Vo ( 1 - 4 + ²) 4/20 where Vo is 34 ft/s, A = 0.2, x is the distance in ft from L² the start of the diffuser (x = 0), and L is the exit of the diffuser (L = 4 ft). The flow is steady and can be treated as one-dimensional. 1. Determine the local acceleration at the entrance and the exit of the diffuser. Water decelerates in a diffuser following the relation V = V1-A- alocal, 0 = 0 ft/s²

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
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ft
vo (1 - 1 = ² ) 14/12
L² S
the start of the diffuser (x = 0), and L is the exit of the diffuser (L = 4 ft). The flow is steady and can be treated as one-dimensional.
1. Determine the local acceleration at the entrance and the exit of the diffuser.
Water decelerates in a diffuser following the relation V = Vo (1-A
alocal, 0 =
0
ft/s²
where Vo is 34 ft/s, A = 0.2, x is the distance in ft from
Transcribed Image Text:ft vo (1 - 1 = ² ) 14/12 L² S the start of the diffuser (x = 0), and L is the exit of the diffuser (L = 4 ft). The flow is steady and can be treated as one-dimensional. 1. Determine the local acceleration at the entrance and the exit of the diffuser. Water decelerates in a diffuser following the relation V = Vo (1-A alocal, 0 = 0 ft/s² where Vo is 34 ft/s, A = 0.2, x is the distance in ft from
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