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Infrasound

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Infrasound arrays at infrasound monitoring station in Qaanaaq, Greenland.

Infrasound, sometimes referred to as low-frequency sound, is sound that is lower in frequency than 20 Hz (Hertz) or cycles per second, the "normal" limit of human hearing. Hearing becomes gradually less sensitive as frequency decreases, so for humans to perceive infrasound, the sound pressure must be sufficiently high. The ear is the primary organ for sensing infrasound, but at higher intensities it is possible to feel infrasound vibrations in various parts of the body.

The study of such sound waves is referred to sometimes as infrasonics, covering sounds beneath 20 Hz down to 0.001 Hz. This frequency range is utilized for monitoring earthquakes, charting rock and petroleum formations below the earth, and also in ballistocardiography and seismocardiography to study the mechanics of the heart. Infrasound is characterized by an ability to cover long distances and get around obstacles with little dissipation.

History and study

Infrasound was used by the Allies of World War I to locate artillery.[1] One of the pioneers in infrasonic research was French scientist, Vladimir Gavreau, who was born in Russia as Vladimir Gavronsky.[2] His interest in infrasonic waves first came about in his laboratory during the 1960s, when he and his laboratory assistants experienced pain in the ear drums and shaking laboratory equipment, but no audible sound was picked up on his microphones. He concluded it was infrasound caused by a large fan and duct system and soon got to work preparing tests in the laboratories. One of his experiments was an infrasonic whistle, an oversized organ pipe.[3][4][5]

Sources

A unique double bass reflex loudspeaker enclosure design intended to efficiently produce infrasonic frequencies ranging from 5 to 25 Hertz which traditional subwoofer designs are not readily capable of.

Infrasound sometimes results naturally from severe weather, surf,[6] lee waves, avalanches, earthquakes, volcanoes, bolides,[7] waterfalls, calving of icebergs, aurorae, meteors, lightning and upper-atmospheric lightning.[8] Nonlinear ocean wave interactions in ocean storms produce pervasive infrasound vibrations around 0.2 Hz, known as microbaroms.[9] According to the Infrasonics Program at the NOAA, infrasonic arrays can be used to locate avalanches in the Rocky Mountains, and to detect tornadoes on the high plains several minutes before they touch down.[10]

Infrasound also can be generated by human-made processes such as sonic booms and explosions (both chemical and nuclear), by machinery such as diesel engines and older designs of down tower wind turbines and by specially designed mechanical transducers (industrial vibration tables) and large-scale subwoofer loudspeakers [11] such as rotary woofers. The Comprehensive Nuclear-Test-Ban Treaty Organization Preparatory Commission uses infrasound as one of its monitoring technologies, along with seismic, hydroacoustic, and atmospheric radionuclide monitoring. The largest infrasound ever recorded by the monitoring system was generated by the 2013 Chelyabinsk meteor.[12]

Whales, elephants,[13] hippopotamuses,[14] rhinoceros,[15][16] giraffes,[17] okapi,[18] and alligators are known to use infrasound to communicate over distances—up to hundreds of miles in the case of whales. In particular, the Sumatran Rhinoceros has been shown to produce sounds with frequencies as low as 3 Hz which have similarities with the song of the humpback whale.[16] The roar of the tiger contains infrasound of 18 Hz and lower,[19] and the purr of felines is reported to cover a range of 20 to 50 Hz.[20][21][22] It has also been suggested that migrating birds use naturally generated infrasound, from sources such as turbulent airflow over mountain ranges, as a navigational aid.[23] Elephants, in particular, produce infrasound waves that travel through solid ground and are sensed by other herds using their feet, although they may be separated by hundreds of kilometres.

