Pinning by constant plus small scale velocity field - Adam Oberman Math

Pinning by constant plus small scale velocity field

Contents

Example from Homogenization of Porous Medium Equation

The next conjecture, which we verify numerically, is that if we take the velocity field

v = V0 + A0sin(x / ε)

i.e., if we add a small scale oscillatory velocity field to the constant velocity field, then in the limit that the scale goes to zero, the pinning set is

P = \{ u_x \in [V_0 - A_0, V_0+ A_0 ] \}

where the derivative is taken at the free boundary (actually we start with a linear profile for the function).


The following computational examples show the steady state, pinned front, which occurs after 2-4 units of time.

Pinning with slope 1, velocity 1 plus oscillating velocity field

The next example shows pinning by a constant velocity field (the constant is 1) plus a small scale oscillatory velocity field. Here the pinning would occur even without the small scale velocity field.


Pinning with slope 1, velocity 1 plus oscillating velocity field


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Pinning with slope .95, velocity 1 plus oscillating velocity field

The next example shows pinning by a constant velocity field (the constant is 1) plus a small scale oscillatory velocity field. Here the pinning would fail without the small scale velocity field.

We are seeing 5 snapshots, over a time interval of 1, so the speed (without the oscillations) would be .05, and the distance would be .05.

Pinning with slope .95, velocity 1 plus oscillating velocity field


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Pinning with slope 1.05, velocity 1 plus oscillating velocity field

The next example shows pinning by a constant velocity field (the constant is 1) plus a small scale oscillatory velocity field. Here the pinning would fail without the small scale velocity field.

We are seeing 5 snapshots, over a time interval of 1, so the speed (without the oscillations) would be .05, and the distance would be .05.

Pinning with slope 1.05, velocity 1 plus oscillating velocity field


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Pinning

The next example shows pinning by a constant velocity field (the constant is 1) plus a small scale oscillatory velocity field. Here the pinning would occur even without the small scale velocity field.

Pinning with constant 1 plus oscillating velocity field

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Example from Homogenization of Porous Medium Equation

Pinning with slope 1, velocity .9 plus oscillating velocity field

The next example shows pinning by a constant velocity field (the constant is 1) plus a small scale oscillatory velocity field. Here the pinning would fail without the small scale velocity field.

Pinning with slope 1, velocity .9 plus oscillating velocity field


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Pinning with slope 1, velocity 1.1 plus oscillating velocity field

The next example shows pinning by a constant velocity field (the constant is 1) plus a small scale oscillatory velocity field. Here the pinning would fail without the small scale velocity field.

We are seeing 5 snapshots, over a time interval of 1, so the speed (without the oscillations) would be .05, and the distance would be .05.

Pinning with slope 1, velocity 1.1 plus oscillating velocity field


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