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Research on Formation Mechanism of Jiyang Shallow Saline GroundWater

机译:济阳市浅层盐渍地下水形成机理研究

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Shallow salt water in the inland plain has huge development potential. Taking saline water area in SungengTown, Jiyang County as an example, based on field water quality and water table tests., tracing test, methods such asmathematical statistical, hydrochemistry diagram of piper and numerical simulation by PHREEQC are used to analyzesynthetically. 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 presentscharacteristics 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 causeof the forming complex hydrochemistry type. The unique groundwater circulation characteristics of inland plains saltwaterarea makes water dynamic being relatively stable.
机译:内陆平原的浅层盐水具有巨大的发展潜力。以济阳县双溪镇盐碱水区为例,基于田间水质和地下水位试验,示踪试验,数学统计,吹管水化学图和PHREEQC数值模拟等方法进行综合分析。研究了6862组数据。结果表明:(1)地下水典型为“天气蒸发”型,化学类型为Cl.SO4-Mg.Na。和Cl.SO4-Na.Mg类型。 (2)内陆地区咸水具有含水层介质中黏土含量高的滞后水流特征。 (3)蒸发,交替吸附和水-岩相互作用等水文地球化学作用是形成复杂水化学类型的主要原因。内陆平原咸水区独特的地下水循环特征使水动力相对稳定。

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