岩土力学 ›› 2025, Vol. 46 ›› Issue (S1): 354-365.doi: 10.16285/j.rsm.2024.0572CSTR: 32223.14.j.rsm.2024.0572

• 岩土工程研究 • 上一篇    下一篇

环境蒸发条件下石质文物毛细水动态分布规律影响研究

秦立科1, 2,郭瑞琦1, 2,赵皓辰3, 4,甄刚3, 4,王琦1, 2   

  1. 1. 西安科技大学 建筑与土木工程学院,陕西 西安 710054;2. 西安科技大学 岩土文物与遗迹保护研究所,陕西 西安 710054; 3. 陕西省文物保护研究院,陕西 西安 710075;4. 陕西省文物保护研究院 砖石质文物保护国家文物局重点科研基地,陕西 西安 710075
  • 收稿日期:2024-05-15 接受日期:2024-06-24 出版日期:2025-08-08 发布日期:2025-08-28
  • 通讯作者: 甄刚,男,1977年生,学士,研究馆员,主要从事文物保护修复研究。E-mail: zhen-gang@sohu.com
  • 作者简介:秦立科,男,1982年生,博士,硕士研究生导师,副教授,主要从事岩土文物加固研究与保护相关工作。E-mail: 422576294@qq.com
  • 基金资助:
    国家自然科学基金项目(No.42071100,No.42271144)。

Capillary water dynamic distribution of stone relics under environmental evaporation conditions

QIN Li-ke1, 2, GUO Rui-qi1, 2, ZHAO Hao-chen3, 4, ZHEN Gang3, 4, WANG Qi1, 2   

  1. 1. School of Architecture and Civil Engineering, Xi’an University of Science and Technology, Xi’an, Shaanxi 710054, China; 2. Geotechnical Relics and Heritage Conservation Institute, Xi’an University of Science and Technology, Xi’an, Shaanxi 710054, China; 3. Shaanxi Institute for the Preservation of Cultural Heritage, Xi’an, Shaanxi 710075, China; 4. Key Scientific Research Base of the National Cultural Heritage Administration for the Protection of Brick and Stone Cultural Relics, Shaanxi Institute for the Preservation of Cultural Heritage, Xi’an, Shaanxi 710075, China
  • Received:2024-05-15 Accepted:2024-06-24 Online:2025-08-08 Published:2025-08-28
  • Supported by:
    This work was supported by the National Natural Science Foundation of China project (42071100, 42271144).

摘要: 受环境变化影响,自然条件下保存的砂岩表面蒸散速率并不保持恒定,这就导致砂岩内部毛细水在一定范围内产生迁移现象。该现象不仅引起砂岩内部矿物的反复水化膨胀−干燥收缩效应,因毛细迁移现象引起的诸如可溶盐结晶−溶解循环、冻融循环、生物风化等都进一步加速了砂岩的劣化进程。为对石质历史建筑进行的抢救性保护工作提供可靠参考,从毛细水迁移机制的角度出发,以湖北恩施“荆南雄镇”石牌坊为研究对象,对其周围微环境进行了长期监测以及相关室内试验研究。采用数值模拟的研究方式,利用Comsol Multiphysics软件,在砂岩部分连续浸泡条件下,将微环境监测数据和岩石风化联系到一个研究框架中。结果发现:(1)从不同时间液体体积分数分布情况的角度来看,在长时间维度下,湿润锋附近的水力梯度平缓,砂岩体积含水率变化最剧烈,在这一高度范围内岩石劣化现象最为明显;(2)砂岩中毛细水总量达到动态平衡后,体积含水率在竖直向上呈现出上低下高,水平向上呈现出中间向两边递减的分布规律,且湿润锋随蒸散速率的变化而上下起伏,所对应区域与实际调研中的风化区域相吻合;(3)通过降低石质结构历史建筑底部压力水头可显著减少水分进入其中,故而可以通过降低石牌坊周围地下水高度的方法,达到降低底部水压头的目的,从而减小因毛细水迁移引起的的劣化效应。

关键词: 砂岩劣化, 毛细水迁移, Penmane-Monteith方程, Richards方程, 蒸发边界条件

Abstract: Environmental changes cause the surface evapotranspiration rate of naturally preserved sandstone to vary, resulting in capillary water migration within a specific range. This process not only induces repeated hydration expansion and drying shrinkage of minerals within the sandstone but also accelerates rock deterioration due to capillary migration, including salt crystallization, dissolution cycles, freeze-thaw effects, and biological weathering. To provide a reliable reference for the preservation of historical stone buildings, this study investigates the capillary water migration mechanism, focusing on the stone archway of “Jingnanxiongzhen” in Enshi, Hubei Province. Long-term microenvironment monitoring and laboratory experiments were conducted. Numerical simulations using Comsol Multiphysics software integrated microenvironment monitoring data with rock weathering patterns, establishing a research framework under partial continuous immersion conditions. The results show that: 1) From the perspective of liquid volume fraction distribution at different times, in the long time dimension, the hydraulic gradient near the wetting front is gentle, and the volume water content of sandstone changes most sharply, and the deterioration phenomenon of rock is most obvious in this height range. 2) Once capillary water reaches dynamic equilibrium, vertical water content varies, with higher values at the bottom and lower at the top. Horizontally, water content decreases from the center to the sides. The wetting front fluctuates with evapotranspiration rate changes, aligning with observed weathering patterns. 3) Reducing the pressure head at the base of historical stone structures significantly decreases water infiltration. Lowering groundwater levels around the stone archway achieves this reduction, mitigating capillary-induced deterioration.

Key words: damage of rock, capillary water migration, Penmane-Monteith equation, Richards equation, evaporation boundary condition

中图分类号: TU411
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