断开的活层和未结的永久土:讨论与永久土相关的术语和定义
É Devoie1, R F Connon2, R Beddoe3
1Department of Civil Engineering, Queen's University, Canada.
The Science of the total environment
|December 1, 2023
概括
由于基于温度的定义,永久土的监测和建模面临着挑战. 建议将冰含量与温度一起报告,以准确评估永久土.
科学领域:
- 地球科学 地球科学 地球科学
- 地质物理学 地质物理学
- 冰层科学 冰层科学 冰层科学 冰层科学
背景情况:
- 永久土被定义为两年内温度低于0°C的地面,每年有一个活跃层解/结.
- 目前基于温度 (永久土) 和水相 (活性层) 的定义造成了监测和建模的挑战.
- 永久土的关键性质 (例如强度,透性,能量含量) 更多地取决于冰含量而不是温度.
研究的目的:
- 突出永久土研究中基于温度的定义的局限性.
- 倡导将冰含量纳入永久土测量和模型.
- 提高永久土环境评估的准确性.
主要方法:
- 审查现有的永久土定义及其影响.
- 分析永久土特性,温度和冰含量之间的关系.
- 在测量和建模的永久土系统之间的能源比较中发现差异.
主要成果:
- 基于温度的定义忽视了关键的永久土特征,如塔利克和冷.
- 模拟和测量永久土之间的能量差异可以达到90%,尽管温度读数相同.
- 冰含量是永久土的物理和热性质的更重要的决定因素,而不是单独的温度.
结论:
- 基于温度的永久土定义不足以准确监测和建模.
- 报告冰含量以及温度对于强大的永久土研究至关重要.
- 整合冰含量数据将提高永久土研究和应用的可靠性.
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