Characterization of Brazilian palygorskite (Guadalupe region) and adsorptive behaviour for solvatochromic dyes

IF 1.1 4区 地球科学 Q4 CHEMISTRY, PHYSICAL
Clay Minerals Pub Date : 2021-04-28 DOI:10.1180/CLM.2021.16
C. D. de Souza, Tammy Caroline Lima de Jesus, Rafael C. dos Santos, Lívia Melo Bomfim, L. Bertolino, Débora F. de Andrade, L. A. d´Avila, L. Spinelli
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引用次数: 3

Abstract

This work presents the results of the physical characterization of palygorskite and its adsorptive behaviour for three solvatochromic dyes (Nile blue chloride (NBC), methylene blue (MTB) and dithizone (DTZ)). Adsorption isotherms were used to determine the maximum adsorption of the solvatochromic dyes on the palygorskite. The characterization of palygorskite was carried out via mineralogical and chemical analysis with X-ray diffraction, X-ray fluorescence, scanning electron microscopy (SEM), transmission electron microscopy (TEM), Fourier-transform infrared spectroscopy, surface-charge measurement (ζ-potential), thermogravimetric analysis, textural analysis and cation-exchange capacity analysis. The material consists of palygorskite and quartz and its chemistry is dominated by SiO2, MgO and Fe2O3. The specific surface area and cation-exchange capacity of the palygorskite are 142 m2 g–1 and 41 cmol(+) kg–1, respectively. The SEM and TEM analyses showed a fibrous structure with fibres 20–100 nm long. The thermogravimetric analysis showed three endothermic events at 57.3°C, 171.8°C and 439.6°C. The adsorption capacities of the palygorskite for NBC (basic pH), MTB (basic pH) and DTZ (neutral pH) were 0.082, 0.013 and 0.102 g g–1, respectively. The adsorptions of NBC and MTB were fitted with the Langmuir isotherm model and the adsorption of DTZ was fitted with the Sips model.
巴西斜长石(瓜达卢佩地区)的表征及其对溶剂变色染料的吸附行为
本文介绍了坡缕石的物理性质及其对三种溶剂化变色染料(氯化尼罗蓝(NBC)、亚甲基蓝(MTB)和双硫腙(DTZ))的吸附行为。用吸附等温线测定了溶剂化变色染料在坡缕石上的最大吸附量。通过矿物学和化学分析,采用X射线衍射、X射线荧光、扫描电子显微镜(SEM)、透射电子显微镜(TEM)、傅立叶变换红外光谱、表面电荷测量(ζ-电位)、热重分析、结构分析和阳离子交换容量分析,对坡缕石进行了表征。该材料由坡缕石和石英组成,其化学成分以SiO2、MgO和Fe2O3为主。坡缕石的比表面积和阳离子交换容量分别为142 m2 g–1和41 cmol(+)kg–1。SEM和TEM分析显示纤维结构为20–100 nm长。热重分析显示,在57.3°C、171.8°C和439.6°C下发生了三次吸热事件。坡缕石对NBC(碱性pH)、MTB(碱性pH值)和DTZ(中性pH值)的吸附容量分别为0.082、0.013和0.102 g g–1。NBC和MTB的吸附符合Langmuir等温线模型,DTZ的吸附符合Sips模型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Clay Minerals
Clay Minerals 地学-矿物学
CiteScore
3.00
自引率
20.00%
发文量
25
审稿时长
6 months
期刊介绍: Clay Minerals is an international journal of mineral sciences, published four times a year, including research papers about clays, clay minerals and related materials, natural or synthetic. The journal includes papers on Earth processes soil science, geology/mineralogy, chemistry/material science, colloid/surface science, applied science and technology and health/ environment topics. The journal has an international editorial board with members from fifteen countries.
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