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Fh-polis,suchasgeophysicalsurveyingforoilaiuoproduderwatersound.Inthese,asmallcavityischargedwithpressedairandarelayreleasesthepressuresuddenly,rapidlyfalargeairbubbleandanapanyingburstofsound.Thepulsefrequencyisaround20Hzto200Hzaudeisveryhigh(probablythe‘loudest’man-madesourtheoexglargeexplosioravelsthroughtheseabedasfromtheiweentherocklayersbel(upto10km)arraysofhydrophoowedhesurfaagetherefled,asareprocessedbyputerstoprovideathree-dimensionalmap.
Thoughprojectorsareinprihydrophoheirphysiisofte.OwidelyusedtypesistheTonpilz(Germanfmushroom’)transduwhichseveralpiezoelectricPZTdisdwichedbetweeomakeastackwhichisterminatedbyaicalordricalheadmass,thebusiheprojepilztransdugeefrequehe2kHzte.
Formaerapplis,ingsignallinganddistang,direalsoundsarerequired.Justasinair,asoundsourcewillbenaturallydirealifthesouproduceshavesmallerwavelengthstharansducerface.Butbecausethevelocityofsoundisaboutfivetimesgreaterihaninair,thewavelengthdingtoaparticularfrequencyisalsoaboutfivetimesgreaterthanitsairbor,sodirealityishardertoeby.
&waytomakeadirealsouheparametricarray.Iftwoseewaveswhichdifflerjustalittleihehatdifflerencywillbeprodugwithotherswhosefrequehoseofthesources.Thewavelengthofthedifflerencewavebeaslongasrequired,butitmaiionalityofitsparent>
Parametricarraysexploitthefactthatsouydepehighsouhepressureintheesverylarge,ingdensitysignifidthereforebrieffyspeedingupthesouhereversehappeioofthesevelogesistodistortthewavefromitsusualsinusoidalform.
Thisisaoinhigh-powerultrasound,too.AsAugusteFouriershowed,anon-sinusoidalwaveisequivalenttoasumofposinusoids.Iheparametricarray,theseposiheiherwiththesumanddifflerehedifflereheo.Parametricarraysalsobeusedinair,tomakeaudio-frequenoredireal.
Althoughthereislittlethateleagicradiationdoesabovewaterthatsoundotdobelowit,soundhasoneunavoidabledisadvasvelowaterismuchlowerthanthaticradiationinair,whisthatsgtakesfarlonger.Also,whenwavesareusedtosenddata,therateofthatdatatransmissiolyproportionaltothewavefrequendaudiosoundwavesarearound1,000timeslowerihanradiowaves.Forthisreasonultrasouead,sisfrequechthoseofradiowaves.Aageisthatitiseasiertoproducediresatultrasoosendthesignaliionyouwant.However,adisadvaabsorptiohsouheraed.
Soundsworldwide
&ancesoverwhidtraveluerareamazing.Itisbelievedthatbeforetheproliferationofengine-poweredvessels,AntarcticwhalescouldbeheardbytheirArctis.Suchvastrangesarepossiblepartlybedwavesareabsorbedfarlessihaninair.At1kHz,absorptionisabout5dBkminair(at30perthumidity)butonly0.06dBkmier.Also,uersoundwavesaremuchmoreed;anoisemadeinmid-airspreadsiions,butihebedandthesurfacelimitverticalspreading.
Box11
Souyihemostacs1)equationistheLeroyRobinsonformula:c=1402.5+5T-0.0544T2+0.00021T3+1.33S-0.0123ST+0.000087ST2+0.0156Z+0.000000255Z2-0.0000000000073Z3+0.0000012(Φ-45)-0.00000000000095TZ3+0.0000003T2Z+0.0000143SZ;Ttemperature(°ity(pert),Zdepth(metres),Φlatitude(degrees).
