Surface tension
Capillarity
Viscosity
Shear stress in fluids
C. Viscosity
Surface tension
Cohesion of the liquid
Adhesion of the liquid molecules and the molecules on the surface of a solid
All of the above
Surface tension
Coefficient of viscosity
Viscosity
Osmosis
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
Mass of liquid displaced
Viscosity of the liquid
Pressure of the liquid displaced
Depth of immersion
Pascal
Poise
Stoke
Faraday
Venturimeter
Orifice plate
Pitot tube
Rotameter
Pascal law
Newton's law of viscosity
Boundary layer theory
Continuity equation
Less than
More than
Equal to
None of these
100 litres
250 litres
500 litres
1000 litres
Specific weight
Mass density
Specific gravity
None of these
Be horizontal
Make an angle in direction of inclination of inclined plane
Make an angle in opposite direction to inclination of inclined plane
Any one of above is possible
Metres² per sec
kg sec/meter
Newton-sec per meter
Newton-sec² per meter
Above it
Below it
At same point
Above or below depending on area of body
Linearly
First slowly and then steeply
First steeply and then gradually
Unpredictable
Weber's number is the ratio of inertia force to elastic force.
Weber's number is the ratio of gravity force to surface tension force.
Weber's number is the ratio of viscous force to pressure force.
Weber's number is the ratio of inertia force to surface tension force.
Sub-sonic velocity
Super-sonic velocity
Lower critical velocity
Higher critical velocity
It is easier to see through the glass tube
Glass tube is cheaper than a metallic tube
It is not possible to conduct this experiment with any other tube
All of the above
Surface tension force
Viscous force
Gravity force
Elastic force
Local atmospheric pressure depends upon elevation of locality only
Standard atmospheric pressure is the mean local atmospheric pressure a* sea level
Local atmospheric pressure is always below standard atmospheric pressure
A barometer reads the difference between local and standard atmospheric pressure
(H - hf )/H
H/(H - hf )
(H + hf )/H
H/(H + hf )
0.0116 stoke
0.116 stoke
0.0611 stoke
0.611 stoke
A × √(m × i)
C × √(m × i)
AC × √(m × i)
mi × √(A × C)
Pressure energy + kinetic energy + potential energy
Pressure energy - (kinetic energy + potential energy)
Potential energy - (pressure energy + kinetic energy
Kinetic energy - (pressure energy + potential energy)
Pressure
Velocity
Square of velocity
Cube of velocity
Higher
Lower
Same
Higher/lower depending on temperature
Narrow-crested weir
Broad-crested weir
Ogee weir
Submerged weir
There is excessive leakage in the pipe
The pipe bursts under high pressure of fluid
The flow of fluid through the pipe is suddenly brought to rest by closing of the valve
The flow of fluid through the pipe is gradually brought to rest by closing of the valve
0.405 + (0.003/H)
0.003 + (0.405/H)
0.405 + (H/0.003)
0.003 + (H/0.405)
Steady uniform
Non-steady non-uniform
Non-steady uniform
Steady non-uniform
Compressibility
Surface tension
Cohesion
Adhesion