ISSN 1000-3665 CN 11-2202/P

    石窟砂岩内部毛细水迁移可视化试验研究

    Visualization of capillary water migration in grotto sandstones

    • 摘要: 【目的】水分入侵是威胁石窟本体安全、影响其长久保存的重要原因之一,但目前针对石窟砂岩内部毛细水迁移过程及变化特征的研究数量相对较少。【方法】为揭示毛细水在砂岩内部迁移的特征与机制,针对云冈石窟和乐山大佛所在地的新鲜砂岩开展室内的一维竖直毛细上升试验,测定吸水率和毛细上升高度随时间的发展,同时采用核磁共振和红外热成像技术获取砂岩内部水分的时空分布演变规律。【结果】云冈砂岩和乐山砂岩都属于中等毛细吸水能力,因乐山砂岩大孔数量多、孔径分布不均匀,其毛细吸水率和毛细上升高度发展更快,湿润前锋形状十分不规则。试验过程中,微孔饱和度始终高于中孔饱和度,不同类型的孔隙饱和度增加速度差异在乐山砂岩中更为明显,并且有部分较大孔隙无法通过毛细作用达到饱和。毛细水迁移包括水分上升和扩散2个过程,吸水砂岩内部的含水量随着高度增加而逐渐降低,分为湿润区、过渡区和干燥区,其表面温度也相应呈现从低到高渐变的规律。【结论】温度对含水量的细微变化反应敏感,因此红外热成像技术在水分分布快速探查中表现出良好的应用价值。在砂岩质石窟劣化机理、无损检测技术适用性等研究方面进行了探索,以期为文物的预防性保护提供理论依据和实践指导。

       

      Abstract: 【Objective】Moisture intrusion is a critical factor threatening the structural integrity and long-term preservation of sandstone grottoes. However, limited studies have addressed the dynamics and transformation characteristics of capillary water migration within such heritage materials. 【Methods】To elucidate the characteristics and mechanisms of capillary water migration, one-dimensional vertical capillary rise tests were carried out in the laboratory on fresh sandstones from the Yungang Grottoes and the Leshan Giant Buddha site. The development of water absorption rate and height of capillary rise over time was measured. In addition, nuclear magnetic resonance and infrared thermography techniques were used to obtain the evolution of spatiotemporal distribution of moisture within the sandstones. 【Results】The results indicate that both Yungang sandstone and Leshan sandstone show a moderate capability of capillary water absorption. Due to a larger number of large pores and the uneven pore size distribution in Leshan sandstone, its water absorption rate and height of capillary rise change more rapidly, resulting in a highly irregular shape of wetting front. Throughout the testing process, the saturation degree of micropores remains higher than that of mesopores, and the differences in the increasing rate of saturation degree among different types of pores are more pronounced in Leshan sandstone. Additionally, some larger pores are unable to become fully saturated via capillary action. Capillary water migration consists of two processes, i.e., water rising and water diffusion. Within the sandstone absorbing water, moisture content is the highest at the bottom, which gradually decreases with increasing height. It leads to the formation of wet, transitional, and dry zones, with its corresponding surface temperature changing gradually from low to high. 【Conclusions】Changes of temperature can reflect fine variation in moisture content, and therefore, the infrared thermography technique exhibits good applicability in rapid investigation of moisture distribution. This study did some exploration on the deterioration mechanisms of sandstone grottoes and the applicability of non-destructive testing techniques, aiming to provide a theoretical basis and practical guidance for the preventive conservation of cultural heritage.

       

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