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...
Main Authors: | , |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1984
|
Subjects: | |
Online Access: | http://www.dtic.mil/docs/citations/ADA145006 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA145006 |
id |
ftdtic:ADA145006 |
---|---|
record_format |
openpolar |
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 |
_version_ |
1766398725314314240 |