Author(s): Ya. L. Gotlib; F. F. Razzorenov; N. M. Sukolnikov; V. M. Zhidkikh
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Abstract: The characteristic features of the thermal behaviour of the deep reservoirs in Siberia, namely Bratsk and Krasnoyarsk Reservoirs, are considered. A thermal classification of impoundments according to their depth is outlined and a procedure for hydrothermal calculations is suggested. Data are given on the coefficient of both turbulent and convection-free (equivalent) heat conductivity of water derived from the observations of Bratsk Reservoir.
Year: 1972