Same
More
Less
None of these
A. Same
w × Q × H
w × Q × hf
w × Q (H - hf)
w × Q (H + hf)
Directly
Inversely
Both A and B
None of these
Inertia force
Viscous force
Gravity force
All of these
Shear stress to shear strain
Increase in volume to the viscosity of fluid
Increase in pressure to the volumetric strain
Critical velocity to the viscosity of fluid
The bodies A and B have equal stability
The body A is more stable than body B
The body B is more stable than body A
The bodies A and B are unstable
Q = Cd × bH₁ × √(2gh)
Q = Cd × bH2 × √(2gh)
Q = Cd × b (H2 - H1) × √(2gh)
Q = Cd × bH × √(2gh)
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
Inertial force and gravity
Viscous force and inertial force
Viscous force and buoyancy force
Pressure force and inertial force
Supersonics, as with projectile and jet propulsion
Full immersion or completely enclosed flow, as with pipes, aircraft wings, nozzles etc.
Simultaneous motion through two fluids where there is a surface of discontinuity, gravity forces, and wave making effect, as with ship's hulls
All of the above
Higher
Lower
Same
None of these
Same as
Less than
More than
None of these
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
Equal to
Less than
More than
None of these
Pressure head
Velocity head
Pressure head + velocity head
Pressure head - velocity head
Same as
Less than
More than
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
Less than
More than
Equal to
None of these
Gas law
Boyle's law
Charles law
Pascal's law
Increase
Decrease
Remain same
Increase/decrease depending on depth of immersion
Actual velocity of jet at vena contracta to the theoretical velocity
Loss of head in the orifice to the head of water available at the exit of the orifice
Loss of head in the orifice to the head of water available at the exit of the orifice
Area of jet at vena-contracta to the area of orifice
Frictional force
Viscosity
Surface friction
All of the above
Steady flow
Turbulent flow
Laminar flow
Non-uniform flow
wA
wx
wAx
wAx/sinθ
Less than 2000
Between 2000 and 2800
More than 2800
None of these
Sink to bottom
Float over fluid
Partly immersed
Be fully immersed with top surface at fluid surface
Elastic
Surface tension
Viscous
Inertia
Head of water (h)
h²
V/T
h/2
Absolute temperature
Temperature
Density
Modulus of elasticity
When its meatcentric height is zero
When the metacentre is above C.G.
When its e.g. is below its center of buoyancy
Metacentre has nothing to do with position of e.g. for determining stability
p/sinα
2p/sinα
p/2sinα
2p/sin (α/2)