Lyell Collection

Quarterly Journal of Engineering Geology and Hydrogeology

Lyell Centre  |   Lyell Collection  |   Subscriptions   |   Geological Society  |   Email alerts  |   Online bookshop  |   Help


Keywords:
Author:
Advanced search>>
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow Request Permissions
Citing Articles
Right arrow Citing Articles via ISI Web of Science (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Lee, J.Y.
Right arrow Articles by Lee, K.K.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Quarterly Journal of Engineering Geology and Hydrogeology; 2004; v. 37; issue.3; p. 241-256;
DOI: 10.1144/1470-9236/03-050
© 2004 Geological Society of London

Original Article

Evaluation of groundwater chemistry affected by an abandoned metal mine within a dam construction site, South Korea

J.Y. Lee1, J.C. Choi2, M.J. Yi1, J.W. Kim1, J.Y. Cheon1 & K.K. Lee3

1 1GeoGreen21 Co., Ltd., Suite 519, Main Building, Research Park, Pongchon7-Dong, Seoul National University, Seoul 151-818, South Korea (e-mail: hydrolee@empal.com)
2 2Department of Environmental Geosciences, Pukyong National University, Busan 608-737, South Korea
3 3School of Earth and Environmental Sciences, Seoul National University, Seoul 151-747, South Korea

Groundwater chemistry in and around an abandoned metal mine within a large dam construction site was evaluated. For this purpose, a total of 50 groundwater samples were collected and chemically analysed for major ions and toxic metals. The pHs of the groundwaters were near neutral to slightly basic, with an apparent increase along the flow direction away from the mine waste dump. Higher values of electrical conductivity with a mean of 532 µS cm–1 were observed in the mine area. Dissolved oxygen concentrations over 5 mg l–1 clearly indicated an oxygenated groundwater environment. The high concentration of sulphate was derived from weathering and oxidation of sulphide minerals. Hydrochemistry of the groundwater samples is characterized by the relatively significant enrichment of Ca2+ and SO42–. Results of factor analysis also indicated that the dominant mechanisms or continuing processes affecting the distribution of the chemical parameters in the study area are various geochemical reactions including dissolution of sulphide and carbonate minerals, and removal of calcium and sulphate by dilution through mixing with Ca2+– and SO42–-poor groundwaters. In the mine area, substantial groundwater contamination by toxic metals including Zn, Al, Fe and Mn was observed. Most of the toxic metals decreased gradually or dramatically with distance from the mine, although some metals were also found in high concentrations in the downstream areas. Compared with the contamination levels of the surrounding farmland soils and stream sediments, the levels of contamination of groundwater by toxic metals were relatively low. The low concentrations are ascribed to the high pH and highly oxygenated conditions, which reduce toxic metal mobility. Significant groundwater contamination with toxic metals was strictly limited within the immediate vicinity of the mine waste dump but the ubiquitous distribution of the toxic metals with slightly elevated levels all over the study area may be attributed to the same geology and mineralogy as in the mine area.

Key Words: factor and cluster analyses • abandoned mine • sulphate • zinc • toxic metals • Korea