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Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

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56 CHAPTER 3. STABILITY OF THE DRAINED AND UNDRAINED SPLITS<br />

where · L 2 is the L 2 norm. From Equation 3.96,<br />

<br />

dΣ<br />

α<br />

n+1 2<br />

E − dΣn 2 1<br />

E +<br />

2M (dp n+1 2<br />

L2 − dp n 2<br />

L2) <br />

<br />

dΣ<br />

+α (2α − 1)<br />

n+1 − dΣ n 2 1 <br />

+ dp E 2M<br />

n+1 − dp n 2<br />

L2 <br />

≤ 0 . (3.99)<br />

From Equation 3.99, when we solve the mechanical problem, the evolution of the norm at<br />

the discrete time level satisfies<br />

<br />

dχ n+1 2<br />

N − dχn 2<br />

N<br />

= dζ n+1 2<br />

T − dζn 2<br />

T<br />

= dΣ n+1 2<br />

E<br />

≤ −(2α − 1)<br />

<br />

dp n+1 2<br />

1<br />

+<br />

2M L2 − dΣ n 2 1<br />

E −<br />

2M dpn 2<br />

L2 <br />

dΣ n+1 − dΣ n 2 1 <br />

+ dp E 2M<br />

n+1 − dp n 2<br />

L2 <br />

, (3.100)<br />

which indicates that the stability condition of Equation 3.91 is satisfied during the mechan-<br />

ical step if 0.5 ≤ α ≤ 1.<br />

Remark 3.4. Equation 3.98 contains terms associated with pressure, which is character-<br />

istic of the coupled problem. Equation 3.98 is identically zero in the uncoupled mechanical<br />

problem (Simo, 1991).<br />

yields<br />

After the mechanical problem is solved, we deal with the flow problem. Equation 3.89<br />

1 dp<br />

M<br />

n+1 − dpn + Div(dv<br />

∆t<br />

n+α ) = 0, (3.101)<br />

∆dε = 0, ∆dεp = 0, ∆dξ = 0. (3.102)

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