量化衰变是由于湿气大气沉积在玄武岩上造成的
Luis Miguel Urbina Leonor1, Rodolfo Sosa Echeverría2, Ana Luisa Alarcón Jiménez2
1Posgrado de Ingeniería Ambiental, Universidad Nacional Autónoma de México, Mexico City 04510, Mexico.
Materials (Basel, Switzerland)
|August 26, 2023
概括
这项研究表明,红色玄武岩建筑材料从潮湿的大气沉积中腐烂. 吸水能力和开放的孔隙性有效地监测这种衰变,降水量是关键因素.
科学领域:
- 地质科学 地质科学
- 材料科学 材料科学 材料科学
- 保护科学 保护科学
背景情况:
- 像玄武岩这样的火山石是研究不足的建筑材料,对遗产保护至关重要.
- 潮湿的大气沉积对石头建筑遗产的耐用性构成重大威胁.
研究的目的:
- 为了研究红色玄武岩经受潮湿大气沉积的衰变机制.
- 评估吸水能力 (WAC) 和开放孔隙 (OP) 作为衰变监测变量的适用性.
主要方法:
- 红色玄武岩样本暴露在模拟全球性,酸性和无酸性降水的人工雨水溶液中.
- 对液化物进行分析,以了解退化过程.
- 通过质量差,WAC和OP测量量衰变的量化.
主要成果:
- 该方法有效地模拟了加速的气候变化和腐烂.
- 红色玄武岩通过矿物溶解,盐结晶,阴离子交换和化合物洗容易腐烂.
- WAC和OP变化是监测现场衰变的可靠指标.
- 降水量显著影响衰变,比pH值更重要.
结论:
- 开发的方法适用于研究建筑材料的衰变.
- 红色玄武岩遗产易受大气湿沉积的影响,已确定了特定的衰变机制.
- 在现场监测石材腐烂时,WAC和OP是有前途的变量.
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