Quantitative XRD Analysis of the Structural Changes of Ba-Exchanged Montmorillonite: Effect of an in Situ Hydrous Perturbation

The structural changes along the c axis, of the Ba-exchanged montmorillonite (Swy-2-Ba), under variable relative humidity (% RH), is investigated. In this regard, the arrangement, amount and position of both exchangeable cation and the water molecules in the interlamellar space (IS), are evaluated....

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Main Authors: Walid Oueslati, Marwa Ammar, Nejmeddine Chorfi
Format: Article
Language:English
Published: MDPI AG 2015-08-01
Series:Minerals
Subjects:
Online Access:http://www.mdpi.com/2075-163X/5/3/507
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spelling doaj-d162753ade88413fa499d68602c511462020-11-24T21:20:06ZengMDPI AGMinerals2075-163X2015-08-015350752610.3390/min5030507min5030507Quantitative XRD Analysis of the Structural Changes of Ba-Exchanged Montmorillonite: Effect of an in Situ Hydrous PerturbationWalid Oueslati0Marwa Ammar1Nejmeddine Chorfi2Departement de Physique, Faculté des Sciences de Bizerte, Université de Carthage, Zarzouna 7021, TunisiaDepartement de Physique, Faculté des Sciences de Bizerte, Université de Carthage, Zarzouna 7021, TunisiaDepartment of Mathematics, College of Science, King Saud University, P.O. Box 2455, Riyadh 11451, Saudi ArabiaThe structural changes along the c axis, of the Ba-exchanged montmorillonite (Swy-2-Ba), under variable relative humidity (% RH), is investigated. In this regard, the arrangement, amount and position of both exchangeable cation and the water molecules in the interlamellar space (IS), are evaluated. This aim is achieved using the X-ray diffraction (XRD) profile modeling approach that consists of comparing experimental and theoretical patterns calculated from structural models. The contributions of the hydration states and the interlayer water amounts, as a function of the % RH, are registered by quantitative XRD investigation. The validated structural models are heterogeneous, suggesting various proportions of layer types at different RH ranges, which means the coexistence of different mixed layer structure MLS packages, exhibiting different proportions of layers with contrasting hydration states. This result is attributed to the orientation of the applied hydration sequence. Indeed, the interlayer water molecule amounts, which led to the appearance of a logic hydration hysteresis, are strongly affected by hydrous perturbation.http://www.mdpi.com/2075-163X/5/3/507cation exchangedehydrationclay mineralsX-ray diffraction (XRD)
collection DOAJ
language English
format Article
sources DOAJ
author Walid Oueslati
Marwa Ammar
Nejmeddine Chorfi
spellingShingle Walid Oueslati
Marwa Ammar
Nejmeddine Chorfi
Quantitative XRD Analysis of the Structural Changes of Ba-Exchanged Montmorillonite: Effect of an in Situ Hydrous Perturbation
Minerals
cation exchange
dehydration
clay minerals
X-ray diffraction (XRD)
author_facet Walid Oueslati
Marwa Ammar
Nejmeddine Chorfi
author_sort Walid Oueslati
title Quantitative XRD Analysis of the Structural Changes of Ba-Exchanged Montmorillonite: Effect of an in Situ Hydrous Perturbation
title_short Quantitative XRD Analysis of the Structural Changes of Ba-Exchanged Montmorillonite: Effect of an in Situ Hydrous Perturbation
title_full Quantitative XRD Analysis of the Structural Changes of Ba-Exchanged Montmorillonite: Effect of an in Situ Hydrous Perturbation
title_fullStr Quantitative XRD Analysis of the Structural Changes of Ba-Exchanged Montmorillonite: Effect of an in Situ Hydrous Perturbation
title_full_unstemmed Quantitative XRD Analysis of the Structural Changes of Ba-Exchanged Montmorillonite: Effect of an in Situ Hydrous Perturbation
title_sort quantitative xrd analysis of the structural changes of ba-exchanged montmorillonite: effect of an in situ hydrous perturbation
publisher MDPI AG
series Minerals
issn 2075-163X
publishDate 2015-08-01
description The structural changes along the c axis, of the Ba-exchanged montmorillonite (Swy-2-Ba), under variable relative humidity (% RH), is investigated. In this regard, the arrangement, amount and position of both exchangeable cation and the water molecules in the interlamellar space (IS), are evaluated. This aim is achieved using the X-ray diffraction (XRD) profile modeling approach that consists of comparing experimental and theoretical patterns calculated from structural models. The contributions of the hydration states and the interlayer water amounts, as a function of the % RH, are registered by quantitative XRD investigation. The validated structural models are heterogeneous, suggesting various proportions of layer types at different RH ranges, which means the coexistence of different mixed layer structure MLS packages, exhibiting different proportions of layers with contrasting hydration states. This result is attributed to the orientation of the applied hydration sequence. Indeed, the interlayer water molecule amounts, which led to the appearance of a logic hydration hysteresis, are strongly affected by hydrous perturbation.
topic cation exchange
dehydration
clay minerals
X-ray diffraction (XRD)
url http://www.mdpi.com/2075-163X/5/3/507
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AT marwaammar quantitativexrdanalysisofthestructuralchangesofbaexchangedmontmorilloniteeffectofaninsituhydrousperturbation
AT nejmeddinechorfi quantitativexrdanalysisofthestructuralchangesofbaexchangedmontmorilloniteeffectofaninsituhydrousperturbation
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