# 6.4: Motion Under a Central Force

- Last updated

- Save as PDF

- Page ID
- 30743

- Contributed by William F. Trench
- Andrew G. Cowles Distinguished Professor Emeritus (Mathamatics) at Trinity University

We’ll now study the motion of a object moving under the influence of a *central force*; that is, a force whose magnitude at any point \(P\) other than the origin depends only on the distance from \(P\) to the origin, and whose direction at \(P\) is parallel to the line connecting \(P\) and the origin, as indicated in Figure \(\PageIndex{1}\) for the case where the direction of the force at every point is toward the origin. Gravitational forces are central forces; for example, as mentioned in Section 4.3, if we assume that Earth is a perfect sphere with constant mass density then Newton’s law of gravitation asserts that the force exerted on an object by Earth’s gravitational field is proportional to the mass of the object and inversely proportional to the square of its distance from the center of Earth, which we take to be the origin.

If the initial position and velocity vectors of an object moving under a central force are parallel, then the subsequent motion is along the line from the origin to the initial position. Here we’ll assume that the initial position and velocity vectors are not parallel; in this case the subsequent motion is in the plane determined by them. For convenience we take this to be the \(xy\)-plane. We’ll consider the problem of determining the curve traversed by the object. We call this curve the *orbit*.

We can represent a central force in terms of polar coordinates

\[x=r\cos\theta,\quad y=r\sin\theta \nonumber\]

as

\[{\bf F}(r,\theta)=f(r)(\cos\theta\,{\bf i}+\sin\theta\,{\bf j}). \nonumber\]

We assume that \(f\) is continuous for all \(r>0\). The magnitude of \({\bf F}\) at \((x,y)=(r\cos\theta,r\sin\theta)\) is \(|f(r)|\), so it depends only on the distance \(r\) from the point to the origin the direction of \({\bf F}\) is from the point to the origin if \(f(r)<0\), or from the origin to the point if \(f(r)>0\). We’ll show that the orbit of an object with mass \(m\) moving under this force is given by

\[r(\theta)={1\over u(\theta)}, \nonumber\]

where \(u\) is solution of the differential equation

\[\label{eq:6.4.1} {d^2u\over d\theta^2}+u=-{1\over mh^2u^2}f(1/u),\]

and \(h\) is a constant defined below.

Newton’s second law of motion (\({\bf F}=m{\bf a}\)) says that the polar coordinates \(r=r(t)\) and \(\theta=\theta(t)\) of the particle satisfy the vector differential equation

\[\label{eq:6.4.2} m(r\cos\theta\,{\bf i}+r\sin\theta\,{\bf j})''= f(r)(\cos\theta\,{\bf i}+\sin\theta\,{\bf j}).\]

To deal with this equation we introduce the unit vectors

\[{\bf e}_1=\cos\theta\,{\bf i}+\sin\theta\,{\bf j} \quad \text{and} \quad {\bf e}_2=-\sin\theta\,{\bf i}+\cos\theta\,{\bf j}. \nonumber\]

Note that \({\bf e}_1\) points in the direction of increasing \(r\) and \({\bf e}_2\) points in the direction of increasing \(\theta\) (Figure \(\PageIndex{2}\)); moreover,

\[\label{eq:6.4.3} {d{\bf e}_1\over d\theta}={\bf e}_2,\quad {d{\bf e}_2\over d\theta}=-{\bf e}_1,\]

and

\[{\bf e}_1\cdot{\bf e}_2=\cos\theta(-\sin\theta)+\sin\theta\cos\theta=0, \nonumber\]

so \({\bf e}_1\) and \({\bf e}_2\) are perpendicular. Recalling that the single prime \((')\) stands for differentiation with respect to \(t\), we see from Equation \ref{eq:6.4.3} and the chain rule that

\[\label{eq:6.4.4} {\bf e}_1'=\theta'{\bf e}_2\quad \text{and} \quad {\bf e}_2'=-\theta'{\bf e}_1.\]

