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首页> 外文期刊>Journal of environmental sciences >Seasonal and diurnal variations of atmospheric peroxyacetyl nitrate, peroxypropionyl nitrate, and carbon tetrachloride in Beijing
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Seasonal and diurnal variations of atmospheric peroxyacetyl nitrate, peroxypropionyl nitrate, and carbon tetrachloride in Beijing

机译:北京大气过氧乙酰硝酸盐,过氧丙酰硝酸盐和四氯化碳的季节性和昼夜变化

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摘要

Atmospheric peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), and carbon tetrachloride (CC1_4) were measured from September 2010 to August 2011 in Beijing. PAN exhibited low values from mid-autumn to early spring (October to March) with monthly average concentrations ranging from 0.28 to 0.73 ppbV, and increased from early spring to summer (March to August), ranging from 1.37-3.79 ppbV. The monthly variation of PPN was similar to PAN, with low values (below detection limit to 0.18 ppbV) from mid-autumn to early spring, and a monthly maximum in September (1.14 ppbV). The monthly variation of CCl_4 was tightly related to the variation of temperature, exhibiting a minimum in winter (69.3 pptV) and a maximum of 180.6 pptV in summer. Due to weak solar intensity and short duration, PAN and O_3 showed no distinct diurnal patterns from morning to night during winter, whereas for other seasons, they both exhibited maximal values in the late afternoon (ca. 15:00 to 16:00 local time) and minimal values during early morning and midnight. Good linear correlations between PAN and PPN were found in autumn (R = 0.91), spring (R = 0.94), and summer (R = 0.81), with slopes of 0.130, 0.222, and 0.133, respectively, suggesting that anthropogenic hydrocarbons dominated the photochemical formation of PANs in Beijing. Positive correlation between PAN and O_3 in summer with the low slopes (ΔO_3/ΔPAN) ranging from 9.92 to 18.0 indicated serious air pollution in Beijing, and strong negative correlation in winter reflected strong O_3 consumption by NO titration and less thermal decompositin of PAN.
机译:从2010年9月至2011年8月在北京测量了大气过氧乙酰硝酸盐(PAN),过氧丙酰硝酸盐(PPN)和四氯化碳(CC1_4)。 PAN从中秋至初春(十月至三月)显示出较低的值,月平均浓度范围为0.28至0.73 ppbV,而从初春至夏季(三月至八月)则增加,范围为1.37-3.79 ppbV。 PPN的月变化与PAN相似,从中秋到初春的值较低(检测极限低于0.18 ppbV),9月的月最大值(1.14 ppbV)。 CCl_4的每月变化与温度的变化紧密相关,冬季最低(69.3 pptV),夏季最高180.6 pptV。由于太阳强度弱和持续时间短,冬季期间从早到晚,PAN和O_3均没有明显的昼夜模式,而在其他季节,它们在下午晚些时候(当地时间约15:00至16:00)都表现出最大值。 )和清晨和午夜的最小值。在秋季(R = 0.91),春季(R = 0.94)和夏季(R = 0.81)上发现PAN和PPN之间具有良好的线性相关性,其斜率分别为0.130、0.222和0.133,这表明人为碳氢化合物占主导地位。北京地区PANs的光化学形成夏季PAN和O_3之间呈正相关,低坡度(ΔO_3/ΔPAN)在9.92至18.0之间,表明北京空气污染严重,而冬季的强烈负相关反映出NO滴定法消耗的O_3量大,PAN的热分解较少。

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