{"title":"基于水化学方法和多元分析的日本别府热液区温泉水质分类和垂直分布","authors":"Heejun Yang","doi":"10.5917/jagh.63.137","DOIUrl":null,"url":null,"abstract":"To evaluate changes in hot spring water quality and estimate the flow paths from its vertical distribution, multivariate analysis (Hierarchical cluster analysis and Factor analysis) and hydrological analysis were conducted using 52 hot spring wells in the Beppu hydrothermal area, Japan. Hot spring water quality was classified by five groups (G 1 , G 2 a, G 2 b, G 2 c, and G 3 ). G 1 and G 2 a are distributed in the Kamegawa thermal zone, and G 3 and G 2 c are mainly found in the Beppu thermal zone. G 2 b is observed in both thermal zones. The water types of the hot springs were almost consistent with those in the 1980 s but changed from Cl to HCO 3 type in the Beppu thermal zone. The vertical distribution of the hot springs implies that there are two distinct flow paths in the Beppu thermal zone, and confirmed the seawater mixing in the well located near the shore. The mixing rate between the seawater and hot spring water was calculated by Cl - concentration, which was 12 % of seawater.","PeriodicalId":173171,"journal":{"name":"Journal of groundwater hydrology","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-08-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"Water quality classification and vertical distribution of hot springs using hydrochemical methods and multivariate analysis at the Beppu hydrothermal area, Japan\",\"authors\":\"Heejun Yang\",\"doi\":\"10.5917/jagh.63.137\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"To evaluate changes in hot spring water quality and estimate the flow paths from its vertical distribution, multivariate analysis (Hierarchical cluster analysis and Factor analysis) and hydrological analysis were conducted using 52 hot spring wells in the Beppu hydrothermal area, Japan. Hot spring water quality was classified by five groups (G 1 , G 2 a, G 2 b, G 2 c, and G 3 ). G 1 and G 2 a are distributed in the Kamegawa thermal zone, and G 3 and G 2 c are mainly found in the Beppu thermal zone. G 2 b is observed in both thermal zones. The water types of the hot springs were almost consistent with those in the 1980 s but changed from Cl to HCO 3 type in the Beppu thermal zone. The vertical distribution of the hot springs implies that there are two distinct flow paths in the Beppu thermal zone, and confirmed the seawater mixing in the well located near the shore. The mixing rate between the seawater and hot spring water was calculated by Cl - concentration, which was 12 % of seawater.\",\"PeriodicalId\":173171,\"journal\":{\"name\":\"Journal of groundwater hydrology\",\"volume\":\"1 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-08-31\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of groundwater hydrology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5917/jagh.63.137\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of groundwater hydrology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5917/jagh.63.137","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Water quality classification and vertical distribution of hot springs using hydrochemical methods and multivariate analysis at the Beppu hydrothermal area, Japan
To evaluate changes in hot spring water quality and estimate the flow paths from its vertical distribution, multivariate analysis (Hierarchical cluster analysis and Factor analysis) and hydrological analysis were conducted using 52 hot spring wells in the Beppu hydrothermal area, Japan. Hot spring water quality was classified by five groups (G 1 , G 2 a, G 2 b, G 2 c, and G 3 ). G 1 and G 2 a are distributed in the Kamegawa thermal zone, and G 3 and G 2 c are mainly found in the Beppu thermal zone. G 2 b is observed in both thermal zones. The water types of the hot springs were almost consistent with those in the 1980 s but changed from Cl to HCO 3 type in the Beppu thermal zone. The vertical distribution of the hot springs implies that there are two distinct flow paths in the Beppu thermal zone, and confirmed the seawater mixing in the well located near the shore. The mixing rate between the seawater and hot spring water was calculated by Cl - concentration, which was 12 % of seawater.