Ca rbo ny l c o
m
po u nds e xist in air, wate r, fo od, b iolog ic al f lui ds a nd tis s u e s, a sw el l a sn o nb iolog ic al
m
ate rials.M
a nym
ethods ha v eb
e e n de v eloped to dete ct c a rbo ny lc om
po u nds in theair,
i
n clud
ing n um
e r o u s de riv atizatio n r e age nts tom
ake c a rbo ny l c om po u nds more stab le,m
ulti p lee x tr a ctio n
m
ethods, a s wel l a sm
ultip le dete ctio n methods T he s em
ethods c a n be c o stl y a nd ti mec o n s u
m
ing, a nd als om
ake u s e of to x ic s olv e nts.W
e s o ug ht a quick a nd in e x pe n siv em
ethod to dete cta n
d
qu a nti f
y total
c a rb
o nyl
si
n air s am p le s, spe ci fi
c all
yd
ie s el e xh
a u st s am
p le s, a s w el l a se x tr a c el lula r
m
ed ia in b iolog ic al s am
p le s.W
ed
e riv atiz ed sta nda rd c arbo ny l c om
po u nds w ith 2,4 -d initr op he ny l h y dr a zin e
(
D N P H)
;hepta n e
w
a sm
o r e ef f icie nt th
a n pe nta n e o r he x a n e in e x tr a ctio n of the de riv ativ e s a nd le a v e s e x c e s sD N P H al
m
o st e ntir el y in the aqu e o u s p ha s e. To te st the u s efuln e s s of th is te chni qu e c a rbo ny ls fr om
1
^
d ie s el e xha u st we r e c ol le cted
o n Sep-Pak D N P H-S i l ic a c a rtrid
ge s, eluted, e x tr a cte
d
w ith
hepta n e,a n
d
a n alyz ed
b y spe ctr op hotometry a nd H P LC /
U V/
M
S.L in e a r r egr e s sio n a n al ysis ind ic ated a str o ng c o r r elatio n
(
0 9 8 2 1)
betw e e n the U V abs o rb
a n c e(
3 6 5 nm
)
of e a ch
s am
p le a nd
the totalm
a s s of
c a rbo ny l de riv ativ e s s epa r ated b y H P L C a nd
dete r
m
in edb
yM
S. T he u s efuln e s s of
th is te chniqu e wa s als o te sted o n a b iolog ic al s am p le. B E A S-2 B c el ls we r e e xpo s ed to d i f fe ring c o n c e ntr atio n s of r e si du al oi l fl y a sh
(
R O F A)
. U V ab
s o rba n c ein c r e a s ed w ith in c r e a sing R O F A c o n c e ntr atio n s, s ug ge sting that c a rbo ny l gr o ups
(
pr od
u cts of li
p id
pe r o xi datio n
)
in c r e a s ed w ith in c r e a sing c o n c e ntr atio n s of R O F A. T he s e r e s u lts ind ic ate that a quicka n
d i
n e xpe n siv em
ethod
tod
ete ct a nd
qu a ntify
total c a rbo ny ls in air s am
p le s, spe ci fi c al
l y d ie s ele xha u st s a
m
p le s, a s w el l a s e xtr a c el lula rm
edi
a inb
iolog ic al s am
p le s,m
ay be a ch ie v ed
thr o ug h thee xtr a ctio n of c a rbo ny l de riv ativ e s w it
h
hepta n e a nd s ub
s equ e nt dete cti
o n b y spe ctr op hotom
etry. InF
ir s
t, Iw
o ul d l i k
e to tha nkD
r .M
ic
h
a elM
ad d
e n fo r c o o rdin a
tin
g th
ef
ol
low i
ng pr oj
e ct.Dr.
M
ad d
e n ta ugh
tm
e s om
u ch m
o r e tha nI h
ad
e v e r a ntici p
ated l
e a r nin
gd
u ri
ng th
el
a st tw
oye a r s, a n
d w it
ho uth i
s pati
e n c e a nd
e v e rw i l l i
ngn e s s tod i
s c u s s r e s e a r ch d
e si
gn a nd
te ch
ni
c al
is s
ue s, Iw
o ul d
n oth
a v ele a r n e
d
th
e c ri
tic a
l
sk i l l
s ne c e s s a ry i
n c om p l
eting
s cie n
ti fi
c r e s e a r ch
.I
a
m
al
s o gr atef
ul
toD
r Lo uis e
Bal l f
o r al w
ays e n c our agi
ngm
e, a sw
el l
a s al w
aysb
rin
gi
n g as
m
il
e tom
y fa c e thr o u gh h
e rm
a n y sto rie s ToM
s Lis a
Dai l
y a nd
M
r s. Jole e n So uk
up, I am
e xtr eme
l
y ap pr e ci
ativ e
f
o r al l
of
th
eir e x
pe rti
s ein
h
el
pin
gm
e c om
pl
etem
y r e s e a r ch
e xpe ri m
e nts.I a
ls o
ow
e ad
eb
t of
gr atitud
e to Dr .W
i l l i
am
Vi
z u etef
o r s ow i l l i
n gl
y agr e ei
ng tob
e a r e ad
e r o nm
ym
a ste r s te ch
ni
c al
r epo rt c om m i
t te e.T o
m
ym
oth
e r,Su s a n
,m
yb
r oth
e r s B J a nd
M
a x , a nd m
y si
ste r Ol i
vi
a, tha nk
yo u al l f
o ryo u r c o n sta nt s up po rt a n
d
u n c o nd it
i
o n al l
o v e Tom
yf
ath
e r, Lo ui
s(
d
e c e a s ed
)
, th
a nk
yo uf
o rT
A
B L EO
F CO N
T E N T SPage
L I
ST
O
FT A
B L ES
vi i
L I
ST
O
F F IG
U R ES
vi i i
1
0
B AC
K G RO
UN
D9
L I
A
ir Pol lutio n 91.2 So u r c e s o
f A i
r Pol l
utio n 1 11.3
C
a rb
o nyl
sA
s a Com
po n e nt of A i
r Pol lu
ti
o n 13
1.
4 Oth
e rS
o u r c e s of
Ca rb
o ny ls 2 11.5 He a
l
th Ef f
e cts of A l d
eh
yd
e s 2 21.5. 1
F
o rm
al d
eh
yd
e 2 21
.5.2
A
c r ole
in
2
41.
5
.3
A
c etal d
eh
yd
e 25
1.
