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How changes of groundwater level affect the desert riparian forest ecosystem in the Ejina Oasis, Northwest China

机译:地下水位如何影响额济纳绿洲的沙漠河岸森林生态系统

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摘要

Groundwater is a key factor controlling the growth of vegetation in desert riparian systems. It is important to recognise how groundwater changes affect the riparian forest ecosystem. This information will not only help us to understand the ecological and hydrological process of the riparian forest but also provide support for ecological recovery of riparian for-ests and water-resources management of arid inland river basins. This study aims to estimate the suitability of the Water Vegetation Energy and Solute Modelling (WAVES) model to simulate the Ejina Desert riparian forest ecosystem changes, China, to assess effects of groundwater-depth change on the canopy leaf area index (LAI) and water budgets, and to ascer-tain the suitable groundwater depth for preserving the stability and structure of desert riparian forest. Results demonstrated that the WAVES model can simulate changes to ecological and hydrological processes. The annual mean water consump-tion of a Tamarix chinensis riparian forest was less than that of a Populus euphratica riparian forest, and the canopy LAI of the desert riparian forest should increase as groundwater depth decreases. Groundwater changes could significantly in-fluence water budgets for T. chinensis and P. euphratica riparian forests and show the positive and negative effects on veg-etation growth and water budgets of riparian forests. Maintaining the annual mean groundwater depth at around 1.7?2.7 m is critical for healthy riparian forest growth. This study highlights the importance of considering groundwater-change im-pacts on desert riparian vegetation and water-balance applications in ecological restoration and efficient water-resource management in the Heihe River Basin.
机译:地下水是控制沙漠河岸系统植被生长的关键因素。重要的是要认识到地下水的变化如何影响河岸森林生态系统。这些信息不仅将有助于我们了解河岸带森林的生态和水文过程,而且还将为河岸带森林的生态恢复和干旱内陆河流域的水资源管理提供支持。这项研究旨在评估水生植被能量和溶质模型(WAVES)模型的适用性,以模拟中国额济纳沙漠沿岸森林生态系统的变化,以评估地下水深度变化对冠层叶面积指数(LAI)和水的影响预算,并确定合适的地下水深度,以保持沙漠河岸森林的稳定性和结构。结果表明,WAVES模型可以模拟生态和水文过程的变化。 Ta柳河岸林的年平均耗水量少于胡杨河岸林的年耗水量,并且随着地下水深度的减少,沙漠河岸林的冠层LAI应增加。地下水变化可能会显着影响中华锥and和胡杨林河林的水平衡,并显示出对植被生长和河林水平衡的正反作用。将年均地下水深度维持在1.7?2.7 m左右对于健康的河岸森林生长至关重要。这项研究强调了在黑河流域中考虑地下水变化对沙漠河岸植被的影响和水平衡应用在生态恢复和有效水资源管理中的重要性。

著录项

  • 来源
    《寒旱区科学(英文版)》 |2019年第1期|62-80|共19页
  • 作者单位

    Key Laboratory of Ecohydrology of Inland River Basin, Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Alashan Desert Eco-hydrology Experimental Research Station, Ejina, Inner Mongolia 735400, China;

    Key Laboratory of Ecohydrology of Inland River Basin, Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    University of Chinese Academy of Sciences, Beijing 100049, China;

    Key Laboratory of Ecohydrology of Inland River Basin, Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Alashan Desert Eco-hydrology Experimental Research Station, Ejina, Inner Mongolia 735400, China;

    CSIRO Land and Water Flagship, Canberra, ACT 2601, Australia;

    Key Laboratory of Ecohydrology of Inland River Basin, Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Alashan Desert Eco-hydrology Experimental Research Station, Ejina, Inner Mongolia 735400, China;

    Key Laboratory of Ecohydrology of Inland River Basin, Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Alashan Desert Eco-hydrology Experimental Research Station, Ejina, Inner Mongolia 735400, China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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