Electrical Conductivity-Based Estimation of Unfrozen Water Content in Saturated Saline Frozen Sand

The salinity of the pore solution is closely associated with the unfrozen water content and can be reflected by variation in electrical conductivity in frozen soils. However, the influence of salinity was not considered in the existing models for estimation of unfrozen water content based on electri...

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Main Authors: Zejin Lai, Xiaodong Zhao, Rui Tang, Jinhong Yang
Format: Article
Language:English
Published: Hindawi Limited 2021-01-01
Series:Advances in Civil Engineering
Online Access:http://dx.doi.org/10.1155/2021/8881304
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spelling doaj-621a272b945a4763843aac7ebb5510982021-02-15T12:52:53ZengHindawi LimitedAdvances in Civil Engineering1687-80861687-80942021-01-01202110.1155/2021/88813048881304Electrical Conductivity-Based Estimation of Unfrozen Water Content in Saturated Saline Frozen SandZejin Lai0Xiaodong Zhao1Rui Tang2Jinhong Yang3State Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou 221116, ChinaState Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou 221116, ChinaState Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou 221116, ChinaChina Coal Construction Group Limited Corporation, Beijing 102218, ChinaThe salinity of the pore solution is closely associated with the unfrozen water content and can be reflected by variation in electrical conductivity in frozen soils. However, the influence of salinity was not considered in the existing models for estimation of unfrozen water content based on electrical conductivity measurement, and a model considering the effect of salt content was therefore developed to estimate the change of unfrozen water content of saline sands with variation of salt content (0%, 0.2%, and 1%). The unfrozen water content and the electrical resistivity were measured by nuclear magnetic resonance (NRM) and using resistance test equipment under a temperature ranging from 25°C to −15°C, respectively. The results indicated that the model using a cementation exponent expressed by a piecewise function with respect to temperature can produce a reasonable estimation on the content of unfrozen water. There was an essential difference between nonsaline and saline frozen sands in the increase of electrical resistivity due to the different reduction rates of unfrozen water content. The variation of electrical resistivity in nonsaline sand was mainly caused by the decrease of free water when temperature was higher than the freezing point and adsorbed water when temperature was lower than the freezing point, whereas the reduction of free water in two stages was the main reason for the variation of electrical resistivity in saline sand. The results and data obtained provided a basis for further developing a novel approach to measure the unfrozen water content in the field.http://dx.doi.org/10.1155/2021/8881304
collection DOAJ
language English
format Article
sources DOAJ
author Zejin Lai
Xiaodong Zhao
Rui Tang
Jinhong Yang
spellingShingle Zejin Lai
Xiaodong Zhao
Rui Tang
Jinhong Yang
Electrical Conductivity-Based Estimation of Unfrozen Water Content in Saturated Saline Frozen Sand
Advances in Civil Engineering
author_facet Zejin Lai
Xiaodong Zhao
Rui Tang
Jinhong Yang
author_sort Zejin Lai
title Electrical Conductivity-Based Estimation of Unfrozen Water Content in Saturated Saline Frozen Sand
title_short Electrical Conductivity-Based Estimation of Unfrozen Water Content in Saturated Saline Frozen Sand
title_full Electrical Conductivity-Based Estimation of Unfrozen Water Content in Saturated Saline Frozen Sand
title_fullStr Electrical Conductivity-Based Estimation of Unfrozen Water Content in Saturated Saline Frozen Sand
title_full_unstemmed Electrical Conductivity-Based Estimation of Unfrozen Water Content in Saturated Saline Frozen Sand
title_sort electrical conductivity-based estimation of unfrozen water content in saturated saline frozen sand
publisher Hindawi Limited
series Advances in Civil Engineering
issn 1687-8086
1687-8094
publishDate 2021-01-01
description The salinity of the pore solution is closely associated with the unfrozen water content and can be reflected by variation in electrical conductivity in frozen soils. However, the influence of salinity was not considered in the existing models for estimation of unfrozen water content based on electrical conductivity measurement, and a model considering the effect of salt content was therefore developed to estimate the change of unfrozen water content of saline sands with variation of salt content (0%, 0.2%, and 1%). The unfrozen water content and the electrical resistivity were measured by nuclear magnetic resonance (NRM) and using resistance test equipment under a temperature ranging from 25°C to −15°C, respectively. The results indicated that the model using a cementation exponent expressed by a piecewise function with respect to temperature can produce a reasonable estimation on the content of unfrozen water. There was an essential difference between nonsaline and saline frozen sands in the increase of electrical resistivity due to the different reduction rates of unfrozen water content. The variation of electrical resistivity in nonsaline sand was mainly caused by the decrease of free water when temperature was higher than the freezing point and adsorbed water when temperature was lower than the freezing point, whereas the reduction of free water in two stages was the main reason for the variation of electrical resistivity in saline sand. The results and data obtained provided a basis for further developing a novel approach to measure the unfrozen water content in the field.
url http://dx.doi.org/10.1155/2021/8881304
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AT xiaodongzhao electricalconductivitybasedestimationofunfrozenwatercontentinsaturatedsalinefrozensand
AT ruitang electricalconductivitybasedestimationofunfrozenwatercontentinsaturatedsalinefrozensand
AT jinhongyang electricalconductivitybasedestimationofunfrozenwatercontentinsaturatedsalinefrozensand
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