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NASA-CR-2760

Atmospheric absorption of high frequency noise and application to fractional-octave bands

Organization:
NASA - National Aeronautics and Space Administration (NASA)
Year: 1977

Abstract: Pure tone sound absorption coefficients were measured at 1/12 octave intervals from 4 to 100 KHz at 5.5K temperature intervals between 255.4 and 310.9 K and at 10 percent relative humidity increments between 0 percent and saturation in a large cylindrical tube (i.d., 25.4 cm; length, 4.8 m). Special solid-dielectric capacitance transducers, one to generate bursts of sound waves and one to terminate the sound path and detect the tone bursts, were constructed to fit inside the tube. The absorption was measured by varying the transmitter receiver separation from 1 to 4 m and observing the decay of multiple reflections or change in amplitude of the first received burst. The resulting absorption was compared with that from a proposed procedure for computing sound absorption in still air. Absorption of bands of noise was numerically computed by using the pure tone results. The results depended on spectrum shape, on filter type, and nonlinearly on propagation distance. For some of the cases considered, comparison with the extrapolation of ARP-866A showed a difference as large as a factor of 2. However, for many cases, the absorption for a finite band was nearly equal to the pure tone absorption at the center frequency of the band. A recommended prediction procedure is described for 1/3 octave band absorption coefficients.
URI: https://yse.yabesh.ir/std/handle/yse/134195
Subject: ABSORPTIVITY
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    NASA-CR-2760

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contributor authorNASA - National Aeronautics and Space Administration (NASA)
date accessioned2017-09-04T17:10:39Z
date available2017-09-04T17:10:39Z
date copyright01/01/1977
date issued1977
identifier otherYQHOEEAAAAAAAAAA.pdf
identifier urihttps://yse.yabesh.ir/std/handle/yse/134195
description abstractPure tone sound absorption coefficients were measured at 1/12 octave intervals from 4 to 100 KHz at 5.5K temperature intervals between 255.4 and 310.9 K and at 10 percent relative humidity increments between 0 percent and saturation in a large cylindrical tube (i.d., 25.4 cm; length, 4.8 m). Special solid-dielectric capacitance transducers, one to generate bursts of sound waves and one to terminate the sound path and detect the tone bursts, were constructed to fit inside the tube. The absorption was measured by varying the transmitter receiver separation from 1 to 4 m and observing the decay of multiple reflections or change in amplitude of the first received burst. The resulting absorption was compared with that from a proposed procedure for computing sound absorption in still air. Absorption of bands of noise was numerically computed by using the pure tone results. The results depended on spectrum shape, on filter type, and nonlinearly on propagation distance. For some of the cases considered, comparison with the extrapolation of ARP-866A showed a difference as large as a factor of 2. However, for many cases, the absorption for a finite band was nearly equal to the pure tone absorption at the center frequency of the band. A recommended prediction procedure is described for 1/3 octave band absorption coefficients.
languageEnglish
titleNASA-CR-2760num
titleAtmospheric absorption of high frequency noise and application to fractional-octave bandsen
typestandard
page240
statusActive
treeNASA - National Aeronautics and Space Administration (NASA):;1977
contenttypefulltext
subject keywordsABSORPTIVITY
subject keywordsATMOSPHERIC ATTENUATION
subject keywordsBANDWIDTH
subject keywordsBROADBAND
subject keywordsCOMPUTATION
subject keywordsFREQUENCY RANGES
subject keywordsGRAPHS (CHARTS)
subject keywordsHIGH FREQUENCIES
subject keywordsNOISE SPECTRA
subject keywordsSOUND TRANSMISSION
subject keywordsTRANSMITTER RECEIVERS
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