Content deleted Content added
→Converses and generalizations: Continuation of previous edit in this section Tags: Mobile edit Mobile web edit Advanced mobile edit |
Inline markers; removal of repeatedly specified limits; spacing and wrapping around punctuation; the {{block indent}} thing of previous edits |
||
Line 3:
[[Isaac Newton]] proved the shell theorem<ref name="Newton philo">{{cite book|last=Newton|first=Isaac|title=Philosophiae Naturalis Principia Mathematica|url=https://archive.org/details/philosophinatur03newtgoog|date=1687|___location=London|pages=Theorem XXXI}}</ref> and stated that:
# A [[sphere|spherically]] [[symmetry|symmetric]] body affects external objects gravitationally as though all of its [[mass]] were concentrated at a [[point mass|point]] at its
# If the body is a spherically symmetric shell (i.e., a hollow ball), no net [[gravitational force]] is exerted by the shell on any object inside, regardless of the object's ___location within the shell.
A corollary is that inside a solid sphere of constant density, the gravitational force within the object varies linearly with distance from the
These results were important to Newton's analysis of planetary motion; they are not immediately obvious, but they can be proven with [[calculus]]. (Alternatively, [[Gauss's law for gravity]] offers a much simpler way to prove the same results.)
Line 18:
:<math>E_\text{point}=\frac{GM}{p^2}</math>
<blockquote>[[File:Point2.png|frameless|300x300px]]</blockquote>
Suppose that this mass is moved upwards along the ''y''-axis to point {{nowrap|<math>(0,R)</math>.}} The distance between <math>P</math> and the point mass is now longer than before; It becomes the hypotenuse of the right triangle with legs <math>p</math> and <math>R</math> which is {{nowrap|<math display="inline">\sqrt{p^2+R^2}</math>.}} Hence, the gravitational field of the elevated point is:
:<math>E_\text{elevated point}=\frac{GM}{p^2+R^2}</math>
<blockquote>[[File:Pointy2.png|frameless|270x270px]]</blockquote>
The magnitude of the gravitational field that would pull a particle at point <math>P</math> in the ''x''-direction is the gravitational field multiplied by <math>\cos(\theta)</math> where <math>\theta</math> is the angle adjacent to the ''x''-axis. In this case, {{nowrap|<math>\cos(\theta)=\frac{p}{\sqrt{p^2+R^2}}</math>.}} Hence, the magnitude of the gravitational field in the ''x''-direction, <math>E_x</math> is:
:<math>E_x=\frac{GM\cos{\theta}}{p^2+R^2}</math>
Substituting in <math>\cos(\theta)</math> gives
:<math>E_x=\frac{GMp}{\left(p^2+R^2\right)^{3/2}}</math>
Suppose that this mass is evenly distributed in a ring centered at the origin and facing point <math>P</math> with the same radius {{nowrap|<math>R</math>.}} Because all of the mass is located at the same angle with respect to the ''x''-axis, and the distance between the points on the ring is the same distance as before, the gravitational field in the ''x''-direction at point <math>P</math> due to the ring is the same as a point mass located at a point <math>R</math> units above the ''y''-axis:
:<math>E_\text{ring}=\frac{GMp}{\left(p^2+R^2\right)^{3/2}}</math>
<blockquote>[[File:Wider ring2.png|frameless|280x280px]]</blockquote>
