The “groundwater benefit zone”, proposals, contributions and new scientific issues

Ying Zhao
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Abstract

The groundwater has great potential for water resource utilization, accounting for about a quarter of vegetation transpiration globally and contributing up to 84% in shallow groundwater areas. However, in irrigated agricultural regions or coastal areas with shallow groundwater levels, due to the high groundwater salinity, the contribution of groundwater to transpiration is small and even harmful. This paper proposes a new conception of groundwater benefit zone in the groundwater-soil–plant-atmosphere continuum (GSPAC) system. Firstly, it analyzes the mutual feedback processes of the underground hydrological process and aboveground farmland ecosystem. Secondly, it elaborates on the regional water and salt movement model proposed vital technologies based on the optimal regulation of the groundwater benefit zone and is committed to building a synergy that considers soil salt control and groundwater yield subsidies. Finally, based on the GSPAC system water-salt coupling transport mechanism, quantitative model of groundwater benefit zone, and technical parameters of regional water-salt regulation and control, the scientific problems and development opportunities related to the conception of groundwater benefit zone have been prospected.
“地下水效益带”,建议,贡献和新的科学问题
地下水具有巨大的水资源利用潜力,约占全球植被蒸腾的四分之一,在浅层地下水地区贡献高达84%。然而,在灌溉农业区或地下水位较浅的沿海地区,由于地下水盐度较高,地下水对蒸腾的贡献很小,甚至有害。本文提出了地下水-土壤-植物-大气连续体(GSPAC)系统地下水效益带的新概念。首先,分析了地下水文过程与地上农田生态系统的相互反馈过程。其次,阐述了基于地下水效益带优化调控的区域水盐运动模型提出的关键技术,致力于构建兼顾土壤盐分控制和地下水产量补贴的协同效应。最后,基于GSPAC系统水盐耦合输运机制、地下水效益带定量模型和区域水盐调控技术参数,对地下水效益带概念相关的科学问题和发展机遇进行了展望。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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