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Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

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6.3. STAGGERED NEWTON SCHEME WITH IMPES 177<br />

where B m ss =<br />

⎡<br />

⎢<br />

⎣<br />

A oo,k<br />

f hγe + T k o ∆t<br />

h 2(1 − cos θ)γe + b2So KdrBo (γe − 1) A ow,k<br />

f hγe A o,k<br />

u 2i sin θ<br />

2<br />

A wo,k<br />

f hγe + T k w ∆t<br />

h 2(1 − cos θ)γe + b2Sw KdrBw (γe − 1) A ww,k<br />

f hγe A w,k<br />

u 2i sin θ<br />

2<br />

b2i sin θ<br />

2 γe<br />

From det (B m ss) = 0, the γe is<br />

which yields unconditional convergence.<br />

0<br />

Kdr<br />

h 2(1 − cos θ)γe<br />

⎤<br />

⎥<br />

⎦ .<br />

γe = 0, (6.49)<br />

6.3 Staggered Newton scheme with IMPES<br />

From the one-dimensional flow equations, the IMPES pressure equation is expressed as<br />

<br />

− Aww<br />

f<br />

A oo<br />

f<br />

+ Awo<br />

f<br />

<br />

Aow f<br />

<br />

= Aww<br />

f<br />

Aow f<br />

As p<br />

<br />

wo<br />

∂<br />

∂x<br />

ρo,0<br />

dpo<br />

dt +<br />

<br />

− Aww<br />

f<br />

<br />

− ∂<br />

<br />

ww<br />

∂x ρw,0<br />

A o u + A w u<br />

<br />

Aow f<br />

<br />

A s u<br />

− Aww<br />

f<br />

Aow f<br />

dεv<br />

dt<br />

<br />

f f<br />

+ , (6.50)<br />

B o B w<br />

where all the coefficients <strong>and</strong> saturation values are explicit except <strong>for</strong> the pressure. Neglect-<br />

ing the source terms of Equation 6.50, we discretize Equation 6.50 based on the IMPES<br />

method, which produces<br />

hA s,n∆P<br />

p<br />

n o,j<br />

− T n s<br />

h<br />

hAs,n u<br />

+<br />

∆t (−<br />

∆Un j− 1<br />

2<br />

− ∆U n<br />

j+ 1<br />

2<br />

)<br />

∆t h<br />

<br />

P n+1<br />

<br />

n+1 n+1<br />

o,j+1 − 2Po,j + Po,j−1 = 0, (6.51)<br />

where Ts = − Aww<br />

f<br />

Aow To + Tw. The discretized equation <strong>for</strong> mechanics is the same as Equa-<br />

f<br />

tion 6.18. The flow problem is itself conditionally stable because we treat saturation <strong>and</strong><br />

all the coefficients explicitly (Aziz <strong>and</strong> Settari, 1979). When the coupled problem is solved

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