Multivariable-Calculus Β· Unit 6 Β· Video 4 Β· Interactive Practice
Equal Areas in Equal Times: Kepler's Second Law and the Length of r Γ v \mathbf{r} \times \mathbf{v} r Γ v
I Key Formulas
Key Insight: Equal areas in equal times β
β βΊ β
β \iff βΊ β£ r Γ v β£ |\mathbf{r} \times \mathbf{v}| β£ r Γ v β£ is the same at every point of the orbit, even though r \mathbf{r} r and v \mathbf{v} v themselves keep changing.
II Visualization 1 β Equal Times, Equal Areas
The sunβplanet line sweeps area at a constant rate, so wedges between equally spaced times all have equal area.
III Visualization 2 β Wedge, Triangle, Half a Parallelogram
As Ξ t \Delta t Ξ t shrinks, the swept wedge approaches the triangle with sides r \mathbf{r} r and Ξ r \Delta\mathbf{r} Ξ r , of area 1 2 β£ r Γ Ξ r β£ \tfrac{1}{2}|\mathbf{r} \times \Delta\mathbf{r}| 2 1 β β£ r Γ Ξ r β£ .
βΆ shrink Ξt
Ξt
1.00
Start
near the sun (t = 11.5)
far from the sun (t = 5.5)
IV Visualization 3 β Short β£ r β£ |\mathbf{r}| β£ r β£ , Fast Sideways
Around the orbit β£ r β£ |\mathbf{r}| β£ r β£ and the perpendicular part v β₯ v_\perp v β₯ β trade off, while their product β£ r Γ v β£ |\mathbf{r} \times \mathbf{v}| β£ r Γ v β£ never changes.
π‘ This is the area half of Kepler's second law, and it fixes only the length of r Γ v \mathbf{r} \times \mathbf{v} r Γ v . The other half, motion in a plane, fixes its direction.
V Quiz Questions
Problem 1 Β· The Area Rate
Given: at some instant a planet has position r = β¨ 3 , 0 , 0 β© \mathbf{r} = \langle 3, 0, 0\rangle r = β¨ 3 , 0 , 0 β© and velocity v = β¨ 1 , 2 , 0 β© \mathbf{v} = \langle 1, 2, 0\rangle v = β¨ 1 , 2 , 0 β© , with the sun at the origin β find the rate d A d t \dfrac{dA}{dt} d t d A β at which the sunβplanet line sweeps out area.
a d A d t = 6 \dfrac{dA}{dt} = 6 d t d A β = 6
b d A d t = 3 5 2 \dfrac{dA}{dt} = \tfrac{3\sqrt{5}}{2} d t d A β = 2 3 5 β β
c d A d t = 3 \dfrac{dA}{dt} = 3 d t d A β = 3
d d A d t = 3 2 \dfrac{dA}{dt} = \tfrac{3}{2} d t d A β = 2 3 β
β
Correct! r Γ v = β¨ 0 , 0 , 6 β© \mathbf{r} \times \mathbf{v} = \langle 0, 0, 6\rangle r Γ v = β¨ 0 , 0 , 6 β© , and the swept region is the triangle, half the parallelogram:
1 2 β
6 = 3 \tfrac{1}{2} \cdot 6 = 3 2 1 β β
6 = 3 .
β The factor of 1 2 \tfrac{1}{2} 2 1 β got lost. β£ r Γ v β£ = 6 |\mathbf{r} \times \mathbf{v}| = 6 β£ r Γ v β£ = 6 is the parallelogram rate; the swept wedge is only the triangle, half of it.
β That is 1 2 β£ r β£ β β£ v β£ \tfrac{1}{2}|\mathbf{r}|\,|\mathbf{v}| 2 1 β β£ r β£ β£ v β£ with no sin β‘ ΞΈ \sin\theta sin ΞΈ . r \mathbf{r} r and
v \mathbf{v} v are not perpendicular here, so only the perpendicular part of
v \mathbf{v} v sweeps area.
