Gravitation Inside Earth — Question 6

Section 13-4 · Physics pages 1962–1963

Question 6 A dense core can make interior gravity exceed surface gravity A spherical planet has radius R, core radius c = R/2, core density 4ρ and mantle density ρ. Let C = 4πGρ/3. 4ρ ρ Cross-section of a spherically symmetric mass distribution. (a) Find g(r) in the core and mantle, and compare g(c) with g(R). (b) Locate any stationary point in the mantle and determine the global maximum of g.
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Question 6 - Solution A dense core can make interior gravity exceed surface gravity 4ρ ρ (a) Derivation and calculation With C = 4πGρ/3, the core has M(r) = 4(4πρ/3)r3. The mantle contains the core plus its own shells: g(r) = { 4Cr, 0 ≤r ≤c, C(r + 3c3/r2), c ≤r ≤R. For c = R/2, g(c) = 4Cc = 2CR, g(R) = C(R + 3R/8) = 11 8 CR. (b) Result and interpretation In the mantle, g′(r) = C(1 −6c3/r3) = 0 =⇒ r∗= 61/3c = (3/4)1/3R. g′′(r) = 18Cc3/r4 > 0, so r∗is a minimum. The core rises monotonically, the exterior field decreases, and g(c) > g(R); therefore gmax = 2CR at r = R/2 . Physical check The field is continuous at the core boundary even though its derivative changes sign there.

Question 6

A dense core can make interior gravity exceed surface gravity

A spherical planet has radius RR, core radius c=R/2c=R/2, core density 4ρ4\rho and mantle density ρ\rho. Let C=4πGρ/3C=4\pi G\rho/3.

Diagram shown in the original SVG worksheet.

  1. Find g(r)g(r) in the core and mantle, and compare g(c)g(c) with g(R)g(R).

  2. Locate any stationary point in the mantle and determine the global maximum of gg.

Question 6 - Solution

A dense core can make interior gravity exceed surface gravity

Diagram shown in the original SVG worksheet.

(a) Derivation and calculation

With C=4πGρ/3C=4\pi G\rho/3, the core has M(r)=4(4πρ/3)r3M(r)=4(4\pi\rho/3)r^3. The mantle contains the core plus its own shells: g(r)={4Cr,0≤r≤c,C(r+3c3/r2),c≤r≤R.\boxed{g(r)=\begin{cases}4Cr,&0\le r\le c,\\C(r+3c^3/r^2),&c\le r\le R.\end{cases}} For c=R/2c=R/2, g(c)=4Cc=2CR,g(R)=C(R+3R/8)=118CR.g(c)=4Cc=2CR,\quad g(R)=C(R+3R/8)=\frac{11}{8}CR.

(b) Result and interpretation

In the mantle, g′(r)=C(1−6c3/r3)=0⇒r*=61/3c=(3/4)1/3R.g'(r)=C(1-6c^3/r^3)=0 \quad\Longrightarrow\quad r_*=6^{1/3}c=(3/4)^{1/3}R. g″(r)=18Cc3/r4>0,g''(r)=18Cc^3/r^4>0, so r*r_* is a minimum. The core rises monotonically, the exterior field decreases, and g(c)>g(R)g(c)>g(R); therefore gmax=2CRat r=R/2.\boxed{g_{\max}=2CR\quad\text{at }r=R/2}.

Physical check

The field is continuous at the core boundary even though its derivative changes sign there.