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Investigating the expanding behavior and thermal stability of HDPy modified organo-bentonite by X-ray diffraction technique

机译:用X射线衍射技术研究HDPy改性有机膨润土的膨胀行为和热稳定性

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摘要

Bentonites are commonly used in scientific investigations and industrial applications due to their superior properties. As they have high cation exchange capacity (CEC), they are widely used as an adsorbent in pollution control. Although their cation adsorption capability is greater, their organic and anionic material adsorption ability is very limited or non-existent. Fortunately, this limitation can be eliminated by intercalation of organic or/and inorganic cations into their structure. Changes due to modification should be identified by characterization techniques in order to figure out realized structural changes. In this study, it is aimed to use X-ray powder diffraction (XRD) technique in order to clarify the expanding behavior and thermal stability of HDPy modified organo-bentonite. For this purpose, organo-bentonite (OBent) was synthesized by intercalation of organic surfactant, hexadecylpyridinium cation (HDPy), into purified bentonite (PBent). Products were characterized by X-ray powder diffraction (XRD) using CuK alpha radiation under various conditions: solvation with water and ethylene glycol (EG) and heat treatments at 100 degrees C, 350 degrees C and 550 degrees C. Existence of mixed-layer clay formation was investigated and PBent and OBent XRD patterns were simulated by NEWMOD software. The PBent sample contains small amounts of mixed layer illite/smectite. Results of XRD analysis supports the notion that HDPy+ is intercalated within interlayer and basal spacing increases from 12.29 to 18.84 angstrom. Degradation of the organic cation is observed, however some residues from intercalate still appears to remain in the structure upon heating up to 550 degrees C. The persistence of these intercalates in OBent over a wide range of temperature holds promise for their use in environmental remediation studies and gaining a better understanding of the mechanisms of interaction with pollutants. Furthermore, this study presents a new perspective in examining the expanding behavior and thermal stability of organo-bentonites and investigating the existence of mixed-layer clay in organo-bentonites by using X-ray powder diffraction (XRD) technique with different treatments. (C) 2016 Elsevier B.V. All rights reserved.
机译:膨润土由于其优异的性能而通常用于科学研究和工业应用。由于它们具有高阳离子交换容量(CEC),因此在污染控制中被广泛用作吸附剂。尽管它们的阳离子吸附能力更大,但它们对有机和阴离子材料的吸附能力却非常有限或根本不存在。幸运的是,可以通过将有机或/和无机阳离子插入其结构中来消除这种限制。因修改而引起的变化应通过特性分析技术加以识别,以便找出已实现的结构变化。在本研究中,目的是使用X射线粉末衍射(XRD)技术来阐明HDPy改性有机膨润土的膨胀行为和热稳定性。为此,通过将有机表面活性剂十六烷基吡啶鎓阳离子(HDPy)嵌入纯化的膨润土(PBent)中来合成有机膨润土(OBent)。通过在各种条件下使用CuKα辐射通过X射线粉末衍射(XRD)对产品进行表征:用水和乙二醇(EG)进行溶剂化,并在100摄氏度,350摄氏度和550摄氏度进行热处理。存在混合层研究了粘土的形成,并通过NEWMOD软件模拟了PBent和OBent XRD图谱。 PBent样品包含少量的混合层伊利石/蒙脱石。 XRD分析的结果支持以下观点:HDPy +插入层间,并且基底间距从12.29埃增加到18.84埃。观察到有机阳离子的降解,但是在加热到550摄氏度时,嵌入物的一些残留物似乎仍然保留在结构中。这些嵌入物在很宽的温度范围内在OBent中的持久性为其在环境修复研究中的应用提供了希望并更好地了解与污染物相互作用的机制。此外,本研究为研究有机膨润土的膨胀行为和热稳定性以及通过使用不同处理的X射线粉末衍射(XRD)技术研究有机膨润土中混合层粘土的存在提供了新的视角。 (C)2016 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《Applied clay science》 |2016年第11期|90-95|共6页
  • 作者

    Orucoglu E.; Schroeder P. A.;

  • 作者单位

    Istanbul Tech Univ, Fac Mines, TR-34469 Istanbul, Turkey;

    Istanbul Tech Univ, Fac Mines, TR-34469 Istanbul, Turkey|Univ Georgia UGA, Dept Geol, Athens, GA 30602 USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Organo-bentonite; Bentonite; HDPy+; X-ray diffraction; NEWMOD;

    机译:有机膨润土;膨润土;HDPy +;X射线衍射;NEWMOD;
  • 入库时间 2022-08-17 13:54:01

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