Friction loss and flow
Length and diameter
Flow and length
Friction factor and diameter
A. Friction loss and flow
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
Energy/unit area
Velocity/unit area
Both of the above
It has no units
Steady flow
Unsteady flow
Laminar flow
Uniform flow
Centre of pressure
Centre of gravity
Centre of buoyancy
Metacentre
Sill or crest
Nappe or vein
Orifice
None of these
At normal pressure of 760 mm
At 4°C temperature
At mean sea level
All the above
Inversely proportional to H3/2
Directly proportional to H3/2
Inversely proportional to H5/2
Directly proportional to H5/2
2.4 m above the hydraulic gradient
6.4 m above the hydraulic gradient
10.0 m above the hydraulic gradient
5.0 above the hydraulic gradient
Tensile stress
Compressive stress
Shear stress
Bending stress
0.34 times
0.67 times
0.81 times
0.95 times
4.5 kN/m3
6 kN/m3
7.5 kN/m3
10 kN/m3
Moving
Viscous
Viscous and static
Viscous and moving
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
Pressure
Flow
Velocity
Discharge
One dimensional flow
Uniform flow
Steady flow
Turbulent flow
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
Higher
Lower
Same
Higher/lower depending on temperature
The nature of the liquid and the solid
The material which exists above the free surface of the liquid
Both of die above
Any one of the above
Adhesion
Cohesion
Surface tension
Viscosity
Notch
Weir
Mouthpiece
Nozzle
Decreases
Increases
Remain same
None of these
Pascal law
Newton's law of viscosity
Boundary layer theory
Continuity equation
Meta centre should be above e.g.
Centre of buoyancy and e.g. must lie on same vertical plane
A righting couple should be formed
All of the above
103 kN/m2
10.3 m of water
760 mm of mercury
All of these
Are viscous
Possess surface tension
Are compressible
Possess all the above properties
Keeps on increasing
Keeps on decreasing
Remain constant
May increase/decrease
One dimensional flow
Uniform flow
Steady flow
Turbulent flow
100 litres
250 litres
500 litres
1000 litres
Cylindrical shape
Convergent shape
Divergent shape
Convergent-divergent shape
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