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考虑水软化作用的片麻岩内部损伤演化研究

Investigation of internal damage evolution in gneiss considering water softening.

作者信息

Sun Changhai, Xie Bingxin, Wang Rui, Deng Xianghui, Wu Jin

机构信息

Shaanxi Transportation Holding Group Co., Ltd., Xi'an, 710065, China.

School of Civil and Architecture Engineering, Xi'an Technological University, Xi'an, 710021, China.

出版信息

Sci Rep. 2023 Aug 4;13(1):12672. doi: 10.1038/s41598-023-39664-8.

Abstract

In soft rock tunnels, there are often large deformations during construction, especially when the groundwater seepage and softens the surrounding rock. For achieving the purpose of studying the softening effect of water immersion on strength and stability of surrounding rock, 15 rock samples were selected for physical and mechanical tests under 5 conditions: natural state and free immersion for 1, 3, 6, and 9 months, and nuclear magnetic resonance technology(NMR) was also adopted to test the internal pore structure of specimens with different immersion durations, thus the micro structure features of the gneiss, such as the NMR relaxation time T2 spectrum distribution, porosity, and pore volume ratio of different pore sizes under water softening were then obtained. The NMR results shows that the longer the free immersion duration of the rock sample, the greater the porosity; at the same time, the number of micropores in the rock gradually decreases under the interaction of water and rock, and the mesopores increase slightly first and then decrease all the time. The number of macropores is gradually increasing. When the immersion duration is 6 months, the number of macropores begins to increase significantly, and the mechanical properties of the specimens begin to drop significantly. By 9 months, the proportion of macropores in the rock has reached 57.6%. The results showed that the number growth of macropores is the root cause of the macroscopic failure of rock sample. The study results have significance for on-site construction in water-rich areas.

摘要

在软岩隧道施工过程中,常常会出现大变形,尤其是当地下水渗流并使围岩软化时。为了研究水浸对围岩强度和稳定性的软化作用,选取了15块岩石样本,在天然状态以及自由浸泡1个月、3个月、6个月和9个月这5种条件下进行物理力学试验,还采用核磁共振技术(NMR)对不同浸泡时长的试样内部孔隙结构进行测试,从而得到片麻岩在水软化作用下的微观结构特征,如NMR弛豫时间T2谱分布、孔隙率以及不同孔径的孔隙体积比。核磁共振结果表明,岩石样本的自由浸泡时间越长,孔隙率越大;同时,在水与岩石的相互作用下,岩石中的微孔数量逐渐减少,中孔先略有增加而后一直减少,大孔数量则逐渐增加。当浸泡时长为6个月时,大孔数量开始显著增加,试样的力学性能也开始显著下降。到9个月时,岩石中大孔的比例已达57.6%。结果表明,大孔数量的增长是岩石样本宏观破坏的根本原因。该研究结果对富水地区的现场施工具有重要意义。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/271f/10403494/73a243438193/41598_2023_39664_Fig1_HTML.jpg

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