5
4Pr o
pi
o n al d
eh
yd
e 26
1.5 5 Ac eto n e 2
6
1.5.6 Be n z al
d
eh
yd
e 2 71 6
M
eth
od
s of
Dete cti
ngA i
rb
o r n e Al d
eh
yd
e s 2 71.
6
1R
e ag
e ntsb
a s ed
o n n itr o a r om
atic
h
yd
r a zin e s
2 71.6 2 1
-D i
m
eth y lam
in o n ap hthale n -5-s u
lf
o ny l d y dr a zi de 3 1
1
6 3
R
e age ntsb
a s ed
o nb
e n z o o x ad ia z o
le
str u ctu r e s 3 11 6.
4
2
-
d
i ph
e ny
la c e
tyl
- l ,3
-
i
nd
a nd io n e
-l
-h
y
d
r a z o n e(
DA
I H)
3 31.
6
.5
H
al
og
e n ated
a r om
ati
ch
yd
r a zi
n e r e age nts 3 41.
6
.6
0
-Al k
y
la
ted h
yd
r o x yl
am i
n e s34
2. 1
M
ate ria
l
s 3 82. 1. 1 B
i
o ch
em i
c als a nd
Re aga nts3 8
2.1.2
Pa r
ti
cl
eS
o u r c e a nd C
ol l
e cti
o n3 8
2.1.3 A n al ytic a
l
a nd
Expe ri m
e ntal
In str um
e nts 3 92
.1 4
I
n Vi
tr oE
xpo s u r e s3 9
2
.2
. Extr a cti
o nSo
lv e n
t V al i da
tio n
4 02
.3
En vi
r o nm
e ntal
Sam
pl
e Extr a ctio n s a
nd
An al
ysi
s 43
2
.4
Bi
ol
ogic a
l Sa
m
pl
e Extr a ctio
ns and A
n al
ysi
s 45
3
.0 R
ESU
L TS
4 7
3 1 Extr a ct
io n
of d i
n itr oph
e nyl h
yd
r a z o n e sb
yd
if f
e r e nt s olv e n
ts 4 73
.2 Extr a ctio n
a nd A
n al
ysi
s of G
a s e o u sD i
e s el
Exh
a u st54
3.3 Extr a ctio n a nd
A
n al ysis of B iolog ic al s am
p le 6 44
.0 D I SC U S SI
O N
AN D C O N C
LU S
IO N S
6
75.
0 R E
F E R EN C
ES
76
A
pp
e nd i
xA C h
e v r o n Ph i l l i
psC h
em ic a
l C
o ., Bo rge r, T
X
; 0 5 LS C
e rti f
i c ati
o n Fu el
, ty pe II
,s u
l f
u r c o nte nt ap pr o xi m
atel
y3
4 7 p pm
8 0A p
p
e nd i
x B : Ga s Ph
a s e a nd
PM
Pa r am
ete r s of D i
e s el
Exh
a u st af
te r 1:3 0 d i
lutio nw
ithh
um i d
ifi
ed
a nd
pu ri fi
ed
ai
r 8 1A
pp
e nd i
x C :Expe rim
e ntal
De si
gnf
o rD i
e s el
Exh
a u stSa
m p l
e Extr a ctio n s
8 2
A p
p
e nd i
x D Ind i
vi d
u al d i
ni
tr oph
e nylh y d
r a z o n em
ola r
c o ntri b
uti
on toU V
ab
s o rp ti
on8 4
A
p pe nd i
x E: S pe ctr oph
otom
etri
cA b
s o rb
a n c e(
3 6 5 nm
)
of
Sep-Pak DN
P H -Si l i
c a Ca rtrid
ge se x po s e
d
tod ie s e
l
e xh
a u st 8 7A p
p
e nd i
x F: Total
M
a s s of Ca r
b
o nyl
sin
Di
e s el
Exh
a u stC
ol l
e cted
o nD N P H C
a rtri d
ge s a nd
A
p pe nd ix G: Gr ub b
s' Te stf
o r Outli
e r s fo r Total Ca rbo ny lM
a s s 8 9A
pp
e nd i
xH
: Av e r age c o n c e ntr atio n
(
n=6
)
of
spe ci f
i c c a rb
o nyl
gr o upsf
o rSe
p-P
ak
DN
PH
-Si l i
c aCa rtri
d
ge s e xpo s ed
tod i
e s el
e xh
austf
o r 2h
our s a nd b l
a nk
, u ne xpo s ed Se
p-Pa
k
DN
PH
-S i l i
c ac a rtr
i d
ge s aft
e r s epa r ati
o nb
y H P L C,d
ete cti
o nb
yM
S, a nd
c o n c e ntr atio nd
e ri
v ati
o n via sta nd
a rd
c u r v e s
f
o r spe ci f
i c c arb
o nyl
s9 0
A
p pe nd
ix I:A
v e r age pe ak
a r e a(
n= 4)
of
spe ci f
i c c a rb
o nyl
s aft
e r H P L C s epa r ati
o n a nd
M
S
L I
ST
O
F TA
B L ES
T a
b le
1.3
. 1:M
ain
C
a rb
o nyl
Com
po u nd
s, B yC
o n c e ntr atio n
, InA m b ie n
t a nd
Ind
o o r air
2 0T a
b l
e 2 2 1 H P L C S ystem G
r ad i
e nt Pr ogr am
4 2Tab le 3 1. 1:
A
bs o rba n c e of a 3 X he x a n e e xtr a ctio n v e r s u s a 5X
he x a n e e xtr a ctio n of am
ixtu r e ofd i
ni
tr oph
e nyl h
yd
r a z o n e s 48
T a
b le
3
.1.2 U
V D ete ctio
n of
DN
PH A ft
e r Extr a ctio
nW
it
h
Pen tane o rH
epta n e 5 1T a
b le
3
.1.3
Com
pa ri
s o n of U
nd i l
uted A
E0 0
0 4 3 Sta nd
a rd
Extr a ctio n s of
Pe nta n e v e r s u s Hepta n eM
e a s u r ed b
yM
S
5 2
T a
b le
3.1.4 Ind iv
i d
u al d i
nit
r op
h
e nyl h
yd
r a z o n em
ola r c o n
tri b
uti
o n toU
V ab
s o rpti
o n5 3
T a
b le
3
2.1 Pe r c e nt of
Fo rm
al d
eh
yd
e a nd A
c etal d
eh
yd
e v e r s u s T otal C
a rb
o nyl
sM
e a s u r ed
60
T a
b le
3
2.2 A i
rb
o r n eC
o n c e ntr ati
o nin
D i
e s el
Exh
a u stC h
am
b
e r of S
pe ci f
i cA l d
eh
yd
e s u si
ng th
eL I S T
O
F F IG
UR
ES
F
i
gu r e 1.3 1: C hem
ic al Pha s e s of D ie s el
Exh
a u st a nd
Pr oporti
o n of
