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近20年科尔沁沙地植被覆盖变化研究
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摘要
沙漠化是荒漠化的主要类型,它作为极其重要的环境和社会经济问题正困扰着当今世界,威胁着人类的生存和发展。植被盖度是影响土地荒漠化的重要因子,是植物群落覆盖地表程度的一个综合量化指标,易于观测,并与土壤的水土流失、土地沙漠化关系密切。科尔沁沙地地处我国北方农牧交错带东段,属季风气候边缘区,具有典型的环境敏感性和脆弱性,很长时间以来,也是我国发生发展的典型区。但自20世纪末沙地出现了土地沙漠化的整体逆转,成为了我国从沙地中的环境改善之例。鉴于此,本文以沙地的典型区科尔沁左翼后旗为例,在对当前植被盖度测算方法的分析与研究的前提上,基于土地覆盖分类运用亚像元模型中的低密度模型对科尔沁左翼后旗1989年、2000年和2007年三个时期的植被覆盖度变化情况进行了定量分析,拟找出近20年来沙地土地沙漠化的趋势及其特征,进而分析沙漠化逆转的最根本原因,从而为今后沙地环境改善和生态保护提供科学的决策依据。通过研究发现:
     1.应用亚像元模型对科左后旗的植被覆盖度进行监测,经验证平均精度达到76%,实践证明该方法适用于科左后旗植被覆盖信息的提取。该方法可为沙区大范围植被覆盖度估算提供一种有效途径,基本能够满足生态及气候模型研究的需要;
     2.科左后旗2007年植被覆盖度等级的空间分布格局是:高植被覆盖主要分布在科左后旗东部的沿辽平原农业区和位于旗西南的大青沟自然保护区,中植被覆盖在科左后旗植被覆盖类型中占相当大的优势,分布比较广泛,几乎遍布全旗,低植被覆盖主要分布在中西北部沙丘沙地牧林区,无植被覆盖比较少,在全旗有零星分布,分布的主要位置是在位于西北部沙丘沙地牧林区的一些流动沙丘和湖泊等区域。从面积来说,2007年科左后旗的中植被覆盖占绝对优势,其所占的比例为72%,高植被覆盖19%,低植被覆盖8%,无植被覆盖所占的比例为1%;
     3.科左后旗的植被覆盖变化是复杂多样的,各个类型之间在不断的相互转化。1989—2007年近20年期间,有高植被覆盖和中植被覆盖两个类型的面积发生了波动,高植被覆盖从1989年的721km~2减少到2000年的644km~2,但是在2000—2007年期间,面积增长幅度比较大,增长到了2140km~2;中植被覆盖正好相反,先由6455km~2增加到9126km~2后减小到了8277km~2。高植被覆盖类型先减后增,中植被覆盖类型先增后减。其它各植被覆盖类型面积的变化都呈持续性减少变化。在空间分布上,植被覆盖强烈提高的区域主要集中在科左后旗的中西北部沙丘沙地牧林区和南部浅丘甸农林牧区,轻度提高分布比较广泛,几乎遍布全区域,轻度降低主要分布在东部的沿辽平原农业区,强烈降低的区域比较少,只有零星分布;
     4.1989年到2000年再到2007年,科左后旗植被覆盖等级的空间景观格局变化特点是:无植被覆盖和低植被覆盖的优势度在持续降低,而高植被覆盖在持续增大,中植被覆盖则先是明显增加,然后是略微减少,植被覆盖等级的多样性指数的计算结果,反映科左后旗植被覆盖处于变化发展阶段;全旗整体表现为先规整后破碎的特点,全区的斑块数先减少后增加,由1989年的256252块减到2000年的173860块又增到2007年的196908块。两时间段虽变化趋势不一致,但从各植被覆盖类型的面积变化情况反映出该区的生态环境是在逐步好转;
     5.通过对1989到2000年,以及2000年到2007年两个区间的植被覆盖变化情况分析,可以看出科左后旗植被覆盖的变化是受自然因子和人文因子共同作用决定的,但发挥主导作用的是人文因子。科左后旗生态环境建设仍将是一项长期而艰巨的任务。
Sandy desertification is the main type of the desertification, it is extremely as the important environment and socio-economic problems of plaguing the world today, and threat to human survival and development. Vegetation coverage is the important factor that influences the land desertification , it is a comprehensive evaluation index that describe the plant community to overlay the earth's surface , be easy to observe, and turn a close relation with the soil erosion , water losses and the land desertification. The Horqin sandy land is at the east of northern agro-grazing ecotone in our country, belonging to the monsoon margin areas, and having typical model of the environment sensitivity and vulnerability. For a long time, it was a typical area of the development of desertification in China. But since the end of the 20th century sandy desertification in the overall reversal, had once again become China's sandy land from the environmental improvement of the cases. In view of this, this paper took a typical sandy area Keerqinzuoyihouqi as an example.With the analysis and research the calculate method of the vegetation coverage , this paper showed the quantitative analysis of 1989,2000 and third period in 2007 of vegetation coverage in the Keerqinzuoyihouqi with the method of sub-pixel model for vegetation coverage estimation based on land cover classification, and prepared to find out the trend of sandy land desertification and its characteristics in recent 20 years, then analysisd the most fundamental reasons of the desertification reversing, so as to improve the environment and provide a scientific decision making for ecological protection for future. Through the study found that:
