ZIMÁK, Jiří, Jindřich ŠTELCL and Dalibor VŠIANSKÝ. Reflectance colourimetry as a method for estimating the approximate quantity of non-carbonate components in limestones: A case study in the Mokrá Quarry (Czech Republic). Catena. Elsevier Science, 2018, vol. 169, October 2018, p. 90-95. ISSN 0341-8162. Available from: https://dx.doi.org/10.1016/j.catena.2018.05.028.
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Basic information
Original name Reflectance colourimetry as a method for estimating the approximate quantity of non-carbonate components in limestones: A case study in the Mokrá Quarry (Czech Republic)
Authors ZIMÁK, Jiří (203 Czech Republic, guarantor), Jindřich ŠTELCL (203 Czech Republic, belonging to the institution) and Dalibor VŠIANSKÝ (203 Czech Republic, belonging to the institution).
Edition Catena, Elsevier Science, 2018, 0341-8162.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10505 Geology
Country of publisher Netherlands
Confidentiality degree is not subject to a state or trade secret
WWW URL
Impact factor Impact factor: 3.851
RIV identification code RIV/00216224:14310/18:00103519
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1016/j.catena.2018.05.028
UT WoS 000437380300009
Keywords in English Reflectance colourimetry Cement raw materials; Limestones; Non-carbonate components; Moravian Karst
Changed by Changed by: Dana Nesnídalová, učo 831. Changed: 10/3/2021 10:52.
Abstract
This paper demonstrates the applicability and usefulness of colourimetry as a fast and simple tool to assess the quality of limestones for cement and lime industry raw materials, a field where colourimetric measurements have not yet been applied. The results of the colourimetric analysis in a large sample set from the Mokrá Quarry in the Moravian Karst (NE from Brno, Czech Republic) and comparisons with the results obtained by other methods are presented here. The studied samples belong to two lithologically different series of strata: the Macocha Formation and the Líšeň Formation. Limestones of these formations differ in structure, the contents of their non-carbonate components and, therefore, in colour as well. The samples were prepared in four ways for the purposes of colourimetric measurements: i) unpolished bulk samples (fracture planes were measured), ii) polished sections, iii) powder in a plastic bag, and iv) uncovered powder. Each of these four ways led to different results, which were expressed using the CIE L*a*b* colour space. The L* (specific lightness) value gives an approximate estimate as to the amount of non-carbonate components. The specific lightness value can be used for assigning a sample to a lithostratigraphic member and, in many cases, possibly also to a correlation among members.
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