Mineral composition of Rendzic Leptosols in protected areas of the Czech Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F14%3A00424598" target="_blank" >RIV/67985831:_____/14:00424598 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.13168/AGG.2013.0056" target="_blank" >http://dx.doi.org/10.13168/AGG.2013.0056</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.13168/AGG.2013.0056" target="_blank" >10.13168/AGG.2013.0056</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Mineral composition of Rendzic Leptosols in protected areas of the Czech Republic

Popis výsledku v původním jazyce

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 l

Název v anglickém jazyce

Mineral composition of Rendzic Leptosols in protected areas of the Czech Republic

Popis výsledku 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 l

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DF - Pedologie

OECD FORD obor

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Projekt

<a href="/cs/project/GAP210%2F10%2F2351" target="_blank" >GAP210/10/2351: Paleomagnetismus a geochemie vulkanických hornin: Implikace pro paleopozici a vývoj pražské pánve (sv. ordovik - sp. devon)</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Acta geodynamica et geomaterialia

ISSN

1214-9705

e-ISSN

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Svazek periodika

11

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

12

Strana od-do

77-88

Kód UT WoS článku

000331805300008

EID výsledku v databázi Scopus

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