L. Medici

ORCID: 0000-0001-9426-4653
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About
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Research Areas
  • Clay minerals and soil interactions
  • Crystal Structures and Properties
  • Geological and Geochemical Analysis
  • Iron oxide chemistry and applications
  • Mineralogy and Gemology Studies
  • Geochemistry and Elemental Analysis
  • Paleontology and Stratigraphy of Fossils
  • Minerals Flotation and Separation Techniques
  • Arsenic contamination and mitigation
  • Radioactive element chemistry and processing
  • Adsorption and biosorption for pollutant removal
  • Mercury impact and mitigation studies
  • Metal Extraction and Bioleaching
  • Heavy metals in environment
  • Advanced Thermoelectric Materials and Devices
  • Geochemistry and Geologic Mapping
  • Chemical Synthesis and Characterization
  • Coal and Its By-products
  • X-ray Diffraction in Crystallography
  • Recycling and utilization of industrial and municipal waste in materials production
  • Plant Micronutrient Interactions and Effects
  • Layered Double Hydroxides Synthesis and Applications
  • Zeolite Catalysis and Synthesis
  • Therapeutic Uses of Natural Elements
  • Mine drainage and remediation techniques

National Research Council - Institute of Methodologies for Environmental Analysis
2014-2023

National Research Council
2012-2023

National Academies of Sciences, Engineering, and Medicine
2009

University of Modena and Reggio Emilia
1995-2006

University of Antwerp
2005

University of Bari Aldo Moro
2005

Abstract Silicon (Si) is a beneficial element for plants as it increases their resistance to several biotic and abiotic stresses. In the rhizosphere, root exudates, especially when released by nutritionally stressed plants, promote mineral weathering and, consequently, influence Si biogeochemistry. This study aims at evaluating mineralogical alterations in rhizosphere of Fe‐deficient or Fe‐sufficient barley grown either natural an artificial calcareous soil, focusing on dynamics both Fe Si....

10.1002/jpln.201500535 article EN Journal of Plant Nutrition and Soil Science 2016-05-03

Other| August 01, 1996 Crystal chemistry and petrologic significance of Fe (super 3+) -rich phlogopite from the Tapira carbonatite complex, Brazil Maria Franca Brigatti; Brigatti Universite di Modena, Dipartimento Scienze della Terra, Italy Search for other works by this author on: GSW Google Scholar Luca Medici; Medici Emilio Saccani; Saccani Carmela Vaccaro Author Article Information Publisher: Mineralogical Society America First Online: 02 Mar 2017 Online ISSN: 1945-3027 Print 0003-004X...

10.2138/am-1996-7-814 article EN American Mineralogist 1996-08-01

This study deals with the process of zeolite formation in an agricultural soil artificially polluted by high amounts Cu (15 mg Cu/g dry weight) and treated fused coal fly ash at 30 60 °C how this affects mobility availability metal. As a consequence treatment, amount dissolved Cu, thus its mobility, was strongly reduced, percentage metal stabilized solid phase increased over time, reaching values 30% 40% °C. The physicochemical phenomena responsible for stabilization have been evaluated EDTA...

10.1021/es050079d article EN Environmental Science & Technology 2005-07-16

A clean and cheap procedure for the synthesis of zeolites is presented, using glass aluminum wastes as starting materials. The products are aluminosilicate materials with a high cation exchange capacity (CEC: 259–389.5 meq/100 g) containing 25–30% crystalline zeolites. Since synthesized free potentially toxic elements, they could be safely used environmental agricultural applications. More specifically, material 30% zeolite has been at 60°C in one week, NaOH mineralizing agent. About 15%...

10.1002/clen.201400091 article EN CLEAN - Soil Air Water 2014-06-20

Abstract Mineralogical, geochemical and grain‐size composition of soil pore‐water chemistry parameters were characterized on both eroded (south‐facing) non‐eroded (north‐facing) clayey‐silt slopes in the Basilicata region (southern Italy). Only a few clay mineralogy discriminate from substrates. Compared with latter, former have fractions over 63 µm 1–4 lower 4–63 higher. Grain‐size characters crusts did not respect to substrate. Bulk rock was distinctive, but mineral assemblage shows that...

10.1002/esp.1449 article EN Earth Surface Processes and Landforms 2006-12-08
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