目的建立下颌第一前磨牙楔状缺损及不同材料嵌体修复后的三维有限元模型,并进行应力分析,以期为临床嵌体修复楔状缺损提供理论参考。方法通过CBCT扫描取得牙体原始数据,借助Mimics 17.0,Geomagic Studio 13.0等软件建立下颌第一前磨牙...目的建立下颌第一前磨牙楔状缺损及不同材料嵌体修复后的三维有限元模型,并进行应力分析,以期为临床嵌体修复楔状缺损提供理论参考。方法通过CBCT扫描取得牙体原始数据,借助Mimics 17.0,Geomagic Studio 13.0等软件建立下颌第一前磨牙楔状缺损模型及三维有限元模型,并分别进行树脂嵌体(A)、瓷嵌体(B)、金合金嵌体(C)修复,以未进行修复的楔状缺损模型作为对照组,再利用Abaqus 6.14有限元软件进行牙颈部的应力分析。结果从应力分布来看垂直载荷楔状缺损后剩余牙体组织及嵌体修复后模型均出现两个应力集中区,其中楔状缺损后剩余牙体组织模型主要应力集中在楔状缺损处,嵌体修复后模型主要应力在牙颈部,并发现不同材料嵌体修复后最大主应力值均明显降低。结论不同材料嵌体修复楔状缺损后可使缺损附近的应力集中明显改善,其中瓷嵌体(B)和金合金嵌体(C)与树脂嵌体(A)相比相对理想。展开更多
From Global Position System(GPS) measurements,there is a clockwise rotation around the eastern Himalayan syntax in the Tibetan Plateau.This phenomenon is difficult to be interpreted by simple two-dimensional modeling ...From Global Position System(GPS) measurements,there is a clockwise rotation around the eastern Himalayan syntax in the Tibetan Plateau.This phenomenon is difficult to be interpreted by simple two-dimensional modeling from a geodynamic point of view.Because of the extremely thick crust and the lower crust with relatively high temperature in the Tibetan Plateau,the lithospheric rheology in Tibet and surrounding areas present a complex structure.In general,the tectonic structure of the Tibetan Plateau consists of brittle upper crust,ductile lower crust,high viscosity lithospheric upper mantle,and low viscosity asthenosphere,the same as the case in many other continental regions.However,the lower crust in the Tibetan Plateau is much more ductile with a lower viscosity than those of its sur-roundings at the same depth,and the effective viscosity is low along the collision fault zone.In this study,we construct a three-dimensional Maxwell visco-elastic model in spherical coordinate system,and simulate the deformation process of the Tibetan Plateau driven by a continuous push from the Indian plate.The results show that the existence of the soft lower crust under the plateau makes the entire plateau uplift as a whole,and the Himalayas and the eastern Himalayan syntax uplift faster.Since the lower crust of surrounding blocks is harder except in the southeastern corner where the high-temperature material is much softer and forms an exit channel for material transfer,after the whole plateau reaches a certain height,the lower crustal and upper mantle material begins to move eastward or southeastward and drag the upper crust to behave same way.Thus,from the macroscopic point of view,a relative rigid motion of the plateau with a clockwise rotation around the eastern Himalayan syntax is developed.展开更多
文摘目的建立下颌第一前磨牙楔状缺损及不同材料嵌体修复后的三维有限元模型,并进行应力分析,以期为临床嵌体修复楔状缺损提供理论参考。方法通过CBCT扫描取得牙体原始数据,借助Mimics 17.0,Geomagic Studio 13.0等软件建立下颌第一前磨牙楔状缺损模型及三维有限元模型,并分别进行树脂嵌体(A)、瓷嵌体(B)、金合金嵌体(C)修复,以未进行修复的楔状缺损模型作为对照组,再利用Abaqus 6.14有限元软件进行牙颈部的应力分析。结果从应力分布来看垂直载荷楔状缺损后剩余牙体组织及嵌体修复后模型均出现两个应力集中区,其中楔状缺损后剩余牙体组织模型主要应力集中在楔状缺损处,嵌体修复后模型主要应力在牙颈部,并发现不同材料嵌体修复后最大主应力值均明显降低。结论不同材料嵌体修复楔状缺损后可使缺损附近的应力集中明显改善,其中瓷嵌体(B)和金合金嵌体(C)与树脂嵌体(A)相比相对理想。
基金Supported by Knowledge Innovation Project of the Chinese Academy of Sciences (Grant No.KZCX2-YW-123)National Natural Science Foundation of China (Grant Nos.40774048 and 90814014)
文摘From Global Position System(GPS) measurements,there is a clockwise rotation around the eastern Himalayan syntax in the Tibetan Plateau.This phenomenon is difficult to be interpreted by simple two-dimensional modeling from a geodynamic point of view.Because of the extremely thick crust and the lower crust with relatively high temperature in the Tibetan Plateau,the lithospheric rheology in Tibet and surrounding areas present a complex structure.In general,the tectonic structure of the Tibetan Plateau consists of brittle upper crust,ductile lower crust,high viscosity lithospheric upper mantle,and low viscosity asthenosphere,the same as the case in many other continental regions.However,the lower crust in the Tibetan Plateau is much more ductile with a lower viscosity than those of its sur-roundings at the same depth,and the effective viscosity is low along the collision fault zone.In this study,we construct a three-dimensional Maxwell visco-elastic model in spherical coordinate system,and simulate the deformation process of the Tibetan Plateau driven by a continuous push from the Indian plate.The results show that the existence of the soft lower crust under the plateau makes the entire plateau uplift as a whole,and the Himalayas and the eastern Himalayan syntax uplift faster.Since the lower crust of surrounding blocks is harder except in the southeastern corner where the high-temperature material is much softer and forms an exit channel for material transfer,after the whole plateau reaches a certain height,the lower crustal and upper mantle material begins to move eastward or southeastward and drag the upper crust to behave same way.Thus,from the macroscopic point of view,a relative rigid motion of the plateau with a clockwise rotation around the eastern Himalayan syntax is developed.
