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multivariate production systems optimization - Stanford University

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q is the mass <strong>production</strong> rate from the reservoir, the source-sink term, and<br />

∇.<br />

k ρ ∇P<br />

μ<br />

VB<br />

is the mass flux term across the reservoir boundaries.<br />

A material balance considers the reservoir to be a single cell with no-flow boundaries.<br />

Therefore the mass flux term is zero and the equation simplifies to<br />

∂m<br />

∂t<br />

Discretizing and multiplying by a time interval Δt yields<br />

+ q = 0 (2.6)<br />

Δm + q Δt = 0 (2.7)<br />

which simply states that the change of fluid mass in the reservoir must be equivalent to the<br />

mass of fluid that was produced or injected.<br />

Equation 2.7 consists of a mass accumulation term and mass source-sink term. The<br />

accumulation term consists of the change in the mass of the reservoir fluids over time. The<br />

fluid mass in the reservoir at any given time (implied standard conditions) may be given as<br />

where<br />

m O = m OO + m OG<br />

m G = m GG + m GO<br />

mOO = φ SO<br />

S<br />

ρOO BO<br />

mOG = φ SG<br />

S<br />

ρOG BG<br />

mGG = φ SG<br />

S<br />

ρGG BG<br />

mGO = φ SO<br />

S<br />

ρGO BO<br />

10<br />

VB<br />

VB<br />

VB<br />

VB<br />

(2.8)<br />

(2.9)<br />

(2.10)<br />

(2.11)<br />

(2.12)

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