Ch
em
ic alsw i
thin
V ol
ati l
eOrga nic Ga s P ha s e 14
F
i
gu r e 1 6. 1.1 D e ri
v atiz ation of
c a rb
o ny l gr oups
w i
th
DN
P H 28
F
i
gu r e 1.6 1.2M
ole c u
la r s
tr u ctu r e of
ni
tr o a r om
ati
ch
yd
r a zin e s
p N
P H a nd
M
DN
P H 28
F i gu r e 1.6.2.1 D
N
S Hm
ole c ula r str u ctu r e 3 1F
i
gu r e1 6
.3
.1M
ole c u
la r
str u ctu r e of b
e n z o o x ad ia z o
le
b
a ck b
o n e3 2
F i
gu r e1
.6
.4
.1
M
ol
e c u la r str u ctu r e of DA
I H3 3
F
i
gu r e 1.6
.5 1M
ol
e c u la r str u ctu r e of
T C P H a nd
P F P H3 4
F
i g
u r e1
6.6. 1M
ole c u la rStr u c
tu r e of
P F B OA
3
5F i g
u r e2
.2. 1A
E 0 0 0 4 3 Sta nd
a rd C h
r om
atogr a
m
4 3
F i
gu r e3
.1
.1
:A
v e r age pe r c e nt e x tr a ctio n
b
y pe nta n e,
h
e x a n e, o rh
ep
ta n e of D N P H
o nl
y s am p l
e sb
a s ed
o nS
pe ctr oph
otom
etric
A b
s o rb
a n c e s 49
F
i
gu r e 3 1.2A
v e r age pe r c e nt e xtr a cti
o nb
y Pe nta n e, He x a n e, o r H epta n e o f Und
i luted A
E 0 0 0 4 3St
a nd
a rd Sa
m
ple s
b
a s ed
o nS
pe ctr oph
otom
etri
cA b
s o rb
a n c e s 5 0F i gu r e 3.2. 1 S pe ctr o
p
h
otom
etric ab
s o rb
a n c e of i
n c r e a si
ngfr a c
tio n s o
f d
ie s el
e xh
a u st s am
ple s
.5 5
F i
gu r e 3.2 2 S pe ctr op hotom
etric a
b
s o rb
a n c e of i
n c r e a singf
r a ctio n s o
fd
ie s el e x ha u st s am
p le s.5 7F i g
u r e3
.2 3
:M
a s s of
c a rb
o nyl
s r e c o v e r ed f
r om
s am
ple
of d i
e s el
e xh
a u st59
F i
gu r e3
.2
.4:S
pe ctr oph
otom
etri
c ab
s o rb
a n c e v e r s u sm
a s s of
c a rb
o nyls r e c o v e r e
d f
r om d i
e s el
e x
h
a u st6 1
F i
gu r e3
.2.5: Av e r age spe ctr op
h
otom
etri
c ab
s o rb
a n c e v e r s u s a v e r agem
a s s of
c a rb
o nyls
r e c o v e r e
d fr o
m d i
e s el
e xh
a u st 6 3F i gu r e 3 3 1 Av e r a
g
e sp
e ctr oph
otom
etri
c ab
s o rb
a n c e of
c el l
ula r a n
d
e xtr a c el lula rm
ed
ia6
5C h
e ape rM
ethod
toQ
u an ti f
y Total Ca rb
o n yl
sB y
La r s
D
. Pe rl m
ut t1
.0
BA C K G R O U
N D1.1 A
i
r Pol lu tio n
T
h
eh i
sto ry of
ai
r pol l
utio n
a nd i
tsd
ele
te ri
o u s ef f
e cts o nh
um
a n si
sw
el l
ch
r o ni
cl
ed
.A
sf
a rb
a ck
a s 13
0 6K i
n g Ed w
a rd
stated
"b
ei
tk
now
n to al l w i
th i
n th
e s o u nd
of
m
y v oi
c e,w h
o s o e v e r sh
al lb
ef
o u nd
gui
lty of b
u r ni
ng c o al shal l
s uf f
e r th
el
o s s of h i
sh
e ad
, "thu s
b
a n nin
gt
h
e u s e of
c o al
(
H a z u ch
a,2 0 0 7
)
. Th
e s e rio u s c o n s e
qu e n c e s of
e xpo s u r e to
h i
gh l
e v els o
f
am b i
e nta
ir
pol lu
ti
o nb
e c am
e e vi d
e nt a s a r e s ul
t of
s e v e r ali
n ci d
e ntsin
th
e 20
' c e ntu ry. T he a r e a of
L
ie
ge o n th
e Ri
v e rM
e u s ein
Bel
gi
um w
a s o n c e o n e of
th
em
o sth
e a vi l
yin
d
u stri
al i
z ed
a r e a s of
E
u r ope,w i
th
ste el m i l l
s, zin
c sm
el
te r s, gl
a s sm
a n uf
a ctu ri
ngf
a cto ri
e s, a sw
el l
a sf
e rti l i
z e r a nd
e x p
lo s
iv e s
pl
a nts Fr om
De c em b
e r 1 to De c em b
e r 5, 1 9 3 0, a th i
ck f
og c o v e r ed
th
e r egi
o nBeg
ir
m i
n g o n De c em b
e r3
,19 3 0
,h
u nd
r ed
sb
ega n to e xpe ri
e n c e r e spi
r ato ry sym
ptom
s,w i
th
o v e r6 0 pe op
l
ed
yin
g th
e n e x t th
r e ed
ays. T he c om
m
i
t te e r epo rt o n th i
sf
og c o n clu
d
ed
th
atm
o rb i d
itya nd
m
o rtal ityw
a s s ole
l
yd
u e to r e spir a
to ry tr a ct alte r atio n s(
N
em
e ry et al
, 2 0 0 0)
.A
ls od
etai l
ed
f
o r th
e f ir st ti m
eis
the r ol
e of
tem
pe r atu r e in v e r sio n a nd f
ogin
air
pol lu
tio n
. Itw
a s c o n clu
d
ed
t
h
at th
eb
urni
ng of
c o al
,b
oth byf
a cto ri
e s and h
o u s eh
ol d
sw
a s th
em
ai
nf
a cto ri
nm
o rb i d i
ty and
m
o rtal i
ty(
N em
e ry et al
,2 0 0 1
)
.In t
h
eU
ni
ted
State s, th
efi
r st s e v e r e ph
oto ch
em i
c al
sm
og epi
s od
e o c c u r r ed i
n Lo sep is ode in that the ep is ode o c c ur re
