Water quality classification and vertical distribution of hot springs using hydrochemical methods and multivariate analysis at the Beppu hydrothermal area, Japan

Heejun Yang
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引用次数: 2

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.
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
以日本别武热液区52口温泉井为研究对象,进行了多变量分析(层次聚类分析和因子分析)和水文分析,从垂直分布角度评价温泉水质的变化和水流路径。将温泉水质分为g1、g2 a、g2 b、g2 c、g3 5组。g1和g2a主要分布在龟川热带,g3和g2c主要分布在别府热带。在两个热区均观测到g2b。别府热区温泉的水型与80年代基本一致,但由Cl型变为hco3型。温泉的垂直分布表明别府热区存在两种不同的流动路径,并证实了靠近海岸的井中存在海水混合。海水与温泉水的混合率以Cl -浓度计算,为海水的12%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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