• 文献检索
  • 文档翻译
  • 深度研究
  • 学术资讯
  • Suppr Zotero 插件Zotero 插件
  • 邀请有礼
  • 套餐&价格
  • 历史记录
应用&插件
Suppr Zotero 插件Zotero 插件浏览器插件Mac 客户端Windows 客户端微信小程序
定价
高级版会员购买积分包购买API积分包
服务
文献检索文档翻译深度研究API 文档MCP 服务
关于我们
关于 Suppr公司介绍联系我们用户协议隐私条款
关注我们

Suppr 超能文献

核心技术专利:CN118964589B侵权必究
粤ICP备2023148730 号-1Suppr @ 2026

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验

中国青藏高原含软弱夹层预应力锚索支护岩质边坡地震响应研究

Seismic response investigation of prestressed anchor cable supporting rock slope with weak interlayer in Qinghai-Tibet Plateau, China.

作者信息

Fan Yaojiang, Yang Guoxiang, Ye Hailin, Liu Yun

机构信息

School of Engineering and Technology, China University of Geosciences (Beijing), Beijing, 100083, China.

Beijing Special Engineering Design and Research Institute, Beijing, 100028, China.

出版信息

Sci Rep. 2024 Aug 5;14(1):18088. doi: 10.1038/s41598-024-69291-w.

DOI:10.1038/s41598-024-69291-w
PMID:39103438
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11300609/
Abstract

Earthquake-induced rock landslides in the eastern mountains of the Tibetan Plateau, especially landslides with weak interlayers pose a significant threat to major construction projects. Prestressed anchor cable is one of the main reinforcement methods of rock slopes. This paper combines shaking table model tests and numerical simulation to study the reinforcement effect and dynamic response characteristics of prestressed anchor cables applied to rock slopes with weak interlayers under strong earthquakes. The research results show that prestressed anchor cables can effectively reinforce slopes with weak interlayers. A small cable inclination, a small spacing and a high prestress are recommended in the seismic reinforcement design of prestressed anchor cable. In addition, the characteristics of slope progressive damage and prestress loss under the earthquake are found by the shaking table test. The results have been applied in hazard prevention and control of rock slopes on the Chengdu-Lanzhou Railway at the eastern Qinghai-Tibet Plateau.

摘要

青藏高原东部山区地震诱发的岩石滑坡,尤其是存在软弱夹层的滑坡,对重大建设工程构成重大威胁。预应力锚索是岩石边坡主要的加固方法之一。本文结合振动台模型试验和数值模拟,研究了强震作用下预应力锚索对含软弱夹层岩石边坡的加固效果及动力响应特性。研究结果表明,预应力锚索能有效加固含软弱夹层的边坡。在预应力锚索抗震加固设计中,建议采用较小的锚索倾角、较小的间距和较高的预应力。此外,通过振动台试验发现了地震作用下边坡渐进破坏及预应力损失的特征。研究成果已应用于青藏高原东部成都 - 兰州铁路岩石边坡的灾害防治。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/fc656f00bcfc/41598_2024_69291_Fig25_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/fdd130b442f9/41598_2024_69291_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/02971dc025ea/41598_2024_69291_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/a3eaa4090f4a/41598_2024_69291_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/f973602d8f5e/41598_2024_69291_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/9c51f6bcabc7/41598_2024_69291_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/9f26cefb67af/41598_2024_69291_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/4d1fd55bc1a0/41598_2024_69291_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/e74365e24c99/41598_2024_69291_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/9c4a71884a64/41598_2024_69291_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/d7f81665ec2f/41598_2024_69291_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/616c50fd29a4/41598_2024_69291_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/bfccd5e7ee96/41598_2024_69291_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/6c8a06ae4ab6/41598_2024_69291_Fig13_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/6780dfe09c95/41598_2024_69291_Fig14_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/8ae91c5ca5b0/41598_2024_69291_Fig15_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/b8937e3c4593/41598_2024_69291_Fig16_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/e2510b685e02/41598_2024_69291_Fig17_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/9d09603960da/41598_2024_69291_Fig18_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/74f39579f0e5/41598_2024_69291_Fig19_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/5a31bf84ae16/41598_2024_69291_Fig20_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/b81ea1c7ce6e/41598_2024_69291_Fig21_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/2ca1b0d3050a/41598_2024_69291_Fig22_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/58b2e9ea505f/41598_2024_69291_Fig23_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/3fe31531d47a/41598_2024_69291_Fig24_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/fc656f00bcfc/41598_2024_69291_Fig25_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/fdd130b442f9/41598_2024_69291_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/02971dc025ea/41598_2024_69291_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/a3eaa4090f4a/41598_2024_69291_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/f973602d8f5e/41598_2024_69291_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/9c51f6bcabc7/41598_2024_69291_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/9f26cefb67af/41598_2024_69291_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/4d1fd55bc1a0/41598_2024_69291_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/e74365e24c99/41598_2024_69291_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/9c4a71884a64/41598_2024_69291_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/d7f81665ec2f/41598_2024_69291_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/616c50fd29a4/41598_2024_69291_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/bfccd5e7ee96/41598_2024_69291_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/6c8a06ae4ab6/41598_2024_69291_Fig13_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/6780dfe09c95/41598_2024_69291_Fig14_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/8ae91c5ca5b0/41598_2024_69291_Fig15_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/b8937e3c4593/41598_2024_69291_Fig16_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/e2510b685e02/41598_2024_69291_Fig17_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/9d09603960da/41598_2024_69291_Fig18_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/74f39579f0e5/41598_2024_69291_Fig19_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/5a31bf84ae16/41598_2024_69291_Fig20_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/b81ea1c7ce6e/41598_2024_69291_Fig21_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/2ca1b0d3050a/41598_2024_69291_Fig22_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/58b2e9ea505f/41598_2024_69291_Fig23_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/3fe31531d47a/41598_2024_69291_Fig24_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0bd6/11300609/fc656f00bcfc/41598_2024_69291_Fig25_HTML.jpg

