在恒温和动态负载下,研究冰层下层的热液过程
Jinbang Zhai1, Ze Zhang2, Linzhen Yang3,4,5
1School of Transportation/Ministry of Education Observation and Research Station of Permafrost Geo-Environment System in Northeast China/Permafrost Institute, Northeast Forestry University, Harbin, 150040, People's Republic of China.
Scientific reports
|February 17, 2024
概括
动态负载对永久土地区的道路地下水热状态产生重大影响. 控制土壤温度至关重要,以防止冰层下层积累水分.
科学领域:
- 地质技术工程 地质技术工程
- 永久土科学 永久土科学
- 土木工程 土木工程是指土木工程.
背景情况:
- 岛屿永久土地区的道路分层含有冰层,使它们易受环境变化的影响.
- 了解这些次级的热水行为对于基础设施的稳定性至关重要.
研究的目的:
- 在恒温和动态负载下研究冰层下层土壤的热水反应.
- 分析动态负载对温度,湿度和孔水压力分布的影响.
主要方法:
- 在含有冰层的地下土壤样本上进行了热水学研究.
- 应用恒温条件和动态负载来模拟环境和交通压力.
- 监测温度,水分和孔隙水压的变化.
主要成果:
- 动态负载改变了温度,湿度和孔隙水压的分布.
- 在测试开始时,在上层冰层土壤中观察到热水和孔水压力状态的显著变化.
- 动态负载诱导空间孔水压差,驱动水分迁移,并将水分集中在负载以下.
结论:
- 动态负载会影响冰层下层的热水状态和湿度分布.
- 降低土壤温度可以减轻动态负载的影响.
- 控制土壤温度至关重要,以防止冰层冰的冷次级积累水分.
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