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基于RS的安寧河上游植被覆蓋時空變化研究
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國家科技支撐計劃資助項目(2008BAK51B02)和四川省科技支撐計劃資助項目(2013SZ0110)


Temporal and Spatial Variation of Vegetation Coverage on Upper Anning River Based on RS
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    摘要:

    以TM和ETM+遙感影像為數(shù)據(jù)源,利用RS和GIS技術(shù),提取和分析了1999—2010年安寧河上游植被覆蓋度及其時空變化特征,并結(jié)合Aster DEM數(shù)據(jù)分析了不同海拔高度帶和坡度帶的植被覆蓋分布及變化特征。研究結(jié)果表明,研究區(qū)植被覆蓋狀況總體較好,植被覆蓋度fc≥0.5的區(qū)域面積占研究區(qū)總面積的比例達60%以上;研究區(qū)植被覆蓋度總體呈增加趨勢,Ⅰ級(fc≥0.7)、Ⅱ級(0.5 ≤fc<0.7)和Ⅲ級(0.3≤fc<0.5)植被覆蓋度區(qū)域面積分別增加了1.24%、4.36%和2.28%,而Ⅳ級(0.1≤fc<0.3)和Ⅴ級(fc<0.1)植被覆蓋度區(qū)域面積呈減少特征,分別減少了25.72%和12.28%;植被覆蓋度較低的區(qū)域主要分布在海拔高度相對較低的地帶,隨著海拔高度的升高植被覆蓋度呈現(xiàn)出先增加后減少的趨勢,海拔高度低于3000m的地帶植被覆蓋變化較為明顯,主要表現(xiàn)為低植被覆蓋度向高植被覆蓋度轉(zhuǎn)化,其中海拔高度低于2500m的地帶變化最為顯著,海拔高度大于3000m的地帶受人為活動影響小,植被覆蓋變化相對較小;研究區(qū)植被覆蓋度較高的區(qū)域主要分布在坡度相對較陡的地帶,而植被覆蓋度較低的區(qū)域主要分布在坡度相對較緩的地帶,植被覆蓋度變化較為明顯的區(qū)域主要集中在坡度25°~45°的地帶,其次是坡度0°~25°的地帶;坡度45°以上的地帶受人為活動影響小,植被覆蓋變化不明顯;受水熱條件的影響,研究區(qū)植被覆蓋度隨坡向的變化特征呈現(xiàn)從大到小依次為陽坡(135°~225°)、半陽坡(45°~135°)、半陰坡(225°~315°)、陰坡(0°~45°,315°~360°),1999—2010年各坡向地帶的植被覆蓋度均有不同程度的提高,其中,陽坡提高幅度相對較大,陰坡提高幅度相對較小。

    Abstract:

    In order to reveal the temporal and spatial variation on vegetation coverage and provide evidence for ecological environment construction on the upper Anning River, the temporal and spatial variation on vegetation coverage, during 1999—2010, on the upper Anning River was extracted and analyzed based on two periods of remote sensing images (TM in 1999, ETM+ in 2010), which was based on RS and GIS technology. Meanwhile, combined with Aster DEM data, the vegetation distribution and its variation characteristics in different altitude and slope regions were also analyzed. The results showed that the vegetation coverage condition in study area overall was good. And the area of vegetation coverage (fc) above 0.5 was more than 60%. Besides, a trend emerged during 11 years in the study area that vegetation cover overall increased. The area of first grade vegetation coverage (fc≥0.7), second grade vegetation coverage (0.5≤fc<0.7) and third grade vegetation coverage (0.3≤fc<0.5) increased by 1.24%, 4.36% and 2.28%, respectively. However, the area of fourth grade vegetation coverage (0.1≤fc<0.3) and fifth grade vegetation coverage (fc<0.1) reduced by 25.72% and 12.28%, respectively. Low vegetation coverage was mainly distributed in relatively low altitude areas. With the increase of altitude, vegetation cover increased firstly and then decreased. Variation on vegetation coverage that low vegetation coverage was transformed into high vegetation cover degree was obvious in regions below 3000m, especially lower than 2500m. With influenced less by human activity, vegetation cover above 3000m seemed to hold relatively little change. High vegetation cover was mainly located in high slope regions, while low vegetation cover was mainly located in relatively moderate slope regions. An obvious variation on vegetation coverage was concentrated in regions with slope range from 25° to 45°, regions below 25° ranked secondly. While no obvious change of vegetation cover in regions with slope above 45° appeared, with less influenced by human activity. Under hydrothermal condition,the vegetation coverage on aspect is sunny slope (135°~225°)> half sunny slope (45°~135°)> half shady slope (225°~315°)> shady slope (0°~45°, 315°~360°); the vegetation coverage increased in each aspect from 1999 to 2010, and sunny slope increased significantly while no obvious increase on shady slope.

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胡玉福,蔣雙龍,劉 宇,李 翔,王鈺婷,陳 波.基于RS的安寧河上游植被覆蓋時空變化研究[J].農(nóng)業(yè)機械學報,2014,45(5):205-215. Hu Yufu, Jiang Shuanglong, Liu Yu, Li Xiang, Wang Yuting, Chen Bo. Temporal and Spatial Variation of Vegetation Coverage on Upper Anning River Based on RS[J]. Transactions of the Chinese Society for Agricultural Machinery,2014,45(5):205-215.

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  • 收稿日期:2013-11-25
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  • 在線發(fā)布日期: 2014-05-10
  • 出版日期: 2014-05-10