air pollution episodes (3)

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    AIR POLLUTIONEPISODES

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    DISEASE OFWEALTH

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    EPISODES• EPISODE – used as a refned orm o

    the word disaster/ incident.

    Indeed it was the shoc o these disastersthat stimu!ated the frst modern!e"is!ati#e action to contro! o air$o!!utants.

    • %are u! stud& o di'erent nown e$isodesre#ea! that a!! o the incidents hadsomethin" in common.

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    AIR POLLUTIONEPISODES

    • CRUCIAL INGREDIENTS FOR ANEPISODE TO HAPPEN:

    – Lar"e num(er o $o$u!ation sources – A restricted air #o!ume – Fai!ure o o)cia!s to reco"ni*e that

    an&thin" is wron" – The $resence o water dro$!ets o

    the ri"ht si*eSource+ ,o!dsmith - 0

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    AIR POLLUTIONEPISODES

    Major air pollution episo es !"HO#$%&$' Donora#

    $%()Lon on# $%*+

    1o$u!ation -23455 035553555Weather Antic&c!one

    in#ersion ando"

    Antic&c!one

    in#ersion ando"

    To$o"ra$h& 6i#er #a!!e& 6i#er $!ain

    7ost $ro(a(!esource o Industr&stee! and *inc Househo!d andcoa! (urnin

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    Major air pollution episo es !"HO#

    $%&$' Donora# $%() Lon on# $%*+8ature o

    i!!nesses

    %hemica! irritationo e9$osedmem(ranoussur aces

    %hemica!irritation oe9$osedmem(ranoussur aces

    : o deaths -;

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    FOG – o" dro$!ets o the ri"ht si*e3 inthe - to 2 μm diameter or in the range below0.5 μm is one of the most crucial element in air

    pollution episodes.

    AIR POLLUTIONEPISODES

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    • An >in#ersion? occurs when a sectiono the atmos$here (ecomes warmeras the e!e#ation increases.

    In,ersion La-ersIn,ersion La-ers

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    Air@conditioneris usua!!&

    insta!!ed hi"h

    on the wa!!

    immersionheater is f9ed

    near the(ottom

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    In a fre3 wh& shou!d &ou craw! c!ose tothe oor in a smo e@f!!ed roomB

    Smo e is warmer than the surroundin" air.

    It rises C its $!aceswou!d (e re$!aced (&the surroundin"coo!er air.

    Smo e

    is to9ic.

    We shou!d craw! c!ose

    to the oor to $re#entsmo e inha!ation.

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    • On a sma!!er sca!e nearcoast!ines3 con#ection isres$onsi(!e or sea (ree*es.

    • Durin" the da&time3 !and is

    much hotter than the ocean.• A sea (ree*e is created

    when hot air o#er the !andrises due to con#ection andis re$!aced (& coo!er air

    rom the ocean.• At ni"ht the tem$erature

    re#erses so a !and (ree*e

    CON.ECTION

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    7uch o the Earth s c!imate is re"u!ated (& "iantcon#ection currents in the ocean.

    CON.ECTION

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    At/osp0eri1 pressure !/illi2ars'3 +33 (33 &33 )33 $#333$+3

    $$3

    $33%3

    )3

    43

    &3

    *3

    (3

    53+3

    $3

    3!SeaLe,el'

    6)3 6(3 3 (3 )3 $+3Pressure 7 $#333

    /illi2ars at8roun le,elTe/perature !9C'

    A l t i t u

    e

    ! : i l o / e

    t e r s

    '

    A l t i t u

    e ! /

    i l e s '

    4*

    &*

    **

    (*

    5*

    +*

    $*

    *

    T0er/osp0ere

    Heatin8 ,ia o;one

    Mesosp0ere

    Stratosp0ere

    O;one ro/ t0e eart0

    Troposp0ere

    Te/peraturePressure

    Hi80li80ts:

    1ressure decreaseswith a!titude unti! itreaches *ero

    Tro$os$here is the!a&er we !i#e inmost!& 8 and Oweather co!der as&ou "o u$

    Stratos$here+ has theo*one !a&er warmeras &ou "o u$

    En#ironmenta! science

    ocuses most!& onthose two !a&ers

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    "ar/er air

    In,ersion la-er

    Cool la-er

    MountaiMountain

    .alle-

    De1reasin8 te/perature

    I n 1 r e a s i n 8 a

    l t i t u

    e

    Tem$erature In#ersion

    Tra$s $o!!utants near sur ace. 7ountains $re#ent

    wind in area and shadow sun to ee$ !ower air coo!.

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    In,ersion la-er

    Mountainran8e

    Sea 2ree;e

    Des1en in8 ?ar/ air /ass

    De1reasin8 te/perature

    I n 1 r e a s i n 8 a

    l t i t u

    e

    Tem$erature In#ersion

    Tra$s $o!!utants near sur ace. 7ountains $re#ent

    $o!!utants !ea#in". Sea (ree*e (!ows in3 not out.