To find the gravitational field at point <math>P</math> due to a disc, an infinite number of infinitely thin rings facing {{nowrap|<math>P</math>,}} each with a radius {{nowrap|<math>y</math>,}} width of {{nowrap|<math>dy</math>,}} and mass of <math>dM</math> may be placed inside one another to form a disc. The mass of any one of the rings <math>dM</math> is the mass of the disc multiplied by the ratio of the area of the ring <math>2\pi y\,dy</math> to the total area of the disc {{nowrap|<math>\pi R^2</math>.}} So, {{nowrap|<math display="inline">dM=\frac{M\cdot 2y\,dy}{R^2}</math>.}} Hence, a small change in the gravitational field, <math>E</math> is:
:<math>dE=\frac{Gp\,dM}{(p^2+y^2)^{3/2}}</math>
<blockquote>[[File:Wider ring with inside ring2.png|frameless|350x350px]]</blockquote>
Substituting in <math>dM</math> and integrating both sides gives the gravitational field of the disk:
:<math>E=\int \frac{GMp\cdot \frac{2y\, dy}{R^2}}{(p^2+y^2)^{3/2}}</math>
Adding up the contribution to the gravitational field from each of these rings will yield the expression for the gravitational field due to a disc. This is equivalent to integrating this above expression from <math>y=0</math> to {{nowrap|<math>y=R</math>,}} resulting in:
:<math>E_\text{disc}=\frac{2GM}{R^2} \left( 1-\frac{p}{\sqrt{p^2+R^2}}\right)</math>
To find the gravitational field at point <math>P</math> due to a sphere centered at the origin, an infinite amount of infinitely thin discs facing {{nowrap|<math>P</math>,}} each with a radius {{nowrap|<math>R</math>,}} width of {{nowrap|<math>dx</math>,}} and mass of <math>dM</math> may be placed together.
These discs' radii <math>R</math> follow the height of the cross section of a sphere (with constant radius <math>a</math>) which is an equation of a semi-circle: {{nowrap|<math display="inline">R=\sqrt{a^2-x^2}</math>.}} <math>x</math> varies from <math>-a</math> to {{nowrap|<math>a</math>.}}
The mass of any of the discs <math>dM</math> is the mass of the sphere <math>M</math> multiplied by the ratio of the volume of an infinitely thin disc divided by the volume of a sphere (with constant radius {{nowrap|<math>a</math>).}} The volume of an infinitely thin disc is {{nowrap|<math>\pi R^2\, dx</math>,}} or {{nowrap|<math display="inline">\pi\left(a^2-x^2
Each discs' position away from <math>P</math> will vary with its position within the 'sphere' made of the discs, so <math>p</math> must be replaced with {{nowrap|<math>p+x</math>.
[[File:Series of discs2.png|frameless|350x350px]]
Replacing <math>M</math> with {{nowrap|<math>dM</math>,}} <math>R</math> with {{nowrap|<math>\sqrt{a^2-x^2}</math>,}} and <math>p</math> with <math>p+x</math> in the 'disc' equation yields:
:<math>dE=\frac{\left( \frac{2G\left[3M\left(a^2-x^2\right)\right]}{4a^3} \right) }{\sqrt{a^2-x^2}^2}\cdot \left(1-\frac{p+x}{\sqrt{(p+x)^2+\sqrt{a^2-x^2}^2}}\right)\, dx</math>
Simplifying,
:<math>\int dE=\int_{-a}^a \frac{3GM}{2a^3} \left(1-\frac{p+x}{\sqrt{p^2+a^2+2px}}\right)\, dx</math>
Integrating the gravitational field of each thin disc from <math>x=-a</math> to <math>x=+a</math> with respect to {{nowrap|<math>x</math>,}} and doing some careful algebra, yields Newton's shell theorem:
:<math>E=\frac{GM}{p^2}</math>
where <math>p</math> is the distance between the center of the spherical mass and an arbitrary point {{nowrap|<math>P</math>.}} The gravitational field of a spherical mass may be calculated by treating all the mass as a point particle at the center of the sphere.
