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Determination of chlorite, muscovite, albite and quartz in claystones and clay shales by infrared spectroscopy and partial least-squares regression

  1. 1.
    SYSNO ASEP0449356
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleDetermination of chlorite, muscovite, albite and quartz in claystones and clay shales by infrared spectroscopy and partial least-squares regression
    Author(s) Ritz, M. (CZ)
    Vaculíková, Lenka (UGN-S) RID, ORCID
    Plevová, Eva (UGN-S) RID, ORCID
    Matýsek, D. (CZ)
    Mališ, J. (CZ)
    Number of authors5
    Source TitleActa geodynamica et geomaterialia. - : Ústav struktury a mechaniky hornin AV ČR, v. v. i. - ISSN 1214-9705
    Roč. 9, č. 4 (2012), s. 511-520
    Number of pages10 s.
    Publication formOnline - E
    Languageeng - English
    CountryCZ - Czech Republic
    Keywordsclaystone and clay shale ; infrared spectroscopy ; chemometrics ; chlorite ; muscovite
    Subject RIVCB - Analytical Chemistry, Separation
    R&D ProjectsED2.1.00/03.0082 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Institutional supportUGN-S - RVO:68145535
    UT WOS000312605700009
    AnnotationThe objective of this work is the chemometric quantification of minerals in rocks. A chemometric method was developed for the determination of chlorite, muscovite, albite and quartz in claystones and clay shales using infrared spectroscopy. Bromide pellets and diffuse reflectance were used to measure the infrared spectra; principal component analysis and partial least-squares regression were used as chemometric methods. Spectral regions (4000-3000 cm(-1) and 1300-400 cm(-1)) containing important spectral information were chosen by principal component analysis. The calibration models were created by a partial least-squares regression. The mean relative error and relative standard deviation were calculated for the assessment of accuracy and reproducibility. The value of the mean relative error was about 10 % for most of the calibration models. The value of the relative standard deviation ranged from 1.1 to 3.0 % for most calibration models based on diffuse reflectance spectra and from 4.0 to 9.2 % for most calibration models based on spectra obtained with bromide pellets.
    WorkplaceInstitute of Geonics
    ContactLucie Gurková, lucie.gurkova@ugn.cas.cz, Tel.: 596 979 354
    Year of Publishing2016
    Electronic addresshttps://www.irsm.cas.cz/materialy/acta_content/2012_04/9.Ritz.pdf
Number of the records: 1  

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