A new model for capturing void ratio-dependent unfrozen water characteristics curves

A new unfrozen water characteristics curve (UWCC) model is proposed with explicit considerations of both capillarity and adsorption. Capillarity is considered to be dominant when the freezing of soil pore water occurs at higher temperatures, whereas the effects of adsorption are pronounced at lower...

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Published in:Computers and Geotechnics
Main Authors: Mu, Q. Y., Ng, C. W. W., Zhou, C., Zhou, G. G. D., Liao, H. J.
Format: Report
Language:English
Published: ELSEVIER SCI LTD 2018
Subjects:
Unfrozen water characteristics curve
Capillary water
Adsorbed water
Void ratio
HYDRAULIC CONDUCTIVITY
POROUS-MEDIA
FROZEN SOILS
FROST HEAVE
SUCTION
PERMAFROST
RETENTION
Computer Science
Engineering
Geology
Interdisciplinary Applications
Geological
Geosciences
Multidisciplinary
permafrost
Online Access:http://ir.imde.ac.cn/handle/131551/32308
https://doi.org/10.1016/j.compgeo.2018.04.019
id ftchinacadscimhe:oai:ir.imde.ac.cn:131551/32308
record_format openpolar
spelling ftchinacadscimhe:oai:ir.imde.ac.cn:131551/32308 2023-05-15T17:57:36+02:00 A new model for capturing void ratio-dependent unfrozen water characteristics curves Mu, Q. Y. Ng, C. W. W. Zhou, C. Zhou, G. G. D. Liao, H. J. 2018-09-01 http://ir.imde.ac.cn/handle/131551/32308 https://doi.org/10.1016/j.compgeo.2018.04.019 英语 eng ELSEVIER SCI LTD COMPUTERS AND GEOTECHNICS http://ir.imde.ac.cn/handle/131551/32308 doi:10.1016/j.compgeo.2018.04.019 Unfrozen water characteristics curve Capillary water Adsorbed water Void ratio HYDRAULIC CONDUCTIVITY POROUS-MEDIA FROZEN SOILS FROST HEAVE SUCTION PERMAFROST RETENTION Computer Science Engineering Geology Interdisciplinary Applications Geological Geosciences Multidisciplinary 期刊论文 2018 ftchinacadscimhe https://doi.org/10.1016/j.compgeo.2018.04.019 2022-12-19T18:22:56Z A new unfrozen water characteristics curve (UWCC) model is proposed with explicit considerations of both capillarity and adsorption. Capillarity is considered to be dominant when the freezing of soil pore water occurs at higher temperatures, whereas the effects of adsorption are pronounced at lower temperatures. The proposed model is applied to predict UWCCs of silt at different initial void ratios and clay over a wide range of temperatures. It was found that the new model can capture the effects of void ratio on the UWCC. Moreover, the new model can better predict the UWCC over a wide range of temperatures. Report permafrost IMHE OpenIR (Institute of Mountain Hazards and Environment, Chinese Academy of Sciences) Computers and Geotechnics 101 95 99
institution Open Polar
collection IMHE OpenIR (Institute of Mountain Hazards and Environment, Chinese Academy of Sciences)
op_collection_id ftchinacadscimhe
language English
topic Unfrozen water characteristics curve
Capillary water
Adsorbed water
Void ratio
HYDRAULIC CONDUCTIVITY
POROUS-MEDIA
FROZEN SOILS
FROST HEAVE
SUCTION
PERMAFROST
RETENTION
Computer Science
Engineering
Geology
Interdisciplinary Applications
Geological
Geosciences
Multidisciplinary
spellingShingle Unfrozen water characteristics curve
Capillary water
Adsorbed water
Void ratio
HYDRAULIC CONDUCTIVITY
POROUS-MEDIA
FROZEN SOILS
FROST HEAVE
SUCTION
PERMAFROST
RETENTION
Computer Science
Engineering
Geology
Interdisciplinary Applications
Geological
Geosciences
Multidisciplinary
Mu, Q. Y.
Ng, C. W. W.
Zhou, C.
Zhou, G. G. D.
Liao, H. J.
A new model for capturing void ratio-dependent unfrozen water characteristics curves
topic_facet Unfrozen water characteristics curve
Capillary water
Adsorbed water
Void ratio
HYDRAULIC CONDUCTIVITY
POROUS-MEDIA
FROZEN SOILS
FROST HEAVE
SUCTION
PERMAFROST
RETENTION
Computer Science
Engineering
Geology
Interdisciplinary Applications
Geological
Geosciences
Multidisciplinary
description A new unfrozen water characteristics curve (UWCC) model is proposed with explicit considerations of both capillarity and adsorption. Capillarity is considered to be dominant when the freezing of soil pore water occurs at higher temperatures, whereas the effects of adsorption are pronounced at lower temperatures. The proposed model is applied to predict UWCCs of silt at different initial void ratios and clay over a wide range of temperatures. It was found that the new model can capture the effects of void ratio on the UWCC. Moreover, the new model can better predict the UWCC over a wide range of temperatures.
format Report
author Mu, Q. Y.
Ng, C. W. W.
Zhou, C.
Zhou, G. G. D.
Liao, H. J.
author_facet Mu, Q. Y.
Ng, C. W. W.
Zhou, C.
Zhou, G. G. D.
Liao, H. J.
author_sort Mu, Q. Y.
title A new model for capturing void ratio-dependent unfrozen water characteristics curves
title_short A new model for capturing void ratio-dependent unfrozen water characteristics curves
title_full A new model for capturing void ratio-dependent unfrozen water characteristics curves
title_fullStr A new model for capturing void ratio-dependent unfrozen water characteristics curves
title_full_unstemmed A new model for capturing void ratio-dependent unfrozen water characteristics curves
title_sort new model for capturing void ratio-dependent unfrozen water characteristics curves
publisher ELSEVIER SCI LTD
publishDate 2018
url http://ir.imde.ac.cn/handle/131551/32308
https://doi.org/10.1016/j.compgeo.2018.04.019
genre permafrost
genre_facet permafrost
op_relation COMPUTERS AND GEOTECHNICS
http://ir.imde.ac.cn/handle/131551/32308
doi:10.1016/j.compgeo.2018.04.019
op_doi https://doi.org/10.1016/j.compgeo.2018.04.019
container_title Computers and Geotechnics
container_volume 101
container_start_page 95
op_container_end_page 99
_version_ 1766166066387484672

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