Airborne Resistivity Mapping of Permafrost Near Fairbanks, Alaska

Airborne resistivity methods using radio waves in three frequency bands were tested in the vicinity of Fairbanks, Alaska. The test sites were selected because much ground control is available for this area. The objectives of this study were to determine the ability of these methods to map permafrost...

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Bibliographic Details
Main Authors: Hoekstra, P., Sellmann, P. V., Delaney, A. J.
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH
Format: Text
Language:English
Published: 1974
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA000694
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA000694
id ftdtic:ADA000694
record_format openpolar
spelling ftdtic:ADA000694 2023-05-15T16:36:56+02:00 Airborne Resistivity Mapping of Permafrost Near Fairbanks, Alaska Hoekstra, P. Sellmann, P. V. Delaney, A. J. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH 1974-09 text/html http://www.dtic.mil/docs/citations/ADA000694 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA000694 en eng http://www.dtic.mil/docs/citations/ADA000694 Approved for public release; distribution is unlimited. DTIC AND NTIS Geology Geochemistry and Mineralogy Snow Ice and Permafrost *PERMAFROST *AERIAL PHOTOGRAPHY *GEOLOGICAL SURVEYS *SOIL SURVEYS *ALASKA SUBSURFACE ELECTRICAL RESISTANCE TOPOGRAPHIC MAPS FAIRBANKS(ALASKA) Text 1974 ftdtic 2016-02-22T16:33:51Z Airborne resistivity methods using radio waves in three frequency bands were tested in the vicinity of Fairbanks, Alaska. The test sites were selected because much ground control is available for this area. The objectives of this study were to determine the ability of these methods to map permafrost and other soils and to investigate the advantages of multifrequency mapping. The airborne resistivity data obtained in this study were contoured and the contour maps were compared with surficial geological maps and other ground truth data available. The following conclusions were reached: (1) in areas where the near- surface sediments are relatively uniform, VLF resistivity best delineates permafrost; and (2) in areas where surface sediments vary widely (e.g., recent flood plains), resistivity at all frequencies gives little information on permafrost conditions, but provides other important information, such as bedrock type, depth to bedrock, soil type and layering. Text Ice permafrost Alaska Defense Technical Information Center: DTIC Technical Reports database Fairbanks
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Geology
Geochemistry and Mineralogy
Snow
Ice and Permafrost
*PERMAFROST
*AERIAL PHOTOGRAPHY
*GEOLOGICAL SURVEYS
*SOIL SURVEYS
*ALASKA
SUBSURFACE
ELECTRICAL RESISTANCE
TOPOGRAPHIC MAPS
FAIRBANKS(ALASKA)
spellingShingle Geology
Geochemistry and Mineralogy
Snow
Ice and Permafrost
*PERMAFROST
*AERIAL PHOTOGRAPHY
*GEOLOGICAL SURVEYS
*SOIL SURVEYS
*ALASKA
SUBSURFACE
ELECTRICAL RESISTANCE
TOPOGRAPHIC MAPS
FAIRBANKS(ALASKA)
Hoekstra, P.
Sellmann, P. V.
Delaney, A. J.
Airborne Resistivity Mapping of Permafrost Near Fairbanks, Alaska
topic_facet Geology
Geochemistry and Mineralogy
Snow
Ice and Permafrost
*PERMAFROST
*AERIAL PHOTOGRAPHY
*GEOLOGICAL SURVEYS
*SOIL SURVEYS
*ALASKA
SUBSURFACE
ELECTRICAL RESISTANCE
TOPOGRAPHIC MAPS
FAIRBANKS(ALASKA)
description Airborne resistivity methods using radio waves in three frequency bands were tested in the vicinity of Fairbanks, Alaska. The test sites were selected because much ground control is available for this area. The objectives of this study were to determine the ability of these methods to map permafrost and other soils and to investigate the advantages of multifrequency mapping. The airborne resistivity data obtained in this study were contoured and the contour maps were compared with surficial geological maps and other ground truth data available. The following conclusions were reached: (1) in areas where the near- surface sediments are relatively uniform, VLF resistivity best delineates permafrost; and (2) in areas where surface sediments vary widely (e.g., recent flood plains), resistivity at all frequencies gives little information on permafrost conditions, but provides other important information, such as bedrock type, depth to bedrock, soil type and layering.
author2 COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH
format Text
author Hoekstra, P.
Sellmann, P. V.
Delaney, A. J.
author_facet Hoekstra, P.
Sellmann, P. V.
Delaney, A. J.
author_sort Hoekstra, P.
title Airborne Resistivity Mapping of Permafrost Near Fairbanks, Alaska
title_short Airborne Resistivity Mapping of Permafrost Near Fairbanks, Alaska
title_full Airborne Resistivity Mapping of Permafrost Near Fairbanks, Alaska
title_fullStr Airborne Resistivity Mapping of Permafrost Near Fairbanks, Alaska
title_full_unstemmed Airborne Resistivity Mapping of Permafrost Near Fairbanks, Alaska
title_sort airborne resistivity mapping of permafrost near fairbanks, alaska
publishDate 1974
url http://www.dtic.mil/docs/citations/ADA000694
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA000694
geographic Fairbanks
geographic_facet Fairbanks
genre Ice
permafrost
Alaska
genre_facet Ice
permafrost
Alaska
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA000694
op_rights Approved for public release; distribution is unlimited.
_version_ 1766027249005363200