Variability of Molecular Hydrogen in the Urban Atmosphere Based on Continuous Measurements in Kraków
Jarosław M. Nęcki1, Łukasz Chmura1,2, Jarosław Bielewski3, Damian Zięba1
More details
Hide details
1Faculty of Physics and Applied Computer Science, AGH University of Science and Technology,
al. Mickiewicza 30, 30-059 Kraków, Poland
2Institute of Meteorology and Water Management, National Research Institute, IMGW-PIB Branch of Kraków,
Piotra Borowego 14, 30-215 Kraków, Poland
3Institute of Nuclear Physics, Polish Academy of Science,
Radzikowskiego 152, 31-342 Kraków, Poland
Pol. J. Environ. Stud. 2014;23(2):427–434
With respect to the atmospheric budget of molecular hydrogen (H2), Kraków represents a typical central European urban agglomeration with intense traffic and a relatively high proportion of low-level emissions associated with burning of fossil fuel (mainly coal and gas) for heating. The vehicle fleet in the city still contains a relatively high fraction of cars without properly operating catalysts, which constitutes a considerable source of atmospheric hydrogen. The mixing ratios of hydrogen in near-ground atmosphere were measured quasi-continuously over two years (from 01.2007 till 12.2008) at two different locations within the urban area of Kraków: close to the city center and at the outskirts of the city. Although both measurement locations were under the influence of local traffic, they differ with respect to the structure of local terrain (proportions of buildings, roads, and area covered by vegetation), as well as by local micrometeorological conditions.
A very wide range of H2 mixing ratios was observed at both sites, with peak mixing ratios reaching 2,800 ppb. Distinct seasonality of H2 mixing ratios was observed, with higher values recorded during winter months. Also, distinct daily variations of H2 levels often were observed, with morning and evening H2 maxima associated with traffic rush hours. Diurnal variation of hydrogen concentrations at both locations differs seasonally due to different micrometeorological conditions and source patterns, including car traffic intensity.