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中国东部山东济南北部岩溶地热水文地球化学特征演变及成因机制

Evolution of Karst Geothermal Hydrochemical Characteristics and Genesis Mechanism in Northern Jinan, Shandong, Eastern China.

作者信息

Wang Shuchun, Liu Zhiqing, Zhou Wei, Jiang Yanyu, Ding Hongliang, Dong Fangying

机构信息

Shandong Geology and Mineral Engineering Group Co., Ltd., Jinan 250200, China.

College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, Shandong 266590, China.

出版信息

ACS Omega. 2024 Aug 16;9(34):36299-36313. doi: 10.1021/acsomega.4c02870. eCollection 2024 Aug 27.

DOI:10.1021/acsomega.4c02870
PMID:39220514
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11360018/
Abstract

The study of geothermal water hydrochemical characteristics and solute transport evolution can provide a reliable hydrogeochemical basis for the development and protection of geothermal resources. Currently, there is a lack of systematic research on the hydrochemical evolution mechanism of geothermal fields in northern Jinan, which limits the development and use of geothermal fields. In this study, the hydrochemical properties of groundwater in northern Jinan were described by analyzing the hydrochemical characteristics of 16 geothermal water samples and 3 cold water samples. The results show that during the transformation from cold water in the south to geothermal water in the north, the contents of major ions all show an increasing trend and the hydrochemical characteristics show obvious zoning characteristics. The hydrochemical type evolved from HCO-Ca to HCO-Ca·Mg type, and then further evolved SO-Ca and SO-Ca·Na type water. Dissolution-precipitation of carbonate, sulfate, halite, and silicate minerals is one of the important processes that controls the chemical characteristics of geothermal water. The water source is mainly from the atmospheric precipitation in the Taiyi Mountain, with an altitude of 698.99-1464.91 m.s.a.l. The thermal reservoir temperature in the study area is estimated to be 55.62-98.16 °C. This paper proposes a conceptual model of the karst geothermal water flow system in northern Jinan, which provides a new idea for exploring the geothermal water genesis mechanism under similar geological conditions.

摘要

对地下热水水化学特征及溶质运移演化的研究可为地热资源的开发与保护提供可靠的水文地球化学依据。目前，济南北部地热田地水化学演化机制缺乏系统研究，这限制了地热田的开发利用。本研究通过分析16个地下热水样品和3个冷水样品的水化学特征，描述了济南北部地下水的水化学性质。结果表明，在从南部冷水向北部地下热水转化过程中，主要离子含量均呈增加趋势，水化学特征呈现明显的分带性。水化学类型由HCO-Ca型演变为HCO-Ca·Mg型，进而进一步演化为SO-Ca型和SO-Ca·Na型水。碳酸盐、硫酸盐、石盐和硅酸盐矿物的溶解-沉淀是控制地下热水化学特征的重要过程之一。水源主要来自海拔698.99-1464.91米的太沂山大气降水。研究区热储温度估计为55.62-98.16℃。本文提出了济南北部岩溶地下热水流动系统的概念模型，为探索类似地质条件下的地下热水成因机制提供了新思路。

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