How Does Non-Uniform Circular Motion Align with Complex Plane Calculations?

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Discussion Overview

The discussion revolves around the relationship between non-uniform circular motion and complex plane calculations, particularly how derivatives of position vectors in polar coordinates correspond to radial and tangential components of motion. Participants explore the mathematical representation of these components and question the implications for traditional physics equations, such as centripetal force.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • Some participants express curiosity about why differentiating complex representations of polar coordinates yields radial and tangential components, questioning the underlying principles.
  • Others argue that the radial acceleration term in the equations aligns with the traditional expression for centripetal acceleration, although some suggest that changes in radius complicate this relationship.
  • A few participants propose that the direction of the radial vector in polar coordinates does not necessarily align with the direction of centripetal acceleration, especially in non-uniform motion.
  • One participant introduces an example of uniform circular motion shifted from the origin to illustrate the differences in radial acceleration and centripetal acceleration.
  • There is a discussion about the implications of using polar coordinates for analyzing elliptical orbits and how gravitational forces can be treated in this context.
  • Some participants highlight the mathematical properties of complex numbers, such as the rotation induced by differentiation, as a key to understanding the relationship between the components.
  • Concerns are raised about whether the terms derived from differentiation are necessarily the correct radial and tangential components or if they could represent something else.

Areas of Agreement / Disagreement

Participants do not reach a consensus on the implications of the equations for traditional physics problems. There are multiple competing views regarding the interpretation of radial and tangential components and their relationship to centripetal acceleration.

Contextual Notes

Some participants note that the discussion involves assumptions about the constancy of radius and the nature of motion, which may not hold in all scenarios, particularly in non-uniform circular motion.

Who May Find This Useful

This discussion may be of interest to those studying advanced mechanics, mathematical physics, or anyone exploring the applications of complex numbers in physical contexts.

davidbenari
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sTPO2.jpg


These equations model circular motion. Equation R is the position vector given in polar coordinates. What I've done is represent this vector onto the complex plane via equation (1). Equation (2) and (3) are the first and second time-derivatives, respectively.

Now, the question I have is this one: It seems "magical" to me that these derivatives actually give me the radial and tangential components for velocity and acceleration. How do I demystify this? Why is this obvious, apart from the fact that e^(itheta) and ie^(itheta) model the polar unit vectors?

In other words, why doesn't projecting vectors given in polar coordinates onto the complex plane produce contradictions? Why does it work? Why is it that the terms actually represent the tangential and radial components?

Also, do these equations imply that the typical introductory physics problem where we have to find the centripetal force at the bottom of a ditch as simply mv^2/r wrong? Because of the term given for radial acceleration by equation (3).

Thanks. I hope my question is clear.

If it's useful I got this from http://farside.ph.utexas.edu/teaching/301/lectures/node89.html
 
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The radial acceleration term in equation (3) is the same as the oft-taught ##v^2/r##.
 
Only the negative part. The other part is referring to how my radius might be changing, which I think happens in a ditch.
 
If the radius in polar coordinates is non constant, then it isn't clear that the polar radial vector is the same direction as the "radius" in the centripetal acceleration.
 
I think the fact that the term is being multiplied by e^(itheta) means it is radial, it doesn't necessarily mean that it's in the direction of the "radius" of centripetal acceleration (meaning it doesn't have to point towards the center, because it's just radial). If you consider the case r''=0 then the radial acceleration is just -r*omega^2 whose magnitude is (v^2/r) and points towards the center.
 
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Well here's something that might be worth checking:

Suppose you have uniform linear motion, with no centripetal acceleration at all, along the path ##x = 1, \, y(t) = t##.
What does ##(\ddot{r} - r\dot{\theta}^2)## come out to be?

(I just scribbled this out but I haven't checked the answer carefully.)
 
No idea, it's making my brain hurt, what do you suggest? I think both terms (tangential and radial acceleration) would have to be zero.
 
Okay, even easier example:

Linear motion in the outward radial direction (away from the origin) with constant acceleration ##\ddot{r} = a_0##. This implies ##\dot{\theta} = 0##.

