Gravitation Inside Earth — Question 10

Section 13-4 · Physics pages 1970–1971

Question 10 A density jump changes the slope of gravity without making gravity jump A spherical body has a finite density discontinuity at radius c, but no infinitesimally thin massive surface layer. Let g(r) = GM(r)/r2 be its inward field magnitude. r g c ρ1 ρ2 < ρ1 Illustrative field profile across a finite downward density jump: the field is continuous but has a kink. (a) Derive dg/dr in terms of local density and g. (b) Explain the continuity of g and calculate the outward jump in slope if density falls from ρ1 to ρ2.
Show solutionHide solution
Question 10 - Solution A density jump changes the slope of gravity without making gravity jump r g c ρ1 ρ2 < ρ1 (a) Derivation and calculation Differentiate the inward field magnitude: g(r) = GM(r) r2 , dg dr = G r2 dM dr −2GM(r) r3 . Since M′(r) = 4πr2ρ(r), g′(r) = 4πGρ(r) −2g(r) r . (b) Result and interpretation Without a massive surface sheet, the enclosed mass is continuous: M(c+) −M(c−) = lim δ→0 ∫c+δ c−δ 4πr2ρ(r) dr = 0. Hence g(c+) = g(c−) and the −2g/r terms cancel in the slope difference: g′(c+) −g′(c−) = 4πG(ρ2 −ρ1) < 0 . Physical check A finite downward density jump lowers the slope, but need not make the field itself decrease immediately.

Question 10

A density jump changes the slope of gravity without making gravity jump

A spherical body has a finite density discontinuity at radius cc, but no infinitesimally thin massive surface layer. Let g(r)=GM(r)/r2g(r)=GM(r)/r^2 be its inward field magnitude.

Diagram shown in the original SVG worksheet.

  1. Derive dg/drdg/dr in terms of local density and gg.

  2. Explain the continuity of gg and calculate the outward jump in slope if density falls from ρ1\rho_1 to ρ2\rho_2.

Question 10 - Solution

A density jump changes the slope of gravity without making gravity jump

Diagram shown in the original SVG worksheet.

(a) Derivation and calculation

Differentiate the inward field magnitude: g(r)=GM(r)r2,dgdr=Gr2dMdr−2GM(r)r3.g(r)=\frac{GM(r)}{r^2},\quad \frac{dg}{dr}=\frac G{r^2}\frac{dM}{dr}-\frac{2GM(r)}{r^3}. Since M′(r)=4πr2ρ(r)M'(r)=4\pi r^2\rho(r), g′(r)=4πGρ(r)−2g(r)r.\boxed{g'(r)=4\pi G\rho(r)-\frac{2g(r)}r}.

(b) Result and interpretation

Without a massive surface sheet, the enclosed mass is continuous: M(c+)−M(c−)=limδ→0∫c−δc+δ4πr2ρ(r)dr=0.M(c^+)-M(c^-)=\lim_{\delta\to0}\int_{c-\delta}^{c+\delta}4\pi r^2\rho(r)\,dr=0. Hence g(c+)=g(c−)g(c^+)=g(c^-) and the −2g/r-2g/r terms cancel in the slope difference: g′(c+)−g′(c−)=4πG(ρ2−ρ1)<0.\boxed{g'(c^+)-g'(c^-)=4\pi G(\rho_2-\rho_1)<0}.

Physical check

A finite downward density jump lowers the slope, but need not make the field itself decrease immediately.