== Outside a shell ==
Line 58:
[[File:shell-diag-1.svg|center|500px]]
(Note: the <math>d\theta</math> in the diagram refers to the small angle, not the [[arclength|arc length]]. The arc length is {{nowrap|<math display="inline">R\
Applying [[Newton's Universal Law of Gravitation]], the sum of the forces due to the mass elements in the shaded band is
:<math>dF = \frac{Gm
However, since there is partial cancellation due to the [[Euclidean vector|vector]] nature of the force in conjunction with the circular band's symmetry, the leftover [[Vector (geometry)#Vector components|component]] (in the direction pointing towards {{nowrap|<math>m</math>)}} is given by
:<math>dF_r = \frac{Gm
The total force on {{nowrap|<math>m</math>,}} then, is simply the sum of the force exerted by all the bands. By shrinking the width of each band, and increasing the number of bands, the sum becomes an integral expression:
:<math>F_r = \int dF_r</math>
Line 70:
Since <math>G</math> and <math>m</math> are constants, they may be taken out of the integral:
:<math>F_r = Gm \int \frac{\cos(\varphi
To evaluate this integral, one must first express <math>dM</math> as a function of <math>d\theta</math>
Line 77:
:<math>4\pi R^2 </math>
while the surface area of the thin slice between <math>\theta</math> and <math>\theta+d\theta</math> is
:<math>2\pi R\sin(\theta)
If the mass of the shell is {{nowrap|<math>M</math>,}} one therefore has that
:<math>dM = \frac {2\pi R^2\sin(\theta) }{4\pi R^2} M\,d\theta = \frac{1}{2} M\sin(\theta) \,d\theta</math>
and
:<math>F_r = \frac{GMm}{2} \int \frac{\sin(\theta) \cos(\varphi)} {s^2}\,d\theta </math>
By the [[law of cosines]],
:<math>\cos(\varphi) = \frac{r^2 + s^2 - R^2}{2rs}</math>
and
:<math>\cos(\theta) = \frac{r^2 + R^2 - s^2}{2rR}.</math>
These two relations link the three parameters {{nowrap|<math>\theta</math>,}} <math>\varphi</math> and <math>s</math> that appear in the integral together. As <math>\theta</math> increases from <math>0</math> to <math>\pi</math> radians, <math>\varphi</math> varies from the initial value 0 to a maximal value before finally returning to zero {{nowrap|at
[[File:Shell-diag-1-anim.gif|center]]
(Note: As viewed from {{nowrap|<math>m</math>,}} the shaded blue band appears as a thin [[annulus (mathematics)|annulus]] whose inner and outer radii converge to <math>R \sin
To find a [[primitive function]] to the integrand, one has to make <math>s</math> the independent integration variable instead of {{nowrap|<math>\theta</math>.}}
Performing an [[implicit differentiation]] of the second of the "cosine law" expressions above yields
:<math>-\sin(\theta) \
and thus
:<math>\sin(\theta) \
It follows that
:<math>F_r = \frac{GMm}{2} \frac{1}{rR} \int \frac{s\cos(\varphi)} {s^2}\,ds = \frac{GMm}{2rR} \int \frac{\cos(\varphi)} s \,ds </math>
where the new integration variable <math>s</math> increases from <math>r-R</math> {{nowrap|to
Inserting the expression for <math>\cos
:<math>F_r = \frac{GMm}{4r^2 R} \int \left( 1 + \frac{r^2 - R^2}{s^2} \right)\ ds\ .</math>
Line 126:
and inserting the bounds <math>r-R</math> and <math>r+R</math> for the integration variable <math>s</math> in this primitive function, one gets that
:<math>F_r = \frac{GMm}{r^2},</math>
saying that the gravitational force is the same as that of a point mass in the
Finally, integrate all infinitesimally thin spherical shell with mass of {{nowrap|<math>dM</math>,}} and we can obtain the total gravity contribution of a solid ball to the object outside the ball
:<math>F_{total} = \int dF_r = \frac{Gm}{r^2} \int dM.</math>
Between the radius of <math>x</math> to {{nowrap|<math>x+dx</math>,}} <math>dM</math> can be expressed as a function of {{nowrap|<math>x</math>,}} i.e.,
:<math>dM = \frac{4 \pi x^2 dx}{\frac{4}{3} \pi R^3} M = \frac{3Mx^2 dx}{R^3}</math>
Line 140:
:<math>F_\text{total} = \frac{3GMm}{r^2 R^3} \int_0^R x^2 \, dx = \frac{GMm}{r^2}</math>
which suggests that the gravity of a solid spherical ball to an exterior object can be simplified as that of a point mass in the
== Inside a shell ==
For a point inside the shell, the difference is that when ''θ'' is equal to zero, ''ϕ'' takes the value {{pi}} radians and ''s'' the value {{nowrap|''R''
This can all be seen in the following figure
Line 158:
saying that the net gravitational forces acting on the point mass from the mass elements of the shell, outside the measurement point, cancel out.
