Clayton V. Deutsch, 2013. "Multiple-scale Geologic Models for Heavy Oil Reservoir Characterization", Heavy-oil and Oil-sand Petroleum Systems in Alberta and Beyond, Frances J. Hein, Dale Leckie, Steve Larter, John R. Suter
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Numerical geologic models are built for many purposes. Models at a cubic-millimeter resolution are required to understand how small-scale heterogeneity observed in core photographs and image logs affects vertical permeability. Models at 1 dm3 (0.001 m3) resolution are required to understand the variability of properties within the grid blocks that will be used in the flow simulator. Models at a 1000 m3 (3531 ft3) resolution are required to understand the variability between grid blocks to model specific recovery processes. Models at the 1012 m3 (3.53 to 1013 ft3) scale are required to assess resources over large areas. No single numerical geologic model is fit for all purposes. Many of the same tools are used at different scales, but notable differences related to the use of categorical and/or continuous variables, the number of variables, and conditioning to different data types exist. Three important model types and the implemented choices are described: (1) large-scale multivariate mapping for resource and/or reserve assessment, (2) reservoir-scale three-dimensional (3-D) modeling for reservoir development planning, and (3) high-resolution modeling to understand effective flow parameters at the flow-simulation scale.
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Oil sands, including the Athabasca Oil Sands in northern Alberta, are the second largest hydrocarbon resource on earth. In the last decade, engineering technology has evolved that can now economically produce the bitumen resource in the oil sands. This volume showcases the geology of oil sands from around the world. It highlights the Athabasca Oil sands of northern Alberta and the geochemistry of the associated bitumen resource, but points directionally toward the development of other oil-sand deposits in the world. A novel feature is the ‘case study’ approach. Although much of the perspective is sedimentological and/or stratigraphic, the substance of the book should fine wide appeal to Earth scientists working in all geoscience domains.