β That uses the dot product. 1 2 β r β
v = 3 2 \tfrac{1}{2}\,\mathbf{r} \cdot \mathbf{v} = \tfrac{3}{2} 2 1 β r β
v = 2 3 β measures the motion
along r \mathbf{r} r , which sweeps no area; the area comes from the cross product.
Show solution
Compute the cross product:
r Γ v = β£ i j k 3 0 0 1 2 0 β£ = β¨ 0 β
0 β 0 β
2 , Β 0 β
1 β 3 β
0 , Β 3 β
2 β 0 β
1 β© = β¨ 0 , 0 , 6 β© \mathbf{r} \times \mathbf{v} = \begin{vmatrix} \mathbf{i} & \mathbf{j} & \mathbf{k} \\ 3 & 0 & 0 \\ 1 & 2 & 0 \end{vmatrix} = \langle 0\cdot 0 - 0\cdot 2,\ 0\cdot 1 - 3\cdot 0,\ 3\cdot 2 - 0\cdot 1\rangle = \langle 0, 0, 6\rangle r Γ v = β i 3 1 β j 0 2 β k 0 0 β β = β¨ 0 β
0 β 0 β
2 , Β 0 β
1 β 3 β
0 , Β 3 β
2 β 0 β
1 β© = β¨ 0 , 0 , 6 β©
Its length is 6 6 6 , the area rate of the parallelogram spanned by r \mathbf{r} r and v \mathbf{v} v . The swept triangle is half of that:
d A d t = 1 2 β β£ r Γ v β£ = 1 2 β
6 = 3 \frac{dA}{dt} = \tfrac{1}{2}\,|\mathbf{r} \times \mathbf{v}| = \tfrac{1}{2} \cdot 6 = 3 d t d A β = 2 1 β β£ r Γ v β£ = 2 1 β β
6 = 3
Problem 2 Β· Perihelion to Aphelion
Given: a comet passes closest to the sun at distance 1 1 1 AU with speed 40 40 40 km/s; at its farthest point it is 5 5 5 AU away. At both points its velocity is perpendicular to r \mathbf{r} r β find its speed at the farthest point.
a 1.6 1.6 1.6 km/s
b 40 40 40 km/s
c 200 200 200 km/s
d 8 8 8 km/s
β
Correct! β£ r β£ β v β₯ |\mathbf{r}|\,v_\perp β£ r β£ v β₯ β is fixed:
1 β
40 = 5 β
v 1 \cdot 40 = 5 \cdot v 1 β
40 = 5 β
v , so
v = 8 v = 8 v = 8 km/s β five times as far, one fifth as fast.
β That divides by 5 2 5^2 5 2 . The conserved quantity is
β£ r β£ β v β₯ |\mathbf{r}|\,v_\perp β£ r β£ v β₯ β , linear in
β£ r β£ |\mathbf{r}| β£ r β£ : five times farther means one fifth of the perpendicular speed, not one twenty-fifth.
β The area rate is constant, not the speed. Far from the sun the wedge is long and thin, so the planet covers less orbit in the same time.
β Backwards. Keeping
β£ r β£ β v β₯ |\mathbf{r}|\,v_\perp β£ r β£ v β₯ β fixed while
β£ r β£ |\mathbf{r}| β£ r β£ grows fivefold forces
v β₯ v_\perp v β₯ β to shrink fivefold.
Show solution
Equal areas in equal times means β£ r Γ v β£ = β£ r β£ β β£ v β£ sin β‘ ΞΈ |\mathbf{r} \times \mathbf{v}| = |\mathbf{r}|\,|\mathbf{v}|\sin\theta β£ r Γ v β£ = β£ r β£ β£ v β£ sin ΞΈ is the same everywhere. At both points ΞΈ = 90 Β° \theta = 90\degree ΞΈ = 90Β° , so sin β‘ ΞΈ = 1 \sin\theta = 1 sin ΞΈ = 1 :
β£ r 1 β£ β β£ v 1 β£ = β£ r 2 β£ β β£ v 2 β£ βΉ 1 β
40 = 5 β β£ v 2 β£ |\mathbf{r}_1|\,|\mathbf{v}_1| = |\mathbf{r}_2|\,|\mathbf{v}_2| \quad\Longrightarrow\quad 1 \cdot 40 = 5\,|\mathbf{v}_2| β£ r 1 β β£ β£ v 1 β β£ = β£ r 2 β β£ β£ v 2 β β£ βΉ 1 β
40 = 5 β£ v 2 β β£
β£ v 2 β£ = 40 5 = 8 Β km/s |\mathbf{v}_2| = \frac{40}{5} = 8 \text{ km/s} β£ v 2 β β£ = 5 40 β = 8 Β km/s
(Mixing AU with km/s is harmless: the distance units cancel in the ratio 1 / 5 1/5 1/5 .)
