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广东某地高岭土的特征研究
引用本文:李晨, 管俊芳, 方纪, 吕灏. 广东某地高岭土的特征研究[J]. 西北地质, 2017, 50(3): 140-145.
作者姓名:李晨  管俊芳  方纪  吕灏
作者单位:武汉理工大学 资源与环境工程学院, 湖北 武汉 430070
基金项目:中央高校基本科研业务费专项资金资助项目(155208002,2015-zy-078)
摘    要:通过光学显微镜、X射线衍射(XRD)、X射线荧光光谱(XRF)、电子探针和扫描电镜(SEM)等手段,对广东某高岭土进行了系统研究。研究表明,该高岭土淘洗率为71%。石英和钾长石在+0.045 mm粒级中富集;白云母在+0.030 mm粒级富集;高岭石(埃洛石)在-0.045 mm粒级中富集。各粒级烧成白度较高,-0.010+0.005 mm粒级烧成白度最高,达到85.69%。目的矿物高岭石为片状和叠片状,埃洛石为管状。高岭土中Ti含量较低,为0.051%,Fe含量较高,为1.009%,主要以表面铁和晶格铁形式存在。

关 键 词:高岭土   工艺矿物学   煅烧增白
收稿时间:2017-01-10
修稿时间:2017-05-08

Study on the Characteristics of Kaolin from Some Area in Guangdong Province
LI Chen, GUAN Junfang, FANG Ji, LÜ Hao. Study on the Characteristics of Kaolin from Some Area in Guangdong Province[J]. Northwestern Geology, 2017, 50(3): 140-145.
Authors:LI Chen  GUAN Junfang  FANG Ji  LÜ Hao
Affiliation:School of Resource and Environmental Engineering, Wuhan University of Technology, Wuhan 430070, Hubei, China
Abstract:This paper made systematic studies on kaolin by means of optical microscope, X-ray diffraction (XRD), X-ray fluorescence spectrum(XRF), electron probe and scanning electron microscope (SEM). Results show that the elutriation rate of kaolin is 71%.Quartz and potash feldspar were enriched as -0.045mm size; Muscovite and kaolinite (halloysite) were enriched as +0.030 mm and -0.045mm size, respectively.After calcinations, the whiteness of each particle size is high, especially in -0.010+0.005mm, with the whiteness reached to 85.69%. Kaolinite, the objective mineral, shows patchy and overlapping shape. Halloysiteshows tubular form. The titanium content of kaolin is 0.051%. However, itsiron content is higher,which reaches 1.009% and mainly exists as the forms of surface iron and lattice iron.
Keywords:kaolin  process mineralogy  whiteness
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