在水平结过程中对高粘土的冰加重的演变特征和影响因素的研究
Yue Liu1, Yupeng Shen2, Peng Jing1
1School of Civil Engineering, Beijing Jiaotong University, Beijing, 100044, China.
Scientific reports
|January 3, 2025
概括
寒冷地区的水平潮受土壤含水量和干燥密度的影响. 较高的水含量增加了升,而较高的干燥密度减少了它,影响了结构安全.
科学领域:
- 地质技术工程 地质技术工程
- 土壤科学 土壤科学
- 土木工程 土木工程是指土木工程.
背景情况:
- 在寒冷的气候下,水平伤对基础设施构成重大风险.
- 结的边缘是土壤结的关键区域,它决定了水分的分配和升的行为.
研究的目的:
- 为了研究初始水含量和干密度对高粘土水平冷边缘发展的影响.
- 分析土壤属性与升幅度之间的关系.
- 提出和验证一个改进的冷边缘预测模型.
主要方法:
- 使用自主研发的水平升设备进行了七次实验.
- 考林粘土样本的初始水含量和干密度各不相同.
- 测量了冰的升高和观察到的结边缘迁移模式.
主要成果:
- 增加的初始含水量加速了水的迁移,增加了升 (3.43毫米/5%的增加).
- 增加的初始干密度降低了和水的迁移速度 (3.26毫米每0.1g/cm3增加).
- 观察到冷边缘的非垂直推进,可能会影响结构完整性.
结论:
- 最初的水含量和干燥密度是控制冷边缘发展和升的关键因素.
- 非垂直边缘迁移凸显了对结构稳定的潜在风险.
- 一个改进的结边缘预测模型,基于Mizoguchi模型,并与现场数据验证,为工程设计和在寒冷地区减轻冰的理论基础.
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