Soil N2O emissions in French Guiana after the conversion of tropical forest to agriculture with the chop-and-mulch method
•A fire-free method was used to convert 2ha of French Guianese forest to agriculture.•We measured in situ soil N2O fluxes and compared 4 land uses.•Soil N2O fluxes measured at Combi site ranged between −4.5 and 65.8gNha−1day−1.•Nitrogen inputs led to higher N2O fluxes from croplands compared to the...
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| Published in: | Agriculture, ecosystems & environment ecosystems & environment, 2015-10, Vol.208, p.64-74 |
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| Main Authors: | , , , , , , , , |
| Format: | Article |
| Language: | eng |
| Subjects: | |
| Online Access: | Get full text |
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| Summary: | •A fire-free method was used to convert 2ha of French Guianese forest to agriculture.•We measured in situ soil N2O fluxes and compared 4 land uses.•Soil N2O fluxes measured at Combi site ranged between −4.5 and 65.8gNha−1day−1.•Nitrogen inputs led to higher N2O fluxes from croplands compared to the forest.
In French Guiana, the population growth will result in an increase in demand for agricultural products and thus, will lead to an increase in the amount of tropical forests converted into cropland or pasture. Impacts of different agricultural systems on greenhouse gas (GHG) fluxes have not been studied in French Guiana. In this context, the fire-free chop-and-mulch method was used to convert a tropical forest site to agriculture. This study focused on soil nitrous oxide (N2O) emissions and we compared four land uses: (1) the undisturbed tropical forest, (2) recently converted grassland and recently converted croplands (fertilized soybean/maize rotation) with either (3) disk tillage or (4) no tillage.
N2O measurements were obtained through the chamber technique and conducted over a 1-year period (measurements began 19 months after the forest was cleared). N2O fluxes were related to soil parameters measured at each sampling date: nitrate and ammonium contents, gravimetric water content (GWC) and temperature.
Through the entire period, the mean (±standard error) and median N2O fluxes were 3.8±0.5 and 2.7gNha−1day−1, respectively for undisturbed tropical forest and 2.4±0.9 and 0.8gNha−1day−1, respectively for grassland (mowed Brachiaria ruziziensis). For croplands, no significant difference was found for N2O emissions between both agricultural practices. The mean (±standard error) and median N2O fluxes were 8.5±1.2 and 4.0gNha−1day−1, respectively for disk tillage plots and 8.5±1.3 and 3.6gNha−1day−1, respectively for no tillage plots. Nitrogen inputs (due to the application of fertilizer or due to the mineralization of crop residues) led to higher N2O fluxes, resulting in significantly higher mean N2O emissions from croplands compared to the forest, when only considering land use effect on N2O fluxes in a statistical model. The soil nitrate content, GWC and temperature had a significant positive effect on N2O fluxes. Taking into account these soil parameters in another statistical model, N2O emissions from croplands were not higher than the natural N2O emissions from tropical forest soils. Our results suggest that, if more forest will have to be converted in |
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| ISSN: | 0167-8809 1873-2305 |