material balance john_mcmullan_presentation
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Technology ServicesReservoir & Well Performance
Material Balance:The Forgotten
ReservoirEngineering Tool
John McMullan
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Understanding the OilAnd Gas ReservoirUsing Material BalanceLafayette, LouisianaOctober 21, 2004
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http://www.cgrpttc.lsu.edu/products/matbal/
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Possible Talk Titles
Material Balance: The Forgotten Reservoir Engineering Tool
Are Traditional Material Balance Calculations Obsolete?
Material Balance: Obsolete in 2005?
Material Balance: A Quaint Reservoir Engineering Tool from the Past
Material Balance, Why Bother?
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Material Balance
Can Provide an estimate of initial HC in place– independent of geological interpretation
– can be used to verify volumetric estimates
Determines the degree of aquifer influence– understanding of the “drive mechanism”
– estimate recovery factor
Estimate of recoverable reserves
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Uses of Material Balance
As a precursor to reservoir simulation
Identify undrained hydrocarbons
Can be used as a forecasting tool in certain situations
Can be used to help evaluate operating strategies such as new wells, accelerated rate, compression
In some cases can be used to screen for enhanced recovery
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Gas Material Balance
G ≡ initial gasvolume - SCF
Bgi – bbl/SCF Vgi = G × Bgi
Vgi ≡ initial gasvolume - bbls
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Gas Material Balance
G × Bgi
Bg is a functionof new pressure
Expansion (bbls)
= Vg - Vgi
= G (Bg – Bgi)}Vg = G × Bg
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Gas Material Balance
Expansion (bbls)
= Vg - Vgi
= G (Bg – Bgi)}
Expansion mustequal production:
Gp Bg = G (Bg – Bgi)
Fix piston
Bleed off Gp SCFof gas until
pressure equalsthe same as before.
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Gas Material Balance
Vti = Vgi + Vwi (bbls)
Vgi = Vti (1-Sw) = G Bgi
Vti = G Bgi / (1-Sw)
Vwi = Vti Sw = G Bgi Sw / (1-Sw)
Vgi = G × Bgi
Vwi = G Bgi Sw / (1-Sw)
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Gas Material Balance
The change in water volume can be found:
∆Vwi = Vwi cw ∆p
Since
Vwi = Vti Sw = G Bgi Sw / (1-Sw)
Substituting:
∆Vwi = G Bgi cw ∆p Sw / (1-Sw)
(the expansion of water with a drop in pressure)
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Gas Material Balance
G × BgiExpansion (bbls)
= G (Bg – Bgi) +
G Bgi cw ∆p Sw / (1-Sw)
}Vwi =
G Bgi Sw / (1-Sw)
Vg = G × Bg
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Gas Material Balance
As before,
Expansion must equal production:
G (Bg – Bgi) + G Bgi cw ∆p Sw / (1-Sw)
= Gp Bg + WpBwFix piston
Bleed off Gp SCFof gas, Wp water until
pressure equalsthe same as before.
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Expansion (bbls)
= G (Bg – Bgi)
+
G Bgi cw ∆p Sw / (1-Sw) + We
}
Suppose while the pressure drops, weinject We reservoir barrels of water.
Expansion must equal production:
G (Bg – Bgi) + G Bgi cw ∆p Sw / (1-Sw) + We
= Gp Bg + WpBw
Gas Material Balance
We
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Gas Material BalanceFinally, consider the possibility that the actual
initial pore volume will reduce as the pressure falls:
∆Vti = Vti cf ∆p
Recall,
Vti = G Bgi / (1-Sw)
Substituting:
∆Vti = cf ∆p G Bgi / (1-Sw)
This loss in original volume results inan additional amount of expansion from
the original volume.
