在多孔介质中的盐溶液的异质冰核化
Xin Lin1, Chao Zhang2, Shaojie Hu2
1College of Civil Engineering, Hunan University, Changsha 410082, China.
The Journal of chemical physics
|March 1, 2024
概括
在多孔介质中的盐溶液的结温度下降是由水固体界面的异质冰核化 (HIN) 控制的. 溶解盐通过改变透潜力影响HIN,其中度是关键因素.
科学领域:
- 孔隙介质物理学的物理
- 解决方案化学 解决方案化学
- 材料科学是一种材料科学.
背景情况:
- 含有溶解盐的水在自然和人工多孔介质中很常见.
- 了解结点压力对于有孔的介质的力学和物理学至关重要.
- 冷温度下降和离子影响的确切机制尚不清楚.
研究的目的:
- 研究孔介质内的盐溶液中结温度下降的物理机制.
- 确定溶解离子如何影响结行为.
- 适应核化理论,以模拟孔隙溶液中的结.
主要方法:
- 通过使用管子进行受控孔径,溶液体积和固体-液体界面面积的孔径实验.
- 盐溶液中的各种离子度和类型.
- 通过结合透电位术语来适应古典核化理论.
主要成果:
- 在水固体界面上,结温度低压是由异质冰核化 (HIN) 控制的.
- 结温度随着固体-液体界面面积的减少而降低,而不依赖于孔径大小或体积.
- 溶解盐通过改变透潜力来影响HIN,度是主要决定因素,而不是离子类型.
结论:
- 异质冰核化 (HIN) 是控制孔隙溶液中结温度下降的主要机制.
- 由于溶解盐的奥斯莫斯电位变化显著影响HIN过程.
- 一个适应的核化理论模型准确地预测了孔隙溶液中的结行为,验证了HIN机制.
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