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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Estimating petrophysical parameters and average mud-filtrate invasion rates using joint inversion of induction logging and pressure transient data
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Estimating petrophysical parameters and average mud-filtrate invasion rates using joint inversion of induction logging and pressure transient data

机译:利用感应测井和压力瞬变数据联合反演估算岩石物理参数和平均泥浆渗透率

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摘要

We introduce an inversion approach for determining the water-based mud-filtrate invasion profile, as well as the formation porosity and horizontal permeability, from the induction logging data. The inversion is constrained by a multiphase fluid flow simulator that simulates the mud-filtrate invasion process to obtain the spatial distributions of the water saturation and the salt concentration, which are in turn transformed into the formation resistivity using a resistivity-saturation formula. By ignoring the diffusion effect, we assume that the mud-filtrate invasion process is mainly convective so that it can be equivalently simulated by providing an average invasion rate and the duration of invasion. The average invasion rate can be directly inverted from the fluid-flow-constrained inversion of induction logging data. We also obtain the mud-filtrate invasion profile, which is consistent with the fluid flow physics. The reconstructed mud-filtrate invasion profile benefits the interpretation of the formation test. When the pressure transient data are available, this approach can be also used to jointly invert both induction logging data and pressure transient data to obtain the mud-filtrate invasion profile, as well as a parametric distribution of the TI-anisotropic formation permeability and porosity. Assuming a vertical well penetrating horizontal formations, the fluid flow problem is solved using an implicit black oil finite-difference simulator with brine tracking option based on a cylindrical, axially symmetric grid, whereas the response of the induction logging tool is simulated using a frequency-domain finite-difference solver based on a Cartesian grid. A Gauss-Newton inversion scheme using the multiplicative regularization technique is used for either the fluid-flow-constrained inversion or the joint inversion. The reliability of the inversion results depends on the accuracy of a priori knowledge of the reservoir, which needs to be confirmed via sensitivity analysis.
机译:我们引入一种反演方法,根据感应测井数据确定水基泥浆滤液的侵入剖面以及地层孔隙度和水平渗透率。该反演受多相流体流动模拟器的约束,该模拟器模拟泥浆滤液的侵入过程,以获得水饱和度和盐分浓度的空间分布,然后使用电阻率-饱和度公式将其转换为地层电阻率。通过忽略扩散效应,我们假设泥浆滤液的侵入过程主要是对流的,因此可以通过提供平均侵入速率和侵入持续时间来等效地模拟它。平均侵入率可以直接从流体流量约束的感应测井数据反演得到。我们还获得了泥浆滤液的侵入剖面,这与流体流动物理学相一致。重建的泥浆滤液侵入剖面有利于解释地层试验。当压力瞬变数据可用时,该方法还可用于联合反演感应测井数据和压力瞬变数据,以获得泥浆滤液侵入剖面以及TI各向异性地层渗透率和孔隙度的参数分布。假设垂直井穿透水平地层,则使用隐式黑油有限差分模拟器(基于圆柱形轴向对称网格的盐水跟踪选项)解决流体流动问题,而感应测井工具的响应则使用频率-笛卡尔网格的有限域有限差分求解器。使用乘法正则化技术的高斯-牛顿反演方案可用于流体流约束反演或联合反演。反演结果的可靠性取决于储层先验知识的准确性,这需要通过敏感性分析加以确认。

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