『Abstract
In Madagascar, no-tillage practices were developed since the
early 90s to prevent soil erosion and improve soil fertility.
Although such practices have helped to restore soil carbon in
most cases, the impact on N2O emissions has
not been investigated yet. The soil N2O fluxes
and concentrations were measured during the growing season of
an intercropping maize-soybean on a clayey soil of the Malagasy
Highlands. Management treatments consisted of direct seeding mulch
based croping system (DMC) and traditional hand-ploughing after
the preceding crop residues were harvested (HP), both with low
N inputs (55-57 kg N ha-1). No significant difference
in N2O emissions was observed between treatments
(DMC vs. HP). The N2O fluxes were weakly
correlated to soil mineral N contents (R2=0.13; P=0.03)
while no relationship was emphasized with soil water filled pore
space (WFPS). N2O concentrations in the soil
atmosphere were correlated to fluxes at the soil surface and to
soil WFPS. N2O emissions at the soil surface
were low ranging from 0 to 8.84 g N-N2O ha-1
d-1, probably due to the low mineral N content of soil.
The cumulative annual N2O emission was 0.26
kg N ha-1 for both systems. The corresponding N loss
as N2O-N was around 0.5% of applied N. This
is in the uncertainty range of IPCC N2O emission
factor (EF), but the IPCC EF mean estimate (1%) would overestimate
true N2O emissions for the soil under evaluation.
Keywords: Tropical soil; No-tillage; N2O
emissions; Soil mineral N; WFPS; IPCC N2O
emission factor』
1. Introduction
2. Materials and methods
2.1. Experimental site and design
2.2. Local climatic data and soil temperature
2.3. N2O flux measurements
2.3.1. At the soil surface
2.3.2. At different soil depths
2.4. Soil sampling and analyses
2.4.1. Soil total N and C contents
2.4.2. Soil mineral N and water contents
2.5. Statistical analyses
3. Results
3.1. Climatic data and soil temperature
3.2. Soil total C and N
3.3. Soil bulk density and water-filled pore space
3.4. Soil mineral N
3.5. N2O emissions
3.5.1. N2O fluxes at the soil surface
3.5.2. N2O concentrations in soil profile
4. Discussion
4.1. N2O emissions from tropical agricultural
soils and related factors
4.2. Effect of management practices
5. Conclusion
References