Problem 3 Β· From Two Positions to the Rate
Given: a planet is at r = β¨ 2 , 0 β© \mathbf{r} = \langle 2, 0\rangle r = β¨ 2 , 0 β© and, a short time Ξ t = 0.1 \Delta t = 0.1 Ξ t = 0.1 later, at β¨ 1.9 , Β 0.3 β© \langle 1.9,\ 0.3\rangle β¨ 1.9 , Β 0.3 β© (sun at the origin) β estimate the area swept in that time, then the area rate d A d t \dfrac{dA}{dt} d t d A β .
Area swept in Ξ t = 0.1 \Delta t = 0.1 Ξ t = 0.1
a Ξ A β 0.6 \Delta A \approx 0.6 Ξ A β 0.6
b Ξ A β 0.3 \Delta A \approx 0.3 Ξ A β 0.3
c Ξ A β 10 10 β 0.32 \Delta A \approx \tfrac{\sqrt{10}}{10} \approx 0.32 Ξ A β 10 10 β β β 0.32
d Ξ A β 0.1 \Delta A \approx 0.1 Ξ A β 0.1
Area rate
a d A d t β 0.03 \dfrac{dA}{dt} \approx 0.03 d t d A β β 0.03
b d A d t β 6 \dfrac{dA}{dt} \approx 6 d t d A β β 6
c d A d t β 30 \dfrac{dA}{dt} \approx 30 d t d A β β 30
d d A d t β 3 \dfrac{dA}{dt} \approx 3 d t d A β β 3
β
Correct! Ξ r = β¨ β 0.1 , 0.3 β© \Delta\mathbf{r} = \langle -0.1, 0.3\rangle Ξ r = β¨ β 0.1 , 0.3 β© , the triangle has area
1 2 β£ r Γ Ξ r β£ = 0.3 \tfrac{1}{2}|\mathbf{r} \times \Delta\mathbf{r}| = 0.3 2 1 β β£ r Γ Ξ r β£ = 0.3 , and dividing by
Ξ t = 0.1 \Delta t = 0.1 Ξ t = 0.1 gives a rate of
3 3 3 .
β That is the whole parallelogram. β£ r Γ Ξ r β£ = 0.6 |\mathbf{r} \times \Delta\mathbf{r}| = 0.6 β£ r Γ Ξ r β£ = 0.6 ; the swept wedge is close to the triangle, half of it.
β That is 1 2 β£ r β£ β β£ Ξ r β£ \tfrac{1}{2}|\mathbf{r}|\,|\Delta\mathbf{r}| 2 1 β β£ r β£ β£Ξ r β£ . It ignores the angle between
r \mathbf{r} r and
Ξ r \Delta\mathbf{r} Ξ r ; the cross product keeps only the part of
Ξ r \Delta\mathbf{r} Ξ r perpendicular to
r \mathbf{r} r .
β That comes from the dot product. 1 2 β£ r β
Ξ r β£ = 0.1 \tfrac{1}{2}|\mathbf{r} \cdot \Delta\mathbf{r}| = 0.1 2 1 β β£ r β
Ξ r β£ = 0.1 measures motion along
r \mathbf{r} r ; area needs
r Γ Ξ r \mathbf{r} \times \Delta\mathbf{r} r Γ Ξ r .
