Frost heave – pipeline interaction using continuum mechanics

As a chilled pipeline crosses a transition from frozen to unfrozen ground or shallow permafrost, a differential frost heave problem may develop causing strains in the pipe. Soil–structure interaction models that are currently available to handle this problem concentrate on the pipe as the dominant s...

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Published in:Canadian Geotechnical Journal
Main Authors: Nixon, J. F., Morgenstern, N. R., Reesor, S. N.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1983
Subjects:
Online Access:http://dx.doi.org/10.1139/t83-029
http://www.nrcresearchpress.com/doi/pdf/10.1139/t83-029
id crcansciencepubl:10.1139/t83-029
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spelling crcansciencepubl:10.1139/t83-029 2023-12-17T10:48:34+01:00 Frost heave – pipeline interaction using continuum mechanics Nixon, J. F. Morgenstern, N. R. Reesor, S. N. 1983 http://dx.doi.org/10.1139/t83-029 http://www.nrcresearchpress.com/doi/pdf/10.1139/t83-029 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Geotechnical Journal volume 20, issue 2, page 251-261 ISSN 0008-3674 1208-6010 Civil and Structural Engineering Geotechnical Engineering and Engineering Geology journal-article 1983 crcansciencepubl https://doi.org/10.1139/t83-029 2023-11-19T13:39:16Z As a chilled pipeline crosses a transition from frozen to unfrozen ground or shallow permafrost, a differential frost heave problem may develop causing strains in the pipe. Soil–structure interaction models that are currently available to handle this problem concentrate on the pipe as the dominant structural member and represent the soil mass as a series of unconnected springs. This paper considers the soil to be an elastic or nonlinear viscous continuum and imposes a nonlinear boundary condition to represent the frost heaving soil and the dependence of frost heave on applied pressure. The pipe is assumed to be a completely passive structural member and the soil strains at the pipe elevations are studied. The dependence of the maximum pipe strains on the length of the heaving section and on the thickness of frozen ground beneath the pipe have been established for a typical set of soil and frost heaving conditions. It is found that, for the conditions studied, when the thickness of shallow permafrost or frozen soil is greater than about 7–8 m, the strains that a flexible pipe experiences are less than the strain criteria currently in use on many pipeline projects. Keywords: frost heave, pipeline, interaction, stress analysis, finite elements, continuum mechanics, thermo-elasticity. Article in Journal/Newspaper permafrost Canadian Science Publishing (via Crossref) Canadian Geotechnical Journal 20 2 251 261
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic Civil and Structural Engineering
Geotechnical Engineering and Engineering Geology
spellingShingle Civil and Structural Engineering
Geotechnical Engineering and Engineering Geology
Nixon, J. F.
Morgenstern, N. R.
Reesor, S. N.
Frost heave – pipeline interaction using continuum mechanics
topic_facet Civil and Structural Engineering
Geotechnical Engineering and Engineering Geology
description As a chilled pipeline crosses a transition from frozen to unfrozen ground or shallow permafrost, a differential frost heave problem may develop causing strains in the pipe. Soil–structure interaction models that are currently available to handle this problem concentrate on the pipe as the dominant structural member and represent the soil mass as a series of unconnected springs. This paper considers the soil to be an elastic or nonlinear viscous continuum and imposes a nonlinear boundary condition to represent the frost heaving soil and the dependence of frost heave on applied pressure. The pipe is assumed to be a completely passive structural member and the soil strains at the pipe elevations are studied. The dependence of the maximum pipe strains on the length of the heaving section and on the thickness of frozen ground beneath the pipe have been established for a typical set of soil and frost heaving conditions. It is found that, for the conditions studied, when the thickness of shallow permafrost or frozen soil is greater than about 7–8 m, the strains that a flexible pipe experiences are less than the strain criteria currently in use on many pipeline projects. Keywords: frost heave, pipeline, interaction, stress analysis, finite elements, continuum mechanics, thermo-elasticity.
format Article in Journal/Newspaper
author Nixon, J. F.
Morgenstern, N. R.
Reesor, S. N.
author_facet Nixon, J. F.
Morgenstern, N. R.
Reesor, S. N.
author_sort Nixon, J. F.
title Frost heave – pipeline interaction using continuum mechanics
title_short Frost heave – pipeline interaction using continuum mechanics
title_full Frost heave – pipeline interaction using continuum mechanics
title_fullStr Frost heave – pipeline interaction using continuum mechanics
title_full_unstemmed Frost heave – pipeline interaction using continuum mechanics
title_sort frost heave – pipeline interaction using continuum mechanics
publisher Canadian Science Publishing
publishDate 1983
url http://dx.doi.org/10.1139/t83-029
http://www.nrcresearchpress.com/doi/pdf/10.1139/t83-029
genre permafrost
genre_facet permafrost
op_source Canadian Geotechnical Journal
volume 20, issue 2, page 251-261
ISSN 0008-3674 1208-6010
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/t83-029
container_title Canadian Geotechnical Journal
container_volume 20
container_issue 2
container_start_page 251
op_container_end_page 261
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