在多孔介质中表面蒸发和演变:对柱阵微型的研究
1Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, Hubei 430071, China; State Key Laboratory of Geomechanics and Geotechnical Engineering Safety, Wuhan, Hubei 430071, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Journal of colloid and interface science
|August 24, 2025
概括
在狭窄的毛孔中,蒸发是由接口的形状决定的,而不仅仅是毛孔的大小. 了解孔尺度液体-蒸汽接口可以改善土壤水文和海水淡化模型.
科学领域:
- 多孔介质的物理
- 多相流量
- 接口现象
背景情况:
- 在狭窄的孔隙中蒸发对于土壤盐化和海水淡化至关重要.
- 传统模型忽略了空气入侵后的动态液体-蒸汽界面演变.
- 孔隙封闭和界面形态显著影响局部蒸发率.
研究的目的:
- 研究孔隙封闭和界面形态对蒸发速度的影响.
- 开发一个用于预测多孔介质相变的机制框架.
主要方法:
- 使用支柱阵列微模型作为2D多孔介质模拟.
- 使用实时可视化和高分辨率图像处理.
- 界面区域和曲率的量化时空变化.
主要成果:
- 外部接口占相位变化的85-92%,内部接口贡献<15%.
- 蒸发动力学显示,随着界面曲率半径的减少而呈指数增长.
- 一个特有的界面曲率长度尺度 (1-50μm) 指定的蒸发速度.
结论:
- 孔封闭和界面几何增强了蒸发动力.
- 这些发现澄清了土壤水留在较小的孔隙中明显抑制了蒸发.
- 建立了一个机械框架,将界面几何与多孔介质的相变预测联系起来.
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