Trends and analysis of ambient NO, NOy, CO, and ozone concentrations in Raleigh, North Carolina

被引:16
作者
Aneja, VP
Kim, DS
Chameides, WL
机构
[1] KUNSAN NATL UNIV, DEPT ENVIRONM ENGN, CHONJU 573701, SOUTH KOREA
[2] GEORGIA INST TECHNOL, SCH EARTH & ATMOSPHER SCI, ATLANTA, GA 30332 USA
关键词
D O I
10.1016/S0045-6535(96)00393-1
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Ambient concentrations of NO and NOy as well as O-3 and CO were measured during August 19 to September 1, 1991 in downtown Raleigh, North Carolina as a part of the Southern Oxidants Study-Southern Oxidants Research Program on Ozone Non-Attainment (SOS-SORP/ONA). These measurements were made in an effort to provide insight into the characteristics of nitrogen oxides and their role in the formation of ozone in the urban Southeast U.S. environment. NO and NOy, showed bimodal diurnal variations with peaks in the morning (06:00 - 08:00 EST) and in the late evening (21:00 - 23:00 EST). These peaks at this urban site correspond to the coupled effects of rush hour traffic and meteorological conditions (i.e., variation of mixing height and dispersion conditions). The overall average NO and NOy concentrations were found to be 6.1 +/- 5.4 ppbv (range: 0 to 70 ppbv) and 14.9 +/- 8.1 ppbv (range: 0.3 to 110 ppbv), respectively. Average daily maxima of NO and NOy (18.3 ppbv and 27.4 ppbv) occurred during the morning. O-3 showed a diurnal variation with a maximum in the afternoon between 14:00 and 16:00 EST; and a mean concentration 20 +/- 10 ppbv (range: 1 to 62 ppbv). Maximum O-3 and CO concentrations during weekdays result from NO and CO emitted from mobile sources during the morning rush hour. Background CO concentration at Raleigh was estimated to be - 470 +/- 52 ppbv. A linear correlation of r(2) = 0.53 between CO and NOy was observed. The ratio of CO to NOy (similar to 16) at the Raleigh site suggests that mobile sources are the major contributor to NO and NOy concentrations at the site. (C) 1997 Elsevier Science Ltd.
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页码:611 / 623
页数:13
相关论文
共 18 条
[1]  
ANJEA VP, 1984, TR2 AIR POLL CONTR A, P430
[2]   NATURAL HYDROCARBONS, URBANIZATION, AND URBAN OZONE [J].
CARDELINO, CA ;
CHAMEIDES, WL .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1990, 95 (D9) :13971-13979
[3]   PHOTOCHEMICAL THEORY OF TROPOSPHERIC OZONE [J].
CHAMEIDES, W ;
WALKER, JCG .
JOURNAL OF GEOPHYSICAL RESEARCH, 1973, 78 (36) :8751-8760
[4]   MODIFICATION OF A COMMERCIAL NOX DETECTOR FOR HIGH-SENSITIVITY [J].
DELANY, AC ;
DICKERSON, RR ;
MELCHIOR, FL ;
WARTBURG, AF .
REVIEW OF SCIENTIFIC INSTRUMENTS, 1982, 53 (12) :1899-1902
[5]   FURTHER MODIFICATION OF A COMMERCIAL NOX DETECTOR FOR HIGH-SENSITIVITY [J].
DICKERSON, RR ;
DELANY, AC ;
WARTBURG, AF .
REVIEW OF SCIENTIFIC INSTRUMENTS, 1984, 55 (12) :1995-1998
[6]   A GROUND-BASED INTERCOMPARISON OF NO, NOX, AND NOY MEASUREMENT TECHNIQUES [J].
FEHSENFELD, FC ;
DICKERSON, RR ;
HUBLER, G ;
LUKE, WT ;
NUNNERMACKER, LJ ;
WILLIAMS, EJ ;
ROBERTS, JM ;
CALVERT, JG ;
CURRAN, CM ;
DELANY, AC ;
EUBANK, CS ;
FAHEY, DW ;
FRIED, A ;
GANDRUD, BW ;
LANGFORD, AO ;
MURPHY, PC ;
NORTON, RB ;
PICKERING, KE ;
RIDLEY, BA .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1987, 92 (D12) :14710-14722
[7]  
Finlayson-Pitts B. J., 1986, ATMOSPHERIC CHEM
[8]   OBSERVATIONAL AND THEORETICAL EVIDENCE IN SUPPORT OF A SIGNIFICANT INSITU PHOTO-CHEMICAL SOURCE OF TROPOSPHERIC OZONE [J].
FISHMAN, J ;
SOLOMON, S ;
CRUTZEN, PJ .
TELLUS, 1979, 31 (05) :432-446
[9]   MEASUREMENTS OF NITROGEN-OXIDES IN THE ARCTIC [J].
HONRATH, RE ;
JAFFE, DA .
GEOPHYSICAL RESEARCH LETTERS, 1990, 17 (05) :611-614
[10]   NITROGEN-OXIDES IN THE TROPOSPHERE - GLOBAL AND REGIONAL BUDGETS [J].
LOGAN, JA .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1983, 88 (NC15) :785-807