Now we can write Equation \ref{eq:6.4.2} as

\[\label{eq:6.4.5} m(r{\bf e}_1)''=f(r){\bf e}_1.\]

But

\[(r{\bf e}_1)'=r'{\bf e}_1+r{\bf e}_1'=r'{\bf e}_1+r\theta'{\bf e}_2 \nonumber\]

(from Equation \ref{eq:6.4.4}), and

\[\begin{aligned} (r{\bf e}_1)''&=(r'{\bf e}_1+r\theta'{\bf e}_2)'\\ &=r''{\bf e}_1+r'{\bf e}_1'+(r\theta''+r'\theta'){\bf e}_2 +r\theta'{\bf e}_2'\\ &=r''{\bf e}_1+r'\theta'{\bf e}_2+(r\theta''+r'\theta'){\bf e}_2 -r(\theta')^2{\bf e}_1 \quad \mbox{from \eqref{eq:6.4.4}}\\ &=\left(r''-r(\theta')^2\right){\bf e}_1+(r\theta''+2r'\theta'){\bf e}_2.\end{aligned}\]

Substituting this into Equation \ref{eq:6.4.5} yields

\[m\left(r''-r(\theta')^2\right){\bf e}_1+m(r\theta''+2r'\theta'){\bf e}_2=f(r){\bf e}_1. \nonumber\]

By equating the coefficients of \({\bf e}_1\) and \({\bf e}_2\) on the two sides of this equation we see that

\[\label{eq:6.4.6} m\left(r''-r(\theta')^2\right)=f(r)\]

and

\[r\theta''+2r'\theta'=0. \nonumber\]

Multiplying the last equation by \(r\) yields

\[r^2\theta''+2rr'\theta'=(r^2\theta')'=0, \nonumber\]

so

\[\label{eq:6.4.7} r^2\theta'=h,\]

where \(h\) is a constant that we can write in terms of the initial conditions as

\[h=r^2(0)\theta'(0). \nonumber\]

Since the initial position and velocity vectors are

\[r(0){\bf e}_1(0)\quad \text{and} \quad r'(0){\bf e}_1(0)+r(0)\theta'(0){\bf e}_2(0), \nonumber\]

our assumption that these two vectors are not parallel implies that \(\theta'(0)\ne0\), so \(h\ne0\).

Now let \(u=1/r\). Then \(u^2=\theta'/h\) (from Equation \ref{eq:6.4.7}) and

\[r'=-{u'\over u^2}=-h\left(u'\over \theta'\right),\nonumber\]

which implies that

\[\label{eq:6.4.8} r'=-h{du\over d\theta},\]

since

\[{u'\over\theta'}={du\over dt}\left/{d\theta\over dt}\right.= {du\over d\theta}.\nonumber\]

Differentiating Equation \ref{eq:6.4.8} with respect to \(t\) yields

\[r''=-h{d\over dt}\left({du\over d\theta}\right) =-h{d^2u\over d\theta^2}\theta',\nonumber\]

which implies that

\[r''=-h^2u^2{d^2u\over d\theta^2} \quad \text{since} \quad \theta'=hu^2.\nonumber\]

Substituting from these equalities into Equation \ref{eq:6.4.6} and recalling that \(r=1/u\) yields

\[-m\left(h^2u^2{d^2u\over d\theta^2}+{1\over u}h^2u^4\right) =f(1/u),\nonumber\]

and dividing through by \(-mh^2u^2\) yields Equation \ref{eq:6.4.1}.

Equation \ref{eq:6.4.7} has the following geometrical interpretation, which is known as *Kepler’s Second Law*.

