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Transect 1 time-domain electromagnetic soundings to delineate saline groundwater in the Genesee valley-fill aquifer system, New York (2016-2017)

Dates

Publication Date
Start Date
2016-10-26
End Date
2017-11-16

Citation

White, E.A., Johnson, C.D., Williams, J.H., and Kappel, W.M., 2021, Time-domain electromagnetic soundings to delineate saline groundwater in the Genesee valley-fill aquifer system, New York (2016-2017): U.S. Geological Survey data release, https://doi.org/10.5066/P9VQOCRZ.

Summary

This folder contains the raw and processed TEM data and inverted soundings showing resistivity (in ohm-m) with depth for all survey sites that were part of transect 1. In October and November 2016-2017, transient electromagnetic (TEM) data, also called time domain electromagnetic (TDEM) surveys, were acquired at 120 locations in the Genesee Valley, Livingston County, in New York, in order to characterize the subsurface resistivity structure in support of a U.S. Geological Survey groundwater investigation. The TEM data were collected as part of a project to evaluate geophysical methods to characterize the valley-fill sediments, underlying bedrock, and salinity of the subsurface. TEM data were collected using an ABEM WalkTEM unit (acquisition [...]

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Attached Files

Click on title to download individual files attached to this item.

LVTDEM3.zip 1.05 MB application/zip
LVTDEM4.zip 1.04 MB application/zip
LVTDEM5.zip 1.05 MB application/zip
LVTDEM6.zip 917.33 KB application/zip
LVTDEM15.zip 1.23 MB application/zip
LVTDEM16.zip 1.26 MB application/zip
LVTDEM91.zip 1.28 MB application/zip
LVTDEM92.zip 1.09 MB application/zip
LVTDEM93.zip 1.77 MB application/zip

Purpose

Surface geophysical methods can provide information for the characterization of the subsurface structure of the earth for aquifer investigations. Transient electromagnetic induction (TEM) surveys (also called time domain electromagnetic (TDEM) surveys) provide resistivity soundings of the subsurface, which can be related to lithology and hydrogeology and be used to inform and/or constrain regional hydrogeological models.

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