塔里木河下游植被覆盖变化遥感定量分析

doi:10.11849/zrzyxb.2013.04.013

自然资源学报 ›› 2013, Vol. 28 ›› Issue (4): 668-677.doi: 10.11849/zrzyxb.2013.04.013

塔里木河下游植被覆盖变化遥感定量分析

万红梅^1,2, 李霞¹, 董道瑞¹, 林海军¹

1. 新疆农业大学草业与环境科学学院, 乌鲁木齐 830052;
2. 新疆林业科学研究院, 乌鲁木齐 830000

收稿日期:2012-03-06 修回日期:2012-09-09 出版日期:2013-04-20 发布日期:2013-04-20
作者简介:万红梅(1986-),女,新疆哈密人,硕士研究生,主要从事资源生态遥感相关研究。E-mail:wanhongmei0508@163.com
基金资助:
国家自然科学基金资助项目(40961027)。

Remote Sensing Quantitative Analysis on Vegetation Coverage Change in Lower Reaches of the Tarim River

WAN Hong-mei^1,2, LI Xia¹, DONG Dao-rui¹, LIN Hai-jun¹

1. College of Pratacultural and Environmental Science, Xinjiang Agricultural University, Urumqi 830052;
2. Xinjiang Academy of Forestry Science, Urumqi 830000, China

Received:2012-03-06 Revised:2012-09-09 Online:2013-04-20 Published:2013-04-20

摘要/Abstract

摘要：

在RS与GIS技术支持下,采用空间模型分析法,以2 a为一研究时段,定量分析塔里木河下游输水后植被覆盖变化。结果表明:输水11 a来,Ⅳ级低覆盖植被、Ⅴ级裸地及沙地仍是研究区主要地类。与2000年相比,2010年Ⅰ级极高覆盖植被、Ⅱ级高覆盖植被、Ⅲ级中覆盖植被、Ⅳ级低覆盖植被均呈现逐级增加的趋势,分别增加了986.76、 681.84、 1 091.88、 8 641.89 hm²;Ⅴ级裸地、沙地减少了11 420.37 hm²。整个研究时段,Ⅲ级与Ⅳ级间、Ⅳ级与Ⅴ级间的转化为研究区主要转化类型。随着输水次数和年输水量的稳步增加,研究区植被覆盖类型将向覆盖度、面积稳步增长的平衡态发展,而随着输水量的减少,植被覆盖又转向类型变化频繁的非平衡态。植被覆盖度的增减变化客观反映了输水状况(输水量、输水持续时间),持续、稳定的输水是植被覆盖(覆盖度、面积)稳步增长的前提。

关键词: 植被覆盖, 空间模型法, RS和GIS, 塔里木河下游

Abstract:

Based on the technology of RS and GIS, vegetation coverage changes were analyzed quantitatively every two years with spatial models after water delivery in lower reaches of the Tarim River. The result indicates that low coverage vegetation, bare land and sandy land were the key land categories in the study area. The area of vegetation coverage (Ⅰ-Ⅳ) increased 986.76, 681.84, 1091.88 and 8641.89 hm² in 2010 compared with that in 2000, while the bare land and sandy land (Ⅴ) decreased 11420.37 hm², indicating that the water delivery was effective. The conversion between Ⅲ and Ⅳ as well as between Ⅳ and Ⅴ was the major transformation type of vegetation coverage throughout the study period in the study area. The development of vegetation coverage turned to be an equilibrium state characterized by steady increase with increasing frequency and volume accumulation of water supply, while it turned to be a non-equilibrium state characterized by frequent changes with decrease of water supply. Changes in vegetation cover can reflect the water situation objectively, and the continuous and stable water supply was the premise of steady growth of vegetation coverage.

Key words: vegetation coverage, spatial models analysis, RS and GIS, lower reaches of Tarim River

中图分类号:

Q948

万红梅, 李霞, 董道瑞, 林海军. 塔里木河下游植被覆盖变化遥感定量分析[J]. 自然资源学报, 2013, 28(4): 668-677.

WAN Hong-mei, LI Xia, DONG Dao-rui, LIN Hai-jun. Remote Sensing Quantitative Analysis on Vegetation Coverage Change in Lower Reaches of the Tarim River[J]. JOURNAL OF NATURAL RESOURCES, 2013, 28(4): 668-677.

参考文献

[1] Price J C. Estimating leaf area index from satellite data [J]. IEEE Transactions on Geoscience and Remote Sensing, 1993, 31: 727-734.

[2] Qi J, Marsett R C, Moran M S, et al. Spatial and temporal dynamics of vegetation in the San Pedro River basin area [J]. Agricultural and Forest Meteorology, 2000, 105(1/3): 55-68.

[3] 高志海, 李增元, 魏怀东, 等. 干旱地区植被指数(VI)的适宜性研究[J]. 中国沙漠, 2006, 26(2): 243-248.[GAO Zhi-hai, LI Zeng-yuan, WEI Huai-dong, et al. Study on the suitability of vegetation indices (VI) in arid area. Journal of Desert Research, 2006, 26(2): 243-248.]

[4] Leprieur C, Kerr Y H, Mastorchio S, et al. Monitoring vegetation cover across semi-arid regions: Comparison of remote observations from various scales [J]. International Journal of Remote Sensing, 2000, 21(2): 281-300.

