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EnvironmentalScience
Brewer 1
ES2.1:TheThinBlueBlanket
atmosphere:amixtureagasesthatsurroundstheplanetEarth.
78%nitrogen
21%oxygen
theatmosphereisheldtotheEarthbytheforceofgravity.
DuetothesmallermassofplanetslikeMercury,lessatmospherecanbeheldinplace.
Thinneratmospheremeanslessinsulation.
Therefore,Mercuryhasgreatertemperatureextremes(840to275Fahrenheit)
EnvironmentalScience
Brewer 2
ES2.1:TheThinBlueBlanket
ConsidertheplanetVenus
approximatelythesamesizeandmassasEarth
96%oftheatmosphereiscomposedofthegreenhousegascarbondioxide.
temperaturesareneverbelow750Fahrenheit
ConsiderUranus
gasgiantwiththickcloudsofdeadlymethanegas
temperaturesaverage360Fahrenheit
NotehowmuchlargerUranusisthantheEarth.
WhateffectwouldtherelativesizeofUranushaveonthetotalatmosphereoftheplanet?
EnvironmentalScience
Brewer 3
ES2.1:TheThinBlueBlanket
TherelativethicknessoftheEarth'satmospheretotherestoftheEarthcanbecomparedtotheskinofanapplecomparedtotherestofanapple
EnvironmentalScience
Brewer 4
ES2.1:TheThinBlueBlanket
TheEarth'satmospherebecomesthinnerwithincreasingelevation.
Thisisduetoadecreaseintheforceofgravitywithincreasingdistancefromacenterofmass(i.e.centeroftheEarth)
mountainclimberw/O2tank
warmclothingduetolowtemperaturescausedbythinningatmosphere
EnvironmentalScience
Brewer 5
ES2.1:TheThinBlueBlanket
TheOzoneShieldaNaturalSunscreen
Recallapproximately21%oftheatmosphereisO2
O2moleculescanbesplitbyultravioletlightandlightning.
ThesefreeOatomsthencombinewithotherO2moleculestoformozone,O3
MoleculeBuildingactivity
EnvironmentalScience
Brewer 6
EnvironmentalScience
Brewer 7
ES2.1:TheThinBlueBlanket
TheOzoneShieldaNaturalSunscreen
Ozoneismeasureinpartspermillion(ppm)byvolume
Thecycleofozonecreation(UVlight)anddestruction(nitricoxide)iscontinuousandnatural.
OzoneformationdependsontheamountofUVlightandtemperature
Equilibriumisachievedwhentherateofcreationequalstherateofdestructionofozone.
Ozonedepletionoccurswhentherateofdestructionisgreaterthanthatofcreation.
EnvironmentalScience
Brewer 8
ES2.1:TheThinBlueBlanket
CFCsTheRisksandBenefitsofTechnology
Beginninginthe1970's,scientistsbegantostudytheeffectofchemicalsproducedbyhumanactivitiesontheozoneshield
PaulCrutzendiscoveredthatnitrogenoxidesfromsupersonicjetscoulddamagetheozonelayer.
EnvironmentalScience
Brewer 9
ES2.1:TheThinBlueBlanket
chlorofluorocarbons(CFC's):compoundscontainingcarbon,fluorine,andchlorinethatcandestroytheozonelayer
WhenCFCsmeetOzone.mpeg
CharacteristicsofCFC's:1)nontoxic2)nonflammable3)inexpensivetoproduce
Usedasareplacementcoolantinrefrigeratorsandairconditionersbecausethemethylchlorideusedwastoxic.
Extremelystableinthetroposphere,whereUVlightsplitschlorinefromCFC's.AsingleClatomcanthendestroy100,000ozonemolecules.
CFC'seventuallyreturntotheloweratmosphereandarewashedoutbyrain.