Animal reactions to infrasound

Animals have been known to perceive the infrasonic waves going through the earth by natural disasters and can use these as an early warning. A recent example of this is the 2004 Indian Ocean earthquake and tsunami. Animals were reported to flee the area hours before the actual tsunami hit the shores of Asia.[24][25] It is not known for sure if this is the exact reason, as some have suggested that it may have been the influence of electromagnetic waves, and not of infrasonic waves, that prompted these animals to flee.[26]

Infrasound also may be used for long-distance communication in African elephants.[27] These calls range from 15–35 Hz and can be as loud as 117 dB, allowing communication for many kilometres, with a possible maximum range of around 10 km (6 mi).[28] These calls may be used to coordinate the movement of herds and allow male elephants to find mates.

Recent research by Jon Hagstrum of the US Geological Survey suggests that homing pigeons use low frequency infrasound to navigate. [29]

Human reactions to infrasound

20 Hz is considered the normal low-frequency limit of human hearing. When pure sine waves are reproduced under ideal conditions and at very high volume, a human listener will be able to identify tones as low as 12 Hz.[30] Below 10 Hz it is possible to perceive the single cycles of the sound, along with a sensation of pressure at the eardrums.

The dynamic range of the auditory system decreases with decreasing frequency. This compression can be seen in the equal-loudness-level contours, and it implies that a slight increase in level can change the perceived loudness from barely audible, to loud. Combined with the natural spread in thresholds within a population, it may have the effect that a very low-frequency sound which is inaudible to some people may be loud to others.

One study has suggested that infrasound may cause feelings of awe or fear in humans. It also was suggested that since it is not consciously perceived, it may make people feel vaguely that odd or supernatural events are taking place.[31]

Infrasonic 17 Hz tone experiment

On 31 May 2003, a group of  United Kingdom researchers held a mass experiment where they exposed some 700 people to music laced with soft 17 Hz sine waves played at a level described as "near the edge of hearing", produced by an extra-long-stroke subwoofer mounted two-thirds of the way from the end of a seven-meter-long plastic sewer pipe. The experimental concert (entitled Infrasonic) took place in the Purcell Room over the course of two performances, each consisting of four musical pieces. Two of the pieces in each concert had 17 Hz tones played underneath. In the second concert, the pieces that were to carry a 17 Hz undertone were swapped so that test results would not focus on any specific musical piece. The participants were not told which pieces included the low-level 17 Hz near-infrasonic tone. The presence of the tone resulted in a significant number (22%) of respondents reporting anxiety, uneasiness, extreme sorrow, nervous feelings of revulsion or fear, chills down the spine, and feelings of pressure on the chest.[32][33] In presenting the evidence to British Association for the Advancement of Science, Professor Richard Wiseman said, "These results suggest that low frequency sound can cause people to have unusual experiences even though they cannot consciously detect infrasound. Some scientists have suggested that this level of sound may be present at some allegedly haunted sites and so cause people to have odd sensations that they attribute to a ghost—our findings support these ideas."[31]

Suggested relationship to ghost sightings

Research by Vic Tandy, a lecturer at Coventry University, suggested that an infrasonic signal of 19 Hz might be responsible for some ghost sightings. Tandy was working late one night alone in a supposedly haunted laboratory at Warwick, when he felt very anxious and could detect a grey blob out of the corner of his eye. When Tandy turned to face the grey blob, there was nothing.

The following day, Tandy was working on his fencing foil, with the handle held in a vise. Although there was nothing touching it, the blade started to vibrate wildly. Further investigation led Tandy to discover that the extractor fan in the lab was emitting a frequency of 18.98 Hz, very close to the resonant frequency of the eye given as 18 Hz by NASA.[34] This was why Tandy had seen a ghostly figure—it was an optical illusion caused by his eyeballs resonating. The room was exactly half a wavelength in length, and the desk was in the centre, thus causing a standing wave which caused the vibration of the foil.[35]

Tandy investigated this phenomenon further and wrote a paper entitled The Ghost in the Machine.[36] Tandy carried out a number of investigations at various sites believed to be haunted, including the basement of the Tourist Information Bureau next to Coventry Cathedral[37][38] and Edinburgh Castle.[39][40]

