陇东地区砂岩石窟病害区域特征研究
CSTR:
作者:
作者单位:

(1.西北大学文化遗产学院,陕西西安 710127;2.文化遗产研究与保护技术教育部重点实验室(西北大学),陕西西安 710127)

作者简介:

孙满利(1968—),男,2006年博士毕业于兰州大学地质工程专业,教授,研究方向为石窟寺、土遗址保护,E-mail: sunml68@sohu.com 通信作者:沈云霞(1987—),女,研究方向为土遗址和石窟寺保护研究,E-mail:shenyx17@nwu.edu.cn

通讯作者:

中图分类号:

基金项目:

甘肃省科技重大专项计划项目资助(18ZD2FA001)


Study on the regional characteristics of sandstone grotto deterioration in the Longdong area
Author:
Affiliation:

(1. School of Cultural Heritage, Northwest University, Xi’an 710127, China;2. Key Laboratory of Cultural Heritage Research and Conservation (Northwest University), Ministry of Education, Xi’an 710127, China)

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    陇山以东、子午岭以西的甘肃陇东地区保存有大量砂岩石窟,受自然、人为因素的影响,石窟病害类型多样。以省级以上文物保护单位为样本,通过系统调查,将陇东地区砂岩石窟按照地貌地形特征分为泾河流域、平定川地区和六盘山地区三个区域。岩体失稳病害、水蚀病害和浅表层风化病害在研究区砂岩石窟皆有发育。泾河流域岩体失稳病害主要表现为卸荷裂隙、节理发育,存在崩塌、滑坡类边坡失稳问题,崩塌规模一般较大,大型洞窟存在洞顶塌落病害;水蚀病害水蚀病害类型多,规模大,以窟内渗水、窟内潮湿和崖面冲蚀三类病害为主;浅表层风化病害较发育,表面粉化剥落、表面泛盐、表层结壳剥落及孔洞状风化普遍存在,其次为生物病害,主要体现为微生物及地衣苔藓覆盖。平定川地区石窟岩体失稳病害主要为小块危岩体掉落及窟顶塌落病害;水蚀病害类型多、规模小,以窟内渗水、窟内潮湿、岩体潮湿、坡脚冲蚀为主;浅表层风化病害较为发育,以表面粉化剥落、风化掏蚀最为显著。六盘山地区石窟岩体失稳病害不发育,卸荷裂隙、节理数量较少,存在洞顶崩塌病害;水蚀病害相对不发育,以崖面冲蚀为主,有少量窟内渗水;浅表层风化病害发育类型少,以表层结壳剥落及表面不均匀变色两类病害最为突出。研究结果对指导该地区石窟保护研究与规划有着重要意义。

    Abstract:

    There are a large number of sandstone grottoes in the Longdong area of Gansu. Affected by natural and human factors, the grottoes have various types of diseases. Through a systematic survey of samples from provincial and national heritage conservation units, the sandstone grottoes in Longdong area were divided into three regions, namely the Jing River Basin, the Pingding River area and the Liupan Mountain area, according to the topographic features. The instability of rock mass, water erosion and superficial weathering have all developed in the study areas. In the Jing River Basin, the instability of rock mass was mainly manifested by the development of unloading cracks and joints. There were also problems of slope instability, such as collapse and landslide, with the collapse scale being generally larger and there being roof collapse diseases in large caves. There were many types of water erosion, the main diseases being water seepage, wetting in the grotto and cliff erosion. With regard to superficial weathering, powdering exfoliation, efflorescence, crust and alveolization were widespread; the second cause was the biological disease, mainly reflected by microorganisms and lichen moss cover. In the Pingding River area, the instability of rock mass was mainly caused by the falling of small pieces of rock and the collapse of the roof. The water erosion was of many types and of small scale, such as water seepage, dampness and erosion at the foot of the slope. The superficial weathering was also prevalent, and powdering exfoliation and recess erosion were more serious. In the Liupan Mountain area, the instability of rock mass was not developed, although there was some collapse of the roof. Water erosion was relatively undeveloped, with erosion on the cliff and a small amount of water seepage. The superficial weathering was less developed, with surface crust spalling and uneven surface discoloration being the most prominent. The results of the study have important implications for guiding research and planning for grotto conservation.

    参考文献
    相似文献
    引证文献
引用本文
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2022-11-21
  • 最后修改日期:2023-06-06
  • 录用日期:
  • 在线发布日期: 2024-12-30
  • 出版日期:
文章二维码
您是第位访问者
主办单位:上海博物馆 编辑出版:《文物保护与考古科学》编辑委员会
地址:上海市徐汇区龙吴路1118号,上海博物馆文物保护科技中心,《文物保护与考古科学》编辑部
电话:021-54362886 传真:021-54363740 E-mail:wwbhykgkx@163.com
文物保护与考古科学 ® 2025 版权所有
沪ICP备10003390号-3
沪公网安备 31010102005301号