β Check the swept area. Find
Ξ r \Delta\mathbf{r} Ξ r first, then take half the length of
r Γ Ξ r \mathbf{r} \times \Delta\mathbf{r} r Γ Ξ r .
β Multiplied instead of divided. Ξ A β d A d t β Ξ t \Delta A \approx \tfrac{dA}{dt}\,\Delta t Ξ A β d t d A β Ξ t , so the rate is
Ξ A / Ξ t = 0.3 / 0.1 \Delta A / \Delta t = 0.3 / 0.1 Ξ A /Ξ t = 0.3/0.1 .
β That is β£ r Γ v β£ |\mathbf{r} \times \mathbf{v}| β£ r Γ v β£ , twice the area rate. The rate is
1 2 β£ r Γ v β£ = Ξ A / Ξ t = 0.3 / 0.1 \tfrac{1}{2}|\mathbf{r} \times \mathbf{v}| = \Delta A / \Delta t = 0.3 / 0.1 2 1 β β£ r Γ v β£ = Ξ A /Ξ t = 0.3/0.1 .
β That divides by Ξ t \Delta t Ξ t twice. 0.3 / 0.1 2 = 30 0.3 / 0.1^2 = 30 0.3/0. 1 2 = 30 ; the rate is the swept area over the elapsed time once,
Ξ A / Ξ t = 0.3 / 0.1 \Delta A / \Delta t = 0.3 / 0.1 Ξ A /Ξ t = 0.3/0.1 .
β Check the rate. Divide the swept area by the elapsed time:
Ξ A / Ξ t \Delta A / \Delta t Ξ A /Ξ t .
Show solution
Step 1: the change in position is
Ξ r = β¨ 1.9 β 2 , Β 0.3 β 0 β© = β¨ β 0.1 , Β 0.3 β© \Delta\mathbf{r} = \langle 1.9 - 2,\ 0.3 - 0\rangle = \langle -0.1,\ 0.3\rangle Ξ r = β¨ 1.9 β 2 , Β 0.3 β 0 β© = β¨ β 0.1 , Β 0.3 β©
Step 2: for plane vectors the cross product has only a k \mathbf{k} k component, x 1 y 2 β y 1 x 2 x_1 y_2 - y_1 x_2 x 1 β y 2 β β y 1 β x 2 β :
r Γ Ξ r = ( 2 β
0.3 β 0 β
( β 0.1 ) ) β k = 0.6 β k , Ξ A β 1 2 β β£ r Γ Ξ r β£ = 0.3 \mathbf{r} \times \Delta\mathbf{r} = \big(2 \cdot 0.3 - 0 \cdot (-0.1)\big)\,\mathbf{k} = 0.6\,\mathbf{k}, \qquad \Delta A \approx \tfrac{1}{2}\,|\mathbf{r} \times \Delta\mathbf{r}| = 0.3 r Γ Ξ r = ( 2 β
0.3 β 0 β
( β 0.1 ) ) k = 0.6 k , Ξ A β 2 1 β β£ r Γ Ξ r β£ = 0.3
Step 3: divide by the elapsed time:
d A d t β Ξ A Ξ t = 0.3 0.1 = 3 \frac{dA}{dt} \approx \frac{\Delta A}{\Delta t} = \frac{0.3}{0.1} = 3 d t d A β β Ξ t Ξ A β = 0.1 0.3 β = 3
Equivalently, v β Ξ r / Ξ t = β¨ β 1 , 3 β© \mathbf{v} \approx \Delta\mathbf{r}/\Delta t = \langle -1, 3\rangle v β Ξ r /Ξ t = β¨ β 1 , 3 β© and 1 2 β£ r Γ v β£ = 1 2 β β£ 2 β
3 β 0 β
( β 1 ) β£ = 3 \tfrac{1}{2}|\mathbf{r} \times \mathbf{v}| = \tfrac{1}{2}\,|2 \cdot 3 - 0 \cdot (-1)| = 3 2 1 β β£ r Γ v β£ = 2 1 β β£2 β
3 β 0 β
( β 1 ) β£ = 3 .
