Intensity and Sound Level — Question 6

Section 17-5 · Physics pages 2722–2723

Question 6 Absorption can be isolated after removing geometric spreading A spherical wave has intensity I(r) = Cr−2e−αr, where α is an intensity attenuation coefficient. Levels measured at r1 = 10 m and r2 = 20 m differ by 8.00 dB, with the farther level lower. r Ir2 Removing inverse-square spreading leaves the absorption factor. (a) Infer α. (b) Find the additional distance that halves intensity by absorption alone. State the corresponding pressure-amplitude attenuation coefficient.
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Question 6 - Solution Absorption can be isolated after removing geometric spreading r Ir2 (a) Method and calculation Take the logarithm of the intensity ratio: β1 −β2 = 20 log10(r2/r1) + 10α(r2 −r1) ln 10 . α = [8.00 −20 log10 2] ln 10 10(10) = 0.045577 m−1. Geometric spreading accounts for 6.0206 dB; the remainder is absorption. (b) Interpretation and further calculation The absorption-only half-intensity length satisfies e−αℓ1/2 = 1 2, ℓ1/2 = ln 2 α = 15.21 m. Because intensity is proportional to pressure amplitude squared, pressure carries the factor e−αr/2. Its attenuation coefficient is α/2, in addition to the geometrical 1/r factor. Physical check A measured drop below 6.0206 dB would imply negative α and contradict passive absorption under this model.

Question 6

Absorption can be isolated after removing geometric spreading

A spherical wave has intensity I(r)=Cr−2e−αrI(r)=C r^{-2}e^{-\alpha r}, where α\alpha is an intensity attenuation coefficient. Levels measured at r1=10mr_1=10\,\mathrm m and r2=20mr_2=20\,\mathrm m differ by 8.00dB8.00\,\mathrm{dB}, with the farther level lower.

Diagram shown in the original SVG worksheet.

  1. Infer α\alpha.

  2. Find the additional distance that halves intensity by absorption alone. State the corresponding pressure-amplitude attenuation coefficient.

Question 6 - Solution

Absorption can be isolated after removing geometric spreading

Diagram shown in the original SVG worksheet.

(a) Method and calculation

Take the logarithm of the intensity ratio:β1−β2=20log⁡10(r2/r1)+10α(r2−r1)ln⁡10.\beta_1-\beta_2=20\log_{10}(r_2/r_1)+\frac{10\alpha(r_2-r_1)}{\ln10}.α=[8.00−20log⁡102]ln⁡1010(10)=0.045577m−1.\alpha=\frac{[8.00-20\log_{10}2]\ln10}{10(10)}=0.045577\,\mathrm{m^{-1}}.Geometric spreading accounts for 6.0206dB6.0206\,\mathrm{dB}; the remainder is absorption.

(b) Interpretation and further calculation

The absorption-only half-intensity length satisfiese−αℓ1/2=12,ℓ1/2=ln⁡2α=15.21m.e^{-\alpha\ell_{1/2}}=\tfrac12,\qquad\ell_{1/2}=\frac{\ln2}{\alpha}=15.21\,\mathrm m.Because intensity is proportional to pressure amplitude squared, pressure carries the factor e−αr/2e^{-\alpha r/2}. Its attenuation coefficient is α/2\alpha/2, in addition to the geometrical 1/r1/r factor.

Physical check

A measured drop below 6.0206dB6.0206\,\mathrm{dB} would imply negative α\alpha and contradict passive absorption under this model.