MATH 141 Calculus 2 • McGill University, Montreal

Revision sheet: moments, centres of mass and hydrostatic force (MATH 141)

This sheet is not a summary of section 8.3 of Stewart: you already have the course notes. It answers one question only, what makes students lose marks on moments, centroids and hydrostatic force in MATH 141 at McGill University, and which precise gesture avoids each loss.

Every number below is done by hand, as on the final, and every centroid quoted has been checked twice: by the integral, and by a symmetry, a bounding box or a second method. Forces are left as multiples of ρg\rho g, with ρg=9800\rho g = 9800 N/m3^3 for water.

The thread of the chapter

Every quantity of the chapter is a sum of pieces times their ARM: slice, then ask each slice how much and how far. For a moment the arm is the distance to the AXIS, for a pressure it is the depth below the SURFACE, and a strip's arm is taken at its MIDDLE.

This chapter is part of MATH 141, Calculus 2 (McGill)

The essentials

Moments: a piece times its distance to the axis

  • • Point masses: My=∑mixiM_y = \sum m_i x_i (arm = distance to the yy-axis), Mx=∑miyiM_x = \sum m_i y_i (arm = distance to the xx-axis). Then xˉ=Mym\bar{x} = \frac{M_y}{m}, yˉ=Mxm\bar{y} = \frac{M_x}{m}.
  • • Uniform plate between ff on top and gg below, on [a,b][a, b]: a vertical strip has area (f−g) dx(f - g)\,dx, abscissa xx and MIDPOINT at height f+g2\frac{f + g}{2}.
  • • Hence A=∫ab(f−g) dxA = \int_a^b (f - g)\,dx, My=∫abx(f−g) dxM_y = \int_a^b x(f - g)\,dx, Mx=∫ab12(f2−g2) dxM_x = \int_a^b \frac{1}{2}(f^2 - g^2)\,dx, and (xˉ,yˉ)=(MyA,MxA)(\bar{x}, \bar{y}) = \left(\frac{M_y}{A}, \frac{M_x}{A}\right). The density cancels.
  • • Symmetry principle: a uniform plate symmetric about a line has its centroid on that line. Composite plate: add the moments, subtract those of a hole, divide by the total area.
  • • Pappus: a region of area AA on ONE side of an axis, with its centroid at distance dd from the axis, sweeps a volume V=2πdAV = 2\pi d A.
0.510.51y = √xy = x²MC
The strip's arm is its midpoint MM, at height f+g2\frac{f + g}{2}; the region is symmetric about the dashed line y=xy = x, so its centroid CC lies on it.

Before any integral, write the strip with its two attributes: how much (its area) and how far (its arm). The formulas follow from that sentence, and so does every trap below.

Hydrostatic force: a pressure times an area, the depth from the surface

  • • At depth xx below the surface, P=ρgxP = \rho g x: ρg=9800\rho g = 9800 N/m3^3 for water in SI units, δ=62.5\delta = 62.5 lb/ft3^3 in imperial units.
  • • Slice the plate into HORIZONTAL strips, each at a single depth. With xx the depth and w(x)w(x) the width: F=∫ρg x w(x) dxF = \int \rho g\,x\,w(x)\,dx.
  • • ∫x w(x) dx\int x\,w(x)\,dx is the first moment of the plate about the surface line, so F=ρg dˉ AF = \rho g\,\bar{d}\,A with dˉ\bar{d} the depth of the CENTROID.
  • • Inclined plate at angle θ\theta to the horizontal: the strip has area w(x)dxsin⁡θw(x)\frac{dx}{\sin\theta}.
  • • The volume of water behind the plate never enters: only the depth and the shape of the wetted face. The resultant acts at the centre of pressure, ∫x2w dx∫x w dx\frac{\int x^2 w\,dx}{\int x\,w\,dx}, deeper than the centroid.

Say in words, on the first line of the answer, what xx measures and in which direction. Half the errors in hydrostatics are a depth measured from the wrong end.

