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Title: Assessment of Karst activity at construction sites using the electrical resistivity method (Greene and Jefferson Counties, Missouri)
Author (s): Anderson, Neil L.
Apel, Derek
Ismail, Ahmed
Department/Lab Affiliations: Geological Sciences & Engineering
Mining & Nuclear Engineering
Keywords: Electric resistivity method
Highway construction sites
Karst
Subject Terms: Roads--Design and construction.
Issue Date: 2006
Publisher: Missouri Department of Transportation MODOT
Citation: Anderson, Neil, Ahmed Ismail, and Derek Apel. “Assessment of Karst Activity at Highway Construction Sites using the Electrical Resistivity Method (Greene and Jefferson Counties, Missouri). ” Missouri Department of Transportation, 2006.
Abstract: Two-dimensional (2-D) electrical resistivity data were acquired across and in proximity to active sinkholes at two Missouri Department of Transportation (MoDOT) highway-construction sites. Construction site #1 is located in Greene County, Missouri; site #2 is located in Jefferson County, Missouri. Two relatively dense grids (“1A” and “1B”) of electrical resistivity data were acquired at Greene County site #1 as part of a geotechnical investigation of a proposed interchange. Several active sinkholes with exposed throat diameters on the order of 1.5 ft had been discovered during a routine visual inspection of the site, and the District Geologist decided that a geophysical investigation was warranted prior to routine boring. The primary objective of the electrical resistivity study was to determine if substantive air-filled karstic cavities were present in the subsurface. Secondary objectives were to estimate depth to bedrock and identify anomalous subsurface conditions that might compromise the integrity of the proposed intersection or complicate construction. The electrical resistivity data proved to be of significant utility. Substantive air-filled voids were not imaged on the resistivity profiles. A depth to bedrock structure contour map was generated for the site, and prominent clay-filled and apparently inactive karstic cavities were identified beneath segments of proposed new roadway. A relatively dense grid of electrical resistivity data was also acquired at Jefferson County site #2. These electrical resistivity data were acquired because a previously unmapped, oval-shaped, clay-filled, sinkhole (approximately 50 ft x 35 ft x 15 ft; length x width x height) near the centerline of the northbound lanes effectively “emptied” overnight after overlying soil had been stripped by earth moving equipment. The supervising geologist authorized the acquisition of the geophysical data in order to image the subsurface immediately beneath and adjacent to the sinkhole. The primary concern was that the sinkhole was underlain by a large air-filled cavity. The interpretation of the resistivity data indicated the reactivated sinkhole was not underlain by a substantive cavity. Rather, the soil in the sinkhole appears to have “flowed” into the subsurface through solution-widened system of joints that do not underlie the sinkhole and probably do not pose a significant risk in terms of catastrophic collapse under load.
Type: Article
text
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Publisher URL:
http://168.166.124.22/RDT/reports/Ri05049/or07003.pdf
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titleAssessment of Karst activity at construction sites using the electrical resistivity method (Greene and Jefferson Counties, Missouri)
contributor.authorAnderson, Neil L.
contributor.authorApel, Derek
contributor.authorIsmail, Ahmed
contributor.deptlabGeological Sciences & Engineering
contributor.deptlabMining & Nuclear Engineering
subjectElectric resistivity method
subjectHighway construction sites
subjectKarst
subject.LCSHRoads--Design and construction.
date.issued2006
publisherMissouri Department of Transportation MODOT
identifier.citationAnderson, Neil, Ahmed Ismail, and Derek Apel. “Assessment of Karst Activity at Highway Construction Sites using the Electrical Resistivity Method (Greene and Jefferson Counties, Missouri). ” Missouri Department of Transportation, 2006.
identifier.pub.URI
http://168.166.124.22/RDT/reports/Ri05049/or07003.pdf
description.abstractTwo-dimensional (2-D) electrical resistivity data were acquired across and in proximity to active sinkholes at two Missouri Department of Transportation (MoDOT) highway-construction sites. Construction site #1 is located in Greene County, Missouri; site #2 is located in Jefferson County, Missouri. Two relatively dense grids (“1A” and “1B”) of electrical resistivity data were acquired at Greene County site #1 as part of a geotechnical investigation of a proposed interchange. Several active sinkholes with exposed throat diameters on the order of 1.5 ft had been discovered during a routine visual inspection of the site, and the District Geologist decided that a geophysical investigation was warranted prior to routine boring. The primary objective of the electrical resistivity study was to determine if substantive air-filled karstic cavities were present in the subsurface. Secondary objectives were to estimate depth to bedrock and identify anomalous subsurface conditions that might compromise the integrity of the proposed intersection or complicate construction. The electrical resistivity data proved to be of significant utility. Substantive air-filled voids were not imaged on the resistivity profiles. A depth to bedrock structure contour map was generated for the site, and prominent clay-filled and apparently inactive karstic cavities were identified beneath segments of proposed new roadway. A relatively dense grid of electrical resistivity data was also acquired at Jefferson County site #2. These electrical resistivity data were acquired because a previously unmapped, oval-shaped, clay-filled, sinkhole (approximately 50 ft x 35 ft x 15 ft; length x width x height) near the centerline of the northbound lanes effectively “emptied” overnight after overlying soil had been stripped by earth moving equipment. The supervising geologist authorized the acquisition of the geophysical data in order to image the subsurface immediately beneath and adjacent to the sinkhole. The primary concern was that the sinkhole was underlain by a large air-filled cavity. The interpretation of the resistivity data indicated the reactivated sinkhole was not underlain by a substantive cavity. Rather, the soil in the sinkhole appears to have “flowed” into the subsurface through solution-widened system of joints that do not underlie the sinkhole and probably do not pose a significant risk in terms of catastrophic collapse under load.
typeArticle
type.DCMITypetext
rightsThis material is presented to ensure timely dissemination of scholarly and technical work. Copyright and all rights therein are retained by authors or by other copyright holders. All persons copying this information are expected to adhere to the terms and constraints invoked by each author's copyright. In most cases, these works may not be reposted without the explicit permission of the copyright holder.
rightsCopyright holder unclear, no full text.
rights.URI
http://www.modot.org/general/sitemap.htm
date.available2008-08-05T18:28:13Z
identifier.persist.URI
http://scholarsmine.mst.edu/post_prints/AssessmentOfKarstActivityAtConstructionSitesUs_09007dcc80540dc8.html