Zobrazeno 1 - 10
of 70
pro vyhledávání: '"Hövelmann, Jörn"'
Autor:
Stawski, Tomasz M., Besselink, Rogier, Chatzipanagisad, Konstantinos, Hoevelmann, Joern, Benning, Liane G., Van Driessche, Alexander E. S.
Publikováno v:
J. Phys. Chem. C 2020
CaSO4 minerals (i.e. gypsum, anhydrite and bassanite) are widespread in natural and industrial environments. During the last several years, a number of studies have revealed that nucleation in the CaSO4-H2O system is non-classical, where the formatio
Externí odkaz:
http://arxiv.org/abs/2002.02185
Autor:
Besselink, Rogier, Stawski, Tomasz M., Freeman, Helen M., Hoevelmann, Joern, Tobler, Dominique J., Benning, Liane G.
Although clays are crucial mineral phases in Earth's weathering engine, it is unclear how they form in surface environments under (near-)ambient pressures and temperature. Most synthesis routes, attempting to give insights into the plausible mechanis
Externí odkaz:
http://arxiv.org/abs/1906.07479
Autor:
Stawski, Tomasz M., Freeman, Helen M., Van Driessche, Alexander E. S., Hövelmann, Jörn, Besselink, Rogier, Wirth, Richard, Benning, Liane G.
Calcium sulfate minerals are found under the form of three crystalline phases: gypsum (CaSO4.2H2O), bassanite (CaSO4.0.5H2O), and anhydrite (CaSO4). Due to its relevance in natural and industrial processes, the formation pathways of these calcium sul
Externí odkaz:
http://arxiv.org/abs/1812.03022
Autor:
Karafiludis, Stephanos, Scoppola, Ernesto, Wolf, Stephan E., Kochovski, Zdravko, Matzdorff, David, Van Driessche, Alexander E. S., Hövelmann, Jörn, Emmerling, Franziska, Stawski, Tomasz M.
Publikováno v:
Journal of Chemical Physics; 10/7/2023, Vol. 159 Issue 13, p1-12, 12p
Publikováno v:
In LITHOS July 2016 256-257:228-242
Publikováno v:
In Chemical Geology 12 December 2012 334:254-265
Publikováno v:
In Geochimica et Cosmochimica Acta 2011 75(22):6760-6779
Autor:
Hövelmann, Jörn1 jhoevelm@gfz-potsdam.de, Putnis, Christine V.2,3 putnisc@uni-muenster.de, Benning, Liane G.1,4,5 benning@gfz-potsdam.de
Publikováno v:
Minerals (2075-163X). Aug2018, Vol. 8 Issue 8, p346. 21p.
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Although quartz is a stable mineral at Earth surface conditions, field samples have shown its rapid dissolution in combination with the precipitation of Mg-silicate phases. Atomic force microscopy (AFM) experiments were performed to investigate the d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2471695e69bc06aec3aac475f191dfc6
https://doi.org/10.31223/osf.io/27uky
https://doi.org/10.31223/osf.io/27uky