Is the polar radial acceleration ##(\ddot{r} - r\dot{\theta}^2) = 0?##
 
I would say no. I would say polar radial acceleration is just r''
 
  • #10
But what's your point are you saying | (r''-romega^2) | = v^2/r and always points towards the center of the circle? Because if that's it, I don't think it's true since there is a radial velocity term in equation (2).
 
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  • #11
The radial velocity term in (2) is by definition radial relative to (0, 0i) in the complex/polar plane. What I'm saying is that the radial "vector" ##e^{i\theta}## in complex/polar coordinates doesn't always coincide with the "radial" vector with respect to the circular motion.

One last example that you should be able to work out geometrically:

Consider uniform circular motion around the point (1, 0): that is, the usual uniform motion around the unit circle, except shifted to the right by 1 unit:
$$
\begin{align}
\theta(t) &= t \\
r(t) &= 2 \cos t
\end{align}
$$
The centripetal acceleration is always directed toward (1, 0), not (0, 0), and has a fixed magnitude ##v^2/r_{(1, 0)}##, where ##r_{(1, 0)}## is the distance to (1, 0).

Now compare the "radial" acceleration term in (3) to the (constant) centripetal acceleration at the two positions: ##\theta = 0## and ##\theta = \pi/4##.
 
  • #12
What is this thread really about? davidbenari, can you ask more specific questions?
 
  • #13
voko: I want to know why this method works; why is that just differentiating this complex number will actually give me the radial and tangential components? I want to demystify this as I said in my original question. Thanks.

olivermsun: I see your point, maybe this is only useful if you're considering stuff relative to the origin, which I'm fine with. By the way, do you know any other mathematical ways to deal with non-uniform circular motion? Do you know of any sources I could checkout? Thanks. BTW, if I'm considering some elliptical orbit, and say the sun is in (0,0i) then the radial acceleration cannot be simply v^2/r, right? Or instead of an elliptical orbit, if I consider a non-circular ditch or hill, the same goes right?
 
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  • #14
davidbenari,

If you are considering circular motion, then you can always find the center of the circle and then use the polar method you showed. Also, gravity acting on a orbiting body is always inward radial with respect to the origin (i.e., the sun) so you should be able to analyze elliptical orbits without a problem.

One alternative way I've seen the ##v^2/r## thing derived in mechanics and vector calculus is to use a moving "TNB" (tangent-normal-binormal) frame of reference. The tangent ##\vec{T}## is in the direction of your velocity , the "normal" direction ##\vec{N}## is chosen by ##d\vec{T}/dt##, and "binormal" is just ##\vec{T} \times \vec{N}## by convention. In this construction you can quickly see how ##\vec{N}## might not line up with your ##\vec{r}## in polar coordinates.

This is a bit more general than the polar coordinates method since it can be used for a arbitrary (non-circular) paths. A search for "TNB frame" on Wikipedia turns up Frenet–Serret formulas, which looks a little more complicated than it needs to be, but I think you can get the idea.
 
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  • #15
I do not see any mystery. The differentiation uses the standard chain rule. Multiplication by ##i## rotates the other multiplicand by 90 degrees counter-clock wise without changing its magnitude. But you probably know all of that. What is the real difficulty here?
 
  • #16
voko:

I know that, but I'm actually new to complex numbers so don't assume I'm knowledgeable in this. The mystery for me is this:

I can see how r*e^(itheta) models some position vector. Differentiating yields just another complex number, which I can rearrange such that I have some term multiplying e^(itheta) and another multiplying ie(itheta), which gives me some expression that looks as if it were a vector. Mysteriously (for me) these two terms are the actual radial and tangential components. Why is it that this is not just incidental, why was it necessarily the case that they have to be the tangential and radial components?
 
  • #17
If you see that ##r e^{i\theta} ## is a vector, why do you not see that the products of the differentiation are also vectors? They have the same structure, after all.
 
  • #18
I can see that they can be interpreted as vectors, but why does it happen to be that they actually correspond to the radial and tangential components? Why didn't something else come up as terms form my "unit vectors" ? Is this a useless question? I'm asking for why is the term for each "unit vector" the actual correct radial and tangential component.
 
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  • #19
The radial part is easy. Every complex number is a radial vector.

