466 4TH CAN. PERMAFROST CONF. (1982) In situ frost heave testing using cold plates

The concept is introduced of a circular cold plate as a device for determining the frost heave char-acteristics or susceptibility of soils in situ. The advantages include (i) the ability to test the in situ, undisturbed soil and groundwater conditions, not subjected to possible sampling disturbance,...

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Main Authors: J. F. Nixon, J. R. Ellwood, W. A. Slusarchuk
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.534.4806
http://pubs.aina.ucalgary.ca/cpc/CPC4-466.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.534.4806 2023-05-15T17:57:55+02:00 466 4TH CAN. PERMAFROST CONF. (1982) In situ frost heave testing using cold plates J. F. Nixon J. R. Ellwood W. A. Slusarchuk The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.534.4806 http://pubs.aina.ucalgary.ca/cpc/CPC4-466.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.534.4806 http://pubs.aina.ucalgary.ca/cpc/CPC4-466.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/cpc/CPC4-466.pdf text ftciteseerx 2016-01-08T10:45:21Z The concept is introduced of a circular cold plate as a device for determining the frost heave char-acteristics or susceptibility of soils in situ. The advantages include (i) the ability to test the in situ, undisturbed soil and groundwater conditions, not subjected to possible sampling disturbance, and (ii) the ability to test a much larger volume of soil than is possible in standard laboratory tests. A parallel might be drawn with the use of the plate bearing test in conjunction with standard laboratory compres-sion tests in determining the stress-strain characteristics of soils in conventional geotechnical practice. The design, fabrication, installation, and instrumentation of several 0.76 m diameter cold plates are described. Instrumentation includes heave measurement rods, thermistors, and earth pressure cells. These plates have been successfully installed and operated in the south Yukon and Calgary. Results from these tests provide a bridging between small-scale laboratory testing and eventual frost heave design for large diameter, buried, chilled gas pipelines. Results from one of two cold plate installations at the pipeline research facility in Calgary are pre-sented in detail, and brief comparisons are made with the behaviour of full-size pipeline test sections. The in situ cold plate test provides valuable test data within a few months that are a valuable aid to long-term frost heave predictions. Text permafrost Yukon Unknown Sion ENVELOPE(13.758,13.758,66.844,66.844) Yukon
institution Open Polar
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language English
description The concept is introduced of a circular cold plate as a device for determining the frost heave char-acteristics or susceptibility of soils in situ. The advantages include (i) the ability to test the in situ, undisturbed soil and groundwater conditions, not subjected to possible sampling disturbance, and (ii) the ability to test a much larger volume of soil than is possible in standard laboratory tests. A parallel might be drawn with the use of the plate bearing test in conjunction with standard laboratory compres-sion tests in determining the stress-strain characteristics of soils in conventional geotechnical practice. The design, fabrication, installation, and instrumentation of several 0.76 m diameter cold plates are described. Instrumentation includes heave measurement rods, thermistors, and earth pressure cells. These plates have been successfully installed and operated in the south Yukon and Calgary. Results from these tests provide a bridging between small-scale laboratory testing and eventual frost heave design for large diameter, buried, chilled gas pipelines. Results from one of two cold plate installations at the pipeline research facility in Calgary are pre-sented in detail, and brief comparisons are made with the behaviour of full-size pipeline test sections. The in situ cold plate test provides valuable test data within a few months that are a valuable aid to long-term frost heave predictions.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author J. F. Nixon
J. R. Ellwood
W. A. Slusarchuk
spellingShingle J. F. Nixon
J. R. Ellwood
W. A. Slusarchuk
466 4TH CAN. PERMAFROST CONF. (1982) In situ frost heave testing using cold plates
author_facet J. F. Nixon
J. R. Ellwood
W. A. Slusarchuk
author_sort J. F. Nixon
title 466 4TH CAN. PERMAFROST CONF. (1982) In situ frost heave testing using cold plates
title_short 466 4TH CAN. PERMAFROST CONF. (1982) In situ frost heave testing using cold plates
title_full 466 4TH CAN. PERMAFROST CONF. (1982) In situ frost heave testing using cold plates
title_fullStr 466 4TH CAN. PERMAFROST CONF. (1982) In situ frost heave testing using cold plates
title_full_unstemmed 466 4TH CAN. PERMAFROST CONF. (1982) In situ frost heave testing using cold plates
title_sort 466 4th can. permafrost conf. (1982) in situ frost heave testing using cold plates
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.534.4806
http://pubs.aina.ucalgary.ca/cpc/CPC4-466.pdf
long_lat ENVELOPE(13.758,13.758,66.844,66.844)
geographic Sion
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genre permafrost
Yukon
genre_facet permafrost
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op_source http://pubs.aina.ucalgary.ca/cpc/CPC4-466.pdf
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http://pubs.aina.ucalgary.ca/cpc/CPC4-466.pdf
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