Multi-scale quantitative analysis of grotto sandstone degradation considering inorganic salt phase transitions

IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL
Sicheng Lin , Luqi Wang , Wengang Zhang , Shuo Wang , Zihua Xiong , Siwei Jiang , Gang Zhao
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Abstract

The salt deterioration of the surface and host rock mass of grottoes poses a serious challenge to the protection of grottoes. The existing indoor experimental research on salt weathering mainly focuses on characterizing the deterioration process. It is challenging to realize the multi-scale quantitative analysis of the complex salt weathering process, especially the lack of systematic research on time factors and inorganic salt phase transition. This study selected the fresh sandstone on the south bank of Baoding Mountain in Dazu and performed the dry-wet cycle test of mixed salt solution by a multi-scale experimental method. The experimental variables included concentration and cycle times. Combined with acoustic emission monitoring technology, qualitatively and quantitatively studied the time-dependent deterioration of grotto sandstone under salt weathering, and the water-salt system revealed the key mechanism of time-dependent deterioration of Big Buddha Bay rock mass. The low concentration mixed salt has little effect on sandstone samples due to the limited number of cycles. The image comparison analysis shows that the deterioration degree of the sample at 1.5 mol/L (referred to as 1.5 M) concentration is similar to that of the existing grottoes, which can effectively simulate the salt weathering in the actual environment. When the concentration increases to 2.0 M, the salt crystal penetrates the sample, and the erosion depth can reach 4.5 mm. The acoustic emission analysis shows that the proportion of tensile cracks is always higher than that of shear cracks. Under the action of dry-wet cycles, as the number of cycles increases, the failure mode of the sample gradually changes from shear-dominated to tension-dominated. The phase change of inorganic salt on grotto sandstone shows that sodium sulfate caused significant volume expansion and crystallization stress due to different hydrate phase changes, and the damage was the most significant.
考虑无机盐相变的溶洞砂岩退化多尺度定量分析
石窟地表和围岩的盐渍变质对石窟的保护提出了严峻的挑战。现有的盐风化室内试验研究主要集中在表征变质过程上。实现复杂盐风化过程的多尺度定量分析具有一定的挑战性,特别是缺乏对时间因素和无机盐相变的系统研究。本研究选取大足保定山南岸新鲜砂岩,采用多尺度试验方法进行混合盐溶液干湿循环试验。实验变量包括浓度和循环时间。结合声发射监测技术,定性和定量研究了盐风化作用下石窟砂岩的时变性,水盐体系揭示了大佛湾岩体时变性的关键机理。由于旋回次数有限,低浓度混合盐对砂岩样品的影响不大。图像对比分析表明,样品在1.5 mol/L(简称1.5 M)浓度下的变质程度与现有石窟相似,可有效模拟实际环境下的盐风化。当浓度增加到2.0 M时,盐晶体渗透到样品中,侵蚀深度可达4.5 mm。声发射分析表明,拉伸裂纹的比例始终高于剪切裂纹的比例。在干湿循环作用下,随着循环次数的增加,试样的破坏模式逐渐由剪切为主转变为拉伸为主。岩洞砂岩上无机盐的相变表明,硫酸钠由于不同的水合物相变引起了显著的体积膨胀和结晶应力,且损伤最为显著。
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来源期刊
CiteScore
14.00
自引率
5.60%
发文量
196
审稿时长
18 weeks
期刊介绍: The International Journal of Rock Mechanics and Mining Sciences focuses on original research, new developments, site measurements, and case studies within the fields of rock mechanics and rock engineering. Serving as an international platform, it showcases high-quality papers addressing rock mechanics and the application of its principles and techniques in mining and civil engineering projects situated on or within rock masses. These projects encompass a wide range, including slopes, open-pit mines, quarries, shafts, tunnels, caverns, underground mines, metro systems, dams, hydro-electric stations, geothermal energy, petroleum engineering, and radioactive waste disposal. The journal welcomes submissions on various topics, with particular interest in theoretical advancements, analytical and numerical methods, rock testing, site investigation, and case studies.
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