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Fallout-radionuclide activity in samples collected from fine-grained, streambed sediment in the Black Creek, Indiana stream-channel network, 2019

Dates

Publication Date
Start Date
2019-07-22
End Date
2019-07-25

Citation

Karwan, D.L., and Williamson, T.N., 2023, Fallout-radionuclide activity in samples collected from fine-grained, streambed sediment in the Black Creek, Indiana stream-channel network, 2019: U.S. Geological Survey data release, https://doi.org/10.5066/P9L5P7BZ.

Summary

These data provide beryllium-7 (7Be) and excess lead-210 (210Pbxs) activity for fine-grained, mobile, streambed sediment in the Black Creek, Indiana (IN) stream-channel network. This basin is monitored in cooperation with the Great Lakes Restoration Initiative (GLRI). During the period July 22-25, 2019 (summer low flow), the thickness and spatial extent of soft, mobile, fine-grained (mainly silt and clay) streambed sediment was inventoried and sampled along 150-meter (m) transects. A combination of stream corridor land-use distribution, valley type, channel slope, stream order (Strahler, 1957), and ecoregion (Omernik and Griffith, 2014) was used to select 30 rapid geomorphic assessment reaches using methods of Fitzpatrick and others [...]

Contacts

Point of Contact :
Tanja N Williamson
Originator :
Diana L Karwan, Tanja N Williamson
Metadata Contact :
Tanja N Williamson
Publisher :
U.S. Geological Survey
Distributor :
U.S. Geological Survey - ScienceBase
SDC Data Owner :
Ohio-Kentucky-Indiana Water Science Center
USGS Mission Area :
Water Resources

Attached Files

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FRN_blk_2019.csv 467 Bytes text/csv

Purpose

Fallout radionuclides, including 7Be and 210Pbxs, are primarily delivered during rain events to exposed surface soil or sediment. Their different half-lives (7Be: 53.3 days, 210Pb: 22.3 years) provide a mechanism to differentiate material that has moved within weeks to months versus that moving on the order of decades (Matisoff and others, 2005). Excess 210Pb accounts for the 210Pb that exceeds that from Radium-226 (226Ra) decay and is attributed to atmospheric deposition of the 210Pb decay product of Radon-222 (222Rn), which diffused from the subsurface to the atmosphere.

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9L5P7BZ

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