Role of position within the windthrow in forest floor chemistry in the flysh zone of the Carpatians

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43410%2F08%3A00146192" target="_blank" >RIV/62156489:43410/08:00146192 - isvavai.cz</a>

Výsledek na webu

—

DOI - Digital Object Identifier

—

Jazyk výsledku

angličtina

Název v původním jazyce

Role of position within the windthrow in forest floor chemistry in the flysh zone of the Carpatians

Popis výsledku v původním jazyce

A hypothesis was verified that forest floor chemistry varies according to position within the windthrow (mound, pit, or control). A parallel assessment was made of differences in the chemistry of horizons and treir forms. A total number of 1720 windthrows were studied in the fir-beech primeval forest in the flysh zone of the Western Carpathians. A total of 100 samples were taken on three positions from following horizons and their forms (in brakects): litter, fermented (amphigenous, zoogenous, or mycogenous), humification (unresolved, zoogenous, residues, or humic), and mineral. A random sampling eliminated the effect of correlation between the horizons and positions. Parameters assessed were ited a significant difference in the forest floor chemistryeven at a level of horizons forms. The position's significant decreased with the horozon depth. Organic horizons in the pit, in particular, exhibited the lowest content of total humic substances, fulvic acids, and the lowest colour coeffi

Název v anglickém jazyce

Role of position within the windthrow in forest floor chemistry in the flysh zone of the Carpatians

Popis výsledku anglicky

A hypothesis was verified that forest floor chemistry varies according to position within the windthrow (mound, pit, or control). A parallel assessment was made of differences in the chemistry of horizons and treir forms. A total number of 1720 windthrows were studied in the fir-beech primeval forest in the flysh zone of the Western Carpathians. A total of 100 samples were taken on three positions from following horizons and their forms (in brakects): litter, fermented (amphigenous, zoogenous, or mycogenous), humification (unresolved, zoogenous, residues, or humic), and mineral. A random sampling eliminated the effect of correlation between the horizons and positions. Parameters assessed were ited a significant difference in the forest floor chemistryeven at a level of horizons forms. The position's significant decreased with the horozon depth. Organic horizons in the pit, in particular, exhibited the lowest content of total humic substances, fulvic acids, and the lowest colour coeffi

Druh

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

CEP obor

GK - Lesnictví

OECD FORD obor

—

Projekt

—

Návaznosti

N - Vyzkumna aktivita podporovana z neverejnych zdroju

Rok uplatnění

2008

Kód důvěrnosti údajů

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

Název periodika

Canadian Journal of Forest research

ISSN

0045-5067

e-ISSN

—

Svazek periodika

38

Číslo periodika v rámci svazku

6

Stát vydavatele periodika

CA - Kanada

Počet stran výsledku

15

Strana od-do

—

Kód UT WoS článku

—

EID výsledku v databázi Scopus

—