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中国天津拟议水库初期蓄水期水盐度风险评估

A risk assessment of water salinization during the initial impounding period of a proposed reservoir in Tianjin, China.

机构信息

Key Laboratory of Integrated Regulation and Resource Development on Shallow Lakes, Ministry of Education, Nanjing 210098, China.

出版信息

Environ Sci Process Impacts. 2013 Sep;15(9):1743-51. doi: 10.1039/c3em00162h.

Abstract

Water salinization of coastal reservoirs seriously threatens the safety of their water supply. To elucidate the mechanism of salinization and to quantitatively analyze the risk in the initial period of the impoundment of a proposed reservoir in Tianjin Binhai New Area, laboratory and field simulation experiments were implemented and integrated with the actual operation of Beitang Reservoir, which is located in the same region and has been operational for many years. The results suggested that water salinization of the proposed reservoir was mainly governed by soil saline release, evaporation and leakage. Saline release was the prevailing factor in the earlier stage of the impoundment, then the evaporation and leakage effects gradually became notable over time. By referring to the actual case of Beitang Reservoir, it was predicted that the chloride ion (Cl(-)) concentration of the water during the initial impounding period of the proposed reservoir would exceed the standard for quality of drinking water from surface water sources (250 mg L(-1)), and that the proposed reservoir had a high risk of water salinization.

摘要

滨海地区水库的水盐化严重威胁着其供水安全。为了阐明盐化机制,并定量分析天津滨海新区拟建水库在蓄水初期的风险,进行了实验室和现场模拟实验,并结合位于同一地区、已运行多年的北塘水库的实际运行情况进行了综合分析。结果表明,拟建水库的水盐化主要受土壤盐分释放、蒸发和渗漏的控制。在蓄水初期,盐分释放是主要因素,随着时间的推移,蒸发和渗漏的影响逐渐显著。参照北塘水库的实际情况,预测拟建水库在初期蓄水期间的水中氯离子(Cl(-))浓度将超过地表水水源水质标准(250mg/L(-)),且该水库存在较高的水盐化风险。

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