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了解地下水和地表水之间的交换过程,使用迷你驱动点压力计和数学模型来确定合适的管理下水层充电点

Sudipa Halder^1,2, Malabika Biswas Roy³, Pankaj Kumar Roy⁴

¹School of Water Resources Engineering, Jadavpur University, Kolkata, West Bengal, India.

Environmental science and pollution research international

|July 26, 2023

概括

这项研究估计了印度Shilabati盆地的地下特征,使用了压力计和数值建模. 它确定了管理水表补充 (MAR) 的最佳地点,以应对干旱,实现12.096 MLD的安全产量.

科学领域:

水文地质学水文地质学
环境工程环境工程
水资源管理水资源管理

背景情况:

研究了印度西孟加拉邦Shilabati盆地 (3888平方公里) 的地表特征.
了解流床液压导电性 (K_h) 是至关重要的,特别是在获得和失去流的过程中,但记录不完善.
流床中相反的流量条件可以显著影响毛孔大小,细颗粒含量和K_h.

研究的目的:

为了估计在希拉巴蒂盆地内的地下特征和流水层相互作用.
确定适合管理水表充填 (MAR) 实施的地点,以减轻干旱事件.
确定水基础设施的最佳设计参数,例如辐射收集井.

主要方法:

一个稳定状态的数值模型,使用具有成本效益的平移计和MIKE FEFLOW包.
模糊的多标准决策分析 (MCDA) 基于9个标准 (河流排水,湿度,多孔性,排水,降雨量,土地使用,地质,含水层材料,K_h) 进行 MAR 选址.
试验,以优化安全收益率的基础设施设计在异型,均质,不受限制的,半无限的含水层.

主要成果:

盆地的地下水位在160.33至0.32米以上.
在Dakshin Pairachali现场记录的最高K_h值为6.765m/day,表明当地的含水层排放到溪流中.
辐射采集井和透画廊的优化安全产量为12.096 MLD.

结论:

这项研究提供了宝贵的洞察力,了解了Shilabati流域的水文地质学和流水层动态.
已识别的MAR网站为西孟加拉邦的干旱管理提供了可持续的解决方案.
该方法为其他地区的类似水地质评估和水资源管理策略提供了框架.

关键词:

模糊的哥布拉斯 (COPRASAS) 是一个模糊的哥布拉斯.这是一个模糊的TOPSISIS.液压导电能力液压导电能力迈克·费弗洛 (Mike Feflow) 是一个著名的演员.迷你驱动点压力计迷你驱动点压力计

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