石窟寺作为重要历史文物,其保护利用工作越来越重要,但在冷热交替的长期作用下,石窟岩体的物理力学性质会发生一定程度的改变。本文选取重庆大足石刻砂岩,通过质量对比、纵波波速测试、CT扫描、X射线衍射(XRD)、X射线荧光(XRF)分析,对冷热交替作用后石窟砂岩的劣化特性开展研究。试验过程设计不同冷热循环次数、不同高温和低温持续时间、不同冷却方式等多种试验工况,分析了石窟砂岩质量、纵波波速、裂隙发育、矿物元素组成和内部孔隙的变化规律。结果表明:(1) 经过多次冷热循环,砂岩纵波波速降低,并且变化幅度受冷热循环次数和冷却方式的影响;(2) 当冷热循环过程中采用水冷却方式,砂岩中可溶盐矿物会逐渐流失,导致岩样孔隙增大,进而产生裂隙。
Grotto temples are important historical relics, and their protection and utilization are becoming increasingly important. However, under the effect of cooling and heating for a long time, the physical and mechanical properties of the grotto rock mass will change in a certain. In this paper, the sandstone of Dazu grottoes in Chongqing was taken as the research object, and the deterioration properties of the grotto sandstone were studied through the mass, longitudinal wave velocity test, CT scanning, X-ray diffraction (XRD), X-ray fluorescence (XRF) analysis. The experimental process involves multiple conditions such as different heating-cooling cycle times, different durations of high and low temperatures, and different cooling methods. These test conditions are designed to analyze the effects of different temperature changes on the quality, longitudinal wave velocity, fracture development, mineral element composition, and internal pores of grotto sandstone. The results show that: (1) The longitudinal wave velocity of sandstone decreased after multiple heating-cooling cycles. The degree of reduction was influenced by the number cycles and the cooling methods. (2) As water cooling method was used during the experiment, soluble salt minerals in sandstone would gradually lose, which leaded to an increase in pore size of the rock sample and the formation of cracks.
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