Soil Nitrous Oxide Emissions Following Band-Incorporation of Fertilizer Nitrogen and Swine Manure

被引:94
作者
Chantigny, Martin H. [1 ]
Rochette, Philippe [1 ]
Angers, Denis A. [1 ]
Bittman, Shabtai [2 ]
Buckley, Katherine [3 ]
Masse, Daniel [4 ]
Belanger, Gilles [1 ]
Eriksen-Hamel, Nikita [1 ]
Gasser, Marc-Olivier [5 ]
机构
[1] Agr & Agri Food Canada, Soils & Crops Res & Dev Ctr, Quebec City, PQ G1V 2J3, Canada
[2] Agr & Agri Food Canada, Pacific Agr Res Ctr, Agassiz, BC V0M 1A0, Canada
[3] Agr & Agri Food Canada, Brandon Res Ctr, Brandon, MB R7A 5Y3, Canada
[4] Agr & Agri Food Canada, Dairy Cattle & Swine Res Ctr, Sherbrooke, PQ J1M 1Z3, Canada
[5] Inst Rech & Dev Agroenvironm, Quebec City, PQ G1P 3W8, Canada
关键词
VOLATILE FATTY-ACIDS; N2O EMISSIONS; ANAEROBIC-DIGESTION; CATTLE SLURRY; ANIMAL SLURRY; LIQUID; CARBON; RAW; PIG; IMMOBILIZATION;
D O I
10.2134/jeq2009.0482
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Treatment of liquid swine manure (LSM) offers opportunities to improve manure nutrient management. However, N(2)O fluxes and cumulative emissions resulting from application of treated LSM are nor well documented. Nitrous oxide emissions were monitored following band-incorporation of 100 kg N ha(-1) of either mineral fertilizer, raw LSM, or four pretreated LSMs (anaerobic digestion; anaerobic digestion + flocculation; filtration; decantation) at the four-leaf stage of corn (Zea mays L.). In a clay soil, a larger proportion of applied N was lost as N(2)O with the mineral fertilizer (average of 6.6%) than with LSMs (3.1-5.0%), whereas in a loam soil, the proportion of applied N lost as N(2)O was lower with the mineral fertilizer (average of 0.4%) than with LSMs (1.2-2.4%). Emissions were related to soil NO(3) intensity in the clay soil, whereas they were related to water-extractable organic C in the loam soil. This suggests that N(2)O production was N limited in the clay soil and C limited in the loam soil, and would explain the interaction found between N sources and soil type. The large N(2)O emission coefficients measured in many treatments, and the contradicting responses among N sources depending on soil type, indicate that (i) the Intergovernmental Panel on Climate Change (IPCC) default value (1%) may seriously underestimate N(2)O emissions from fine-textured soils where fertilizer N and manure are band-incorporated, and (ii) site-specific factors, such as drainage conditions and soil properties (e.g., texture, organic matter content), have a differential influence on emissions depending on N source.
引用
收藏
页码:1545 / 1553
页数:9
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