Gravitation Near Earth's Surface — Question 7

Section 13-3 · Physics pages 1944–1945

Question 7 The width of a gravity anomaly can reveal a buried depth After subtracting the background field, a compact excess mass ∆M is modeled as a point at depth d below a flat surface. Let x be horizontal distance from the point directly above it. ∆M d x Schematic; labels, not drawing lengths, specify the data. (a) Derive the downward gravity anomaly ∆gz(x). (b) If the anomaly falls to half its central value at x = w, infer d in terms of w.
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Question 7 - Solution The width of a gravity anomaly can reveal a buried depth ∆M d x (a) Derivation and calculation Let s = √ x2 + d2. The downward projection of the point-source field is ∆gz = G∆M s2 d s = G∆Md (x2 + d2)3/2 . At the central point, ∆gz(0) = G∆M d2 , ∆gz(x) ∆gz(0) = [1 + (x/d)2]−3/2. (b) Result and interpretation The half-height condition gives [1 + (w/d)2]−3/2 = 1 2 =⇒ 1 + (w/d)2 = 22/3. d = w √ 22/3 −1 ≃1.30477w , ∆M = d2∆gz(0) G . Width determines depth and amplitude then determines excess mass within the stated model. Physical check The anomaly is symmetric in x and decreases to zero far from the buried source.

Question 7

The width of a gravity anomaly can reveal a buried depth

After subtracting the background field, a compact excess mass ΔM\Delta M is modeled as a point at depth dd below a flat surface. Let xx be horizontal distance from the point directly above it.

Diagram shown in the original SVG worksheet.

  1. Derive the downward gravity anomaly Δgz(x)\Delta g_z(x).

  2. If the anomaly falls to half its central value at x=wx=w, infer dd in terms of ww.

Question 7 - Solution

The width of a gravity anomaly can reveal a buried depth

Diagram shown in the original SVG worksheet.

(a) Derivation and calculation

Let s=x2+d2s=\sqrt{x^2+d^2}. The downward projection of the point-source field is Δgz=GΔMs2ds=GΔMd(x2+d2)3/2.\Delta g_z=\frac{G\Delta M}{s^2}\frac ds =\boxed{\frac{G\Delta M d}{(x^2+d^2)^{3/2}}}. At the central point, Δgz(0)=GΔMd2,Δgz(x)Δgz(0)=[1+(x/d)2]−3/2.\Delta g_z(0)=\frac{G\Delta M}{d^2},\quad \frac{\Delta g_z(x)}{\Delta g_z(0)}=[1+(x/d)^2]^{-3/2}.

(b) Result and interpretation

The half-height condition gives [1+(w/d)2]−3/2=12⇒1+(w/d)2=22/3.[1+(w/d)^2]^{-3/2}=\frac12 \quad\Longrightarrow\quad 1+(w/d)^2=2^{2/3}. d=w22/3−1≃1.30477w,ΔM=d2Δgz(0)G.\boxed{d=\frac{w}{\sqrt{2^{2/3}-1}}\simeq1.30477w},\qquad \Delta M=\frac{d^2\Delta g_z(0)}G. Width determines depth and amplitude then determines excess mass within the stated model.

Physical check

The anomaly is symmetric in xx and decreases to zero far from the buried source.