• Authors:
    • Mielniczuk, J.
    • Dieckow, J.
    • Zanatta, J.
    • Bayer, C.
    • Vieira, F.
    • He, Z.
  • Source: Soil & Tillage Research
  • Volume: 96
  • Issue: 1/2
  • Year: 2007
  • Summary: The carbon management index (CMI) is derived from the total soil organic C pool and C lability and is useful to evaluate the capacity of management systems to promote soil quality. However, the CMI has not been commonly used for this purpose, possible due to some limitations of the 333 mM KMnO 4-chemical oxidation method conventionally employed to determine the labile C fraction. We hypothesized, however, that physical fractionation of organic matter is an alternative approach to determine the labile C. The objectives of this study were (i) to assess the physical fractionation with density (NaI 1.8 Mg m -3) and particle-size separation (53 m mesh) as alternative methods to the KMnO 4-chemical oxidation (60 and 333 mM) in determining the labile C and thus the CMI, and (ii) to evaluate the capacity of long-term (19 years) no-till cropping systems (oat/maize: O/M, oat + vetch/maize: O + V/M, oat + vetch/maize + cowpea: O + V/M + C, and pigeon pea + maize: P + M) and N fertilization (0 and 180 kg N ha -1) to promote the soil quality of a Southern Brazilian Acrisol, using the CMI as the main assessment parameter. Soil samples were collected from 0 to 12.5 cm layer, and the soil of an adjacent native grassland was taken as reference. The mean annual C input of the cropping systems varied from 3.4 to 6.0 Mg ha -1 and the highest amounts occurred in legume-based cropping systems and N fertilized treatments. The C pool index was positively related to the annual C input ( r2=0.93, P
  • Authors:
    • Okazaki, M.
    • Toyota, K.
    • Yanai, Y.
  • Source: Soil Science and Plant Nutrition
  • Volume: 53
  • Issue: 2
  • Year: 2007
  • Summary: Laboratory experiments were conducted to examine the effect of charcoal addition on N2O emissions resulting from rewetting of air-dried soil. Rewetting the soil at 73% and 83% of the water-filled pore space (WFPS) caused a N2O emission peak 6 h after the rewetting, and the cumulative N2O emissions throughout the 120-h incubation period were 11 ± 1 and 13 ± 1 mg N m-2 , respectively. However, rewetting at 64% WFPS did not cause detectable N2O emissions (-0.016 ± 0.082 mg N m-2 ), suggesting a severe sensitivity to soil moisture. When the soils were rewetted at 73% and 78% WFPS, the addition of charcoal to soil at 10 wt% supressed the N2O emissions by 89% . In contrast, the addition of the ash from the charcoal did not suppress the N2O emissions from soil rewetted at 73% WFPS. The addition of charcoal also significantly stimulated the N2O emissions from soil rewetted at 83% WFPS compared with the soil without charcoal addition (P < 0.01). Moreover, the addition of KCl and K2SO4 did not show a clear difference in the N2O emission pattern, although Cl- and SO42-, which were the major anions in the charcoal, had different effects on N2O-reducing activity. These results indicate that the suppression of N2O emissions by the addition of charcoal may not result in stimulation of the N2O-reducing activity in the soil because of changes in soil chemical properties.
  • Authors:
    • Mielniczuk, J.
    • Vieira, F. C. B.
    • Dieckow, J.
    • Bayer, C.
    • Zanatta, J. A.
  • Source: Soil & Tillage Research
  • Volume: 94
  • Issue: 2
  • Year: 2007
  • Summary: Conservation management systems can improve soil organic matter stocks and contribute to atmospheric C mitigation. This study was carried out in a 18-year long-term experiment conducted on a subtropical Acrisol in Southern Brazil to assess the potential of tillage systems [conventional tillage (CT) and no-till (NT)], cropping systems [oat/maize (O/M), vetch/maize (V/M) and oat + vetch/maize + cowpea (OV/MC)] and N fertilization [0 kg N ha-1 year-1 (0 N) and 180 kg N ha-1 year-1 (180 N)] for mitigating atmospheric C. For that, the soil organic carbon (SOC) accumulation and the C equivalent (CE) costs of the investigated management systems were taken into account in comparison to the CT O/M 0 N used as reference system. No-till is known to produce a less oxidative environment than CT and resulted in SOC accumulation, mainly in the 0-5 cm soil layer, at rates related to the addition of crop residues, which were increased by legume cover crops and N fertilization. Considering the reference treatment, the SOC accumulation rates in the 0-20 cm layer varied from 0.09 to 0.34 Mg ha-1 year-1 in CT and from 0.19 to 0.65 Mg ha-1 year-1 in NT. However, the SOC accumulation rates peaked during the first years (5th to 9th) after the adoption of the management practices and decreased exponentially over time, indicating that conservation soil management was a short-term strategy for atmospheric C mitigation. On the other hand, when the CE costs of tillage operations were taken into account, the benefits of NT to C mitigation compared to CT were enhanced. When CE costs related to N-based fertilizers were taken into account, the increases in SOC accumulation due to N did not necessarily improve atmospheric C mitigation, although this does not diminish the agricultural and economic importance of inorganic N fertilization.
  • Authors:
    • Denmead, O. T.
    • Macdonald, B. C. T.
    • Bryant, G.
    • Wang, W.
    • White, I.
    • Moody, P.
  • Source: Proceedings of the Australian Society of Sugar Cane Technologists
  • Volume: 29
  • Year: 2007
  • Authors:
    • Amado, T. J. C.
    • Pontelli, C. B.
    • Santi, A. L.
    • Viana, J. H. M.
    • Sulzbach, L. A. de S.
  • Source: Brazilian Journal of Agricultural Research (PAB)
  • Volume: 42
  • Issue: 8
  • Year: 2007
  • Summary: The objective of this work was to analyze the spatial and temporal yield variability of soybean, corn and wheat in a 57 ha cropland, without irrigation, under no-till for more than ten years in a Typic Hapludox, located in Palmeira das Missões, RS. Yield data of crops from 2000 to 2005 were collected using a combine equipped with yield monitor. Statistical and geostatistical analysis were performed to monitor the range of the spatial variability and its spatial dependence, as well as its behavior over the years. Soybean, corn and wheat yield present spatial variability, which is maintained over time. In dry years, yield variance coefficient increases compared to wet years. Corn was more efficient than soybean to identify spatial yield variability in the cropland.
  • Authors:
    • Grace,P.
  • Source: Healthy Soils Symposium
  • Year: 2007
  • Authors:
    • Grace, P.
    • Rowlings, D.
    • Peterson, N.
    • Weier, K.
    • Kiese, R.
    • Butterbach-Bahl, K.
  • Source: Non-CO2 Greenhouse Gas Fluxes in Australian-New Zealand Landscapes
  • Year: 2007
  • Authors:
    • Kelly, K.
    • Phillips, F.
    • Baigent, R.
  • Source: Greenhouse Gases and Animal Agriculture
  • Year: 2007
  • Authors:
    • Chen, D.
    • Kelly, K.
    • Li, Y.
  • Source: ASA-CSSA-SSSA International Annual Meetings (November 4-8, 2007)
  • Year: 2007
  • Authors:
    • Denmead, O. T.
    • Kelly, K. B.
    • Baigent, R.
    • Leuning, R.
    • Phillips, F. A.
  • Source: Agricultural and Forest Meteorology
  • Volume: 143
  • Issue: 1-2
  • Year: 2007