'''Generalization:''' If {{nowrap|<math>f=\frac{k}{r^p}</math>,}} the resultant force inside the shell is:
:<math>F(r) = \frac{GMm}{4r^2 R} \int_{R-r}^{R+r} \left( \frac{1}{s^{p-2}} + \frac{r^2 - R^2}{s^p} \right) \, ds</math>
Line 171:
The shell theorem is an immediate consequence of [[Gauss's law for gravity]] saying that
where ''M'' is the mass of the part of the spherically symmetric mass distribution that is inside the sphere with radius ''r'' and
is the [[surface integral]] of the [[gravitational field]] '''g''' over any [[closed surface]] inside which the total mass is ''M'', the [[unit vector]] <math>
The gravitational field of a spherically symmetric mass distribution like a mass point, a spherical shell or a homogeneous sphere must also be spherically symmetric. If <math>\hat\mathbf{
where ''g''(''r'') only depends on the distance ''r'' to the point of symmetry
Selecting the closed surface as a sphere with radius ''r'' with center at the point of symmetry the outward normal to a point on the surface, {{nowrap|<math>
One, therefore, has that
and
as the area of the sphere is 4{{pi}}''r''<sup>2</sup>.
From Gauss's law it then follows that
or,
== Converses and generalizations ==
Line 206:
It is natural to ask whether the [[Theorem#Converse|converse]] of the shell theorem is true, namely whether the result of the theorem implies the law of universal gravitation, or if there is some more general force law for which the theorem holds. More specifically, one may ask the question:
{{block indent|Suppose there is a force <math>F</math> between masses ''M'' and ''m'', separated by a distance ''r'' of the form <math>F = M m f(r)</math> such that any spherically symmetric body affects external bodies as if its mass were concentrated at its
In fact, this allows exactly one more class of force than the (Newtonian) inverse square.<ref name=Gurzadyan>{{cite journal| last=Gurzadyan |first=Vahe |authorlink=vahe Gurzadyan|title=The cosmological constant in McCrea-Milne cosmological scheme|journal=The Observatory|date= 1985|volume=105|pages=42–43|bibcode=1985Obs...105...42G}} http://adsabs.harvard.edu/full/1985Obs...105...42G</ref><ref name=Arens>{{cite journal| last=Arens| first=Richard| authorlink=Richard Friederich Arens|title=Newton's observations about the field of a uniform thin spherical shell|journal=Note di Matematica|date=January 1, 1990|volume=X|issue=Suppl. n. 1|pages=39–45}}</ref> The most general force as derived in <ref name="Gurzadyan"/> is:
Line 216:
If we further constrain the force by requiring that the second part of the theorem also holds, namely that there is no force inside a hollow ball, we exclude the possibility of the additional term, and the inverse square law is indeed the unique force law satisfying the theorem.
On the other hand, if we relax the conditions, and require only that the field everywhere outside a spherically symmetric body is the same as the field from some point mass at the
Another generalization can be made for a disc by observing that
:<math>dM=\frac{R^2}{2} \frac{d\theta \, \sin^2(\theta)}{\pi R^2}M=\frac{ \sin^2(\theta)}{2 \pi}M \, d\theta </math>
so:
:<math>F_r = \frac{GMm}{2 \pi} \int \frac{ \sin^2 (\theta) \cos(\varphi)} {s^2} \, d\theta,</math>
where {{nowrap|<math>M=\pi R^2 \rho</math>,}} and <math>\rho</math> is the density of the body.
