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wright1237579784.pdf (8.31 MB)
ETD Abstract Container
Abstract Header
The Continuity of High-Permeability Zones in Sedimentary Deposits
Author Info
Guin, Arijit
Permalink:
http://rave.ohiolink.edu/etdc/view?acc_num=wright1237579784
Abstract Details
Year and Degree
2009, Doctor of Philosophy (PhD), Wright State University, Environmental Sciences PhD.
Abstract
Cubic lattice models were used to represent sedimentary deposits and their role as georeservoirs. The percolation of high-permeability zones was studied using both analytical and simulation approaches. The analytical approach was developed for single-scale sedimentary architecture. The approach showed that percolation is affected by cluster spatial correlation and by lattice size. It showed that correlation affects both high-permeability and low-permeability clusters equally, and thus correlation does not likely affect the percolation threshold for infinite lattices. On finite lattices, the analysis showed that the effect of correlation on lowering the percolation threshold can be understood through the truncation of low-permeability cluster-size distributions, without the need for Monte Carlo simulations. The simulation approach was used to study multiscale, hierarchical sedimentary architecture. A computer code was developed to create a digital model representing hierarchical stratal architecture found in channel-belt deposits. The code uses a geometric-based approach to simulate strata observed over multiple scales (levels). Larger-scale unit types form the bounding surfaces of associations of smaller-scale unit types. The different scales of bounding surfaces were each found to create a finite lattice effect on percolation. When using realistic length distributions, the high-permeability zones percolate across boundaries at all hierarchical levels if volume proportions are above 0.18, as is common. This threshold value is lower than the threshold proportion of 0.3116 required for percolation on the infinite random lattice. Thus, in sedimentary deposits as represented here, percolation in the high-permeability zones is expected.
Committee
Robert Ritzi, PhD (Committee Chair)
David Dominic, PhD (Committee Member)
Mark Goltz, PhD (Committee Member)
Allen Hunt, PhD (Committee Member)
Thaddeus Tarpey, PhD (Committee Member)
Pages
231 p.
Subject Headings
Hydrology
Keywords
High-permeability Zones
;
Preferential Flowpathways
;
Hierarchical Sedimentary Architecture
;
Sedimentary Deposits
;
Percolation Theory
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Citations
Guin, A. (2009).
The Continuity of High-Permeability Zones in Sedimentary Deposits
[Doctoral dissertation, Wright State University]. OhioLINK Electronic Theses and Dissertations Center. http://rave.ohiolink.edu/etdc/view?acc_num=wright1237579784
APA Style (7th edition)
Guin, Arijit.
The Continuity of High-Permeability Zones in Sedimentary Deposits.
2009. Wright State University, Doctoral dissertation.
OhioLINK Electronic Theses and Dissertations Center
, http://rave.ohiolink.edu/etdc/view?acc_num=wright1237579784.
MLA Style (8th edition)
Guin, Arijit. "The Continuity of High-Permeability Zones in Sedimentary Deposits." Doctoral dissertation, Wright State University, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=wright1237579784
Chicago Manual of Style (17th edition)
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Document number:
wright1237579784
Download Count:
764
Copyright Info
© 2009, all rights reserved.
This open access ETD is published by Wright State University and OhioLINK.