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Determination of the effect of temperature (Q10) on denitrification rates in sediments collected from a groundwater discharge site in Ashumet Pond on Cape Cod, MA

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Repert, D.A., Stoliker, D.L., Smith, R.L., Kent, D.B., and LeBlanc, D.R., 2020, Determination of the effect of temperature (Q10) on denitrification rates in sediments collected from a groundwater discharge site in Ashumet Pond on Cape Cod, MA: U.S. Geological Survey data release, https://doi.org/10.5066/P9CTT78O.

Summary

This data release presents results from a laboratory study designed to measure the effect of temperature on denitrification rates in sediments collected from 5- to 30-cm depth below the lake bottom, at a location where groundwater discharges to the lake. Sediment cores were collected June 25, 2014 from the West site (Fishermans Cove) in Ashumet Pond, Cape Cod, MA then shipped to Boulder, CO for laboratory experiments. Groundwater used for these experiments was collected from a well just upgradient of the sediment collection site. Denitrification rates were determined on sediment plus groundwater slurries maintained under anaerobic conditions and employing the acetylene block method. Nitrous oxide concentrations were measured several [...]

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DSCN2502.JPG
“Sediment collection site in Ashumet Pond. Photo by Richard L. Smith.”
thumbnail 1.27 MB image/jpeg
Ashumet Pond_data descriptions.csv 12.62 KB text/csv
Ashumet Pond_site information.csv 726 Bytes text/csv
Ashumet Pond_Denitrification Data.csv 2.21 KB text/csv
Ashumet Pond_DNF Q10 results.csv 357 Bytes text/csv

Purpose

The purpose of the data release is to provide a measure of denitrification rates that can be applied to various models to assess biogeochemical processes predominant in Ashumet Pond sediments subjected to discharge from a groundwater wastewater plume.
Sediment collection site in Ashumet Pond. Photo by Richard L. Smith.
Sediment collection site in Ashumet Pond. Photo by Richard L. Smith.

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DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9CTT78O

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