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- W2090977105 abstract "Results of limnological recordings made during 1967 on Lake Kariba are described. Kariba is monomictic, mesotrophic, and has five defined basins, each of which exhibits its own individuality. The two upstream basins are riverine; they are flushed out in May by the Zambezi River floods and thereby assume turnover characteristics earlier than the other three basins, which are truly lacustrine with temperature-induced turnover. Great amplitude of variation in water chemistry exists relating to the basin locality, biotope (river, estuary, cleared area, open water), time of year (turnover winter/summer), and depth. Generally, values of dissolved oxygen, conductivity, alkalinity, and pH fall from surface to bottom. When H2S is present, alkalinity and conductivity values increase. A chemocline follows the profile of the thermocline. Occasionally density currents occur at depth, particularly after the first seasonal floods. Transparency decreases toward the head of the lake and in all areas decreases after turnover. The source of H2S is the Salvinia-infested rivers. Dissolved oxygen in the hypolimnion is depleted 4 to 5 months after turnover. The hydrobiological effects of Salvinia are discussed, and the influence of the bottom topography is described." @default.
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- W2090977105 date "1970-09-01" @default.
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- W2090977105 title "LIMNOLOGICAL OBSERVATIONS ON LAKE KARIBA DURING 1967 WITH EMPHASIS ON SOME SPECIAL FEATURES1" @default.
- W2090977105 doi "https://doi.org/10.4319/lo.1970.15.5.0776" @default.
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