Why the derivative of ##e^{i\theta}## is tangential is more interesting. Algebraically, this is because ##e^{i\theta}## gets multiplied by ##i##, which means a 90-degree rotation. Geometrically, this is because the image of ##e^{i\theta}## is a set of unit vectors - the unit circle - so when a particular unit vector turns into one infinitesimally close to it, the direction of travel is perpendicular to the radius - in other word, tangential to the unit circle.
 
  • #20
In other words, ##d\theta## is tangential (or at least normal to ##\vec{r}##) in polar coordinates.
 
  • #21
Yeah I can see that. (I'm sorry if I'm being frustrating). Here's my proof for why the first time derivative produces the actual radial and tangential components. I hope this clears up what the actual question I'm asking is.
7GzWdRK.jpg


Z is the area of the square enclosed by sides e^(itheta) and r. dz is the sum of the rectangle above and the rectangle on the right. The square on the corner is ignored because its a double differential. (This is how I've seen the product rule been proven, btw).

Now equation (1) tells me how z changes as r is kept constant and I'm just changing e^(itheta) which is equivalent to a rotation on the complex plane. Equation (2) tells me how z changes as theta or e^(itheta) is kept constant, which is equivalent to moving radially relative to (0,0i). Equation (3) gives me the total change. I'll bring out dt to be on the bottom of dz and represent the derivative (dz/dt). And there it is, one side of the addition tells me how z changes keeping 'r' constant, and the other how it changes keeping 'theta' constant. Here I can see that the actual "components" do correspond to what I was looking for.

Now this way of doing things will be very tedious as I proceed. I want something general that tells me that the "components" will be what I'm looking for.
 
  • #22
I do not think that your diagram is correct. It seems to me that you treat ##e^{i\theta}## as a real number. It is not. Are you familiar with the concept "complex plane" (or the Argand plane)? Look it up. Read again what I said earlier about unit vectors.
 
  • #23
Yeah I'm familiar with the complex plane, that's why I feel comfortable with treating e^(itheta) and ie^(itheta) as vectors (and I know they're perpendicular). I think it's not invalid to do this type of diagram because you could work backwards by multiplying dz/dt * dt , and you would get equation (3). In any case, did this show what my actual question is? I'm completely OK with why e^(itheta) and ie^(itheta) are vectors, I just want to know why they produce the correct physical results when you differentiate 'z' . :(
 
  • #24
##e^{i\theta}## and ##ie^{i\theta}## are orthogonal unit vectors, radial and transverse, respectively. So their multipliers in the first and second derivatives of ##r e^{i\theta}## are necessarily the radial and transverse components of velocity and acceleration.
 
  • #25
I don't agree (and I hope you can prove me wrong), because my view is that those are just numbers that have the unique property that they can be interpreted as vectors. But they are not vectors, they are just numbers.
 
  • #26
So my suspicion that you were confusing complex numbers with real numbers was not entirely unfounded. A complex number is not "just a number". It is a pair of real numbers: ##(a, b) = a + ib ##. A 2D vector is also a pair of real numbers. This is why we can represent 2D vectors as complex numbers and vice versa.
 
  • #27
I know that it is similar to a vector. A complex number is "just a number" except that isn't necessarily a real number. I see the similarity with a vector, but my question still holds. I argue that it just can't be the same as a vector no matter how similar. I think the "proof" I posted in the image above is something similar to what I'm looking for. Was my point clear in the image I posted? (I'm sorry if I'm being annoying).
 
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  • #28
davidbenari,

Your diagram is perfectly clear. The radial and tangential parts really do come straight out of the chain rule in polar coordinates.
 
  • #29
olivermsun: But I think this way of doing things is going to be very tedious when I consider the second derivative. How can I generalise this or make it simpler?
 
  • #30
Well, it isn't so bad considering the usefulness of the polar form. Also, once you've derived it, you have the formula in-hand and don't need to do it again. :smile:

If your interest is in elliptical planetary orbits, I also recommend looking through the wikipedia entry on Kepler's[/PLAIN] laws.

If it's a more general motion you're looking at, then I'd probably start with vector paths in cartesian coordinates, [x(t), y(t), z(t)], which have very easy derivatives. Or perhaps the TNB frame I linked to earlier.
 
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