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    Marine In,ersionMarine In,ersion

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    Re8ional Su2si en1eRe8ional Su2si en1eIn,ersionIn,ersion

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    Hi80 Pressure In,ersionHi80 Pressure In,ersion

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    ORIGIN AND FATE OF AIRPOLLUTANTS

    CAR@ON MONO IDE @Incom$!ete com(ustion o car(on

    @8atura! anaero(ic decom$osition ocar(onaceous materia!s (& mo s@Anthro$o"enic sources #ehic!es3

    ossi! ue! (urnin"3 industria!$rocesses3 $ower $!ants3 so!id wastedis$osa!3 misce!!aneous (urnin"sG

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    HABARDOUS AIR POLLUTANTS!HAPs'@Fue! com(ustion3 7eta! $rocessin"@$etro!eum/natura! "as s&nthesis

    @refnin"3 sur ace coatin" $rocesses@Waste treatment dis$osa!s3 e!ectro$!atin"@A"ricu!tura! chemica! $roduction

    @1o!&mer/resin $roduction3 Dr& c!eanin"

    @Atmos$heric trans ormation

    ORIGIN AND FATE OF AIRPOLLUTANTS

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    P0otol-sis – the chemica!ra"mentation or rearran"ement o a

    chemica! u$on adsor$tion o radiationo the a$$ro$riate wa#e!en"th.

    ORIGIN AND FATE OF AIRPOLLUTANTS

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    LEAD@o!canic acti#it&@Air(orne soi!@Sme!ters3 refnin" $rocesses@Incineration

    SULFUR O IDES@1ower $!ants3 industr&3 #o!canic eru$tions@Ocean aeroso!s3 com(ustion o ossi! ue!s

    ORIGIN AND FATE OF AIRPOLLUTANTS

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    NITROGEN DIO IDE@=acteria! action@%om(ustion $rocesses

    PHOTOCHEMICAL O IDANTS@Atmos$heric reactions secondar& $o!!utantG

    PARTICULATES@Sea sa!t3 soi! dust3 #o!canic $artic!es3 orestfres

    @Anthro$o"enic sources

    ORIGIN AND FATE OF AIRPOLLUTANTS

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    An I!!inois coa! is (urned at a rate o-.55 " $er second. I the ana!&sis o

    the coa! re#ea!s a su! ur content o 4.553 what is the annua! rate o emission

    o SO 2 B

    Su! ur in

    Su! ur

    dio9ideSO2G

    Su! urdio9ide

    ashG

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    MASS @ALANCE:S in J S ash K S SO2

    S in J - "/s 9 5.545 J 5.545 "/s

    S in J .< 9 -5 "/&r

    S ash J 5.5 G .< 9 -5 "/&rG J

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    Determine whether or not a $u!#eri*ed coa!3dr& (ottom3 wa!!@fred (oi!er usin" (ituminous

    coa! at $ower $!ant rate at - 7W meets the8S1S or SO 23 $articu!ate matter3 and 8O 9.

    The $ower $!ant (urns (ituminous coa! with asu! ur content o -.0 and ash content o .2

    . The coa! has a heatin" #a!ue o -

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    %oa! frin" rate J - 7W / 5.4 J -;

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    C0e1 e/ission rate:Estimated SO 2 emission rate

    J 0.< !(/ton coa! . 9 -50

    =tuG - ton/2555!(G5.- G -

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    %hec the $articu!ate emission rate+Msin" the E1A emission actor o -5A or a

    $u!#eri*ed coa!3 dr& (ottom3 wa!!@fred (oi!er+Mncontro!!ed $articu!ate emission

    J -5G .2G J 2.5 !(/ton coa! (urned

    Estimated $articu!ate emission with contro!J 2.5 !(/ton coa! . 9 -5 0 =tuG - ton/2555!(G

    5.5-G -

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    1articu!ate emission rate $er mi!!ion =tuJ -4.2 !(/ . 9 -5 0 =tuG -5 GJ 5.522 !(/ -5 =tu

    %omment+

    meets the standard o 5.54 !(/-5 =tu%hec the 8O9 emission rate+Msin" the E1A emission actor o 22 !(/ton3

    Estimated emission rateJ 22.5 !(/ton coa! . 9 -5 0 =tuG - ton/2555!(G -

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    Estimated emission rateJ < ;. !(/ . 9 -5 0 =tuJ ;.0 9 -5 @; !(/=tuJ 5.; !(/ -5 / =tu

    %omment+-.The standard or (ituminous coa! is5. 5 !(/-5 / =tu. The $ower $!ant does

    not meet the 8O P standard.

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    6ecommendations+-. The su(stitution o su(@(ituminousor !i"nite coa! or the (ituminous coa!2. 7odifcation o (urner.

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    6eaction 1a$er6eaction 1a$er• What did we !earn rom theWhat did we !earn rom the

    e$isodesBe$isodesB•

    What s di'erent with Donora andWhat s di'erent with Donora andLondon with then and nowBLondon with then and nowB• What made the e$isode ha$$enWhat made the e$isode ha$$en

    (e oreB(e oreB• What ma es us certain it won tWhat ma es us certain it won t

    ha$$en a"ainBha$$en a"ainB

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    A M R T OI @ L C T

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    A M R T OI @ L C T

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    A M G N OI " L R T