Evolution of Weathering Characteristics of Building Limestone Under Freeze-Thaw Cycles
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摘要:
冻融循环是影响北方灰岩质文物的主要因素之一,普遍诱发多种表层风化病害,严重威胁文物的长久保存. 针对新鲜灰岩开展浸水冻融模拟风化试验,综合多种表征技术获取物理力学性质指标发展规律,结合孔隙结构变化从宏观和微观尺度定量揭示灰岩的冻融损伤机制,并通过熵权-线性加权法实现灰岩风化的综合评估. 结果表明:冻融循环50次后,纵波波速、表面硬度显著下降,损失率均在10%以上,毛细吸水系数提升了1倍以上;单轴抗压强度衰减率为30.6%,循环次数越大灰岩压缩后的结构完整性越差;灰岩孔隙主要由介孔(0.1 ~
1000.0 μm)组成,冻融循环导致孔隙数量和体积增加,同时伴随颗粒磨损以及裂隙扩张;力学性能的半衰期是衡量灰岩抗冻融能力的重要参数,基于无损指标构建的多元回归模型能够有效预测单轴抗压强度变化;毛细吸水系数对风化损伤的响应最为敏感,引入完整度指标,有助于从多维度实现建筑灰岩风化等级的量化评估. 研究成果为灰岩材料的科学认知和文物风化的现状评估提供了理论依据和实践指导.Abstract:Freeze-thaw cycles are among the primary factors affecting the limestone cultural relics in northern China. These cycles often result in various forms of surface weathering, seriously threatening the long-term preservation of these cultural relics. Water immersion freeze-thaw simulation weathering experiments were conducted on fresh limestone. The development patterns of physical and mechanical property indicators were obtained by utilizing various characterization techniques. By examining variations in pore structure, the freeze-thaw damage mechanism of limestone was quantitatively revealed from both macro and micro scales, and a comprehensive evaluation of weathered limestone was performed using an entropy weight-linear weighting method. The results have shown that after 50 freeze-thaw cycles, the P-wave velocity and surface hardness significantly decrease, with a loss rate of over 10%. The capillary water absorption coefficient increases by more than one time; The uniaxial compressive strength decay rate was 30.6%. As the number of cycles increases, the structural integrity of the compressed limestone becomes worse. The pores of limestone are primarily composed of mesopores (0.1-
1000 μm). Freeze-thaw cycles lead to an increase in both the number and volume of pores, accompanied by particle wear and the expansion of cracks. The mechanical-property half-life is a key parameter for evaluating limestone’s freeze-thaw resistance. A multivariate regression model based on non-destructive measurements can effectively predict the variation in uniaxial compressive strength. The capillary water absorption coefficient exhibits the greatest sensitivity to weathering damage. The introduction of an integrity index enables a multidimensional and quantitative assessment of the weathering severity of building limestone. The research findings provide a theoretical basis and practical guidance for the scientific understanding of limestone materials and the assessment of the current state of cultural relics’ weathering. -
表 1 新鲜灰岩的基本物理力学性质
Table 1. Basic physical and mechanical properties of fresh limestone
性质 干密度/
(g•cm−3)饱和吸水率/
%开口孔隙率/
%毛细吸水系数/
(kg•m−2•h−0.5)纵波波速/
(m•s−1)表面硬度/
HLD单轴抗压强度/
MPa数值 2.71 ~ 2.75 0.45 ~ 0.51 1.23 ~ 1.36 0.189 ~ 0.216 3639 ~3981 645 ~ 682 146.78 ~ 169.88 表 2 冻融循环中灰岩的汞注入量变化
Table 2. Variation of mercury intrusion volume of limestone during freeze-thaw cycles
循环次数/次 孔隙0.1~10.0 μm 孔隙10~1000.0 μm 全孔径范围 汞注入量/(mL•g−1) 占比/% 汞注入量/(mL•g−1) 占比/% 汞注入量/(mL•g−1) 占比/% 0 0.0017 12.50 0.0119 87.50 0.0136 100.00 20 0.0018 10.17 0.0159 89.83 0.0177 100.00 30 0.0021 10.71 0.0175 89.29 0.0196 100.00 50 0.0024 10.86 0.0197 89.14 0.0221 100.00 -
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