Unfrozen water content in saline soils: results using time-domain reflectometry
The use of time-domain reflectometry (TDR) for determining the phase composition of saline permafrost from measurement of the apparent dielectric constant, K a , is examined.Combined TDR–dilatometry experiments were performed to assess whether the TDR method could be used on frozen soil samples with...
Published in: | Canadian Geotechnical Journal |
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Language: | English |
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Canadian Science Publishing
1985
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Online Access: | http://dx.doi.org/10.1139/t85-009 http://www.nrcresearchpress.com/doi/pdf/10.1139/t85-009 |
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crcansciencepubl:10.1139/t85-009 2024-09-15T18:29:57+00:00 Unfrozen water content in saline soils: results using time-domain reflectometry Patterson, D. E. Smith, M. W. 1985 http://dx.doi.org/10.1139/t85-009 http://www.nrcresearchpress.com/doi/pdf/10.1139/t85-009 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Geotechnical Journal volume 22, issue 1, page 95-101 ISSN 0008-3674 1208-6010 journal-article 1985 crcansciencepubl https://doi.org/10.1139/t85-009 2024-07-25T04:10:07Z The use of time-domain reflectometry (TDR) for determining the phase composition of saline permafrost from measurement of the apparent dielectric constant, K a , is examined.Combined TDR–dilatometry experiments were performed to assess whether the TDR method could be used on frozen soil samples with high pore water salinity. In general, unfrozen water content determinations by TDR were within ±0.025 cm 3 ∙cm −3 of those obtained by dilatometry, with no marked influence due to salinity. A novel probe design for use on saline core samples shows promise as a means for determining unfrozen water contents in the field. Article in Journal/Newspaper permafrost Canadian Science Publishing Canadian Geotechnical Journal 22 1 95 101 |
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Open Polar |
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Canadian Science Publishing |
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crcansciencepubl |
language |
English |
description |
The use of time-domain reflectometry (TDR) for determining the phase composition of saline permafrost from measurement of the apparent dielectric constant, K a , is examined.Combined TDR–dilatometry experiments were performed to assess whether the TDR method could be used on frozen soil samples with high pore water salinity. In general, unfrozen water content determinations by TDR were within ±0.025 cm 3 ∙cm −3 of those obtained by dilatometry, with no marked influence due to salinity. A novel probe design for use on saline core samples shows promise as a means for determining unfrozen water contents in the field. |
format |
Article in Journal/Newspaper |
author |
Patterson, D. E. Smith, M. W. |
spellingShingle |
Patterson, D. E. Smith, M. W. Unfrozen water content in saline soils: results using time-domain reflectometry |
author_facet |
Patterson, D. E. Smith, M. W. |
author_sort |
Patterson, D. E. |
title |
Unfrozen water content in saline soils: results using time-domain reflectometry |
title_short |
Unfrozen water content in saline soils: results using time-domain reflectometry |
title_full |
Unfrozen water content in saline soils: results using time-domain reflectometry |
title_fullStr |
Unfrozen water content in saline soils: results using time-domain reflectometry |
title_full_unstemmed |
Unfrozen water content in saline soils: results using time-domain reflectometry |
title_sort |
unfrozen water content in saline soils: results using time-domain reflectometry |
publisher |
Canadian Science Publishing |
publishDate |
1985 |
url |
http://dx.doi.org/10.1139/t85-009 http://www.nrcresearchpress.com/doi/pdf/10.1139/t85-009 |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Canadian Geotechnical Journal volume 22, issue 1, page 95-101 ISSN 0008-3674 1208-6010 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/t85-009 |
container_title |
Canadian Geotechnical Journal |
container_volume |
22 |
container_issue |
1 |
container_start_page |
95 |
op_container_end_page |
101 |
_version_ |
1810471443885981696 |