Rectification and geometric applications

Rectification is the classical name for finding the length of a curve using integral calculus — literally "straightening" a bent path into an equivalent straight-line length. It sits inside the "Integral calculus and multiple integrals" unit of MA10002, right after the analytical machinery (reduction formulae, Beta and Gamma functions, Leibnitz's rule) and just before you start using the definite integral to measure genuinely geometric things: not just area under a curve, but the length of the curve itself, and later the areas and volumes swept out when curves revolve. The idea is the same one behind every application of the definite integral — chop the curve into tiny pieces, use Pythagoras on each piece, and sum (integrate) the results. What changes from problem to problem is only which form the curve is given in — Cartesian y=f(x)y=f(x), parametric x(t),y(t)x(t),y(t), or polar r(θ)r(\theta) — because each form leads to a differently dressed version of the same square-root integrand.

The core insight

Arc length is the integral of the infinitesimal Pythagorean distance (dx)2+(dy)2\sqrt{(dx)^2+(dy)^2} along the curve, rewritten in whichever variable — xx, tt, or θ\theta — the curve is naturally parametrised by.

The core idea

Cartesian form. For a smooth curve y=f(x)y=f(x) on [a,b][a,b], a tiny piece of the curve over a step dxdx has horizontal run dxdx and vertical rise dy=y′ dxdy = y'\,dx, so by Pythagoras its length is (dx)2+(dy)2=1+(y′)2 dx\sqrt{(dx)^2+(dy)^2} = \sqrt{1+(y')^2}\,dx. Summing every such piece gives the arc length

s=∫ab1+(dydx)2 dx,s = \int_a^b \sqrt{1+\left(\frac{dy}{dx}\right)^2}\,dx,

where: ss is the arc length, and y′=dy/dxy' = dy/dx is the slope of the curve at each point.

Parametric form. When the curve is handed to you as x=x(t)x=x(t), y=y(t)y=y(t) for t∈[t1,t2]t\in[t_1,t_2], do not fight to eliminate tt and force it back into y=f(x)y=f(x) — differentiate both coordinates with respect to tt instead:

s=∫t1t2(dxdt)2+(dydt)2 dt,s = \int_{t_1}^{t_2} \sqrt{\left(\frac{dx}{dt}\right)^2+\left(\frac{dy}{dt}\right)^2}\,dt,

where: dx/dtdx/dt and dy/dtdy/dt are the component speeds along each axis; the integrand is again just (dx)2+(dy)2\sqrt{(dx)^2+(dy)^2}, now factored out by dtdt.

Polar form. For r=r(θ)r=r(\theta) on [θ1,θ2][\theta_1,\theta_2],

s=∫θ1θ2r2+(drdθ)2 dθ,s = \int_{\theta_1}^{\theta_2} \sqrt{r^2+\left(\frac{dr}{d\theta}\right)^2}\,d\theta,

where: rr is the radius at angle θ\theta and dr/dθdr/d\theta its rate of change; this follows from the parametric formula via x=rcos⁡θx=r\cos\theta, y=rsin⁡θy=r\sin\theta, differentiated with the product rule. The one decision that matters before you touch an integral sign is which of these three to use, and that is dictated purely by how the curve is presented: y=f(x)y=f(x) calls for the Cartesian form, a pair (x(t),y(t))(x(t),y(t)) stays parametric, and a spiral- or cardioid-type curve given as r(θ)r(\theta) is far easier to rectify directly in polar form than after converting to Cartesian coordinates. Trying to force a parametric or polar curve back into y=f(x)y=f(x) before integrating is almost always the slower path — sometimes the elimination is algebraically painful, and sometimes it is not possible at all, so recognising the given form early saves real time in an exam. All three formulas are, underneath, the same statement: arc length is a definite integral of the local speed of tracing the curve, whether that tracing is with respect to xx, an abstract parameter tt, or the polar angle θ\theta. This is exactly the same "sum of infinitesimal pieces" logic that gives area under a curve — only here the pieces being summed are lengths of tiny line segments rather than thin rectangles of area, so the resulting integrand always carries a square root rather than a bare function value.

