Pressure force
Elastic force
Gravity force
Surface tension force
C. Gravity force
Higher surface tension
Lower surface tension
Surface tension is no criterion
High density and viscosity
l/d² = (l₁/d₁²) + (l₂/d₂²) + (l₃/d₃²)
l/d³ = (l₁/d₁³) + (l₂/d₂³) + (l₃/d₃³)
l/d⁴ = (l₁/d₁⁴) + (l₂/d₂⁴) + (l₃/d₃⁴)
l/d⁵ = (l₁/d₁⁵) + (l₂/d₂⁵) + (l₃/d₃⁵)
Gauge pressure + atmospheric pressure
Gauge pressure - atmospheric pressure
Atmospheric pressure - gauge pressure
Gauge pressure - vacuum pressure
Sub-sonic flow
Sonic flow
Super-sonic flow
Hyper-sonic flow
Does not change
Decreases
Increases
None of these
w × Q × H
w × Q × hf
w × Q (H - hf)
w × Q (H + hf)
Is uniform flow
Is steady uniform flow
Takes place in straight lines
Involves zero transverse component of flow
Inertial force and gravity
Viscous force and inertial force
Viscous force and buoyancy force
Pressure force and inertial force
0.62
0.76
0.84
0.97
Has constant viscosity
Has zero viscosity
Is in compressible
None of the above
Orifice
Notch
Weir
Dam
Pressure in pipes, channels etc.
Atmospheric pressure
Very low pressure
Difference of pressure between two points
Inertia force
Viscous force
Gravity force
All of these
Volumetric strain
Volumetric index
Compressibility
Adhesion
Kinematic viscosity in C. G. S. units
Kinematic viscosity in M. K. S. units
Dynamic viscosity in M. K. S. units
Dynamic viscosity in S. I. units
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
The magnitude and direction of the velocity do not change from point to point in the fluid
The fluid particles move in plane or parallel planes and the streamline patterns are identical in each plane
Increase
Remain unaffected
May increase or decrease depending on the characteristics of liquid
Decrease
Pressure in gases
Liquid discharge
Pressure in liquids
Gas velocities
At C.G. of body
At center of pressure
Vertically upwards
At metacentre
H/3
H/2
2H/3
3H/4
4.1 s
5.2 s
10.4 s
14.1 s
Venturimeter
Orifice plate
Nozzle
All of the above
Less than 2000
Between 2000 and 2800
More than 2800
None of these
Adhesion
Cohesion
Surface tension
Viscosity
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
Critical flow
Turbulent flow
Tranquil flow
Torrential flow
200 kg/m3
400 kg/m3
600 kg/m3
800 kg/m3
Continuity equation
Bernoulli's equation
Pascal's law
Archimedess principle
100 cm3
250 cm3
500 cm3
1000 cm3
Velocity of approach
Lower critical velocity
Higher critical velocity
None of these