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Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

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124 CHAPTER 5. FIXED-STRAIN AND FIXED-STRESS SPLITS<br />

different from those <strong>for</strong> the undrained split. Interestingly, they are identical to those <strong>for</strong> the<br />

fully coupled method.<br />

Remark 5.2. When the mechanical problem has complicated boundary conditions in<br />

multiple dimensions, we might not obtain the exact local value of Kdr in the flow problem<br />

of Equation 5.20 <strong>for</strong> the fixed-stress split. Let K est<br />

dr be an estimated local Kdr. We define η =<br />

Kdr/K est<br />

dr<br />

as the deviation factor between the true <strong>and</strong> estimated local drained bulk moduli.<br />

Then, following the same procedure of the Von Neumann method with the backward Euler<br />

time discretization, we obtain the condition <strong>for</strong> the linear stability as<br />

η ≥ 1<br />

<br />

1 −<br />

2<br />

1<br />

<br />

, (5.26)<br />

τ<br />

where one of the amplification factors is negative if η < 1, but all the amplification factors<br />

are positive if η > 1. From Equation 5.26, η ≥ 0.5 provides unconditional stability <strong>for</strong> linear<br />

problems.<br />

Suppose we use K est<br />

dr<br />

= K3D<br />

dr <strong>for</strong> incompressible fluid <strong>and</strong> solid grains when the true Kdr<br />

is K1D dr . In this case, τ = ∞ <strong>and</strong> η = 3(1 − ν)/(1 + ν), where ν is Poisson’s ratio. Since<br />

0 ≤ ν ≤ 0.5, 1.0 ≤ η ≤ 3.0, which gives unconditional stability with monotonic behavior.<br />

On the other h<strong>and</strong>, we obtain η = (1 + ν)/3(1 − ν) where we use K est<br />

dr<br />

= K1D<br />

dr<br />

while the<br />

true Kdr is K3D dr . In this case, instabilities may occur because 0.33 ≤ η ≤ 1.0 (e.g., η = 0.33<br />

when ν = 0.0), <strong>and</strong> we may lead to oscillatory behaviors, even though the scheme is stable.<br />

Hence, a less stiff K est<br />

dr than the true Kdr yields unconditional stability with monotonicity<br />

because it guarantees 1.0 ≤ η ≤ 3.0. Thus, it is appropriate to choose K 1D<br />

dr<br />

as Kest dr ’s <strong>for</strong> one, two, <strong>and</strong> three dimensional problems, respectively.<br />

, K2D<br />

dr , <strong>and</strong> K3D<br />

dr

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