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re: patience on morganza

Posted on 5/13/11 at 2:59 pm to
Posted by SCOTLANDtheBRAVE
louisiana
Member since Jul 2008
811 posts
Posted on 5/13/11 at 2:59 pm to
the power of the flow comes from the height differential. if there is 4 feet between the miss and the spillway, you get that sort of falling power. if the height is greater, you get exponentially more power. if the river is allowed to silt on the other side of the morganza spillway, you reduce the effectiveness of it with each foot of sedimentation allowed in the first couple of miles from the river. when you release the beast, you solve the sedimentation problem for many miles and for at least this year's flood (not to suggest it won't cause problems in the flood of 2015).
Posted by Quidam65
Q Continuum
Member since Jun 2010
19324 posts
Posted on 5/13/11 at 3:03 pm to
quote:

not to suggest it won't cause problems in the flood of 2015


Haven't you heard? The Mayans predicted the end of the world in December 2012. So what 2015 flood?
Posted by glb
Atlanta
Member since Sep 2008
1599 posts
Posted on 5/13/11 at 3:36 pm to
quote:

the power of the flow comes from the height differential. if there is 4 feet between the miss and the spillway, you get that sort of falling power. if the height is greater, you get exponentially more power. if the river is allowed to silt on the other side of the morganza spillway, you reduce the effectiveness of it with each foot of sedimentation allowed in the first couple of miles from the river.


I wasn't really asking for an explanation. What you are saying just isn't making sense. The water is going to have enough velocity that sediment deposition is not going to be a problem.
Posted by MountainTiger
The foot of Mt. Belzoni
Member since Dec 2008
14679 posts
Posted on 5/13/11 at 5:36 pm to
quote:

the power of the flow comes from the height differential. if there is 4 feet between the miss and the spillway, you get that sort of falling power. if the height is greater, you get exponentially more power.

This is not true. Pressure varies linearly with depth.
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