Mineralogical and Chemical Characterization of Rocks, Soils, Sediments, and Water Containing Hazardous Substances

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Environmental Mineralogy and Biogeochemistry".

Deadline for manuscript submissions: 31 July 2025 | Viewed by 548

Special Issue Editors


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Guest Editor
Earth Sciences Department, University of Pisa, Via S. Maria 53, 56126 Pisa, Italy
Interests: potentially toxic elements; mercury; arsenic; chromium; nickel; environmental geochemistry; ore deposits; direct mercury analyzer (DMA-80); ICP-MS; trace element; geochemistry; environmental remediation; minerals; geological processes; field geology; soil; sediments; water; applied mineralogy; mineralization; asbestos; mine waste; mining critical raw materials; geochemical background; geochemical baseline

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Guest Editor
Institute of Geology and Geophysics named after Kh.M.Abdullaev, University of Geological Sciences, Ministry of Mining Industry and Geology of the Republic of Uzbekistan, 64G Olimlar street, Tashkent 100164, Uzbekistan
Interests: biogeochemistry; environmental geochemistry, mineralogy, and microbiology of contaminated soils in mining sites and industrial cities; organic contaminants (PAHs, OPAHs) and air-born metal reach particles in soil surface in mining industrial areas; bioindication and bioremediation aspects of polluted sites
Special Issues, Collections and Topics in MDPI journals

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Guest Editor
Center for Ecological Noosphere Studies of the National Academy of Sciences of the Republic of Armenia, Yerevan, 0025, Abovian-68, Armenia
Interests: environmental geochemistry; urban geochemistry, soil survey; mining areas; sediments; water; potentially toxic elements; rare earth elements; risk assessment; nature-based solutions; XRF; XRD; geochemical background; geochemical baseline; geostatistics; geospatial mapping
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

Hazardous substances (HSs) include inorganic contaminants such as potentially toxic elements (PTEs) and technology-critical elements (TCEs) and organic contaminants such as emerging contaminants, pesticides, POPs, mycotoxins, PAHs. These substances can naturally accumulate in soil, sediments, and/or water during the weathering of rocks or other natural processes. In addition, they can be supplied by anthropogenic activities such as mining, industrial, urban, or agricultural activities.

The environmental contamination of HSs is becoming increasingly serious in many countries around the world, along with urbanization and industrialization, which pose a severe hazard to ecosystems and human health. The increased content of HSs can adversely affect the biological properties of the soil–sediment–water system, cause changes in the food chain, have a toxic effect on plants, and can contaminate groundwater.

The main aim of this Special Issue “Mineralogical and Chemical Characterization of Rocks, Soils, Sediments, and Water Containing Hazardous Substances” is to further our understanding of the natural and anthropogenic processes that occur in different environmental matrices at various scales, from a bulk, micron-scale, and nanoscale to an atomic scale. For this reason, we encourage the submission of original papers related to field studies, laboratory experiments, and mineralogical and chemical characterizations with a focus on inorganic and organic geochemistry, metal speciation, contaminant and pollutant mobility and behavior, the distribution and weathering of minerals, and the dynamics of natural and anthropogenic materials and elements in rocks, soils, sediments, and water.

This Special Issue aims to cover a broad range of topics relevant to the presence of HSs in different ecosystems, including (but not limited to):

  • The main factors conditioning HS mobility under specified conditions and consequences.
  • Detailed HS partition among minerals and associated potential mobility.
  • Establishment of sources of HS causing contamination in soil, sediments, or water.
  • Weathering of HS-bearing rocks and mining wastes.

The aim of this Special Issue is to bring together researchers from different fields involving geochemistry and mineralogy in soil, sediment, and water to provide a more comprehensive understanding of the natural and anthropogenic cycles of trace elements.

We look forward to receiving your contribution.

Dr. Silvia Fornasaro
Prof. Dr. Nosir Shukurov
Dr. Gevorg Tepanosyan
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. 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 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

  • potentially toxic elements
  • emerging organic contaminants
  • technology-critical elements
  • elemental mobility
  • risk assessment
  • rock weathering
  • geogenic vs. anthropogenic sources
  • persistent organic pollutants
  • metal-rich airborne particles

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Published Papers (1 paper)

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29 pages, 11095 KiB  
Article
Uranium Mineral Particles Produced by Weathering in Sierra Peña Blanca, Chihuahua, Mexico: A Synchrotron-Based Study
by Cristina Hernández-Herrera, Jesús G. Canché-Tello, Yair Rodríguez-Guerra, Fabián G. Faudoa-Gómez, Diane M. Eichert, Konstantin Ignatyev, Rocío M. Cabral-Lares, Victoria Pérez-Reyes, Hilda E. Esparza-Ponce and María-Elena Montero-Cabrera
Minerals 2025, 15(4), 333; https://doi.org/10.3390/min15040333 - 22 Mar 2025
Viewed by 203
Abstract
Some of the largest Mexican uranium (U) deposits are located in Chihuahua. The most important is in Sierra Peña Blanca, northwest of the capital, which was explored and partially exploited in the 1980s. After the closure of activities, the mining projects were left [...] Read more.
Some of the largest Mexican uranium (U) deposits are located in Chihuahua. The most important is in Sierra Peña Blanca, northwest of the capital, which was explored and partially exploited in the 1980s. After the closure of activities, the mining projects were left exposed to weathering. To characterize the spread of U minerals towards the neighboring Laguna del Cuervo, sediment samples were collected in the main streams of the drainage pattern of the largest deposits. The U mineral fragments from the fine sand portion were extracted using fluorescence light at 365 nm. The morphology and elemental composition of these particles were analyzed by focused ion beam microscopy (FIB) and scanning transmission electron microscopy (STEM). The particle density in samples close to the U sources was quantified using gamma spectrometry. The highest density was 2500 part./g, and the lowest was 124 part./g. X-ray absorption spectroscopy (XAS) allowed us to establish via XANES the speciation of U in the U particles, confirming the U(VI) oxidation state, while the exploitation of the EXAFS spectrum put in evidence of the presence of uranophane. Finally, the Fe, Sr, and U distributions in the particle and its matrix were obtained via X-ray fluorescence microtomography (XRF-µCT). It was concluded that the particle is composed of uranophane, imbricated with quartz and other oxides. Full article
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