Calculating Borehole Geometry from Standard Measurements of Borehole Inclinometry.

This report describes two new methods for computing borehole geometry from discrete measurements of borehole inclination (theta) and azimuth (alpha). In the first method theta and alpha are assumed to vary linearly with arc length. This results in an analytic model of the borehole that is continuous...

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Main Authors: Jezek,K C, Alley,R B
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH
Format: Text
Language:English
Published: 1984
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA145006
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA145006
id ftdtic:ADA145006
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spelling ftdtic:ADA145006 2023-05-15T16:03:05+02:00 Calculating Borehole Geometry from Standard Measurements of Borehole Inclinometry. Jezek,K C Alley,R B COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH 1984-06 text/html http://www.dtic.mil/docs/citations/ADA145006 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA145006 en eng http://www.dtic.mil/docs/citations/ADA145006 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Theoretical Mathematics *BOREHOLES MATHEMATICAL MODELS MEASUREMENT TRANSFORMATIONS(MATHEMATICS) APPROXIMATION(MATHEMATICS) SLOPE GEOMETRY AZIMUTH GREENLAND CALCULATORS ICE CAPS CARTESIAN COORDINATES Linear variation models Quadratic variation models Inclinometry data Text 1984 ftdtic 2016-02-20T23:09:06Z This report describes two new methods for computing borehole geometry from discrete measurements of borehole inclination (theta) and azimuth (alpha). In the first method theta and alpha are assumed to vary linearly with arc length. This results in an analytic model of the borehole that is continuous but not smooth. The second model, which takes theta and alpha to vary quadratically with arc length between three measuring points, improves the smoothness of the model but the analysis must be carried out numerically. These models were applied to the borehole inclinometry data collected at DYE-3, Greenland. The methods were found convenient to use and it is claimed that the results represent physically reasonable approximations to the borehole geometry. (Author) Text Dye 3 Dye-3 Greenland Ice permafrost Defense Technical Information Center: DTIC Technical Reports database Greenland
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
Theoretical Mathematics
*BOREHOLES
MATHEMATICAL MODELS
MEASUREMENT
TRANSFORMATIONS(MATHEMATICS)
APPROXIMATION(MATHEMATICS)
SLOPE
GEOMETRY
AZIMUTH
GREENLAND
CALCULATORS
ICE CAPS
CARTESIAN COORDINATES
Linear variation models
Quadratic variation models
Inclinometry data
spellingShingle Snow
Ice and Permafrost
Theoretical Mathematics
*BOREHOLES
MATHEMATICAL MODELS
MEASUREMENT
TRANSFORMATIONS(MATHEMATICS)
APPROXIMATION(MATHEMATICS)
SLOPE
GEOMETRY
AZIMUTH
GREENLAND
CALCULATORS
ICE CAPS
CARTESIAN COORDINATES
Linear variation models
Quadratic variation models
Inclinometry data
Jezek,K C
Alley,R B
Calculating Borehole Geometry from Standard Measurements of Borehole Inclinometry.
topic_facet Snow
Ice and Permafrost
Theoretical Mathematics
*BOREHOLES
MATHEMATICAL MODELS
MEASUREMENT
TRANSFORMATIONS(MATHEMATICS)
APPROXIMATION(MATHEMATICS)
SLOPE
GEOMETRY
AZIMUTH
GREENLAND
CALCULATORS
ICE CAPS
CARTESIAN COORDINATES
Linear variation models
Quadratic variation models
Inclinometry data
description This report describes two new methods for computing borehole geometry from discrete measurements of borehole inclination (theta) and azimuth (alpha). In the first method theta and alpha are assumed to vary linearly with arc length. This results in an analytic model of the borehole that is continuous but not smooth. The second model, which takes theta and alpha to vary quadratically with arc length between three measuring points, improves the smoothness of the model but the analysis must be carried out numerically. These models were applied to the borehole inclinometry data collected at DYE-3, Greenland. The methods were found convenient to use and it is claimed that the results represent physically reasonable approximations to the borehole geometry. (Author)
author2 COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH
format Text
author Jezek,K C
Alley,R B
author_facet Jezek,K C
Alley,R B
author_sort Jezek,K C
title Calculating Borehole Geometry from Standard Measurements of Borehole Inclinometry.
title_short Calculating Borehole Geometry from Standard Measurements of Borehole Inclinometry.
title_full Calculating Borehole Geometry from Standard Measurements of Borehole Inclinometry.
title_fullStr Calculating Borehole Geometry from Standard Measurements of Borehole Inclinometry.
title_full_unstemmed Calculating Borehole Geometry from Standard Measurements of Borehole Inclinometry.
title_sort calculating borehole geometry from standard measurements of borehole inclinometry.
publishDate 1984
url http://www.dtic.mil/docs/citations/ADA145006
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA145006
geographic Greenland
geographic_facet Greenland
genre Dye 3
Dye-3
Greenland
Ice
permafrost
genre_facet Dye 3
Dye-3
Greenland
Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA145006
op_rights APPROVED FOR PUBLIC RELEASE
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