Особливості фізико-хімічних властивостей солотвинських соляних озер

Abstract

The results of the investigation monitoring of the Solotvino Salt Lakes from 1997 to 2001 are presented. It is demonstrated that the salt lake water mineralization is increased with the depth. The study of the temperature dependence of the salt lake water on the depth contributed to determine the anomalies which lie in the presence of the salt water layer with the higher temperature. Moreover the location of this layer depends on the season of the year, i,e. the outside conditions. The influence of the ecological factors on the lake water layer properties was analyzed. The analysis of the temperature anomaly permitted to analyze the convectional floods inside the lake.