Vegetation history of chernozems in the Czech Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10190148" target="_blank" >RIV/00216208:11310/14:10190148 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/60076658:12310/14:43887209

Výsledek na webu

<a href="http://dx.doi.org/10.1007/s00334-014-0441-7" target="_blank" >http://dx.doi.org/10.1007/s00334-014-0441-7</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s00334-014-0441-7" target="_blank" >10.1007/s00334-014-0441-7</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Vegetation history of chernozems in the Czech Republic

Popis výsledku v původním jazyce

Chernozem is a soil type which can be characterised by a thick dark surface horizon. Such a horizon consists of organic matter and tends to changing into a carbonate horizon, or more often into a loess horizon. Chernozem is being defined as a zonal soilthat has developed under steppe vegetation in a dry continental climate. Nevertheless, chernozems can be also found in Central Europe, where there are no climatic conditions for the existence of any steppe. This study is focused on the vegetation aspectof the pedogenesis of chernozems. There were three sorts of chernozems examined on their charcoal and pedological characteristics: the functional chernozems, the chernozems buried in Holocene and the chernozems buried in Pleistocene. The charcoal examination has proved the presence of forest species in the areas of chernozems in different periods of time. The results of this study reveal that the high stability of soil organic matter has caused the persistence of chernozems in the areas

Název v anglickém jazyce

Vegetation history of chernozems in the Czech Republic

Popis výsledku anglicky

Chernozem is a soil type which can be characterised by a thick dark surface horizon. Such a horizon consists of organic matter and tends to changing into a carbonate horizon, or more often into a loess horizon. Chernozem is being defined as a zonal soilthat has developed under steppe vegetation in a dry continental climate. Nevertheless, chernozems can be also found in Central Europe, where there are no climatic conditions for the existence of any steppe. This study is focused on the vegetation aspectof the pedogenesis of chernozems. There were three sorts of chernozems examined on their charcoal and pedological characteristics: the functional chernozems, the chernozems buried in Holocene and the chernozems buried in Pleistocene. The charcoal examination has proved the presence of forest species in the areas of chernozems in different periods of time. The results of this study reveal that the high stability of soil organic matter has caused the persistence of chernozems in the areas

Druh

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

CEP obor

DF - Pedologie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach<br>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

Vegetation History and Archaeobotany

ISSN

0939-6314

e-ISSN

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Svazek periodika

23

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

12

Strana od-do

97-108

Kód UT WoS článku

000334936100009

EID výsledku v databázi Scopus

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