本文選題：熱示蹤法　切入點：洪水過程　出處：《水電能源科學(xué)》2017年10期

【摘要】：為分析第二松花江下游洪水過程對河水-地下水交換的影響,以第二松花江下游德惠河段2016年10月15日~11月16日經(jīng)歷的一次漲洪—退洪過程為例,根據(jù)熱示蹤法,運用VFLUX2.0.0程序計算了該河段河水—地下水交換強度,探討了洪水前和洪水過程中研究區(qū)河水—地下水交換模式及交換強度的變化。結(jié)果表明,洪水過程改變了河水—地下水交換模式,使交換強度增加。研究結(jié)果為該流域地下水資源的評價與管理、地表水與地下水的綜合利用提供理論依據(jù)。
[Abstract]:For the analysis of second flood process impact on the lower reaches of the Songhua River River groundwater exchange, to experience the second Songhua River in lower reaches of Dehui in October 15, 2016 ~11 month 16 days a flood - retreating flood process as an example, according to the heat tracing method, the river water and groundwater exchange intensity was calculated by using VFLUX2.0.0 program, discusses the changing process and before the flood the flood water in study area groundwater exchange mode and exchange strength. The results show that the flood process changed River groundwater exchange mode, the exchange strength increase. The results for the evaluation of groundwater resources in this basin and the management, and provide a theoretical basis for the comprehensive utilization of surface water and groundwater.

【作者單位】： 吉林大學(xué)環(huán)境與資源學(xué)院;吉林大學(xué)水資源與環(huán)境研究所;吉林大學(xué)建設(shè)工程學(xué)院;
【基金】：國家水體污染控制與治理科技重大專項項目(2014ZX07201-010)
【分類號】：P339;P641
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本文編號：1693400