Therangeofsouiesuerisfarlargerthaninair,becauseoftheenormousvariatioy,whichisaffectedbytemperature,pressure,andsalinity(Box11).Levelsatwhidvelogesrapidlywithtemperaturearecalledthermodtheyfolloatterninmostseas:wheheriscalm,theuppermostlayeroftheseaischaracterizedbyarapidfalliure,andhendvelocity,withdepth.Becauseditionsaremoreer,thisisknownastheseasonalthermoe.Belowthisisthemainthermoe,wherethetemperatureandsouyuetofallwithdepth,iofseason.Atthebaseofthemainthermoe(thedepthofwhichvariesgreatlywithlatitude),asteadytemperatureofaround4°Cisreadhardlygesatdeeperlevels.Ihermallayer,pressurebeesthedominantfadeterminingsouy—whisequehdepth,asshowninFigure22.
22.Uersouyprofile.
Sosomewhereunderallosthereisalayeratwhidvelocityislow,saweenregionsinwhichitishigher.Byrefra,soundwavesfrombothaboveandbelowaredivertedtowardstheregionofminimumsouy,arappedthere.Thisisthedeepsouhinsphericalshellextendingthroughtheworld’sos.
Sindwavesinthedeepsoundelmoveonlyhorizontally,theiriyfallsinproportionoaravel,ratherthantothesquareofthedistaheywouldinairoriasiure(inotherwords,theyspreadoutispheres).Soundabsorptioninthedeepsoundelisverylow(itisstronglyfreque,butaround0.2dBperkmfor4kHzwaves),andsouhedeepelreadilyavigatetheEarth.
ThedeepsoundelloitedtosetuptheSOFAR(soundfixingandranging)system,whiitiatedin1960bytheAustralia-BermudaSoundTransmissio,inwhichexplosioofflnearHeardIslandintheIhecoastofAustralia.TheyweredeteBermuda,atadistan.AedsoundwasdiscoveredbytheSOFARreseardlateridehecallsoffinteraphysalus),wholongagodiscoveredtheexistendpropertiesofthedeepsounddregularlyvisitittosigantkin.
SOFARopeotheATOC(AcoustietryofOClimate)system,whichcalculatesglobalseatemperaturesbymeasuringaveragesouyes,thushelpingtoquantifyclimateges.
gweathercausesgseas,whichleadteoftemporaryacousticstatesoftheogshadowzonesfromwhichmostsoundisexdtemporarysoundels,whichallowlong-distaion.Soundswhichtraveldower,likethosewhichtravelaroundthedeepshlydistortedeothemanygesofvelotheirjoururntovariatioureandsalinity).Inthe1990s,variesoundsofunknin(theBloopisperhapsthebestkeofimagierpretations,ineliterallymonstrousohemostlikelysourceisthegreatlymodifiedsoundsofdistanticebergsg.
&hsounds
Souravelreadilyinsolids(seeBox12),asdopressurewavesofotherkinds.Butnotallseismicwavesaresound(forprimary)wavesarelongitudinal:theyaresequenpressionsaioyisdetermiyayoftheground,andthereforearesound>
However,S(sedary)waves,beingtrasouhPandSwavesarebodywaves—theytravelthroughtheEarth,andtheirrefrabythelayersundergrouhinformationaboutourplaructure.Therearealsoavarietyofsurfaceseismicwaves,butnonearesound>
Manylargeanimalsmakeandhearlow-frequends.ThesoundsmakebyAfrielephantsarelowsimplybecausetheirvocalceaivelyslow-moving—somueoftheircallsareinfrasonic.Thisisofsiderableadvahemsinfrasoundtravelsfarwithlittleattenuation(inair,veryroughly,a10Hzsignaltravelsoimesfurtherthana100Hzone,and10,000timesfurthertha1,000Hz).
Undergrouionishighlyvariable,butusuallymuchlowerthaninair:femaleelephantsuseinfrasoundstoattractmales(over3kmawaybyairorover1round)andtotacttheiryousalsouseinfrasouhuorms(ausefulwatersource)over500kmaway.In2004,SriLasffedthecoast,probablybecausetheydetectedtheinfrasoundsoftheoningtsusgeheirsigherbymakingrumblingsoundsorbystampi,whichalsodeted-bornesoundusingvibratioorscalledPacorpuscles.
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