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Nitrous oxide emissions following incorporation of improved‐fallow residues in the humid tropics
Author(s) -
Millar N.,
Ndufa J. K.,
Cadisch G.,
Baggs E. M.
Publication year - 2004
Publication title -
global biogeochemical cycles
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.512
H-Index - 187
eISSN - 1944-9224
pISSN - 0886-6236
DOI - 10.1029/2003gb002114
Subject(s) - tropics , nitrous oxide , environmental science , environmental chemistry , agronomy , chemistry , atmospheric sciences , ecology , geology , biology , organic chemistry
The rotation of crops with fast‐growing tree, shrub, and herbaceous N 2 ‐fixing legume species (improved fallows) is a central agroforestry technology for soil fertility management in the humid tropics. Maize yields are increased following improved fallows compared with continuous maize cropping or traditional natural‐fallow systems consisting of broadleaved weeds and grasses. However, the effect of these improved‐fallow systems on N availability and N 2 O emissions following residue application has yet to be determined. Emissions from these systems not only have a detrimental effect on the environment, but are of additional concern in that they represent a potentially significant loss of N and a reduction in N‐use efficiency. Emissions of N 2 O were measured from improved‐fallow agroforestry systems in western Kenya, being characteristic of agroforestry systems in the humid tropics. Emissions were increased after incorporation of fallow residues and were higher after incorporation of improved‐fallow legume residues ( Sesbania sesban , Crotalaria grahamiana , Macroptilium atropurpureum ) than natural‐fallow residues (mainly consisting of Digitaria abyssibica , Habiscus cannabinus , Bidens pilosa , Guizotia scabra , Leonotis nepetifolia , Commelina benghalensis ). Following incorporation of Sesbania and Macroptilium residues (7.4 t dry matter ha −1 ; 2.9% N) in a mixed fallow system, 4.1 kg N 2 O‐N ha −1 was emitted over 84 days. The percentages of N applied emitted as N 2 O following residue incorporation in these tropical agroforestry systems were of the same magnitude as in temperate agricultural systems. N 2 O (log e ) emissions were positively correlated with residue N content (r = 0.93; P < 0.05), and thus the residue composition, particularly its N content, is an important consideration when proposing management practices to mitigate N 2 O emissions from these systems.