Radio and Atmospheric Sciences Division, National Physical Laboratory, Council of Scientific and Industrial Research, Dr KS Krishnan Road, New Delhi-ll0 012, India.
J Environ Sci (China). 2010;22(7):1023-8. doi: 10.1016/s1001-0742(09)60213-8.
We present the diurnal and seasonal variability of ambient NH3, NO, NO2 and SO2 over Delhi, India. Ambient NH3, NO and NO2 were measured continuously during winter, summer and autumn seasons using NH3- and NOx-analyzer, which operates by chemiluminescence method with a higher estimation efficiency (> 90%) than the chemical trap method (reproducibility 4.7%). Prominent diurnal, day-to-day and seasonal variations of ambient mixing ratio of NH3, NO, NO2 and SO2 were observed during the study period. Seasonal variation with higher mixing ratio in winter was observed for all measured trace gases except NO. Day-night variation of all measured trace gases observed was higher in winter in comparison with summer. Late morning increase in NO2 mixing ratio might be attributed to conversion of NO to NO2 with the interaction of O3.
我们展示了印度德里地区环境 NH3、NO、NO2 和 SO2 的日变化和季节变化。在冬季、夏季和秋季,使用 NH3 和 NOx 分析仪连续测量环境 NH3、NO 和 NO2,该分析仪通过化学发光法运行,估计效率(>90%)高于化学阱法(重现性 4.7%)。在研究期间,观察到环境混合比的明显日变化、逐日变化和季节变化NH3、NO、NO2 和 SO2。除了 NO 以外,所有测量的痕量气体在冬季都表现出较高的混合比季节变化。与夏季相比,冬季所有测量的痕量气体的日夜变化都更高。NO2 混合比的午后升高可能归因于 O3 的相互作用将 NO 转化为 NO2。