乐山大佛胸腹区渗水损伤表征

S. Bo, Zhang Peng, Shen Xiwang, Li Yuyuan
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摘要

乐山大佛胸腹区渗水损伤显著,造成佛像体内砂岩腐蚀开裂,使佛像表面的修复材料镂空脱皮,导致生物损伤生长。本研究对乐山大佛胸腹区渗水和大气降水进行了连续监测和采样。佛像胸腹部位的渗水主要受大气降水和蒸发控制。渗水的滞后效应反映了左侧基岩裂隙相对发育,透水性明显。在大气降水监测期间,大气降水的平均pH值为8.13,为弱碱性。2009年以后,佛州年平均大气降水pH值大于5.6,且呈逐年增加趋势。佛祖的渗水中含有大量的离子。胸腹区渗水的化学类型为碳酸钙(caco3)和硫酸钙(caso4)。岩石风化作用贡献了佛州渗水中90%以上的离子。岩石显微分析表明,岩石主要成分为caco3和sio2,具有明显的层状形态,在空气和水的存在下易溶解。水化学离子组成表明,h2co3和h2so4都参与了砂岩的风化过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Characterizing-water seepage damage in the chest-abdomen area of the Leshan Giant Buddha
The water seepage damage in the chest-abdomen area of the Leshan Giant Buddha is significant, which causes the sandstone in the body of the Buddha to corrode and crack, makes the repair materials on the surface of the Buddha hollow and desquamate, and leads to the growth of biological damage. In this study, continuous monitoring and sampling of the water seepage in the chest-abdomen area of the Leshan Giant Buddha and the atmospheric precipitation were performed. The water seepage in the chest-abdomen area of the Buddha is primarily controlled by atmospheric precipitation and evaporation. The hysteresis effect of water seepage reflects that the bedrock fissure on the left is relatively developed with significant water transmissibility. During the atmospheric precipitation monitoring period, the average pH of atmospheric precipitation was 8.13, i.e., weakly alkaline. After 2009, the annual average pH of atmospheric precipitation for the Buddha was greater than 5.6 and increased year by year. The water seepage of the Buddha contained a large amount of ions. The chemistry type of water seepage in the chest-abdomen ares is calcium carbonate (CaCO 3 ) and calcium sulfate (CaSO 4 ). Rock weathering contributes more than 90% of the ions in the Buddha water seepage. The microscopic analysis of the rock shows that the main components of the rock are CaCO 3 and SiO 2 , and there is obvious layered morphology, is easy to be dissolved in the presence of air and water. The composition of water chemical ions indicates that H 2 CO 3 and H 2 SO 4 are both involved in the process of the weathering of the sandstone.
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