CORE LABORATORIES (U.K.) LIMITED Basic Formation ... - why SCAL.pdf · AFES Seminar “Basic...
Transcript of CORE LABORATORIES (U.K.) LIMITED Basic Formation ... - why SCAL.pdf · AFES Seminar “Basic...
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AFES Seminar
“Basic FormationEvaluation –
So what’s so Special aboutCore Analysis?”
Presented byRichard Arnold
CORE LABORATORIES (U.K.) LIMITED
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AFES Seminar
•Cores are the only representative element ofthe reservoir rock that are physicallyavailable for examination and modelling forbasic flow processes.
•Special Core Analysis reduces uncertaintyand reduces risk
Why Core Analysis?
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AFES Seminar
Why Core Analysis?
• Reservoir Geological Model –defines volumetrics• Total hydrocarbons in place (= total assets)
• Productivity Index (= cash flow)
• Recovery, STOIP - STOresidual (= bankable assets)
t
n
o
b
hh
BSwV
STOIP .)1.(.
noo
hB
KPI .
.
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AFES Seminar
Where? - Data Sources
SEISMIC &GEOLOGICAL DATA
Reservoir StorageCapacity
Fluid SaturationsHydrocarbons in place
Fluid Flow
FIELD DATALABORATORY
DATA
Reservoir Engineering Model
Hydrocarbon Recovery Predictions
PorosityCompressibility
Capillary PressureResistivities
Single & MultiphasePermeabilities, PVT
Porosity Tools
Resistivity Tools
Well Flow Tests
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AFES Seminar
How?- Methods
CORING PROCESS
CORE
ROUTINE
Porosity, Permeability,Log, Grain Density,
Fluid Saturations
OVERBURDEN
ADVANCED
Air/BrineAir/Mercury
Oil/Brine
FRF m + aRI n
Shale effects
CompressibilityPermeability
Rock Mechanics
RelativePermeability
CAPILLARY PRESS. ELECTRICAL WETTABILITY FLUID FLOW
SinglePhase
FormationDamage,
Stimulation
Gas/Oil/BrineDrainage/Imbibition
Unsteady/Steady StateRoom/Reservoir Conditions
GEOLOGICAL
Core DescriptionThin Section, XRD, SEM
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AFES Seminar
Sample Preparation
•How do we select representative samples?•How do we prepare suitable samples for
testing?
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AFES Seminar
CT Images
Preserved Whole Sample Plug Sample
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AFES Seminar
Directional Plugging
BeddingPlane
Direction
‘Horizontal’Plug
Unsuitable Plug
‘Vertical’Plug
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AFES Seminar
Petrographic Analysis
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AFES Seminar
Clay Minerals
General clay effects on petrophysical properties:
• Reduce permeability and porosity
• Increased retention of water–Microporosity –capillary bound water; localized or
continuous–Water of Hydration –“Clay Bound Water”(CBW)
• Suppression of resistivity
• Over-estimation of porosity by Neutron log
• Increased potential to reduce productivity–Pore plugging by fines migration and/or swelling
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AFES Seminar
Clay Types
Main clay types:
KaoliniteKaolinite
ChloriteChlorite
IlliteIllite
SmectiteSmectite
Mixed layerMixed layer
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AFES Seminar
Kaolinite
• Non-expanding• Low cation exchange
capacity• Platelets or booklets
• May migrate
AluminaAlumina
SilicaSilica
7.27.2 ÅÅ
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AFES Seminar
Chlorite
• Non-expanding• Low cation exchange capacity• Platelets or honeycomb
aggregates• May migrate• Contact with HCl Acid releases
iron (Ferric Hydroxide)
AluminaAlumina
SilicaSilica
SometimesSometimesIronIron
1414 ÅÅ
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AFES Seminar
Illite
• Non-expanding• Moderate to low cation
exchange capacity• Fibrous or thin irregular
platelets• May migrate• May be susceptible to
damage on drying in cores
AluminaAlumina
SilicaSilicaKK
1010 ÅÅ
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AFES Seminar
Smectite
• Expanding• High cation exchange
capacity• Honeycomb or cornflake
texture
• May swell and migrate
SilicaSilica
H2O, Na, Ca, Mg
AluminaAlumina
1010 -- 1717 ÅÅ
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AFES Seminar
Illite-Smectite Mixed Layer
• Moderately high cationexchange capacity
• Platey or fibrous
• May swell and migrate
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AFES Seminar
Sample Cleaning
••Hot SoxhletHot Soxhlet
••Cool SoxhletCool Soxhlet
••Dean and StarkDean and Stark
•• ImmersionImmersion
••FlowFlow--throughthroughcleaningcleaning
Flow (cold) solvent
400 psi
FLOW-THROUGH
Condensed solvent (hot) liquid
SOXHLETSolventVapour
Methanol
Toluene
Toluene
Methanol
Methanol
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AFES Seminar
Sample Drying
••Convection oven dryingConvection oven drying ~ 100C
••Humidity oven dryingHumidity oven drying 60C & 40% RH (or similar)
••Vacuum oven dryingVacuum oven drying ~ 60C
••Critical point drying using liquid COCritical point drying using liquid CO22
••Brine saturationBrine saturation
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AFES Seminar
Porosity
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AFES Seminar
Porosity
Porosity Precision ± 0.005 (or better)Grain Density Precision ± 0.01g.cm-3
