Soil carbon accumulation after open-cast coal and oil shale mining in Northern Hemisphere: a quantitative review
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F13%3A10126650" target="_blank" >RIV/00216208:11310/13:10126650 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1007/s12665-012-2004-5" target="_blank" >http://dx.doi.org/10.1007/s12665-012-2004-5</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s12665-012-2004-5" target="_blank" >10.1007/s12665-012-2004-5</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Soil carbon accumulation after open-cast coal and oil shale mining in Northern Hemisphere: a quantitative review
Popis výsledku v původním jazyce
Meta-analysis and other statistical methods were used to evaluate how changes in soil organic carbon (SOC) content in post-mining soils are related to different factors; the data were obtained from 17 studies covering 93 temperate post-mining sites in the Northern Hemisphere that had been revegetated by forest or grassland either by reclamation or natural succession. Because many studies have failed to report any measures of variance, only part of the data were used for meta-analysis. According to the meta-analysis, the rate of SOC accumulation was unrelated to vegetation type. In a separate analysis that included all available data and in which rates of SOC accumulation at each site were used as individual entries, the rate of SOC accumulation differed depending on the age of the site and vegetation type. Under deciduous forests, the rate reached a maximum after 5-10 years and then decreased. Under coniferous forests, the initial SOC values were lower than under deciduous forests, but
Název v anglickém jazyce
Soil carbon accumulation after open-cast coal and oil shale mining in Northern Hemisphere: a quantitative review
Popis výsledku anglicky
Meta-analysis and other statistical methods were used to evaluate how changes in soil organic carbon (SOC) content in post-mining soils are related to different factors; the data were obtained from 17 studies covering 93 temperate post-mining sites in the Northern Hemisphere that had been revegetated by forest or grassland either by reclamation or natural succession. Because many studies have failed to report any measures of variance, only part of the data were used for meta-analysis. According to the meta-analysis, the rate of SOC accumulation was unrelated to vegetation type. In a separate analysis that included all available data and in which rates of SOC accumulation at each site were used as individual entries, the rate of SOC accumulation differed depending on the age of the site and vegetation type. Under deciduous forests, the rate reached a maximum after 5-10 years and then decreased. Under coniferous forests, the initial SOC values were lower than under deciduous forests, but
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DF - Pedologie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)<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
Environmental Earth Sciences
ISSN
1866-6280
e-ISSN
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Svazek periodika
69
Číslo periodika v rámci svazku
5
Stát vydavatele periodika
BR - Brazilská federativní republika
Počet stran výsledku
19
Strana od-do
1685-1698
Kód UT WoS článku
000320327900018
EID výsledku v databázi Scopus
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