d i
n th
e s um
m
e r, yetw
a s sti l l
inf lu e n c ed b
y ani
n v e r sio n
laye r,w
h ich
tr ap ped
air pol l
uta nts at th
e s u rf
a c e. Th i
s in v e r si
o nl
aye r, in c om
b in a
ti
o nw it
h low
h
o ri
z o ntal
air
m
o v em
e nt a nd l
a ck
of
tu rb
ul
e n c e, pr e v e nted
c o ntam
in a ntsf
r om d
ispe r sing in th
eup pe r atmo sp
h
e r e. Th
e pri
n ci
pal h
e al
th
ef f
e ctsf
r om
th
e sm
og epi
s od
ew
e r e tem
po r a ry eyei
r ritatio n,w i
th
th
e s o u r c e s of ir ritatio n
r epo rted
a s u nkn ow
n at th
e ti m
e(
Se rm
et al
, 1 9 4 8)
.P
e rh
ap
s th
em
o stf
am
o u s ai
rp
ol l
utio n
d i
s a ste ri
s th
eL
o nd
o n Fog ep i
s od
e of
19 52W
it
h
f
og g yw
e ath
e r, c o al
-b
u r nin
g
h
om
e s,f
a cto ri
e s a nd
pow
e r p la nts, ad
e n s ef
ogla
i d
o v e r Lo nd
o nf
r om
D e c em b
e r 5, 1 9 52 to De c em b
e r8
, 1 9 5 2O f f
i ci
al
go v e r nm
e nt r epo rtsi
nd i
c ate that th
ef
o gr e s u
l
ted i
n ap pr o xi m
atel
y3 0 0 0 m
o r ed
e ath
s th
a n n o rm
al d
u ri
n g th
ef
i r st thr e e
w
e ek
s of
De c e
m b
e r.H
ow
e v e r, a r e a s s e s s
m
e nt of d
atab
y Bel l
et al
(
2
0 0 1)
i
nd i
c ate s th
at ab
o ut 12,0 0
0e x c e s s
d
e ath
s o c c u r r ed fr o
m D
e c em b
e r 19 5
2 to Feb
r u a ry 19 5 3 d
u e to th
e a c ute, asw
el l
a spe r s
i
stin
g ef f
e ctsf
r om
th
e D e c em b
e r 1 9 5 2f
o g epi
s od
eM
o rtal it
y r ate sf
r om
th i
s pe ri
od w
e r e5 0-
3 00
%
h i
g
h
e r th
a n th
e pr e vio u s
ye a r . Fu rth
e r, S O2le v e
l
s(
a v e r age c o n c e ntr atio n of
0.5 7 p pm
)
w
e r e 1 9 ti m
e s gr e ate r th
a n c u r r e ntU S N A A
Q
S
sta nd
a rd
sf
o rS O
2(
2 4-hr
a v e r age
0 0 3
p pm
) (
Bel l
et a
l
, 2 0 0 1)
. Fi
n al l
y,f
r om
De c em b
e r3
to De c em b
e r 10
, th
e r ela
tiv e r
i
skf
o rd
ai l
ym
o rtal it
y a nd
the pr e v
i
o u sd
ay 's pol l
utio nle v e
ls
w
a s1
.2 7 f
o r a0
1 0
-p -p
m i
n c r e a s ei
n th
e pr e vi
o u sd
ay'sSO
2l
e v el
.T
otal
s u spe nd
ed m
at te r(
TS
M )
w
a s, at a v e r age c o n c e ntr atio n s o
f 14
0 0 l
ag
W
f
r om
De c e
m b
e r 5-8
, 1 9 5 2, a
l m
o st 1 0 ti m
e sh
i gh
e r th
a n th
e c u r r e ntU
.S
.N A A
Q
Sf
o r PM
i o(
1 50
^ gW
)
(
U S E P A, 2 0 0 9)
. Fo r a 1 0 0 \iglrx
iin c r e a s e
in
T SM
fr om
th
epr e v
i
o u sd
ay s, the a s s o cia
ted
r e
l
ativ e ri
sk f
o rm
o rtal i
t yw
a s1
.0 8
(
B
el l
et al
,2 0 0
1)
.A i
r pol l
uti
o n r em
ai
n s e xpa n siv e
th
r o u gh
o ut th
ew
o rl d
, r epr e s e nti
ng o n e of
them
o stw i d
e spr e ad
ris
k s to popula
tio n
he al
th. Som
e air qu al i
ty pr oj
e ctio n s
h
a v e sh
ow
n th
atin
m
a nyr edu c ed si gni
fi c a
n tl y o v er th
e n e x t 1 5 to2 0
ye ars(
Crai
g et al
, 2 0 0 8)
. Ev e n in p la c e sw
he r e airqu a
l i
ty sta nd
a rd
s a r e beingm
et, e x te n siv e s ci
e nti f ic data ind ic ate s a c o r r elatio n betw
e e nb
oths
h
o rt-te rm
a nd l
o n g-te r
m
e xp
o s u r e to am b i
e nt air
p
ol l
uti
o n a nd h
um
anh
e alt
h
ef f
e cts(
Cr ai
g eta
l
, 2 00 8
)
. T
h
eW
o rl d
He al
th O
rga ni
z atio n
e sti mate s that air
pol
luti
o ni
s r e spo n si b l
ef
o r 1.4%
of
d
e athsw
o rld w i d
e, a sw
el l a s 0.8%
of d
is ab i l i
ty
-a
d
j
u sted
l i fe ye a r s(W
H O, 2 0 0 2)
In a stud y b yCo
h
e n et al
(
2 00
5)
, o utd
o o rp
a rtic ula
tem
atte r(
PM
)
air
pol l
utio n
i
n u rb
a n a r e a si
s e sti m
ated
tob
e r e spo n si b l
ef
o r ap
pr o xi m
atel
y 3%
of
ad
ul
t c a rd io
pul m
o n a ryd is e a s e
m
o rtal i
ty , 5% of
tr a ch
e a,b
r o n ch
u s, a nd l
u n g c a n c e rm
o rtal i
ty, a nd
ab
o ut1%
of m
o rtal i
t yi
n ch i l d
r e n a s a r e s ul
t of
a c uter e sp
i
r ato ryin
f
e ctio n . Th
e s ef
igu r e s am
o u nt to 0.80 m i l l i
o n pr em
atu r ed
e ath
s(
1.2
%
)
a nd 6
.4
m i l l i
o nl
o stl i f
e ye a r s(
0.5%) (
Coh
e n et al
, 2 0 0 5)
.1.2
S
