W2- O&G Geology Flashcards
Rock suitability for reservoir
particle size, sorting (uniformity), composition, rounding, sphericity
Mud logging
Process of monitoring reservoir rock;
Drill cutting emergence safe indicators
Main rock types
Igneous: formed from magma as cools and hardens;
limited porosity/permeability, i.e. granite basalt, obsidian
Sedimentary: layers of material deposit over time;
interconnected pores to trap organics, i.e. limestone, sandstone
Metamorphic: formed after physicochemical transformation of igneous/sedimentary under high T&P, i.e. slate, marble
Reservoirs
Porous rock regions (mainly sedimentary) filled with HCs after organic material buried under extreme T+P
Organisms dies at bottom of lake- sediments accumulate & rock later buried deeper and T&P increase
Kerogen formed (via organic material decay anaerobically)
Constant T&P increase over Ma converts Kerogen to HCs
Reservoir formation (5 methods)
Source rock: sedimentary porous rock carries trapped organics and is buried under more sediment & decays under anoxic conditions to kerogen.
Under high T&P kerogen -> HCs
Migration: movement of HC out source rock into reservoir;
Primary(to reservoir) or secondary (to cap/trap)
Accumulation: HC migrates and accumulates from source to reservoir rock
Cap rock containment: non porous/low permeability material atop reservoir to prevent HC flow out = capillary seal;
membrane (buoyancy P) or hydraulic seals
Traps- sealing: Trap formed when change in subsurface geology that cuts off reservoir from any formations;
Structural, stratigraphic, hydrodynamic
Reflection seismology
Energy release and transmission after shock events;
Produce waves that travel and reflect off rock under seabed
Waves: Primary (P waves) & secondary (S waves)
Porosity, total, effective and ineffective porosity
Porosity: Ratio of pore volume (void space) in reservoir rock to total volume as a percentage
Total: total pore volume/total volume
Effective porosity: vol of all pores/total volume
Ineffective porosity: vol of completely disconnected pores/total volume
3D & 4D seismic techniques
Pressure and composition changes monitor how reservoir responds
More expensive setup, but higher recovery possible & increase reservoir yield as stagnant regions targeted
Absolute & relative permeability
Absolute: ability for petroleum reserves to flow through rock - saturation of a single fluid
Relative: permeation of more than one fluid
Darcy law
Q = [kA/muL)]*(P1-P2)
k = absolute permeability (m2)
A = CS area (m2)
L = length (m)
P1-P2 = flowing pressure drop (N/m2)
Inclined flow darcy law
Q = (kA/mu)[((P1-P2)/L) - pgsina]
Radial flow darcy law
Q = (kA/mu)(dP/dr)
-> Q = {[2PIkh(Pe-Pwf)]/[mu*ln(re/rw)]}
Absolute permeability: Parallel flow
Q = Q1+Q2+Q3
h = h1+h2+h3
-> kavg = {[sum(kihi)]/[sum(hi)]}
-> kavg = {[sum(kiAi)]/[sum(Ai)]}
where Ai = sum(Wi*hi)
Absolute permeability: Series flow
Q = Q1=Q2=Q3
L/kavg = L1/k1 + l2/k2 + L3/k3
-> kavg = {[sum(Li)]/[sum(Li)/Ki]}