Doing all the intermediate calculations we get:
:<math>F(r) = \frac{
== Newton's proofs ==
Line 240:
His proof of Propositions 70 is trivial. In the following, it is considered in slightly greater detail than Newton provides.
The proof of Proposition 71 is more historically significant. It forms the first part of his proof that the gravitational force of a solid sphere acting on a particle outside it is inversely proportional to the square of its distance from the
Although the following are completely faithful to Newton's proofs, very minor changes have been made to attempt to make them clearer.
Line 248:
[[File:Attraction Interior Sphere.png|Attraction interior sphere]]
Fig. 2 is a cross-section of the hollow sphere through the
The surface of the sphere that the cones intersect can be considered to be flat, and {{nowrap|<math> \angle PJI = \angle PMK </math>
Since the intersection of a cone with a plane is an ellipse, in this case the intersections form two ellipses with major axes IH and KL, where {{nowrap|<math> \frac{IH}{KL} = \frac{PJ}{PM} </math>
By a similar argument, the minor axes are in the same ratio. This is clear if the sphere is viewed from above. Therefore the two ellipses are similar, so their areas are as the squares of their major axes. As the mass of any section of the surface is proportional to the area of that section, for the 2 elliptical areas the ratios of their masses {{nowrap|<math> \propto \frac{PJ^2}{PM^2} </math>.}}
Since the force of attraction on P in the direction JM from either of the elliptic areas, is direct as the mass of the area and inversely as the square of its distance from P, it is independent of the distance of P from the sphere. Hence, the forces on P from the 2 infinitesimal elliptical areas are equal and opposite and there is no net force in the direction JM.
Line 267 ⟶ 266:
[[File:Attraction Exterior Sphere.png|Attraction exterior sphere]]
Fig. 1 is a cross-section of the hollow sphere through the
Let arc IH be extended perpendicularly out of the plane of the diagram, by a small distance ζ. The area of the figure generated is {{nowrap|<math> IH\cdot \zeta </math>,}} and its mass is proportional to this product.
The force due to this mass on the particle at P <math> \propto \frac{IH\cdot \zeta}{PI^2} </math> and is along the line PI.
The component of this force towards the
If now the arc ''HI'' is rotated completely about the line ''PS'' to form a ring of width ''HI'' and radius ''IQ'', the length of the ring is 2{{pi}}·''IQ'' and its area is 2{{pi}}·''IQ''·''IH''. The component of the force due to this ring on the particle at ''P'' in the direction PS becomes {{nowrap|<math> \propto \frac{IH\cdot IQ\cdot PQ}{PI^3} </math>.}}
The perpendicular components of the force directed towards ''PS'' cancel out since the mass in the ring is distributed symmetrically about ''PS''. Therefore, the component in the direction ''PS'' is the total force on ''P'' due to the ring formed by rotating arc ''HI'' about ''PS''.
From similar triangles: {{nowrap|<math> \frac{IQ}{PI} = \frac{FS}{D}</math>;}} {{nowrap|<math> \frac{PQ}{PI} = \frac{PF}{D}</math>,}} and {{nowrap|<math> \frac{RI}{PI} = \frac{DF}{PF}</math>.}}
If HI is sufficiently small that it can be taken as a straight line, <math> \angle SIH </math> is a right angle, and {{nowrap|<math> \angle RIH = \angle FIS </math>,}} so that {{nowrap|<math> \frac{HI}{RI} = \frac{a}{IF}</math>.}}
Hence the force on ''P'' due to the ring {{nowrap|<math> \propto \frac{IH\cdot IQ\cdot PQ}{PI^3} = \frac{a\cdot DF\cdot FS\cdot PF}{IF\cdot PF\cdot D\cdot D} = \frac{a\cdot DF\cdot FS}{IF\cdot D^2} </math>.}}
Assume now in Fig. 2 that another particle is outside the sphere at a point ''p'', a different distance ''d'' from the
Generate a ring with width ih and radius iq by making angle <math> fiS = FIS </math> and the slightly larger
The total force on p due to this ring is
Clearly {{nowrap|<math> fS = FS </math>,}} {{nowrap|<math> if = IF </math>,}} and {{nowrap|<math> eS = ES </math>.}}
Newton claims that DF and df can be taken as equal in the limit as the angles DPF and dpf 'vanish together'. Note that angles DPF and dpf are not equal. Although DS and dS become equal in the limit, this does not imply that the ratio of DF to df becomes equal to unity, when DF and df both approach zero. In the finite case DF depends on D, and df on d, so they are not equal.
