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The Keban dam foundation on karstified limestone—A case history
Abstract The Keban dam on the Firat was erected on a limestone ridge deeply karstified mainly by hydrothermal activity. Extensive highly interconnected percolation paths resulted in and below the dam foundation which convey inpounded water below the 250 m deep grouted cut-off into Keban Creek and to sources downstream of the dam. The cut-off, the cavern discovered after filling the lake and its treatment, the leakages before and after remedial measures were achieved, are presented.
The Keban dam foundation on karstified limestone—A case history
Abstract The Keban dam on the Firat was erected on a limestone ridge deeply karstified mainly by hydrothermal activity. Extensive highly interconnected percolation paths resulted in and below the dam foundation which convey inpounded water below the 250 m deep grouted cut-off into Keban Creek and to sources downstream of the dam. The cut-off, the cavern discovered after filling the lake and its treatment, the leakages before and after remedial measures were achieved, are presented.
The Keban dam foundation on karstified limestone—A case history
Bozovic, A. (author) / Budanur, H. (author) / Nonveiller, E. (author) / Pavlin, B. (author)
1981
Article (Journal)
English
The Keban dam foundation on karstified limestone—A case history
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