Metacentre
Center of pressure
Center of buoyancy
Center of gravity
C. Center of buoyancy
Friction loss and flow
Length and diameter
Flow and length
Friction factor and diameter
One-half
One-third
Two-third
None of these
Streamline flow
Turbulent flow
Steady flow
Unsteady flow
Less than 2000
Between 2000 and 2800
More than 2800
None of these
0.417 H5/2
1.417 H5/2
4.171 H5/2
7.141 H5/2
v²/2g
0.5v²/2g
0.375v²/2g
0.75v²/2g
Wake
Drag
Lift
Boundary layer
1
1000
100
101.9
Velocity
(Velocity)2
(Velocity)3
(Velocity)4
Higher
Lower
Same
Higher/lower depending on temperature
Underground flow
Flow past tiny bodies
Flow of oil in measuring instruments
All of these
Less
More
Equal
Less at low temperature and more at high temperature
At C.G. of body
At center of pressure
Vertically upwards
At metacentre
Steady uniform flow
Steady non-uniform flow
Unsteady uniform flow
Unsteady non-uniform flow
10-2 m2/s
10-3 m2/s
10-4 m2/s
10-6 m2/s
Circular
Square
Rectangular
Trapezoidal
Mach number
Froude number
Reynoldss number
Weber's number
p/sinα
2p/sinα
p/2sinα
2p/sin (α/2)
Pascal's law
Dalton's law of partial pressure
Newton's law of viscosity
Avogadro's hypothesis
w1a1 = w2a2
w1v1 = w2v2
a1v1 = a2v2
a1/v1 = a2/v2
Critical point
Vena contracta
Stagnation point
None of these
Principle of conservation of mass holds
Velocity and pressure are inversely proportional
Total energy is constant throughout
The energy is constant along a streamline but may vary across streamlines
Sub-sonic velocity
Super-sonic velocity
Lower critical velocity
Higher critical velocity
Equal to
Less than
More than
None of these
9.81 kN/m3
9.81 × 103 N/m3
9.81 × 10-6 N/mm3
Any one of these
Centre of gravity
Centre of pressure
Metacentre
Centre of buoyancy
The center of gravity of the body and the metacentre
The center of gravity of the body and the center of buoyancy
The center of gravity of the body and the center of pressure
Center of buoyancy and metacentre
1 %
1.5 %
2 %
2.5 %
Inertia
Gravity
Viscous
None of these
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 pleasure