摘要
2009年春季在福建南平市茫荡山地区进行观测,测量了.OH源O3、HONO、HCHO和H2O2的浓度.结果表明O3、HCHO、HONO、H2O2浓度分别为4.96×10-8、3.97×10-10、2.53×10-10、1.18×10-10,低于华北农村的浓度.利用CMAQ计算O3、HCHO、HONO、H2O2对.OH的贡献率,分别为57.0%、7.7%、34.9%、0.4%.O3光解是该地区最重要的.OH来源.O3、HCHO、H2O2对.OH的贡献呈现单峰变化,在12:00~13:00达到峰值.HONO对.OH的贡献曲线呈波动状,和人类居住环境清晨出现峰值的情况不同.
The observation was conducted in Mangdang Mountain,Nanping,Fujian Province in the spring of 2009.Ozone,HONO,HCHO and H2O2 which are regarded as the sources of.OH and other atmospheric components were measured.Mixing ratios of O3,HCHO,HONO and H2O2 were determined to be 4.96 × 10-8,3.97 ×10-10,2.53 ×10-10 and 1.18 × 10-10 respectively,which were lower than the previous observation at the rural areas in Northern China.Using CMAQ,the contribution factors to the.OH of O3,HCHO,HONO,and H2O2 were calculated to be 57.0%,7.7%,34.9% and 0.4% respectively.The photolysis of O3 was the most important source of OH radicals in the atmosphere.The contribution factors of O3,HCHO,and H2O2 had a single peak during 12: 0013: 00 local time.For HONO,the contribution factor showed fluctuations during the daytime,unlike the human living environment in which it peaked in the morning.
出处
《环境科学》
EI
CAS
CSCD
北大核心
2013年第9期3352-3357,共6页
Environmental Science
基金
国家重点基础研究发展规划(973)项目(2005CB422204)