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海洋大气边界层内臭氧和氮氧化物浓度日变化的模拟研究
引用本文:王 琦,高会旺,林绍迎.海洋大气边界层内臭氧和氮氧化物浓度日变化的模拟研究[J].环境科学研究,2006,19(6):9-14.
作者姓名:王 琦  高会旺  林绍迎
作者单位:中国海洋大学,海洋环境与生态教育部重点实验室,山东,青岛,266003
基金项目:国家自然科学基金 , 教育部跨世纪优秀人才培养计划
摘    要:利用MECCA大气化学模式,考虑卤素类(Br,Cl和I)物质的化学过程,对海洋大气边界层内臭氧和NOx的日变化进行了模拟,并与实测数据进行了对比.结果表明,当考虑这些影响后,ψ(O3)略有降低并且产生峰值的时间提前,这主要是由于Br,BrO,Cl和ClO等物质浓度在日出后很快达到峰值所致,基于同样的原因,NO2变化也有类似的特点.在清洁环境下,海洋大气边界层内臭氧的消耗主要由HOx,O(1D)+H2O和卤素控制,白天以卤素对臭氧的消耗为主.此外还模拟了不同ψ(NOx)下臭氧的日变化,得出在高ψ(NOx)情况下,边界层内臭氧可由净损耗变为净增长. 

关 键 词:卤素    海洋大气边界层    臭氧    NOx
文章编号:1001-6929(2006)06-0009-06
收稿时间:2006-03-20
修稿时间:2006-03-20

A Simulation Study of Diurnal Variation of Ozone and NOx in Marine Atmospheric Boundary Layer
WANG Qi,GAO Hui-wang and LIN Shao-ying.A Simulation Study of Diurnal Variation of Ozone and NOx in Marine Atmospheric Boundary Layer[J].Research of Environmental Sciences,2006,19(6):9-14.
Authors:WANG Qi  GAO Hui-wang and LIN Shao-ying
Affiliation:Lab of Marine Environmental Science and Ecology,Ministry of Education,Ocean University of China,Qingdao 266003,China
Abstract:The diurnal variation of ozone and NO_x in marine atmospheric boundary layer was studied by atmospheric chemical model MECCA,with the modeling results compared with the observed data.Halogen(Br,Cl and I) chemical processes were considered in this model.When the influence of halogen chemical processes was included in the model,a decrease of ozone concentrations and time advance of the peak concentration of ozone are revealed.The main reason is that the reactive halogen radicals such as Br,BrO,Cl and ClO show peaks after sunrise.As the same reason,the NO_2 has the same change tendency with ozone.In clean environment,ozone destruction rate in marine atmospheric boundary layer was mainly controlled by HO_x, O(()~1D)+H_2O and halogen species,and during the daytime,the ozone destruction was mainly derived from reactive halogen species.The impact of variation of initial NO_x concentration on ozone concentration was also studied.In high NO_x situation,there is a net production of ozone in marine atmospheric boundary layer.
Keywords:halogen  marine atmospheric boundary layer  ozone  NOx
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