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Localized Computation of Newton Updates for General Fully-implicit Reservoir Simulation

机译:一般完全隐式储层模拟的牛顿更新的本地化计算

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Reported observations suggest that Newton updates that are computed during the course of a fully-implicit time step are often sparse. The level of sparsity can vary dramatically from nonlinear iteration to the next. and across time steps. Reported observations suggest that the level of sparsity can be as large as 95%. This work develops an algorithm that accurately predetermines the nonzero elements of the Newton update, and subsequently, can compute it by only solving a truncated linear system. Several alternative ad hoc sparsity prediction strategies have been proposed. Due to their inability to consistently and accurately predetermine the sparsity set. the resulting Newton updates that are computed are inaccurate, leading to a severe degradation of the nonlinear convergence rate. An exact strategy based on an analysis of the sparsity graph of the Jacobian matrix was also proposed for two phase incompressible flow without gravity. Although exact, the proposed strategy cannot be generalized to more complex physics or numerical approximations Recently, a theoretically sharp and conservative estimate for the sparsity set was derived specifically for the pressure and saturation variables in two-phase sequential-implicit simulation. In this strategy, the discrete Newton update was related to analytical solutions of linear Partial Differential Equations for flow and transport independently. The analytical solutions were evaluated and projected onto the computational domain, thereby providing an estimate of the sparsity set. The theoretically reliable algorithm was demonstrated to reduce the sequential-implicit simulation time for general two phase flow in the full SPE 10 comparative geological model by 5 fold In this work, the approach is extended to general fully-implicit simulation of coupled flow and mullicomponent transport. This is accomplished by considering a canonical functional form of the equations for flow and a system of transported quantities. The analytical estimate is derived by solving the system of linear differential equations using the Schur complement decomposition in functional space. When applied to various simulations of three-phase flow recovery processes in the full SPE 10 model, the observed reduction in computational effort ranged between four and tenfold depending on the level of total compressibility in the system and on the time step size. To investigate the scalability of the algorithm, we applied it to refined models of the SPE 10 case and to multicomponent problems. The improvement in computational speed scales strongly with the number of transport components, and to a lesser degree with problem size.
机译:报告的观察结果表明,在完全隐式时间步长过程中计算的牛顿更新通常是稀疏的。稀疏性水平可以从非线性迭代到下一个速度急剧变化。并跨越时间步骤。报告的观察结果表明,稀疏程度可以大约95%。这项工作开发了一种准确地预先确定牛顿更新的非零元素的算法,随后可以通过求解截断的线性系统来计算它。已经提出了几种替代的临时稀疏预测策略。由于它们无法持续准确地预先确定稀疏结构。由此产生的牛顿更新是不准确的,导致非线性收敛速度的严重降解。还提出了一种基于雅可比基质的稀疏性图的分析的精确策略,用于两个没有重力的两相可不可压缩的流动。尽管精确地,所提出的策略近来不能推广到更复杂的物理学或数值近似,但是对于两相顺序隐式仿真中的压力和饱和变量来得出对稀疏结构的理论上急剧和保守的估计。在该策略中,离散牛顿更新与独立流动和运输的线性部分微分方程的分析解。评估分析溶液并投影到计算结构域上,从而提供稀疏结构的估计。证明了理论上可靠的算法,以减少整个SPE 10比较地质模型中的一般两相流量的顺序隐式模拟时间5倍,该方法延伸到耦合流动和脉冲运输的一般完全隐含模拟。这是通过考虑用于流动的方程的规范功能形式和运输量的系统来实现。通过使用功能空间中的SCUR补充分解来解决线性微分方程的系统来源的分析估计。当应用于完整SPE 10模型中的三相流恢复过程的各种模拟时,根据系统中的总可压缩性和时间步长,观察到的计算工作的减少范围在四个和十倍之间。为了调查算法的可扩展性,我们将其应用于SPE 10案例的精制模型和多组分问题。计算速度的改善强烈地缩小了传输组件的数量,并且具有问题大小的较小程度。

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