Premium
Soil N 2 O emissions following cover‐crop residues application under two soil moisture conditions
Author(s) -
Pimentel Laisa Gouveia,
Weiler Douglas Adams,
Pedroso Gabriel Munhoz,
Bayer Cimélio
Publication year - 2015
Publication title -
journal of plant nutrition and soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.644
H-Index - 87
eISSN - 1522-2624
pISSN - 1436-8730
DOI - 10.1002/jpln.201400392
Subject(s) - vicia villosa , agronomy , lablab purpureus , legume , cover crop , cajanus , soil water , vigna , crop residue , chemistry , green manure , water content , crop , crop rotation , biology , environmental science , agriculture , soil science , ecology , geotechnical engineering , engineering
Cover crops in rotation or intercropped with annual crops are important strategies to increase C and N input in agricultural soils. However, these practices may also enhance soil N 2 O emissions. The effect on N 2 O emissions may be dependent upon the biochemical composition of cover crop residues. A 47‐d incubation study was conducted to determine soil N 2 O emissions following the addition of residues from three summer legume species [pigeon pea ( Cajanus cajan L. Millsp.), cowpea ( Vigna unguiculata L. Walp.), lablab bean ( Lablab purpureus )], one winter legume [vetch ( Vicia sativa L.)], one winter monocotyledon [black oat ( Avena strigosa Schreb.)], and maize ( Zea mays L.) under two water‐filled pore space levels (40 and 70% WFPS). Short‐term peaks of N 2 O fluxes were observed after the addition of all crop residues, but were much greater under 70 than 40% WFPS (5.2 and 5133 µg N‐N 2 O kg −1 soil for 40 and 70% WFPS, respectively). Under both WFPS, significantly higher peaks were detected after the application of N‐rich legume residues (7.7 and 3,356 µg N‐N 2 O kg −1 soil under 40 and 70% WFPS, respectively) than after the application of grass residues (2.8 and 1,777 µg N‐N 2 O kg −1 soil under 40 and 70% WFPS, respectively). Cumulative soil N 2 O produced under 70% WFPS was approx. 110 times greater than under 40% WFPS. Soil N 2 O emissions increased linearly as residue N content increased. Soil N 2 O emissions also increased linearly as the content of the recalcitrant compounds lignin and polyphenols increased, because residues with high N content also had high lignin and polyphenols content. When the content of C and recalcitrant compounds were expressed on an N basis, soil N 2 O emission decreased linearly as residue C/N, lignin/N, polyphenol/N, and (lignin + polyphenols)/N ratios increased. Indices that include recalcitrant compounds on N basis may be useful for the selection of cover‐crop species with the least impact on soil N 2 O emissions. However, our results show that these ratio indices had similar correlation coefficients compared to C/N ratio, indicating that C/N ratio is an efficient index to predict soil N 2 O emission following cover crop application.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom