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Automated Geologically-Consistent History Matching of Facies Distribution and Reservoir Properties in Inter-Well Space by Adjoint Methods

机译:通过伴随方法自动化地质 - 一致的历史匹配井间空间中的相片分布和储层特性

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Comprehensive geological analysis at the stage of 3D geological modeling is necessary to obtain a high- quality flow model. The next important step is history matching to dynamic well data without distortion of the initial geological basis of the model. It is necessary to preserve static data on facies indexes, porosity and other parameters in the well gridcells, adjusting their distributions in the inter-well space, while maintaining the geological concepts of the object. The purpose of the study presented in this paper was the development of automated computationally efficient algorithms for solving this problem. Earlier, based on the computationally efficient adjoint methods, we developed algorithms and their implementation in the in-house SimMatch~R simulator for geologically consistent history matching with identification of parameters of the variograms and porosity-to-permeability relations for a given distribution of facies in the inter-well space. In this study, we make transition from the discrete representation of facies at wells to the continuous values in the inter-well space reflecting the fractional contribution of the facies in the formation of model cell properties. Considering implicit parametric dependencies on static data at wells and variogram parameters for properties and facies, a computationally efficient algorithm was developed for consistent adjustment of the distributions of facies and reservoir properties during history matching of the 3D model. The algorithms developed are implemented within the frameworks of the forward and inverse problems. In the forward problem, a distribution of a continuous facies parameter is constructed, taking into account well data and the variogram for the facies. In current implementation, the continuous "facie" value is interpreted as being transitional (weighted) between the adjacent integer values, which is typical for geological environments with sequential change of facies usually modeled by methods such as the truncated Gaussian simulation. Further, for each facie, distribution of the reservoir parameters (porosity, permeability) is independently constructed, taking into account the variogram for porosity and the porosity- to-permeability relation for this facie. The resulting property value in each cell is determined by weighing by the portions of the "pure" facies. Within the framework of the inverse problem, the parameters of anisotropic variograms for the facies and for the reservoir properties within each facie, as well as the coefficients in the porosity-to-permeability relation for each facie, serve as the control parameters. For efficient implementation of the automated gradient procedure for adjustment control parameters, the adjoint problem is solved at each iteration, and the object function gradient with respect to the control parameters is calculated taking into account the implicit dependencies of the reservoir properties in the model cells on the variogram parameters for the facies and reservoir properties. The results of approbation of the approach on a realistic example of the 3D reservoir model and on a 3D model of a real deposit section are presented. During the study, effecient algorithms for consistent adjustment of the facies and reservoir properties distributions in a 3D model were for the first time constructed on the basis of adjoint methods and implemented in the in-house simulator. The advantage of the approach is the significant reduction in computational costs (number of simulator runs) for solution of the inverse problem in comparison with alternative methods of automated history matching, while preserving the consistency of the facies and reservoir properties distributions with the original principles of the geological model construction.
机译:在3D地质模型阶段进行综合地质分析,是获得高质量的流动模型。下一个重要步骤是历史与动态井数据匹配而没有模型的初始地质基础的失真。有必要保留井栅格中的相位指数,孔隙度和其他参数的静态数据,调整它们在井间空间中的分布,同时保持对象的地质概念。本文介绍了该研究的目的是开发自动化计算有效算法,以解决这个问题。早些时候,根据计算有效的伴随方法,我们开发了在内部Simmatch〜R模拟器中开发了算法及其在地质上一致的历史匹配,其识别变速仪和孔隙率和孔隙率关系的参数,以及给定的相片在井间空间中。在这项研究中,我们从井间的离散表示转变为井间空间中的连续值,反映了面部在模型细胞性质的形成中的小数贡献。考虑到隐式参数依赖性在井的静态数据和变速仪参数的性质和相参数,开发了一种计算有效的算法,以一致地调整3D模型的历史匹配期间的面部和储层特性的分布。开发的算法在前向和逆问题的框架内实现。在前向问题中,构建连续面部参数的分布,考虑到井数据和面部的变形仪。在当前实现中,将连续的“面部”值被解释为在相邻的整数值之间的过渡(加权),这对于具有由诸如截断的高斯模拟等方法建模的相似的地质环境的典型地质环境。此外,对于每个面,考虑到孔隙率和该面的孔隙率关系的变形仪,考虑到储层参数(孔隙率,渗透率)的分布。通过由“纯”相的部分称重来确定每个单元中所得到的属性值。在逆问题的框架内,每个面部的各向异性变速器和用于每个面内的储存性能的参数,以及每个面部的孔隙磁性关系中的系数用作控制参数。为了有效地实现调整控制参数的自动梯度过程,在每次迭代时求解伴随问题,并且考虑到模型单元中的储库属性的隐式依赖性,计算相对于控制参数的对象功能梯度面部和储层属性的变形仪参数。介绍了在3D储层模型和实际沉积部分的3D模型的现实示例中对方法的认可结果。在研究期间,在3D模型中的相和储库特性分布的一致调整的有效算法是在伴随方法的基础上构建并在内部模拟器中实现的第一次。该方法的优点是与自动历史匹配的替代方法相比,用于解决逆问题的计算成本(模拟器数量)的显着降低,同时保留了具有原始原理的相和水库属性分布的一致性地质模型建设。

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