上游山河流域的地表地下水相互作用和充电源:从稳定的同位素特征和水地化学过程的洞察力

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Updated: May 13, 2025

Continuous Instream Monitoring of Nutrients and Sediment in Agricultural Watersheds
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Continuous Instream Monitoring of Nutrients and Sediment in Agricultural Watersheds

Published on: September 26, 2017

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Shijin Rajan1, Janardhana Raju Nandimandalam1

  • 1School of Environmental Sciences, Jawaharlal Nehru University, New Delhi, 110067, India.

Environmental research
|April 13, 2025
PubMed
概括

这项研究揭示了河水和地下水如何相互作用,以及利用稳定的同位素和水地化学方法在山河上游盆地产生充电源的地方. 调查结果显示,冰川融水充电了上游流域,而季风降雨充电了下游地区,这对水资源管理至关重要.

关键词:
水地地化学 水地地化学当地的流星水线是当地流星水线.多变量统计的多变量统计.充电来源 充电来源稳定的同位素是稳定的.亚木纳河是亚木纳河的一条河流.

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