Soil characteristics of selected localities on Smrk Mt. and Kněhyně Mt. in the Moravian-Silesian Beskids (Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43410%2F11%3A00173867" target="_blank" >RIV/62156489:43410/11:00173867 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Soil characteristics of selected localities on Smrk Mt. and Kněhyně Mt. in the Moravian-Silesian Beskids (Czech Republic)

Popis výsledku v původním jazyce

The paper deals with soil characteristics of selected localities on Smrk Mt. and Kněhyně Mt. in the Moravian-Silesian Beskids (38 segments of forest ecosystems). Based on the main soil forming factors defined for studied soils the correctness of classification of groups of forest types into edaphic categories localities were evaluated. Six main soil forming factors were detected. Some of the soils were strongly influenced by surplus of water in the profile. Regardless the altitude, the most soils contained considerable share of skeleton. On the rest of the localities, the main soil forming factors were the cambic and podzolization processes. Both of these pedogenic processes (either of them being dominant) were found at most of the localities. Two of the forest soils were predominantly affected by fluvial processes. This soil survey was a part of an extensive multithematic research.

Název v anglickém jazyce

Soil characteristics of selected localities on Smrk Mt. and Kněhyně Mt. in the Moravian-Silesian Beskids (Czech Republic)

Popis výsledku anglicky

The paper deals with soil characteristics of selected localities on Smrk Mt. and Kněhyně Mt. in the Moravian-Silesian Beskids (38 segments of forest ecosystems). Based on the main soil forming factors defined for studied soils the correctness of classification of groups of forest types into edaphic categories localities were evaluated. Six main soil forming factors were detected. Some of the soils were strongly influenced by surplus of water in the profile. Regardless the altitude, the most soils contained considerable share of skeleton. On the rest of the localities, the main soil forming factors were the cambic and podzolization processes. Both of these pedogenic processes (either of them being dominant) were found at most of the localities. Two of the forest soils were predominantly affected by fluvial processes. This soil survey was a part of an extensive multithematic research.

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

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2011

Kód důvěrnosti údajů

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

Název periodika

Beskydy

ISSN

1803-2451

e-ISSN

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Svazek periodika

4

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

14

Strana od-do

59-72

Kód UT WoS článku

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EID výsledku v databázi Scopus

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