Line Integrals
Integrate a scalar function or a vector field along a curve, via parameterization.
The idea. Every integral so far added up a function over a straight domain — an interval, a flat region, a solid. A line integral adds up a function along a curve. Instead of integrating over [a, b] on the x-axis, you integrate along a path that bends through space. The trick that makes it work: parameterize the curve, which collapses the whole thing back to an ordinary single-variable integral in t.
Ready to put it into practice?
Start practicingParameterize the curve C as x = x(t), y = y(t) for t in [a, b]. The arc-length element is:
Arc-length element
- The curve (path) you integrate along.
- Parameterization of the curve.
- Arc-length element — a little bit of distance traveled along the curve.
What ds is: a little bit of arc length — the distance traveled along the curve for a little step dt. That square root is speed: how fast the point moves along the path as t ticks. Notice it's the same square-root shape as the surface-area stretch factor — both measure how much a step gets stretched.
The integral becomes a plain integral in t:
Line integral of a scalar function (with respect to arc length)
Line integral of a vector field — the physics-heavy one — work. Here F(x, y) = ⟨P(x, y), Q(x, y)⟩ is a vector field, and you're adding up the component of F along the direction of travel.
With r(t) = ⟨x(t), y(t)⟩:
Line integral of a vector field (work)
- Velocity vector — tangent to the curve, points in the direction of travel.
- A vector field.
- Work done by F along C; depends on the direction (orientation) of travel.
What it means physically: if F is a force, this is the work done moving along C. The dot product picks out how much of the force points the way you're going — force perpendicular to motion does no work, force along it does the most. This is the central object of the chapter.
The one big difference from every prior integral: orientation matters. A line integral of a vector field depends on which direction you traverse the curve. Reverse the path and the integral flips sign. (The scalar ds version does not flip — arc length is arc length regardless of direction. Only the vector/work version cares about orientation.)
Orientation
Worked example
Parameterize — already given.
Find r'(t): differentiate each component.
Evaluate F along the curve: substitute x = t, y = t^2 into F = ⟨y, x⟩.
Take the dot product.
Integrate over t. The parameterization turned a curve integral into an ordinary Calc 1 integral — that collapse is the whole method.
Answer:
How to solve one of these
- 1.
Parameterize the curve. Write , (and in 3D) for over some interval. If not given, you construct it — a line segment, a circle (, ), etc.
- 2.
Identify the type. Scalar needs the arc-length . Vector needs and a dot product.
- 3.
Scalar: compute ds and integrate. Compute , substitute the curve into , integrate.
- 4.
Vector: compute r'(t), evaluate F, and dot. Compute , evaluate along the curve, take , integrate.
- 5.
Integrate over t. It's now a single-variable integral. Substitute the -bounds.
- 6.
Mind the orientation. For vector line integrals, confirm you've parameterized in the direction the problem specifies — reversing flips the sign.
Take the component of F along the direction of travel at each point, and add it all up along the curve.
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