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利用聚类、分组分析和模糊集方法,并结合 GIS 平台对地下水水文地球化学过程和质量状况进行综合研究:以韩国蔚山市大川为例。

Comprehensive studies of hydrogeochemical processes and quality status of groundwater with tools of cluster, grouping analysis, and fuzzy set method using GIS platform: a case study of Dalcheon in Ulsan City, Korea.

机构信息

Department of Earth & Environmental Sciences, Institute of Environmental Geosciences, Pukyong National University, 599-1 Daeyeon-dong, Nam-gu, Busan, 608-737, South Korea,

出版信息

Environ Sci Pollut Res Int. 2015 Aug;22(15):11209-23. doi: 10.1007/s11356-015-4290-4. Epub 2015 Mar 18.

Abstract

This research aimed at developing comprehensive assessments of physicochemical quality of groundwater for drinking and irrigation purposes at Dalcheon in Ulsan City, Korea. The mean concentration of major ions represented as follows: Ca (94.3 mg/L) > Mg (41.7 mg/L) > Na (19.2 mg/L) > K (3.2 mg/L) for cations and SO4 (351 mg/L) > HCO3 (169 mg/L) > Cl (19 mg/L) for anions. Thematic maps for physicochemical parameters of groundwater were prepared, classified, weighted, and integrated in GIS method with fuzzy logic. The maps exhibited that suitable zone of drinking and irrigation purpose occupied in SE, NE, and NW sectors. The undesirable zone of drinking purpose was observed in SW and central parts and that of irrigation was in the western part of the study area. This was influenced by improperly treated effluents from an abandoned iron ore mine, irrigation, and domestic fields. By grouping analysis, groundwater types were classified into Ca(HCO3)2, (Ca,Mg)Cl2, and CaCl2, and CaHCO3 was the most predominant type. Grouping analysis also showed three types of irrigation water such as C1S1, C1S2, and C1S3. C1S3 type of high salinity to low sodium hazard was the most dominant in the study area. Equilibrium processes elucidated the groundwater samples were in the saturated to undersaturated condition with respect to aragonite, calcite, dolomite, and gypsum due to precipitation and deposition processes. Cluster analysis suggested that high contents of SO4 and HCO3 with low Cl was related with water-rock interactions and along with mining impact. This study showed that the effluents discharged from mining waste was the main sources of groundwater quality deterioration.

摘要

本研究旨在对韩国蔚山市大川地区的饮用水和灌溉地下水的理化质量进行综合评估。主要离子的平均浓度如下:阳离子中 Ca(94.3mg/L)>Mg(41.7mg/L)>Na(19.2mg/L)>K(3.2mg/L),阴离子中 SO4(351mg/L)>HCO3(169mg/L)>Cl(19mg/L)。地下水理化参数的专题地图是使用 GIS 方法和模糊逻辑进行编制、分类、加权和综合的。这些地图显示,适宜的饮用水和灌溉用途区域位于东南部、东北部和西北部。不适宜的饮用水用途区域位于西南部和中心部分,而不适宜的灌溉用途区域位于研究区的西部。这是由于一个废弃铁矿的污水未经适当处理、灌溉和家庭农田的影响。通过分组分析,将地下水类型分为 Ca(HCO3)2、(Ca,Mg)Cl2 和 CaCl2,其中 CaHCO3 是最主要的类型。分组分析还显示了三种灌溉水类型,即 C1S1、C1S2 和 C1S3。在研究区域中,高盐度到低盐度危害的 C1S3 类型最为普遍。平衡过程表明,由于沉淀和沉积过程,地下水样品处于方解石、白云石、石膏和文石的过饱和到不饱和状态。聚类分析表明,高含量的 SO4 和 HCO3 与低 Cl 与水岩相互作用和采矿影响有关。本研究表明,采矿废物排放的废水是地下水质量恶化的主要来源。

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