Figure
Three tiny curve segments each shown as a hypotenuse of a right triangle with legs dx and dy labelled, one drawn under a Cartesian curve, one under a parametric curve, one under a polar curve, illustrating that all three arc length formulas come from the same Pythagorean step
One Pythagorean step, three parametrisations dx dy y = f(x) ds = sqrt(1+y'^2) dx dx dy x(t), y(t) ds = sqrt(x-dot^2+y-dot^2) dt r dr r(theta) ds = sqrt(r^2+r'^2) dtheta
Derivation AThe parametric arc-length formula and the cycloid

The goal is to derive the general parametric arc-length formula from the Pythagorean step and then apply it to find the length of one complete arch of the cycloid x=a(θ−sin⁡θ)x=a(\theta-\sin\theta), y=a(1−cos⁡θ)y=a(1-\cos\theta) for θ∈[0,2π]\theta\in[0,2\pi], where a>0a>0 is a constant, reducing a square root that looks intractable at first glance into a single clean trigonometric term using a half-angle identity.

Step 1. Start from the infinitesimal right-triangle length ds=(dx)2+(dy)2ds=\sqrt{(dx)^2+(dy)^2} used for any smooth curve. If xx and yy are both functions of a single parameter tt, factor dt2dt^2 out from under the root: ds=(dx/dt)2+(dy/dt)2 dtds=\sqrt{(dx/dt)^2+(dy/dt)^2}\,dt. Summing (integrating) these pieces from t1t_1 to t2t_2 gives s=∫t1t2(dx/dt)2+(dy/dt)2 dts=\int_{t_1}^{t_2}\sqrt{(dx/dt)^2+(dy/dt)^2}\,dt, the parametric formula.

Step 2. Apply it with θ\theta as the parameter for the cycloid. Differentiate: dx/dθ=a(1−cos⁡θ)dx/d\theta = a(1-\cos\theta) and dy/dθ=asin⁡θdy/d\theta = a\sin\theta. Squaring and adding, (dx/dθ)2+(dy/dθ)2=a2(1−cos⁡θ)2+a2sin⁡2θ=a2[1−2cos⁡θ+cos⁡2θ+sin⁡2θ]=a2[2−2cos⁡θ](dx/d\theta)^2+(dy/d\theta)^2 = a^2(1-\cos\theta)^2+a^2\sin^2\theta = a^2\left[1-2\cos\theta+\cos^2\theta+\sin^2\theta\right] = a^2[2-2\cos\theta], using cos⁡2θ+sin⁡2θ=1\cos^2\theta+\sin^2\theta=1.

Step 3. Simplify the square root with the half-angle identity 1−cos⁡θ=2sin⁡2(θ/2)1-\cos\theta=2\sin^2(\theta/2): a2⋅2(1−cos⁡θ)=4a2sin⁡2(θ/2)a^2\cdot2(1-\cos\theta)=4a^2\sin^2(\theta/2), so the integrand becomes 4a2sin⁡2(θ/2)=2a∣sin⁡(θ/2)∣=2asin⁡(θ/2)\sqrt{4a^2\sin^2(\theta/2)}=2a\left|\sin(\theta/2)\right|=2a\sin(\theta/2) for θ∈[0,2π]\theta\in[0,2\pi], since sin⁡(θ/2)≥0\sin(\theta/2)\ge0 on that whole range.

Step 4. Integrate: s=∫02π2asin⁡(θ/2) dθ=2a[−2cos⁡(θ/2)]02π=−4a[cos⁡π−cos⁡0]=−4a(−1−1)=8as=\int_0^{2\pi}2a\sin(\theta/2)\,d\theta = 2a\left[-2\cos(\theta/2)\right]_0^{2\pi} = -4a\left[\cos\pi-\cos0\right] = -4a(-1-1) = 8a metres. One complete arch of the cycloid is exactly eight times the constant aa — a clean, memorable result that also serves as a check on the algebra. Verified: (dx/dθ)2+(dy/dθ)2=4a2sin⁡2(θ/2)(dx/d\theta)^2+(dy/d\theta)^2=4a^2\sin^2(\theta/2), giving arc length 8a8a.

Worked example

Problem. Find the length of the curve y=23x3/2y=\dfrac{2}{3}x^{3/2} from x=0x=0 to x=3x=3 (all lengths in metres).

Step 1. Differentiate: dydx=x1/2\dfrac{dy}{dx}=x^{1/2}, so 1+(y′)2=1+x1+(y')^2 = 1+x.

Step 2. Set up the Cartesian arc-length integral: s=∫031+x dxs=\int_0^3\sqrt{1+x}\,dx.

Step 3. Substitute u=1+xu=1+x, du=dxdu=dx; the limits become u=1u=1 (at x=0x=0) and u=4u=4 (at x=3x=3):

s=∫14u du=[23u3/2]14=23(43/2−13/2)=23(8−1)=143 m.s=\int_1^4\sqrt{u}\,du=\left[\frac{2}{3}u^{3/2}\right]_1^4=\frac{2}{3}\left(4^{3/2}-1^{3/2}\right)=\frac{2}{3}(8-1)=\frac{14}{3}\text{ m}.

