Temperature evaluation of the Bugok geothermal system, South Korea

Seong Sook Park, Seong Taek Yun, Gi Tak Chae, Ian Hutcheon, Yong Kwon Koh, Chil Sup So, Hyeon Su Choi

Research output: Contribution to journalArticle

8 Citations (Scopus)

Abstract

Using a variety of chemical geothermometers and statistical analysis, we estimate the temperature of a possible deeper geothermal reservoir at Bugok, Southern Korea. Shallow thermal aquifers (down to about 400 m depth) are under exploitation in this area; the temperatures (up to 78 °C) of the produced fluids are the highest found in South Korea. Based on hydrochemical data and occurrence, the groundwaters at Bugok can be classified under three groups: Na-SO4 thermal groundwaters (CTGW) occurring in the central (about 0.24 km2) part of the area; Ca-HCO3 cold groundwater (SCGW) found in shallow peripheral parts of the CTGW; the intermediate-type groundwater (STGW). The CTGW type is typical of the Bugok thermal waters; they have the highest discharge temperatures and contain very high concentrations of Na (75.1-101.0 mg/L), K (2.9-6.9 mg/L) and SiO2 (62.0-84.5 mg/L) and are rich in sulfates. The major ion composition of the CTGW suggests that these waters are in partial equilibrium with rocks at depth. The application of various alkali-ion geothermometers yields temperature estimates in the 88-198 °C range for the thermal reservoir. Multiple-mineral equilibrium calculations indicate a similar but narrower temperature range (from about 100 to 155 °C). These estimates for CTGW are significantly higher than the measured discharge temperatures. Considering the heat losses occurring during the ascent of the waters, one can infer the presence of a deeper (around 1.8 km) thermal reservoir in the Bugok area that could be developed for district heating or other direct applications of geothermal heat.

Original languageEnglish
Pages (from-to)448-469
Number of pages22
JournalGeothermics
Volume35
Issue number4
DOIs
Publication statusPublished - 2006 Aug 1

Fingerprint

geothermal system
Groundwater
groundwater
temperature
Temperature
Water
District heating
ion
thermal water
Ions
Chemical analysis
Heat losses
Aquifers
chemical analysis
evaluation
Hot Temperature
Statistical methods
statistical analysis
Minerals
Rocks

Keywords

  • Bugok
  • Geothermal potential
  • Geothermometer
  • South Korea
  • Spa
  • Sulfate-rich geothermal water

ASJC Scopus subject areas

  • Geology
  • Geotechnical Engineering and Engineering Geology
  • Renewable Energy, Sustainability and the Environment

Cite this

Park, S. S., Yun, S. T., Chae, G. T., Hutcheon, I., Koh, Y. K., So, C. S., & Choi, H. S. (2006). Temperature evaluation of the Bugok geothermal system, South Korea. Geothermics, 35(4), 448-469. https://doi.org/10.1016/j.geothermics.2006.07.002

Temperature evaluation of the Bugok geothermal system, South Korea. / Park, Seong Sook; Yun, Seong Taek; Chae, Gi Tak; Hutcheon, Ian; Koh, Yong Kwon; So, Chil Sup; Choi, Hyeon Su.

In: Geothermics, Vol. 35, No. 4, 01.08.2006, p. 448-469.

Research output: Contribution to journalArticle

Park, SS, Yun, ST, Chae, GT, Hutcheon, I, Koh, YK, So, CS & Choi, HS 2006, 'Temperature evaluation of the Bugok geothermal system, South Korea', Geothermics, vol. 35, no. 4, pp. 448-469. https://doi.org/10.1016/j.geothermics.2006.07.002
Park, Seong Sook ; Yun, Seong Taek ; Chae, Gi Tak ; Hutcheon, Ian ; Koh, Yong Kwon ; So, Chil Sup ; Choi, Hyeon Su. / Temperature evaluation of the Bugok geothermal system, South Korea. In: Geothermics. 2006 ; Vol. 35, No. 4. pp. 448-469.
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