Problem 4 Β· When v Is Not Perpendicular
Given: at one point of its orbit a planet is β£ r β£ = 6 |\mathbf{r}| = 6 β£ r β£ = 6 from the sun, moving with speed β£ v β£ = 2 |\mathbf{v}| = 2 β£ v β£ = 2 at an angle ΞΈ = 30 Β° \theta = 30\degree ΞΈ = 30Β° to r \mathbf{r} r . At its closest point, β£ r β£ = 1.5 |\mathbf{r}| = 1.5 β£ r β£ = 1.5 and v β₯ r \mathbf{v} \perp \mathbf{r} v β₯ r β find its speed there.
a β£ v β£ = 4 |\mathbf{v}| = 4 β£ v β£ = 4
b β£ v β£ = 8 |\mathbf{v}| = 8 β£ v β£ = 8
c β£ v β£ = 4 3 |\mathbf{v}| = 4\sqrt{3} β£ v β£ = 4 3 β
d β£ v β£ = 1 2 |\mathbf{v}| = \tfrac{1}{2} β£ v β£ = 2 1 β
β
Correct! β£ r Γ v β£ = 6 β
2 β
sin β‘ 30 Β° = 6 |\mathbf{r} \times \mathbf{v}| = 6 \cdot 2 \cdot \sin 30\degree = 6 β£ r Γ v β£ = 6 β
2 β
sin 30Β° = 6 at the first point, so at the closest point
1.5 β β£ v β£ = 6 1.5\,|\mathbf{v}| = 6 1.5 β£ v β£ = 6 and
β£ v β£ = 4 |\mathbf{v}| = 4 β£ v β£ = 4 .
β The sin β‘ ΞΈ \sin\theta sin ΞΈ is missing. Only the perpendicular part of the velocity,
2 sin β‘ 30 Β° = 1 2 \sin 30\degree = 1 2 sin 30Β° = 1 , counts toward
β£ r Γ v β£ |\mathbf{r} \times \mathbf{v}| β£ r Γ v β£ .
β That uses cos β‘ ΞΈ \cos\theta cos ΞΈ . β£ v β£ cos β‘ ΞΈ |\mathbf{v}|\cos\theta β£ v β£ cos ΞΈ is the part of
v \mathbf{v} v along
r \mathbf{r} r ; the cross product needs the perpendicular part,
β£ v β£ sin β‘ ΞΈ |\mathbf{v}|\sin\theta β£ v β£ sin ΞΈ .
β Speed is not proportional to distance. The product
β£ r β£ β v β₯ |\mathbf{r}|\,v_\perp β£ r β£ v β₯ β is constant, so a closer planet moves sideways
faster .
Show solution
At the first point:
β£ r Γ v β£ = β£ r β£ β β£ v β£ sin β‘ ΞΈ = 6 β
2 β
sin β‘ 30 Β° = 6 β
2 β
1 2 = 6 |\mathbf{r} \times \mathbf{v}| = |\mathbf{r}|\,|\mathbf{v}|\sin\theta = 6 \cdot 2 \cdot \sin 30\degree = 6 \cdot 2 \cdot \tfrac{1}{2} = 6 β£ r Γ v β£ = β£ r β£ β£ v β£ sin ΞΈ = 6 β
2 β
sin 30Β° = 6 β
2 β
2 1 β = 6
By Kepler's second law this length is the same at the closest point, where ΞΈ = 90 Β° \theta = 90\degree ΞΈ = 90Β° :
1.5 β
β£ v β£ β
1 = 6 βΉ β£ v β£ = 4 1.5 \cdot |\mathbf{v}| \cdot 1 = 6 \quad\Longrightarrow\quad |\mathbf{v}| = 4 1.5 β
β£ v β£ β
1 = 6 βΉ β£ v β£ = 4
Note that v β₯ v_\perp v β₯ β went from 1 1 1 to 4 4 4 as β£ r β£ |\mathbf{r}| β£ r β£ went from 6 6 6 to 1.5 1.5 1.5 : a factor of 4 4 4 each way.
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