     1.Used sub-pixel model to monitor the vegetation coverage of the Kezuohouqi,and mean precision validation of the extraction results was 76%, practicing to express that method can be used in the extraction of vegetation coverage in Kezuohouqi. That method could take an effective way for the sandy area’s vegetation coverage estimation, to meet the basic demand of the ecosystem and the climate model research;
     2. The vegetation coverage levels of Kezuohouqi in 2007 was that: the type of high coverage was mainly in the eastern part and in the southwest of the Daqinggou Nature Reserve, the type of medium coverage had a great advantage and a broader distribution, the type of low coverage mainly located in the northwest, and the type of no coverage mainly located at the northwest and the number of mobile sand dunes and lake areas. From the area, the type of medium coverage covered in the absolute superiority, its shared of 72%, the type of high coverage shared of 19%, the type of low coverage shared of 8% and the type of no coverage shared of 1%;
     3.The vegetation coverage of Kezuohouqi was complications and diverse, of each type at continuously of convert mutually. In the recent 20 years from 1989 to 2007, the type of high coverage decreased 721km~2 to 644km~2 from 1989 to 2000,but increased 2140km~2 from 2000 to 2007. The type of medium coverage increased 6455km~2 to 9126km~2 and then decreased to 8277km~2 .The other types area of the varieties kept on decreasing variety. In the spatial distribution, the vegetation coverage of the strong increase mainly concentrated in the region of the north-west and south , Mild increase almost throughout the entire region, mild decreased mainly in the eastern part , strongly reduced the relatively small region;
     4.From 1989 to 2000 and again to 2007, the space landscape change of Kezuohouqi’s vegetation coverage grade was that the index dominance of the type of no coverage and low coverage keep on decreasing, but the type of high coverage kept on increasing, and the type of medium coverage was first increased obviously and then decreased slightly; the calculation results of the vegetation coverage rating’s diversity index showed that Kezuohouqi’s vegetation coverage is in the variety development stage; The whole region performanced the features that first standardization and then crusher, The spot number of the region decreased first and then increased, from 256252 patches in 1989 decreasing to 173860 patches in 2000 and then increasing to 196908 patches again in2007. Although the variety trend inconformity in the two time segment, the area variety circumstance of each type of vegetation coverage showed an ecosystem environment of that area was turning for the better gradually.
     5.With the analysis of vegetation coverage variety circumstance in the two segments, one was from 1989 to 2000 and the other was from 2000 to 2007, we could see that the natural factor and the humanities factor played the common role to decide the Kezuohouqi’s vegetation coverage variety circumstance, but the humanities factor played a leading role. The ecological environment construction of the Kezuohouqi will still be one long-term and the arduous duty.
引文
[1]王涛.走向世界的中国沙漠化防治的研究与实践[J].中国沙漠,2001,21(1):1-3.
    [2]朱震达,王涛.从若干典型地区的研究对近十余年来中国土地沙漠化演变趋势的分析[J].地理学报, 1990,45(04):430-440.
    [3]王涛,赵哈林,肖洪浪.中国沙漠化研究的进展[J].中国沙漠,1999,19(4):299-311.
