Differences in PM10 concentrations measured by β-gauge monitor and hi-vol sampler

被引:44
作者
Chang, CT
Tsai, CJ [1 ]
Lee, CT
Chang, SY
Cheng, MT
Chein, HM
机构
[1] Natl Chiao Tung Univ, Inst Environm Engn, Hsinchu, Taiwan
[2] Natl Cent Univ, Inst Environm Engn, Chungli 32054, Taiwan
[3] Natl Chunghsing Univ, Inst Environm Engn, Taichung 40227, Taiwan
[4] Ind Technol Res Inst, Hsinchu, Taiwan
关键词
beta-gauge; water content; PM10; relative humidity;
D O I
10.1016/S1352-2310(01)00369-7
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In this paper. differences between the 24-h average PM10 concentrations of Wedding beta -gauge monitor and Andersen or Wedding hi-vol sampler were studied. When the deliquescent point is not exceeded, PM10 concentrations of the beta -gauge are close to those of the manual samplers. The ratio of beta -gauge PM10 to Andersen PM10 and Wedding PM10 is 1.08 +/-0.06 and 1.09 +/-0.12, respectively. However, when the deliquescent point is exceeded, water absorption by the inorganics of aerosols leads to higher PM10 concentrations of the beta -gauge compared to those of the manual sampler. The ratio of beta -gauge PM10 to Andersen PM10 and Wedding PM10 is 1.21 +/-0.22 and 1.27 +/-0.15, respectively. However., due to evaporation of water from the aerosols collected on the filter tape of the beta -gauge, differences in PM10 concentrations are much less than theoretically calculated. (C) 2001 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:5741 / 5748
页数:8
相关论文
共 19 条
[1]   Evaporation loss of ammonium nitrate particles during filter sampling [J].
Cheng, YH ;
Tsai, CJ .
JOURNAL OF AEROSOL SCIENCE, 1997, 28 (08) :1553-1567
[2]  
Environmental Protection Agency, 1987, FED REGISTER, V52, P24634
[3]   PARTICLE DEAGGLOMERATION AND REENTRAINMENT IN A PM-10 SAMPLER [J].
JOHN, W ;
WINKLMAYR, W ;
WANG, HC .
AEROSOL SCIENCE AND TECHNOLOGY, 1991, 14 (02) :165-176
[4]   LABORATORY TESTING METHOD FOR PM-10 SAMPLERS - LOWERED EFFECTIVENESS FROM PARTICLE LOADING [J].
JOHN, W ;
WANG, HC .
AEROSOL SCIENCE AND TECHNOLOGY, 1991, 14 (01) :93-101
[5]   ATMOSPHERIC GAS-AEROSOL EQUILIBRIUM .2. ANALYSIS OF COMMON APPROXIMATIONS AND ACTIVITY-COEFFICIENT CALCULATION METHODS [J].
KIM, YP ;
SEINFELD, JH ;
SAXENA, P .
AEROSOL SCIENCE AND TECHNOLOGY, 1993, 19 (02) :182-198
[6]   ATMOSPHERIC GAS AEROSOL EQUILIBRIUM .1. THERMODYNAMIC MODEL [J].
KIM, YP ;
SEINFELD, JH ;
SAXENA, P .
AEROSOL SCIENCE AND TECHNOLOGY, 1993, 19 (02) :157-181
[7]  
MCFARLAND AR, 1987, 4716010881ARM TEX A, P15
[8]   CONTRIBUTION OF WATER TO PARTICULATE MASS IN THE SOUTH COAST AIR BASIN [J].
MENG, ZY ;
SEINFELD, JH ;
SAXENA, P ;
KIM, YP .
AEROSOL SCIENCE AND TECHNOLOGY, 1995, 22 (01) :111-123
[9]   ISORROPIA: A new thermodynamic equilibrium model for multiphase multicomponent inorganic aerosols [J].
Nenes, A ;
Pandis, SN ;
Pilinis, C .
AQUATIC GEOCHEMISTRY, 1998, 4 (01) :123-152
[10]   Systematic biases in measured PM10 values with US Environmental Protection Agency-approved samplers at Owens Lake, California [J].
Ono, DM ;
Hardebeck, E ;
Parker, J ;
Cox, BG .
JOURNAL OF THE AIR & WASTE MANAGEMENT ASSOCIATION, 2000, 50 (07) :1144-1156