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Monitoring the hydrological and ecological response to water diversion in the lower reaches of the Tarim River, Northwest China

机译:监测塔里木河下游引水的水文和生态响应

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摘要

During the past twelve years, the assessment of hydro-ecological response of degraded floodplain ecosystems to the emergent water diversion practices in the lower reaches of the Tarim River has become a key research topic. This paper presents the current ecological conditions and analyzes what the water diversion has achieved. The limitations of this floodplain restoration program are discussed, based on the review of literature and long term field work data (groundwater data, eco-morphological parameters of riparian forests, Quick Bird remote sensing data) collected from three transects (Yingsu, Karday, Arghan). The results show that annual average groundwater depth responded to a certain degree after water diversion since May 2000. After a second water diversion, groundwater depth within 300 m distance from the river channel recovered significantly from 9.4 m in 1997 to 4.28 m in 2001 at Yingsu. With the exception of relatively favorable groundwater depth for floodplain forests within 150 m distance from the riverbed, groundwater depth at larger distances remained far below 5 m, and most forest plants excluding Tamarix sp. will suffer from water scarcity. The average crown loss (CL) and crown diameter (CD) of Populus euphratica trees in different distances from the riverbed have shown various degrees of responses. The effects of recovery were notable within 200 m distance to the riverbed. Distribution patterns of young seedlings, new shoots and root suckers of P. euphratica generated by water diversion also demonstrated that most were distributed close to the riverbed and reduced sharply with increasing distance. Twelve water diverting actions in the lower reaches of the Tarim River have made significant achievements in forest recovery near the riverbed, but had limited positive effects on more distant floodplain sites.
机译:在过去的十二年中,评估塔里木河下游退化的洪泛区生态系统对紧急引水措施的水生态响应已成为关键研究课题。本文介绍了目前的生态条件,并分析了调水取得的成就。在回顾文献和从三个样貌(Yingsu,Karday,Arghan)收集的长期野外工作数据(地下水数据,河岸森林生态形态参数,Quick Bird遥感数据)的基础上,讨论了该洪泛区恢复计划的局限性)。结果表明,自2000年5月以来,引水后年平均地下水深度有一定程度的响应。第二次引水后,距河道300 m范围内的地下水深度从1997年的9.4 m恢复到2001年的4.28 m。 。除了距河床150 m范围内的洪泛区森林相对有利的地下水深度外,较大距离处的地下水深度仍远低于5 m,除Tamarix sp。以外的大多数森林植物。将遭受缺水的困扰。胡杨在距河床不同距离处的平均树冠损失(CL)和树冠直径(CD)表现出不同程度的响应。在距河床200 m的范围内,恢复效果显着。引水产生的胡杨幼苗,新芽和根吸盘的分布格局也表明,大部分分布在河床附近,并随着距离的增加而急剧减少。塔里木河下游的十二种引水行动在河床附近的森林恢复方面取得了显著成就,但对较远的洪泛区却没有起到积极的作用。

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  • 来源
    《Quaternary International》 |2013年第17期|155-162|共8页
  • 作者单位

    Key Laboratory of Oasis Ecology, College of Resources & Environmental Science, Xinjiang University, Urumqi 830046, China,Applied Physical Geography, Catholic University of Eichstaett-Ingolstadt, Eichstaett 85071, Germany;

    Key Laboratory of Oasis Ecology, College of Resources & Environmental Science, Xinjiang University, Urumqi 830046, China,Applied Physical Geography, Catholic University of Eichstaett-Ingolstadt, Eichstaett 85071, Germany;

    Applied Physical Geography, Catholic University of Eichstaett-Ingolstadt, Eichstaett 85071, Germany;

    Applied Physical Geography, Catholic University of Eichstaett-Ingolstadt, Eichstaett 85071, Germany;

    Key Laboratory of Oasis Ecology, College of Resources & Environmental Science, Xinjiang University, Urumqi 830046, China,Faculty of Forest and Environment, Eberswalde University for Sustainable Development, Eberswalde 16255, Germany;

    Key Laboratory of Oasis Ecology, College of Resources & Environmental Science, Xinjiang University, Urumqi 830046, China;

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