lesson

Unit 3 - Accumulation in Geometry, Physics, and Models · AP

Work, Fluid Force, and Variable Density

Model a changing force or weight one thin piece at a time and accumulate the physical contributions with an integral.

Why a single multiplication may fail

In elementary physics, work is often written as force times displacement: W=FdW=Fd. That formula is exactly right when the force is constant and acts along the direction of motion. Many physical systems are not so accommodating. A spring becomes harder to stretch as it lengthens, the weight of a hanging cable decreases as more cable reaches the floor, and water pressure increases with depth. In each case, the useful strategy is the same: describe one tiny piece whose force is nearly constant, find its small contribution, and add all such contributions.

The word work has a precise unit. In SI units, force is measured in newtons, abbreviated mathrmNmathrm{N}, and displacement is measured in meters, abbreviated mathrmmmathrm{m}. Their product is mathrmN⋅mmathrm{N}\cdot\mathrm{m}, called a joule, abbreviated mathrmJmathrm{J}. Writing units through a setup is more than bookkeeping. It distinguishes force from work and exposes a missing distance factor immediately.

L5-V01 — A variable-force graph. Create a vector graph in the established light grey-blue, black-bordered panel. Plot a positive increasing force F(x)F(x)F(x) against displacement xxx, shade one thin vertical rectangle, and label its approximate area F(x) dxF(x)\,dxF(x)dxThe work done over a very small displacement is approximated by force times the small displacement.
L5-V01 — A variable-force graph. Create a vector graph in the established light grey-blue, black-bordered panel. Plot a positive increasing force F(x)F(x)F(x) against displacement xxx, shade one thin vertical rectangle, and label its approximate area F(x) dxF(x)\,dxF(x)dx

Work as accumulated force-distance

Suppose a spring obeys Hooke’s law F(x)=kxF(x)=kx, where xx is extension from its relaxed length and kk is the spring constant. The constant kk has units mathrmN/mmathrm{N}/\mathrm{m}, so kxkx has units of force. To stretch the spring from x=0x=0 to x=ax=a, the small work needed to increase its extension by dxdx is

dW=F(x) dx=kx dx.dW=F(x)\,dx=kx\,dx.

Adding those small contributions gives

W=∫0akx dx=12ka2.W=\int_0^a kx\,dx=\frac{1}{2}ka^2.

For example, if k=200 N/mk=200\,\mathrm{N}/\mathrm{m} and a=0.10 ma=0.10\,\mathrm{m}, then the work is 1.0 J1.0\,\mathrm{J}. The result is not F(a)a=2.0 JF(a)a=2.0\,\mathrm{J} because that calculation incorrectly uses the final, largest force throughout the whole stretch. The graph makes the correction visible: the work is the triangular area under an increasing line, half of the rectangle with the same final height and width.

When a force points opposite the displacement, its work is negative. This sign is meaningful: it records energy transferred out of the moving object by the force. A problem must therefore state or imply a direction. In the examples here, F(x)F(x) is the magnitude of the applied force in the direction of motion, so each small contribution is positive. Never insert a sign only because an integral looks unfamiliar; derive it from the chosen coordinate direction.

L5-V02 — Spring work is area. Draw a force-versus-extension line from the origin, a shaded triangle below it, and a neighboring rectangle with the same final force and extension. Label the triangular area 12ka2\frac12ka^221​ka2 and the rectangle ka2ka^2ka2A linearly increasing spring force produces triangular work area, not final force multiplied by total extension.
L5-V02 — Spring work is area. Draw a force-versus-extension line from the origin, a shaded triangle below it, and a neighboring rectangle with the same final force and extension. Label the triangular area 12ka2\frac12ka^221​ka2 and the rectangle ka2ka^2ka2

Fluid force begins with pressure

Pressure is force per area. In a fluid at rest, pressure increases with depth because deeper material supports more fluid above it. If hh is depth below the surface, the pressure can be modeled as p(h)=ρghp(h)=\rho gh, where ρ\rho is mass density and gg is gravitational acceleration. In SI units, ho ho has units mathrmkg/m3mathrm{kg}/\mathrm{m}^3 and gg has units mathrmm/s2mathrm{m}/\mathrm{s}^2, giving pressure units of mathrmN/m2mathrm{N}/\mathrm{m}^2.

Take a horizontal strip of a vertical plate at depth hh with width w(h)w(h) and small height dhdh. Its area is w(h) dhw(h)\,dh, so the small fluid force is

dF=p(h)w(h) dh=ρgh w(h) dh.dF=p(h)w(h)\,dh=\rho gh\,w(h)\,dh.

The total force is found by integrating over the plate’s depth interval. Notice that this is not a volume calculation. The strip’s thickness is a vertical distance used to make an area strip, then pressure times that area gives force. The units confirm it: (N/m2)(m2)=N(\mathrm{N}/\mathrm{m}^2)(\mathrm{m}^2)=\mathrm{N}. Calling every dxdx or dhdh “volume” obscures the physical model.

L5-V03 — Fluid pressure on strips. Show a vertical rectangular plate submerged in water, divided into thin horizontal strips. Use longer arrows at deeper strips to show greater pressure, label depth hhh, width w(h)w(h)w(h), and strip area w(h) dhw(h)\,dhw(h)dhDeeper horizontal strips on a submerged plate experience greater pressure and therefore greater force.
L5-V03 — Fluid pressure on strips. Show a vertical rectangular plate submerged in water, divided into thin horizontal strips. Use longer arrows at deeper strips to show greater pressure, label depth hhh, width w(h)w(h)w(h), and strip area w(h) dhw(h)\,dhw(h)dh

Variable density makes the same idea portable

Density can vary along an object. A rod on the xx-axis with linear density λ(x)\lambda(x) measured in mathrmkg/mmathrm{kg}/\mathrm{m} has a small mass dm=λ(x) dxdm=\lambda(x)\,dx. Its weight contribution is gλ(x) dxg\lambda(x)\,dx, measured in newtons. If that piece must be lifted a distance D(x)D(x), then its small work contribution is

dW=gλ(x)D(x) dx.dW=g\lambda(x)D(x)\,dx.

This expression is worth reading in words: gravity times mass-per-length times a thin length gives the piece’s weight, and multiplying by lift distance gives its work. Different contexts merely change the factor that varies. In a cable-lifting problem, D(x)D(x) may depend on where the piece starts. In a pumping problem, a fluid slice’s weight is determined by its volume and density, while its lift distance is determined by its depth. The integral is a concise record of this local accounting.

Before integrating, make a table with four columns: the small piece, its amount or area, the force on it, and the distance through which that force acts. This is more reliable than hunting for a memorized formula. It makes assumptions testable and keeps dimensions attached to every factor. If two terms describe the same physical feature, the table will often reveal that you counted it twice.

Retrieval check

A cable of length 12 m12\,\mathrm{m} has constant linear density 3 kg/m3\,\mathrm{kg}/\mathrm{m} and hangs vertically from a platform. Set up, but do not yet evaluate, the work required to pull the entire cable onto the platform. Choose a coordinate, describe the representative piece, state its weight and its lifting distance, and check the units of your integrand. Then explain why multiplying the total cable weight by 12 m12\,\mathrm{m} would overestimate the work. The next lesson uses the same representative-piece discipline to locate centers, moments, and probability-weighted averages.

Knowledge Map

Where this lesson fits

Prerequisites

Unit 3 - Accumulation in Geometry, Physics, and ModelsArc Length and Surface Area

Next lessons

Unit 3 - Accumulation in Geometry, Physics, and ModelsMoments, Centers, and Probability