Water-and-mud inrush disasters have become a major challenge in underground engineering for the construction of tunnels in sandstone and slate interbedded Presinian strata.Disaster prediction and prevention rely in pa...Water-and-mud inrush disasters have become a major challenge in underground engineering for the construction of tunnels in sandstone and slate interbedded Presinian strata.Disaster prediction and prevention rely in part on realistic modeling and observation of the disaster process,as well as the identification and examination of the underlying mechanisms.Based on the geological conditions and the historical records of the Xinping Tunnel on the China–Laos Railway,an engineering geological model of the water-and-mud inrush was established.A physical model test that accurately reproduced water-and-mud inrush during tunnel excavation in sandstone and slate interbedded strata was also carried out.Then,testing was conducted that examined the stress and strain,seepage pressure,and high-leakage flow of the surrounding rock.The results indicated that the water-and-mud inrush proceeded through three stages:seepage stage,high-leakage flow stage,and attenuation stage.In essence,the disaster was a catastrophic process,during which the water-resistant stratum was reduced to a critical safety thickness,a water-inrush channel formed,and the water-resistant stratum gradually failed under the influence of excavation unloading and in situ stress–seepage coupling.Parameters such as the stress and strain,seepage pressure,and flow of the surrounding rock had evident stage-related features during water-and-mud inrush,and their variation indicated the formation,development,and evolution of the disaster.As the tunnel face advanced,the trend of the stress–strain curve of the surrounding rock shifted from sluggish to rapid in its speed of increase.The characteristics of strain energy density revealed the erosion and weakening effect of groundwater on the surrounding rock.The seepage pressure and the thickness of the water-resistant stratum had a positive linear relationship,and the flow and thickness a negative linear relationship.There was a pivotal point at which the seepage pressure changed from high to low and the flow shifted from low to high.The thickness of the water-resistant stratum corresponding to the pivotal point was deemed the critical safety thickness.展开更多
Helium in China highly depends on import at present,so the most practical way to change the situation is searching for medium-to-large natural gasfields with high helium content.Therefore,the hydrocarbon accumulation ...Helium in China highly depends on import at present,so the most practical way to change the situation is searching for medium-to-large natural gasfields with high helium content.Therefore,the hydrocarbon accumulation mechanism and the helium origin of the Weiyuan high-helium natural gas reservoir have been analyzed tofind out the feasibility offinding natural gasfield with high helium content in the Presinian strata of the Sichuan Basin.Based on twelve outcrop sections and drilling data of four wells encountering the Presinian strata,the petrological features,sedimentary facies and source rocks of Presinian strata were systematically analyzed,which shows that the sedimentary formation developed in the Presinian is the Nanhua system,and the stratigraphic sequence revealed by outcrop section in the eastern margin includes the Nantuo,Datangpo,Gucheng and Liantuo Fms,and it is inferred that the same stratigraphic sequence may occur inside the basin.The Nantuo,Gucheng and Liantuo Fms are mainly glacial deposits of glutenite interbedded with mudstone;the Datangpo Fm is interglacial deposits of sandstone and shale,the lower part shale,rich in organic matter,is fairly good source rock.Further study showed that the Nantuo coarse-grained clastic reservoir,Datangpo source rock and the intruded granite“helium source rock”make up a good high-helium gas system.Controlled by the early rift,the thick Presinian sedimentary rocks occur primarily inside the rift.The distribution of sedimentary rocks and granite in the basin was predicted by use of the seismic data,which shows that the feasibility offinding high-helium gas reservoirs in Ziyang area of the Sichuan Basin is great.展开更多
基金the National High-Speed Rail United Foundation of China(No.U1934213)。
文摘Water-and-mud inrush disasters have become a major challenge in underground engineering for the construction of tunnels in sandstone and slate interbedded Presinian strata.Disaster prediction and prevention rely in part on realistic modeling and observation of the disaster process,as well as the identification and examination of the underlying mechanisms.Based on the geological conditions and the historical records of the Xinping Tunnel on the China–Laos Railway,an engineering geological model of the water-and-mud inrush was established.A physical model test that accurately reproduced water-and-mud inrush during tunnel excavation in sandstone and slate interbedded strata was also carried out.Then,testing was conducted that examined the stress and strain,seepage pressure,and high-leakage flow of the surrounding rock.The results indicated that the water-and-mud inrush proceeded through three stages:seepage stage,high-leakage flow stage,and attenuation stage.In essence,the disaster was a catastrophic process,during which the water-resistant stratum was reduced to a critical safety thickness,a water-inrush channel formed,and the water-resistant stratum gradually failed under the influence of excavation unloading and in situ stress–seepage coupling.Parameters such as the stress and strain,seepage pressure,and flow of the surrounding rock had evident stage-related features during water-and-mud inrush,and their variation indicated the formation,development,and evolution of the disaster.As the tunnel face advanced,the trend of the stress–strain curve of the surrounding rock shifted from sluggish to rapid in its speed of increase.The characteristics of strain energy density revealed the erosion and weakening effect of groundwater on the surrounding rock.The seepage pressure and the thickness of the water-resistant stratum had a positive linear relationship,and the flow and thickness a negative linear relationship.There was a pivotal point at which the seepage pressure changed from high to low and the flow shifted from low to high.The thickness of the water-resistant stratum corresponding to the pivotal point was deemed the critical safety thickness.
文摘Helium in China highly depends on import at present,so the most practical way to change the situation is searching for medium-to-large natural gasfields with high helium content.Therefore,the hydrocarbon accumulation mechanism and the helium origin of the Weiyuan high-helium natural gas reservoir have been analyzed tofind out the feasibility offinding natural gasfield with high helium content in the Presinian strata of the Sichuan Basin.Based on twelve outcrop sections and drilling data of four wells encountering the Presinian strata,the petrological features,sedimentary facies and source rocks of Presinian strata were systematically analyzed,which shows that the sedimentary formation developed in the Presinian is the Nanhua system,and the stratigraphic sequence revealed by outcrop section in the eastern margin includes the Nantuo,Datangpo,Gucheng and Liantuo Fms,and it is inferred that the same stratigraphic sequence may occur inside the basin.The Nantuo,Gucheng and Liantuo Fms are mainly glacial deposits of glutenite interbedded with mudstone;the Datangpo Fm is interglacial deposits of sandstone and shale,the lower part shale,rich in organic matter,is fairly good source rock.Further study showed that the Nantuo coarse-grained clastic reservoir,Datangpo source rock and the intruded granite“helium source rock”make up a good high-helium gas system.Controlled by the early rift,the thick Presinian sedimentary rocks occur primarily inside the rift.The distribution of sedimentary rocks and granite in the basin was predicted by use of the seismic data,which shows that the feasibility offinding high-helium gas reservoirs in Ziyang area of the Sichuan Basin is great.
