Atmospheric Aerosol. Source/Air Quality Relationships by Edward S. Macias, Philip K. Hopke, Chemical Congress of the

By Edward S. Macias, Philip K. Hopke, Chemical Congress of the North American

content material: New advancements in receptor modeling thought / S.K. Friedlander --
the applying of issue research to city aerosol resource answer / Philip ok. Hopke --
Composition of resource parts wanted for aerosol receptor versions / Glen E. Gordon, William H. Zoller, Gregory S. Kowalczyk, and Scott W. Rheingrover --
assessment of the chemical receptor version of aerosol resource apportionment / John A. Cooper --
The cutting-edge of receptor versions concerning ambient suspended particulate subject to resources / John G. Watson, Ronald C. Henry, John A. Cooper, and Edward S. Macias --
Air particulate keep an eye on process improvement : a brand new technique utilizing chemical mass stability equipment / John E. middle, Patrick L. Hanrahan, and John A. Cooper --
Chemical species contributions to gentle scattering via aerosols at a distant arid web site : comparability of statistical and theoretical effects / J.R. Ouimette, R.C. Flagan, and A.R. Kelso --
Aerosols from a laboratory pulverized coal combustor / D.D. Taylor and R.C. Flagan --
Elemental composition of atmospheric high quality debris emitted from coal burned in a latest electrical energy plant outfitted with a flue-gas desulfurization process / J.M. Ondov, A.H. Biermann, R.E. Heft, and R.F. Koszykowski --
assets and fates of atmospheric polycyclic fragrant hydrocarbons / Ronald A. Hites --
Atmospheric particulate natural topic : multivariate versions for making a choice on assets and estimating their contributions to the ambient aerosol / J.M. Daisey and T.J. Kneip --
an automatic thermal-optical process for the research of carbonaceous aerosol / Richard L. Johnson, Jitendra J. Shah, Robert A. Cary, and James J. Huntzicker --
Wintertime carbonaceous aerosols in l. a. : an exploration of the position of elemental carbon / M.H. Conklin, G.R. Cass, L.-C. Chu, and E.S. Macias --
Carbonaceous city aerosol : fundamental or secondary? / Lih-Ching Chu and Edward S. Macias --
Comparisons among size-segregated resuspended soil samples and ambient aerosols within the western usa / T.A. Cahill, L.L. Ashbaugh, R.A. Eldred, P.J. Feeney, B.H. Kusko, and R.G. Flocchini --
Aerosol composition on the subject of air mass activities in north China / John W. Winchester, Michael Darzi, Alistair C.D. Leslie, Wang Mingxing, Ren Lixin, and Lü Weixiu --
assets of airborne calcium in rural important Illinois / Donald F. Gatz, Gary J. Stensland, Michael V. Miller, and Alistair C.D. Leslie --
The impression of Owens Dry Lake on air caliber within the Owens Valley with implications for the Mono Lake quarter / J.B. Barone, L.L. Ashbaugh, B.H. Kusko, and T.A. Cahill.

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09 46400. 96 235. 0. 9500. 74 27700. 47 122. 0 6060. 65000. 2 250. 52 Average Error a - n o t r e p o r t e d by Bowman e t a l . » 1973 Th Sm U Na Sc Mn Cs La Fe Al Dy Hf Ba Rb Ce Lu Nd Yb Tb Ta Eu K Sb Zn Cr Ti Co Ca V Element Phase A 9. 10 46000. 1 45. 4 300. 40 10400. 245. 7 27600. 76 134. 7 6700. 65000. 6 Reported T a b l e 5. 64 2480. 20 118. 186. 9380. 6 78900. 302. 18 135. 54 24600. 0 1420. 0. 5 80100. 84300. 63 2510. 20 118. 186. 9370. 6 78800. 301. 54 24600. 0 1420. 0. 5 80100. 84300.

Carbonate l e v e l s would be expected t o be s m a l l and covary with c a l c i u m . Humic m a t e r i a l s i n s o i l s should vary w i t h the elements found i n the f i r s t f a c t o r . T h i s f a c t o r may account f o r p o l l e n s i n c e these samples were taken i n l a t e summer. Without a wider p r o f i l e o f elements, i t i s d i f f i c u l t t o be more s p e c i f i c . The n i t r o g e n and s u l f u r f a c t o r s may r e p r e s e n t the h i g h e r u n c e r t a i n t i e s i n these d e t e r m i n a t i o n s than f o r the f i n e p a r t i c l e f r a c t i o n where they were i n g r e a t e r abundance.

While t r y i n g to r e s o l v e which sources are present i n the data, one s t a r t s with an i n i t i a l guess of the elemental composition of the source material. T h i s c o n c e n t r a t i o n p r o f i l e i s then used as the t e s t v e c t o r , b, i n equation 21. From the r o t a t i o n v e c t o r and b, a p r e d i c t e d v e c t o r , b', can be c a l c u l a t e d . The e r r o r observed between the o r i g i n a l t e s t v e c t o r b and the p r e d i c t e d t e s t v e c t o r b' g i v e s an i n d i c a t i o n as t o whether the t e s t v e c t o r i s a reasonable r e p r e s e n t a t i o n of a f a c t o r .

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