Please use this identifier to cite or link to this item: http://hdl.handle.net/11455/44676
標題: Identification of the origin of salinization in groundwater using multivariate statistical analysis and geochemical modeling: a case study of Kaohsiung, Southwest Taiwan
作者: Lu, H.Y.
彭宗仁
Peng, T.R.
Liou, T.S.
關鍵字: boron;environmental isotopes;geochemical modeling;factor analysis;Taiwan;formation brines;natural-waters;paris basin;boron;chemistry;evolution;aquifer;france
Project: Environmental Geology
期刊/報告no:: Environmental Geology, Volume 55, Issue 2, Page(s) 339-352.
摘要: 
The study of brine aquifers in southern Taiwan is highly complicated by hybrid geochemical reactions, which obscure important geochemical information. Using multivariate analysis on major and minor ion compositions normalized by Cl(-) content, chemical constituents were combined into two principal components representing brine mixing and mineral precipitation. Comparing to multivariate analysis on the original data, this procedure reveals more geochemical information. It demonstrates that the brine groundwater of the region is primarily composed of highly evaporated seawater. The evaporation ratio is > 70%; a point at which calcite, dolomite and gypsum precipitate. Oxygen and hydrogen isotopic compositions confirm this inference; and further, geochemical modeling quantitatively determined the evaporation ratio to be about 85%. Natural boron contamination is a consequence of brine groundwater. Two evolutionary trends in the plotting of the Cl/B ratio versus Cl(-) can be identified: (1) Cl/B ratio decreases with boron being released from clay minerals when brine aquifers are flushed with freshwater; and (2) Cl/B ratio increases when seawater of a high Cl/B ratio infiltrates coastal aquifers.
URI: http://hdl.handle.net/11455/44676
ISSN: 0943-0105
DOI: 10.1007/s00254-007-0979-0
Appears in Collections:土壤環境科學系

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