Tillage, Cropping Sequence, and Nitrogen Fertilization Effects on Dryland Soil Carbon Dioxide Emission and Carbon Content
Влияние обработки почвы, последовательности севооборота и азотного удобрения на выбросы диоксида углерода из сухих почв и содержание углерода
2010-04-16
SCID: 54.1/6znyhv5z
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dryland CO2 emissionsnitrogen fertilization (0 and 80 kg N ha^-1)soil CO2 flux (seasonal cumulative)soil total carbon content (0-120 cm)tillage and cropping sequence
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Abstract (AI)
Management practices are needed to reduce dryland soil CO(2) emissions and to increase C sequestration. We evaluated the effects of tillage and cropping sequence combinations and N fertilization on dryland crop biomass (stems + leaves) and soil surface CO(2) flux and C content (0- to 120-cm depth) in a Williams loam from May to October, 2006 to 2008, in eastern Montana. Treatments were no-tilled continuous malt barley (Hordeum vulgaris L.) (NTCB), no-tilled malt barley-pea (Pisum sativum L.) (NTB-P), no-tilled malt barley-fallow (NTB-F), and conventional-tilled malt barley-fallow (CTB-F), each with 0 and 80 kg N ha(-1). Measurements were made both in Phase I (malt barley in NTCB, pea in NTB-P, and fallow in NTB-F and CTB-F) and Phase II (malt barley in all sequences) of each cropping sequence in every year. Crop biomass varied among years, was greater in the barley than in the pea phase of the NTB-P treatment, and greater in NTCB and NTB-P than in NTB-F and CTB-F in 2 out of 3 yr. Similarly, biomass was greater with 80 than with 0 kg N ha(-1) in 1 out of 3 yr. Soil CO(2) flux increased from 8 mg C m(-2) h(-1) in early May to 239 mg C m(-2) h(-1) in mid-June as temperature increased and then declined to 3 mg C m(-2) h(-1) in September-October. Fluxes peaked immediately following substantial precipitation (>10 mm), especially in NTCB and NTB-P. Cumulative CO(2) flux from May to October was greater in 2006 and 2007 than in 2008, greater in cropping than in fallow phases, and greater in NTCB than in NTB-F. Tillage did not influence crop biomass and CO(2) flux but N fertilization had a variable effect on the flux in 2008. Similarly, soil total C content was not influenced by treatments. Annual cropping increased CO(2) flux compared with crop-fallow probably by increasing crop residue returns to soils and root and rhizosphere respiration. Inclusion of peas in the rotation with malt barley in the no-till system, which have been known to reduce N fertilization rates and sustain malt barley yields, resulted in a CO(2) flux similar to that in the CTB-F sequence.
Key Findings
1
Annual cropping increased CO2 flux compared with crop-fallow, likely due to greater crop residue returns and root/rhizosphere respiration.
2
Application of 80 kg N ha(-1) increased biomass relative to 0 kg N ha(-1) in 1 of 3 years, indicating variable fertilization response.
3
Crop biomass varied among years and was greater in barley phases than pea phases, and higher in NTCB and NTB-P than NTB-F and CTB-F in 2 of 3 years.
4
Cumulative May–October CO2 flux was higher in 2006 and 2007 than 2008, higher during cropping phases than fallow, and greater in no-till continuous barley (NTCB) than no-till barley-fallow (NTB-F).
5
Including peas in a no-till rotation produced CO2 flux similar to the conventional-tilled barley-fallow (CTB-F) sequence while potentially reducing N fertilizer needs without reducing barley yields.
6
Soil CO2 flux rose with temperature from 8 mg C m(-2) h(-1) in early May to 239 mg C m(-2) h(-1) in mid-June, then declined to ~3 mg C m(-2) h(-1) by September-October.
7
Tillage did not affect crop biomass or CO2 flux, and soil total carbon content (0–120 cm) was not influenced by treatments.
Research Object
Dryland Williams loam soil under different tillage, cropping sequence, and nitrogen fertilization treatments in eastern Montana
Research Subject
Effects of tillage, cropping sequence (including barley, pea, and fallow rotations) and N fertilization on crop biomass, soil surface CO2 flux (May–October) and soil carbon content (0–120 cm)
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2010-04-16
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