济阳浅层咸化地下水形成机理研究

Zhang Fengjuan, Xing Liting, Wang Song, Zhuang Huibo, Dou Tongwen, Yang Zengyuan
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引用次数: 0

摘要

内陆平原浅层咸水具有巨大的开发潜力。以济阳县孙耕镇咸水区为例,通过现场水质和地下水位测试。采用数理统计、管道水化学图、PHREEQC数值模拟等方法进行综合分析。共研究6862组资料。结果表明:(1)地下水表现为典型的“天气-蒸发”型,化学类型为Cl.SO4-Mg.Na。和Cl.SO4-Na。Mg类型。(2)内陆咸水区含水层介质粘土含量高,呈现滞后水流特征。地下水矿化明显。(3)蒸发、交替吸附、水岩相互作用等水文地球化学作用是复杂水化学类型形成的主要原因。内陆平原咸水区独特的地下水循环特征,使得水动力相对稳定。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Research on Formation Mechanism of Jiyang Shallow Saline GroundWater
Shallow salt water in the inland plain has huge development potential. Taking saline water area in Sungeng Town, Jiyang County as an example, based on field water quality and water table tests., tracing test, methods such as mathematical statistical, hydrochemistry diagram of piper and numerical simulation by PHREEQC are used to analyze synthetically. 6862 groups data were studied. Results showed: (1) The groundwater presents typically "weather - evaporation" type, chemistry type is Cl.SO4-Mg.Na. and Cl.SO4-Na.Mg type. (2) In area of inland saline water presents characteristics of lagging water flow with high clay content in aquifer medium. Groundwater mineralization is obvious. (3) Hydrogeochemistry actions such as evaporation, alternate adsorption and water-rock interaction are the primary cause of the forming complex hydrochemistry type. The unique groundwater circulation characteristics of inland plains salt- water area makes water dynamic being relatively stable.
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