONG Peng,et al. Monitoring dynamic changes of global land cover types:fluctuations of major lakes in China every 8 days during 2000-2010[J]. Chinese Science Bulletin,2014,59(2): 171-189.]

[11] 连连,陈建飞. 基于遥感技术的珠江三角洲地区水域面积时空变化分析[C]//智能信息技术应用协会. 环境科学与信息应用技术(ESIAT2011 部分3-1). 2011 年第三届国际会议论文集. 智能信息技术应用协会,2011:6．[LIAN Lian,CHEN Jianfei. Spatial-temporal change analysis of water area in Pearl River Delta based on remote sensing technology[C]// Intelligent Information Technology Application Association. Proceedings of the 2011 3rd International Conference on Environmental Science and Information Application Technology(ESIAT 2011 Part 3-1). Intelligent Information Technology Application Association, 2011:6.]

[12] 尹立河,王晓勇,黄金廷,等. 大克泊湖床垂向渗透系数试验研究[J]. 盐湖研究,2011,19(1):1-8.[YING Lihe,WANG Xiaoyong, HUANG Jingting,et al. Estimation of lakebed vertical hydraulic conductivity through insitu experiments for Habor Lake[J]. Journal of Salt Lake Research,2011,19(1):1-8.]

[13] 车向红. 2000-2014 年青藏高原湖泊动态遥感监测与分析[D]. 太原:太原理工大学,2015.[CHE Xianghong. Monitoring and analyzing of lake dynamics in Qinghai-Tibet Plateau using remote sensing from 2000 to 2014[D]. Taiyuan:Taiyuan University of Technology,2015.]

[14] 朱刚,高会军,曾光. 近35 a来新疆干旱区湖泊变化及原因分析[J]. 干旱区地理,2015,38(1):103-110.[ZHU Gang,GAO Huijun, ZENG Guang. Lake change research and reasons analysis in Xinjiang arid regions during the past 35 years[J]. Arid Land Geography,2015,38(1):103-110.]

[15] 陶胜利,方精云. 有关蒙古高原湖泊快速萎缩的研究[J]. 美国科学院论文集,2015,112(7):2281-2286.[TAO Shengli,FANG Jingyun,ZHAO Xia,et al. Rapid loss of lakes on the Mongolian Plateau Rapid loss of lakes on the Mongolian Plateau[J]. Proceedings of The National Academy of Sciences,2015,112(7): 2281-2286.]

[16] 邓铭江. 新疆十大水生态环境保护目标及其对策探析[J]. 干旱区地理,2014,37(5):865-874.[DENG Mingjiang. Top ten ecological environment protection targets and its solutions in Xinjiang,China[J]. Arid Land Geography,2014,37(5):865- 874.]