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Motion graphs and their interpretation

Learning objectives

  • Outcome

    Determine average velocity from the slope of a segment of an x(t)x(t) graph and instantaneous velocity from the slope of the tangent.

  • Outcome

    Find acceleration from the slope of a v(t)v(t) graph and displacement from the area between the graph and the time axis, taking the sign of the area into account.

  • Outcome

    Sketch matching x(t)x(t) and v(t)v(t) graphs for a described motion: rest, constant velocity, uniformly accelerated motion.

  • Outcome

    Distinguish displacement from distance travelled by summing signed areas under a v(t)v(t) graph and comparing average velocity with average speed.

Understand the idea

Motion graphs: reading and drawing them

Text

A motion graph plots a kinematic quantity against time, and the physics is carried by the shape of the curve, not by a picture of the path. On a position–time graph x(t)x(t), the slope of a segment between two instants gives the average velocity vavg=ΔxΔtv_{\mathrm{avg}}=\frac{\Delta x}{\Delta t}, while the slope of the tangent at one instant gives the instantaneous velocity. A horizontal line therefore means rest, a slanted straight line means motion at constant velocity, and a curve means motion with changing velocity, that is, with acceleration. On a velocity–time graph v(t)v(t), the slope gives acceleration a=ΔvΔta=\frac{\Delta v}{\Delta t}, and the area between the graph and the time axis gives displacement Δx=∑v Δt\Delta x=\sum v\,\Delta t. Areas above the axis count as positive and areas below it as negative, so after a reversal they partly cancel and the displacement is smaller than the distance travelled. Always read the axis labels and units first: confusing x(t)x(t) with v(t)v(t) is the most common error in graph reading.

Worked examples

Direct

Problem

A pedestrian walks along a straight street. The x(t)x(t) graph is a broken line through the points (0 s,0 m)(0\ \text{s}, 0\ \text{m}), (4 s,12 m)(4\ \text{s}, 12\ \text{m}), (10 s,12 m)(10\ \text{s}, 12\ \text{m}), (14 s,0 m)(14\ \text{s}, 0\ \text{m}). Find the average velocity on each of the three intervals and describe the pedestrian's motion.

Solution

On each interval the slope equals ΔxΔt\frac{\Delta x}{\Delta t}.

  • 00–4 s4\ \text{s}: Δx=12 m\Delta x = 12\ \text{m}, Δt=4 s\Delta t = 4\ \text{s}, so vavg=+3 m/sv_{\mathrm{avg}} = +3\ \text{m/s} — moving forward.
  • 44–10 s10\ \text{s}: Δx=0\Delta x = 0, so vavg=0v_{\mathrm{avg}} = 0 — the pedestrian is standing still (horizontal line).
  • 1010–14 s14\ \text{s}: Δx=−12 m\Delta x = -12\ \text{m}, Δt=4 s\Delta t = 4\ \text{s}, so vavg=−3 m/sv_{\mathrm{avg}} = -3\ \text{m/s} — walking back towards the start; the minus sign marks the opposite direction.

Application

Problem

A car's velocity–time graph v(t)v(t) is a broken line: during the first 4 s4\ \text{s} the velocity rises uniformly from 00 to 8 m/s8\ \text{m/s}, for the next 4 s4\ \text{s} it stays at 8 m/s8\ \text{m/s}, and during the last 4 s4\ \text{s} it falls uniformly to 00. Find the acceleration in each stage and the total displacement.

Solution

Acceleration is the slope of the v(t)v(t) graph:

a=ΔvΔta = \frac{\Delta v}{\Delta t}

  • 00–4 s4\ \text{s}: a=8−04=2 m/s2a = \frac{8-0}{4} = 2\ \text{m/s}^2.
  • 44–8 s8\ \text{s}: a=0a = 0, the velocity is constant.
  • 88–12 s12\ \text{s}: a=0−84=−2 m/s2a = \frac{0-8}{4} = -2\ \text{m/s}^2, the car is slowing down.

Displacement is the area under the graph. The first and third stages are triangles, the second is a rectangle:

Δx=12⋅4⋅8+8⋅4+12⋅4⋅8=16+32+16=64 m.\Delta x = \tfrac{1}{2}\cdot 4\cdot 8 + 8\cdot 4 + \tfrac{1}{2}\cdot 4\cdot 8 = 16 + 32 + 16 = 64\ \text{m}.

Check on the whole trip: vavg=6412≈5.3 m/sv_{\mathrm{avg}} = \frac{64}{12}\approx 5.3\ \text{m/s}, which lies between 00 and 8 m/s8\ \text{m/s} — a plausible result.

Transfer

Problem

A trolley moves along a straight rail. Its v(t)v(t) graph is: +6 m/s+6\ \text{m/s} from t=0t=0 to 3 s3\ \text{s}, then −2 m/s-2\ \text{m/s} from 3 s3\ \text{s} to 5 s5\ \text{s}, then +1 m/s+1\ \text{m/s} from 5 s5\ \text{s} to 9 s9\ \text{s}. (a) Find the displacement and the distance travelled. (b) Find the average velocity and the average speed over the whole 9 s9\ \text{s}. (c) Explain why these two averages differ.

Solution

(a) Displacement is the sum of signed areas:

Δx=6⋅3+(−2)⋅2+1⋅4=18−4+4=18 m.\Delta x = 6\cdot 3 + (-2)\cdot 2 + 1\cdot 4 = 18 - 4 + 4 = 18\ \text{m}.

Distance travelled adds the magnitudes of the areas:

s=18+4+4=26 m.s = 18 + 4 + 4 = 26\ \text{m}.

