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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Linear iterative refinement method for the rapid simulation of borehole nuclear measurements: Part 2 — High-angle and horizontal wells
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Linear iterative refinement method for the rapid simulation of borehole nuclear measurements: Part 2 — High-angle and horizontal wells

机译:快速模拟井孔核测量的线性迭代优化方法:第2部分:大角度和水平井

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摘要

Based on previous research, we developed and successfully tested a new linear iterative refinement method to rapidly simulate borehole nuclear measurements acquired in vertical wells. The approximation considers 2D spatial properties of Monte Carlo-derived flux-sensitivity functions FSFs to simulate neutron and density measurements. Based on new research, we implemented the linear iterative refinement method with explicit 3D spatial properties of FSFs to approximate nuclear borehole measurements acquired in high-angle and horizontal HA/HZ wells.We used generic neutron and density tools that are close to commercial tool designs to construct 3D FSFs in the proximity of a bed boundary between layers of contrasting petrophysical properties. Likewise, to benchmark the approximation, we consider adjacent layers of 5% and 30% porosity water-saturated sandstone. For the case of neutron measurements, variations of azimuthal geometric factors are as large as 20° and 57° for the near and far detectors, respectively. Variations in the radial length of investigation J-factors are as large as 3.61 cm for near and far detectors. In the case of density measurements, radial and azimuthal geometric factors are approximately invariant. Linear iterative refinement approximations yield errors in the simulated neutron porosity ranging from 1.6% to 4.3% with respect to Monte Carlo-simulated logs in wells deviating from 60° to 85° from the vertical.
机译:基于先前的研究,我们开发并成功测试了一种新的线性迭代优化方法,可以快速模拟在垂直井中采集的井眼核测量值。该近似值考虑了蒙特卡洛派生的通量敏感度函数FSF的二维空间特性,以模拟中子和密度测量。在新的研究基础上,我们利用FSF的显式3D空间特性实施了线性迭代细化方法,以近似于在高角度和水平HA / HZ井中获得的核井眼测量值。在具有不同岩石物理特性的层之间的床边界附近构造3D FSF。同样,为了近似,作为基准,我们考虑了孔隙度为5%和30%的水饱和砂岩的相邻层。对于中子测量,近,远探测器的方位角几何因子变化分别高达20°和57°。对于近距离和远距离探测器,调查J因子的径向长度变化高达3.61 cm。在密度测量的情况下,径向和方位角几何因子近似不变。相对于蒙特卡洛模拟的测井,与垂直方向偏离60°至85°的井,线性迭代精细修正近似值在模拟中子孔隙率中产生的误差为1.6%至4.3%。

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