| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1742457 | Geothermics | 2013 | 10 Pages |
Episodes of high atmospheric load of hydrogen sulfide (H2S), where the concentration is over 50 μg m−3 hourly average value, occur about 80 times a year in Reykjavik (data from 2007 to 2009). H2S originates mainly from two geothermal power plants 25–30 km (south-)east of Reykjavik, at Hellisheidi and Nesjavellir. Certain weather-dependent dispersion conditions, such as wind, cloud cover and air temperature, allow the transport of emissions towards Reykjavik and the neighboring cities, causing local air pollution. High concentrations of H2S occur within a narrow range of weather conditions, namely slow (mean value 2 ± 1 m s−1) easterly (114° ± 23°) winds, together with cold air temperatures (median value −3 °C) and preferably no, or little, cloud cover. A classification of weather types shows the preferred occurrence of high H2S concentrations in connection with low atmospheric exchange and autochthonous weather. Stable atmospheric stratification and inversions enable the transport of H2S emissions to Reykjavik. The measured concentrations, the short lived peaks in concentration and different values at nearby measurement stations, indicate a very narrow plume, which fits well with a Gaussian plume distribution model.
► Measurements of H2S emitted by geothermal power plants in a sub-polar oceanic climate. ► Meteorological parameters, weather type and stability clearly determine concentration. ► Modeled concentration, narrow plumes, explains differences between nearby stations. ► Results can be used for planning of new power plants and urban districts. ► The annual average is near the health limit, effects on health need to be studied.
