地球科学进展 ›› 2018, Vol. 33 ›› Issue (7): 702 -718. doi: 10.11867/j.issn.1001-8166.2018.07.0702

生态水文学与水安全 上一篇    下一篇

旱区地下水文与生态效应研究现状与展望
王文科( ), 宫程程, 张在勇, 陈立   
  1. 长安大学环境科学与工程学院,旱区地下水文与生态效应教育部重点实验室,陕西 西安 710054
  • 收稿日期:2018-03-26 修回日期:2018-06-16 出版日期:2018-07-20
  • 基金资助:
    *国家自然科学基金联合基金重点项目“准噶尔盆地典型流域地表水与地下水转换的动力学机制与生态效应”(编号:U1603243);国家自然科学基金重点项目“旱区地表—地下水系统界面动力学与水循环研究”(编号:41230314)资助.

Research Status and Prospect of the Subsurface Hydrology and Ecological Effect in Arid Regions

Wenke Wang( ), Chengcheng Gong, Zaiyong Zhang, Li Chen   

  1. School of Environmental Science and Engineering, Chang’an University, Key Laboratory of Subsurface Hydrology and Ecological Effects in Arid Regin, Ministry of Education, Xi’an 710054, China
  • Received:2018-03-26 Revised:2018-06-16 Online:2018-07-20 Published:2018-08-30
  • About author:

    First author: Wang Wenke(1962-), male, Qishan County, Shaanxi Province, Professor. Research areas include subsurface hrdrology and ecological effects in arid regin. E-mail:wenkew@chd.edu.cn

  • Supported by:
    Project supported by the National Natural Science Foundation of China “Dynamic mechanism of river-groundwater transformation and its ecological effect in typical catchment of Junggar Basin”(No.U1603243) and “Interface dynamics and water cycle research of the surface-groundwater system in arid regions ”(No.41230314).

围绕旱区地下水文与生态效应面临的科学问题以及国家生态文明与“一路一带”建设对地下水学科研究需求的紧迫性,分析了旱区地下水形成演化机理,研究了旱区地下水的功能。在此基础上,围绕6个重大科学问题分析了国内外研究现状、存在的问题与发展趋势,针对旱区地下水文与生态效应研究存在的瓶颈和国家的需求,提出了亟待解决的关键科学问题,助力于我国地下水科学的创新发展和国家经济建设。

Centering on the scientific problems faced by subsurface hydrology in arid regions and ecological effect, the urgency of national ecological civilization and the Belt and Road construction towards the research of groundwater discipline, this article analyzed the formation and evolution mechanisms of groundwater and studied the groundwater function of arid regions. Based on the analysis and research, this article discussed domestic and overseas research status, existing problems and developing trend from six aspects, raised key and scientific problems which urgently need to be addressed, aiming at the existing bottlenecks of subsurface hydrology and ecological effect in arid regions and national requirement, so as to make some contribution to the innovative development of China’s groundwater science and national economic construction.

中图分类号: 

图1 西北内陆盆地流域地下水文过程示意图
Fig.1 Schematic diagram of the groundwater hydrological processes of the catchment scale in northwest inland basin, China
图1 西北内陆盆地流域地下水文过程示意图
Fig.1 Schematic diagram of the groundwater hydrological processes of the catchment scale in northwest inland basin, China
图2 地表—地下水系统主要界面分布示意图
Fig.2 Schematic diagram of surface-subsurface water system interface distribution
图2 地表—地下水系统主要界面分布示意图
Fig.2 Schematic diagram of surface-subsurface water system interface distribution
图3 旱区近地表土壤热通量及裸土蒸发变化趋势图 (a)和(b)鄂尔多斯盆地风沙滩地区不同地下水位埋深区地表以下10和20 cm处的热通量随时间的分布;(c)准噶尔盆地裸土不同月份的蒸发强度
Fig.3 The heat flux on the surface ground and the evaporation intensity on the bare ground in arid area (a),(b) Heat flux distributions below the surface ground 10 and 20 cm under the conditions of different water table depths at the blown-sand area of Ordos Basin; (c) The evaporation intensity of different months on the bare ground in Junggar Basin
图3 旱区近地表土壤热通量及裸土蒸发变化趋势图 (a)和(b)鄂尔多斯盆地风沙滩地区不同地下水位埋深区地表以下10和20 cm处的热通量随时间的分布;(c)准噶尔盆地裸土不同月份的蒸发强度
Fig.3 The heat flux on the surface ground and the evaporation intensity on the bare ground in arid area (a),(b) Heat flux distributions below the surface ground 10 and 20 cm under the conditions of different water table depths at the blown-sand area of Ordos Basin; (c) The evaporation intensity of different months on the bare ground in Junggar Basin
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