Center of Mass of Hemisphere

In summary, the center of mass of a hemisphere of radius R can be found by using the formula R_cm = (rho/M) Integral[(vector r) dv] where dv = r^2 Sin[theta] dr d[theta] d[phi]. In this case, the position vector r is replaced with r cos(theta) to account for the perpendicular distance above the x-y plane. This can also be understood by using the mathematical definition of moment, which is the same as the physics definition, and is often taught in calculus courses.
  • #1
Adoniram
94
6

Homework Statement


Find the center of mass of a hemisphere of radius R.

Homework Equations


R_cm = (rho/M) Integral[ (vector r) dv]

dv = r^2 Sin[theta] dr d[theta] d[phi]

The Attempt at a Solution


[/B]
In spherical polar coordinates, vector r = r r-hat, so the argument of the integral should be:
r^3 Sin[theta] dr d[theta] d[phi]

Well, that's what I would expect... I keep ending up with 3R/4, but other sources have it as 3R/8, and I see that the volume element dv is written with an extra Cos[theta] which I do not understand...

I have no problem integrating over volumes in E&M problems, so I do not get why this is such an issue for me.
 
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  • #2
Ok, I started to figure it out, but I'm not all the way there yet:

Obviously, by symmetry the CM is along the vertical Z-axis if the flat part of the hemisphere lies in the XY plane.

The height at any random r is: z = r Cos[theta]

If I plug THIS value into the integral, in lieu of the extra "r" I put in earlier, the integral comes out to 3R/8, exactly as I have seen from other sources.

What I don't understand is:
Why on Earth do you replace "r" (from the position vector r) with "r Cos[theta]" or "z"? Why doesn't it work without this?
 
  • #3
Adoniram said:
Ok, I started to figure it out, but I'm not all the way there yet:

Obviously, by symmetry the CM is along the vertical Z-axis if the flat part of the hemisphere lies in the XY plane.

The height at any random r is: z = r Cos[theta]

If I plug THIS value into the integral, in lieu of the extra "r" I put in earlier, the integral comes out to 3R/8, exactly as I have seen from other sources.

What I don't understand is:
Why on Earth do you replace "r" (from the position vector r) with "r Cos[theta]" or "z"? Why doesn't it work without this?
The extra factor of cos θ is included because in calculating the moment of dV, you are interested in the perpendicular distance of dV above the x-y plane, i.e., z, not the total distance r. This goes back to the definition of what a moment is.
 
  • #4
The mathematical 'centroid' of a three dimensional figure, which is the same as the center of mass of a solid with constant density, is the given by [itex]\overline{x}= \\int\int\int x dV[/itex]/V, [itex]\overline{y}= \int\int\int y dV/V[/itex], [itex]\overline{y}= \int\int\int z dV/V[/itex] where V is the volume, [itex]\int\int\int dV[/itex]. (The density, being constant, can be factored out of the integral in the numerator, as well as the mass integral in the denominator, and canceled).

Since this figure is symmetric around the z axes, it is immediate that [itex]\overline{x}= \overline{y}= 0[/itex]. To find [itex]\overline{z}[/itex], we can imagine the hemisphere divided into thin layers, each layer a circle with center at (0, 0, z), radius [itex]r= \sqrt{x^2+ y^2}= \sqrt{R^2- z^2}[/itex] and thickness dz. The area of such a disk is [itex]\pi (R^2- z^2)[/itex] and volume [itex]\pi (R^2- z^2)dz[/itex]. So [itex]\int\int\int z dV[/itex] reduces to [itex]\int_0^R (R^2z- z^3)dz[/itex].. The volume is, of course, [itex]\frac{2}{3}\pi R^3[/itex].
 
  • #5
I'm going through John Taylor's Classical Mechanics, and in the next section he talks about moments of inertia, but this has not been introduced yet where this problem arises. Is it possible to understand this problem without the use of the definition of the moment?

I understand it's easier to hand-wave away the horizontal components and see that the problem has symmetry along the XY plane, but I would rather be able to do it rigorously through math, rather than by assumption. Assumptions and hand-waving are all well and good once you've got a good hold of the problem, but I'd like to be able to work it out completely at least once before jumping to that part.
 
  • #6
Adoniram said:
In spherical polar coordinates, vector r = r r-hat, so the argument of the integral should be:
r^3 Sin[theta] dr d[theta] d[phi]

You left out the r-hat unit vector in the integrand.
 
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  • #7
Adoniram said:
I'm going through John Taylor's Classical Mechanics, and in the next section he talks about moments of inertia, but this has not been introduced yet where this problem arises. Is it possible to understand this problem without the use of the definition of the moment?

The moment of inertia is ∫ z2 dV, which is sometimes called the second moment, but this is irrelevant to the calculation of the centroid.

For calculating the centroid, you are interested in finding the first moment, which is ∫ z dV.

This distinction about moments should have been encountered in your mechanics classes at some point, and possibly also covered in a calculus class somewhere, as well.
 
  • #8
TSny said:
You left out the r-hat unit vector in the integrand.

Thank you for the tip. I did indeed forget to include r-hat, which is not constant. I put in r-hat = sincos(etc)...xhat, yhat, zhat, and indeed the xhat and yhat integrals evaluate to 0, and the z-hat integral gives exactly the right answer :)

I'm sure everything regarding the moments is true, but I really wanted to be able to understand this on a more fundamental level (mathematically) before including additional physics.
 
  • #9
Adoniram said:
I'm sure everything regarding the moments is true, but I really wanted to be able to understand this on a more fundamental level (mathematically) before including additional physics.

There's not much physics to include here.

The mathematical definition of moment and the physics definition are pretty much the same. If you study statistics to any depth, you'll come across these same concepts in figuring out things like expectation and variance and whatnot, which is why these concepts are often taught in calculus courses: Their utility is not confined to just one subject.
 

1. What is the center of mass of a hemisphere?

The center of mass of a hemisphere is the point at which the mass of the hemisphere is evenly distributed in all directions. It is the point at which the hemisphere would balance if it were placed on a pivot.

2. How is the center of mass of a hemisphere calculated?

The center of mass of a hemisphere can be calculated by taking the average of the x, y, and z coordinates of all the particles that make up the hemisphere. This can be done using calculus or by using the formula: x̄ = 0, ȳ = 0, z̄ = 3r/8, where r is the radius of the hemisphere.

3. What factors affect the center of mass of a hemisphere?

The center of mass of a hemisphere is affected by the radius of the hemisphere and the distribution of mass within the hemisphere. The center of mass will be closer to the curved surface if the mass is more evenly distributed, and it will be closer to the base if the mass is concentrated near the bottom.

4. How does the center of mass of a hemisphere relate to its stability?

The stability of a hemisphere depends on the position of its center of mass. If the center of mass is located above the base, the hemisphere will be stable. However, if the center of mass is located outside the base, the hemisphere will be unstable and will topple over.

5. Can the center of mass of a hemisphere be outside of the hemisphere?

No, the center of mass of a hemisphere will always be located within the hemisphere itself. This is because the hemisphere is a closed system and all the mass is contained within its boundaries. The center of mass cannot be located outside of the hemisphere.

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