MEASUREMENTS OF 3-METHYL FURAN, METHYL VINYL KETONE, AND METHACROLEIN AT A RURAL FORESTED SITE IN THE SOUTHEASTERN UNITED-STATES

被引:71
作者
MONTZKA, SA
TRAINER, M
ANGEVINE, WM
FEHSENFELD, FC
机构
[1] NOAA, AERON LAB, BOULDER, CO 80303 USA
[2] UNIV COLORADO, COOPERAT INST RES ENVIRONM SCI, BOULDER, CO 80309 USA
关键词
D O I
10.1029/95JD01132
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Three oxygenated hydrocarbons were measured in ambient air above a rural forested site in western Alabama. Mixing ratios of methyl vinyl ketone (MVK), methacrolein (MACR), and 3-methyl furan were determined during a 3-week period in the summer of 1992. While the mean mixing ratio for methyl vinyl ketone was determined to be 740 parts per 10(12) (ppt), the mean mixing ratio for methacrolein was 480 ppt. The results for methyl vinyl ketone and methacrolein are compared to previously reported measurements from this same location during the summer of 1990. Although isoprene levels were lower by similar to 50% in 1992, mixing ratios of the carbonyls were reduced by only similar to 25%. These differences are discussed in light of the changes that had occurred to the forest canopy in the time elapsed between the two measurement campaigns. Despite the differences observed during the 2 years, a consistent diurnal variability is observed for methyl vinyl ketone, relative to methacrolein, during both years. In addition to a weak correlation observed between the carbonyls and temperature, levels of MVK and MACR in air sampled from just above the forest canopy are influenced by the depth of the mixed layer. A third oxidation product of isoprene, 3-methyl furan, was identified and measured in ambient air. Mean daytime mixing ratios were estimated at 60 ppt. Nighttime levels were lower, averaging 40 ppt. Mixing ratios of 3-methyl furan were highly correlated with isoprene (R(2) = 0.82), and during the day, were typically similar to 2% of levels measured for isoprene.
引用
收藏
页码:11393 / 11401
页数:9
相关论文
共 34 条
[1]   BOUNDARY-LAYER DEPTH AND ENTRAINMENT ZONE CHARACTERIZATION WITH A BOUNDARY-LAYER PROFILER [J].
ANGEVINE, WM ;
WHITE, AB ;
AVERY, SK .
BOUNDARY-LAYER METEOROLOGY, 1994, 68 (04) :375-385
[2]   FORMATION YIELDS OF METHYL VINYL KETONE AND METHACROLEIN FROM THE GAS-PHASE REACTION OF O3 WITH ISOPRENE [J].
ASCHMANN, SM ;
ATKINSON, R .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1994, 28 (08) :1539-1542
[3]   FORMATION OF 3-METHYLFURAN FROM THE GAS-PHASE REACTION OF OH RADICALS WITH ISOPRENE AND THE RATE-CONSTANT FOR ITS REACTION WITH THE OH RADICAL [J].
ATKINSON, R ;
ASCHMANN, SM ;
TUAZON, EC ;
AREY, J ;
ZIELINSKA, B .
INTERNATIONAL JOURNAL OF CHEMICAL KINETICS, 1989, 21 (07) :593-604
[4]   FORMATION OF OH RADICALS IN THE GAS-PHASE REACTIONS OF O3 WITH A SERIES OF TERPENES [J].
ATKINSON, R ;
ASCHMANN, SM ;
AREY, J ;
SHOREES, B .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D5) :6065-6073
[5]   RATE CONSTANTS FOR THE GAS-PHASE REACTIONS OF O-3 WITH THE NATURAL HYDROCARBONS ISOPRENE AND ALPHA-PINENE AND BETA-PINENE [J].
ATKINSON, R ;
WINER, AM ;
PITTS, JN .
ATMOSPHERIC ENVIRONMENT, 1982, 16 (05) :1017-1020
[6]   GAS-PHASE TROPOSPHERIC CHEMISTRY OF ORGANIC-COMPOUNDS - A REVIEW [J].
ATKINSON, R .
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1990, 24 (01) :1-41
[7]   KINETICS OF THE REACTIONS OF O-3 AND OH RADICALS WITH FURAN AND THIOPHENE AT 298 +/- 2 K [J].
ATKINSON, R ;
ASCHMANN, SM ;
CARTER, WPL .
INTERNATIONAL JOURNAL OF CHEMICAL KINETICS, 1983, 15 (01) :51-61
[8]  
BUHR M, 1995, J GEOPHYS RES
[9]   THE ROLE OF BIOGENIC HYDROCARBONS IN URBAN PHOTOCHEMICAL SMOG - ATLANTA AS A CASE-STUDY [J].
CHAMEIDES, WL ;
LINDSAY, RW ;
RICHARDSON, J ;
KIANG, CS .
SCIENCE, 1988, 241 (4872) :1473-1475
[10]  
FEHSENFELD F, 1992, CYCLES, V6, P389