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15.3: Moment and Center of Mass

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Using a single integral we were able to compute the center of mass for a one-dimensional object with variable density, and a two dimensional object with constant density. With a double integral we can handle two dimensions and variable density.

Just as before, the coordinates of the center of mass are

ˉx=MyMˉy=MxM,

where M is the total mass, My is the moment around the y-axis, and Mx is the moment around the x-axis. (You may want to review the concepts in Section 9.6.)

The key to the computation, just as before, is the approximation of mass. In the two-dimensional case, we treat density σ as mass per square area, so when density is constant, mass is (density)(area). If we have a two-dimensional region with varying density given by σ(x,y), and we divide the region into small subregions with area ΔA, then the mass of one subregion is approximately σ(xi,yj)ΔA, the total mass is approximately the sum of many of these, and as usual the sum turns into an integral in the limit:

M=x1x0y1y0σ(x,y)dydx,

and similarly for computations in cylindrical coordinates. Then as before

Mx=x1x0y1y0yσ(x,y)dydxMy=x1x0y1y0xσ(x,y)dydx.

Example 15.3.1

Find the center of mass of a thin, uniform plate whose shape is the region between y=cosx and the x-axis between x=π/2 and x=π/2. Since the density is constant, we may take σ(x,y)=1.

It is clear that ˉx=0, but for practice let's compute it anyway. First we compute the mass:

M=π/2π/2cosx01dydx=π/2π/2cosxdx=sinx|π/2π/2=2.

Next,

Mx=π/2π/2cosx0ydydx=π/2π/212cos2xdx=π4.

Finally,

My=π/2π/2cosx0xdydx=π/2π/2xcosxdx=0.

So ˉx=0 as expected, and ˉy=π/4/2=π/8. This is the same problem as in example 9.6.4; it may be helpful to compare the two solutions.

Example 15.3.2

Find the center of mass of a two-dimensional plate that occupies the quarter circle x2+y21 in the first quadrant and has density k(x2+y2). It seems clear that because of the symmetry of both the region and the density function (both are important!), ˉx=ˉy. We'll do both to check our work.

Jumping right in:

M=101x20k(x2+y2)dydx=k10x21x2+(1x2)3/23dx.

This integral is something we can do, but it's a bit unpleasant. Since everything in sight is related to a circle, let's back up and try polar coordinates. Then x2+y2=r2 and

M=π/2010k(r2)rdrdθ=kπ/20r44|10dθ=kπ/2014dθ=kπ8.

Much better. Next, since y=rsinθ,

Mx=kπ/2010r4sinθdrdθ=kπ/2015sinθdθ=k15cosθ|π/20=k5.

Similarly,

My=kπ/2010r4cosθdrdθ=kπ/2015cosθdθ=k15sinθ|π/20=k5.

Finally, ˉx=ˉy=85π.

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This page titled 15.3: Moment and Center of Mass is shared under a CC BY-NC-SA 4.0 license and was authored, remixed, and/or curated by David Guichard via source content that was edited to the style and standards of the LibreTexts platform.

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