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Special Issue "Clay Minerals as Element Sources and Sinks in Diagenetic-Metamorphic Environments"
A special issue of Minerals (ISSN 2075-163X).
Deadline for manuscript submissions: 1 April 2020.
Dr. Andre Baldermann Website 1 Website 2 E-Mail
Institute of Applied Geosciences, Graz University of Technology, Graz, Austria
Interests: minerals; clay mineralogy; environmental geochemistry; fluid–rock interaction; global element cycles; iron biogeochemistry; interface and nanoscale processes
Prof. Dr. Laurence Noel Warr Website 1 Website 2 E-Mail
Institute for Geography and Geology, University of Greifswald, Greifswald, Germany
Interests: diagenesis and low-temperature metamorphism; bacteria–clay interactions; fault rocks; radiogenic isotope dating; disposal of nuclear waste; geopolymer cement; gas storage in reservoirs
The distribution and abundance of clay minerals in surface and upper crustal environments of the Earth has played a key role in the origin of life, the evolution of ocean biogeochemistry, and climate change. As a result, these minerals have significantly influenced the petrography, mineralogy, and geochemistry of sediments across time and space. Although clay mineral reactions are generally considered to be slow, there is increasing evidence of them acting as important element sources and sinks in a great variety of rocks (e.g., sedimentary, hydrothermal, and metamorphic). They are also important carrier materials for elements and nutrients in developing soils, modern marine/continental deposits, and ancient sedimentary–metamorphic rocks. Clay minerals provide important reactive surfaces for adsorption and desorption of elements and compounds, controlling metal ion transport in aquatic media. However, quantitative estimates of the contribution of clay minerals in the global element cycles (Fe, Mg, Si, trace elements, etc.) are still scarce, and the role of clay mineral reactions on element mobility under various environmental conditions is poorly constrained. This Special Issue welcomes papers that confirm the important role of clay minerals as element sources, carriers, and sinks in diagenetic–metamorphic environments based on the full range of mineralogical, nano- to microstructural and (isotope) geochemical investigation observations. Studies that aim at resolving the physicochemical processes at the clay/water interface, as well as papers providing experimental and modelling data to unravel the relations between clay mineral reactivity and element transport, (re-)cycling and sequestration processes, are particularly welcome.
Dr. Andre Baldermann
Prof. Dr. Laurence Noel Warr
Manuscript Submission Information
Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All papers will be peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.
Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Minerals is an international peer-reviewed open access monthly journal published by MDPI.
Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 1400 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.
- clay minerals
- reactive transport
- interface processes