Longitudinal Deformation Model and Parameter Analysis of Canal Lining under Nonuniform Frost Heave

Due to the unique hydrothermal environments, the frost heave failure of the concrete lining of water conveyance canals in cold regions is still frequent. The deformation of lining after frost heaving and the stress distribution calculated by the mechanical model can be the reference for the lining d...

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Main Authors: Pengfei He, Jianhua Dong, Xin Ren, Xiaolei Wu
Format: Article
Language:English
Published: Wiley 2021-01-01
Series:Advances in Materials Science and Engineering
Online Access:http://dx.doi.org/10.1155/2021/5519035
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author Pengfei He
Jianhua Dong
Xin Ren
Xiaolei Wu
author_facet Pengfei He
Jianhua Dong
Xin Ren
Xiaolei Wu
author_sort Pengfei He
collection DOAJ
description Due to the unique hydrothermal environments, the frost heave failure of the concrete lining of water conveyance canals in cold regions is still frequent. The deformation of lining after frost heaving and the stress distribution calculated by the mechanical model can be the reference for the lining design. However, previous research mainly focused on the mechanical model of the cross-section while having little attention for the longitudinal nonuniform frost heave damage. In this study, a mechanical model of the bottom lining under the nonuniform frost heave deformation is built based on the Euler–Bernoulli beam and the Pasternak foundation model, and the analytical solution of the model is obtained. The internal stress of the lining is analyzed during the changes of subgrade coefficient, shear rigidity, transition section length, and frost heave amount inside the model. Also, the calculation process is proved to be correct. The result shows that dangerous cross-sections are at the start and the end of the transition sections. The maximum normal stress and the tangential stress increase when the subgrade coefficient and the frost heave amount increase and the shear modulus and transition section length decrease. The frost heave amount in the frozen ground subgrade increases constantly, while the temperature decreases, but at the same time, the shear rigidity of the subgrade increases with it. The former increases the stress of lining, and the latter decreases it. Therefore, during the frost heaving process, the internal force of lining is coupled with these two elements. By analyzing a water conveyance canal lining under the nonuniform frost heave in the Xinjiang Tarim irrigation district, the maximum normal stress of the dangerous lining cross-section is greater than its tensile strength when the transition section length smaller than 7 m at the frost heave amount is 0.031 m.
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spelling doaj-art-63a796235e2e439688b6e51b01889dd12025-02-03T01:28:28ZengWileyAdvances in Materials Science and Engineering1687-84341687-84422021-01-01202110.1155/2021/55190355519035Longitudinal Deformation Model and Parameter Analysis of Canal Lining under Nonuniform Frost HeavePengfei He0Jianhua Dong1Xin Ren2Xiaolei Wu3School of Science, Lanzhou University of Technology, Lanzhou 730050, ChinaSchool of Civil Engineering, Lanzhou University of Technology, Lanzhou 730050, ChinaSchool of Civil Engineering, Lanzhou University of Technology, Lanzhou 730050, ChinaSchool of Civil Engineering, Lanzhou University of Technology, Lanzhou 730050, ChinaDue to the unique hydrothermal environments, the frost heave failure of the concrete lining of water conveyance canals in cold regions is still frequent. The deformation of lining after frost heaving and the stress distribution calculated by the mechanical model can be the reference for the lining design. However, previous research mainly focused on the mechanical model of the cross-section while having little attention for the longitudinal nonuniform frost heave damage. In this study, a mechanical model of the bottom lining under the nonuniform frost heave deformation is built based on the Euler–Bernoulli beam and the Pasternak foundation model, and the analytical solution of the model is obtained. The internal stress of the lining is analyzed during the changes of subgrade coefficient, shear rigidity, transition section length, and frost heave amount inside the model. Also, the calculation process is proved to be correct. The result shows that dangerous cross-sections are at the start and the end of the transition sections. The maximum normal stress and the tangential stress increase when the subgrade coefficient and the frost heave amount increase and the shear modulus and transition section length decrease. The frost heave amount in the frozen ground subgrade increases constantly, while the temperature decreases, but at the same time, the shear rigidity of the subgrade increases with it. The former increases the stress of lining, and the latter decreases it. Therefore, during the frost heaving process, the internal force of lining is coupled with these two elements. By analyzing a water conveyance canal lining under the nonuniform frost heave in the Xinjiang Tarim irrigation district, the maximum normal stress of the dangerous lining cross-section is greater than its tensile strength when the transition section length smaller than 7 m at the frost heave amount is 0.031 m.http://dx.doi.org/10.1155/2021/5519035
spellingShingle Pengfei He
Jianhua Dong
Xin Ren
Xiaolei Wu
Longitudinal Deformation Model and Parameter Analysis of Canal Lining under Nonuniform Frost Heave
Advances in Materials Science and Engineering
title Longitudinal Deformation Model and Parameter Analysis of Canal Lining under Nonuniform Frost Heave
title_full Longitudinal Deformation Model and Parameter Analysis of Canal Lining under Nonuniform Frost Heave
title_fullStr Longitudinal Deformation Model and Parameter Analysis of Canal Lining under Nonuniform Frost Heave
title_full_unstemmed Longitudinal Deformation Model and Parameter Analysis of Canal Lining under Nonuniform Frost Heave
title_short Longitudinal Deformation Model and Parameter Analysis of Canal Lining under Nonuniform Frost Heave
title_sort longitudinal deformation model and parameter analysis of canal lining under nonuniform frost heave
url http://dx.doi.org/10.1155/2021/5519035
work_keys_str_mv AT pengfeihe longitudinaldeformationmodelandparameteranalysisofcanalliningundernonuniformfrostheave
AT jianhuadong longitudinaldeformationmodelandparameteranalysisofcanalliningundernonuniformfrostheave
AT xinren longitudinaldeformationmodelandparameteranalysisofcanalliningundernonuniformfrostheave
AT xiaoleiwu longitudinaldeformationmodelandparameteranalysisofcanalliningundernonuniformfrostheave