Part 2: Microscopic Momentum Balances with the Navier-Stokes
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I wish you were my professor...
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Hey, I'm from JHU and this lecture is way better than what I'm having right now.
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Thanks so much! I missed a lecture because of an EWB-VCU trip, and this got me up to speed.
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The end of part two was like the end of halo two. Biggest cliffhamger ever!!!!
Btw thanks this is very helpful
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it looks so easy when you doing it..Thank you so much...
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greetings from germany! i do love your style Dr. Morrison!
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Thank you.
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this is so awesome. please keep posting.
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Dr Morrison: I think you have made a mistake. The pressure along z is not constant, since gravity has a component in its direction. So the layering of equal pressures in the fluid will be horizontally, and the pressure does vary along z.
jzsfvss 1 year ago
@jzsfvss
Good morning! Gravity does have a component in the z-direction, as you say. This component of gravity causes the flow to move in the z-direction. You're thinking of fluid statics - if the fluid were not moving in the z-direction, there would be the isobars horizontally that you speak of. But the fluid can move in the z-direction, so the force of gravity goes into motion, not into fluid statics (rho g h). In the x-direction there is no motion and hence a pressure gradient.
DrMorrisonMTU 1 year ago 6