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    塔里木河下游生态输水下植被时空演变及其影响因素

    Spatiotemporal evolution of vegetation and its influencing factors under ecological water conveyance in the lower reaches of the Tarim River, northwestern China

    • 摘要:
      目的 揭示2000—2023年生态输水背景下塔里木河下游植被时空演变特征及其主要影响因素,为干旱区生态输水调控与生态恢复提供依据。
      方法 基于2000—2023年生态输水量数据及综合植被指数(CVI),分析植被覆盖时空变化、空间与时间变异系数、冷热点格局及突变特征,并采用地理探测器识别植被空间分布的主要环境因子及其交互作用。
      结果 (1)研究期内低植被覆盖区面积占比由98.6%降至75.6%,高覆盖区沿河道两侧展宽,局部形成连续绿色廊道;全区热点与冷点面积比为1.6∶1.0。(2)CVI平均空间变异系数和时间变异系数分别为0.03和0.07。显著突变中76.3%为“中断型增加a”,突变在2012年相对集中,并与当年生态输水量的阶段性减少在时间序列上对应。(3)地下水埋深对植被空间分布的解释力最高(q = 0.346),地下水埋深与蒸散发的交互解释力达到0.452。
      结论 生态输水通过改善沿岸地下水等水分条件促进了荒漠植被恢复,但植被长期稳定生长对持续水分补给具有较高依赖性;保持水文调度相对平稳有利于巩固干旱区生态恢复成果。

       

      Abstract:
      Objective This paper aims to reveal the spatiotemporal evolution of vegetation and its main influencing factors in the lower reaches of the Tarim River under ecological water conveyance from 2000 to 2023, and to provide a basis for ecological water regulation and restoration in arid regions.
      Method Based on ecological water conveyance volume and the comprehensive vegetation index (CVI) from 2000 to 2023, the spatiotemporal changes in vegetation coverage, spatial and temporal coefficients of variation, hotspot and coldspot patterns, and abrupt changes were analyzed. Geodetector was used to identify the main environmental factors influencing vegetation spatial distribution and their interactions.
      Result During the study period, the proportion of low-vegetation-coverage area decreased from 98.6% to 75.6%, while high-coverage areas expanded along both sides of the river and locally formed continuous green corridors. The area ratio of hotspots to coldspots was 1.6∶1.0. The mean spatial and temporal coefficients of variation of CVI were 0.03 and 0.07, respectively. Among significant abrupt changes, 76.3% were classified as “interrupted increase a”, and abrupt changes were relatively concentrated in 2012, corresponding temporally to the phased reduction in ecological water conveyance that year. Depth to groundwater had the greatest explanatory power for vegetation spatial distribution (q = 0.346), and the interaction between depth to groundwater and evapotranspiration reached 0.452.
      Conclusion Ecological water conveyance promoted desert vegetation recovery by improving riparian groundwater and other moisture conditions, but long-term stable vegetation growth remained highly dependent on continuous water supply. Maintaining relatively stable hydrological regulation is beneficial for consolidating ecological restoration achievements in arid regions.

       

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