Simulation of Electromagnetic Wave Logging Response in Deviated Wells Based on Vector Finite Element Method

The vector finite element method of tetrahedral elements is used to model 3D electromagnetic wave logging response. The tangential component of the vector field at the mesh edges is used as a degree of freedom to overcome the shortcomings of node-based finite element methods. The algorithm can simulate inhomogeneous media with arbitrary distribution of conductivity and magnetic permeability. The electromagnetic response of well logging tools are studied in dipping bed layers with the borehole and invasion included. In order to simulate realistic logging tools, we take the transmitter antennas consisting of circular wire loops instead of magnetic dipoles. We also investigate the apparent resistivity of inhomogeneous formation for different dip angles.     

二维板声发射源定位实验的一种简易实现方法

对声发射技术中的二维平面定位问题提出一种新的简易实验方案.采用新三角时差算法实现二维板的声源定位和GPS模拟,同时利用简易实验方法,仅用两个超声波传感器完成实验,简化实验器材,降低实验成本,适合普及,计算过程简单,同时也利于物理问题深入地理解.     

利用井孔偶极弯曲波反演横向各向同性孔隙地层渗透率的研究

对利用井孔偶极弯曲波衰减特性反演横向各向同性孔隙地层的纵、横向渗透率进行了理论方法和数值研究.对软地层,在方差函数极值行为分析的基础上,用最小二乘反演对多组理论模拟数据进行处理,得到的纵、横向渗透率精度都比较高,这与软地层弯曲波衰减对纵向渗透率的敏感程度明显比硬地层高有关;用添加不同强度的随机噪声综合反映现场资料可能带来的误差,对多道间提取的衰减叠加求平均可明显的抵消噪声的影响;对快速孔隙地层偶极声测井理论模拟数据也尝试性地进行了纵、横向渗透率反演,发现,虽然硬地层弯曲波的衰减对纵向渗透率很不敏感,但纵向渗透率的取值偏离真值却对横向渗透率的反演结果有明显影响.     

Seismoelectric waves in a borehole excited by an external explosive source

The conversion of energy between seismic and electromagnetic wave fields has been described by Pride’s coupled equations in porous media. In this paper, the seismoelectric field excited by the explosive point source located at the outside of the borehole is studied. The scattering fields inside and outside a borehole are analyzed and deduced under the boundary conditions at the interface between fluid and porous media. The influences of the distance of the point source, multipole components of the eccentric explosive source, and the receiving position along the axis of vertical borehole, on the converted waves inside the borehole are all investigated. When the distance from the acoustic source to the axis of a borehole is far enough, the longitudinal and coseismic longitudinal wave packets dominate the acoustic and electric field, respectively. The three components of both electric field and magnetic field can be detected, and the radial electric field is mainly excited and converted by the dipole component. Owing to the existence of borehole, the electric fields and magnetic fields in the borehole are azimuthal. The distance from the point where the maximum amplitude of the axial components of electric field is recorded, to the origin of coordinate indicates the horizontal distance from the explosive source to the axis of vertical borehole.