The rules in table form

Each row reads from left to right: the assumptions, then the result. A red cell is not an answer, it is the finding that the form settles nothing and the instruction to rewrite it. Every case is followed by a worked example.

Piece, arm, contribution: the whole chapter in one grid

Read a line as: the piece of the first column, multiplied by the arm of the second, gives the contribution of the third. The examples use the region between y=xy = \sqrt{x} and y=x2y = x^2, of area 13\frac{1}{3}. The red lines are the rules students invent.

QuantityPieceArmContribution
MyM_y, point masses mim_i xix_i mixim_i x_i

Example: 33 kg at (1,2)(1, 2) contributes 33 to MyM_y and 66 to MxM_x.

MyM_y, plate (f−g) dx(f - g)\,dx xx x(f−g) dxx(f - g)\,dx

Example: ∫01x(x−x2) dx=25−14=320\int_0^1 x(\sqrt{x} - x^2)\,dx = \frac{2}{5} - \frac{1}{4} = \frac{3}{20}, so xˉ=920\bar{x} = \frac{9}{20}.

MxM_x, vertical strip (f−g) dx(f - g)\,dx f+g2\frac{f + g}{2} 12(f2−g2) dx\frac{1}{2}(f^2 - g^2)\,dx

Example: 12∫01(x−x4) dx=320\frac{1}{2}\int_0^1 (x - x^4)\,dx = \frac{3}{20}, so yˉ=920\bar{y} = \frac{9}{20}.

MxM_x, horizontal strip (y−y2) dy(\sqrt{y} - y^2)\,dy yy y(y−y2) dyy(\sqrt{y} - y^2)\,dy

Example: ∫01(y3/2−y3) dy=25−14=320\int_0^1 (y^{3/2} - y^3)\,dy = \frac{2}{5} - \frac{1}{4} = \frac{3}{20} again, with no factor 12\frac{1}{2}.

Force on a plate w(x) dxw(x)\,dx depth xx ρg x w(x) dx\rho g\,x\,w(x)\,dx

Example: Triangle, base 44 on the surface, height 33: ρg∫03x⋅43(3−x) dx=6ρg\rho g\int_0^3 x \cdot \frac{4}{3}(3 - x)\,dx = 6\rho g.

Volume, Pappus AA 2πd2\pi d 2πdA2\pi d A

Example: About the xx-axis: 2π⋅920⋅13=3π102\pi \cdot \frac{9}{20} \cdot \frac{1}{3} = \frac{3\pi}{10}.

MxM_x with (f−g)2(f - g)^2 (f−g) dx(f - g)\,dx f−g2\frac{f - g}{2} 12(f−g)2 dx\frac{1}{2}(f - g)^2\,dx no such rule

Example: 12∫01(x−x2)2 dx=9140\frac{1}{2}\int_0^1 (\sqrt{x} - x^2)^2\,dx = \frac{9}{140} gives yˉ=27140\bar{y} = \frac{27}{140}, not 920\frac{9}{20}.

What to do: The arm is the MIDPOINT height f+g2\frac{f + g}{2}, not half the length: (f−g)⋅f+g2=12(f2−g2)(f - g) \cdot \frac{f + g}{2} = \frac{1}{2}(f^2 - g^2).

Composite plate each piece its centroid average of centroids no such rule

Example: Rectangle 6×46 \times 4 plus half-disc of radius 33: the average gives 3.643.64, the true yˉ\bar{y} is 3.213.21.

What to do: Add the moments AkyˉkA_k\bar{y}_k and divide by the total area ∑Ak\sum A_k.

Every blue line is (piece) ×\times (arm), and the arm is always measured from the axis or from the surface, at the centre of the piece. The red lines are what you get by guessing the arm.

The mistakes that cost marks

These are the errors I correct most often in session. Each one costs marks on a paper, even when the reasoning behind it is right.

1. Building M_x from the x-coordinates

the whole centroid, reflected in the line y = x

What not to write

“33 kg at (1,2)(1, 2) and 11 kg at (−2,4)(-2, 4): Mx=3(1)+1(−2)=1M_x = 3(1) + 1(-2) = 1.”

