The liquid particles at all sections have the same velocities
The liquid particles at different sections have different velocities
The quantity of liquid flowing per second is constant
Each liquid particle has a definite path
B. The liquid particles at different sections have different velocities
Q = Cd × a × 2gh
Q = (2/3). Cd × a × h
Q = (Cd × a)/√(2gh)
Q = (3Cd × a)/√(2h)
Unity
Greater than unity
Greater than 2
Greater than 4
Weir
Notch
Orifice
None of these
High velocity
High pressure
Weak material
Low pressure
Equal to
Directly proportional
Inversely proportional
None of these
Buoyancy
Equilibrium of a floating body
Archimedes' principle
Bernoulli's theorem
Pascal
Poise
Stoke
Faraday
Remain unaffected
Increases
Decreases
None of these
Low density
High density
Low surface tension
High surface tension
0° C
0° K
4° C
20° C
Higher
Lower
Same as
None of these
Circular
Square
Rectangular
Trapezoidal
Velocity of flow in an open channel
Depth of flow in an open channel
Hydraulic jump
Depth of channel
Centre of pressure
Centre of gravity
Centre of buoyancy
Metacentre
Has constant viscosity
Has zero viscosity
Is in compressible
None of the above
Mach number
Froude number
Reynoldss number
Weber's number
Smooth and streamline flow
Laminar flow
Steady flow
Highly turbulent flow
0.83
0.6
0.4
0.3
dp/ρ + g.dz + v.dv = 0
dp/ρ - g.dz + v.dv = 0
ρ.dp + g.dz + v.dv = 0
ρ.dp - g.dz + v.dv = 0
d/6
d/4
d/2
d
The size of orifice is large
The velocity of flow is large
The available head of liquid is more than 5 times the height of orifice
The available head of liquid is less than 5 times the height of orifice
The direction and magnitude of the velocity at all points are identical
The velocity of successive fluid particles, at any point, is the same at successive periods of time
The magnitude and direction of the velocity do not change from point to point in the fluid
The fluid particles move in plane or parallel planes and the streamline patterns are identical in each plane
Law of gravitation
Archimedes principle
Principle of buoyancy
All of the above
2gH
H × √(2g)
2g × √H
√(2gh)
Pressure energy + kinetic energy + potential energy
Pressure energy - (kinetic energy + potential energy)
Potential energy - (pressure energy + kinetic energy
Kinetic energy - (pressure energy + potential energy)
2A × √H₁/Cd × a × √(2g)
2A × √H₂/Cd × a × √(2g)
2A × (√H₁ - √H₂)/Cd × a × √(2g)
2A × (√H3/2 - √H3/2)/Cd × a × √(2g)
Remain same
Decreases
Increases
None of these
Metres² per sec
kg sec/meter
Newton-sec per meter
Newton-sec² per meter
Steady uniform flow
Steady non-uniform flow
Unsteady uniform flow
Unsteady non-uniform flow
wA
wx
wAx
wAx/sinθ