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Scientific Investigations Report 2009–5090

In cooperation with Texas A&M University AgriLife

Direct-Current Resistivity Profiling at the Pecos River Ecosystem Project Study Site near Mentone, Texas, 2006

By Andrew P. Teeple1, Alyson K. McDonald2, Jason D. Payne1, and Wade H. Kress1

1 U.S. Geological Survey, West Texas Program Office, San Angelo, Texas.
2 Texas AgriLife Extension Service, Texas A&M University, Fort Stockton, Texas.

Abstract

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The U.S. Geological Survey, in cooperation with Texas A&M University AgriLife, did a surface geophysical investigation at the Pecos River Ecosystem Project study site near Mentone in West Texas intended to determine shallow (to about 14 meters below the water [river] surface) subsurface composition (lithology) in and near treated (eradicated of all saltcedar) and control (untreated) riparian zone sites during June–August 2006. Land-based direct-current resistivity profiling was applied in a 240-meter section of the riverbank at the control site, and waterborne direct-current continuous resistivity profiling (CRP) was applied along a 2.279-kilometer reach of the river adjacent to both sites to collect shallow subsurface resistivity data. Inverse modeling was used to obtain a nonunique estimate of the true subsurface resistivity from apparent resistivity calculated from the field measurements. The land-based survey showed that the sub­surface at the control site generally is of relatively low resis­tivity down to about 4 meters below the water surface. Most of the section from about 4 to 10 meters below the water surface is of relatively high resistivity. The waterborne CRP surveys convey essentially the same electrical representation of the lithology at the control site to 10 meters below the water surface; but the CRP surveys show considerably lower resistivity than the land-based survey in the subsection from about 4 to 10 meters below the water surface. The CRP surveys along the 2.279-kilometer reach of the river adjacent to both the treated and control sites show the same relatively low resistivity zone from the riverbed to about 4 meters below the water surface evident at the control site. A slightly higher resistivity zone is observed from about 4 to 14 meters below the water surface along the upstream approximately one-half of the profile than along the downstream one-half. The variations in resistivity could not be matched to variations in lithology because sufficient rock samples were not available.

First posted June 16, 2009

For additional information contact:
Director, Texas Water Science Center
U.S. Geological Survey
8027 Exchange Drive
Austin, TX 78754-4733

http://tx.usgs.gov/

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Suggested citation:

Teeple, A.P., McDonald, A.K., Payne, J.D., and Kress, W.H., 2009, Direct-current resistivity profiling at the Pecos River Ecosystem Project study site near Mentone, Texas, 2006: U.S. Geological Survey Scientific Investigations Report 2009–5090, 11 p.



Contents

Abstract

Introduction

Direct-Current Resistivity Profiling

Summary

References

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