Profiles of temperature, oxygen, and electrical conductivity were obtained for 3 sites in Sandy Lake on Oct 3, 2017, as shown below.
The depths for sites 1, 2 and 3 were 17.5, 10 and 5.5 m.
Profiles at Sites 1 and 2 were similar with a distinct surface layer in the top 7 m, and then continuous declines in temperature and oxygen, and increases in conductivity to the bottom. It’s likely that in the summer when surface water temperature want up to 25 degrees C or higher, there were distinct surface and deep layers (epilimnion and hypolimnion) with a thermal gradient between them (the metalimnion), and that on Oct 3, that 2 -layer systems was in the process of breaking down.Two features to note:
(i) there is a distinct gradient in conductivity (a measure of dissolved ions) in deeper layers;
(ii) for the deepest profile (Site 1), the oxygen content of the deeper layers is below guidelines for both warm water and cold water aquatic life.
View profile data in text tables
For some background info about stratification of temperate lakes, see Density Stratification at www.lakeaccess.org/