In order to analyze mechanism of casing damage,the uniaxial compression experiment and creep experiment of interbedded mudstone samples from Sanan development area of Daqing Oilfield under different water contents wer...In order to analyze mechanism of casing damage,the uniaxial compression experiment and creep experiment of interbedded mudstone samples from Sanan development area of Daqing Oilfield under different water contents were carried out.The changes of the mudstone's mechanical parameters and creep characteristics with the increment of water saturation were studied.The results indicate that the rock strength and elastic modulus decrease rapidly with the increment of water content,at the same time,the creep strain and creep strain rate of steady state increase with the increment of water content,and also the steady state creep strain rate is enhanced with the increment of deviatoric stress.Through the creep characteristic curves,a non-linear creep constitutive equation of mudstone considering the change of water contents is established,which will be used in future numerical analysis.展开更多
On the basis of the creep test of bigh-water materisl solidifying backfill body(abb. HW body), This paper discusses its creep properties- The visco-elasto-plastic model, which shows the creep properties of HW body, is...On the basis of the creep test of bigh-water materisl solidifying backfill body(abb. HW body), This paper discusses its creep properties- The visco-elasto-plastic model, which shows the creep properties of HW body, is developed, and the creep contitutive equations are deduced. The visco-elastoplastic model is proved by the experiments and practice.展开更多
The rheological behavior of a soft interlayer is critical to understanding slope stability, which is closely related to the water content of the soft interlayer. This study used the soft interlayer of the Permian Maok...The rheological behavior of a soft interlayer is critical to understanding slope stability, which is closely related to the water content of the soft interlayer. This study used the soft interlayer of the Permian Maokou Formation in Southwest China as an example to perform ring shear creep tests with different water content amounts. The effect of water content on the creep properties of the soft interlayer was analyzed, and a new shear rheological model was established. This research produced several findings. First, the ring shear creep deformation of the soft interlayer samples varied with the water content and the maximum instantaneous shear strain increment occurred near the saturated water content. As the water content increased, the cumulative creep increment of the samples increased. Second, the water content significantly affected the long-term strength of the soft interlayer, which decreased with the increase of water content, exhibiting a negative linear correlation. Third, a constitutive equation for the new rheological model was derived, and through fitting of the ring shear creep test data, the validity and applicability of the constitutive equation were proven. This study has developed an important foundation for studying the long-term deformation characteristics of a soft interlayer with varying water content.展开更多
为探明库水位周期性升降作用下消落带岩体蠕变损伤机制,基于PFC中的平行黏结模型(parallel bond model,PBM),考虑水-岩作用对黏结的弱化和材料特性随时间的变化,提出水-岩作用下砂岩蠕变的离散元模拟方法,并在室内试验基础上开展水-岩...为探明库水位周期性升降作用下消落带岩体蠕变损伤机制,基于PFC中的平行黏结模型(parallel bond model,PBM),考虑水-岩作用对黏结的弱化和材料特性随时间的变化,提出水-岩作用下砂岩蠕变的离散元模拟方法,并在室内试验基础上开展水-岩作用下砂岩蠕变模拟。研究结果表明:在破坏应力水平下,试样微裂纹扩展与蠕变应变规律相似,可分为衰减扩展阶段、稳定扩展阶段、加速扩展阶段,且随水-岩作用周期增加,加速扩展阶段的耗时占总耗时的比例增大;试样蠕变破坏时,随水-岩作用周期增加,剪切裂纹占比逐渐增加,微裂纹倾角分布逐渐分散,倾角分布在65°和115°附近的微裂纹逐渐增加,试样的张性破坏减弱,剪性破坏增强;水-岩作用下,试样能储存的最大胶结能不断降低,且储存相同胶结能时对应的应变不断增大,与实际岸坡在水-岩作用下岩体整体承载能力降低、变形增大的规律一致。提出的水-岩作用下砂岩蠕变模拟方法具有较好的可行性,为库岸边坡岩石在库水位升降影响下的模型研究提供理论基础。展开更多
基金Project(2002CB412704) supported by the Major State Basic Research Development Program of China
文摘In order to analyze mechanism of casing damage,the uniaxial compression experiment and creep experiment of interbedded mudstone samples from Sanan development area of Daqing Oilfield under different water contents were carried out.The changes of the mudstone's mechanical parameters and creep characteristics with the increment of water saturation were studied.The results indicate that the rock strength and elastic modulus decrease rapidly with the increment of water content,at the same time,the creep strain and creep strain rate of steady state increase with the increment of water content,and also the steady state creep strain rate is enhanced with the increment of deviatoric stress.Through the creep characteristic curves,a non-linear creep constitutive equation of mudstone considering the change of water contents is established,which will be used in future numerical analysis.
文摘On the basis of the creep test of bigh-water materisl solidifying backfill body(abb. HW body), This paper discusses its creep properties- The visco-elasto-plastic model, which shows the creep properties of HW body, is developed, and the creep contitutive equations are deduced. The visco-elastoplastic model is proved by the experiments and practice.
基金supported by the National Natural Science Foundation of China(Grant No.41521001)the Natural Science Foundation of Hubei Province(Grant No.2018CFB385)
文摘The rheological behavior of a soft interlayer is critical to understanding slope stability, which is closely related to the water content of the soft interlayer. This study used the soft interlayer of the Permian Maokou Formation in Southwest China as an example to perform ring shear creep tests with different water content amounts. The effect of water content on the creep properties of the soft interlayer was analyzed, and a new shear rheological model was established. This research produced several findings. First, the ring shear creep deformation of the soft interlayer samples varied with the water content and the maximum instantaneous shear strain increment occurred near the saturated water content. As the water content increased, the cumulative creep increment of the samples increased. Second, the water content significantly affected the long-term strength of the soft interlayer, which decreased with the increase of water content, exhibiting a negative linear correlation. Third, a constitutive equation for the new rheological model was derived, and through fitting of the ring shear creep test data, the validity and applicability of the constitutive equation were proven. This study has developed an important foundation for studying the long-term deformation characteristics of a soft interlayer with varying water content.
文摘为探明库水位周期性升降作用下消落带岩体蠕变损伤机制,基于PFC中的平行黏结模型(parallel bond model,PBM),考虑水-岩作用对黏结的弱化和材料特性随时间的变化,提出水-岩作用下砂岩蠕变的离散元模拟方法,并在室内试验基础上开展水-岩作用下砂岩蠕变模拟。研究结果表明:在破坏应力水平下,试样微裂纹扩展与蠕变应变规律相似,可分为衰减扩展阶段、稳定扩展阶段、加速扩展阶段,且随水-岩作用周期增加,加速扩展阶段的耗时占总耗时的比例增大;试样蠕变破坏时,随水-岩作用周期增加,剪切裂纹占比逐渐增加,微裂纹倾角分布逐渐分散,倾角分布在65°和115°附近的微裂纹逐渐增加,试样的张性破坏减弱,剪性破坏增强;水-岩作用下,试样能储存的最大胶结能不断降低,且储存相同胶结能时对应的应变不断增大,与实际岸坡在水-岩作用下岩体整体承载能力降低、变形增大的规律一致。提出的水-岩作用下砂岩蠕变模拟方法具有较好的可行性,为库岸边坡岩石在库水位升降影响下的模型研究提供理论基础。
基金Project(52009131) supported by the National Natural Science Foundation of ChinaProject(GJNY-20-113-05) supported by the Open Funds of State Key Laboratory of Water Resource Protection and Utilization in Coal Mining,ChinaProject(2020RGET03) supported by the Fundamental Science on Radioactive Geology and Exploration Technology LaboratoryEast China University of Technology,China。