Microstructural Characterization of the Mn Lepidolite Distribution in Dark Red Clay Soils

Lepidolite is one of a small number of minerals that contains a significant amount of lithium. Some areas, like the Apuseni and Metalifer Mountains in Romania, present dark red layers intercalated with reddish-yellow clay soils with interesting aspects. X-ray diffraction (XRD) analysis coupled with...

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Main Authors: Simona Elena Avram, Lucian Barbu Tudoran, Gheorghe Borodi, Ioan Petean
Format: Article
Language:English
Published: MDPI AG 2025-06-01
Series:Applied Sciences
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Online Access:https://www.mdpi.com/2076-3417/15/12/6445
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author Simona Elena Avram
Lucian Barbu Tudoran
Gheorghe Borodi
Ioan Petean
author_facet Simona Elena Avram
Lucian Barbu Tudoran
Gheorghe Borodi
Ioan Petean
author_sort Simona Elena Avram
collection DOAJ
description Lepidolite is one of a small number of minerals that contains a significant amount of lithium. Some areas, like the Apuseni and Metalifer Mountains in Romania, present dark red layers intercalated with reddish-yellow clay soils with interesting aspects. X-ray diffraction (XRD) analysis coupled with polarized light optical microscopy (POM) revealed that this dark red soil contains a large amount of fine microstructured lepidolite (24–35%) mixed with quartz sand and fine traces of kaolinite and muscovite. Scanning electron microscopy (SEM) elemental analysis revealed a typical clay composition with Mn traces (specific to red lepidolite), confirming POM observation. SEM also revealed fine tabular platelets of lepidolite with a maximum size of 1.5 µm surrounding quartz particles (5–50 µm), indicating the presence of numerous nano fractions. Their presence was confirmed by atomic force microscopy (AFM), which showed particle sizes ranging from 40 to 60 nm, closely matching the crystallite size estimated using the Scherrer formula. The finest fraction allows easy separation from the quartz sand through bi-distilled water washing. Quartz particles settle at the bottom of the container, while the finest lepidolite particles are easily separated. Water evaporation ensures their recovery. Thus, the enriched lepidolite powder could be utilized for specific applications in the lithium industry. On the other hand, the large number of the finest particles found in the samples investigated presents the risk of PM1, PM2.5m, and PM10 emission, with impacts on atmospheric environmental safety.
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spelling doaj-art-781b9575bec44e53b4d1a848ea1c6b4e2025-08-20T03:26:09ZengMDPI AGApplied Sciences2076-34172025-06-011512644510.3390/app15126445Microstructural Characterization of the Mn Lepidolite Distribution in Dark Red Clay SoilsSimona Elena Avram0Lucian Barbu Tudoran1Gheorghe Borodi2Ioan Petean3Faculty of Materials and Environmental Engineering, Technical University of Cluj-Napoca, 103-105 Muncii Bd., 400641 Cluj-Napoca, RomaniaFaculty of Biology and Geology, Babes-Bolyai University, 44 Gheorghe Bilaşcu Street, 400015 Cluj-Napoca, RomaniaNational Institute for Research and Development of Isotopic and Molecular Technologies, 65-103 Donath Street, 400293 Cluj-Napoca, RomaniaFaculty of Chemistry and Chemical Engineering, Babes-Bolyai University, 11 Arany Janos Street, 400028 Cluj-Napoca, RomaniaLepidolite is one of a small number of minerals that contains a significant amount of lithium. Some areas, like the Apuseni and Metalifer Mountains in Romania, present dark red layers intercalated with reddish-yellow clay soils with interesting aspects. X-ray diffraction (XRD) analysis coupled with polarized light optical microscopy (POM) revealed that this dark red soil contains a large amount of fine microstructured lepidolite (24–35%) mixed with quartz sand and fine traces of kaolinite and muscovite. Scanning electron microscopy (SEM) elemental analysis revealed a typical clay composition with Mn traces (specific to red lepidolite), confirming POM observation. SEM also revealed fine tabular platelets of lepidolite with a maximum size of 1.5 µm surrounding quartz particles (5–50 µm), indicating the presence of numerous nano fractions. Their presence was confirmed by atomic force microscopy (AFM), which showed particle sizes ranging from 40 to 60 nm, closely matching the crystallite size estimated using the Scherrer formula. The finest fraction allows easy separation from the quartz sand through bi-distilled water washing. Quartz particles settle at the bottom of the container, while the finest lepidolite particles are easily separated. Water evaporation ensures their recovery. Thus, the enriched lepidolite powder could be utilized for specific applications in the lithium industry. On the other hand, the large number of the finest particles found in the samples investigated presents the risk of PM1, PM2.5m, and PM10 emission, with impacts on atmospheric environmental safety.https://www.mdpi.com/2076-3417/15/12/6445clay soilsLepidolitemicrostructural distributionwashing separation
spellingShingle Simona Elena Avram
Lucian Barbu Tudoran
Gheorghe Borodi
Ioan Petean
Microstructural Characterization of the Mn Lepidolite Distribution in Dark Red Clay Soils
Applied Sciences
clay soils
Lepidolite
microstructural distribution
washing separation
title Microstructural Characterization of the Mn Lepidolite Distribution in Dark Red Clay Soils
title_full Microstructural Characterization of the Mn Lepidolite Distribution in Dark Red Clay Soils
title_fullStr Microstructural Characterization of the Mn Lepidolite Distribution in Dark Red Clay Soils
title_full_unstemmed Microstructural Characterization of the Mn Lepidolite Distribution in Dark Red Clay Soils
title_short Microstructural Characterization of the Mn Lepidolite Distribution in Dark Red Clay Soils
title_sort microstructural characterization of the mn lepidolite distribution in dark red clay soils
topic clay soils
Lepidolite
microstructural distribution
washing separation
url https://www.mdpi.com/2076-3417/15/12/6445
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AT lucianbarbutudoran microstructuralcharacterizationofthemnlepidolitedistributionindarkredclaysoils
AT gheorgheborodi microstructuralcharacterizationofthemnlepidolitedistributionindarkredclaysoils
AT ioanpetean microstructuralcharacterizationofthemnlepidolitedistributionindarkredclaysoils