By Djebbar Tiab, Erle C. Donaldson
"Presenting options, theories, and lab methods concerning porous rocks and gases, hydrocarbon drinks, and aqueous strategies, this 3rd version reference (the first was once released in 1996, and the second one in 2003) has been up-to-date and accelerated. new chapters on reservoir characterization and on uncomplicated well-log interpretation supply the elemental introductory fabric meant as a beginning for additional examine of the subjects. Djebbar (petroleum engineering, U. of Oklahoma) and Donaldson (retired after an extended profession in public, deepest, and educational spheres) introduce mineralogy and petroleum geology prior to overlaying porosity and permeability, formation resistivity and water saturation, capillary strain, wettability, functions of Darcys legislation, evidently fractured reservoirs, and the impression of rigidity on reservoir rock houses, between different topics." --Reference and examine publication News
, Pages i-iii
, Page ii
, Page iv
, Page xiii
About the Authors
, Pages xv-xvi
, Page xvii
, Pages xix-xx
Chapter 1 - advent to Mineralogy
, Pages 1-26
Chapter 2 - creation to Petroleum Geology
, Pages 27-83
Chapter three - Porosity and Permeability
, Pages 85-219
Chapter four - Formation Resistivity and Water Saturation
, Pages 221-326
Chapter five - Capillary Pressure
, Pages 327-370
Chapter 6 - Wettability
, Pages 371-418
Chapter 7 - purposes of Darcy’s Law
, Pages 419-483
Chapter eight - evidently Fractured Reservoirs
, Pages 485-552
Chapter nine - impact of pressure on Reservoir Rock Properties
, Pages 553-666
Chapter 10 - Reservoir Characterization
, Pages 667-714
Chapter eleven - Fluid–Rock Interactions
, Pages 715-801
Chapter 12 - simple Well-Log Interpretation
, Pages 803-827
Appendix - dimension of Rock and Fluid Properties
, Pages 829-912
, Pages 913-950
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Extra info for Petrophysics. Theory and Practice of Measuring Reservoir Rock and Fluid Transport Properties
The Great Lakes area of the United States, Canada, and the 36 Petrophysics Scandinavian Peninsula are still gradually rising in response to the melting of Pleistocene glaciers. Continental masses have stable interiors known as cratons, or shields, which are composed of ancient metamorphosed rocks. Examples are the Canadian, Brazilian, Fennoscandian, and Indian shields that form the nuclei of their respective continents. Sedimentary deposits from the cratons have accumulated to form much of the dry land of the Earth’s surface, filling depressions and accumulating on the shelves of continental margins.
The Earth’s lithosphere is composed of six major plates whose boundaries are outlined by zones of high seismic activity . The continents appear to be moved by the convection currents within the mantle at rates of 2 to 3 in. 6 cm) per year. The convection cells apparently occur in pairs and thus provide the kinetic energy for movement of the continental masses. Mid-ocean ridges form a network of about 65,000 km of steep mountains with branches circling the globe. Some of the mountains are as high as 5,500 m above the ocean floor, and some emerge above the ocean as islands.
The calculated values matched the experimentally determined permeability within 10%. She was then able to show the relative amount of fluid flowing through pores of selected pore sizes. Thus the HagenÀPoiseuille equation, with modification to account for the tortuous flow path in a rock, may be used for non-rigorous analysis of fluid flow characteristics. The general expression for fluid flow in porous media was developed by Darcy in 1856 from investigations of the flow of water through sand filter beds .