在复杂的地质条件下研究超深软岩道的应力和变形特性
Qi-Bing Zhan1,2, Lei Tang3,4, Yu-Kun Wang2,5
1State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan, 430072, China.
Scientific reports
|November 21, 2024
概括
这项对深道的研究表明,周围的岩石挤出会导致压力和孔水压力增加. 分段支有效控制变形,特别是在道腰部.
科学领域:
- 地质技术工程 地质技术工程
- 道工程 道工程是指道工程.
- 水文地质学 水文地质学
背景情况:
- 深度道面临复杂的压力条件,由于高位压力和孔水压力,威胁到水输送安全.
- 达通河到黄河分流道带来了超级深度和复杂的地质挑战.
研究的目的:
- 在不对称的3D高现场应力和孔隙水压下,在软岩道中调查应力变形和损伤演变.
- 分析道周围岩石上的段支措施的有效性.
主要方法:
- 开发了一种参数反转方法,其中包含了多点周围岩石变形.
- 考虑了流体结构相互作用效应来分析应力变形特征.
- 在不同的现场应力和孔隙水压下分析了损害演变.
主要成果:
- 周围强烈的岩石挤出导致体积压缩,导致应力度和多余的孔水压.
- 最大的变形和涌水潜力发生在道腰部.
- 分段支显著控制了周围岩石变形,在道腰部显著减少了干扰深度.
结论:
- 道周围的岩石损伤深度与现场应力和孔隙水压正相关,现场应力是主要因素.
- 分段支对于缓解道变形和深处高压环境中的损伤至关重要.
- 调查结果为类似的深建设项目提供了宝贵的见解.
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