40 research outputs found

    Nitrogen cycling drives a strong within-soil CO2-sink

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    This is the published version of a paper published in Tellus. Series B, Chemical and physical meteorology. Citation for the original published paper (version of record): Fleischer, S., Bouse, I. (2008) Nitrogen cycling drives a strong within-soil CO2-sink. A B S T R A C T For about three decades, it has not been possible to completely balance global carbon emissions into known pools. A residual (or 'missing') sink remains. Here evidence is presented that part of soil respiration is allocated into an internal soil CO 2 -sink localized to the saprophytic subsystem (roots excluded). The process occurs in forest, agricultural and grassland soils and is favoured by high N-deposition. Chemoautotrophic nitrification has a key role, and the most efficient internal CO 2 -sequestration occurs concurrently with lowest soil nitrate (NO 3 − ) concentrations, despite considerable N-loading. Not until drastic N-supply occurs, does the CO 2 -sink successively breakdown, and nitrate concentrations increase, leading to NO 3 − -leaching. Within-soil CO 2 -uptake seems to be of the same magnitude as the missing carbon sink. It may be gradually enforced by the ongoing input of nitrogen to the biosphere

    Prima pars commentariorum in constitutiones taurinas

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    Restaurado; 2001/11/19; FanjareReclamos. - Sign: [cruz latina]12, A-Z8, Aa-Gg8, Hh6. - Colofón. - Texto a dos col. - Port. orlada con grab. y esc. heráldico xil. - Cap. grab. xil
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