See also

References

  1. ^ Wired Article, The Sound of Silence by John Geirland. 2006.
  2. ^ "Gavreau", in Lost Science by Gerry Vassilatos. Signals, 1999. ISBN 0-932813-75-5
  3. ^ *Gavreau V., Infra Sons: Générateurs, Détecteurs, Propriétés physiques, Effets biologiques, in: Acustica, Vel .17, No. 1 (1966), p.1–10
  4. ^ Gavreau V.,infrasound,in: Science journal 4(1) 1968,S.33
  5. ^ Gavreau V., "Sons graves intenses et infrasons" in: Scientific Progress – la Nature (Sept. 1968) p. 336–344
  6. ^ Garces, M. (2003). "Observations of surf infrasound in Hawai'i". Geophysical Research Letters. 30 (24): 2264. Bibcode:2003GeoRL..30xOCE5G. doi:10.1029/2003GL018614. Retrieved 15 December 2007. Comparison of ocean buoy measurements with infrasonic array data collected during the epic winter of 2002–2003 shows a clear relationship between breaking ocean wave height and infrasonic signal levels. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  7. ^ Garces, M. (2006). "Modeling and Characterization of Microbarom Signals in the Pacific". Retrieved 24 November 2007. Naturally occurring sources of infrasound include (but are not limited to) severe weather, volcanoes, bolides, earthquakes, mountain waves, surf, and, the focus of this research, nonlinear ocean wave interactions. {{cite journal}}: Cite journal requires |journal= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  8. ^ Haak, Hein (1 September 2006). "Probing the Atmosphere with Infrasound : Infrasound as a tool" (PDF). CTBT: Synergies with Science, 1996–2006 and Beyond. Preparatory Commission for the Comprehensive Nuclear-Test-Ban Treaty Organization. Archived from the original (PDF) on 2 July 2007. Retrieved 24 November 2007.
  9. ^ "Microbaroms". Infrasonic Signals. University of Alaska Fairbanks, Geophysical Institute, Infrasound Research Group. Retrieved 22 November 2007. The ubiquitous five-second-period infrasonic signals called "microbaroms", which are generated by standing sea waves in marine storms, are the cause of the low-level natural-infrasound background in the passband from 0.02 to 10 Hz.
  10. ^ "NOAA ESRL Infrasonics Program". Retrieved 10 April 2012.
  11. ^ Chen, C.H., ed. (2007). Signal and Image Processing for Remote Sensing. Boca Raton: CRC. p. 33. ISBN 0-8493-5091-3.
  12. ^ Paul Harper (20 February 2013). "Meteor explosion largest infrasound recorded". The New Zealand Herald. APN Holdings NZ. Retrieved 31 March 2013.
  13. ^ Katharine B. Payne, William R. Langbauer, Elizabeth M. Thomas: Infrasonic calls of the Asian elephant (Elephas maximus), Behavioral Ecology and Sociobiology, Volume 18, Number 4, pp. 297–301, 1986, doi:10.1007/BF00300007
  14. ^ William E. Barklow: Low‐frequency sounds and amphibious communication in Hippopotamus amphibious, Journal of the Acoustical Society of America, Volume 115, Issue 5, pp. 2555–2555 (2004)
  15. ^ E.K. von Muggenthaler, J.W. Stoughton, J.C. Daniel, Jr.: Infrasound from the rhinocerotidae, from O.A. Ryder (1993): Rhinoceros biology and conservation: Proceedings of an international conference, San Diego, U.S.A. San Diego, Zoological Society
  16. ^ a b E. von Muggenthaler, P. Reinhart, B. Lympany, R.D. Craft: Songlike vocalizations from the Sumatran Rhinoceros (Dicerorhinos sumatrensis), Acoustic Research Letters ARLO 4(3), July 2003, pp. 83–88, DOI 10.1121/1.1588271. Also cited by: West Marrin: Infrasonic signals in the environment, Acoustics 2004 Conference
