Determination of filtration losses from the Kronotsky HPP reservoir
Abstract
The Kronotskaya River is located on the eastern coast of Kamchatka, to the northeast of Petropavlovsk-Kamchatsky. It is about 45 km long, with a total drop of 375 m. On its way from Kronotsky Lake to Kronotsky Bay, the river crosses two areas that differ both in topography and geological structure: in its upper reaches, the Eastern Volcanic Region; in its lower reaches, the Kronotsky Coastal Plain.
Область исследования:
(Archived) Without section
Funding:
None
References
- Polubarinova-Kochina P. Ya. Theory of groundwater movement. Gostekhteoretizdat, 1952. (in Russian)
- Verigin N. N. On unsteady groundwater flow near reservoirs. DAN SSSR, new ser., vol. XVI, No. 6, 1949. (in Russian)
- Bindeman N. N. Hydrogeological calculations of groundwater backwater and filtration from reservoirs. Ugletekhizdat, 1951. (in Russian)
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