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新疆玛纳斯河流域2000—2010年土地利用/覆盖变化及影响因素
引用本文:刘金巍,靳甜甜,刘国华,李宗善,杨荣金.新疆玛纳斯河流域2000—2010年土地利用/覆盖变化及影响因素[J].生态学报,2014,34(12):3211-3223.
作者姓名:刘金巍  靳甜甜  刘国华  李宗善  杨荣金
作者单位:中国科学院生态环境研究中心城市与区域生态国家重点实验室, 北京 100085;中国水利水电科学研究院, 北京 100012;中国科学院生态环境研究中心城市与区域生态国家重点实验室, 北京 100085;中国科学院生态环境研究中心城市与区域生态国家重点实验室, 北京 100085;中国环境科学研究院, 北京 100038
基金项目:西北(甘青新)重点区域和行业发展战略环境评价生态专题资助项目(D237)
摘    要:在2000年和2010年两期遥感影像解译的基础上,从土地利用类型的结构、变化速率、变化方向及土地利用程度等方面分析了玛纳斯河流域土地利用的变化特征,并分析了影响土地利用变化的主要因素及不同因素之间的交互作用。结果表明:(1)近10年来,流域土地利用程度增强,人工绿洲呈扩张趋势,耕地和城乡工矿居民用地大量增加,林地和未利用地减少;上游地区草地和冰川积雪覆盖地面积增加。(2)耕地向内部外部双向扩张,主要来源于林地、荒漠和盐碱地;新增草地以山地裸地和山前荒漠的转变为主;林地主要转变为中游的耕地和城乡工矿居民用地及上游的草地和裸地;城乡工矿居民用地的增加主要来自荒漠、耕地和林地;未利用地变化以向人工绿洲土地类型的转变为主。(3)上游土地利用变化主要受气候变化的影响,降水量增加可能是冰川积雪面积扩张的主要原因;中游人类活动密集,耕地和城乡工矿居民用地扩张,荒漠植被退化;下游受气候和人类活动共同作用,尾闾湖泊萎缩,河岸和湖周植被退化。

关 键 词:玛纳斯河流域  土地利用变化  气候变化  人类活动
收稿时间:2013/4/23 0:00:00
修稿时间:2013/11/19 0:00:00

Analysis of land use/cover change from 2000 to 2010 and its driving forces in Manas River Basin, Xinjiang
LIU Jinwei,JIN Tiantian,LIU Guohu,LI Zongshan and YANG Rongjin.Analysis of land use/cover change from 2000 to 2010 and its driving forces in Manas River Basin, Xinjiang[J].Acta Ecologica Sinica,2014,34(12):3211-3223.
Authors:LIU Jinwei  JIN Tiantian  LIU Guohu  LI Zongshan and YANG Rongjin
Institution:State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China;China Institute of Water Resources and Hydropower Research, Beijing 100012, China;State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China;State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China;Chinese Research Academy of Environmental Sciences, Beijing 100038, China
Abstract:Based on Landsat TM/ETM (Thematic Mapper/Enhanced Thematic Mapper) image data from 2000 and 2010 and some other survey and statistical data, this paper first analyzed the characteristics of land use/cover change in the Manas River Basin of Xinjiang. We used numerical computation methods and index models, including land use/cover structural changes, the single land use/cover dynamic index, the land-use transfer matrix and the land use degree index, to determine the features of land use/cover change both temporally and spatially. Subsequently, the main drivers of land use/cover change and the interaction between different factors were analyzed based on a comprehensive consideration of natural factors and human factors. The findings of this study may be summarized here. (1) The land use/cover structure of this basin was dominated by unused land in both 2000 and 2010, followed by cultivated land and grassland, and lastly by water (the smallest area). The extent of land use in 2010 increased compared with that in 2000 across the whole basin. The cultivated land and built-up land increased at an accelerated rate, especially in the middle region, which at the same time resulted in a significant expansion of artificial oasis and led to an evidently decreasing trend of woodland and unused land. In the upper reaches, the most obvious change of land use/cover was the areas of grassland, glaciers and snow-covered land-a clear sign of expansion. (2) The cultivated land indicated a quite remarkable outward and inward expansion trend. According to our data for the conversion of land use/cover in 2010, the new cultivated land was mainly derived from desert shrubbery land, desert and saline-alkali land. Grassland was mostly concentrated in the upper reaches and experienced an obvious increasing trend second only to cultivated land. The increased area was mainly converted from bare rock on the mountain and piedmont desert. Built-up land also showed a noticeable increase because of the occupation of desert, cultivated land and woodland. According to our data for the change in destination of land use/cover in 2000, the reduced woodland primarily evolved to cultivated land and built-up land in the middle reaches, and to grassland and bare land in the upper reaches. Additionally, the reduced unused land was mainly transformed into artificial oasis land types. A greater proportion of bare land and sand, saline-alkali land and desert was converted into cultivated and built-up land. (3) The climate of this basin was characterized by a warming and wet trend from 1959 to 2010. Climate change was the dominant factor of land use/cover change in the upper reaches. The increase in precipitation, especially short-term heavy rainfall, might be the primary cause of the advance of glaciers and snow-covered land. In the middle reaches, the most noticeable features were the increase in cultivated and built-up land and the degradation of desert vegetation. It could be speculated that this was mainly attributable to the intensified anthropogenic activities concomitant with economic growth and the increase in population. Moreover, the reduction in gross irrigation water uptake led to an even greater reduction in return water, which led to an even greater reduction in the water needed ecologically and a degradation of natural oasis land. The evident decline in terminal lakes and serious degradation of the associated vegetation in the lower reaches are directly attributable to the combined impact of climate change and human activities.
Keywords:Manas River Basin  land use change  climate change  human activities
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