o u r c e s of A ir Pol lu t io nA
i
r pol l
uta nts c a n ei
th
e rb
e em i
t ted d ir e c
tl
yi
nto th
e atm
o sph
e r e(p
ri m
a ry pol l
uta nts)
o rm
ayb
ef
o rm
ed w i
th in
the atm
o sp h
e r eit
s el f
(
s e c o nd
a ry pol l
uta nts)
. Pol l
uta nts c a nb
ed
efi
n ed b
y thei
rp h
ysi
c al
state(g
a s e o u s o r pa rti
c ula
tem
at te r)
, a sw
el l
a sb
y th
eir
ge og
r aph i
c al
s c al
e(p
oi
nt,l i
n e,a r e a, a n
d
r egi
o n al
s o u r c e s)
. Pri m
a ry pol l
uta ntsin c
l
ud
e s ul f
u rd io x
i d
e(
S
O2)
, o xi d
e s of
ni
tr oge n(
N O
x)
, c a rb
o nm
o n o xi d
e(
C O
)
, v ol
ati le o rga ni
c c om
po u nd
s(
V O C
)
, ca rb
o n a c e o u sp
a rtic
l
e s, a nd
n o n
-c a r
b
o n a c e o u s pa rtic
l
e s. Pa rtic ul
atem
at te r(
PM )
i
s cl
a s si fi
ed b
y th
ed i
am
ete r of
th
e pa rti
cle
,a n
d
the E P Ah
a s sta nd
a rd
sf
o r both
PM
j o(
c o a r s e pa rtic
l
e s)
, pa rticl
e sb
etw
e e n 2.5 \i r a a nd
1 0 [im
,a n
d
PM
2 5(
fi
n ep
a rticle s
)
,f
o r tho s e pa rticle s sm
al l
e r th
a n 2.5 [jm i
nd
iam
ete r. Ul
tr af
i n e pa rtic
l
e s(
PM
0 2)
a r e als o
a pri m
a ry pol l
uta nt pr e s e nti
n th
e atm
o sp h
e r e(
US
EP A
, 2 00 9
)
Th
e o nl
ye ntir e
l
y s e c o nd
a ryp
ol l
uta nt r eg
ul
ated b
y theU S
E PA N
ati
o n al A m b i
e nt Ai
rQ
u al i
tySt
a nd
a rd
si
sor ga n ic a e rosols, w h ich ar e ox i d iz ed organic co
m
p o u ndsfo r
m
ed via r eactio n s of
V O C(
Ha r ris o n ,2 0 0 6
)
T
h
em
ai
n s o u r c e of SO
2i
s th
e c om b
u sti
o n of f
u el
s o u r c e s c o ntai
ni
ng s ul f
u r,l i k
e c o al
a nd
oi l
.V
i
a c om b
u stio n, s ul f
u r in the s o u r c ei
s al m
o st c o n v e r tedq
u a nti
tati
v el y to S O 2(
H a r ri
s o n et al
,2 0 0 6
)
. T he am
o u nt of s ulf
u r in fo s sil f
i i el v a rie s, a nd ind
e v el
oped
c o u ntrie s,m
o st is r em
o v ed
f
r om m
oto rf
u el
sd
u ri
ng th
e r efi
ni
ng pr o c e s s. In Eu r ope, t
h
e u s e of h
i g h s ul f
u r c o al f
o rp
ow
e rge n e r at
i
o n a nd
v eh i
cl
ef
u el h
a sd
e cl
in ed
a nd
th
u s th
em
aj
o r s o u r c e of S O
2 in th
e atm
o sph
e r eh
a v ed
e cl i
n ed
o v e r al l
(
Li
pm
a nn et al
, 2 0 0 6)
. Th
e ad
v e nt of h i g h
ch i m
n ey sta ck
si
nd
e v el
op
ed
n at
i
o n sh
a s al
s ol
ed
toi
n c r e a s e si
nS O
2 c o n c e ntr ati
o n si
n r u r al
a r e a s,d
u e to tr a n spo rt,w i
th
s om
er u r a
l
a r e a sh
a vi
ng h i gh
e r S O2 c o n c e ntr ati
o n s th
a n u rb
a n a r e a s. Th
e u s e of h
i gh
-s u l fu r c o a
l i
nd
e v el
opi
ng n ati
o n si
s a ctu al l
y o n th
e ri
s ef
o r pow
e r pr od
u cti
on, a sw
el l
a si
ts u s ei
nd
om
e sti
cc o o
k i
n g, a nd
e ati
ng
a nd
am b i
e nt c o n c e ntr ati
o n s of
S O2 the r ef
o r e r em
ai
n ath i g h
c o n c e ntr ati
o n s(
Li
pm
a nn, 2 0 0 6)
. Fi
n al l
y, n atu r al
s o u r c e s of
S O2 e xi
st, s u ch
a s v ol
c a n o e s.A
sw i
th
s ulf
u r, th
e c om b
u stio n of f
u el
c on taining n itr og
e n c o n v e rts th
e ni
tr oge n into o xi d
e so
f
ni
tr o ge n. O i l a nd
ga s c o ntain am
u ch l
ow
e r nitr oge n c o nte nt, s o c o al i
s th
em
ai
n c ul prit in th
ef
o rm
ati
o n of N O
x . But,N
Ox a r e al
s of
o rm
ed w h
e n atm
o sp h
e ri
c ni
tr oge n c om b i
n e sw i
th o xy ge nd
u ri
ngh i
gh
-te
m p
e r atu r e c om b
u sti
o n,w h i
ch
o c c u r si
n al l h i
gh
-tem
pe r atu r e c o
m b
u sti
o np
r o c e s s e sa n
d i
s th
u s ah
uge r e a s o n r o ad
tr af fi
c a nd
pow
e r ge n e r ati
o n a r e th
em
aj
o r s o u r c e s of N
Ox(
Ha r ris o n et al
, 2 0 0 6)
. On a gl
ob
al
s c al
e, how
e v e r, n atu r al em
is sio n s of N O
xf
a r o utw
ei
gh
a nt
h
r opoge ni
c s o u r c e s.S
u ch
s o u r c e si
n cl
ud
e v ol
c a ni
c a nd b
a cte ri
al
a cti
o n,l i g h
tni
n g, a nd
i
ntr u si
o n of
str ato sp h
e ri
c ni
tr oge n o xi d
e s. Th
e s e gl
ob
al
