Nitrogen Transformations and Microbial Population Dynamics in Soil Amended with Fermentation Residue
Autor: | M. G. Volz, G. H. Heichel |
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Rok vydání: | 1979 |
Předmět: |
education.field_of_study
Environmental Engineering Aerobic bacteria Chemistry Soil organic matter Population food and beverages Growing season Management Monitoring Policy and Law Pollution Agronomy Loam Soil water Fermentation Leaching (agriculture) education Waste Management and Disposal Water Science and Technology |
Zdroj: | Journal of Environmental Quality. 8:434-439 |
ISSN: | 1537-2537 0047-2425 |
DOI: | 10.2134/jeq1979.00472425000800030033x |
Popis: | To evaluate the fate of N in an agricultural soil treated with an N-rich industrial byproduct, fermentation residue was applied to Yalesville fine, sandy loam at a loading rate of 75 dry metric tons/ha, or 2,130 and 1,780 kg N/ha during 1975 and 1976, respectively. Treated and control plots were planted to soybeans (Glycine max L. Merr.) each year. The treated plots yielded 4,350 kg/ha of soybean grain compared with 3,600 kg/ha for the controls in 1975, and 4,100 kg/ha compared with 3,700 kg/ha in 1976. Yield enhancements attributable to fermentation residue application were significant (P = 0.05) each year despite the severe repression of nodulation on treated plants compared with controls. During the growing season, NO₃⁻-N accumulations >80 µg/g oven dry soil were observed in the top 5 cm of treated soil, compared with accumulations of 15 µg/g or less in the control. Further, elevated NO₃‘-N levels were observed in the top 91 cm of treated soil throughout the fallow and growing seasons, when compared with control plots, suggesting that some of the applied N may have been transported to the water table as NO₃⁻. Populations of five physiological groups of microorganisms closely mirrored soil levels of NO₃⁻-N and NH₄⁺-N in both experiments. Denitrifying bacteria reached population densities of 3.0 × 10⁹/g oven dry treated soil compared with a maximum of 6.8 × 10⁵/g for control soil during the growing season. Enhanced N transforming activity by microorganisms in soil receiving fermentation residue compared with the control soil was supported by the elevated populations of NH₄⁺ and NO₂⁻ oxidizing bacteria, and NO₃⁻ reducing-, denitrifying-, and heterotrophic aerobic bacteria observed throughout the fallow and growing seasons. Although application of fermentation residue significantly increased soybean yields, the limited recovery of added N by the crop and the likelihood of substantial N losses suggest a reassessment of application rates or efforts to stabilize N applied to soils from fermentation residues. |
Databáze: | OpenAIRE |
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