ZIMÁK, Jiří, Jindřich ŠTELCL a 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, roč. 169, October 2018, s. 90-95. ISSN 0341-8162. Dostupné z: https://dx.doi.org/10.1016/j.catena.2018.05.028.
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Základní údaje
Originální název 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)
Autoři ZIMÁK, Jiří (203 Česká republika, garant), Jindřich ŠTELCL (203 Česká republika, domácí) a Dalibor VŠIANSKÝ (203 Česká republika, domácí).
Vydání Catena, Elsevier Science, 2018, 0341-8162.
Další údaje
Originální jazyk angličtina
Typ výsledku Článek v odborném periodiku
Obor 10505 Geology
Stát vydavatele Nizozemské království
Utajení není předmětem státního či obchodního tajemství
WWW URL
Impakt faktor Impact factor: 3.851
Kód RIV RIV/00216224:14310/18:00103519
Organizační jednotka Přírodovědecká fakulta
Doi http://dx.doi.org/10.1016/j.catena.2018.05.028
UT WoS 000437380300009
Klíčová slova anglicky Reflectance colourimetry Cement raw materials; Limestones; Non-carbonate components; Moravian Karst
Změnil Změnila: Dana Nesnídalová, učo 831. Změněno: 10. 3. 2021 10:52.
Anotace
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.
VytisknoutZobrazeno: 27. 7. 2024 13:39