Linear
Parabolic
Hyperbolic
Inverse type
A. Linear
One dimensional flow
Uniform flow
Steady flow
Turbulent flow
Centroid of the displaced volume of fluid
Center of pressure of displaced volume
Does not exist
None of the above
Length of both the pipes is same
Diameter of both the pipes is same
Loss of head and discharge of both the pipes is same
Loss of head and velocity of flow in both the pipes is same
Same as
Less than
More than
None of these
Atmospheric pressure
Pressure in pipes and channels
Pressure in Venturimeter
Difference of pressures between two points in a pipe
One-dimensional flow
Two-dimensional flow
Three-dimensional flow
Four-dimensional flow
Real fluid
Ideal fluid
Newtonian fluid
Non-Newtonian fluid
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
Velocity, depth, pressure, etc. change from point to point in the fluid flow.
The fluid particles move in plane or parallel planes and the streamline patterns are identical in each plane
Decreases linearly with elevation
Remain constant
Varies in the same way as the density
Increases exponentially with elevation
Velocity of liquid
Pressure of liquid
Area of mouthpiece
Length of mouthpiece
Dissolved air
Dissolved salt
Suspended matter
All of the above
Meta center
Center of pressure
Center of buoyancy
Center of gravity
Inversely proportional to H3/2
Directly proportional to H3/2
Inversely proportional to H5/2
Directly proportional to H5/2
N/mm2
N/m2
Head of liquid
All of these
(bd²/12) + x
(d²/12 x) + x
b²/12 + x
d²/12 + x
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
Up-thrust
Buoyancy
Center of pressure
All the above are correct
1/16 to 1/8
1/8 to 1/4
1/4 to 1/3
1/3 to 1/2
Above it
Below it
At same point
Above or below depending on area of body
Higher
Lower
Same
Higher/lower depending on temperature
Below the center of gravity
Below the center of buoyancy
Above the center of buoyancy
Above the center of gravity
Increases
Decreases
Remain unaffected
Unpredictable
103 kN/m2
10.3 m of water
760 mm of mercury
All of these
0.1 N-s/m2
1 N-s/m2
10 N-s/m2
100 N-s/m2
Acts in the plane of the interface normal to any line in the surface
Is also known as capillarity
Is a function of the curvature of the interface
Decreases with fall in temperature
Pressure head
Velocity head
Pressure head + velocity head
Pressure head - velocity head
ω.r/2g
ω².r²/2g
ω.r/4g
ω².r²/4g
Atmospheric pressure
Surface tension
Force of adhesion
Force of cohesion
Pressure in pipe, channels etc.
Atmospheric pressure
Very low pressures
Difference of pressure between two points
4μvl/wd²
8μvl/wd²
16μvl/wd²
32μvl/wd²