Impact of the "Missing Scale" on Block Effective Permeability

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Abstract/Contents

Abstract
Traditional upscaling addresses only averaging of permeability values from the geostatistical grid cell to the flow simulation block (2 to 3 orders of magnitude larger). The difference of scale between core measurements and the geostatistical grid cell (from 6 to 10 orders magnitude larger) is most often ignored. The impact of this latter missing scale on the calculation of whole-field effective permeabilities is documented for a variety of heterogenous permeability fields. The conclusion is that the missing scale problem cannot be ignored.

Description

Type of resource text
Date created May 1999

Creators/Contributors

Author Ji, Fang
Primary advisor Journel, Andre G.
Degree granting institution Stanford University, Department of Petroleum Engineering

Subjects

Subject School of Earth Energy & Environmental Sciences
Genre Thesis

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User agrees that, where applicable, content will not be used to identify or to otherwise infringe the privacy or confidentiality rights of individuals. Content distributed via the Stanford Digital Repository may be subject to additional license and use restrictions applied by the depositor.

Preferred citation

Preferred Citation
Ji, Fang. (1999). Impact of the "Missing Scale" on Block Effective Permeability. Stanford Digital Repository. Available at: https://purl.stanford.edu/rp576mp1187

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Master's Theses, Doerr School of Sustainability

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