Hydrogeochemical Characterization and Its Seasonal Changes of Groundwater Based on Self-Organizing Maps

Water resources are scarce in arid or semiarid areas; groundwater is an important water source to maintain residents’ lives and the social economy; and identifying the hydrogeochemical characteristics of groundwater and its seasonal changes is a prerequisite for sustainable use and protection of gro...

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Autores principales: Chu Wu, Xiong Wu, Chuiyu Lu, Qingyan Sun, Xin He, Lingjia Yan, Tao Qin
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Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:defdcac1f3bb40bdac81f723b11f660a2021-11-11T19:56:13ZHydrogeochemical Characterization and Its Seasonal Changes of Groundwater Based on Self-Organizing Maps10.3390/w132130652073-4441https://doaj.org/article/defdcac1f3bb40bdac81f723b11f660a2021-11-01T00:00:00Zhttps://www.mdpi.com/2073-4441/13/21/3065https://doaj.org/toc/2073-4441Water resources are scarce in arid or semiarid areas; groundwater is an important water source to maintain residents’ lives and the social economy; and identifying the hydrogeochemical characteristics of groundwater and its seasonal changes is a prerequisite for sustainable use and protection of groundwater. This study takes the Hongjiannao Basin as an example, and the Piper diagram, the Gibbs diagram, the Gaillardet diagram, the Chlor-alkali index, the saturation index, and the ion ratio were used to analyze the hydrogeochemical characteristics of groundwater. Meanwhile, based on self-organizing maps (SOM), quantification error (QE), topological error (TE), and the K-means algorithm, groundwater chemical data analysis was carried out to explore its seasonal variability. The results show that (1) the formation of groundwater chemistry in the study area was controlled by water–rock interactions and cation exchange, and the hydrochemical facies were HCO<sub>3</sub>-Ca type, HCO<sub>3</sub>-Na type, and Cl-Na type. (2) Groundwater chemical composition was mainly controlled by silicate weathering and carbonate dissolution, and the dissolution of halite, gypsum, and fluorite dominated the contribution of ions, while most dolomite and calcite were in a precipitated state or were reactive minerals. (3) All groundwater samples in wet and dry seasons were divided into five clusters, and the hydrochemical facies of clusters 1, 2, and 3 were HCO<sub>3</sub>-Ca type; cluster 4 was HCO<sub>3</sub>-Na type; and cluster 5 was Cl-Na type. (4) Thirty samples changed in the same clusters, and the groundwater chemistry characteristics of nine samples showed obvious seasonal variability, while the seasonal changes of groundwater hydrogeochemical characteristics were not significant.Chu WuXiong WuChuiyu LuQingyan SunXin HeLingjia YanTao QinMDPI AGarticleself-organizing maphydrogeochemistryseasonal variationcluster analysisHongjiannaoHydraulic engineeringTC1-978Water supply for domestic and industrial purposesTD201-500ENWater, Vol 13, Iss 3065, p 3065 (2021)
institution DOAJ
collection DOAJ
language EN
topic self-organizing map
hydrogeochemistry
seasonal variation
cluster analysis
Hongjiannao
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
spellingShingle self-organizing map
hydrogeochemistry
seasonal variation
cluster analysis
Hongjiannao
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
Chu Wu
Xiong Wu
Chuiyu Lu
Qingyan Sun
Xin He
Lingjia Yan
Tao Qin
Hydrogeochemical Characterization and Its Seasonal Changes of Groundwater Based on Self-Organizing Maps
description Water resources are scarce in arid or semiarid areas; groundwater is an important water source to maintain residents’ lives and the social economy; and identifying the hydrogeochemical characteristics of groundwater and its seasonal changes is a prerequisite for sustainable use and protection of groundwater. This study takes the Hongjiannao Basin as an example, and the Piper diagram, the Gibbs diagram, the Gaillardet diagram, the Chlor-alkali index, the saturation index, and the ion ratio were used to analyze the hydrogeochemical characteristics of groundwater. Meanwhile, based on self-organizing maps (SOM), quantification error (QE), topological error (TE), and the K-means algorithm, groundwater chemical data analysis was carried out to explore its seasonal variability. The results show that (1) the formation of groundwater chemistry in the study area was controlled by water–rock interactions and cation exchange, and the hydrochemical facies were HCO<sub>3</sub>-Ca type, HCO<sub>3</sub>-Na type, and Cl-Na type. (2) Groundwater chemical composition was mainly controlled by silicate weathering and carbonate dissolution, and the dissolution of halite, gypsum, and fluorite dominated the contribution of ions, while most dolomite and calcite were in a precipitated state or were reactive minerals. (3) All groundwater samples in wet and dry seasons were divided into five clusters, and the hydrochemical facies of clusters 1, 2, and 3 were HCO<sub>3</sub>-Ca type; cluster 4 was HCO<sub>3</sub>-Na type; and cluster 5 was Cl-Na type. (4) Thirty samples changed in the same clusters, and the groundwater chemistry characteristics of nine samples showed obvious seasonal variability, while the seasonal changes of groundwater hydrogeochemical characteristics were not significant.
format article
author Chu Wu
Xiong Wu
Chuiyu Lu
Qingyan Sun
Xin He
Lingjia Yan
Tao Qin
author_facet Chu Wu
Xiong Wu
Chuiyu Lu
Qingyan Sun
Xin He
Lingjia Yan
Tao Qin
author_sort Chu Wu
title Hydrogeochemical Characterization and Its Seasonal Changes of Groundwater Based on Self-Organizing Maps
title_short Hydrogeochemical Characterization and Its Seasonal Changes of Groundwater Based on Self-Organizing Maps
title_full Hydrogeochemical Characterization and Its Seasonal Changes of Groundwater Based on Self-Organizing Maps
title_fullStr Hydrogeochemical Characterization and Its Seasonal Changes of Groundwater Based on Self-Organizing Maps
title_full_unstemmed Hydrogeochemical Characterization and Its Seasonal Changes of Groundwater Based on Self-Organizing Maps
title_sort hydrogeochemical characterization and its seasonal changes of groundwater based on self-organizing maps
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/defdcac1f3bb40bdac81f723b11f660a
work_keys_str_mv AT chuwu hydrogeochemicalcharacterizationanditsseasonalchangesofgroundwaterbasedonselforganizingmaps
AT xiongwu hydrogeochemicalcharacterizationanditsseasonalchangesofgroundwaterbasedonselforganizingmaps
AT chuiyulu hydrogeochemicalcharacterizationanditsseasonalchangesofgroundwaterbasedonselforganizingmaps
AT qingyansun hydrogeochemicalcharacterizationanditsseasonalchangesofgroundwaterbasedonselforganizingmaps
AT xinhe hydrogeochemicalcharacterizationanditsseasonalchangesofgroundwaterbasedonselforganizingmaps
AT lingjiayan hydrogeochemicalcharacterizationanditsseasonalchangesofgroundwaterbasedonselforganizingmaps
AT taoqin hydrogeochemicalcharacterizationanditsseasonalchangesofgroundwaterbasedonselforganizingmaps
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