Srovnání depozičních toků na volné ploše a ve smrkových porostech s různou hustotou

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43410%2F09%3A00141394" target="_blank" >RIV/62156489:43410/09:00141394 - isvavai.cz</a>

Výsledek na webu

—

DOI - Digital Object Identifier

—

Jazyk výsledku

angličtina

Název v původním jazyce

Comparison of deposition fluxes on the open area and in mountain spruce stands of different density

Popis výsledku v původním jazyce

To better understand the chemical transformation of the rainfall after the passage through the canopies it is necessary to study throughfall deposition fluxes within forest stands. The comparison of bulk deposition fluxes of Ca, Mg, K, S-SO4, N-NO3 and N-NH4 within the mountain spruce stands with different stand density and bulk deposition fluxes on the open area was made at the study site of Bílý Kříž (Moravian-Silesian Beskids Mts., the Czech Republic) during the period of 1999-2006. Linear relationship between the amount of rainfall on the open area and the amount of throughfall within the spruce stand was found. Throughfall deposition fluxes of selected elements within the dense as well as within the sparse spruce stands were higher when compared with bulk deposition fluxes on the open area. Mostly there were statistical significant differences between the bulk deposition fluxes on the open area and within the studied spruce stands. The throughfall deposition fluxes of Ca, Mg, K an

Název v anglickém jazyce

Comparison of deposition fluxes on the open area and in mountain spruce stands of different density

Popis výsledku anglicky

To better understand the chemical transformation of the rainfall after the passage through the canopies it is necessary to study throughfall deposition fluxes within forest stands. The comparison of bulk deposition fluxes of Ca, Mg, K, S-SO4, N-NO3 and N-NH4 within the mountain spruce stands with different stand density and bulk deposition fluxes on the open area was made at the study site of Bílý Kříž (Moravian-Silesian Beskids Mts., the Czech Republic) during the period of 1999-2006. Linear relationship between the amount of rainfall on the open area and the amount of throughfall within the spruce stand was found. Throughfall deposition fluxes of selected elements within the dense as well as within the sparse spruce stands were higher when compared with bulk deposition fluxes on the open area. Mostly there were statistical significant differences between the bulk deposition fluxes on the open area and within the studied spruce stands. The throughfall deposition fluxes of Ca, Mg, K an

Druh

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

CEP obor

GK - Lesnictví

OECD FORD obor

—

Projekt

—

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2009

Kód důvěrnosti údajů

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

Název periodika

Journal of Forest Science

ISSN

1212-4834

e-ISSN

—

Svazek periodika

55

Číslo periodika v rámci svazku

9

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

8

Strana od-do

—

Kód UT WoS článku

—

EID výsledku v databázi Scopus

—