What to write

“Mx=∑miyi=3(2)+1(4)=10M_x = \sum m_i y_i = 3(2) + 1(4) = 10 and My=∑mixi=3(1)+1(−2)=1M_y = \sum m_i x_i = 3(1) + 1(-2) = 1, so (xˉ,yˉ)=(14,52)(\bar{x}, \bar{y}) = \left(\frac{1}{4}, \frac{5}{2}\right).”

Why: A moment about the xx-axis measures a rotation ABOUT that axis, and the arm is the distance to it, ∣y∣|y|. A mass sitting on the xx-axis turns nothing about it, whatever its xx. The subscript names the axis, then xˉ=Mym\bar{x} = \frac{M_y}{m} and yˉ=Mxm\bar{y} = \frac{M_x}{m} cross over.

2. Squaring the difference instead of taking the difference of the squares

3 to 4 marks, the whole of the y-coordinate

What not to write

“Between y=xy = \sqrt{x} and y=x2y = x^2: Mx=12∫01(x−x2)2 dx=9140M_x = \frac{1}{2}\int_0^1 (\sqrt{x} - x^2)^2\,dx = \frac{9}{140}, so yˉ=27140\bar{y} = \frac{27}{140}.”

What to write

“Mx=12∫01((x)2−(x2)2)dx=12(12−15)=320M_x = \frac{1}{2}\int_0^1 \left((\sqrt{x})^2 - (x^2)^2\right)dx = \frac{1}{2}\left(\frac{1}{2} - \frac{1}{5}\right) = \frac{3}{20}, so yˉ=3/201/3=920\bar{y} = \frac{3/20}{1/3} = \frac{9}{20}.”

Why: The strip has length f−gf - g and its MIDPOINT is at height f+g2\frac{f + g}{2}: the product is 12(f−g)(f+g)=12(f2−g2)\frac{1}{2}(f - g)(f + g) = \frac{1}{2}(f^2 - g^2). Squaring f−gf - g slides every strip down to the xx-axis. Here yˉ=27140≈0.19\bar{y} = \frac{27}{140} \approx 0.19 would also break the symmetry xˉ=yˉ\bar{x} = \bar{y} of this region.

3. Using the top of the strip as its arm

the whole y-coordinate, and it goes unnoticed

What not to write

“yˉ=1A∫abf(x) dx\bar{y} = \frac{1}{A}\int_a^b f(x)\,dx, the height of the curve averaged over the region.”

What to write

“yˉ=1A∫ab12[f(x)]2 dx\bar{y} = \frac{1}{A}\int_a^b \frac{1}{2}[f(x)]^2\,dx: the strip of area f(x) dxf(x)\,dx has its own centroid at height 12f(x)\frac{1}{2}f(x).”

Why: Since ∫abf dx=A\int_a^b f\,dx = A, the wrong formula returns AA=1\frac{A}{A} = 1 for EVERY region, a pebble or a mountain. A formula that cannot see the region is not a centroid formula. For y=xy = \sqrt{x} on [0,4][0, 4] the true value is 34\frac{3}{4}.

4. Averaging the centroids of the pieces of a composite plate

2 to 3 marks

What not to write

“Rectangle 6×46 \times 4 with centroid at height 22, half-disc of radius 33 on top with centroid at 4+4π4 + \frac{4}{\pi}: yˉ=12(6+4π)≈3.64\bar{y} = \frac{1}{2}\left(6 + \frac{4}{\pi}\right) \approx 3.64.”

What to write

“Moments add: yˉ=24⋅2+9π2(4+4π)24+9π2=4(11+3π)16+3π≈3.21\bar{y} = \frac{24 \cdot 2 + \frac{9\pi}{2}\left(4 + \frac{4}{\pi}\right)}{24 + \frac{9\pi}{2}} = \frac{4(11 + 3\pi)}{16 + 3\pi} \approx 3.21.”

Why: A plain average treats the two pieces as equally heavy. The rectangle has area 2424 and the half-disc about 14.114.1: the weights are the AREAS (the masses, if the densities differ). A hole enters with a NEGATIVE area and a negative moment.