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Gas General MaterialBalance Equation
G (Bg – Bgi) + G Bgi cw ∆p Sw / (1-Sw) + We + cf ∆p G Bgi / (1-Sw)
= Gp Bg + WpBw
GasProduction
WaterProduction+=
GasExpansion
WaterExpansion
WaterInflux
FormationExpansion+++
Note that all terms are a function of pressure
Equation can not be directly solved
An iterative approach is required for solution
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Oil General MaterialBalance Equation
N (Bt – Bti) + N m Bti (Bg - Bgi ) + (N Bti + N m Bti ) cw ∆p Sw / (1-Sw)
+ cf ∆p (N Bti + N m Bti ) / (1-Sw) + We + WI BwI + GI BgI
= Np Bt + Np (Rp – Rsoi) Bg + WpBw
Bgi
OilExpansion
WaterExpansion+ +Gas Cap
Expansion
WaterInflux
FormationExpansion+ + Water
Injection+ GasInjection+
Free GasProduction
WaterProduction++Oil & Dissolved
Gas Production=
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Gas Material Balance as aStraight Line
G (Bg – Bgi) + Bgi cw Sw + cf ∆p = Gp Bg + WpBw - We
1-Sw
⎡⎢⎣
⎤⎥⎦⎩
⎧⎨
⎫⎬⎭
Xg ≡ (Bg – Bgi) + Bgi cw Sw + cf ∆p1-Sw
⎡⎢⎣
⎤⎥⎦
Yg ≡ Gp Bg + WpBw - We
Yg = G Xg
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Yg - rb
Xg – rb/SCF
m = G
Yg - rb
Xg – rb/SCF
m = G
Gas Material Balance as aStraight Line
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Water Influx
Aquifers come in all shapes and sizes– Aquifers can be extremely large relative to the reservoir
size, even infinite “acting”.
– Aquifers can be small, even neglected.
– Aquifer productivity can be either high or low (relative to the withdrawal rates from the reservoir).
Aquifers can be hydraulically connected to more than one reservoir.
Aquifers can even be connected to the surface.
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Steady-State and Semisteady-state Aquifer Models
dWedt = qaq = k’ × (Paq – P)
qaq = instantaneous aquifer flow rate (rb/day)
k’ = aquifer influx constant (rb/day/psi)
Paq = average aquifer pressure (psi)
P = average reservoir pressure (psi)
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Steady-State and Semisteady-state Aquifer Models
k’ is similar to the “Productivity Index” often usedto describe an individual well’s productivity.
Using a similar definition:
qaq = Jaq × (Paq – Pr)
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Steady-State and Semisteady-state Aquifer Models
If the pore volume (Vaq), compressibilities, and averageaquifer pressure are known, the total water influx atany point in time can be estimated by:
We = Vaq × cavg × (Pi – Paq)
Recall: Cavg = SoCo + SwCw + SgSg + Cf
So for aquifers, Cavg = Cw + Cf
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Steady-State and Semisteady-state Aquifer Models
Define a term Wei that we will refer to as the“maximum encroachable water”:
Wei = Vaq × cavg × (Pi – Paq)
0
Wei = Vaq × cavg × Pi
In words, this is the volume of water that will flowfrom an aquifer if it’s pressure is lowered to zero.
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Steady-State and Semisteady-state Aquifer Models
The average aquifer pressure at any point in timecan then be estimated by:
Paq = Pi × (1 – We / Wei)
qaq = Jaq × (Paq – Pr)
This equation, along with the previously shown equation below, form the basis for steady-state and semisteady-
state aquifer models.
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Steady-State and Semisteady-state Aquifer Models
“Pot” aquifer– defined as an aquifer where the aquifer and reservoir pressure
remain (nearly) equal as the reservoir depletes
– this implies a small aquifer with high productivity
“Schilthuis” steady-state aquifer– aquifer is extremely large and consequently, the aquifer pressure
can be assumed to remain constant
“Fetkovitch” semisteady-state aquifer– aquifer rate and pressure are assumed to both change with time as
described by the previous equations
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Pot AquiferDefinition: P = Paq
Recall:Paq = Pi × (1 – We / Wei)
Then:
P = Pi × (1 – We / Wei)
Solving for We yields:
We = Wei × (1 – P / Pi)
We can be directly substituted into any ofthe material balance equations.
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Steady-state Aquifer
Definition: Paq = Pi
Recall:
qaq = Jaq × (Paq – P)
Then:
qaq = Jaq × (Pi – P)
(∆We )n = Jaq × Pi –⎡⎣ ⎦
⎤Pn + Pn-1
2× ∆t
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Fetkovich AnalyticalAquifer
Recall “encroachable” water was defined by:
W ei = V aq × P i × c aq
AquiferPore
Volume
InitialPressure
AquiferCompressibility
Aquifer pressure at any point in time is given by:
P aq = P i × (1 - W e / W ei )
Cumulative Water Influx
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Fetkovich AnalyticalAquifer
Finally, the influx rate at any point in time is given by:
q aq = J aq × ( P aq - P res ) =
AquiferProductivity
Index
ReservoirPressure
dWe
dt
Note: A large J and small W ei models a pot aquifer. A large W ei models an infinite aquifer.
