{"title":"刚果(金)东部Twangiza金矿周边地下水理化特征及水质评价","authors":"Mukungilwa Myango , Lefranc Basima , Kavatsurwa Muyisa , Isaac Chungachako , Patient Zamukulu , Lina Aleke , Muhigwa Bahananga","doi":"10.1016/j.jafrearsci.2025.105767","DOIUrl":null,"url":null,"abstract":"<div><div>The present study focuses on groundwater around the Twangiza gold mine, which serve as a source of drinking water for the local population, with the aim of characterizing it based on its physicochemical properties. A total of 13 water samples were collected for analysis of physicochemical characteristics (pH, TDS, EC, TSS, major cations and anions), using conventional analytical methods. The results indicated acidic to neutral and ranged from 4.5 to 7.1, with 76.9 % acidic (pH 4–6.5), below WHO and EU permissible limits. The hydrochemical facies of groundwater revealed Mg-Ca-SO<sub>4</sub> water types in the vicinities of the mine, indicating sulphate imprint related to the dissolution of gold bearing sulphides, and Ca-Mg-HCO<sub>3</sub> types downstream the mine, more associated with carbonate minerals. Multivariate statistical analysis grouped groundwater based on similarities of physicochemical parameters and indicated the parts of geogenic process and anthropogenic activities in the mineralization. Water-rock interactions involved mainly silicate weathering and indicated the role of sulphide dissolution in the surrounding areas close to the mine. The sodium adsorption rate classified the water as excellent to good, with an overall low alkalizing power, which makes the water suitable for irrigation. The Water Quality Index (WQI) indicated that local groundwater quality ranged from excellent to good across most stations, with the exception of one station within the active mine classified as poor. These findings are helpful for the understanding of groundwater mineralization processes and would assist in the sustainable use of groundwater.</div></div>","PeriodicalId":14874,"journal":{"name":"Journal of African Earth Sciences","volume":"231 ","pages":"Article 105767"},"PeriodicalIF":2.2000,"publicationDate":"2025-07-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Physicochemical characterization and quality assessment of groundwater around the Twangiza gold mine (Eastern D.R. Congo)\",\"authors\":\"Mukungilwa Myango , Lefranc Basima , Kavatsurwa Muyisa , Isaac Chungachako , Patient Zamukulu , Lina Aleke , Muhigwa Bahananga\",\"doi\":\"10.1016/j.jafrearsci.2025.105767\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The present study focuses on groundwater around the Twangiza gold mine, which serve as a source of drinking water for the local population, with the aim of characterizing it based on its physicochemical properties. A total of 13 water samples were collected for analysis of physicochemical characteristics (pH, TDS, EC, TSS, major cations and anions), using conventional analytical methods. The results indicated acidic to neutral and ranged from 4.5 to 7.1, with 76.9 % acidic (pH 4–6.5), below WHO and EU permissible limits. The hydrochemical facies of groundwater revealed Mg-Ca-SO<sub>4</sub> water types in the vicinities of the mine, indicating sulphate imprint related to the dissolution of gold bearing sulphides, and Ca-Mg-HCO<sub>3</sub> types downstream the mine, more associated with carbonate minerals. Multivariate statistical analysis grouped groundwater based on similarities of physicochemical parameters and indicated the parts of geogenic process and anthropogenic activities in the mineralization. Water-rock interactions involved mainly silicate weathering and indicated the role of sulphide dissolution in the surrounding areas close to the mine. The sodium adsorption rate classified the water as excellent to good, with an overall low alkalizing power, which makes the water suitable for irrigation. The Water Quality Index (WQI) indicated that local groundwater quality ranged from excellent to good across most stations, with the exception of one station within the active mine classified as poor. These findings are helpful for the understanding of groundwater mineralization processes and would assist in the sustainable use of groundwater.</div></div>\",\"PeriodicalId\":14874,\"journal\":{\"name\":\"Journal of African Earth Sciences\",\"volume\":\"231 \",\"pages\":\"Article 105767\"},\"PeriodicalIF\":2.2000,\"publicationDate\":\"2025-07-04\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of African Earth Sciences\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1464343X25002341\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of African Earth Sciences","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1464343X25002341","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Physicochemical characterization and quality assessment of groundwater around the Twangiza gold mine (Eastern D.R. Congo)
The present study focuses on groundwater around the Twangiza gold mine, which serve as a source of drinking water for the local population, with the aim of characterizing it based on its physicochemical properties. A total of 13 water samples were collected for analysis of physicochemical characteristics (pH, TDS, EC, TSS, major cations and anions), using conventional analytical methods. The results indicated acidic to neutral and ranged from 4.5 to 7.1, with 76.9 % acidic (pH 4–6.5), below WHO and EU permissible limits. The hydrochemical facies of groundwater revealed Mg-Ca-SO4 water types in the vicinities of the mine, indicating sulphate imprint related to the dissolution of gold bearing sulphides, and Ca-Mg-HCO3 types downstream the mine, more associated with carbonate minerals. Multivariate statistical analysis grouped groundwater based on similarities of physicochemical parameters and indicated the parts of geogenic process and anthropogenic activities in the mineralization. Water-rock interactions involved mainly silicate weathering and indicated the role of sulphide dissolution in the surrounding areas close to the mine. The sodium adsorption rate classified the water as excellent to good, with an overall low alkalizing power, which makes the water suitable for irrigation. The Water Quality Index (WQI) indicated that local groundwater quality ranged from excellent to good across most stations, with the exception of one station within the active mine classified as poor. These findings are helpful for the understanding of groundwater mineralization processes and would assist in the sustainable use of groundwater.
期刊介绍:
The Journal of African Earth Sciences sees itself as the prime geological journal for all aspects of the Earth Sciences about the African plate. Papers dealing with peripheral areas are welcome if they demonstrate a tight link with Africa.
The Journal publishes high quality, peer-reviewed scientific papers. It is devoted primarily to research papers but short communications relating to new developments of broad interest, reviews and book reviews will also be considered. Papers must have international appeal and should present work of more regional than local significance and dealing with well identified and justified scientific questions. Specialised technical papers, analytical or exploration reports must be avoided. Papers on applied geology should preferably be linked to such core disciplines and must be addressed to a more general geoscientific audience.