By John Fanchi
Content material:
Front matter
, Pages i-ii
Copyright
, Page iv
Preface
, Pages ix-x
About the Author
, Page xi
1 - Introduction
, Pages 1-16
2 - Fluid Properties
, Pages 17-32
3 - Geology
, Pages 33-48
4 - Porosity and Permeability
, Pages 49-69
5 - Geophysics
, Pages 71-88
6 - Petrophysics
, Pages 89-108
7 - good Logging
, Pages 109-124
8 - good Testing
, Pages 125-144
9 - construction assessment Techniques
, Pages 145-166
10 - Rock–Fluid Interactions
, Pages 167-185
11 - Reservoir Characterization
, Pages 187-204
12 - Fluid Displacement
, Pages 205-222
13 - Reservoir Simulation
, Pages 223-241
14 - facts Management
, Pages 243-256
15 - Reservoir circulate Modeling
, Pages 257-278
16 - glossy Reservoir administration Applications
, Pages 279-293
Appendix A - Unit Conversion Factors
, Pages 295-297
Appendix B - IFLO User's Manual
, Pages 299-342
References
, Pages 343-353
Index
, Pages 355-361
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Extra info for Integrated Reservoir Asset Management. Principles and Best Practices
Example text
4 Tortuosity. 2 45 Saturation We can rearrange Eq. 2) to show that pore volume is the product of bulk volume and porosity: VP ¼ fVB ð3:7:3Þ When sedimentary rocks are being deposited, the pore space is usually filled with water. The pores of a rock can be filled at a later time with commercially important fluids ranging from potable water to oil and gas. Bulk volume and pore volume are measures of the gross volume in a system. To determine the volume of the system that is commercially significant, the gross volume must be adjusted by introducing the concept of net thickness.
Typically, the formation of new rock occurs at plate boundaries, but it can also occur over “hot spots” within the earth’s mantle. As plates collide, pressure and heat may cause part of the plate to melt and result in molten rock being thrust to the surface. After cooling, surface rock is subjected to atmospheric phenomena. Chemical and physical processes cause exposed rock to break into smaller and smaller particles. Wind and water transport these particles from their source location in a process called erosion.
Plot the oil and gas PVT data in Table CS-2A as a function of pressure. Make a semilog plot of gas formation volume factor versus pressure to see more detail at higher pressures. 2-5. 0 2-6. As a rule of thumb, the temperature of the earth’s crust increases by about 1 F for every 100 feet of depth. Use this information to estimate the temperature of the earth at two miles. Assume the temperature at the earth’s surface is 60 F. 2-7. dat and find the PVT data for the model. What is the oil formation volume factor at the bubble point pressure?