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No-till only increases N 2 O emissions in poorly-aerated soils

No-till only increases N 2 O emissions in poorly-aerated soils

No-till only increases N 2 O emissions in poorly-aerated soils

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100P. Rochette / Soil & Tillage Research 101 (2008) 97–100MacKenzie, A.F., Fan, M.X., Cadr<strong>in</strong>, F., 1997. Nitrous oxide emission as affected by<strong>till</strong>age, corn–soybean–alfalfa rotations and nitrogen fertilization. Can. J. Soil Sci.77, 145–152.Malhi, S.S., Lemke, R.L., Wang, Z., Chhabra, B., 2006. Tillage, nitrogen and cropresidue effects on crop yield, nutrient uptake, soil quality, and greenhouse gas<strong>emissions</strong>. Soil Till. Res. 90, 171–183.Malhi, S.S., Lemke, R.L., 2007. Tillage, crop residue and N fertilizer effects on cropyield, nutrient uptake, soil quality and nitrous oxide gas <strong>emissions</strong> <strong>in</strong> a second4-yr rotation cycle. Soil Till. Res. 96, 269–283.Metay, A., Oliver, R., Scopel, E., Douzet, J.-M., Alves Moreira, J.A., Maraux, F., Feigl, B.J.,Feller, C., 2007. N 2 O and CH 4 <strong>emissions</strong> from <strong>soils</strong> under conventional and no<strong>till</strong>management practices <strong>in</strong> Goiânia (Cerrados, Brazil). Geoderma 141, 78–88.M<strong>in</strong>asny, B., McBratney, A.B., Bristow, K.L., 1999. Comparison of differentapproaches to the development of pedotransfer functions for water-retentioncurves. Geoderma 93, 225–253.Mosier, A.R., Halvorson, A.D., Reule, C., Liu, X., 2006. Net global warm<strong>in</strong>g potentialand greenhouse gas <strong>in</strong>tensity <strong>in</strong> irrigated cropp<strong>in</strong>g systems <strong>in</strong> northeasternColorado. J. Environ. Qual. 35, 1584–1598.Mummey, D.L., Smith, J.L., Bluhm, G., 1998. Assessment of alternative soil managementpractices on N 2 O <strong>emissions</strong> from US agriculture. Agric. Ecosyst. Environ.70, 79–87.Oorts, K., Merckx, R., Gréhan, E., Labreuche, J., Nicolardot, B., 2007. Determ<strong>in</strong>ants ofannual fluxes of CO 2 and N 2 O <strong>in</strong> long-term no-<strong>till</strong>age and conventional <strong>till</strong>agesystems <strong>in</strong> northern France. Soil Till. Res. 95, 133–148.Palma, R.M., Rimolo, M., Saubidet, M.I., Conti, M.E., 1997. Influence of <strong>till</strong>age systemon denitrification <strong>in</strong> maize-cropped <strong>soils</strong>. Biol. Fertil. Soils 25, 142–146.Park<strong>in</strong>, T.B., Kaspar, T.C., 2006. Nitrous oxide <strong>emissions</strong> from corn–soybean systems<strong>in</strong> the midwest. J. Environ. Qual. 35, 1496–1506.Rochette, P., Angers, D.A., Chantigny, M.H., Bertrand, N., 2008. N 2 O <strong>emissions</strong>respond differently to no-<strong>till</strong> <strong>in</strong> a loam and a heavy clay soil. Soil Sci. Soc.Am. J. 72, 1363–1369.Six, J., Feller, C., Denef, K., Ogle, S.M., de Moraes Sa, J.C., Albrecht, A., 2002. Soilorganic matter, biota and aggregation <strong>in</strong> temperate and tropical <strong>soils</strong>—effects ofno-<strong>till</strong>age. Agronomie 22, 755–775.Six, J., Ogle, S.M., Breidt, F.J., Conant, R.T., Mosier, A.R., Paustian, K., 2004.The potential to mitigate global warm<strong>in</strong>g with no-<strong>till</strong>age management is <strong>only</strong>realized when practised <strong>in</strong> the long term. Global Change Biol. 10, 155–160.Smith, M.S., Tiedje, J.M., 1979. Phases of denitrification follow<strong>in</strong>g oxygen depletion<strong>in</strong> soil. Soil Biol. Biochem. 11, 261–267.VandenBygaart, A.J., McConkey, B.G., Angers, D.A., Smith, W., de Gooijer, H., Bentham,M., Mart<strong>in</strong>, T., 2008, <strong>in</strong> press. Soil carbon change factors for the CanadianAgriculture National Greenhouse Gas Inventory. Can. J. Soil Sci.

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