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Mineralogy, Geochemistry and Physical Properties of Soil

A special issue of Applied Sciences (ISSN 2076-3417). This special issue belongs to the section "Earth Sciences".

Deadline for manuscript submissions: closed (20 November 2023) | Viewed by 1596

Special Issue Editors


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Guest Editor
Academy of Biology and Biotechnology, Southern Federal University, Stachki Ave. 194/1, 344090 Rostov-on-Don, Russia
Interests: soil science; ecology of soils; land assessment

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Guest Editor
Academy of Biology and Biotechnology Named D.I. Ivanovsky, Southern Federal University, 344090 Rostov-on-Don, Russia
Interests: nanobioremediation; nanomaterials; biotechnology; plant growth and development; toxicity; biological synthesis; characterization of NPs
Special Issues, Collections and Topics in MDPI journals

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Guest Editor
Laboratory of Biogeochemistry, Scientific Center "Innovative Chemical and Biotechnologies", Tula State Lev Tolstoy Pedagogical University, 300026 Tula, Russia
Interests: bioavailability and speciation of trace elements in soils; adsorption of metals and metalloids by abiotic and biotic soil components; construction of model ternary bio-mineral; organo-mineral systems to study heavy metals behavior

Special Issue Information

Dear Colleagues,

Soil mineralogy deals with the exploration of soil mineral phase, which contributes 90% of the solid volume of mineral soils. Soil minerals are indicators of the weathering rates of surface materials, the determination of soil age, as well as sediment and soil formation and the reconstruction of paleoenvironmental conditions during pedogenesis. Soil provides a medium to store water and support plants in addition to contributing both an available and a labile pool of plant nutrients. Mineral composition is a basic feature of soils which affects physiochemical and biological properties. Comprehensive knowledge on the mineralogy, geochemistry and physical properties of soils is limited. Thus, the Guest Editors are inviting quality research and comprehensive reviews or perspective papers on exploring insights into the mineralogy, geochemistry and physical properties of soil. Manuscripts submitted to this Special Issue will be subjected to a rigorous blind peer-review process.

Dr. Inna Zamulina
Dr. Sudhir S. Shende
Dr. Leonid Perelomov
Guest Editors

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 submissions that pass pre-check are 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. Applied Sciences is an international peer-reviewed open access semimonthly 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 2400 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.

Keywords

  • soil
  • quantitative mineralogy
  • mineral composition
  • soil monitoring
  • mineralization
  • humification

Published Papers (1 paper)

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Research

24 pages, 13905 KiB  
Article
Geochemical and Mineralogical Approaches in Unraveling Paleoweathering, Provenance, and Tectonic Setting of the Clastic Sedimentary Succession (Western Central Paratethys)
by Kristina Ivančič, Rok Brajkovič and Mirijam Vrabec
Appl. Sci. 2024, 14(2), 537; https://doi.org/10.3390/app14020537 - 8 Jan 2024
Viewed by 1053
Abstract
Pronounced tectonic and paleogeographic changes were detected in the Alpine–Pannonian region during the Miocene at the interface between the Alps, the Dinarides, and the Pannonian Basin. To understand the major tectonic, paleogeographic, and paleoclimatic changes during this period, geochemical and mineralogical investigations were [...] Read more.
Pronounced tectonic and paleogeographic changes were detected in the Alpine–Pannonian region during the Miocene at the interface between the Alps, the Dinarides, and the Pannonian Basin. To understand the major tectonic, paleogeographic, and paleoclimatic changes during this period, geochemical and mineralogical investigations were carried out on the fine-grained clastic sedimentary rocks in the Tunjice Hills. The paleoweathering indicates a cold and/or arid to a warm and humid period. The paleoclimate and the regional climatic conditions correspond well with the Middle Miocene Climatic Optimum. The mineral composition shows an abundance of quartz and calcite. Quartz is associated with detrital origin from volcanic and metamorphic rocks of the Eastern and Southern Alps and with authigenic processes in sediments. Calcite is related to authigenic origin formed in shallow marine environments and to detrital provenance from the Southern Alps. Not all discriminant functions based on major oxides provided adequate results in determining the tectonic setting. The source rocks were subjected to oceanic island arc and collision. Moreover, sedimentation was influenced by both active and passive margin settings. The former is related to the Alpine collision, which continued from the Cenozoic onward, and the latter is connected to the processes associated with the formation of the Pannonian Basin System, which began in the late Early Miocene. Full article
(This article belongs to the Special Issue Mineralogy, Geochemistry and Physical Properties of Soil)
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