Page Updated, more profile data added on Dec 13, 2020
For some background info on lake stratification, see this page.
Vertical profiles of temperature, oxygen, electrical conductivity, and pH were obtained at 3 locations on Oct 3, 2017, at one location (at precisely the deepest spot in the lake) on Sep 30, 2019 and on Apr 19, 2010. View Methods.
1. Oct 3, 2017
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).
(ii) For the deepest profile (Site 1), the oxygen content of the deeper layers (2.25 mg/L) is below guidelines for both salmonids and more generally, aquatic life. The 2017 value is less than half of the value obtained on Aug 30 1971 when the lake was still in the oligotrophic range (that’s the only comparable historical data for Sandy Lake).
View 2017 data file
2. Sep 30, 2019
These data posted Dec 13, 2020
Using the same equipment and procedure, Ed Glover obtained these profiles at the deepest point in the lake on Sep 30, 2019:
View 2019 data file
These observations were at a deeper point than sampled at nearby site 1 in 2017.
Distinct stratification with a hypolimnion, thermocline (metalimnion) and hypolimnion are evident.
The overall patterns are similar to those for site #1 above with low O2 and saltier water in the deepest layer (hypolimnion).
The deepest water in 2019 was warmer (7.3 degrees at 17 meters; 7.2 at 21 m) than in 2017 (5.7 at 17.5 meters degrees, the deepest point) and less salty (195 uS/cm at 21 m in 2019 compared to 246 uS/cm at 17.5 m in 2017). Surface temperatures and EC values were more similar (17.1 degrees/169 uS/cm in 2017; 16.9 degrees, 159 uS/cm in 2019).
It also appears that the profile on Sep 30, 2019 was still in its summer, full stratification mode, while on Oct 3, 2017 it appeared to be breaking up.
Without measurements of chloride in the water, it cannot be said with absolute confidence that the higher EC in the hypolimnion compared to the epilimnion is entirely due to road salts. Mobilization of iron and manganese (and phosphorus) under anoxia is another possibility, however, the hypolimnion oxygen values on these two profiles, while low for salmonids, were still above 2 mg/L, the value generally cited for “hypoxic” water (e.g., from Nurnberg 2004: “2 mg L–1 measured by a DO probe about 1 m above the sediment usually coincides with anoxic conditions at the sediment surfaces located at that depth”. Such mobilization results in EC increases up to 30-40 uS/cm (e.g., Mortimer, 1942; OME 1993); the difference top to bottom in 2017 was about 80 uS/cm, in 2019 about 40 uS/cm.
Some pertinent chemical data are available for 1998:
Samples taken at the surface, in the thermocline at 7 m depth, and at the bottom (18 m) on Sep 2, 1998 illustrate differences in EC and chloride, with equivalent differences between the surface and bottom for both EC and chloride: 34/29*125=146.6, i.e. changes in chloride appear to account for the differences in Electrical Conductivity. At the same time, there is some evidence for some mobilization of iron, manganese and phosphorous in the hypolimnion at an oxygen concentration of 3 mg/Lin early September.
3. Apr 19, 2021
(David P and Ed G.) The profiles for temperature, oxygen and EC indicate that a normal spring turnover had occurred and the water column was well and uniformly oxygenated down to 19 m. A thermocline had been formed at 13-17 m (temperature 7 degrees dropping to 5 degrees). It was difficult to tell precisely when the probe was at the bottom. Separately, we lowered a bucket with rocks down; the bottom was at approx. 20 m – so the deepest probe sample (21 m) was likely within soft sediment. There was a sharp increase in EC between 20 m ( 172 uS/cm – compared to values of 169-171 uS/cm for 0 to 19 m ) and 21 m (193 uS/cm); oxygen declined from 86.3 to 78.5 mg/L (compared to values of 96 to 89 mg/L, surface to 19 m depth). View Profile19Apr2021.xlsx
Quantified Hypoxia and Anoxia in Lakes and Reservoirs
Gertrud K. Nürnberg. 2004 The Scientific World Journal 4, 42–54
The Exchange of Dissolved Substances between Mud and Water in Lakes
Clifford H. Mortimer 1942. Journal of Ecology 30: 147-201
Chesley Lake 1991 Water Quality Assessment
Ontario Ministry of Environment, 1993