[5] 张旭. EOS-MODIS影像处理及其在塔里木河下游植被变化中的应用[D]. 乌鲁木齐: 新疆大学, 2004.[ZHANG Xu. On the EOS/MODIS Image Processing and Its Application to the Vegetation Variation of the Lower Reaches of the Tarim River. Urumqi: Xinjiang University, 2004.]

[6] 邓铭江. 塔里木河下游生态输水及植被恢复遥感监测评价[J]. 冰川冻土, 2007, 29(3): 380-385.[DENG Ming-jiang. An appraisal of remote-sensing monitoring on vegetation restoration and ecological Water-conveying in the lower reaches of Tarim River. Journal of Glaciology and Geocryology, 2007, 29(3): 380-385.]

[7] 古丽·加帕尔, 陈曦, 包安明. 干旱区荒漠稀疏植被覆盖度提取及尺度扩展效应[J]. 应用生态学报, 2009, 20(12): 2925-2934.[GULI Jiapaer, CHEN Xi, BAO An-ming. Coverage extraction and up-scaling of sparse desert vegetation in arid area. Journal of Applied Ecology, 2009, 20(12): 2925-2934.]

[8] 弋良朋, 尹林克. 基于遥感和GIS的塔里木河下游土地荒漠化的动态变化[J]. 吉林大学学报: 地球科学版, 2005, 35(l): 86-90.[YI Liang-peng, YIN Lin-ke. Study on dynamic change of land desertification in the lower reaches of Tarim River based on RS and GIS. Journal of Jilin University: Earth Science Edition, 2005, 35(l): 86-90.]

[9] 张建生, 闫正龙, 王晓国, 等. 塔里木河下游沙漠化土地时空变化遥感分析[J]. 农业工程学报, 2009, 25(10): 161-165.[ZHANG Jian-sheng, YAN Zheng-long, WANG Xiao-guo, et al. Remote sensing analysis of spatial-temporal changes of desertificationand in lower reaches of Tarim River. Transactions of the CSAE, 2009, 25(10): 161-165.]

[10] 徐水师, 谭克龙, 闫正龙, 等. 塔里木河下游植被覆盖动态变化遥感分析[J]. 西北大学学报: 自然科学版, 2010, 40(2): 323-326.[XU Shui-shi, TAN Ke-long, YAN Zheng-long, et al. Remote sensing analysis on the dynamic change of vegetation coverage in the lower reaches of Tarim River. Journal of Northwest University: Natural Science Edition, 2010, 40 (2): 323- 326.]

[11] 牛婷. 基于中低分辨遥感数据的塔里木河下游植被恢复分析[D]. 乌鲁木齐: 新疆农业大学, 2008.[NIU Ting. Analysis on Vegetation Recovery in the Lower Reaches of Tarim River Based on Low Resolution Remote Sensing Images. Urumqi: Xinjiang Agricultural University, 2008.]

[12] 闫正龙, 黄强, 畅建霞, 等. 塔里木河干流土地利用动态监测遥感分析[J]. 农业工程学报, 2008, 24(3): 119-123.[YAN Zheng-long, HUANG Qiang, CHANG Jian-xia, et al. Analysis and dynamic monitoring of land use in the main stream of Tarim River valley using remote sensing. Transactions of the CSAE, 2008, 24(3): 119-123.]

[13] 罗格平, 周成虎, 陈曦. 干旱区土地利用与覆被变化过程[J]. 地理学报, 2003, 58(1): 63-72.[LUO Ge-ping, ZHOU Cheng-hu, CHEN Xi. Process of land use/land cover change in the oasis in arid region. Acta Geographica Sinica, 2003, 58(1): 63-72.]

[14] 朱磊, 罗格平, 陈曦, 等. 伊犁河中下游近 40 年土地利用与覆被变化[J]. 地理科学进展, 2010, 29(3): 292-300.[ZHU Lei, LUO Ge-ping, CHEN Xi, et al. Detection of land use/land cover change in the middle and lower reaches of the Ili River, 1970-2007. Progress in Geography, 2010, 29(3): 292-300.]

[15] 王建刚, 李霞, 石瑞花, 等. 塔里木河下游胡杨对输水的生态响应[J]. 自然资源学报, 2008, 23(4): 619-625.[WANG Jian-gang, LI Xia, SHI Rui-hua, et al. Ecological responses of Populus Euphratica to water supply in the lower reaches of Tarim River. Journal of Natural Research, 2008, 23(4): 619-625.]

[16] 李苗苗, 吴炳方, 颜长珍, 周为峰. 密云水库上游植被覆盖度的遥感估算[J]. 资源科学, 2004, 26(4): 153-159.[LI Miao-miao, WU Bin-fang, YAN Chang-qing, et al. Estimation of vegetation fraction in the upper basin of Miyun Reservoir by remote sensing. Resources Science, 2004, 26(4): 153-159.]

[17] 李仁强. 基于"3S"技术的干旱区植被覆盖变化信息提取方法研究[D]. 乌鲁木齐: 新疆大学, 2004.[LI Ren-qiang. Research on the Method of Extracting Vegetation Cover Change Based on "3S" Technology in Arid Area. Urumqi: Xinjiang University, 2004.

[18] 梁长秀. 基于RS和GIS北京市土地利用/覆被变化研究[D]. 北京: 北京林业大学, 2009.[LIANG Chang-xiu. Study on LUCC of Beijing Based on RS and GIS. Beijing: Beijing Forestry University, 2009.]

塔里木河下游植被覆盖变化遥感定量分析

Remote Sensing Quantitative Analysis on Vegetation Coverage Change in Lower Reaches of the Tarim River

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