Profile distribution and temporal changes of sulphate and nitrate contents and related soil properties under beech and spruce forests
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F13%3A10189163" target="_blank" >RIV/00216208:11310/13:10189163 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/60460709:41210/13:60056 RIV/60460709:41320/13:60056
Výsledek na webu
<a href="http://dx.doi.org/10.1016/j.scitotenv.2012.10.053" target="_blank" >http://dx.doi.org/10.1016/j.scitotenv.2012.10.053</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.scitotenv.2012.10.053" target="_blank" >10.1016/j.scitotenv.2012.10.053</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Profile distribution and temporal changes of sulphate and nitrate contents and related soil properties under beech and spruce forests
Popis výsledku v původním jazyce
The behaviour of principal inorganic anions in forest soils, originating mainly from acid deposition, strongly influences the forest ecosystem response on acidification. The aim of this study was to describe seasonal and temporal changes of sulphate andnitrate contents and related soil properties under beech and spruce forests in a region heavily impacted by acidification. The Jizera Mountains area (Czech Republic) was chosen as such a representative mountainous soil ecosystem. Soil samples were collected at monthly intervals from April to October during the years 2008-2010 under both beech and spruce stands. Soil samples were collected from surface fermentation (F) and humified (H) organic horizons, humic (A) organo-mineral horizons and subsurface mineral (B) horizons (cambic or spodic). A deionised water extract was applied to unsieved fresh samples and the content of anions in these extracts was determined by ion chromatography (IC). In the studied soil profiles, the lowest amount
Název v anglickém jazyce
Profile distribution and temporal changes of sulphate and nitrate contents and related soil properties under beech and spruce forests
Popis výsledku anglicky
The behaviour of principal inorganic anions in forest soils, originating mainly from acid deposition, strongly influences the forest ecosystem response on acidification. The aim of this study was to describe seasonal and temporal changes of sulphate andnitrate contents and related soil properties under beech and spruce forests in a region heavily impacted by acidification. The Jizera Mountains area (Czech Republic) was chosen as such a representative mountainous soil ecosystem. Soil samples were collected at monthly intervals from April to October during the years 2008-2010 under both beech and spruce stands. Soil samples were collected from surface fermentation (F) and humified (H) organic horizons, humic (A) organo-mineral horizons and subsurface mineral (B) horizons (cambic or spodic). A deionised water extract was applied to unsieved fresh samples and the content of anions in these extracts was determined by ion chromatography (IC). In the studied soil profiles, the lowest amount
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DD - Geochemie
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/QI92A216" target="_blank" >QI92A216: Obsahy sloučenin hliníku v lesních půdách ? identifikace problémových lokalit, metody omezení degradačních změn v půdách, možnosti hospodaření pro udržení produkční a ostatních funkcí lesa.</a><br>
Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)<br>S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2013
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Science of the Total Environment
ISSN
0048-9697
e-ISSN
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Svazek periodika
442
Číslo periodika v rámci svazku
JANUARY
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
7
Strana od-do
165-171
Kód UT WoS článku
000313918200021
EID výsledku v databázi Scopus
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