Podrobnosti záznamu

Název
    Mineral composition of Rendzic Leptosols in protected areas of the Czech Republic
Autor
    Hladil, Jindřich
    Šťastný, Martin
    Žigová, Anna
Jazyk
    anglicky
Typ dokumentu
    článek v odborném periodiku
Zdrojový dokument - seriál
    Acta geodynamica et geomaterialia
Svazek/č.
    Roč. 11, č. 1
Strany
    s. 77-88
Rok
    2014
Poznámky
    Projekt: GAP210/10/2351, GA ČR3cav_un_auth*0263318
    Rozsah: 12 s. : E
Předmětová kategorie
    limestones
    mineral composition
    process of humification
    Rendzic Leptosols
    soil development
    soil properties
Klíčové slovo
    Areas
    Composition
    Czech
    Leptosols
    Mineral
    Protected
    Rendzic
    Republic
Abstrakt (anglicky)
   This study overviews Rendzic Leptosols developed on different limestones of pre-Mesozoic age in protected areas of the Czech Republic, and characterizes their pedogenesis and mineral composition. The parent material originating from unmetamorphosed, low- and high-grade metamorphic rocks (sites Cikánka, Třesín and Vyšenské kopce, respectively) was evaluated on the basis thin section of petrography and X-ray diffractometry of powder samples. Representative soil sequences were characterized by macromorphological analysis, particle size distribution, chemical properties, parameters of soil organic matter and mineral composition of clay fraction. Soil formation is limited to the thickness of Ahk horizons. The process of humification is controlled by the source of biomass and biological activity. Třesín and Vyšenské kopce have more favourable parameters of humification than Cikánka.
   Mineral composition of Rendzic Leptosols is significantly affected by the petrography of parent material and local conditions of bedrock. Unmetamorphosed limestones from Cikánka are the most characteristic parent material for the development of Rendzic Leptosols.
Přispěvatel
    AV ČR Brno, Geologický ústav
Kód přispěvatele
    AV ČR, GLÚ
Zdrojový formát
    U
Datum importu
    23. 10. 2014