  17. ^ E. von Muggenthaler, C. Baes, D. Hill, R. Fulk, A. Lee: Infrasound and low frequency vocalizations from the giraffe; Helmholtz resonance in biology, proceedings of Riverbanks Consortium on biology and behavior, 1999. Also work by Muggenthaler et al cited by Nicole Herget: Giraffes, Living Wild, Creative Education, 2009, ISBN 978-1-58341-654-9, p. 38
  18. ^ E. Von Muggenthaler: Infrasound from the okapi, invited presentation, student competition award, proceedings from the 1992 American Association for the Advancement of Science (A.A.A.S) 158th conference, 1992
  19. ^ Work by Muggenthaler et al, also referred to in: The Secret Of A Tiger's Roar, ScienceDaily, 1 December 2000, American Institute of Physics, Inside Science News Service (1 December 2000), Retrieved 25 December 2011
  20. ^ Von Muggenthaler, E., Perera, D. (2002), The cat's purr: a healing mechanism?, In review, presented 142nd Acoustical Society of America International Conference, 2001.
  21. ^ Work by Muggenthaler et al, referred to in: David Harrison: Revealed: how purrs are secret to cats' nine lives, The Telegraph, 18 March 2001, Retrieved 25 December 2011
  22. ^ von Muggenthaler, (2006) The Felid Purr: A Biomechanical Healing Mechanism, Proceedings from he 12th International Low Frequency Noise and Vibration Conference, p. 189-208
  23. ^ Goddard Space Flight Center
  24. ^ Elizabeth Malone, Zina Deretsky: After the tsunami, Special Report, National Science Foundation, version of 12 July 2008, downloaded 26 December 2011
  25. ^ "How did animals survive the tsunami?" Christine Kenneally, 30 December 2004. Slate Magazine
  26. ^ Nature. Can Animals Predict Disaster? – PBS: posted November 2005.
  27. ^ Langbauer, W.R.; Payne, K.B.; Charif, R.A.; Rapaport, L.; Osborn, F. (1991). "African elephants respond to distant playbacks of low-frequency conspecific calls" (PDF). The Journal of Experimental Biology. 157 (1): 35–46. Retrieved 27 May 2009.
  28. ^ Larom, D.; Garstang, M.; Payne, K.; Raspet, R.; Lindeque, M. (1997). "The influence of surface atmospheric conditions on the range and area reached by animal vocalizations" (PDF). The Journal of Experimental Biology. 200 (3): 421–431. Retrieved 27 May 2009.
  29. ^ Knight, Kathryn (2013). Disappearing homing pigeon mystery solved. The Company of Biologists. Retrieved 2013-01-31
  30. ^ Olson, Harry F. (1967). Music, Physics and Engineering. Dover Publications. p. 249. ISBN 0-486-21769-8.
  31. ^ a b "Infrasound linked to spooky effects". MSNBC. 7 September 2007. Retrieved 27 January 2010.
  32. ^ Infrasonic concert, Purcell Room, London, 31 May 2003, sponsored by the sciart Consortium with additional support by the National Physical Laboratory (NPL)
  33. ^ Sounds like terror in the air Sydney Morning Herald, 9 September 2003.
  34. ^ NASA Technical Report 19770013810
  35. ^ infrasound
  36. ^ Tandy, V.; Lawrence, T. (1998). "The ghost in the machine" (PDF). Journal of the Society for Psychical Research. 62 (851): 360–364. {{cite journal}}: Unknown parameter |month= ignored (help)
  37. ^ Tandy, V. (2000). "Something in the cellar" (PDF). Journal of the Society for Psychical Research. 64.3 (860). {{cite journal}}: Unknown parameter |month= ignored (help)
  38. ^ Arnot, Chris (11 July 2000). "Ghost buster". The Guardian. London. Retrieved 5 May 2010.
  39. ^ Who ya gonna call? Vic Tandy! – Coventry Telegraph
  40. ^ Internet Archive Wayback Machine. 2007 version of Vic Tandy's Ghost Experiment webpage
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