The spatiotemporal characteristics of a rockburst, such as the distance from the tunnel face, are critical factors related to early warning and control. Therefore, by using the data from over 100 immediate strain rockbursts (ISRs) in three open tunnel boring machine (TBM) granite tunnels, the relationships among their occurrence locations and TBM shield, their impact and control measures are statistically analyzed. The ISRs in open TBM tunnels are categorized into shield area ISRs (SA-ISRs) and main beam area ISRs (MBA-ISRs). The differences in the spatiotemporal characteristics, rockburst pit evolution characteristics and microseismic (MS) activity laws of these two types of ISRs are further analyzed. IS-ISRs occur earlier, and mainly form V-type pits without expansion. MBA-ISRs occur later, with a high proportion of fossa-type pits with more obvious expansion. MS nucleation in the SA-ISR area is high after excavation, with MS activity increasing rapidly and peaking. In contrast, the MS events in the MBA-ISR area are scattered, and MS activity is weak during excavation, gradually increases over time and continues to accumulate in space. On this basis, the influence mechanism of stress level, lithology, structural planes, and construction factors on the spatiotemporal characteristics of ISRs is studied, with the overall stress level identified as the main factor. When the stress level is high, the degree of energy accumulation increases after excavation, making it easier for SA-ISR to occur. Conversely, the degree of energy accumulation after excavation is lower. However, due to the influence of the nearby steep structural plane, energy continues to accumulates during the stress adjustment process in this area, resulting in a delay in MBA-ISR.
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