Experimental Studies of Aerosols in the Atmosphere of Semiarid Landscapes of Kalmykia: 2. Landscape–Geochemical Composition of Aerosol Particles
- Authors: Gubanova D.P.1,2, Kuderina T.M.3, Chkhetiani O.G.2, Iordanskii M.A.1, Obvintsev Y.I.1,2, Artamonova M.S.2
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Affiliations:
- Karpov Research Institute of Physical Chemistry, State Scientific Center of the Russian Federation, State Corporation Rosatom
- Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences
- Institute of Geography, Russian Academy of Sciences
- Issue: Vol 54, No 10 (2018)
- Pages: 1430-1448
- Section: Article
- URL: https://journals.rcsi.science/0001-4338/article/view/148676
- DOI: https://doi.org/10.1134/S0001433818100043
- ID: 148676
Cite item
Abstract
The chemical composition of aerosol particles in the atmospheric surface layer of semiarid regions of Kalmykia is considered. Background landscapes of dry steppes, sandy massifs, and salt marshes have been studied using a landscape–geochemical approach. The results of long-term complex experimental studies (2002–2016) of the elemental composition of surface aerosols, the morphology and chemical composition of soils, and the elemental composition of aerosol particles in the atmospheric surface layer have been summarized. Soils have been confirmed to be the main sources of aerosol emission in semiarid regions. The accumulation of chemical elements in soils and aerosol particles has been estimated. The concentration clarks, aerosol-concentration coefficients, and local aerosol concentration have been calculated. The content of sulfur and some heavy metals in aerosols, which enter into the atmosphere by both removal from the underlying surface and from local anthropogenic sources, has been found to be high.
About the authors
D. P. Gubanova
Karpov Research Institute of Physical Chemistry, State Scientific Center of the Russian Federation, State Corporation Rosatom; Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences
Author for correspondence.
Email: dgubanova@mail.ru
Russian Federation, Moscow, 105064; Moscow, 119017
T. M. Kuderina
Institute of Geography, Russian Academy of Sciences
Author for correspondence.
Email: kuderina@igras.ru
Russian Federation, Moscow, 119017
O. G. Chkhetiani
Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences
Author for correspondence.
Email: lgg@ifaran.ru
Russian Federation, Moscow, 119017
M. A. Iordanskii
Karpov Research Institute of Physical Chemistry, State Scientific Center of the Russian Federation, State Corporation Rosatom
Author for correspondence.
Email: miordan@mail.ru
Russian Federation, Moscow, 105064
Yu. I. Obvintsev
Karpov Research Institute of Physical Chemistry, State Scientific Center of the Russian Federation, State Corporation Rosatom; Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences
Author for correspondence.
Email: obvintyu@mail.ru
Russian Federation, Moscow, 105064; Moscow, 119017
M. S. Artamonova
Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences
Author for correspondence.
Email: artamonova@ifaran.ru
Russian Federation, Moscow, 119017