2019
DOI: 10.1088/1751-8121/ab1100
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Pressure statistics from the path integral for Darcy flow through random porous media

Abstract: The path integral for classical statistical dynamics is used to determine the properties of one-dimensional Darcy flow through a porous medium with a correlated stochastic permeability for several spatial correlation lengths. Pressure statistics are obtained from the numerical evaluation of the path integral by using the Markov chain Monte Carlo method. Comparisons between these pressure distributions and those calculated from the classic finite-volume method for the corresponding stochastic differential equat… Show more

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Cited by 2 publications
(8 citation statements)
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“…Correlations have a pronounced effect of the variations of the conductivity [32], so in this section, we introduce a finite correlation length to the fluctuations to determine its effect on the RG transformations. We consider a system with a finite isotropic correlation length l by defining the correlation function as…”
Section: Finite Correlation Lengthmentioning
confidence: 99%
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“…Correlations have a pronounced effect of the variations of the conductivity [32], so in this section, we introduce a finite correlation length to the fluctuations to determine its effect on the RG transformations. We consider a system with a finite isotropic correlation length l by defining the correlation function as…”
Section: Finite Correlation Lengthmentioning
confidence: 99%
“…We have at our disposal calculations in 1, 2, and 3 dimensions [32,33], so we can investigate the dimensional dependence of the accuracy of our calculations. As noted in the Introduction, RG equations in different spatial dimension have the same diagrammatic structure, but the methods used for the numerical valuation of the path integral are different in d = 1 [32] and d = 2 and d = 3 [33]. This should provide an additional point of interest for our comparisons.…”
Section: Summary and Future Workmentioning
confidence: 99%
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“…The foregoing scenarios span several areas of science and engineering and have led to the implementation of a broad range of theoretical and computational methods [1]. Foremost among these are molecular dynamics [15], lattice Boltzmann methods [16][17][18], fluid dynamics (computational and theoretical) [16,19], path integral [20][21][22], finite-volume [23] and finiteelement [24] methods, and continuous-time random walk theory [25][26][27][28]. These techniques model flow through porous media at various levels of spatial and temporal resolution, ranging from the scale of individual pores to macroscopic pressure and flow rates.…”
Section: Introductionmentioning
confidence: 99%
“…In previous work [22,35], we formulated the solution to one-dimensional Darcy flow in a random porous medium as a path integral over pressure paths within the medium. In discrete form, the path integral is a tool to simulate Darcy pressure paths {p i } on a spatial lattice using Markov chain Monte Carlo methods according to the weighting e −S , where the 'action' S = S({p i }) restricts the paths to follow Darcy's law in the presence of quenched stochastic permeability.…”
Section: Introductionmentioning
confidence: 99%