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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 3
Biogeosciences, 9, 1225–1235, 2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Earth observation for land-atmosphere interaction science

Biogeosciences, 9, 1225–1235, 2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 29 Mar 2012

Research article | 29 Mar 2012

Organohalogen emissions from saline environments – spatial extrapolation using remote sensing as most promising tool

K. Kotte1, F. Löw2, S. G. Huber1, T. Krause1, I. Mulder1, and H. F. Schöler1 K. Kotte et al.
  • 1Institute of Earth Sciences, University of Heidelberg, 69120 Heidelberg, Germany
  • 2Department of Remote Sensing, Institute of Geography, University of Würzburg, 97074 Würzburg, Germany

Abstract. Due to their negative water budget most recent semi-/arid regions are characterized by vast evaporates (salt lakes and salty soils). We recently identified those hyper-saline environments as additional sources for a multitude of volatile halogenated organohalogens (VOX). These compounds can affect the ozone layer of the stratosphere and play a key role in the production of aerosols. A remote sensing based analysis was performed in the Southern Aral Sea basin, providing information of major soil types as well as their extent and spatial and temporal evolution. VOX production has been determined in dry and moist soil samples after 24 h. Several C1- and C2 organohalogens have been found in hyper-saline topsoil profiles, including CH3Cl, CH3Br, CHBr3 and CHCl3. The range of organohalogens also includes trans-1,2-dichloroethene (DCE), which is reported here to be produced naturally for the first time. Using MODIS time series and supervised image classification a daily production rate for DCE has been calculated for the 15 000 km2 ranging research area in the southern Aralkum. The applied laboratory setup simulates a short-term change in climatic conditions, starting from dried-out saline soil that is instantly humidified during rain events or flooding. It describes the general VOX production potential, but allows only for a rough estimation of resulting emission loads. VOX emissions are expected to increase in the future since the area of salt affected soils is expanding due to the regressing Aral Sea. Opportunities, limits and requirements of satellite based rapid change detection and salt classification are discussed.

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