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渗流条件下滨海地层人工冻结多场耦合理论模型

朱紫义 任磊 高国耀 郭伟 任宇晓 冯守中 祝显鹏

岩土工程学报2024,Vol.46Issue(z2):171-176,6.
岩土工程学报2024,Vol.46Issue(z2):171-176,6.DOI:10.11779/CJGE2024S20031

渗流条件下滨海地层人工冻结多场耦合理论模型

Multi-field coupling theoretical model for artificial freezing of coastal soils under seepage

朱紫义 1任磊 2高国耀 1郭伟 1任宇晓 1冯守中 3祝显鹏1

作者信息

  • 1. 天津大学建筑工程学院,天津 300072
  • 2. 安徽滁宁高速公路股份有限公司,安徽 滁州 239000
  • 3. 滁州学院土木与建筑工程学院,安徽 滁州 239000
  • 折叠

摘要

Abstract

A hydro-salt-thermal-mechanical theoretical model for the influences of seepage flow on the artificial freezing process in sand-clay stratum is derived.The influence of momentum conservation of fluid during seepage process is considered by using the Navier-Stokes equation.The good agreement between the results from the theoretical model and laboratory tests in the literature verifies the accuracy of the proposed model.The parametric studies are conducted to investigate the influences of the seepage velocities on the spatial distributions of ice and salinity.It is found that the seepage weakens the freezing effects.With the seepage velocity increases from 0 to 10 m/d,at the left and right sides of the freezing pipe,the soil displacement decreases by 23.1%.The range of water freezing is reduced by 37.8%.The range of salt precipitation is reduced by 42.7%.The mutation position of the adsorbed salt in the upstream of the sand stratum moves by 52%downstream,and that in the downstream moves downstream by 32%.

关键词

人工冻结/冻结管/渗流/砂地层/多场耦合

Key words

artificial freezing/frozen pipe/seepage flow/sand stratum/multi-field coupling theory

分类

建筑与水利

引用本文复制引用

朱紫义,任磊,高国耀,郭伟,任宇晓,冯守中,祝显鹏..渗流条件下滨海地层人工冻结多场耦合理论模型[J].岩土工程学报,2024,46(z2):171-176,6.

基金项目

国家自然科学基金项目(52171273,52108335,52078336) (52171273,52108335,52078336)

天津市科技计划项目(20JCJQJC00220) (20JCJQJC00220)

岩土工程学报

OA北大核心CSTPCD

1000-4548

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