越南西北部莱州省 Nam Mu 河流域地下水和溪水的水文地质化学特征和水质指标

Thu Thi Do, Pham Thị Dung, Tuan Anh Tran, Luong Duc Le, Hai Dinh Vu, Tra Thi Thu Doan, Dao Quang Le, Hien Trong Tran, Dat Ngoc Pham, Lien Thi Nguyen, Dung Thi Phuong Le
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摘要

在越南北部山区等旱季缺水地区,评估地下水和上游水的质量对管理、利用和保护天然水资源具有重要意义。在这项研究中,我们收集并分析了莱州省南木河流域旱季的 54 个地下水和上游溪水样本。我们对这些样本进行了全面的理化参数、主要离子浓度和微量元素分析。一些结果显示,溪水与地下水关系密切,化学成分相似。这些水可根据地质构造进行分类,从而得出该地区的两种主要水类型。第一种类型以 Ca2+ - Mg2+ - HCO3- 为特征,主要分布在三叠纪土著沉积物中。第二种是混合水类型,从 Ca2+ - Mg2+ - Cl- 到 Ca2+ - Na+ - HCO3-,主要分布在二叠纪长石火山岩地层中。这些不同类型的水主要是水与岩石、沉淀过程和离子交换现象相互作用的结果。地球化学模拟结果表明,文石、方解石和白云石矿物过饱和,导致碳酸盐矿物沉淀。同时,模拟结果表明,萤石、石膏、海泡石和钠长石等矿物有溶解的趋势。使用水质指数对水质进行的评估表明,根据 QCVN 01-1:2018/BYT 2018 标准,大部分地下水和溪水适合家庭使用。然而,在某些取样地点存在水质超过允许标准的例外情况,主要是由于铁、锰和 NO3- 浓度水平升高。因此,在将这些特定地点的水用于日常活动之前,必须对其进行水处理,以确保当地居民的安全和福祉。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrogeochemical characteristic and water quality index of groundwater and streamwater at Nam Mu River basin, Lai Chau province in northwest Vietnam
Assessing the quality of groundwater and upstream water in regions experiencing water scarcity during the dry season, such as the mountainous districts of Northern Vietnam, holds immense significance in the management, utilization, and preservation of natural water resources. In this study, we collected and analyzed 54 samples of groundwater and upstream stream water within the Nam Mu River basin in Lai Chau province during the dry season. These samples underwent thorough analysis for physicochemical parameters, major ion concentrations, and trace elements. Some results revealed a close relationship between streamwater and groundwater, indicating a similar chemical composition. These waters could be classified based on geological formations, yielding two primary water types in the area. The first type, characterized by Ca2+ - Mg2+ - HCO3- is prevalent in Triassic terrigenous sediments. The second type is a mixed water type, ranging from Ca2+ - Mg2+ - Cl- to Ca2+ - Na+ - HCO3-, primarily distributed in Permian felsic volcanic formations. These distinct water types are primarily the result of interactions between water and rock, precipitation processes, and ion exchange phenomena. Geochemical simulation results demonstrated the supersaturation of aragonite, calcite, and dolomite minerals, leading to the precipitation of carbonate minerals. Concurrently, the simulation indicated a tendency to dissolve minerals such as fluorite, gypsum, halite, and sylvite. The assessment of water quality using the WQI indicates that, in accordance with QCVN 01-1:2018/BYT 2018 standards, the majority of groundwater and streamwater are suitable for domestic use. However, exceptions exist in certain sample locations where water quality exceeds permissible standards, primarily due to elevated levels of Fe, Mn, and NO3- concentration. Hence, it is important to implement water treatment processes for the water sourced from these specific locations before their utilization in daily activities to ensure the safety and well-being of the local population.
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