Access the full text.
Sign up today, get DeepDyve free for 14 days.
V.N. Kudeyarov (2000)
Contribution of Soil to the Atmospheric CO2 Balance in RussiaDoklady Biol. Sci., 375
I.N. Kurganova, V.N. Kudeyarov, V.O. Lopes de Gerenyu (2010)
Updated Estimate of Carbon Balance on Russian TerritoryTellus, 62B
(2007)
Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change “The Physical Science Basis,”
S. Nilsson, A. Shvidenko, V. Stolbovoi (2000)
Full Carbon Account for Russia
A.A. Romanovskaya (2006)
Carbon Accumulation in Lowland Bog Soils of Fallow Lands in Murmansk OblastRuss. J. Ecol., 37
N.I. Bazilevich (1993)
Biologicheskaya produktivnost’ ekosistem Severnoi Evrazii
V.N. Kudeyarov (2005)
The Role of Soils in the Carbon CycleEurasian Soil Sci., 38
A.A. Romanovskaya (2006)
Organic Carbon in Long-Fallow Lands of RussiaEurasian Soil Sci., 39
The dynamics of carbon pools in the live phytomass, necromass, and soil reservoirs have been analyzed in fallow arable lands of Novgorod oblast. The results show that the amounts of above- and belowground necromass increase with the age of fallows, while the dynamics of live phytomass have no distinct trend. Comparisons with archival data show that the stocks of soil organic carbon in the studied ecosystems have decreased by 1.39 t C/ha since 1983, which is equivalent to an annual loss of 0.03 t C/ha. The main factors accounting for changes in the carbon stocks of fallow soils are the initial organic carbon contents in topsoil, the intensity of agromeliorative measures taken during the period of agricultural land use, and carbon contents in soils of meadow communities typical for a given region (zone).
Russian Journal of Ecology – Springer Journals
Published: Sep 4, 2012
Access the full text.
Sign up today, get DeepDyve free for 14 days.