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GRINDSTONE LAKE
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  Heat and Oxygen Budgets for Grindstone Lake

The RUSS data from Grindstone Lake is summarized to show the lake's average heat and oxygen content on each day. These are calculated by averaging the amount of heat and oxygen contained in each 1 meter thick layer of the lake over the course of the day and then adding them up from 0-3 m, 3-8 m and 8 meters to bottom. Therefore, the sum of the values for the 3 layers is the total amount in the whole lake on that day. - Limnologists say that these values are morphometrically, or volume-weighted.

Charts of heat and oxygen content are provided below. These are "stacked-area" charts - showing the contribution of each layer to the total. Below each chart you will find a more detailed description of the calculations involved for determining the heat content and oxygen content. You can also download the Excel spreadsheet (~80 Kbytes) containing this data and the charts for Grindstone Lake.

These data should be considered "provisional" until otherwise indicated. The data are undergoing several rounds of QA/QC review and some may be modified at a subsequent date. We chose to leave the data hose on full blast whenever possible to familiarize ourselves with the operation and maintenance requirements of the RUSS units and to generate real data for use in developing curricula and lesson plans. Data gaps were associated with various RUSS system upgrades and occasional gremlins.

HEAT CONTENT

Click on image for a larger version
Graph showing the total daily heat budget in Lake Independence -- calculated from RUSS measurement averages

The ability of a body of water to store heat is due primarily to the heat capacity of its water. Water has a specific heat of 1.0 calories per gram per degree Celsius.  This means that it takes 1 calorie of heat energy to raise the temperature of a gram of water by 1°C.  For example, using the data from Grindstone Lake on August 8, 1999 at 2 p.m. we can calculate the heat content of the upper layer, where

heat content = mass x specific heat x temperature (m * C * delta T )

= (grams) x (calories/gram/degree) x (degrees °C)

And since Mass of water = density x volume and density = 1 gram/milliliter which = 1 kg/Liter,

Heat content = volume x density x specific heat x temperature

(m * C * deltaT ) = (liters x kg/Liter) x (calories/gram/degree) x (degrees°C)

 

Layer

Volume
(x 105 m3)

Temperature
(average of layer)

Heat
(calories per layer)

0-1 meters
21.6
23.6
50.98 x 1012
1-2 meters
21.4
23.7
50.72 x 1012
2-3 meters
20.9
23.7
49.53 x 1012
Total (0-3 m)
63.9
 

150.9 x 1012

 

Large bodies of water can modify the weather in their region by their ability to store heat energy during warm periods and release it during cooler times. For instance in Duluth, Minnesota, the weather forecasts typically say "cooler by the lake" in summer because the average surface temperature of the lake is only about 10°C (50°F) then, and "warmer by the lake" in winter because its average temperature is about 4°C (39°F) which is much warmer than the air.

We can follow trends in the lake's "heat budget" by computing the heat content of its layers relative to their minimum values at 0°C. This is the subject of a specific Studying Heat Budgets Lesson and the Investigating Heat Budgets Lesson. Further discussion of the heat balances of lakes can be found in standard limnology and geosciences texts (e.g. Horne, A.J. and C.R. Goldman 1994. Limnology, 2nd edition. McGraw-hill, Inc.).

OXYGEN CONTENT

Click on image for a larger version
Graph showing the total daily dissolved oxygen content in Lake Independence -- calculated from RUSS measurement averages

We plot the dissolved oxygen content of the top (0-3 m), middle (3-8 m) and bottom (8 m - bottom) layers for use in a number of specific lab lessons and for generating hypotheses to explain changes in these values over time. As for heat, the total amount of oxygen in a layer is calculated as the sum of individual layer volumes multiplied by their respective dissolved oxygen concentrations. This yields a mass of oxygen. Using the data set again taken from 2 a.m. on August 8, 1999:

Note: remember that 1 mg/L = 1 g/m3

Layer Volume
(x 105 m3)
Dissolved O2
(mg/L average for layer)
Total O2 mass
(kilograms)
0-1 meters 21.6 13.1 17,280
1-2 meters 21.4 13.1 17,334
2-3 meters 20.9 13.0 17,138
Total (0-3m) 63.9   51,752

That's more than 51 metric tons of oxygen gas!

 

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http://www.waterontheweb.org/data/grindstone/trends/heat_oxygen.html
date last updated: Thursday June 17 2004