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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >A study of precipitation scavenging of semivolatile organic compounds in a tropical area
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A study of precipitation scavenging of semivolatile organic compounds in a tropical area

机译:的沉淀净化的研究半挥发性的有机化合物在热带地区

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Rain samples were collected concurrently with gas phase and particulate samples from June 2007 to May 2008 in Singapore and processed to investigate precipitation scavenging of polycyclic aromatic hydrocarbons (PAHs) and organochlorine pesticides (OCPs). A comprehensive atmospheric scavenging model has been developed with inclusion of major atmospheric deposition processes such as particle scavenging, dissolution (Henry's law), and surface adsorption affecting the total scavenging ratio of SVOCs. This model was subsequently used in this study to calculate precipitation ratios. Total scavenging ratios ranged from (8.9 ± 4.3) x 10~4 to (1.2 ± 0.4) x 10~6 for PAHs and from (8.3 ± 5.1) x 10~4 to (4.9 ± 1.5) x 10~5 for OCPs. Particle scavenging rather than gas scavenging was the dominant removal mechanism, accounting for 86-99% for PAHs and 98-99% for OCPs in terms of the particle contribution to the total scavenging. The variation of both total and particle scavenging ratios over the study period is smaller compared to those reported in the literature, which might be attributed to uniform ambient temperature prevailing throughout the year in this tropical area. The effects of particle fraction, supercooled vapor pressure, and rainfall intensity on particle scavenging of SVOCs were assessed. The relationship between gas scavenging ratio and supercooled vapor pressure implied that the domination of gas scavenging might switch from dissolution to adsorption at supercooled vapor pressures around 10~(-3.5)-10~(-4) Pa, especially for PAHs with five or more aromatic rings. The equations used to estimate total scavenging (W_T) based on the particle fraction (Φ) can be summarized as log W_T = 0.94 log Φ + 6.09 (R~2 = 0.74) for PAHs and log W_T = 0.82 log Φ + 6.34 (R~2 = 0.62) for OCPs.
机译:雨样本进行并发收集气体从2007年6月到阶段和颗粒样品2008年5月在新加坡和处理调查的沉淀净化多环芳烃(多环芳烃)和有机氯农药((ocp)。大气净化模型了包含的主要大气沉积过程,如粒子清除,解散(亨利定律)和表面吸附影响总扫SVOCs的比率。这个模型被用于这项研究计算降水比率。比率范围从(8.9±4.3)x(1.2±10 ~ 40.4) x 10 ~ 6的多环芳烃和(8.3±5.1)x 10 ~ 4(4.9±1.5)x 10 ~ 5 (ocp。扫而不是气体清除了除主导机制,占86 - 99%多环芳烃和98 - 99% (ocp而言的粒子的贡献完全清除。的变化和粒子扫气率在研究期间较小的报道相比文学,这可能归因于制服环境温度的整个在这个热带地区。粒子分数,过冷蒸汽压力,和降雨强度对颗粒的清除SVOCs进行评估。扫气比和过冷蒸汽压暗示气体清除的统治可能从溶解吸附过冷蒸汽压力在10 ~ -10(-3.5) ~(4),尤其是对多环芳烃5个或5个以上芳香环。估计总清除(W_T)的基础上粒子分数(Φ)可以概括为日志日志ΦW_T = 0.94 + 6.09 (R ~ 2 = 0.74)和多环芳烃日志日志ΦW_T = 0.82 + 6.34 (R ~ 2 = 0.62)

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