5. Measuring the depth from the bottom of the plate

the whole force, and here exactly the force on the triangle turned over

What not to write

“Triangle, base 44 along the surface, vertex 33 m down. With yy up from the vertex, width 43y\frac{4}{3}y: F=ρg∫03y⋅43y dy=12ρgF = \rho g\int_0^3 y \cdot \frac{4}{3}y\,dy = 12\rho g.”

What to write

“With yy up from the vertex, the DEPTH is 3−y3 - y: F=ρg∫03(3−y)43y dy=6ρgF = \rho g\int_0^3 (3 - y)\frac{4}{3}y\,dy = 6\rho g.”

Why: Pressure is ρg\rho g times the depth below the SURFACE. Any other variable is allowed, but the depth must then be rewritten in it. The safest choice is to let xx be the depth itself, measured downward from the surface, so the pressure is simply ρgx\rho g x.

6. Taking the pressure at the deepest point, or at the top

the whole force

What not to write

“The triangle above reaches depth 33, so F=ρg⋅3⋅6=18ρgF = \rho g \cdot 3 \cdot 6 = 18\rho g.”

What to write

“F=ρg dˉ AF = \rho g\,\bar{d}\,A with dˉ\bar{d} the depth of the CENTROID: dˉ=1\bar{d} = 1 (one third of the height, from the base), so F=ρg⋅1⋅6=6ρgF = \rho g \cdot 1 \cdot 6 = 6\rho g.”

surfacedepth 1depth 2F = 6ρgF = 12ρg
Same triangle, same area 66. Base on the surface: centroid at depth 11, F=6ρgF = 6\rho g. Turned over: centroid at depth 22, F=12ρgF = 12\rho g. Only the centroid depth changed.

Why: The pressure varies with depth, so no single point represents the plate, except the centroid: ∫(depth) dA\int (\text{depth})\,dA is the first moment about the surface line, which equals dˉA\bar{d}A. The deepest point overestimates, the top underestimates, and the true value always lies between the two.

7. Believing the centroid must lie on the plate

1 to 2 marks, and a correct answer rejected as absurd

What not to write

“The centroid of the half-ring 2≤r≤32 \le r \le 3, y≥0y \ge 0, is on the ring, so 2≤yˉ≤32 \le \bar{y} \le 3.”

What to write

“Mx=23(27−8)=383M_x = \frac{2}{3}(27 - 8) = \frac{38}{3} and A=π2(9−4)=5π2A = \frac{\pi}{2}(9 - 4) = \frac{5\pi}{2}, so yˉ=7615π<2\bar{y} = \frac{76}{15\pi} < 2, since π>3815\pi > \frac{38}{15}: the centroid is in the hole.”

C023-2-3
The half-ring between radii 22 and 33: its centroid CC, at height 7615π≈1.61\frac{76}{15\pi} \approx 1.61, sits in the hole, on the symmetry axis.

Why: The centroid is the balance point, not a point of the plate. It lies on the plate when the plate is CONVEX; a ring, an L or a crescent can put it in the empty part. Reject a centroid outside the bounding box, never one outside a non-convex plate.

8. Measuring the Pappus distance from the origin, or through the region

the whole volume

What not to write

“The region between x\sqrt{x} and x2x^2 turns about x=2x = 2; its centroid is at x=920x = \frac{9}{20}, so V=2π⋅920⋅13=3π10V = 2\pi \cdot \frac{9}{20} \cdot \frac{1}{3} = \frac{3\pi}{10}.”

What to write

“The distance to the AXIS is 2−920=31202 - \frac{9}{20} = \frac{31}{20}, so V=2π⋅3120⋅13=31π30V = 2\pi \cdot \frac{31}{20} \cdot \frac{1}{3} = \frac{31\pi}{30}.”

Why: In V=2πdAV = 2\pi dA, dd is the radius of the circle travelled by the centroid, measured to the axis of rotation. The theorem also requires the region to lie on ONE side of the axis: a disc turned about a diameter would give V=0V = 0. Shells confirm: 2π∫01(2−x)(x−x2) dx=31π302\pi\int_0^1 (2 - x)(\sqrt{x} - x^2)\,dx = \frac{31\pi}{30}.

