湿热盐与冻融作用下贺兰山岩画劣化机理对比研究OA
Comparative Study on Deterioration Mechanisms of Helan Mountain Rock Art under Hygrothermal-salt and Freeze-thaw Conditions
贺兰山岩画是我国北方地区最具代表性、规模最大的古代岩画群之一,目前正面临着严峻的风化威胁.本研究结合贺兰山岩画遗址所在地区的气候环境特征,设计湿热盐循环与冻融循环两组室内加速老化试验,结合SEM、XRD、孔渗测试及纳米压痕等多尺度分析手段,系统对比了两种环境应力下的岩石劣化效应.结果表明:冻融循环主要通过物理机制引起微裂隙扩展,劣化程度较轻,硬度与弹性模量仅下降约3%和1.3%,孔隙度和渗透率基本无变化.湿热盐循环实验结果显示盐结晶压、胶结物溶蚀与黏土矿物膨胀的化学—物理协同作用,导致岩石结构严重破坏,渗透率增幅达69%~86%,硬度与弹性模量分别下降44%和20.3%,并出现颗粒脱落现象.研究揭示砂岩劣化的本质是胶结相矿物在盐害与冻胀等环境应力作用下发生优先溶解、膨胀与流失,导致岩石颗粒间联结力显著降低、微观结构失稳,进而引发宏观力学性能衰退与表层剥落.建议通过周期性脱盐与湿度控制以延缓岩画风化,为贺兰山岩画的科学保护提供了理论依据与实践指导.
Helan Mountain rock art is one of the most representative and largest ancient rock art groups in northern China,and is currently facing severe weathering threats.Based on the climatic and environmental characteristics of the Helan Mountain rock art site,this study designed two sets of labo-ratory accelerated aging tests:hygrothermal-salt cycle and freeze-thaw cycles,and employed multi-scale analytical techniques such as SEM,XRD,porosity and permeability tests and nanoindentation to systematically compare the rock deterioration effects under two environmental stresses.The results indicated that the freeze-thaw cycle primarily caused microcrack propagation through physical mecha-nisms,resulting in relatively mild deterioration.The hardness and elastic modulus decreased by only approximately 3%and 1.3%,respectively,and limited changes were observed in porosity and perme-ability.In contrast,the test results of the hygrothermal-salt cycle showed that physicochemical syner-gistic effects,including salt crystallization pressure,cement dissolution,and clay mineral expansion,caused severe damage to the rock structure,with a 69%~86%increase in permeability,a 44%reduc-tion in hardness,and a 20.3%reduction in elastic modulus,as well as particle detachment.It was re-vealed that the essence of sandstone deterioration lay in the preferential dissolution,expansion and loss of cement-phase minerals under environmental stresses such as salt damage and frost heave,which led to a significant reduction in the bonding force between rock particles,instability of the micro-structure,and ultimately the degradation of macroscopic mechanical properties and surface spalling.This study suggests that periodic desalination and humidity control can be adopted to mitigate the weathering of rock art,thereby providing a theoretical basis and practical guidance for the scientific conservation of Helan Mountain rock art.
郝泽一;王硕;仉文岗;蒋晓菁;张建国;张艳梅
重庆大学土木工程学院,重庆 400045重庆大学土木工程学院,重庆 400045重庆大学土木工程学院,重庆 400045||山地城镇建设与新技术重点实验室,重庆 400045||库区环境地质灾害防治国家地方联合工程研究中心,重庆 400045||三峡库区库岸滑坡灾害重庆市野外科学观测研究站,重庆 400045大足石刻研究院,重庆 402360贺兰山岩画管理处,宁夏 银川 750001重庆大学航空航天学院,重庆 400045
建筑与水利
贺兰山岩画砂岩劣化湿热盐循环冻融循环胶结物流失
Helan Mountain rock artsandstone deteriorationhygrothermal-salt cyclefreeze-thaw cy-clecementing material loss
《防灾减灾工程学报》 2026 (1)
65-73,9
国家自然科学基金项目(52478325)、重庆市自然科学基金创新发展联合基金(CSTB 2022 NSCQ-LZX0001)、贺兰山岩画遗址保护项目(H20240863)资助
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