How Does Coriolis Force Influence Particle Motion in Rotating Systems?

In summary, the Coriolis force is an apparent force that arises in rotating systems, influencing the motion of particles by causing them to deviate from their initial path. In a rotating frame of reference, moving particles experience this force as a result of the rotation, leading to a rightward deflection in the Northern Hemisphere and a leftward deflection in the Southern Hemisphere. This effect is significant in various phenomena, including atmospheric and oceanic currents, where it plays a crucial role in shaping patterns of motion and stability. Understanding the Coriolis force is essential for predicting the behavior of particles in rotating systems, impacting fields such as meteorology, oceanography, and engineering.
  • #1
Bling Fizikst
96
10
Homework Statement
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Relevant Equations
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Source : JEE Advanced , Physics Sir JEE YT
Screenshot 2024-03-31 234456.png


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I tried to attempt it using Lagrangian , so according to the coordinate axes given in the diagram , the position of the particle is let's say ##(0,d,-z)##
Let ##r## be the distance between the particle and the axis of rotation such that it subtends an angle of ##\theta## from the y axis .
So , ##-z=d\tan\theta\implies -\dot{z}=d\sec^2\theta \dot{\theta}##
$$\mathcal{L}=\frac{1}{2}m\dot{z}^2=\frac{1}{2}md^2\sec^4\theta \dot{\theta}^2$$
Now , writing the euler-lagrange equation and simplifying gives : $$\ddot{\theta}=-2\tan\theta \dot{\theta}^2$$
I am not sure how to deal with this .
 
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  • #2
I suggest that you use Newton's 2nd law in the frame of the rotating disk to derive the equation of motion for the particle. Setting up a Lagrangian would require introducing potential energy functions corresponding to the forces.

You are not choosing your x-y-z coordinate system as given in the problem. Note that it says "We assign x axis along the chord with origin at middle of the chord". The z axis is perpendicular to the disk. With this coordinate system, the y and z coordinates of the small block have trivial values. You only need to derive an equation of motion for the x coordinate.
 
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  • #3
TSny said:
I suggest that you use Newton's 2nd law in the frame of the rotating disk to derive the equation of motion for the particle. Setting up a Lagrangian would require introducing potential energy functions corresponding to the forces.

You are not choosing your x-y-z coordinate system as given in the problem. Note that it says "We assign x axis along the chord with origin at middle of the chord". The z axis is perpendicular to the disk. With this coordinate system, the y and z coordinates of the small block have trivial values. You only need to derive an equation of motion for the x coordinate.
Actually , i already saw the solution using frame of rotating disk , so , i wanted to try it out with lagrangian (if it makes stuff more straightforward) . Also , about the potential energies , can we find them ? for instance if we consider the x axis as the reference for gravitational potential energy then it's value will be zero . So , i am not sure how potential energy for the other forces will be generated . I have attached the figure , but i think it will lead to the same equation as above . Do you think it's worth trying with lagrangian though?
Screenshot 2024-04-01 022029.png
 
  • #4
All motion takes place along the x-axis. Find an expression for the x-component of the net force acting on the particle as a function of ##x## (in the disk frame of reference): ##F^{net}_x (x)##.

Then, find a potential energy function ##V(x)## so that ##F^{net}_x (x) = -\dfrac {\partial V(x)}{\partial x}##. The Lagrangian will be ##L = T - V(x)##, where ##T## is the kinetic energy expressed as a function of ##\dot x##.

Of course, when you then set up the Euler-Lagrange equations, you will just get back ##m \ddot x = F^{net}_x (x)## which you could have written at the beginning. So, I don't see any advantage of the Lagrangian approach here.
 
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FAQ: How Does Coriolis Force Influence Particle Motion in Rotating Systems?

What is the Coriolis force and how does it arise in rotating systems?

The Coriolis force is a fictitious force that acts on particles moving within a rotating reference frame. It arises due to the rotation of the system, causing objects to appear to deflect from their intended path. This deflection is perpendicular to the direction of motion and the axis of rotation, and its magnitude depends on the velocity of the particle and the rate of rotation of the system.

How does the Coriolis force affect the motion of particles on Earth?

On Earth, the Coriolis force causes moving particles, such as air masses and ocean currents, to deflect to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This deflection influences weather patterns, ocean currents, and the general circulation of the atmosphere.

Why do particles appear to deflect to the right in the Northern Hemisphere and to the left in the Southern Hemisphere?

This apparent deflection occurs because the Earth is a rotating sphere. In the Northern Hemisphere, the rotation of the Earth causes moving particles to experience a force to the right of their direction of travel. Conversely, in the Southern Hemisphere, the rotation causes a force to the left. This is a result of the Coriolis effect acting perpendicular to the velocity of the particle and the axis of Earth's rotation.

Does the Coriolis force affect small-scale phenomena, like water draining in a sink?

While the Coriolis force does act on all moving particles in a rotating system, its effect is generally negligible on small-scale phenomena such as water draining in a sink. The Coriolis force is too weak compared to other forces, like surface tension and viscosity, to have a significant impact on such small scales.

How is the Coriolis force mathematically described?

The Coriolis force can be mathematically described by the equation \( \mathbf{F}_c = -2m(\mathbf{\Omega} \times \mathbf{v}) \), where \( \mathbf{F}_c \) is the Coriolis force, \( m \) is the mass of the particle, \( \mathbf{\Omega} \) is the angular velocity vector of the rotating system, and \( \mathbf{v} \) is the velocity vector of the particle. This equation shows that the Coriolis force is proportional to the mass of the particle, the rotation rate of the system, and the velocity of the particle, and it acts perpendicular to both the velocity of the particle and the axis of rotation.

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