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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Format: | Text |
Language: | English |
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1977
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Online Access: | http://www.dtic.mil/docs/citations/ADA039904 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA039904 |
_version_ | 1821682841421873152 |
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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) |
format | Text |
genre | permafrost |
genre_facet | permafrost |
id | ftdtic:ADA039904 |
institution | Open Polar |
language | English |
op_collection_id | ftdtic |
op_relation | http://www.dtic.mil/docs/citations/ADA039904 |
op_rights | APPROVED FOR PUBLIC RELEASE |
op_source | DTIC AND NTIS |
publishDate | 1977 |
record_format | openpolar |
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 |