•Vb, Bulk Volume•Vg, Grain Volume•Vp, Pore Volume, Porosity
Vb = Vg + Vp
= Vp/Vb
GD = Wt/Vg
VpVp
VgVg
Vb
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AFES Seminar
Orthorhombic PackOne Grain Size
= 0.395Tetragonal-Sphenoidal Pack
One Grain Size
= 0.312
Rhombohedral PackOne Grain Size
= 0.26Cubic PackTwo Grain Sizes
= 0.25
Effect of Packing and Sorting
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AFES Seminar
Porosity Definitions
Total Porosity, Neutron log
Total Porosity, Density log
Absolute or Total Porosity
Humidity-dried Core Porosity
Capillarywater
Quartz Claylayers
Smallpores Large pores Isolated
poresClay surfaces& interlayers
Vshale
Oven-dried Core PorosityMatrix
Hydrocarbonpore volume
Structuralwater
Hydration orclay-bound
water
Irreducible orimmobile water
**
**
(after(after EslingerEslinger && PevearPevear, 1988), 1988)
Relative volumes ofcapillary water and
hydrocarbons varieswith height above FWL
* if sample completely disaggregated
Volume dependent onQv of rock and
salinity of pore water
Neglible inmost rocks
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AFES Seminar
Grain Volume Measurement
Boyle’s Law - Shared Volume
VrVr
He
Vc
Vg
PressureRegulator
valvevalve
ReferenceVolume
transducer
P1P2
SampleChamberSample
Chamber
P1Vr = P2 ( Vr + Vc - Vg )
g = Wd / Vg
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AFES Seminar
Porosity - SUMMARY
• Variations exist for definition of effective porosity
• Logs and cores can almost always provide similar total porosity
• Porosity is
–Independent of grain size
–Dependent on sorting, packing, shape, cementation• Fracture porosity contributes little, generally
• Accurate methods available for determining Porosity
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AFES Seminar
Permeability
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AFES Seminar
Permeability
LAPK
Q.
..
Assumes:Assumes:••laminar flowlaminar flow••no reaction between fluid and rockno reaction between fluid and rock••one phase flowingone phase flowing••incompressible fluidincompressible fluid
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AFES Seminar
Liquid vs. Gas Permeabilities
Liquid Gas
Finite velocity at wallVwall = 0
Vmax
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AFES Seminar
Gas Slippage
Pressure Effect Conduit Size Effect Molecular Weight Effect
Lower pressure= greater slippage
Smaller conduit= greater slippage
Lower weight= greater slippage
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AFES Seminar
Klinkenberg Plot
k
k
Air
CO2
1 / Pm
bHe . k
mPb
kk 1
Helium
0
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AFES Seminar
Gas Permeability - Steady State
Hassler Cell
Gas permeability, 5% to 20%,dependent on permeability range
To Vacuum
Sleeve Pressure
Calibrated Orifice
P upstream P downstream
Core Plug
PressureRegulator
Kair =Permeability, millidarcies
Qa =Flow rate, cm3/sec, at Pa
=Viscosity of air, cpL = Length of sample, cmA = Cross sectional area of sample, cm2
P1 = Upstream pressure, atm
P2 = Downstream pressure, atm
Pa = Atmospheric pressure, atm
A)P-(PLQP2000
K 22
21
aaair
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AFES Seminar
Gas Permeability - Unsteady StatePressure Transducer
Helium/Nitrogen Tank(manifold)
HydrostaticConfiningPressure
Carousel
AxialLoad
Core Samples
Computer
Gas escapesthrough core toatmosphere
Open valve forpressure drawdown
P1
P2
t1 t210
20
30
40
50
60
70
80
90
100
0 10 20 30 40 50
Time, seconds
Pre
ssu
re,p
sig
21 PPP
Instantaneous Flow ratedetermined from slope at P
P1
P2
t1 t210
20
30
40
50
60
70
80
90
100
0 10 20 30 40 50
Time, seconds
Pre
ssu
re,p
sig
21 PPP 21 PPP
Instantaneous Flow ratedetermined from slope at P
CMS-300
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AFES Seminar
Forchheimer's Equation
2
kdLdP
dLdP
0
Inertial
Viscous
0
Acceleration in pore throatAcceleration in pore throat
Deceleration in pore bodyDeceleration in pore body
kdL
dP
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AFES Seminar
Overburden Porosity & Permeability
1.0
0.8
0.6
0.4
0.2
2000 4000Sleeve Pressure (psi)
Fra
ctio
nof
base
poro
sity
Porosity
Well cemented Friable Unconsolidated
1.0
0.8
0.6
0.4
0.2
2000 4000400Sleeve Pressure (psi)
Fra
ctio
nof
base
perm
eabi
lity Permeability
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AFES Seminar
Permeability vs. Porosity
1
10
100
1000
0 5 10 15 20 25 30 35
Porosity, %
Per
mea
bilit
y,m
d
Fine GrainedFriable Sand
ChalkyLimestone
IntercrystallineLimestone andDolomite
Well CementedSand
Sucrosic Dolomite
Reef Limestone
Oolitic Limestone
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AFES Seminar
Core Analysis Objectives
•Reservoir QualityPore geometry, mineralogy, cements, clays, depositional environments
•Petrophysical PropertiesPorosity, permeability, effects of stress, effective porosity
•Water SaturationElectrical properties, capillary pressure, Dean Stark if OBM
•Saturation ChangeRelative permeability, gas or water injection, recoverable hydrocarbon
•Rock MechanicsCompressibility, sanding, fracture design, stimulation
CUT CORE!
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AFES Seminar
CORE LABORATORIES (U.K.) LIMITED