Castaldi, S., Bertolini, T., Valente, A.,
Chiti, T., and Valentini, R.:2013. Nitrous oxide emissions from soil of an
African rain forest in Ghana, Biogeosciences, 10, 4179-4187
Abstract
Recent atmospheric studies have evidenced the imprint of large N2O
sources in tropical/subtropical lands. This source might be attributed to
agricultural areas as well as to natural humid ecosystems. The uncertainty
related to both sources is very high, due to the scarcity of data and low
frequency of sampling in tropical studies, especially for the African
continent. The principal objective of this work was to quantify the annual
budget of N2O emissions in an African tropical rain forest. Soil
N2O emissions were measured over 19 months in Ghana, National Park of
Ankasa, in uphill and downhill areas, for a total of 119 days of observation.
The calculated annual average emission was
2.33 ± 0.20 kg N-N2O ha−1 yr−1, taking into
account the proportion of uphill vs. downhill areas, the latter being
characterized by lower N2O emissions. N2O fluxes peaked between
June and August and were significantly correlated with soil respiration on a
daily and monthly basis. No clear correlation was found in the uphill area
between N2O fluxes and soil water content or rain, whereas in the
downhill area soil water content concurred with soil respiration in
determining N2O flux variability. The N2O source strength
calculated in this study is very close to those reported for the other two
available studies in African rain forests and to the estimated mean derived
from worldwide studies in humid tropical forests
(2.81 ± 2.02 kg N-N2O ha−1 yr−1).
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.
Lompo et al. 2012. Gaseous emissions of nitrogen and carbon from urban vegetable gardens in Bobo-Dioulasso, Burkina Faso. Journal of Plant Nutrition and Soil Science 175, 846-853
Lompo, D.J.-P., Sangaré, S.A.K., Compaoré, E., Papoada Sedogo, M., Predotova, M., Schlecht, E., Buerkert, A., 2012. Gaseous emissions of nitrogen and carbon from urban vegetable gardens in Bobo-Dioulasso, Burkina Faso. Journal of Plant Nutrition and Soil Science 175, 846-853
Abstract
Urban and
peri-urban agriculture (UPA) is an important livelihood strategy for the
urban poor in sub-Saharan Africa and contributes to meeting increasing
food demands in the rapidly growing cities. Although in recent years
many research activities have been geared towards enhancing the
productivity of this land-use system, little is known about turnover
processes and nutrient efficiency of UPA. The aim of our study therefore
was to determine horizontal fluxes of N, P, K, and C as well as gaseous
N and C emissions in urban vegetable gardens of Bobo-Dioulasso, Burkina
Faso. Two gardens referred to as “Kodéni” and “Kuinima” were selected
as representative for urban and peri-urban systems classified as: (1)
“commercial gardening + field crops and livestock system” and (2)
“commercial gardening and semicommercial field crop system”,
respectively. A nutrient-balance approach was used to monitor matter
fluxes from March 2008 to March 2009 in both gardens. Ammonia (NH3), nitrous oxide (N2O) and carbon dioxide (CO2)
emissions from the respective soils were measured during the coolest
and the hottest period of the day using a closed-chamber system. Annual
partial balances amounted to 2056 kg N ha–1, 615 kg P ha–1, 1864 kg K ha–1, and 33 893 kg C ha–1 at Kodéni and to 1752 kg N ha–1, 446 kg P ha–1, 1643 kg K ha–1, and 21 021 kg C ha–1
at Kuinima. Emission rates were highest during the hot midday hours
with peaks after fertilizer applications when fluxes of up to 1140 g NH3-N ha–1 h–1, 154 g N2O-N ha–1 h–1, 12 993 g CO2-C ha–1 h–1 were recorded for Kodéni and Kuinima. Estimated annual gaseous N (NH3-N + N2O-N) and C (CO2-C + CH4-C) losses reached 419 kg N ha–1 and 35 862 kg C ha–1 at Kodéni and 347 kg N ha–1 and 22 364 kg C ha–1 at Kuinima. For both gardens, this represented 20% and 106% of the N and C surpluses, respectively. Emissions of NH3,
largely emitted after surface application of manure and mineral
fertilizers, accounted for 73% and 77% of total estimated N losses for
Kodéni and Kuinima. To mitigate N losses nutrient-management practices
in UPA vegetable production of Bobo-Dioulasso would greatly benefit from
better synchronizing nutrient-input rates with crop demands.
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