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Low Frequency Modelling of Layered Media for Logging While Drilling Applications Using FDTD

机译:使用FDTD进行随钻测井的分层介质的低频建模

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In a typical Logging While Drilling (LWD) ap- plication, several coils operating in the frequency range of a few KHz to MHz are used as transmitters and receivers to appropriately characterize the earth formation. Electromagnetic modelling of such a low frequency system poses serious computational challenges. In the Method of Moment (MoM) formulation, contribution of vector potential to the total field becomes several orders of magnitude smaller than that of the scalar potential, thus making the resultant matrix highly ill-conditioned. Finite Difference Time Domain (FDTD) method, on the other hand, requires enormous number of time steps to capture the low frequency information. In this paper, we consider a layered-earth model and compute the electromagnetic field due to electric and magnetic dipoles embedded in the formation. To address the low frequency problem in FDTD, we consider the source and the receiver dipoles to be infinitesimally small and aligned with the computational grid, and we modify the update equations accordingly. This approach reduces the time convergence of FDTD by two-to-three orders of magnitude, and also reduces the memory requirements by the same factor. Numerical results for the fields reflected from the layered interfaces and the corresponding voltages induced in the receive coils are presented for multiple scenarios involving shale and sand zones.
机译:在典型的随钻测井(LWD)应用中,工作在几KHz至MHz频率范围内的几个线圈被用作发射器和接收器,以恰当地表征地层。这种低频系统的电磁建模带来了严重的计算挑战。在矩量法(MoM)中,矢量势对总场的贡献比标量势的贡献小几个数量级,从而使所得矩阵的状态极差。另一方面,时域有限差分(FDTD)方法需要大量的时间步长才能捕获低频信息。在本文中,我们考虑了层状地球模型,并计算了埋在地层中的电磁偶极子引起的电磁场。为了解决FDTD中的低频问题,我们认为源偶极子和接收偶极子非常小,并且与计算网格对齐,并相应地修改了更新方程。这种方法将FDTD的时间收敛减少了两个到三个数量级,并且将内存需求减少了相同的倍数。从分层界面反射的场的数值结果以及在接收线圈中感应的相应电压,针对涉及页岩和砂岩区域的多种情况,给出了数值结果。

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