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AGU: Geophysical Research Letters

 

Keywords

  • ground water
  • percolation
  • permeability

Index Terms

  • Hydrology: Groundwater transport
  • Hydrology: Groundwater hydraulics
  • Mathematical Geophysics: Persistence, memory, correlations, clustering
  • Mathematical Geophysics: Probabilistic forecasting

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L10402, 9 PP., 2008
doi:10.1029/2007GL032717

Studying the effect of correlation and finite-domain size on spatial continuity of permeable sediments

Arijit Guin

Department of Earth and Environmental Sciences, Wright State University, Dayton, Ohio, USA

Robert W. Ritzi Jr.

Department of Earth and Environmental Sciences, Wright State University, Dayton, Ohio, USA

The percolation of high-permeability cells in geo-reservoir models is affected by cluster correlation and by lattice size. These affects are studied using an analytical methodology, presented as a useful augmentation to Monte Carlo approaches. The analytical method compares Euclidean cluster size distributions between random and correlated lattices. It shows that correlation affects both high-permeability (sand) and low-permeability (clay) clusters equally, and thus correlation does not likely affect the percolation threshold for infinite lattices. On finite lattices, the analysis shows that the effect of correlation on lowering the percolation threshold can be understood through the truncation of clay cluster-size distributions, without the need for Monte Carlo simulations.

Received 6 December 2007; accepted 17 March 2008; published 22 May 2008.

Citation: Guin, A., and R. W. Ritzi Jr. (2008), Studying the effect of correlation and finite-domain size on spatial continuity of permeable sediments, Geophys. Res. Lett., 35, L10402, doi:10.1029/2007GL032717.

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