    [4]王涛,吴薇,薛娴等.近 50 年来中国北方沙漠化土地的时空变化[J].地理学报,2004, 59(2):203-212.
    [5]蔡体久,琚存勇,姚月峰等.基于 RS 和 GIS 的毛乌素沙地植被盖度定量估测[J].应用生态学报,2005,16(12):2301-2305.
    [6]卢中正,张光超,高会军等.毛乌素沙地东缘植被盖度变化研究[J].地球信息科学,2001,6(4):42-44.
    [7]师庆生,肖继东,潘晓玲等.近 20a 来新疆植被覆盖变化特征研究[J].干旱区研究,2004,21(4):389-394.
    [8]王力,郭广,胡爱军等.景观生态学原理与方法在荒漠化研究中应用的理论分析[J]. 青海草业,2004,13(3):20-23.
    [9]乌兰图雅.科尔沁的世纪垦殖与土地荒漠化[D].北京:中国科学院,1999.
    [10]吴薇.近 50 a 来科尔沁地区沙漠化土地的动态监测结果与分析[J].中国沙漠,2003,23(6):646-651.
    [11]王涛,吴薇,赵哈林等.科尔沁地区现代沙漠化过程的驱动因素分析[J]. 中国沙漠,2004,24(5):519-528.
    [12]王涛,我国沙漠化研究的若干问题—2.沙漠化的研究内容[J].中国沙漠,2003,23(5):477-482.
    [13]Tucker C J, Dregne H W, Newcomb W W. Expansion and Contraction of Sahara Desert from 1980 to 1990[J]. Science,1990,253: 299-301.
    [14]Hanna N R. Assessment of Desertification Around Deep Wells in Sahel Using Satellite Image[J]. Journal of Applied Ecology,1991,28:173-186.
    [15]Palmer A R,van Rooyen A F. Detecting Vegetation Change in the Southern Kalahari Using Landsat TM Data[J]. Journal of Arid Environments,1998,39(2):143-154.
    [16]Kharin N G. Desertification assessment and mapping: A case study of Turkmenistan[J]. USSR. Annals of Arid Zone,1986,25(1):26-29.
    [17]De Soyza A G,Whitford W G,Herrick J E,et al. Earlywarning indi-cators ofdesertification assessment and mapping in the Chihuahuan Desert[J]. J Arid Environ,1998,39:101—112.
    [18]赵哈林,周瑞莲.科尔沁沙地差不嘎蒿杂类草群落结构功能的沙漠化演变特征[J].草业学报,1993,2(2): 21-27.
    [19]高科,郑明军,王美云.科尔沁沙地景观梯度上植被分布格局研究[J].干旱区资源与环境,2002,14(1): 44-48.
    [20]赵以莲,周国英,陈桂琛.青海湖区东部沙地植被及其特征研究[J].中国沙漠,2007,27(5): 820-825.
    [21]邵立业,陈桂香.沙地植被的恢复和合理利用[J].中国草地,1986,8(6): 6-11.
    [22]赵丽娅,赵哈林.我国沙漠化过程中的植被演替研究[J].中国沙漠,2000,20 (S1):7-14.
    [23]彭鸿嘉,傅伯杰,陈利顶等.甘肃民勤荒漠区植被演替特征及驱动力研究——以民勤为例[J]. 2004,24(5):628-633.
    [24]颜长珍,王一谋,冯毓荪等.1996—2000 年陕甘宁青沙地遥感宏观动态研究[J]. 遥感学报,2002, 6(5):376-381.
    [25] 马金辉,蔡迪花,肖桐等.鄂尔多斯地区沙漠化遥感定量评价[J].兰州大学学报(自然科学版)[J]. 2007,43(4):1-6.
    [26]刘树林,王涛.浑善达克沙地的土地沙漠化过程研究[J]. 中国沙漠,2007,27(5):719-724.
    [27]王莉雯,卫亚星,牛铮.基于 GIS 的沙漠化土地面积遥感分析监测[J]. 地球信息科学,2007, 9(3):132-134.
    [28]刘海江,周成虎,程维明等.基于多时相遥感影像的浑善达克沙地沙漠化监测[J]. 生态学报,2008,28(2):627-635.
    [29]李爱敏,韩致文,黄翠华等.21 世纪初科尔沁沙地沙漠化程度变化动态监测[J].中国沙漠,2007,27(4):546-551.
