Dypingit z produktů hořící haldy v Radvanicích u Trutnova (Česká republika)

A very rare mineral dypingite, Mg5(CO3)4(OH)2·5H2O, was determined at samples from the coal burning pile localized 1.5 km S from Radvanice near Trutnov (eastern Bohemia, Czech Republic). This is the first occurrence of this mineral in the Czech Republic. Dypingite occurs as snow-white hemispherical to spherical aggregates up to 1 mm in size formed by tiny acicular crystals on slag material in association with aragonite. Its X-ray powder diffraction data correspond very well with published ones. The results of energy dispersive analysis confirm cation composition of studied dypingite, dominant Mg is accompanied by only traces of Ca. Its formation is associated with low-temperature weathering processes taking place in an already cooled, burnt-out coal dump material.

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Publication Details

Journal
Bulletin Mineralogie Petrologie
Published
2025-01-01
DOI
https://doi.org/10.46861/bmp.33.114
Primary Topic
Clay minerals and soil interactions
Type
article
Field-Weighted Citation Impact
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article

Dypingit z produktů hořící haldy v Radvanicích u Trutnova (Česká republika)

Petr Rus, Ondřej Pour, Radek Škoda
Bulletin Mineralogie Petrologie
Clay minerals and soil interactions
article

Dypingit z produktů hořící haldy v Radvanicích u Trutnova (Česká republika)

Petr Rus, Ondřej Pour, Radek Škoda
article en

Abstract

A very rare mineral dypingite, Mg5(CO3)4(OH)2·5H2O, was determined at samples from the coal burning pile localized 1.5 km S from Radvanice near Trutnov (eastern Bohemia, Czech Republic). This is the first occurrence of this mineral in the Czech Republic. Dypingite occurs as snow-white hemispherical to spherical aggregates up to 1 mm in size formed by tiny acicular crystals on slag material in association with aragonite. Its X-ray powder diffraction data correspond very well with published ones. The results of energy dispersive analysis confirm cation composition of studied dypingite, dominant Mg is accompanied by only traces of Ca. Its formation is associated with low-temperature weathering processes taking place in an already cooled, burnt-out coal dump material.

Bulletin Mineralogie PetrologieVol. 33(1)
Openalex Percentile: Top 87%
Clay minerals and soil interactions
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