SMART Notebook
EnvironmentalScience
Brewer 10
ES2.1:TheThinBlueBlanket
OzoneReactions
FormationofOzone
O2+UVlight>O+O
O+O+2O2+catalyst>2O3
Net:3O2>2O3
NaturalDestructionofOzone
O3+NO>O2+NO2
O3+UVlight>O2+O
NO2+O>NO+O2
Net:2O3>3O2
OzoneAccumulation
3O2>2O3
3O2
EnvironmentalScience
Brewer 11
CFC'sAttackonOzoneReaction
CFCl3+UVlight>CFCl2+Cl
Cl+O3>ClO+O2
O3+UVlight>O2+O
ClO+O>Cl+O2
Cl+O3>ClO+O2
Result2O3>3O2
EnvironmentalScience
Brewer 12
ES2.1:TheThinBlueBlanket
BiologicalEffects
OzoneprotectslifefromharmfulUV(blacklight)
UVtypes(bywavelength)
UVA:necessaryforsynthesisofvitaminDintheskin
UVB:causesagingoftheskin,skincancers,cataracts,andmayimpairimmunesystemresponse
notnecessaryforphotosynthesis,andcanbeharmfultoplantsandmicrobes
plantsbecomemoresusceptibletoinsectsandpathogens
UVC:mostdeadlyformofUV,butabsorbedbyozoneandoxygeninatmosphere
EnvironmentalScience
Brewer 13
ES2.1:TheThinBlueBlanket
BiologicalEffects
CO2,H2O,nutrientsandheatarefactorsinhowmucheffectUVradiationwillhaveonplants
UVmayalsoreducetherateofphotosynthesisofphytoplanktonintheocean.
FrogeggsandcoralreefsarealsosensitivetoUVlightandinterfereswiththeirdevelopment.
Marineecosystemsnearthepolesexperiencethegreatesteffects.
EnvironmentalScience
Brewer 14
ES2.1:TheThinBlueBlanket
WarningNotHeeded
ScientistsfirstdiscoveredthelinkbetweenCFC'sandozonedepletionin1974.
In1977theU.S.,Canada,andothersbannedtheuseofCFC'sinaerosols
Althoughothersourcesexistedatthattime,industrylobbyistsenticedpoliticianstoallowindustrialuseofCFC's.
Presently,theozoneisbeingdestroyedatafasterratethanitisbeingproduced.
OzonedepletionisgreatestoverAntarctica.Duringthespring,Antarctica'suniqueweatherpatterns furtherthedepletion.
Contrarytopopularbelief,thereisnophysical"hole"intheozonerather,theozonelayerisverythinintheseregions.
EnvironmentalScience
Brewer 15
ES2.1:TheThinBlueBlanket
TheMontrealProtocol
ThemajorcauseofozonedestructionischlorinefromCFC's
Solutions:
1.StopproductionofCFC's
2.PreventthereleaseofCFC'sintheatmosphere
ProtocolnowseekstotaleliminationofCFC's
Theglobalnatureofozonerequiresinternationalcooperationinordertoprovideprotection
Ozonewillnotreturntopre1980levelsuntil2065.
EnvironmentalScience
Brewer 16
ES2.1:TheThinBlueBlanket
FindingAlternatives
CFC'sarebannedinindustrializedcountries
exceptions:whennootheroptionisavailable
DevelopingcountriesstilluseCFC's
RecycledCFC'scanbeusedforequipment
HighcostofreplacementsencouragesillegaluseofCFC's
HCFC'sarelessstableandfewermoleculesreachtheatmosphere
productionmuststopby2030
replacementchemicalmustbe:
1.nonflammable
2.noncorrosive
3.lowtoxicity
4.reasonablypriced
Halonsareusedinfireexstinguishers
replacementbyCO2
CO2onlyworksforcertainkindsoffires
CO2weighsmore(impracticalforairplanes)
HCFCmolecule
CFCmolecule
EnvironmentalScience
Brewer 17
ES2.1:TheThinBlueBlanket
WhatYouCanDo
Recycleyourrefrigerants(don'tforgetyourcar)
Avoidthesunbetween10and3
UsesunscreenthatblocksUVAandUVB
WearsunglassesthatblockUVradiation
Attachments
WhenCFCsmeetOzone.mpeg
SMART Notebook
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