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Water and ecological security: dealing with hydroclimatic challenges at the heart of China's Silk Road

机译:水与生态安全:应对丝绸之路中心的水文气候挑战

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摘要

The Tarim Basin is the heart of China's Silk Road Economic Belt. The contradiction between economic growth and environmental protection is particularly evident in the basin region. For the past 20 years, the groundwater has been increasingly overused, causing water tables to decline precipitously. In the past decade in particular, the total water storage (TWS) in the basin has undergone a significant decreasing trend, losing around -13 x 10(8) m(3)/year from 2002 to 2013. Prior to 1998, the normalized difference vegetation index (NDVI) of natural vegetation exhibited an increasing trend at a rate of 0.012 per decade, but from 1999 onwards, the NDVI started decreasing at a rate of 0.005 per decade. In the 2000s, the bare soil areas of the Taklamakan Desert boundaries expanded by 7.8 %. At the same time, the effects of global warming on water and ecological systems are likewise intensifying in the Tarim Basin. The increases in warming have outpaced increases in precipitation, and the negative effects of climate change on the region's vulnerable ecology have intensified. Potential changes in the usage of limited water resources may further increase the risk of desertification and deepen the area's ecological poverty. Excessive water use and over allocation, including over-pumping of groundwater, are themain factors causing the loss of groundwater, the depletion of total water storage, and the overall ecological degradation, but these are being exacerbated by global warming. To address all of these issues in a holistic way, a unified management mechanism that encompasses both surface water and groundwater must be developed, and the implementation of the government plan to return farmland to natural vegetation should be speed up.
机译:塔里木盆地是中国丝绸之路经济带的心脏。经济增长与环境保护之间的矛盾在流域地区尤为明显。在过去的20年中,地下水的使用量日益增加,导致地下水位急剧下降。特别是在过去的十年中,流域的总储水量(TWS)呈显着下降趋势,从2002年到2013年每年损失约-13 x 10(8)m(3)/年。在1998年之前,天然植被的差异植被指数(NDVI)以每十年0.012的速率呈现增加趋势,但从1999年开始,NDVI开始以每十年0.005的速率降低。在2000年代,塔克拉玛干沙漠边界的裸露土壤面积扩大了7.8%。同时,塔里木盆地的全球变暖对水和生态系统的影响也在加剧。变暖的增加超过了降水的增加,气候变化对该地区脆弱生态的负面影响加剧了。有限水资源利用的潜在变化可能进一步增加荒漠化的风险并加深该地区的生态贫困。过度用水和过度分配,包括地下水过度抽取,是造成地下水流失,总储水量枯竭和整体生态退化的主要因素,但全球变暖加剧了这些因素。为了从整体上解决所有这些问题,必须建立一个涵盖地表水和地下水的统一管理机制,并应加快执行政府将农田恢复为天然植被的计划。

著录项

  • 来源
    《Environmental earth sciences》 |2016年第10期|881.1-881.10|共10页
  • 作者单位

    Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, 818 South Beijing Rd, Urumqi 830011, Peoples R China;

    Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, 818 South Beijing Rd, Urumqi 830011, Peoples R China;

    Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, 818 South Beijing Rd, Urumqi 830011, Peoples R China;

    Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, 818 South Beijing Rd, Urumqi 830011, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

    Chinese Acad Sci, Ctr Agr Resources Res, Key Lab Agr Water Resources, Shijiazhuang 050011, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Climate change; Groundwater; Total water storage; Vegetation degradation; China's Silk Road;

    机译:气候变化;地下​​水;总储水量;植被退化;中国的丝绸之路;

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