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
C. The body B is more stable than body A
An equivalent pipe is treated as an ordinary pipe for all calculations
The length of an equivalent pipe is equal to that of a compound pipe
The discharge through an equivalent pipe is equal to that of a compound pipe
The diameter of an equivalent pipe is equal to that of a compound pipe
Low density
High density
Low surface tension
High surface tension
Bottom surface of the body
C.G. of the body
Metacentre
All points on the surface of the body
One stoke
One centistoke
One poise
One centipoise
Reynold's number
Froude's number
Mach number
Euler's number
Inertia force
Viscous force
Gravity force
All of these
Width of channel at the top is equal to twice the width at the bottom
Depth of channel is equal to the width at the bottom
The sloping side is equal to half the width at the top
The sloping side is equal to the width at the bottom
Q = Cd × bH₁ × √(2gh)
Q = Cd × bH2 × √(2gh)
Q = Cd × b (H2 - H1) × √(2gh)
Q = Cd × bH × √(2gh)
0.34 times
0.67 times
0.81 times
0.95 times
A × √(m × i)
C × √(m × i)
AC × √(m × i)
mi × √(A × C)
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
Meta center
Center of pressure
Center of buoyancy
Center of gravity
Atmospheric pressure
Gauge pressure
Absolute pressure
None of these
Less than
More than
Equal
None of these
Centre of gravity
Centre of pressure
Metacentre
Centre of buoyancy
Smooth and streamline flow
Laminar flow
Steady flow
Highly turbulent flow
Equal to
Directly proportional
Inversely proportional
None of these
Fluid
Water
Gas
Ideal fluid
Law of gravitation
Archimedes principle
Principle of buoyancy
All of the above
Less
More
Equal
Less at low temperature and more at high temperature
Open channel/pipe flow
Compressibility of fluids
Conservation of mass
Steady/unsteady flow
Cohesion pressure is negligible
Cohesion pressure is decreased
Cohesion pressure is increased
There is no cohesion pressure
Centroid of the displaced volume of fluid
Center of pressure of displaced volume
Does not exist
None of the above
flv²/2gd
flv²/gd
3flv²/2gd
4flv²/2gd
Narrow crested weir
Broad crested weir
Ogee weir
Submerged weir
9.81 kN/m3
9.81 × 103 N/m3
9.81 × 10-6 N/mm3
Any one of these
The pressure below the nappe is atmospheric
The pressure below the nappe is negative
The pressure above the nappe is atmospheric
The pressure above the nappe is negative
Continuity equation
Bernoulli's equation
Pascal's law
Archimedess principle
Surface tension force
Viscous force
Gravity force
Elastic force
Inversely proportional to H3/2
Directly proportional to H3/2
Inversely proportional to H5/2
Directly proportional to H5/2