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Geo
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Reservoir Modeling
The process of creating a numerical representation of a subsurface reservoir to understand how fluids such as oil, gas, or water move through the rock.
Why Reservoir Modeling
It allows us to see underground, understand the physics of the reservoir, and make engineering decisions to maximize recovery, or storage and minimize risk.
Routine Core Analysis (RCAL)
Includes basic measurements performed on core samples
Special Core Analysis (SCAL)
Includes more detailed and advanced lab tests that capture the dynamic and rock-fluid parameters in the reservoir
Whole Cores
Flow tests, Enhanced Oil Recovery, rock mechanics, and directional permeability
Standard Plugs
2-3” long and 1.5” in diameter
Porosity
What fraction of the total rock volume is made up of pore spaces where fluids like water, oil, gas, or supercritical CO2 can be stored.
Engineering “Matrix”
Framework
Matrix
Cement
Pores
Measurement of Porosity
Core samples (measure of two) for limited wells
Wireline (wells) logs: usually available for each drilled wells
Helium Porosimeter
a precise instrument using the principle of gas expansion (Boyle's Law) and helium's small atomic size to accurately measure the pore and grain volumes, porosity, and density of porous materials like rocks, powders, and core samples
Measures Grain or Matrix volume
Uses helium because it behaved ideally
Boyle’s Law
The relationship between pressure and volume of gas when the temperature and amount of gas remain constant
Absolute Permeability
Permeability to a single phase
Effective Permeability
Permeability to one phase when more than one phase are present
Relative Permeability
The ratio of effective permeability to a base permeability (absolute permeability)
Who discovered that permeability measurements made with air were always greater than the permeability obtained with liquid?
Klinkenberg (1941)
Kilkenberg gas exhibited ____ at the sand grain surface
Slippage
When pressure increases, the calculated permeability _____
decreases
Interfacial Tension
The force that acts along the boundary between two immiscible fluids because the molecules in each fluid prefer to stay with their own kind
Immiscible fluids
Do not mix
Mixable fluids
Do mix
Wettability
The tendency of one fluid to spread on or adhere to a solid surface in presence of other immiscible fluids. It refers to interaction between fluids and solid phases
Wetting phase fluid
preferentially wets the solid rock surface
Attractive forces between rock and fluid draw the wetting phase into
small pores
Wetting phase fluid often
has low mobility
Attractive forces
Limit reduction in wetting phase
Many hydrocarbon reservoirs are either
totally or partially wet
Water is wetting phase
Theta < 90
Nonwetting phase
does not preferentially wet the solid rock surface
Repulsive forces between rock and fluid cause non-wetting phase to
occupy largest pores
Non wetting phase fluid is often the _________ especially at large non wetting phase saturations
Most mobile fluid
Water is non-wetting phase
Theta > 90
Capillary Pressure
The pressure difference between two immiscible fluids caused by the curvature of their interface inside the pore space
Capillary Pressure Measurments
Mercury injection capillary pressure
Porous plate method
Centrifuge Method
Lithofacies
A “rock type unit” define by its observable features such as grain size, texture, composition, color, and sedimentary structures that tell us how and where it was formed.
MICP Test
Measures the pore-throat size distribution and capillary pressure behavior of a rock by injecting mercury into a dry, vacuumed sample under increasing pressure
Not a good representation for capillary forces because mercury has different fluid properties that make the readings unrealistically high
Is a useful measurement of b distribution