XRD and TEM analyses of a simulated leached rare earth ore deposit: Implications for clay mineral contents and structural evolution

The types, contents, and microstructures of clay minerals play important roles in controlling the adsorption and desorption of ion-absorbed type rare earth ores and heavy metals. By selecting a typical rare earth ore profile, we conducted a leaching experiment and used XRD (X-ray diffraction) and TE...

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Main Authors: Xiongwei Jin, Lingkang Chen, Haixia Chen, Lian Zhang, Wenjing Wang, Hong Ji, Shaofu Deng, Lei Jiang
Format: Article
Language:English
Published: Elsevier 2021-12-01
Series:Ecotoxicology and Environmental Safety
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S014765132100840X
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spelling doaj-8edcb292c5b6462a85eff6759272f7ae2021-10-01T04:42:41ZengElsevierEcotoxicology and Environmental Safety0147-65132021-12-01225112728XRD and TEM analyses of a simulated leached rare earth ore deposit: Implications for clay mineral contents and structural evolutionXiongwei Jin0Lingkang Chen1Haixia Chen2Lian Zhang3Wenjing Wang4Hong Ji5Shaofu Deng6Lei Jiang7College of Sciences, Guangdong University of Petrochemical Technology, Maoming 525000, China; School of Resource and Environmental Engineering, Jiangxi University of Science and Technology, Ganzhou 341000, ChinaCollege of Sciences, Guangdong University of Petrochemical Technology, Maoming 525000, China; School of Resource and Environmental Engineering, Jiangxi University of Science and Technology, Ganzhou 341000, China; Correspondence to: College of Sciences, Guangdong University of Petrochemical Technology, Maoming city of Guangdong Province in 139 Guandu Avenue, Maoming 525000, China.College of Petroleum Engineering, Guangdong University of Petrochemical Technology, Maoming 525000, China; Correspondence to: College of Petroleum Engineering, Guangdong University of Petrochemical Technology, Maoming city of Guangdong Province in 1 Kechuang Avenue, Maoming 525000, China.School of Water Resources and Environment, China University of Geosciences(Beijin), Beijing 100083, ChinaAnalysis and Testing Center, Jiangxi University of Science and Technology, Ganzhou 341000, ChinaCollege of Sciences, Guangdong University of Petrochemical Technology, Maoming 525000, ChinaCollege of Sciences, Guangdong University of Petrochemical Technology, Maoming 525000, ChinaCollege of Sciences, Guangdong University of Petrochemical Technology, Maoming 525000, ChinaThe types, contents, and microstructures of clay minerals play important roles in controlling the adsorption and desorption of ion-absorbed type rare earth ores and heavy metals. By selecting a typical rare earth ore profile, we conducted a leaching experiment and used XRD (X-ray diffraction) and TEM (Transmission electron microscopy) analyses to determine the clay mineral types and microstructural changes after various leaching periods. The XRD phase analyses showed that the main minerals in the simulated rare earth ore were quartz, potassium feldspar, kaolinite, and illite. TEM images showed that the mineral aggregates were broken, disintegrated, and transformed by the leaching process, and a large number of moire fringes were visible. With continuous leaching, REEs (Rare Earth Elements) were gradually re-solved and leached. The results of the leaching experiment indicate that fine-grained minerals in rare earth ores, such as potassium feldspar and clay minerals, migrated downward with the leaching solution. Leaching also promoted the alteration of potassium feldspar to clay minerals, as well as mutual alteration of clay minerals. Under acidic or neutral conditions during the early stage, potassium feldspar was altered to kaolinite or illite, whereas during the middle and late stages of leaching it was altered as follows: illite → mixed-layer illite–kaolinite → kaolinite → mixed-layer kaolinite–illite → illite. This transformation has an important effect on the release of REEs and heavy metals and provides insights into improving the leaching process and explaining heavy metal pollution in rare earth mining areas.http://www.sciencedirect.com/science/article/pii/S014765132100840XIon-absorbed type rare earth oreSimulated leachingClay mineralMicrostructural transformationHeavy metal
collection DOAJ
language English
format Article
sources DOAJ
author Xiongwei Jin
Lingkang Chen
Haixia Chen
Lian Zhang
Wenjing Wang
Hong Ji
Shaofu Deng
Lei Jiang
spellingShingle Xiongwei Jin
Lingkang Chen
Haixia Chen
Lian Zhang
Wenjing Wang
Hong Ji
Shaofu Deng
Lei Jiang
XRD and TEM analyses of a simulated leached rare earth ore deposit: Implications for clay mineral contents and structural evolution
Ecotoxicology and Environmental Safety
Ion-absorbed type rare earth ore
Simulated leaching
Clay mineral
Microstructural transformation
Heavy metal
author_facet Xiongwei Jin
Lingkang Chen
Haixia Chen
Lian Zhang
Wenjing Wang
Hong Ji
Shaofu Deng
Lei Jiang
author_sort Xiongwei Jin
title XRD and TEM analyses of a simulated leached rare earth ore deposit: Implications for clay mineral contents and structural evolution
title_short XRD and TEM analyses of a simulated leached rare earth ore deposit: Implications for clay mineral contents and structural evolution
title_full XRD and TEM analyses of a simulated leached rare earth ore deposit: Implications for clay mineral contents and structural evolution
title_fullStr XRD and TEM analyses of a simulated leached rare earth ore deposit: Implications for clay mineral contents and structural evolution
title_full_unstemmed XRD and TEM analyses of a simulated leached rare earth ore deposit: Implications for clay mineral contents and structural evolution
title_sort xrd and tem analyses of a simulated leached rare earth ore deposit: implications for clay mineral contents and structural evolution
publisher Elsevier
series Ecotoxicology and Environmental Safety
issn 0147-6513
publishDate 2021-12-01
description The types, contents, and microstructures of clay minerals play important roles in controlling the adsorption and desorption of ion-absorbed type rare earth ores and heavy metals. By selecting a typical rare earth ore profile, we conducted a leaching experiment and used XRD (X-ray diffraction) and TEM (Transmission electron microscopy) analyses to determine the clay mineral types and microstructural changes after various leaching periods. The XRD phase analyses showed that the main minerals in the simulated rare earth ore were quartz, potassium feldspar, kaolinite, and illite. TEM images showed that the mineral aggregates were broken, disintegrated, and transformed by the leaching process, and a large number of moire fringes were visible. With continuous leaching, REEs (Rare Earth Elements) were gradually re-solved and leached. The results of the leaching experiment indicate that fine-grained minerals in rare earth ores, such as potassium feldspar and clay minerals, migrated downward with the leaching solution. Leaching also promoted the alteration of potassium feldspar to clay minerals, as well as mutual alteration of clay minerals. Under acidic or neutral conditions during the early stage, potassium feldspar was altered to kaolinite or illite, whereas during the middle and late stages of leaching it was altered as follows: illite → mixed-layer illite–kaolinite → kaolinite → mixed-layer kaolinite–illite → illite. This transformation has an important effect on the release of REEs and heavy metals and provides insights into improving the leaching process and explaining heavy metal pollution in rare earth mining areas.
topic Ion-absorbed type rare earth ore
Simulated leaching
Clay mineral
Microstructural transformation
Heavy metal
url http://www.sciencedirect.com/science/article/pii/S014765132100840X
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