Streamline Flow In Physics : In This Article We will learn that in steady flow the velocity of fluid particles reaching a particular point is the same at all time. Thus, each particle follows the same path as taken by a previous particle passing through that point. If the liquid is pushed in the tube at a rapid rate, the flow may become turbulent. In this case, the velocities of different particles passing through the same point may be different and change erratically with time. The motion of water in a high fall or a fast-flowing river is, in general, turbulent. Steady flow is also called streamline flow .
It is analogous to a line of force in an electric or magnetic field.
Pattern Of Streamline Flow In Physics : In steady flow, the pattern of streamlines is stationary with time and therefore, also called a streamline flow.
No two streamlines can ever cross one another, for if they did, a fluid particle arriving at that point would have possessed two directions (or two velocities) and hence the flow would never be steady.
In order to simplify the discussion, we make several assumptions:
(i) The flow is steady: The velocity and pressure at each point are constant in time
(ii) The fluid is incompressible: The density of fluid is constant throughout.
(iii) The flow is irrotational: A tiny paddle wheel placed in the liquid will not rotate. In rotational flow, for example, in eddies, the fluid has net angular momentum about a given point.
(iv) The fluid is non viscous: There is no dissipation of energy due to internal friction between adjacent layer in the fluid.
Types Of Streamline Flow : In physics, streamline flow can be categorized into two main types: laminar flow and turbulent flow. Laminar flow occurs when a fluid flows in parallel layers with minimal mixing between them, resulting in smooth and predictable motion. This type of flow is characterized by orderly streamlines and is often observed in low-viscosity fluids moving at low velocities. In contrast, turbulent flow involves chaotic and unpredictable movement, with irregularly shaped streamlines and mixing between adjacent fluid layers. It occurs at higher velocities or in fluids with higher viscosity and is commonly found in natural phenomena like rivers or in engineering applications like pipe flow.
Rotational Flow : The flow of liquid is said to be rotational if the angular velocity is non zero.
Irrotational Flow : The flow of the fluid is said to be irrotational if the element of the fluid at each point has no net angular velocity.
When the velocity exceeds a certain critical value, the nature of flow becomes complicated. Random, irregular, local currents (called vortices) develop throughout the fluids. The resistance to the flow increases tremendously. This type of flow is called 'turbulent flow'.
Equation Of Continuity : Consider a steady, irrotational flow of an ideal fluid through a tube of varying cross-section having no source or sink between the entry and the exit. If, A 1 and A 2 are the cross-sectional areas at points 1 and 2 respectively, v 1 and v 2 are the respective velocities of the liquid entering at 1 and leaving at 2 as shown in Figure.
(a) Velocity flux is the measure of the volume of liquid flowing in or out per second for a surface, the surface held normally to the liquid velocity (or liquid flow).
(b) The more the value of velocity flux, the more the number of streamlines cross the surface.
(c) We may also interpret the streamline picture as follows. In a narrow part of the tube the streamlines get closer together than in a wide part. Thus, as the distance between the streamlines decreases, the speed of the fluid increases.
(d) Widely spaced streamlines indicate regions of low speed, whereas closely spaced streamlines indicate regions of high speed.
(e) In hilly region, where the river is narrow and shallow (i.e., small cross-section) the water current will be faster, while in plains where the river is wide and deep (i.e., large cross-section) the current will be slower, and so deep water will appear to be still.
(f) When water falls from a tap, the velocity of falling water under the action of gravity will increase with distance from the tap. So, in accordance with continuity equation the cross section of the water stream will decrease and due to which the falling stream of water becomes narrower.
Consider two such points on the water stream having a separation h , areas A 1 , A 2 and respective velocities v 1 and v 2 , then from Equation of Continuity, we have
A 1 v 1 = A 2 v 2
Now, since we have
(i) If liquid entering a tube leaves the tube at two other points, and assuming that the tube has no source and sink, then we have
a 1 v 1 = a 2 v 2 + a 3 v 3
Water is flowing in a circular pipe of varying cross-sectional area, and at all points the water completely fills the pipe.
(a) At one point in the pipe the radius is 0.2 m. What is the magnitude of the water velocity at this point if the volume flow rate in the pipe is 1.20 m 3 s –1 ?
(b) At a second point in the pipe the water velocity has a magnitude of 3.80 ms –1 . What is the radius of the pipe at this point?
Solution:
(a) Q = volume flow rate = Av
(b) From continuity equation
A 1 v 1 = A 2 v 2
r
2
= 0.317 m