滨海水库沉积物盐分释放水化学特征变化  

Variations in hydrochemical during the process of sediment salt release in coastal reservoirs

作　　者：武建茹 李海明[1,2,3] 李梦娣 肖瀚 WU Jianru;LI Haiming;LI Mengdi;XIAO Han(Laboratory of Coastal Groundwater Utilization&Protection,Tianjin University of Science&Technology,Tianjin 300457,China;Tianjin University of Science and Technology,Tianjin 300453,China;Key Laboratory of Marine Resource Chemistry and Food Technology(TUST),Ministry of Education,Tianjin 300457,China;Chinese Academy of Ervironmental Sciences,State Key Laboratory of Groundwater Pollution Simulation and Control for Ervironmental Protection,Beijing,100012,China)

机构地区：[1]天津科技大学滨海地下水利用与保护实验室,天津300457 [2]天津科技大学海洋与环境学院,天津300457 [3]海洋化学资源与食品技术教育部重点实验室,天津300457 [4]中国环境科学研究院国家环境保护地下水污染模拟与控制重点实验室,北京100012

出　　处：《南水北调与水利科技（中英文）》2023年第2期301-312,共12页South-to-North Water Transfers and Water Science & Technology

基　　金：国家自然科学基金项目(42072288)。

摘　　要：以北大港水库为研究区,通过野外实地采样和批试验相结合的方法,对滨海水库库水和沉积物混合后盐分和各主要离子指标的变化规律进行分析,探究库水和沉积物之间的水文地球化学作用,揭示水库咸化机理。结果表明:库水和沉积物在混合条件下,沉积物中的盐分会释放到库水中,各水化学指标能够快速地达到平衡;各采样点溶解性总固体(TDS)均先快速增加,而后盐分释放达到平衡,平衡后TDS释放量整体呈现出水库下游采样点>水库上游采样点的规律;Na+和Cl-是库水和沉积物水文地球化学作用过程中发生变化的主要离子,Na^(+)、Cl^(-)最大释放量分别为7597.25 mg/kg和11097.00 mg/kg。在库水和沉积物相互作用中各采样点的Na^(+)、K^(+)、Mg^(2+)、Ca^(2+)和SO_(4)^(2-)发生着不同程度的增加或减少,Cl^(-)均有所升高,HCO_(3)^(-)略有降低;除HCO_(3)^(-)和Ca^(2+)外,其他离子的变化均呈现水库下游采样点>水库上游采样点的规律。Completion of the Binhai Reservoir may experience serious salinization or sudden brackishness,thus affecting the normal water supply function.The research on reservoir water salinization mainly focuses on total salinity,chloride ion,or other single indicators,but the release of sediment salt is a complex process.In fact,during the hydrogeochemical process of sediments and reservoir water,various ions may change to different degrees,and the changes of ions will affect the TDS content,which in turn affects the salinity content of the reservoir water.Therefore,the research on the regularity of salt release also needs to carry out a full analysis of ion indicators,to provide theoretical support for the hydrogeochemical interactions between sediments and reservoir water.Taking Beidagang Reservoir as the research area,through the method of combining field sampling and batch experiment,the change law of salinity and main ion indexes after the mixing of coastal reservoir water and sediment is analyzed to explore reservoir water and sediment.The hydrogeochemical interaction between the objects reveal the mechanism of reservoir salinization.Illation condition of reservoir water and sediment,the water chemical indexes can quickly reach equilibrium.The TDS mass concentration of each sampling point increased rapidly at first,and the salt release reached equilibrium after 30 s.Na^(+)and Cl^(-)were the main ions involved in water-rock interaction;the maximum release amounts of Na+and Cl^(-)were 7597.25 mg/kg,11097.00 mg/kg.The Na^(+),K^(+),Mg^(2+),Ca^(2+),SO_(4)^(2-)of each sampling point increased or decreased in different degrees in the sediment-reservoir water interaction.Cl^(-)was increased,HCO_(3)^(-)decreased slightly.Except for HCO_(3)^(-)and Ca^(2+),the changes of other ions showed the rule of sampling points in the downstream of the reservoir>sampling points in the upstream of the reservoir.During the hydrogeochemical process of sediment-reservoir water,the total salt in the sediment was released,and the changes of eac

关 键 词：北大港水库 沉积物 盐分释放 水质咸化 水文地球化学作用 

分 类 号：X524[环境科学与工程—环境工程]