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How do I model a sub-critical flow with FLOW-3D? |
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November 8, 2012, 17:31 |
How do I model a sub-critical flow with FLOW-3D?
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#1 |
New Member
abbas bakhtiari
Join Date: Nov 2012
Posts: 4
Rep Power: 14 |
Hi dear
I want to model a sub-critical flowin FLOW-3D. When the height of the lower boundary is greater than of the upper boundary the water will enter the downstream boundary of the computational region. As a result of my assumptions is destroyed. Please help me |
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November 10, 2012, 15:24 |
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#2 | |
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max
Join Date: Oct 2011
Posts: 10
Rep Power: 15 |
Quote:
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November 11, 2012, 05:40 |
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#3 |
New Member
abbas bakhtiari
Join Date: Nov 2012
Posts: 4
Rep Power: 14 |
Ask better questions:
Why height of downstream is not more than height of upstream? if y2>y1 then flow-3d enter water of downstream boundary condition. y2=height of downstream y1=height of upstream i want y2>y1 and flow direction is upstream --> downstream but after Run flow direction is downstream --> upstream Last edited by abbaspwut; November 11, 2012 at 06:37. |
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November 11, 2012, 05:44 |
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#4 | |
New Member
abbas bakhtiari
Join Date: Nov 2012
Posts: 4
Rep Power: 14 |
Quote:
Why height of downstream is not more than height of upstream? if y2>y1 then flow-3d enter water of downstream boundary condition. y2=height of downstream y1=height of upstream i want y2>y1 and flow direction is upstream --> downstream but after Run flow direction is downstream --> upstream Last edited by abbaspwut; November 11, 2012 at 06:37. |
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November 27, 2012, 12:37 |
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#5 |
Senior Member
Jeff Burnham
Join Date: Apr 2010
Posts: 204
Rep Power: 17 |
FLOW-3D is a transient solver. You are using assumptions of steady-state gradually-varied flow. The only way to model this kind of situation is to include the control structure that causes the downstream free surface elevation to be higher than the upstream elevation. That is, you must model the contraction, critical transition structure, or bed elevation change explicitly, instead of assuming that by setting h2 > h1 you can force FLOW-3D to assume that the flow is steady/gradually-varied.
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