9. Forgetting the slant on an inclined plate

half the force

What not to write

“Plate 44 m wide, inclined at 30∘30^\circ to the horizontal between depths 11 and 22: F=ρg∫124x dx=6ρgF = \rho g\int_1^2 4x\,dx = 6\rho g.”

What to write

“A band between depths xx and x+dxx + dx is dxsin⁡30∘=2 dx\frac{dx}{\sin 30^\circ} = 2\,dx long on the plate, so F=ρg∫12x⋅4⋅2 dx=12ρgF = \rho g\int_1^2 x \cdot 4 \cdot 2\,dx = 12\rho g.”

Why: The strips are still taken at constant depth, but their width ALONG the plate is dxsin⁡θ\frac{dx}{\sin\theta}, θ\theta being the angle with the horizontal. Without that factor you compute the force on the shadow of the plate on a vertical wall.

Which method to choose

Hydrostatic force: which route, by the FORM of the plate

Look at the shape of the plate and at where it sits in the water before writing any integral

dry crestwater surface: x = 0x6 m24 mwidth 56 - 2x/3
Last branch: the crest is dry, so x=0x = 0 moves down to the water line and the width becomes 56−23x56 - \frac{2}{3}x on [0,24][0, 24], not 60−23x60 - \frac{2}{3}x.
  • If a rectangle, a triangle or a disc, vertical → F=ρg dˉ AF = \rho g\,\bar{d}\,A with the known centroid: mid-height, one third from the base, the centre

    Example: triangle with its vertex at the surface, base 44 at depth 33: ρg⋅2⋅6=12ρg\rho g \cdot 2 \cdot 6 = 12\rho g

  • If a plate bounded by curves → horizontal strips, xx = depth from the surface, w(x)w(x) read from the equations and checked at both ends

    Example: gate x2≤y≤4x^2 \le y \le 4: depth 4−y4 - y, width 2y2\sqrt{y}, F=25615ρgF = \frac{256}{15}\rho g

  • If a plate symmetric about a horizontal line → put the origin at its centre: the odd part of the integral vanishes

    Example: porthole of radius RR, centre at depth dd: F=ρg d πR2F = \rho g\,d\,\pi R^2

  • If a plate inclined at θ\theta to the horizontal → same strips at constant depth, area w(x)dxsin⁡θw(x)\frac{dx}{\sin\theta}

    Example: 44 m wide, 30∘30^\circ, depths 11 to 22: F=12ρgF = 12\rho g

  • If the water level is below the top of the plate → integrate the wetted part only, depth 0 at the NEW surface, width rewritten from there

    Example: dam 6060 to 4040 m wide, 3030 m high, water 66 m below the crest: w=56−23xw = 56 - \frac{2}{3}x on [0,24][0, 24]

Whatever the route, finish with the bracket check: ρg dtopA<F<ρg dbottomA\rho g\,d_{\text{top}}A < F < \rho g\,d_{\text{bottom}}A.

How the answer is expected to be written

A marker ticks steps. Here they are in order, with the concluding sentence expected word for word.

Setting up a hydrostatic force integral

When to use it: Any question that asks for the force exerted by a liquid on a plate, a window, a gate or a dam

  1. 1 Draw the plate, the surface, and ONE horizontal strip. State the variable in words: xx = depth below the surface, measured downward, in metres.
  2. 2 Give the bounds as depths: where the wetted plate starts and where it ends.
  3. 3 Write the width w(x)w(x) from the geometry (similar triangles, the equation of a curve), and check it at both bounds.
  4. 4 Write F=∫ρg x w(x) dxF = \int \rho g\,x\,w(x)\,dx and evaluate; keep ρg\rho g as a factor until the end.
  5. 5 Check with ρg dˉ A\rho g\,\bar{d}\,A when the centroid is known, or with the bracket between top and bottom pressures, then give the units.

