Higher than the surface of liquid
The same as the surface of liquid
Lower than the surface of liquid
Unpredictable
C. Lower than the surface of liquid
Internal
External
Both A and B
None of these
4.1 s
5.2 s
10.4 s
14.1 s
Increase
Decrease
Remain same
Increase/decrease depending on depth of immersion
103 kN/m2
10.3 m of water
760 mm of mercury
All of these
Underground flow
Flow past tiny bodies
Flow of oil in measuring instruments
All of these
Pressure head
Velocity head
Pressure head + velocity head
Pressure head - velocity head
Less than
More than
Equal to
None of these
Directly
Inversely
Both A and B
None of these
Has the dimensions of 1/pressure
Increases with pressure
Is large when fluid is more compressible
Is independent of pressure and viscosity
Double
Four times
Eight times
Sixteen times
Head of water (h)
h²
V/T
h/2
0.375
0.5
0.707
0.855
Resultant force acting on a floating body
Equal to the volume of liquid displaced
Force necessary to keep a body in equilibrium
The resultant force on a body due to the fluid surrounding it
p/sinα
2p/sinα
p/2sinα
2p/sin (α/2)
0° C
0° K
4° C
100° C
Directly proportional
Inversely proportional
Square root of velocity
None of these
Cohesion
Adhesion
Viscosity
Surface tension
Cannot be compressed
Occupy definite volume
Are not affected by change in pressure and temperature
None of the above
Less than 2000
Between 2000 and 2800
More than 2800
None of these
Atmospheric pressure
Surface tension
Force of adhesion
Force of cohesion
Pascal's law
Dalton's law of partial pressure
Newton's law of viscosity
Avogadro's hypothesis
Fluids are capable of flowing
Fluids conform to the shape of the containing vessels
When in equilibrium, fluids cannot sustain tangential forces
When in equilibrium, fluids can sustain shear forces
Real fluid
Ideal fluid
Newtonian fluid
Non-Newtonian fluid
Constant
Variable
Zero
Zero under limiting conditions
Same as
Lower than
Higher than
None of these
Equal to
Less than
More than
None of these
Pressure energy + kinetic energy + potential energy
Pressure energy - (kinetic energy + potential energy)
Potential energy - (pressure energy + kinetic energy
Kinetic energy - (pressure energy + potential energy)
Density of liquid
Specific gravity of liquid
Compressibility of liquid
Surface tension of liquid
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
dQ/Q = 3/2 × (dH/H)
dQ/Q = 2 × (dH/H)
dQ/Q = 5/2 × (dH/H)
dQ/Q = 3 × (dH/H)