MEASUREMENT OF SIZE DISTRIBUTION AND PHOTOELECTRIC ACTIVITY OF PARTICLES IN A GAS-DIFFUSION FLAME

被引:11
作者
BURTSCHER, H
MATTER, D
SIEGMANN, HC
机构
[1] Laboratory for Solid State Physics, ETH-Hönggerberg
来源
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS | 1993年 / 27卷 / 08期
关键词
GAS DIFFUSION FLAME; SOOT PARTICLES; PHOTOEMISSION; POLYAROMATIC HYDROCARBONS;
D O I
10.1016/0960-1686(93)90252-T
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The aerodynamic diameter D of the particles in a gas diffusion flame and the concentration of particle-bound polyaromatic hydrocarbons (PAH) are determined by in situ aerosol measurement techniques. Therefore a small gas volume is extracted at different heights from the combustion zone through a thin quartz capillary. By rapid cooling on expansion and approximately 600-fold dilution with air at ambient temperature the physical and chemical processes affecting the particles are quenched. We find 5 less-than-or-equal-to D less-than-or-equal-to 10 nm, and D increases with increasing height above the burner. The number concentration of the particles has, however, a maximum in the middle of the flame, indicating particle formation and growth by condensation and agglomeration up to the middle and annihilation by burning in the upper part of the flame. Photoelectric charging of the particles indicates that PAHs are present in or on the particles everywhere, yet PAH concentration is higher at lower heights and also with smaller particles. Although the total mass of particles in the diffusion mode of the flame is much higher compared to the premixed mode, the size distribution is very similar in both cases. This indicates that the size of the particles and total particulate mass are not directly related.
引用
收藏
页码:1255 / 1259
页数:5
相关论文
共 20 条
[1]   INVESTIGATION OF THE FORMATION OF HIGH MOLECULAR HYDROCARBONS AND SOOT IN PREMIXED HYDROCARBON-OXYGEN FLAMES [J].
BOCKHORN, H ;
FETTING, F ;
WENZ, HW .
BERICHTE DER BUNSEN-GESELLSCHAFT-PHYSICAL CHEMISTRY CHEMICAL PHYSICS, 1983, 87 (11) :1067-1073
[2]   PROBING AEROSOLS BY PHOTOELECTRIC CHARGING [J].
BURTSCHER, H ;
SCHERRER, L ;
SIEGMANN, HC ;
SCHMIDTOTT, A ;
FEDERER, B .
JOURNAL OF APPLIED PHYSICS, 1982, 53 (05) :3787-3791
[3]   INSITU MEASUREMENT OF ADSORPTION AND CONDENSATION OF A POLYAROMATIC HYDROCARBON ON ULTRAFINE C PARTICLES BY MEANS OF PHOTOEMISSION [J].
BURTSCHER, H ;
SCHMIDTOTT, A .
JOURNAL OF AEROSOL SCIENCE, 1986, 17 (04) :699-703
[4]   FORMATION MECHANISMS OF AROMATIC-COMPOUNDS IN ALIPHATIC FLAMES [J].
COLE, JA ;
BITTNER, JD ;
LONGWELL, JP ;
HOWARD, JB .
COMBUSTION AND FLAME, 1984, 56 (01) :51-70
[5]  
DAlessio A., 1981, PART CARBON, P207
[6]   ATMOSPHERIC CARBON PARTICLES IN THE DETROIT URBAN AREA - WINTERTIME SOURCES AND SINKS [J].
DASCH, JM ;
CADLE, SH .
AEROSOL SCIENCE AND TECHNOLOGY, 1989, 10 (02) :236-248
[7]   OPTICAL MEASUREMENTS OF SOOT FORMATION IN PREMIXED FLAMES [J].
FLOWER, WL .
COMBUSTION SCIENCE AND TECHNOLOGY, 1983, 33 (1-4) :17-33
[8]  
Fuchs NA, 1963, GEOFIS PURA APPL, V56, P185, DOI [10.1007/BF01993343, DOI 10.1007/BF01993343]
[9]  
GRIMMER G, 1983, POLYNUCLEAR AROMATIC, P571
[10]  
Hinds W., 1982, AEROSOL TECHNOLOGY