Numerical Studies to Aid Interpretation of an Airborne VLF Resistivity Survey

Airborne resistivity surveys, which use the wavetilt phenomena of radiowaves, are used as a preliminary exploration technique to find suitable areas for either engineering investigations or geologic reconnaissance explorations. Survey results are usually presented as resistivity flight line profiles...

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Main Author: Arcone,Steven A
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1977
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA039904
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA039904
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author Arcone,Steven A
author2 COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
author_facet Arcone,Steven A
author_sort Arcone,Steven A
collection Defense Technical Information Center: DTIC Technical Reports database
description Airborne resistivity surveys, which use the wavetilt phenomena of radiowaves, are used as a preliminary exploration technique to find suitable areas for either engineering investigations or geologic reconnaissance explorations. Survey results are usually presented as resistivity flight line profiles or as contour maps from which the interpretation or site selection process must be initiated. To aid in this process and provide additional understanding of the correlation between data obtained from airborne and ground surveys, an analysis was performed to determine a very-low- frequency airborne system's response to modelled resistivity anomalies assumed to occur at the surface of an idealized flat earth. Some of the assumptions used to simplify the analysis were based on the results of past surveys. The influences of survey altitude, anomaly size, and average ground resistivity upon airborne resistivity patterns were analyzed. The results show that the average resistivity of a region plays an important role in suppressing large resistivity contrasts for anomalies of approximately 1 sq. km. area. Curves are presented to separate the effects of resistivity contrast and anomaly size, and two examples are given to demonstrate how these curves may be applied to the results of actual surveys. (Author)
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spelling ftdtic:ADA039904 2025-01-17T00:16:56+00:00 Numerical Studies to Aid Interpretation of an Airborne VLF Resistivity Survey Arcone,Steven A COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1977-04 text/html http://www.dtic.mil/docs/citations/ADA039904 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA039904 en eng http://www.dtic.mil/docs/citations/ADA039904 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Geology Geochemistry and Mineralogy Electricity and Magnetism *ELECTRICAL CONDUCTIVITY *SURVEYING(GEOGRAPHIC) ANOMALIES GROUND LEVEL AIRBORNE NUMERICAL ANALYSIS GRAVEL SAND SITE SELECTION MAPPING EARTH(PLANET) GROUND WAVES(ELECTROMAGNETIC) SKY WAVES ELECTROMAGNETIC WAVE REFLECTIONS VERY LOW FREQUENCY PERMAFROST ELECTRICAL GROUNDING PE62719A AST42 WU003 Text 1977 ftdtic 2016-02-20T16:18:16Z Airborne resistivity surveys, which use the wavetilt phenomena of radiowaves, are used as a preliminary exploration technique to find suitable areas for either engineering investigations or geologic reconnaissance explorations. Survey results are usually presented as resistivity flight line profiles or as contour maps from which the interpretation or site selection process must be initiated. To aid in this process and provide additional understanding of the correlation between data obtained from airborne and ground surveys, an analysis was performed to determine a very-low- frequency airborne system's response to modelled resistivity anomalies assumed to occur at the surface of an idealized flat earth. Some of the assumptions used to simplify the analysis were based on the results of past surveys. The influences of survey altitude, anomaly size, and average ground resistivity upon airborne resistivity patterns were analyzed. The results show that the average resistivity of a region plays an important role in suppressing large resistivity contrasts for anomalies of approximately 1 sq. km. area. Curves are presented to separate the effects of resistivity contrast and anomaly size, and two examples are given to demonstrate how these curves may be applied to the results of actual surveys. (Author) Text permafrost Defense Technical Information Center: DTIC Technical Reports database
spellingShingle Geology
Geochemistry and Mineralogy
Electricity and Magnetism
*ELECTRICAL CONDUCTIVITY
*SURVEYING(GEOGRAPHIC)
ANOMALIES
GROUND LEVEL
AIRBORNE
NUMERICAL ANALYSIS
GRAVEL
SAND
SITE SELECTION
MAPPING
EARTH(PLANET)
GROUND WAVES(ELECTROMAGNETIC)
SKY WAVES
ELECTROMAGNETIC WAVE REFLECTIONS
VERY LOW FREQUENCY
PERMAFROST
ELECTRICAL GROUNDING
PE62719A
AST42
WU003
Arcone,Steven A
Numerical Studies to Aid Interpretation of an Airborne VLF Resistivity Survey
title Numerical Studies to Aid Interpretation of an Airborne VLF Resistivity Survey
title_full Numerical Studies to Aid Interpretation of an Airborne VLF Resistivity Survey
title_fullStr Numerical Studies to Aid Interpretation of an Airborne VLF Resistivity Survey
title_full_unstemmed Numerical Studies to Aid Interpretation of an Airborne VLF Resistivity Survey
title_short Numerical Studies to Aid Interpretation of an Airborne VLF Resistivity Survey
title_sort numerical studies to aid interpretation of an airborne vlf resistivity survey
topic Geology
Geochemistry and Mineralogy
Electricity and Magnetism
*ELECTRICAL CONDUCTIVITY
*SURVEYING(GEOGRAPHIC)
ANOMALIES
GROUND LEVEL
AIRBORNE
NUMERICAL ANALYSIS
GRAVEL
SAND
SITE SELECTION
MAPPING
EARTH(PLANET)
GROUND WAVES(ELECTROMAGNETIC)
SKY WAVES
ELECTROMAGNETIC WAVE REFLECTIONS
VERY LOW FREQUENCY
PERMAFROST
ELECTRICAL GROUNDING
PE62719A
AST42
WU003
topic_facet Geology
Geochemistry and Mineralogy
Electricity and Magnetism
*ELECTRICAL CONDUCTIVITY
*SURVEYING(GEOGRAPHIC)
ANOMALIES
GROUND LEVEL
AIRBORNE
NUMERICAL ANALYSIS
GRAVEL
SAND
SITE SELECTION
MAPPING
EARTH(PLANET)
GROUND WAVES(ELECTROMAGNETIC)
SKY WAVES
ELECTROMAGNETIC WAVE REFLECTIONS
VERY LOW FREQUENCY
PERMAFROST
ELECTRICAL GROUNDING
PE62719A
AST42
WU003
url http://www.dtic.mil/docs/citations/ADA039904
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA039904