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2000-2020年塔里木河干流生态系统对地下水位变化的响应

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地下水位的深浅直接影响植被的生长状况、生态分布格局及生态系统的稳定性,因此研究生态系统对地下水位变化的响应对于生态修复工作至关重要。塔里木河干流地下水位的波动,主要是生态输水、气候变化和人类活动共同作用产生的结果,地下水位的变化影响生态系统的空间分布。以塔里木河干流为研究对象,基于长期监测的地下水埋深数据和多期遥感数据,运用半变异函数模型、动态度分析、分形维数计算和趋势分析等方法,分析地下水埋深和生态系统的时空特征,探讨生态系统对地下水位变化的响应。结果表明:①2000—2020 年,塔里木河干流的地下水埋深随着与河道距离的增加而逐渐增大,地下水埋深的空间变化受到人为因素(种植制度、灌溉强度)以及自然环境(地形、地貌、气候、土壤类型和含水层)的影响,且空间相关性不断提高。②2000—2020 年,塔里木河干流生态系统变化主要表现为农田生态系统面积的增加和草地生态系统面积的减少,此变化占总变化的 58%。其中,农田生态系统主要由灌丛生态系统转变而来,转变面积为 1 118。00 km2;草地生态系统向其他各生态系统转变面积显著,为 1 258。69 km2。③生态系统的分形维数从 1。470 1 降至 1。135 0,表明其用地的复杂程度降低,稳定性指数从 0。029 9 增至 0。365 0,稳定性增强。④持续的生态输水使塔里木河干流地下水位上升,生态呈现出显著的正面发展态势,77。0%的区域生态轻微改善,8。0%的区域中等程度改善,1。7%的区域明显改善。研究显示,地下水埋深的变化对塔里木河干流生态有显著影响,地下水埋深减小,生态恢复明显,地下水埋深增大则生态退化明显。
Response of Tarim River Mainstream Ecosystem to Groundwater Level Changes from 2000 to 2020
The depth to groundwater directly affects the condition of vegetation growth,the pattern of ecological distribution,and the stability of ecosystems.Therefore,studying the response of the ecosystems to groundwater level changes is of great significance to ecological restoration.The change of the groundwater level in the mainstream of the Tarim River is mainly the result of the combined effects of ecological water diversion,climate change,and human activities.The change of groundwater level affects the spatial distribution of ecosystems.With the Tarim River mainstream as the research object,this study is based on long-term groundwater depth monitoring data and multiperiod remote sensing image data.Semivariogram function modeling,dynamic trend analysis,fractal dimension calculation,and trend analysis are employed to analyze groundwater depth and ecosystem spatial and temporal characteristics.Furthermore,it discusses the response of the ecosystem to changes in groundwater depth.The main conclusions are as follows:(1)The groundwater depth increases with increasing distance from the river.Groundwater depth spatial variation is affected by both human factors such as cropping systems and irrigation intensity,and natural factors such as topography,geomorphology,climate,soil types,and aquifers.The spatial correlation increases annually.(2)From 2000 to 2020,the transformation of ecosystem along the Tarim River mainstream was mainly driven by an increase in farmland and decrease in grassland.They accounted for 58%of the total ecosystem transformation,with farmland mainly replacing shrublands,yielding 1118 km2 conversion.Grasslands was transformed on a large scale into other ecosystems,with a conversion area of 1258.69 km2.(3)The ecosystem fractal dimension decreased from 1.4701 to 1.1350,indicating ecosystem complexity reduction.The stability coefficient increased from 0.0299 to 0.3650,indicating increased ecosystem stability.(4)Continuous ecological water diversion has led to an increase in the groundwater depth in the mainstream of the Tarim River,resulting in a significant positive development trend in the ecosystem,with 77.0%of the areas experiencing slight ecological improvement,8.0%moderate improvement,and 1.7%significant improvement.The changes in groundwater depth has a significant impact on the ecosystem along the Tarim River mainstream.When the groundwater depth decreases,the ecosystem recovers obviously.When the depth increases,the ecosystem degrades obviously.

ecosystemsdepth to groundwaterdynamic characteristicsresponseTarim River mainstream

马晓倩、钟瑞森、吴彬、刘坤、魏光辉、钟文静

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新疆农业大学水利与土木工程学院,新疆 乌鲁木齐 830052

中国科学院新疆生态与地理研究所,荒漠与绿洲生态国家重点实验室,新疆 乌鲁木齐 830011

新疆遥感与地理信息系统应用重点实验室,新疆 乌鲁木齐 830011

新疆水利工程安全与水灾害防治重点实验室,新疆 乌鲁木齐 830052

新疆塔里木河流域管理局,新疆 库尔勒 841000

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生态系统 地下水埋深 动态特征 响应 塔里木河干流

2025

环境科学研究
中国环境科学研究院

环境科学研究

北大核心
影响因子:1.775
ISSN:1001-6929
年,卷(期):2025.38(1)