Theorem \(\PageIndex{1}\) kepler's second law

The position vector of an object moving under a central force sweeps out equal areas in equal times;\(\) more precisely\(,\) if \(\theta(t_1)\le\theta(t_2)\) then the *signed *area of the sector (Figure \(\PageIndex{3}\)):

\[(x,y)=(r\cos\theta,r\sin\theta)\; :\; 0\le r\le r(\theta),\; \theta(t_1)\le\theta(t_2) \nonumber\]

is given by

\[A={h(t_2-t_1)\over2},\nonumber\]

where \(h=r^2\theta',\) which we have shown to be constant.

**Proof**-
Recall from calculus that the area of the shaded sector in Figure \(\PageIndex{3}\) is

\[A={1\over2}\int_{\theta(t_1)}^{\theta(t_2)} r^2(\theta)\,d\theta,\nonumber\]

where \(r=r(\theta)\) is the polar representation of the orbit. Making the change of variable \(\theta=\theta(t)\) yields

\[\label{eq:6.4.9} A={1\over2}\int_{t_1}^{t_2} r^2(\theta(t))\theta'(t)\,dt.\]

However, Equations \ref{eq:6.4.7} and \ref{eq:6.4.9} imply that

\[A={1\over2}\int_{t_1}^{t_2} h\,dt={h(t_2-t_1)\over2},\nonumber\]

which completes the proof.

## Motion Under an Inverse Square Law Force

In the special case where \(f(r)=-mk/r^2=-mku^2\), so \({\bf F}\) can be interpreted as a gravitational force, Equation \ref{eq:6.4.1} becomes

\[\label{eq:6.4.10} {d^2u\over d\theta^2}+u={k\over h^2}.\]

The general solution of the complementary equation

\[{d^2u\over d\theta^2}+u=0\nonumber\]

can be written in amplitude–phase form as

\[u=A\cos(\theta-\phi),\nonumber\]

where \(A\ge0\) and \(\phi\) is a phase angle. Since \(u_p=k/h^2\) is a particular solution of Equation \ref{eq:6.4.10}, the general solution of Equation \ref{eq:6.4.10} is

\[u=A\cos(\theta-\phi)+{k\over h^2};\nonumber\]

hence, the orbit is given by

\[r=\left(A\cos(\theta-\phi)+{k\over h^2}\right)^{-1},\nonumber\]

which we rewrite as

\[\label{eq:6.4.11} r={\rho\over 1+e\cos(\theta-\phi)},\]

where

\[\rho={h^2\over k}\quad \text{and} \quad e=A\rho.\nonumber\]

A curve satisfying Equation \ref{eq:6.4.11} is a conic section with a focus at the origin (*Exercise 6.4.1*). The nonnegative constant \(e\) is the *eccentricity* of the orbit, which is an ellipse if \(e<1\) ellipse (a circle if \(e=0\)), a parabola if \(e=1\), or a hyperbola if \(e>1\).

If the orbit is an ellipse, then the minimum and maximum values of \(r\) are

\[\begin{aligned} r_{\min}&={\rho\over1+e}\quad\mbox{(the perihelion distance is attained when $\theta=\phi$)} \\ r_{\max}&={\rho\over1-e}\quad \mbox{(the aphelion distance is attained when $\theta=\phi+\pi$)}.\end{aligned}\]

Figure \(\PageIndex{4}\) shows a typical elliptic orbit. The point \(P\) on the orbit where \(r=r_{\min}\) is the *perigee* and the point \(A\) where \(r=r_{\max}\) is the *apogee*.

Orbits: Earth and Halley's Comet

Earth’s orbit around the Sun is approximately an ellipse with \(e\approx 0.017\), \(r_{\min}\approx 91 \times 10^6\) miles, and \(r_{\max}\approx 95\times 10^6\) miles. Halley’s comet has a very elongated approximately elliptical orbit around the sun (Figure \(\PageIndex{5; left}\)), with \(e\approx 0.967\), \(r_{\min}\approx 55 \times10^6\) miles, and \(r_{\max}\approx 33 \times 10^8\) miles. Some comets (the nonrecurring type) have parabolic or hyperbolic orbits like the Oumuamua interstellar object (Figure \(\PageIndex{5; right}\)).