    [30]天庆久,闵祥军.植被指数研究进展[J].地球科学进展,1998,13(4):327-333.
    [31]杨建平等.长江黄河源区的高寒植被变化的 NDVI 记录[J].地理学报,2005,60(3):467-477.
    [32]李本纲,陶澍.一种利用多时相 TM 影像分析地表植被变化的新方法—以敦煌地区绿洲植被变化分析为例[J].遥感学报,2000,4(4):295-298.
    [33]陈云浩,李晓兵等.北京海淀区植被覆盖的遥感动态研究[J].植物生态学报,2001,25(5):588-593.
    [34]刘广峰,吴波等.基于像元二分模型的沙漠化地区植被覆盖度提取——以毛乌素沙地为例[J].水土保持研究,2007,14(2):268-271.
    [35]周淑琴,吴发启,荆耀栋.毛乌素沙地南缘植被覆盖度动态监测——以陕西省靖边县为例[J].安徽农业科学,2007,35(27):8550-8551,8573.
    [36]常学礼,邬建国.科尔沁沙地景观格局的特征分析[J」.生态学报,1998,18(3):225 一 232.
    [37]常学礼,高玉葆,何兴东等.科尔沁地区流动沙地景观破碎化与沙漠化过程分析[J]. 南开大学学报(自然科学版),2006,39(1):84-89.
    [38]包慧娟,姚云峰,张学林等.科尔沁沙地景观格局变化的研究[J].干旱区资源与环境,2003,17(2):83—88.
    [39]哈斯其木格.科尔沁沙地甸地的景观格局变化分析——以通辽市科左后旗为例[J].内蒙古师范大学学报(自然科学汉文版),2007,36(1):111-114.
    [40]张远东等.荒漠绿洲 NDVI 与气候、水文因子的相关分析[J].生态学报,2003,27(6):816-821.
    [41]罗修岳,郑柯.脆弱生态环境植被指数和植被盖度数字图像的编制及其应用研究——以晋陕蒙地区为例[A].见:晋陕蒙接壤地区脆弱生态系统遥感监测与管理研究[M].北京:宇航出版社,1994:24-35.
    [42] Gutman G, Ignatov A. The derivation of the green vegetation fraction from NOAA/AVHRR data for use in numerical weather prediction models [J].International Journal of Remote Sensing,1998,19(8):1533—1543.
    [43]内蒙古科左后旗农牧业区划委员会办公室.科尔沁左翼后旗综合农牧业区划报告[R].1986.
    [44] 内蒙古统计局.内蒙古统计年鉴[M].中国统计出版社,2007.
    [45]苏志珠,董光荣.中国土地沙漠化研究现状及问题讨论[J].水土保持研究, 2002,9(3):133-135,145.
    [46]牛宝茹,刘俊蓉,王政伟.干旱半干旱地区植被覆盖度遥感信息提取研究[J].武汉大学学报·信息科学版,2005,第 30(1):27-30.
    [47]吴薇.土地沙漠化监测中 TM 影像的利用[J].2001,16(2):86-90.
    [48]马安青,王一谋等. 基于 RS 和 GIS 的甘肃省沙漠化现状及潜在沙漠化程度评价[J].水土保持学报,2003,l7(6):1-4,8.
    [49] Tyson P O.南部非洲的气候与沙漠化[J].世界沙漠研究,1985(3):12-15.
    [50]刘玉璋等.影响土壤风蚀主要因素的风洞实验研究[J].中国沙漠:1992(4):44-52.
    [51]徐岚.科尔沁沙地盐生植物群落复合体中主要植被群落的盐生生态[J].应用生态学报,1991,2(1):12-31.
    [52]傅星等.科尔沁沙地盐生草甸主要职务群落种群格局的研究[J].应用生态学报,1992,3(4),313-320.
    [53]刘新民,赵哈林,赵爱芬.科尔沁沙地风沙环境与植被[M].科学出版社,1996,1-294.
    [54]内蒙古统计局.内蒙古统计年鉴(1988-2007)[M].中国统计出版社,1988-2007.
    [55]苏永中.放牧干扰后自然恢复的退化沙质草地土壤性状的空间分布[J].土壤学报,2004,41(3):369-374.

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