em i
s si
o n s, th
o ugh
, a r ed i
sp
e r s ed
t
h
r o ugh
o ut th
e Ea rth, a nd
the r ef
o r eb
a ck
gr o u nd l
e v el
s of
NO
x a r e r el
ati
v el
yl
ow
(
Fo r a sti
e r e etVolatile o rganic c o
m
po u nds(
V
O Cs)
i
n clude aw
i de r a n ge of hyd
ro c arbo n s, o xyge n ate s,haloge n ate s, a n d othe r c a rbo n c o ntainin g c o
m
po u nd
s e x isting in the v apo r ph
a s e in theatmo sp
h
e r e. V O Cs, alo ng
w i
th N Ox, a r e th
e pr e c u r s o r si
n th
e c om
pl
e xf
o rm
ati
o n of
tr op
o sph
e ri
co z o n e
A m
aj
o r s o u r c e of
V O C si
n clu
d
e s the c om b
u sti
o n of f
o s si l f
u el
s. Th
e s e pr o c e s s e sc o nta
i
n u nb
um
ed f
u el fr agm
e ntsw h
ich a r e the n em i
t tedi
n th
ef
o rm
of
V O C(
Ha r ris o n et al ,2
0
06
)
.1.3 Ca r
b
o ny lsA
s aC
om
po n e nt o
f A
ir Pol lut io nT
h
em
aj
o rit
y of
c a rb
o nyl
s(
i
.e. al d
eh y d
e s a nd k
eto n e s)
, ty pe s o
f V O C
,i
n th
e atmo sph
e r e a r ec o n s
i d
e r ed
s e c o nd
a ry air
p
ol lu
ta ntsw i
th
th
e pote nti
al f
o rd
ele
te ri
o u sh
um
a nh
e al
th a nd
e n vir o n
m
e ntal eff
e ctsO
the r c a rb
o nyl
s th
at a r e n ot v ol
ati l
e a r e pri m
a ri l
y at ta ch
ed
to pa rti
c ulatem
at te r.A m
aj
o r s o u r c e of
pri m
a ry c a rb
o nyl
sin
th
e air
is
th
e c om
b
u stio n of f
u el
. Com
b
u stio n
of
f
u el i
s a n o xi d
ati
v e pr o c e s sin
w h i
ch
al k
a n e s(
s u ch
a s th
o s ef
o u nd i
nf
o s si l d ie s e
l
)
a r e o xi d i
z ed
toa
l
c oh
ol
s, th
e n c a rb
o nyl
s, n e xt to c a rb
o xyl i
c a ci d
s, th
e n e ste r s a nd fi
n al l
y to c a rb
o nd i
o xi d
e(
G
u a rie
i
r o et al
,2 0 0 8
)
H
ow
e v e r, c om b
u stio n
of f
o s si l f
u el
si
s n ot10 0
%
ef fi
ci
e nt.C
o nd i
tio n s
a r e
f
a v o r ab l
ef
o rh
yd
r o xyl
ati
o n of f
o s si l f
u el
sw h
e n th
ef
u el h
a sb
e e n v apo riz e
d
a nd
ad
equ atel
ym i
x ed w it
h
ai
rb
ef
o r eb
ein
gb
u r n ed
. How
e v e r,
w h
e nb
u r ni
ng c e a s e s, the o xi d
atio n
pr o c e s sh
al
tsat a n
i
nte rm
ed i
ate state,l
e a vin
gb
y pr od
u cts s u ch
a s al d
eh
yd
e s(
Bo e rla
ge et al
, 1 9 3 6)
.In
aty
p i
c al m
ed iu
m
-d
uty
d i
e s el
tr u ck
th
em
aj
o ri
ty of b
y pr od
u cts a s a r e s ul
t of
c om b
u sti
o n a r e ga s-p
h
a s e v ola
ti l
e o rga ni
c s(
5 8
.7
%
)
b
y
w
ei g h
t,w h i l
e 1 4 7%
a r e s em i
-v o
l
ati le
g
a s-p h
a s e u n r e s olv e
d
c o
m
p le xm i
xtu r e(
U CM
)
, 1 1.3
%
pa rtic
l
e-p
h
a s e U CM
, a nd
1 5 2 %) el
em
e ntal
c a rb
o n Of
the ga s-p
h
a s e v olati le o rga nic s
(
Fi
gu r e 1 3 1)
, ap pr o xim
atel y 1 0.3%
is fo rm
ald
eh
yd
e, 1 9.
3
%
al ka n e s, 8.0
%
olefi n s, and 6.5
%
a r om
atic s a nd cycl ic s(
Scha u e r et al, 1 9 9 9
)
. T he s e r e s ults a r ege n e r ate
d
fr om m
ed i
um d
utyd i
e s el
tr u ck
sd
ri
v e n thr o ug h theh
ot-sta rt Fede r al T e st Pr o c ed
u r e.
F
i
gu r e1
.3
.1C
hem
ic al P ha s e s of D ie s el Ex ha u st a nd Pr opo r t io n ofC
hem i
c alsw
i t h inV
olati
leO
rg
a n icG
a s P ha s e(
S
cha u e r et al., 19 9 9
)
%chem ic alpha s e fr om Medium-Du
t y Die s el Tr u clt s
1 5 %
1 1 %
1 5 %
5 9 %
D ga s
-p ha s e v olat ile o rga nic s ■s e r ri-v olat lle
ga s -p ha s UCM
D Pa rticle-Pha s eUcm
Deleme ntalc a rbo n
%Volat ile Orga nic Ga s s e s
1 0 %
D al ka n e s ■ olef in s
□ a r omat ic s a nd cyclic s D fo rmaldeh y de ■ a c etal deh y de ■ pr opa n al ■ a c eto n e D c r oto n aldeh y de ■ ot he r c a rbo ny ls
It
i
s e vi d
e nt th
at c a rb
o nyl
s c om
pris e a h i g hp
e r c e ntage of
th
e ga s-p
h
a s e v ol
ati l
e o rga nic s.W
ith r ega rd
s to pa rtic ulate o rga ni
c c a rb
o n em i
s si
o n s fr om h
e a vy-d
uty
d
ie s el pow
e r ed
v eh i
cl
e s,d
epe nd i
ng o n ope r ati
ng c o nd i
ti
o n s, th
e c a rb
o n yl f
r a cti
o n of
pa rti
c ul
atem
at te ri
sm
e r el
y3
.3
-
3
.