Since the ratio of DF to df in the limit is crucial, more detailed analysis is required. From the similar right triangles, <math> \frac {DF}{PF} = \frac{ED}{ES}</math> and <math> ED^2 = (DF + FS)^2 - ES^2 </math>, giving <math> \frac {(PF^2 - ES^2)DF^2}{PF^2} + 2.FS.DF + FS^2 - ES^2 = 0 </math>. Solving the quadratic for DF, in the limit as ES approaches FS, the smaller root, <math> DF = ES - FS </math>. More simply, as DF approaches zero, in the limit the <math> DF^2 </math> term can be ignored: <math> 2\cdot FS\cdot DF + FS^2 - ES^2 = 0 </math> leading to the same result. Clearly df has the same limit, justifying Newton’s claim.▼
▲Since the ratio of DF to df in the limit is crucial, more detailed analysis is required. From the similar right triangles, <math display="inline"> \frac {DF}{PF} = \frac{ED}{ES}</math> and {{nowrap|<math> ED^2 = (DF + FS)^2 - ES^2 </math>,}} giving {{nowrap|<math> \frac {\left(PF^2 - ES^2\right)DF^2}{PF^2} + 2
Comparing the force from the ring HI rotated about PS to the ring hi about pS, the ratio of these 2 forces equals <math> \frac{d^2}{D^2} </math>.▼
▲Comparing the force from the ring HI rotated about PS to the ring hi about pS, the ratio of these 2 forces equals {{nowrap|<math display="inline"> \frac{d^2}{D^2} </math>.}}
By dividing up the arcs AT and Bt into corresponding infinitesimal rings, it follows that the ratio of the force due to the arc AT rotated about PS to that of Bt rotated about pS is in the same ratio, and similarly, the ratio of the forces due to arc TB to that of tA both rotated are in the same ratio.
Therefore, the force on a particle any distance D from the
== Shell theorem in general relativity ==
Line 310 ⟶ 309:
Spherical symmetry implies that the metric has time-independent Schwarzschild geometry, even if a central mass is undergoing gravitational collapse (Misner et al. 1973; see [[Birkhoff's theorem (relativity)|Birkhoff's theorem]]). The [[Metric tensor (general relativity)|metric]] thus has form
:<math>ds^2 = - (1-2M/r)\, dt^2 + (1-2M/r)^{-1} \, dr^2 + r^2 \, d\Omega^2</math>
(using [[Geometrized unit system|geometrized units]], where {{nowrap|<math>G=c=1</math>).}} For <math>r>R>0</math> (where <math>R</math> is the radius of some mass shell), mass acts as a [[delta function]] at the origin. For {{nowrap|<math>r < R</math>,}} shells of mass may exist externally, but for the metric to be [[Singularity (mathematics)|non-singular]] at the origin, <math>M</math> must be zero in the metric. This reduces the metric to flat [[Minkowski space]]; thus external shells have no gravitational effect.
This result illuminates the [[gravitational collapse]] leading to a black hole and its effect on the motion of light-rays and particles outside and inside the event horizon (Hartle 2003, chapter 12).
|