4.4.22 · D1Multivariable Calculus

Foundations — Applications — mass, centre of mass, moments of inertia

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Before you can compute a single moment of inertia, you must be able to read the notation without stumbling. This page introduces each symbol one at a time, in an order where every new thing is built from the previous thing — never used before it is defined and drawn.


0. The stage: a flat plate sitting in the plane

Everything happens on a plate — a thin flat shape (a "lamina"). We lay it flat on a sheet of paper and draw two number lines through it: a horizontal one and a vertical one.

Figure — Applications — mass, centre of mass, moments of inertia

Why we need this. Every later symbol (, , , …) is a rule that reads off a point's and , both measured from the origin. If you cannot point to where the origin, and live in the picture, none of the formulas mean anything. You will meet these axes again the moment you set up integration limits in Double Integrals over General Regions.


1. The region — the shape we sum over

Look at the triangle in the figure below: is the entire shaded interior. When we write , the little underneath is telling us "only add up tiles that live inside this shape."

Why we need it. A real plate is not the whole infinite plane — it is a bounded shape. names that shape so the integral knows where to start and stop. Describing as inequalities (like ) is exactly the skill of Double Integrals over General Regions.


2. The tiny tile and its area

Here is the heart of the whole subject. We cannot handle a spread-out plate all at once, so we chop it into a grid of tiny rectangular tiles.

Figure — Applications — mass, centre of mass, moments of inertia

Why the word "element"? is the building element — the brick. The whole plate is millions of these bricks. An integral is the machine that adds all the bricks back together as they shrink to zero size.


3. The integral signs and

Why two signs and not one? A plate is two-dimensional: to cover it you sweep in both the direction and the direction. Each direction contributes one . Doing them one after the other (inner then outer) is the whole method of Double Integrals over General Regions; a solid body needs three signs, i.e. Triple Integrals.


4. Density — how heavy each tile is

The Greek letter (say "roh", the curly-p letter) is our name for density.

The mass of ONE tile is then

Why we need . Without it, a large tile and a small tile would count equally, and a heavy region would count the same as a light one. Density is what turns geometry (area) into physics (mass).


5. Distance from an axis — the "lever arm"

The last raw ingredient is distance. Three distances matter, and each is just a coordinate you already own.

Figure — Applications — mass, centre of mass, moments of inertia

Why ? That is the Pythagoras theorem: the straight hop is the hypotenuse of a right triangle whose two legs are (across) and (up). Square each leg, add, square-root — you get the diagonal. The picture above draws exactly this triangle. (Squaring also throws away any minus sign, which is why is always .)

Why the sign matters. Imagine a plate that straddles the -axis, equal and opposite. If we used everywhere, the two halves would add and push the balance point off-centre — wrong. Using signed , the left half's negative contributions subtract from the right half's positive ones, and the balance point lands correctly in the middle. Keep this in mind whenever a region crosses an axis.


6. First power vs second power — the whole plot in one line

Now every symbol is defined, the three recipes read cleanly. Watch only the power of the coordinate:

Because there are two axes, the moment and the inertia each come in two labelled versions — one per axis. Here is the notation the parent topic uses, defined now so it never appears unannounced:

  • Power (multiply by ) → mass . You are just counting stuff.
  • Power (multiply by the signed coordinate) → moment or ; divide by to get the balance point. First power because balance is about leverage, which is linear — and signed so opposite sides can cancel.
  • Power (multiply by coordinate²) → moment of inertia . Second power because spin energy grows with speed², and speed grows with radius. See Rotational Kinetic Energy and Angular Momentum for that story.

Why divide by for the balance point? The moment is "total sideways leverage". A single point mass placed at the balance point must reproduce that same leverage, so , giving . When is constant it cancels and the balance point becomes the pure-geometry centroid — the subject of Centroids and the Pappus Theorems.


7. The bar notation


8. A word about polar tiles (preview)

Sometimes a round region is far easier in polar coordinates, where a point is named not by but by its distance from the origin and a direction.

In these coordinates the tile is not a rectangle but a curved wedge, and its area is

where is a tiny step outward and a tiny turn. That extra is the Jacobian factor; the full story lives in Polar Coordinates and the Jacobian and its general version Change of Variables and Jacobians. For now just log the symbols and so they are not a shock later.


Prerequisite map

origin (0,0) = the zero point

x and y axes = a point address

Region R = the plate shape

Signed coord and distance to an axis

Tiny tile area dA

Integral sign = add all tiles

Density rho

Tile mass dm = rho times dA

Multiply dm by 1, signed coord, coord squared

Mass, Centre of Mass, Moment of Inertia

Read it bottom-up: the origin anchors the axes, axes give you points, points build the region and the lever arms, the region gets chopped into tiles, density turns tile-area into tile-mass, the integral adds them, and the power you raise the coordinate to selects mass vs moment vs inertia.


Equipment checklist

Test yourself — cover the right side and answer each aloud.

What is the origin, and what is it used for?
The point where the axes cross; every coordinate and the distance are measured from it.
What does the symbol mean in plain words?
Mass per unit area at the point ; it can differ from point to point.
What is , and why must it shrink to zero?
The area of one tiny tile; shrinking to zero makes the summed answer exact instead of blocky/approximate.
Write in terms of and .
— the mass of one tile.
Why does a double integral use two integral signs?
A plate is 2-D; you sweep tiles in both the and directions, one per direction.
What is the perpendicular distance from a tile at to the -axis?
The size , because you drop straight to the horizontal axis.
What is the distance from to the origin, and why?
, by Pythagoras — it is the hypotenuse of the right triangle with legs and .
Why do moments use the SIGNED coordinate but inertias use ?
Signed lets left () and right () mass cancel for balance; squaring erases the sign because spin-resistance is the same on both sides.
Define and .
(moment about the -axis), (moment about the -axis).
How do you get the balance point from these moments?
and : a point mass must reproduce the same moments.
Define , , and .
, , — resistance to spinning about the -axis, -axis, and origin.
What do you multiply by to get mass, moment, and moment of inertia?
By , by the signed coordinate, and by the coordinate squared.
What does the overbar in signify?
The one special solved value — the balance-point coordinate, not a running variable.
In polar coordinates, what are and , and what is ?
= distance from the origin, = angle anticlockwise from the positive -axis (radians); , the extra being the Jacobian factor.

This is the full toolkit assumed by the parent topic. Once every checklist line is automatic, the formulas there read like sentences.