z-logo
Premium
Destratification and Thermal Inversion (Reservoir Turnover)
Author(s) -
Beer Charles R.
Publication year - 1977
Publication title -
opflow
Language(s) - English
Resource type - Journals
eISSN - 1551-8701
pISSN - 0149-8029
DOI - 10.1002/j.1551-8701.1977.tb01022.x
Subject(s) - geology , thermal stratification , environmental science , water circulation , bottom water , oceanography , thermocline , inlet
Water in reservoirs usually stratifies into three layers. For purposes of this article, the upper two layers are referred to as the circulation zone and the bottom layer will be known as the stagnation zone. Turnover of reservoir water occurs twice a year, in the winter and summer. Some of the results of the turnover can be offensive tastes and odors in the water. To avoid any sudden water quality changes, the reservoir can be artificially destratified by the addition of oxygen or air into the stagnation zone, or by pumping water from the stagnation zone into the circulation zone to keep the layers of water mixed.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here