Determination of the effect of temperature (Q10) on rates of oxygen consumption in surface sediments collected from Ashumet Pond on Cape Cod, MA (2016)
Dates
Publication Date
2020-01-09
Start Date
2016-06-08
End Date
2016-07-13
Citation
Repert, D.A., Smith, R.L., and LeBlanc, D.R., 2020, Determination of the effect of temperature (Q10) on rates of oxygen consumption in surface sediments collected from Ashumet Pond on Cape Cod, MA (2016): U.S. Geological Survey data release, https://doi.org/10.5066/P9SPP01Q.
Summary
This data release presents results from a laboratory study designed to measure the effect of temperature on rates of oxygen consumption within lake-bottom surface sediments at 0- to 5-cm depth. Sediment and lake water samples were collected June 8, 2016 from the South site in Ashumet Pond, Cape Cod, MA, where lake water recharges to the aquifer. Samples were shipped to Boulder, CO for laboratory experiments. Oxygen concentrations were measured over the course of several days or weeks on serum bottles containing either sieved sediment (<2 mm) combined with filtered lake water, unfiltered lake water only, or deionized water (DIW) only at 3 different incubation temperatures (5, 15, 24 degrees Celsius). The oxygen consumption rates of [...]
Summary
This data release presents results from a laboratory study designed to measure the effect of temperature on rates of oxygen consumption within lake-bottom surface sediments at 0- to 5-cm depth. Sediment and lake water samples were collected June 8, 2016 from the South site in Ashumet Pond, Cape Cod, MA, where lake water recharges to the aquifer. Samples were shipped to Boulder, CO for laboratory experiments. Oxygen concentrations were measured over the course of several days or weeks on serum bottles containing either sieved sediment (<2 mm) combined with filtered lake water, unfiltered lake water only, or deionized water (DIW) only at 3 different incubation temperatures (5, 15, 24 degrees Celsius). The oxygen consumption rates of the sediment plus filtered lake water samples were corrected using the DIW samples and the Q10 temperature coefficient was calculated using the corrected rates. The Q10 for the sediment at Ashumet Pond was calculated to be 2.47, meaning that the rate of oxygen consumption increased by a factor of 2.47 for every 10 degrees of temperature increase.
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Q10 data release_v2.xml Original FGDC Metadata
View
43.87 KB
application/fgdc+xml
DSCN2792.JPG “Sediment Core Collection at Ashumet Pond June 2016. Picture by Ariel Reed.”
1.15 MB
image/jpeg
Ashumet Pond_data descriptions_v2.csv
15.69 KB
text/csv
Ashumet Pond_site information_v2.csv
837 Bytes
text/csv
Ashumet Pond_Oxygen Consumption Data_v2.csv
8.28 KB
text/csv
Ashumet Pond_Q10 results_v2.csv
731 Bytes
text/csv
Purpose
The purpose of the data release is to provide a measure of oxygen consumption rates that can be applied to various models to assess biogeochemical processes predominant in Ashumet Pond surface sediments.
Preview Image
Sediment Core Collection at Ashumet Pond June 2016. Picture by Ariel Reed.