"2010-05-01+02:00"^^ . . " temperature" . . . . . " bioavailability" . . . " ecological stoichiometry" . "Long-term Carbon Storage in Cryoturbeated Arctic Soils"@en . . . . . . "Long-term Carbon Storage in Cryoturbeated Arctic Soils" . "0"^^ . " moisture" . . "7E10073" . "0"^^ . "http://www.isvav.cz/projectDetail.do?rowId=7E10073"^^ . "soil organic matter; bioavailability; carbon quality; temperature; moisture; stable isotopes; ecological stoichiometry; microbial functioning"@en . "1"^^ . "0"^^ . "0"^^ . "Hodnocen\u00ED v\u00FDsledk\u016F \u0159e\u0161en\u00ED ministerstvo neprov\u00E1d\u00ED, nebo\u0165 podm\u00EDnkou podpory je, \u017Ee uchaze\u010D byl vybr\u00E1n mezin\u00E1rodn\u00EDm poskytovatelem v souladu s pravidly p\u0159\u00EDslu\u0161n\u00E9ho programu. Projekt je hodnocen a\u017E po jeho schv\u00E1len\u00ED mezin\u00E1rodn\u00EDm poskytovatelem."@cs . "soil organic matter" . "2014-06-30+02:00"^^ . " carbon quality" . . "Following the condition that the candidate of financial contribution was evaluated and afterwards selected by international provider in accordance with the rules of the program the Ministry of Education, Youth ans Sports does not realize the evaluation of project results. The project is evaluated only after its approval by an international provider."@en . . "The total organic carbon pool of soils (SOC) of the circum-arctic permafrost zone has been estimated to contain ~400 Gt C in the upper 1m and as much as 747 Gt C in the upper 3m, excluding peatlands and carbon in deep loess sediment. This is more than today\u2019s global atmospheric C pool (730 Gt C). This globally significant C reservoir is vulnerable to climate warming through permafrost thawing and may thus become a future source of a large amount of CO2 and CH4 to the atmosphere. The amount of SOC stored in arctic soils remains poorly constrained, which is especially true for arctic Russia. There is increasing evidence that a significant proportion of this SOC is stored in the subducted organic matter of Cryosols, suggesting that cryoturbation may be one of the most important mechanisms of arctic carbon storage. The overarching goal of CryoCARB is to advance organic carbon estimates for cryoturbated soils, focusing on the Eurasian Arctic and to understand the vulnerability of these carbon stocks in"@en . "The total organic carbon pool of soils (SOC) of the circum-arctic permafrost zone has been estimated to contain ~400 Gt C in the upper 1m and as much as 747 Gt C in the upper 3m, excluding peatlands and carbon in deep loess sediment. This is more than today\u2019s global atmospheric C pool (730 Gt C). This globally significant C reservoir is vulnerable to climate warming through permafrost thawing and may thus become a future source of a large amount of CO2 and CH4 to the atmosphere. The amount of SOC stored in arctic soils remains poorly constrained, which is especially true for arctic Russia. There is increasing evidence that a significant proportion of this SOC is stored in the subducted organic matter of Cryosols, suggesting that cryoturbation may be one of the most important mechanisms of arctic carbon storage. The overarching goal of CryoCARB is to advance organic carbon estimates for cryoturbated soils, focusing on the Eurasian Arctic and to understand the vulnerability of these carbon stocks in" . . " stable isotopes" . . . . . "2013-05-01+02:00"^^ .