Answer: s=143 m≈4.667 ms = \dfrac{14}{3}\text{ m} \approx 4.667\text{ m}.

Competitive stretch

The same half-angle trick from the derivation above also rectifies the cardioid r=a(1+cos⁡θ)r=a(1+\cos\theta), θ∈[0,2π]\theta\in[0,2\pi]. Here dr/dθ=−asin⁡θdr/d\theta=-a\sin\theta, so r2+(dr/dθ)2=a2(1+cos⁡θ)2+a2sin⁡2θ=a2[2+2cos⁡θ]=4a2cos⁡2(θ/2)r^2+(dr/d\theta)^2=a^2(1+\cos\theta)^2+a^2\sin^2\theta=a^2[2+2\cos\theta]=4a^2\cos^2(\theta/2) using 1+cos⁡θ=2cos⁡2(θ/2)1+\cos\theta=2\cos^2(\theta/2). Since cos⁡(θ/2)\cos(\theta/2) changes sign over [0,2π][0,2\pi], compute the upper half (θ∈[0,π]\theta\in[0,\pi], where cos⁡(θ/2)≥0\cos(\theta/2)\ge0) and double it: s=2∫0π2acos⁡(θ/2) dθ=4a[2sin⁡(θ/2)]0π=8a[sin⁡(π/2)−sin⁡0]=8as=2\int_0^\pi 2a\cos(\theta/2)\,d\theta=4a\left[2\sin(\theta/2)\right]_0^\pi=8a\left[\sin(\pi/2)-\sin0\right]=8a metres — the same 8a8a as the cycloid, a useful cross-check that the absolute-value handling was done correctly.

Common traps

  • Forgetting the 1+1+ inside the square root in the Cartesian formula — writing s=∫y′ dxs=\int y'\,dx instead of s=∫1+(y′)2 dxs=\int\sqrt{1+(y')^2}\,dx.
  • Mixing up the parametric and Cartesian formulas — the parametric integral runs over tt (or θ\theta), with limits that are parameter values, not xx-values.
  • Dropping the absolute value when simplifying sin⁡2(θ/2)\sqrt{\sin^2(\theta/2)} or cos⁡2(θ/2)\sqrt{\cos^2(\theta/2)}-type expressions — always check the sign of the quantity inside the square root before removing it, and split the range if the sign changes, as in the cardioid.
  • In the polar formula, forgetting the extra r2r^2 term and using (dr/dθ)2(dr/d\theta)^2 alone — both terms are needed under the square root.
  • Confusing rectification (arc length) with quadrature (area) — the two use structurally different integrands even though both are definite integrals.

Ask the tutor: if a half-angle simplification in an arc-length integrand is not falling into place, ask the AI tutor to walk through more trig-identity tricks used in rectification problems.

Why does the arc-length formula always have a square root in it?

Because it comes straight from the Pythagorean theorem. Each tiny piece of curve is treated as the hypotenuse of a right triangle with legs dxdx and dydy (or their equivalents in tt or θ\theta), so its length is (dx)2+(dy)2\sqrt{(dx)^2+(dy)^2}. Integrating sums up all these tiny hypotenuses. The square root is not a stylistic choice — it is baked into the geometry of distance itself, which is why every version of the formula, Cartesian, parametric or polar, keeps that same square-root shape.

How do I decide which of the three arc-length formulas to use for a given problem?

Look at how the curve is written down, not at what it looks like. If you are handed y=f(x)y=f(x) directly, use the Cartesian formula — converting it to another form only adds work. If the curve comes as a pair x(t)x(t), y(t)y(t), stay parametric even if you could in principle eliminate tt, because that elimination is often messy or impossible. If the curve is described as r(θ)r(\theta), such as a spiral or a cardioid, use the polar formula directly rather than converting to Cartesian coordinates first, which usually makes the algebra far worse.

Why do the cycloid and the cardioid both come out to exactly 8a?

It is a coincidence of these two specific curves, not a general law — most curves give arc lengths with no such tidy closed form. Both problems happen to reduce, via the identities 1−cos⁡θ=2sin⁡2(θ/2)1-\cos\theta=2\sin^2(\theta/2) and 1+cos⁡θ=2cos⁡2(θ/2)1+\cos\theta=2\cos^2(\theta/2), to an integrand that is a single trig function of θ/2\theta/2 scaled by 2a2a, and integrating that over the relevant range both times lands on 8a8a. It is a nice memorable check, useful for catching algebra slips, but do not expect it to generalise to other curves built from aa and θ\theta.

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