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Aquifer Productivity Index
Source: Applied Petroleum Reservoir EngineeringCraft, Hawkins, and Terry
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Fetkovich AnalyticalAquifer
Through algebraic manipulation and integration, the waterinflux for a constant drop in pressure for a time “t” becomes:
We = ( pi – p ) (1 - e-J pi t / Wei)Weipi
Fetkovich showed that this equation can be applied in adifference form without the need for superposition tomodel a system with a continuously falling pressure:
∆Wen = ( pn-1 – pRn ) (1 - e -J pi ∆tn / Wei)Weipi
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Aquifer Boundary Pressure
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Some CommentsRegarding Aquifer Models
Steady-state and semisteady-state models are often thought to be less accurate than unsteady-state models (like the often used Hurst and van Everdingen model)
None of the analytical aquifer models directly consider the growing water invaded zone and its impact on aquifer productivity or MB (see SPE papers by Al-Hashim & Bass and Lutes et al)
Truly “rigorous” treatment of aquifer influx requires reservoir simulation
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Material Balance CalculationsTwo Approaches
“Traditional” XY Plot– Uses observed pressures and production in GMBE and
aquifer model to calculate N or G
– Some iteration may be required to estimate gas cap volume, aquifer properties, etc.
– Sparse pressure data, erratic production rates a problem
Alternate method– Uses observed production, aquifer model, and assumed
values of N or G in GMBE to calculate pressure
– Iterate until calculated and observed pressures agree
– Excellent for investigating sensitivities
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Gas Example No. 1
Moderate Water Drive
Project Based on 60-100 BCF Volumetric Estimate
Unconstrained MB Analysis Suggested Reservoir Was Depleted
Subsequent Well Was Dry Hole
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Gas Example No. 2
Weak Water Drive
P/Z Suggested 860 BCF
Downdip Water Production Suggested Limited Water Influx
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Gas Example No. 2 (cont.)
Material Balance 725 BCF
HC Pore Volume 450 MMBbls
Water Influx 100 MMBbls
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Gas Example No. 3
Strong Water Drive
“Classic” Rate Sensitive Reservoir
Used in Field to Establish Production Priority
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Gas Example No. 4
Example of “Pot” Aquifer
Observe the Sensitivity to Formation Compressibility (49.7 to 58.5 BCF)
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Oil Example No. 1
Initially Undersaturated, Moderate Water Drive
Observe the Extreme Sensitivity to Formation Compressibility (11 to 30 MMBO)
Note Culled Points
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Oil Example No. 2
Initially Undersaturated, Weak Water Drive
MB Analysis Reveals Pressure Behavior That Could Not Be Matched
Subsequent Simulation Study Was a Failure
Anomalous Behavior Was Later Determined to be the Result of Several Casing Leaks
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Oil Example No. 3
Small Offshore, Above BP Pressure
N = 35 MMBO from “XY” Plot
N of 66.5 MMBO Agrees with Volumetric Estimate of 65 MMBO
Dominated by Aquifer InfluxFrom Dake, Exercise 3.4The Practice of Reservoir Engineering
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Oil Example No. 4
Venezuela, Water-drive, Water Injection, Gas-cap Expansion, Solution Gas Drive
N = 27 MMBO with “XY” Plot and Fixed Gas Cap Size
N = 34 MMBO Allowing Gas Cap Size to Vary
Note Culled Points
From Havelana and Odeh, JPT, July 1964
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Material Balance Compared To Reservoir Simulation
Reservoir Simulation– expensive– time consuming– requires geologic
description– driven with single
phase– ability to forecast– determines location
and distribution of unswept HC’s
Material Balance– cheap– fast– independent of
geology– uses production of all
phases in calculations– limited forecasting– can determine the existence of unswept HC’s
Technology ServicesReservoir & Well Performance
Material Balance:The Forgotten
ReservoirEngineering Tool
John McMullan