Physical characteristics of microplastic particles and potential for global atmospheric transport: A meta-analysis.

Autor: Fox S; Department of Engineering, Reykjavik University, Reykjavik, Iceland., Stefánsson H; Department of Engineering, Reykjavik University, Reykjavik, Iceland., Peternell M; Department of Earth Sciences, University of Gothenburg, Gothenburg, Sweden. Electronic address: mark.peternell@gu.se., Zlotskiy E; Albert Nenken School of Engineering, The Cooper Union for the Advancement of Science and Art, Brooklyn, NY, USA., Ásbjörnsson EJ; Department of Engineering, Reykjavik University, Reykjavik, Iceland., Sturkell E; Department of Earth Sciences, University of Gothenburg, Gothenburg, Sweden., Wanner P; Department of Earth Sciences, University of Gothenburg, Gothenburg, Sweden., Konrad-Schmolke M; Department of Earth Sciences, University of Gothenburg, Gothenburg, Sweden.

Publikováno v: Environmental pollution (Barking, Essex : 1987) [Environ Pollut] 2024 Feb 01; Vol. 342, pp. 122938. Date of Electronic Publication: 2023 Nov 17.

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Gel-mediated dissolution and reprecipitation - A novel mineral reaction mechanism

Autor: Konrad-Schmolke, M., Halama, R., Wirth, R., Thomen, A., Klitscher, N., Morales, F., Wilke, F.

Publikováno v: Geophysical Research Abstracts
General Assembly European Geosciences Union#

Rates of mineral reactions are controlled by two major factors: surface kinetics and element transport. Dissolution and precipitation of minerals in the presence of a hydrous fluid is assumed to occur predominantly by hydrolysis of the outermost char

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::caac798893c3edb593e6f2872a2608bb
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:3672898

Slab mantle dehydrates beneath Kamchatka – yet recycles water into the deep mantle

Autor: Halama, R, Konrad-Schmolke, M, Manea, V

The subduction of hydrated slab mantle is the most important and yet weakly constrained factor in the quantification of the Earth’s deep geologic water cycle. The most critical unknowns are the initial hydration state and the dehydration behavior o

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::22ef34cf43987109c55e05ffdad6d04c
https://eprints.keele.ac.uk/1894/1/Konrad-Schmolke_et_al_2016_accepted_version.pdf

Boron isotope record of peak metamorphic ultrahigh-pressure and retrograde fluid-rock interaction in white mica (Lago di Cignana, Western Alps).

Autor: Halama R; 1School of Geography, Geology and the Environment, Keele University, Keele, ST5 5BG UK., Konrad-Schmolke M; 2Department of Earth Sciences, University of Gothenburg, Guldhedsgatan 5a, 41320 Gothenburg, Sweden., De Hoog JCM; 3School of GeoSciences, Grant Institute, James Hutton Road, Edinburgh, EH9 3FE UK.

Publikováno v: Contributions to mineralogy and petrology. Beitrage zur Mineralogie und Petrologie [Contrib Mineral Petrol] 2020; Vol. 175 (3), pp. 20. Date of Electronic Publication: 2020 Feb 06.