This study focused on sandstones from the Yungang Grottoes under different degrees of weathering and employed a specially designed experimental setup.Using a mod-ified dew point temperature calculation formula,combined with measured temperature,humidity and electrical resistance data,a quantitative evaluation method was developed for water vapor diffusion and condensation processes in sandstone under varying degrees of weathering.Results showed that weathered sandstone had higher porosity and permeabil-ity,facilitating water vapor diffusion and condensation.During the water vapor diffusion stage,higher degrees of weathering were correlated with faster inward diffusion rates and greater internal relative humidity.During the condensation stage,as the degree of sand-stone weathering increased,the location where condensation water formed became deeper and occurred earlier.In addition,the condensation depth in the rock was positively cor-related with the duration of exposure to high-humidity environments.These findings can help in identifying the patterns of water vapor diffusion and condensation in weathered sandstone,thus providing a scientific basis for dealing with condensation issues at stone cultural heritage sites.
关键词
风化砂岩/石质文物/水气扩散/水气凝结/露点温度
Key words
weathered sandstone/stone culture heritage/water vapor diffusion/water vapor condensation/dew point temperature
维普
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