9 %
(
De stai l l
ats et al
,2 0 0 7
)
.T h
e s ed
ata,h
ow
e v e r ,f
ai l
toi
n cl
ud
e th
e c o ntri b
uti
o n of f
o rm
al d
eh
yd
ea n
d
a c etal d
eh
yd
e to pa rti
c ul
ate o rga ni
c c a rb
o n em i
s si
o n s.J
ak
ob
e r et al
(
2 0 0 6
)
n ote s th
ati
nge n e r al, e
m
is sio n sf
a cto r sf
o r c a rb
o n y ls in th
e ga s ph
a s e e x c e ed
th
o s e of
th
e pa rti
c ul
ate ph
a s e,a n
d f
o r th
o s e c om
po u nd
s th
at a r e ob
s e r v ed i
nb
oth
ph
a s e s, ga s-p
h
a s e em i
s si
o n s a r e atl
e a st af
a cto r of
10 o r gr e ate r th
a n th
o s ef
o r th
e pa rti
c ul
ate ph
a s e.S
e c o nd
a ry c a rb
o nyl
c om
po u nd
si
n th
e atm
o sph
e r e a r ef
o rm
ed
vi
a th
ef
ol l
ow i
ng r e a cti
o n s(
C
a rl i
e r et a/
, 19 8 6
)
:(
1)
R + 0 2^
R0
2(
2)
R O i- +N
O- - ^(
3
)
R O
- + 02 - ^ Ca r
b
o ny l c om
po u nd
+ H O2T
h
u s, a ny o rga ni
c r ad i
c al
,l i k
e h yd
r o xyl
r ad i
c al
s(
0
H)
,w i
th
th
e u npai
r ed
el
e ctr o n o n a c a rb
o nato
m
r e a ctsi
n th
e atm
o sph
e r e tof
o rm
c a rb
o nyl
c om
po u nd
s.A
l k
yl
(
R ON O
2)
a nd
pe r o xyal
k y l ni
tr ate s(
R O ON
O2)
a r e th
e rm
al l y u n stab l
e, a nd
c a nt
h
e r ef
o r eb
e ph
otol
yz ed
, yi
el d i
ngm
o r ef
r e e r ad i
c al
s, a nd
th
u sm
o r e c a rb
o nyl
c om
po u nd
s a r ef
o rm
ed
vi
a th
ef
ol l
ow i
ng
r e a cti
o n s(
C
a rl i
e r et al
,19 8 6
)
:(
4)
R O-+
N
O2 - ^ RO N
O2(
5
)
R 0 2- +N 0
2- - ^
R
O
O N
O2A
t ni
gh
t, ni
tri
c o xi d
e r ad
ic al(
N
O
-)
c o n c e ntr ati
o n s a r el
ow
, s o r e a cti
o n(
2
)
d
o e s n ot o c c u r a nd
R
O
2 r e a ctsm
ai
nl
y vi
a r e a cti
o n 5,b
ut al
s o vi
a th
ef
ol l
ow i
ng r e a cti
o n s(
C
a rl i
e r et al
, 19 8 6
)
:(
6)
R 0
2-+ 0 3
^
RO
- + 2O
2(
7)
R 1O 2 + R2O2^
R iO - +R2O +
O
2(
8
)
R
1O
2 + R2O2 - ^ R 1- O-O-R 2 +O
2(
9
)
R
1O
2 + R2O
2 - ^ al
c oh
ol
+ al d
eh
yd
e s +O
2In r e a ct
i
o n s 7-9
, Ri a n
d R
2 r ef
e r toh
yd
r o ge n o r o rga ni
c gr o ups a nd w h
e n Ri o r Ri equ als H, o nl
yr e a ct
i
o n8
pr o c e ed
s.W
h
e n th
e o rga ni
cg
r o uph
a s a a -H, r e a ct
i
o n 9m
ay pr o c e ed
(
C
a rl i
e r et al
,1
9 8
6)
.Se c o n
d
a ry c a rb
o nyl
gr o ups a r ef
o rm
ed
at th
e gr e ate st r ated
u ri
ng th
ed
ay,w i
th
str o ng
s u n
l i
gh
t, a nd
th
e pr od
u cti
o n of
c a rb
o nyl
si
sd
ete rm
i
n ed b
y th
ef
o rm
ati
o n of f
r e e r ad i
al
s, th
eh
yd
r o x yl
r ad i
c al
,f
r om
o rga ni
c c om
po u nd
si
n th
e atm
o sph
e r e. Th
e s e r e a cti
o n sd
epe nd b
oth
o nt
h
e c o n c e ntr ati
o n of
th
e r e a cti
v e spe ci
e s,l i k
eh
yd
r o x yl
r ad i
c al
s, o z o n e(
O
3)
, a nd
ni
tr ate(
N O
3)
, a sw
el l
a s th
e r ate c o n sta ntsb
etw
e en th
e r e a cti
v e spe ci
e s a nd
o rga ni
c c om p
o u nd
s of
th
e tr opo sph
e r eCar
b
o ny l c om
po u nd
s a r e al
s o a cru cial c om
po n e nt in the fo rm
atio n of
tr opo sph
e ri
c oz o n e.C
a rb
o nyl
s u nd
e rgo ph
otol
ysi
s a nd
r e a ctw i
th
ni
tr ate(
N O
s-)
a nd h
yd
r o xyl
(
0 H
-)
r ad i
c al
s.Fo r
m
al d
eh yd
eg i
v e sh
yd
r o xyl
r ad i
c al
s vi
a ph
otol
ysi
s. Fo rm
ald
eh
y
d
e als o r e a ctsw i
th O
Hr ad ic a
l
s to pr od
u c e H2O a nd
a fo rm
yl
r ad i
c al
(
H C O)
,w h i
ch
th
e n s ub
s equ e ntl
y r e a ctsw i
th
O2 tof
o rm
H O2 a nd C O
(
Sei
nf
el d
et al
,1
9 8 9)
:O H
+H C H O
- ^ H2
O
+ HC O
-H
C O-+
0
2^
HO
2+ C OT
h i
si
si m
po rta nti
n th
at H O 2,i
n th
e pr e s e n c e of N O l
e ad
