We have created this Blog and the database to provide a place where the scientific community can share and update the fast growing knowledge and data on the study of greenhouse gas CO2, CH4, and N2O fluxes in Africa.

We are grateful for the numerous researchers and technicians who provide invaluable data. It is impossible to cite all the references due to limited space allowed and we apologize for the authors whose work has not been cited.

Epron et al., 2006. Soil carbon balance in a clonal Eucalyptus plantation in Congo: effects of logging on carbon inputs and soil CO2 efflux.

Epron, D., Nouvellon, Y., Deleporte, P., Ifo, S., Kazotti, G.U.Y., Thongo M'Bou, A., Mouvondy, W., Andre, L.S., Roupsard, O., Jourdan, C., Hamel, O., 2006. Soil carbon balance in a clonal Eucalyptus plantation in Congo: effects of logging on carbon inputs and soil CO2 efflux. Global Change Biol. 12, 1021-1031.

Abstract

Soil CO2 efflux was measured in clear-cut and intact plots in order to quantify the impact of harvest on soil respiration in an intensively managed Eucalyptus plantation, and to evaluate the increase in heterotrophic component of soil respiration because of the decomposition of harvest residues. Soil CO2 effluxes showed a pronounced seasonal trend, which was well related to the pattern of precipitation and soil water content and were always significantly lower in the clear-cut plots than in the intact plots. On an annual basis, soil respiration represented 1.57 and 0.91 kgC m−2 yr−1 in intact and clear-cut plots, respectively. During the first year following harvest, residues have lost 0.79 kgC m−2 yr−1. Our estimate of heterotrophic respiration was calculated assuming that it was similar to soil respiration in the clear-cut area except that the decomposition of residues did not occur, and it was further corrected for differences in soil water content between intact and clear-cut plots and for the cessation of leaf and fine root turnover in clear cut. Heterotrophic respiration in clear-cut plots was estimated at 1.18 kgC m−2 yr−1 whereas it was only 0.65 kgC m−2 yr−1 in intact plots (41% of soil respiration). Assumptions and uncertainties with these calculations are discussed.

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