Concluding sentence

“Let xx be the depth below the surface. The strip at depth xx has width w(x)=6−2xw(x) = 6 - 2x and area (6−2x) dx(6 - 2x)\,dx, and the pressure there is ρgx\rho g x, so F=ρg∫03x(6−2x) dx=9ρgF = \rho g\int_0^3 x(6 - 2x)\,dx = 9\rho g, that is 88 20088\,200 N.”

The trap: A width function taken from the drawing without checking its two ends, or a depth that silently becomes a height. The check of step 3 costs ten seconds and saves the question.

Marking: Typically 1 mark for the variable and bounds, 1 for the width, 1 for the integral, 1 for the evaluation; the check protects the other four.

Check before you hand in

Five minutes of checking recover more marks than one more problem started in a hurry.

The typical problem, taken apart

The centroid of a region between two curves, checked by symmetry, then used by Pappus

Let RR be the region between y=xy = \sqrt{x} and y=x2y = x^2. Find its centroid, then the volume of the solid obtained by rotating RR about the xx-axis.

No calculator. Every step must be justified as on a MATH 141 final.

Step 1

x=x2\sqrt{x} = x^2 gives x=x4x = x^4, so x=0x = 0 or x=1x = 1. At x=14x = \frac{1}{4}, x=12>116\sqrt{x} = \frac{1}{2} > \frac{1}{16}: x\sqrt{x} is on top. A=∫01(x1/2−x2) dx=23−13=13A = \int_0^1 (x^{1/2} - x^2)\,dx = \frac{2}{3} - \frac{1}{3} = \frac{1}{3}.

Why

Which curve is on top decides every sign that follows. Testing one point between the intersections is faster and safer than reading a sketch.

Step 2

My=∫01x(x1/2−x2) dx=∫01(x3/2−x3) dx=25−14=320M_y = \int_0^1 x(x^{1/2} - x^2)\,dx = \int_0^1 (x^{3/2} - x^3)\,dx = \frac{2}{5} - \frac{1}{4} = \frac{3}{20}, so xˉ=320⋅3=920\bar{x} = \frac{3}{20} \cdot 3 = \frac{9}{20}.

Why

The arm of a vertical strip for MyM_y is its abscissa xx. Rewriting x\sqrt{x} as x1/2x^{1/2} before multiplying by xx keeps the power rule clean.

Step 3

Mx=∫0112((x)2−(x2)2)dx=12∫01(x−x4) dx=12(12−15)=320M_x = \int_0^1 \frac{1}{2}\left((\sqrt{x})^2 - (x^2)^2\right)dx = \frac{1}{2}\int_0^1 (x - x^4)\,dx = \frac{1}{2}\left(\frac{1}{2} - \frac{1}{5}\right) = \frac{3}{20}, so yˉ=920\bar{y} = \frac{9}{20}.

Why

Difference of the squares, from the midpoint f+g2\frac{f + g}{2} of the strip. This is the step where the marks are, and where 12(f−g)2\frac{1}{2}(f - g)^2 would give 27140\frac{27}{140}.

Step 4

Check: y=xy = \sqrt{x} and y=x2y = x^2 are inverse functions on [0,1][0, 1], so RR is symmetric about y=xy = x and xˉ=yˉ\bar{x} = \bar{y} is FORCED. Our 920=920\frac{9}{20} = \frac{9}{20} agrees.

Why

A symmetry check costs one sentence and verifies two independent integrals at once. It also tells you, before computing, that one of them could have been skipped.

Step 5

Pappus: RR lies above the xx-axis, at distance yˉ=920\bar{y} = \frac{9}{20}, so V=2π⋅920⋅13=3π10V = 2\pi \cdot \frac{9}{20} \cdot \frac{1}{3} = \frac{3\pi}{10}. Washers: π∫01(x−x4) dx=3π10\pi\int_0^1 (x - x^4)\,dx = \frac{3\pi}{10}.

Why

About the xx-axis, V=2πMxV = 2\pi M_x exactly, so the two methods share one integral. Pappus pays off most when the axis is a line like y=−1y = -1 or x=2x = 2.