s toN O
2 a nd O
H(
S
ei
nf
el d
et al
,1
9 8 9
)
:H
O
2 +N O
^
N O
2 +O
HN O
2i
s th
u s c r e ated w i
th
o ut u si
ng up am
ol
e c ul
e of O
3, a nd
th
u s e n ab l i
ngO
3 to a c c um
ul
atei
n th
eat
m
o sph
e r eN
O2 u nd
e rgo e s p hotol
ysi
s to pr od
u c eN O
pl
u sO
a nd
O3i
s th
e n pr od
u c ed w h
e n th
eO
H r ad i
c al
s prod
u c ed
vi
a th
ed i
s s o ci
ati
o n of
al d
eh
yd
e s at ta ck
th
eh
yd
r o c a rb
o n s,f
o rm i
ng o rga ni
cpe r o x y r a
d i
c al
s.T h
e o rga nic pe r o xy r a
d i
c al
s,i
n the pr e s e n c e of
O2 a nd
s u nl i
gh
tg
o o ntof
o rm
O 3(
S
ei
nf
el d
et fl/
,19 8 9
)
.N O
2 + /zv^
N O
+O
R
O
2 +O
2 +A
v^
RO
+O
3Ca r
b
o nyl
sh
a v ed i f f
e r e ntd
egr ad
ati
o n r ate si
n th
e atm
o sph
e r e, a sw
el l
a s s e a s o n al
d i f f
e r e n c e si
n r ate s of d
egr ad
ati
o nb
etw
e e n s um
m
e r a nd w i
nte r. Fo rm
al d
eh
y
d
ei
sp h
oto-o xi d i
z ed
i
n s u nl i
gh
t to c a rb
o nd i
o xi d
e, r epr e s e nti
ng th
em
aj
o rm
e ch
a ni
sm i
nw h i
ch f
o rm
al d
eh
yd
ei
sr e
m
o v ed f
r om
th
e atm
o sph
e r e.T h
e a v e r ageh
al f
-
l i f
e of
th i
s r e a cti
o ni
s ap pr o x
i m
atel
y5 0
m
in ute s(
C O
M
EA
P,2 0 0 0
)
. P hoto ch
em i
c al d
egr ad
ati
o n of f
o rm
al d
eh
yd
e, a n
d
oth
e r al d
eh
yd
e s,(
C
OM
EA P
, 2 0 0 0)
. Ith
a sb
e e n e stim
ated b
yA
EA
T e chnolog y(
1 9 99
)
th
at th
eb
ou nd
a ryl
aye rl i f
eti m
e of f
o rm
al d
eh
yd
ew
ith r e spe ct to r em
o v al b
yO
H r ad
ic al
s in th
ew i
nte ri
s o n a v e r age 6 2d
ays a nd i
n the s um m
e r 1 2d
ays, a nd
r em
o v al b
yN
O3 r ad i
c al
si
s o n a v e r age80 d
ays T hea v e r age
b
o u nd
a ryl
aye rl i f
etim
e of
a c etal d
eh yd
ew i
th
r e spe ct to r em
o v al b
y r e a cti
o nw i
th OHr a
d
ic alsi
s, o n a v e r age,3
.7d
ays
in t
hew i
nte r, a nd
1 8h
o u r si
n th
e s um m
e r, a nd b
y r e a cti
o nw
ithN O
3 r ad i
c al
s, o n a v e r age r em
o v al i
s17 d
ays(
A
EA
T e ch
nol
og y,19 9 9
)
R
em
o v al
of
f
o rm
al d
eh
yd
e a nd
a c etal d
eh
yd
ei
n th
ew i
nte r a v e r age,b y d i
r e ct ph
otol
ysi
s, 13 d
ays a nd 6 7 d
ay s,r e spe ct
i
v el
y,w h
i le the s um
m
e rti m
e a v e r age vi
ad i
r e ct ph
otol
ysi
sf
o rf
o rm
al d
eh
yd
ei
s 6 3h
o u r sa n
d
5.2d
aysf
o r a c etal d
eh yd
e(
A
EA
Te chn ol
og y, 1 9 9
9
)
. Th
el
a rge
d i f f
e r e n c eb
etwe e n s um m
e ra n
d w i
nte r r ate si
sd
u e to th
ef
a ct thati
n th
e s um m
e rm
o nth
s,m
o r ei
nte n s e ph
oto r ad i
ati
o n a nd
a
l
s o a sh
i g he r tem
pe r atu r e s pr o vi de the pr ope r c o nd
itio n sf
o r th
e fa ste rd
egr ad
atio n of ch
em
ic als.Out
d
o o r s, them
o st ab
u nd
a nt c a rb
o ny ls e xpr e s s ed
a s pe r c e ntage s of L o sA
ngele s c a rb
o ny l airc o nte nt c o
l l
e cted i
n 1 9 93 w
e r ef
o rm
al d
eh
yd
e(
2 4%
)
, a c etal d
eh
yd
e(
18
%
)
, a nd
a c eto n e(
7 %
)
(
G
r o sj
e a n et ah
, 19 9 6
)
Othe rm
ai
n c a rb
o ny ls in am b
ie nt a nd
ind
o o r ai
r,b
y c o n c e ntr atio ni
n cl
ud
e a c r ol
ei
n,p
r opa n al
, a nd b
e n z al d
eh
yd
e(
Fi
gu r e 13
1)
.Ge n e r a
l l
y ,i
n r em
ote, u npopul
ated r egi
o n s of
th
ew
o rl d
, am b i
e nt ai
r c o n c e ntr ati
o n s of
f
o rm
al d
eh
yd
e a r el
e s s th
a n 0.0 0 1m
gW
(
0.0 08
p pm
) (
C
OM
EA
P, 2 0 0
0
)
.I
n popul
ated
a r e a s ,t
h
o ugh
, c o n c e ntr ati
o n s a r e u s u al l
yi
n th
e r a n ge of 0
.0 0 1
-0
.
0 2 m
g/m
^(
0
.0 0 8
-0
.
0 16
p pm
)
,