(b) Average velocity: vavg=ΔxΔt=189=2 m/sv_{\mathrm{avg}} = \frac{\Delta x}{\Delta t} = \frac{18}{9} = 2\ \text{m/s}. Average speed: sΔt=269≈2.9 m/s\frac{s}{\Delta t} = \frac{26}{9}\approx 2.9\ \text{m/s}.

(c) Between 3 s3\ \text{s} and 5 s5\ \text{s} the trolley moved backwards, so that 4 m4\ \text{m} of path counted towards the distance but was subtracted from the displacement. That is why the average speed exceeds the magnitude of the average velocity; they would be equal only for motion without a reversal.

Practice

Text

A 30–40 minute self-study plan, carried out entirely in a simulation.

  1. Open a motion simulation such as PhET The Moving Man, or any other tool that plots x(t)x(t) and v(t)v(t) graphs. Keep the motion one-dimensional.
  2. Generate three motions and record them: (a) the body is at rest; (b) motion at constant velocity +2 m/s+2\ \text{m/s}; (c) uniformly accelerated motion from rest. For each one, pause and examine both graphs.
  3. For case (b), pick two points on the x(t)x(t) graph, compute the slope by hand as ΔxΔt\frac{\Delta x}{\Delta t} and compare it with the velocity readout. For case (c), take two instants, compute ΔvΔt\frac{\Delta v}{\Delta t} and compare it with the acceleration readout.
  4. Then hide the v(t)v(t) graph and sketch from the x(t)x(t) graph what the velocity graph must look like; afterwards reveal it and correct your sketch.

Safety. Do all measurements in the simulation. Do not time your own motion on roads, stairs or anywhere near traffic.

Visual reference

Purpose

Show that one and the same motion is encoded in two ways: the slope of the x(t)x(t) graph equals the value on the v(t)v(t) graph, and the area under v(t)v(t) equals the change in xx.

Representation

A sketch of two graphs stacked vertically and sharing one horizontal time axis. On top, x(t)x(t) is a slanted straight line with a marked right triangle and the label ΔxΔt\frac{\Delta x}{\Delta t} along its hypotenuse. Below, v(t)v(t) is a horizontal straight line, with the region between it and the time axis shaded and labelled Δx=v Δt\Delta x = v\,\Delta t. A dashed vertical line links the two graphs at one and the same instant.

Real-world examples

100 m sprint: split times on a position–time graph

Scenario

In a school 100 m race the stopwatch is read at five marks. The data are: x=0x=0 m at t=0t=0 s, x=12x=12 m at t=2.0t=2.0 s, x=26x=26 m at t=4.0t=4.0 s, x=42x=42 m at t=6.0t=6.0 s, x=60x=60 m at t=8.0t=8.0 s, x=78x=78 m at t=10.0t=10.0 s and x=100x=100 m at t=12.5t=12.5 s. Plotting xx vertically against tt horizontally gives a curve that is shallow at first and then steepens: the runner covers 1212 m in the first two seconds, 1818 m in 2.02.0 s in the middle of the race, and 2222 m in the last 2.52.5 s.

Connection

The central reading rule is used here: the slope of a segment equals Δx/Δt\Delta x/\Delta t. For the first 2.02.0 s it is 12/2.0=6.012/2.0 = 6.0 m/s, for the middle part 18/2.0=9.018/2.0 = 9.0 m/s, for the last one 22/2.5=8.822/2.5 = 8.8 m/s. The straight line joining (0;0)(0;0) and (12.5;100)(12.5;100) has slope 100/12.5=8.0100/12.5 = 8.0 m/s — the average speed of the whole race — while the steepest part of the curve marks the moment of greatest speed.

The area under a bus speed–time graph

Scenario

A city bus pulls away from a stop on a straight avenue: its speed rises from zero to 2020 m/s in 8.08.0 s, holds at 2020 m/s for 6060 s, then drops to zero in 5.05.0 s at the traffic light. The on-board logger plots speed against time.

Connection

The distance travelled equals the area between the speed line and the time axis: 12⋅20⋅8.0+20⋅60+12⋅20⋅5.0=80+1200+50=1330 m≈1.3 km.\tfrac{1}{2}\cdot 20\cdot 8.0 + 20\cdot 60 + \tfrac{1}{2}\cdot 20\cdot 5.0 = 80 + 1200 + 50 = 1330\ \text{m} \approx 1.3\ \text{km}. The slopes of the rising and falling pieces of the same graph give the accelerations 20/8.0=2.5 m/s220/8.0 = 2.5\ \text{m/s}^2 and −20/5.0=−4.0 m/s2-20/5.0 = -4.0\ \text{m/s}^2.

A thunderstorm front on a radar screen

Scenario

Weather radar tracks the leading edge of a storm line moving east towards a town. The fixes are: 3030 km west of the town at 15:0015{:}00, 1818 km west at 16:0016{:}00, 66 km west at 17:0017{:}00, and the town itself (00 km) at 19:0019{:}00. Taking east as positive, x=−30x=-30 km at 15:0015{:}00, x=−18x=-18 km at 16:0016{:}00, x=−6x=-6 km at 17:0017{:}00 and x=0x=0 km at 19:0019{:}00.

Connection

The first three points lie on a single straight line, and its slope gives the front's velocity: 2424 km in 2.02.0 h, that is 1212 km/h ≈3.3\approx 3.3 m/s eastward. The last segment runs from x=−6x=-6 km to x=0x=0 km in 2.02.0 h, with a slope of only 33 km/h. The kink in the graph at 17:0017{:}00 is direct evidence that the motion stopped being uniform and the front slowed down, even though nobody measured its speed directly.