在石头气候变化中的盐混合物
Sebastiaan Godts1,2,3, Scott Allan Orr4, Michael Steiger5
1Monuments Lab, Royal Institute for Cultural Heritage (KIK-IRPA), Brussels, Belgium. sebastiaan.godts@kikirpa.be.
Scientific reports
|August 16, 2023
概括
了解石头气候变化需要研究盐混合物,而不仅仅是单个盐. 这项研究确定了常见盐混合物及其关键相对湿度 (RH) 点,这对于预测和防止材料衰变至关重要.
科学领域:
- 地质科学 地质科学
- 材料科学 材料科学 材料科学
- 环境科学 环境科学
背景情况:
- 盐化是石材的重要降解过程.
- 岩石衰变是由多孔结构内的盐结晶压力驱动的.
- 相对湿度 (RH) 极大地影响盐溶解和结晶周期.
研究的目的:
- 为了分析在经过气候变化的石头中发现的现实的盐混合物.
- 为了识别常见盐的成分和它们的气候变化行为.
- 为了确定普遍存在的盐混合物的关键RH值.
主要方法:
- 热力学计算被用来分析成千上万种盐混合物.
- 从一个超过85个理论池中识别出经常出现的盐物种.
- 分析重点关注不同RH条件下的盐混合物的行为.
主要成果:
- 鉴定出了在经过气候变化的石头中存在两种普遍存在的盐混合物.
- 在分析的混合物中经常发现14种常见盐物种.
- 确定了这些常见盐及其混合物的临界RH点.
结论:
- 盐混合物的成分显著影响着气候变化过程.
- 了解关键的RH对于预测盐风的情况至关重要.
- 这些发现将指导未来关于石头保护和耐用性的实验研究.
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