Soil?solution partitioning of DOC in acid organic soils. Results from a UK field acidification and alkalization experiment
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67179843%3A_____%2F13%3A00422289" target="_blank" >RIV/67179843:_____/13:00422289 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1111/ejss.12089" target="_blank" >http://dx.doi.org/10.1111/ejss.12089</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1111/ejss.12089" target="_blank" >10.1111/ejss.12089</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Soil?solution partitioning of DOC in acid organic soils. Results from a UK field acidification and alkalization experiment
Popis výsledku v původním jazyce
Dissolved organic carbon (DOC) is an important component of the global carbon (C) cycle and has profound impacts on water chemistry and metabolism in lakes and rivers. Reported increases of DOC concentration in surface waters across Europe and Northern America have been attributed to several drivers, including changing climate, changing land-use to eutrophication and declining acid deposition. The latter of these suggests that acidic deposition suppressed the solubility of DOC, and that this historic suppression is now being reversed by reducing emissions of acidifying pollutants. We studied a set of four parallel acidification and alkalization experiments in organic matter-rich soils, which, after three years of manipulation, have shown distinct soilsolution DOC responses to acidity change. We tested whether these DOC concentration changes were related to changes in the acid/base properties of DOC. Based on laboratory determination of DOC site density (S.D. = amount of carboxylic gro
Název v anglickém jazyce
Soil?solution partitioning of DOC in acid organic soils. Results from a UK field acidification and alkalization experiment
Popis výsledku anglicky
Dissolved organic carbon (DOC) is an important component of the global carbon (C) cycle and has profound impacts on water chemistry and metabolism in lakes and rivers. Reported increases of DOC concentration in surface waters across Europe and Northern America have been attributed to several drivers, including changing climate, changing land-use to eutrophication and declining acid deposition. The latter of these suggests that acidic deposition suppressed the solubility of DOC, and that this historic suppression is now being reversed by reducing emissions of acidifying pollutants. We studied a set of four parallel acidification and alkalization experiments in organic matter-rich soils, which, after three years of manipulation, have shown distinct soilsolution DOC responses to acidity change. We tested whether these DOC concentration changes were related to changes in the acid/base properties of DOC. Based on laboratory determination of DOC site density (S.D. = amount of carboxylic gro
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
EH - Ekologie – společenstva
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/ED1.1.00%2F02.0073" target="_blank" >ED1.1.00/02.0073: CzechGlobe ? Centrum pro studium dopadu globální zmeny klimatu</a><br>
Návaznosti
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
European Journal of Soil Science
ISSN
1351-0754
e-ISSN
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Svazek periodika
64
Číslo periodika v rámci svazku
6
Stát vydavatele periodika
GB - Spojené království Velké Británie a Severního Irska
Počet stran výsledku
10
Strana od-do
787-796
Kód UT WoS článku
000327219600006
EID výsledku v databázi Scopus
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