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Fluxes of CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O from soil of burned grassland savannah of central Africa

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Academic year: 2017

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Table 1. Some chemical characteristics measured for the top 10 cm of soil of the unburned and burned plots during the first and second field campaign
Fig. 1. Soil volumetric water content in function of time after watering (days) during the 1st campaign (A) and the 2nd campaign (B)
Fig. 2. Soil respiration normalized at 25 ◦ C in function of time after watering during the 1st campaign (A) and the 2nd campaign (B)
Fig. 3. Soil respiration normalized at 25 ◦ C in function of water filled pores space (during the 1st campaign (A) and the 2nd campaign (B)
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