相似文献

1
Seismic response investigation of prestressed anchor cable supporting rock slope with weak interlayer in Qinghai-Tibet Plateau, China.中国青藏高原含软弱夹层预应力锚索支护岩质边坡地震响应研究
Sci Rep. 2024 Aug 5;14(1):18088. doi: 10.1038/s41598-024-69291-w.
2
Dynamic acceleration response of a rock slope with a horizontal weak interlayer in shaking table tests.水平软弱夹层岩质边坡在振动台试验中的动力加速度响应。
PLoS One. 2021 Apr 21;16(4):e0250418. doi: 10.1371/journal.pone.0250418. eCollection 2021.
3
A Long-Term Monitoring Method of Corrosion Damage of Prestressed Anchor Cable.一种预应力锚索腐蚀损伤的长期监测方法
Micromachines (Basel). 2023 Mar 31;14(4):799. doi: 10.3390/mi14040799.
4
Analysis on Two Typical Landslide Hazard Phenomena in The Wenchuan Earthquake by Field Investigations and Shaking Table Tests.基于现场调查与振动台试验的汶川地震中两种典型滑坡灾害现象分析
Int J Environ Res Public Health. 2015 Aug 6;12(8):9181-98. doi: 10.3390/ijerph120809181.
5
Study on numerical simulation and mechanical properties of anchor cable with C-shaped tube subjected to shearing.C形管锚索受剪作用的数值模拟与力学性能研究
Sci Rep. 2024 Mar 28;14(1):7425. doi: 10.1038/s41598-024-58085-9.
6
Stability calculation method of slope reinforced by prestressed anchor in process of excavation.预应力锚索加固边坡在开挖过程中的稳定性计算方法
ScientificWorldJournal. 2014 Feb 11;2014:194793. doi: 10.1155/2014/194793. eCollection 2014.
7
Strengthening Device for Improving Shear Performance of Anchor Cable in Rock Support.用于提高岩石支护中锚索抗剪性能的增强装置
Materials (Basel). 2023 Dec 29;17(1):197. doi: 10.3390/ma17010197.
8
Shallow Failure of Weak Slopes in Bayan Obo West Mine.西矿包钢白云鄂博矿软弱边坡浅层破坏
Int J Environ Res Public Health. 2022 Aug 8;19(15):9755. doi: 10.3390/ijerph19159755.
9
Shaking table test on the seismic response of the portal section in soft and hard rock junction.软硬岩交界面处门型断面地震响应的振动台试验
Sci Prog. 2021 Jul-Sep;104(3):368504211031393. doi: 10.1177/00368504211031393.
10
Performance and reinforcement of air-cooled embankments traversing degrading permafrost of the Qinghai-Tibet Plateau.穿越青藏高原退化多年冻土的风冷路堤的性能与加固
Heliyon. 2024 Sep 28;10(19):e38304. doi: 10.1016/j.heliyon.2024.e38304. eCollection 2024 Oct 15.

引用本文的文献

1
Probabilistic failure assessment of bolt-stabilized pro-dip slopes considering shear effect.考虑剪切效应的锚杆稳定顺倾边坡概率失效评估
Sci Rep. 2025 May 26;15(1):18288. doi: 10.1038/s41598-025-02920-0.