莫尔卢卡斯省哈图村天然粘土和酸活性粘土的特征:傅立叶变换红外光谱(FTIR)、X 射线衍射(XRD)、X 射线荧光(XRF)、扫描电子显微镜(SEM-EDX)、电子显微镜(TEM)和 BET 分析

Q3 Chemistry Molekul Pub Date : 2023-11-20 DOI:10.20884/1.jm.2023.18.3.8316
S. J. Sekewael, M. Maahury
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引用次数: 0

摘要

使用傅立叶变换红外光谱(FTIR)、XRD、XRF、SEM-EDX、TEM 和 BET 表面积分析仪,对 Hatu 村的天然粘土和酸活化粘土的化学和物理特性进行了研究。天然粘土用 0.25 M 硫酸回流法活化 3 小时,然后用 700 瓦微波辐射煅烧 10 分钟。总体而言,傅立叶变换红外光谱数据显示了形成粘土矿物的四面体和八面体官能团。由于酸的影响,八面体和层间粘土中的阳离子被溶解,导致吸收强度下降。XRD 分析表明,哈图天然粘土含有蒙脱石、明矾石、高岭石、石英和伊利石矿物。经酸和煅烧处理后,衍射峰变宽,强度降低。活化煅烧前后天然粘土的扫描电镜图像显示了多孔和分层材料的形态,而天然粘土表面的绘图显示了不规则和粗糙的材料形貌。乙二胺四乙酸(EDX)光谱显示,四种元素的组成最为广泛:O、Si、Al 和 Fe。XRF 数据证实了质量百分比最高的三种成分,即 SiO2、Al2O3 和 Fe2O3。由于硫酸的活化和煅烧作用,脱铝率达到 0.95%。TEM 图像清楚地显示了多层硅酸盐材料。活化煅烧天然粘土对氮气的吸收率较高,这与它的大表面积和总孔隙体积成正比。
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Characteristic of Natural and Acid-activated Clay From Hatu Village, Mollucas Province: FTIR, XRD, XRF, SEM-EDX, TEM, and BET Analysis
Research on the chemical and physical characteristics of natural and acid-activated clay from Hatu Village had been carried out using FTIR, XRD, XRF, SEM-EDX, TEM, and BET surface area analyzer instruments. The natural clay had activated with 0.25 M sulfuric acid for 3 hours using the reflux method, then calcined with 700 Watt microwave radiation for 10 minutes. Overall, FTIR data show tetrahedral and octahedral functional groups that create clay minerals. There is a decrease in absorption intensity due to acid's influence, which dissolves cations in the octahedral and interlayer clay. The XRD analysis shows the Hatu natural clay contains montmorillonite, alumina, kaolinite, quartz, and illite minerals. Broadening and decreasing the intensity of diffraction peaks due to treatment by acid and calcination. SEM images of natural clay before and after activation-calcination shows the morphology of porous and layered material, while the mapping of the surface of natural clay shows irregular and rough material topography. The EDX spectra showed four elements with the most extensive composition: O, Si, Al, and Fe. XRF data confirmed three components that have the highest mass percent, namely SiO2, Al2O3, and Fe2O3. Dealumination occurs at 0.95% due to activation by sulfuric acid along with calcination. TEM images clearly show the multilayered silicate materials. The higher nitrogen gas uptake by activated-calcinated natural clay is proportional to the large surface area and total pore volume.
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来源期刊
Molekul
Molekul Chemistry-Chemistry (all)
CiteScore
1.30
自引率
0.00%
发文量
31
审稿时长
4 weeks
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