Trends in aluminium export from a mountainous area to surface waters, from deglaciation to the recent: Effects of vegetation and soil development, atmospheric acidification, and nitrogen-saturation
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F09%3A00328912" target="_blank" >RIV/60077344:_____/09:00328912 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Trends in aluminium export from a mountainous area to surface waters, from deglaciation to the recent: Effects of vegetation and soil development, atmospheric acidification, and nitrogen-saturation
Popis výsledku v původním jazyce
We reconstructed the history of terrestrial export of aluminium (Al) to Plešné Lake (Czech Republic) since the lake origin 12,600 BC, and predicted Al export for 2010?2050 on the basis of mass budget studies, palaeolimnological data, and MAGIC modelling.We focused on three major Al forms; ionic Al (Ali), organically-bound Al (Alo), and particulate Al hydroxide (Alp). In early post-glacial time, Plešné Lake received high terrestrial export of Al, but with a minor proportion of Alp (4?25 ?M), and concentrations of Ali and Alo were negligible. Since the forest and soil development (9900?9000 BC), erosion has declined and soil organic acids increased export of Alo from soils. The terrestrial Alo leaching (7.5 ?M) persisted throughout the Holocene until the industrial period. Then, Ali concentrations continuously increased (up to 28 ?M in the mid-1980s) due to atmospheric acidification. Alo (5.5 ?M) is predicted to dominate Al concentrations around 2050.
Název v anglickém jazyce
Trends in aluminium export from a mountainous area to surface waters, from deglaciation to the recent: Effects of vegetation and soil development, atmospheric acidification, and nitrogen-saturation
Popis výsledku anglicky
We reconstructed the history of terrestrial export of aluminium (Al) to Plešné Lake (Czech Republic) since the lake origin 12,600 BC, and predicted Al export for 2010?2050 on the basis of mass budget studies, palaeolimnological data, and MAGIC modelling.We focused on three major Al forms; ionic Al (Ali), organically-bound Al (Alo), and particulate Al hydroxide (Alp). In early post-glacial time, Plešné Lake received high terrestrial export of Al, but with a minor proportion of Alp (4?25 ?M), and concentrations of Ali and Alo were negligible. Since the forest and soil development (9900?9000 BC), erosion has declined and soil organic acids increased export of Alo from soils. The terrestrial Alo leaching (7.5 ?M) persisted throughout the Holocene until the industrial period. Then, Ali concentrations continuously increased (up to 28 ?M in the mid-1980s) due to atmospheric acidification. Alo (5.5 ?M) is predicted to dominate Al concentrations around 2050.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DJ - Znečištění a kontrola vody
OECD FORD obor
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Návaznosti výsledku
Projekt
Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.
Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)
Ostatní
Rok uplatnění
2009
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Journal of Inorganic Biochemistry
ISSN
0162-0134
e-ISSN
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Svazek periodika
103
Číslo periodika v rámci svazku
11
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
10
Strana od-do
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Kód UT WoS článku
000271436500003
EID výsledku v databázi Scopus
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