岩石力学与工程学报
巖石力學與工程學報
암석역학여공정학보
CHINESE JOURNAL OF ROCK MECHANICS AND ENGINEERING
2009年
z2期
3769-3775
,共7页
郭青林%王旭东%薛平%张国彬%樊再轩%侯文芳%张正模
郭青林%王旭東%薛平%張國彬%樊再軒%侯文芳%張正模
곽청림%왕욱동%설평%장국빈%번재헌%후문방%장정모
工程地质%敦煌莫高窟%岩体%水汽%盐分%空间分布
工程地質%敦煌莫高窟%巖體%水汽%鹽分%空間分佈
공정지질%돈황막고굴%암체%수기%염분%공간분포
engineering geology%Dunhuang Mogao Grottoes%rock mass%moisture%salinity%spatial distribution
著名的世界文化遗产--敦煌莫高窟开凿于第四纪砂砾岩组成的崖壁上,受自然环境及人为因素影响,洞窟内壁画产生起甲、空鼓和酥碱等多种病害,尤其以底层洞窟最为严重.以病害最具代表性的底层洞窟之一莫高窟第98窟为例,通过在98窟西壁下部无壁画部位钻孔取样测定可溶盐,并在钻孔内布设高精度温湿度监测探头,西壁下部由南向北电阻率测定等研究,得出如下结论:98窟西壁表面到岩体内的可溶性盐主要以硫酸盐和氯盐为主,主要富集在表面至35 cm深的岩体内;岩体内的温湿度和盐分有很好的关联性,盐分随着岩体内水汽含量的上升而下降;在岩体深125 cm有凝结水产生;在高湿度和崖体源源不断的盐分来源的作用下,导致背靠崖体的西壁壁画内的含盐量要高于其他各壁,对洞窟环境的变化也更为敏感,病害也要远远严重于其他各壁等,这些结论可为壁画病害产生机制研究和防治提供科学依据.
著名的世界文化遺產--敦煌莫高窟開鑿于第四紀砂礫巖組成的崖壁上,受自然環境及人為因素影響,洞窟內壁畫產生起甲、空鼓和酥堿等多種病害,尤其以底層洞窟最為嚴重.以病害最具代錶性的底層洞窟之一莫高窟第98窟為例,通過在98窟西壁下部無壁畫部位鑽孔取樣測定可溶鹽,併在鑽孔內佈設高精度溫濕度鑑測探頭,西壁下部由南嚮北電阻率測定等研究,得齣如下結論:98窟西壁錶麵到巖體內的可溶性鹽主要以硫痠鹽和氯鹽為主,主要富集在錶麵至35 cm深的巖體內;巖體內的溫濕度和鹽分有很好的關聯性,鹽分隨著巖體內水汽含量的上升而下降;在巖體深125 cm有凝結水產生;在高濕度和崖體源源不斷的鹽分來源的作用下,導緻揹靠崖體的西壁壁畫內的含鹽量要高于其他各壁,對洞窟環境的變化也更為敏感,病害也要遠遠嚴重于其他各壁等,這些結論可為壁畫病害產生機製研究和防治提供科學依據.
저명적세계문화유산--돈황막고굴개착우제사기사력암조성적애벽상,수자연배경급인위인소영향,동굴내벽화산생기갑、공고화소감등다충병해,우기이저층동굴최위엄중.이병해최구대표성적저층동굴지일막고굴제98굴위례,통과재98굴서벽하부무벽화부위찬공취양측정가용염,병재찬공내포설고정도온습도감측탐두,서벽하부유남향북전조솔측정등연구,득출여하결론:98굴서벽표면도암체내적가용성염주요이류산염화록염위주,주요부집재표면지35 cm심적암체내;암체내적온습도화염분유흔호적관련성,염분수착암체내수기함량적상승이하강;재암체심125 cm유응결수산생;재고습도화애체원원불단적염분래원적작용하,도치배고애체적서벽벽화내적함염량요고우기타각벽,대동굴배경적변화야경위민감,병해야요원원엄중우기타각벽등,저사결론가위벽화병해산생궤제연구화방치제공과학의거.
Dunhuang Mogao Grottoes,the very famous world culture heritage,was chiseled in the cliff face of alluvial grit etching by the Daquan River in the Quaternary Period. Undergone natural and human factors,caves of Mogao Grottoes have many diseases and deteriorations including flaking,detachment and disruption;especially the caves of low-layer are most serious. Cave 98,one of the most valuable and representative diseases of low-layer caves in the Five Dynasties(AD914-AD935),is selected as an example. Like all other caves in Mogao Grottoes,it has been affected by the natural environment. From the hole drilled at the lower portion of the western wall without painting,samples obtained for salinity analysis. The temperature and humidity are measured inside the hole. The analysis of electrical resistivity data from south to north of the lower portion of the western wall indicates that the soluble salt contents of the rock mass are mainly vitriolic and chloride,mainly concentrated between the surface and the depth of 35 cm. Water condensation occurs in the rock mass at depth of 125 cm. Inside the rock mass,there is close correlation between relative humidity and salinity. When moisture content rises,salinity drops. Due to the high humidity and abundant supply of salt,the salinity of the western wall,which is backed by the main cliff structure,is higher than the other walls,and it is more sensitive to changes in the environment. These achievements have provided a scientific <http://www.iciba.com/scientific/> basis <http://www.iciba.com/basis/> for conservation wall paintings.