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Sensitivity analyses of random cave groups on karst tunnel stability based on water–rock interaction using a novel contact dynamic method
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作者 Chengzhi Xia Zhenming Shi +2 位作者 Huanjia Kou Shaoqiang Meng Maomao Liu 《Underground Space》 SCIE EI CSCD 2024年第5期162-186,共25页
This paper concentrates on the sensitivity and dynamic simulation of randomly distributed karst cave groups on tunnel stability and connectivity extended ratio based on water–rock interaction using a novel contact dy... This paper concentrates on the sensitivity and dynamic simulation of randomly distributed karst cave groups on tunnel stability and connectivity extended ratio based on water–rock interaction using a novel contact dynamic method(CDM).The concept of karst cave group connectivity extended ratio during tunneling and water inrush is proposed.The effects of cave shape and spatial distribution on Qiyueshan tunnel are investigated.Tunnel deformation and damage index,and connectivity extended ratio with uniform random karst cave groups are evaluated.The results demonstrate that the connectivity extended ratio is verified as a crucial judgment in predicting the safe distance and assessing the stability of the tunnel with the karst cave group.CDM model captures the fracture propagation and contact behavior of rock mass,surface flow,as well as the bidirectional water–rock interaction during the water inrush of Qiyueshan tunnel with multiple caves.A larger cave radius and smaller minimum distance between the cave and tunnel increase the deformation and damage index of the surrounding rock.When the cave radius and cave area ratio increase,the failure pattern shifts from overall to local failure.These findings potentially have broad applications in various surface and subsurface scenarios involving water–rock interactions. 展开更多
关键词 Karst tunnel stability Contact dynamic method Connectivity extended ratio Karst cave groups Qiyueshan tunnel water-rock interaction
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确定砂岩型铀矿体定位新方法——水岩体系Eh-pH法 被引量:8
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作者 刘金辉 孙占学 《吉林大学学报(地球科学版)》 EI CAS CSCD 北大核心 2004年第1期44-48,共5页
水岩体系EhpH方法是根据水岩相互作用原理,来确定砂岩型铀矿体定位的一种新方法。研究结果表明:从氧化带到还原带,水岩体系Eh值明显下降,同一氧化还原环境水岩体系Eh平均值极为接近;不同氧化还原环境,其水岩体系pH值亦有所不同,氧化带... 水岩体系EhpH方法是根据水岩相互作用原理,来确定砂岩型铀矿体定位的一种新方法。研究结果表明:从氧化带到还原带,水岩体系Eh值明显下降,同一氧化还原环境水岩体系Eh平均值极为接近;不同氧化还原环境,其水岩体系pH值亦有所不同,氧化带和还原带处于弱碱性介质环境,过渡带(矿化地段)处于中性介质环境;水岩体系Eh和pH值可以作为划分含矿层氧化还原环境分带及圈定铀矿体位置的重要依据。 展开更多
关键词 水岩体系Eh-pH法 砂岩型铀矿 氧化还原分带 水岩相互作用 矿体定位
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