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Frequency Domain Electromagnetic (FDEM) Geophysical Data Collected near Lake Placid, NY

Dates

Publication Date
Start Date
2019-07-22
End Date
2022-10-20

Citation

Terry, N.C., Anderson, A., Woda, J.C., Baldwin, A.L., Lucia, I.P., and Williams, J.H., 2024, Frequency domain electromagnetic (FDEM) geophysical data collected near Lake Placid, NY, U.S. Geological Survey data release, https://doi.org/10.5066/P9QES2KJ.

Summary

This data release contains frequency domain electromagnetic (FDEM) data collected during discrete times between July 2019 to October 2022 near Lake Placid, NY as part of a multi-method effort to monitor the effects of different road salt treatments on groundwater and the surrounding surface water (West Branch Ausable River). The FDEM instrument used was a Geophex GEM-2; a broadband sensor that measures the bulk conductivity and magnetic susceptibility of the subsurface down to approximately 5 meters (16.4 feet) depth. The instrument is hand carried by a single operator and data are collected at walking speeds. Data were repeatedly collected during each campaign at the three sites nicknamed for the planned road salt treatment at the [...]

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Attached Files

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lp_thumb.JPG thumbnail 2.27 MB image/jpeg
data_dictionary_FDEM.csv 1.72 KB text/csv
Processed.zip 210.77 MB application/zip
Raw.zip 253.53 MB application/zip
README.txt 2.35 KB text/plain

Purpose

Loss of traction due to road ice during the winter months leads to serious automobile accidents every year. Methods to melt road ice in below freezing conditions are necessary for driver safety in areas where ice is prone to form. Salts applied to roads are highly effective at melting dangerous ice but may have negative impacts on the surrounding environment, including waterways, and may persist in groundwater for a long time after initial application. These data are part of an assessment to identify how different road salt treatments impact the groundwater and surface water salinity of surrounding environments. FDEM is sensitive to bulk electrical conductivity changes in the subsurface and can be collected over large (e.g., 100s to 1000s of meters) spatial areas quickly and efficiently (within days). Though FDEM data can be compromised by local infrastructure and other factors controlling bulk subsurface electrical conductivity (e.g., soil type, saturation, and temperature), large changes in groundwater salinity resulting from road salt treatments may impart significant and measurable changes to bulk conductivity.

Additional Information

Identifiers

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DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9QES2KJ

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