The conclusion, written out

“The centroid of RR is (920,920)\left(\frac{9}{20}, \frac{9}{20}\right), on the line of symmetry y=xy = x, and the solid obtained by rotating RR about the xx-axis has volume 3π10\frac{3\pi}{10}.”

The classic mistake on this problem: Writing Mx=12∫01(x−x2)2 dxM_x = \frac{1}{2}\int_0^1 (\sqrt{x} - x^2)^2\,dx, which gives yˉ=27140\bar{y} = \frac{27}{140} and breaks the symmetry; or dividing MyM_y by MxM_x instead of by AA.

Learn by heart

  • • Mx=∑miyiM_x = \sum m_i y_i, My=∑mixiM_y = \sum m_i x_i; xˉ=Mym\bar{x} = \frac{M_y}{m}, yˉ=Mxm\bar{y} = \frac{M_x}{m}. The subscript names the AXIS.
  • • Plate: My=∫x(f−g) dxM_y = \int x(f - g)\,dx, Mx=∫12(f2−g2) dxM_x = \int \frac{1}{2}(f^2 - g^2)\,dx, divide by A=∫(f−g) dxA = \int (f - g)\,dx.
  • • Symmetry line of a uniform plate: the centroid is on it. Composite plate: add moments, never centroids.
  • • Pappus: V=2πdAV = 2\pi d A, dd to the AXIS, region on one side of it.
  • • P=ρgxP = \rho g x with xx the depth below the SURFACE; ρg=9800\rho g = 9800 N/m3^3, δ=62.5\delta = 62.5 lb/ft3^3.
  • • F=∫ρg x w(x) dx=ρg dˉ AF = \int \rho g\,x\,w(x)\,dx = \rho g\,\bar{d}\,A. Inclined plate: dxsin⁡θ\frac{dx}{\sin\theta}.
  • • Triangle: centroid one third of the height from the base. Half-disc: 4r3π\frac{4r}{3\pi} from the diameter.

Frequently asked questions

How do I find the centroid of a region between two curves?

Find where the curves meet and which one is on top. The area is the integral of top minus bottom. The x-coordinate is the integral of x times top minus bottom, divided by the area. The y-coordinate is the integral of one half of top squared minus bottom squared, divided by the area. Then check that the point lies inside the region and on any line of symmetry.

Why is there a one half in the formula for the y-coordinate of the centroid?

A thin vertical strip has its own centroid at its midpoint, halfway between the bottom curve and the top curve. Its moment about the x-axis is its area, top minus bottom times dx, multiplied by that midpoint height, top plus bottom over two. The product is one half of top squared minus bottom squared. The one half comes from the midpoint, not from anything else.

How do I calculate the hydrostatic force on a dam or a vertical plate?

Measure the depth x downward from the water surface. Cut the plate into thin horizontal strips, each at one depth. A strip of width w(x) and thickness dx feels the pressure rho g x, so the force is the integral of rho g times x times w(x). For water, rho g is 9800 newtons per cubic metre. The answer equals rho g times the depth of the centroid times the area.

When can I use the theorem of Pappus?

Whenever a plane region is rotated about a line in its plane that does not cut through the region. The volume is two pi times the distance from the centroid to the axis times the area. It is fastest when the centroid is known from symmetry, like a disc making a torus, and when the axis is not a coordinate axis. The distance is always measured to the axis, never to the origin.

Does the length of a lake change the force on its dam?

No. The pressure at a point depends only on its depth below the surface, not on how much water lies behind it. The force on the dam depends only on the depth of the water and the shape of the wetted face. A dam holding back a small pond and a dam holding back a long lake feel the same force if the depth and the face are the same.

Practise it

Corrected exercises: Moments, centres of mass and hydrostatic force, MATH 141 at McGill

A method is proved on a paper, not on a sheet. The set for the same chapter takes each of these traps into a problem, with the solution written out step by step.

  • 10 corrected exercises
  • 100 points
  • 150 minutes
Do the exercises
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