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  • COMMUNICATIONS  (1)
  • nitrous oxide  (1)
  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 163 (1994), S. 235-241 
    ISSN: 1573-5036
    Keywords: denitrification ; grassland ; nitrification ; nitrous oxide ; sandy soil ; urine
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Denitrification and N2O emission rates were measured following two applications of artificial urine (40 g urine-N m−2) to a perennial rye-grass sward on sandy soil. To distinguish between N2O emission from denitrification or nitrification, urine was also applied with a nitrification inhibitor (dicyandiamide, DCD). During a 14 day period following each application, the soil was frequently sampled, and incubated with and without acetylene to measure denitrification and N2O emission rates, respectively. Urine application significantly increased denitrification and N2O emission rates up to 14 days after application, with rates amounting to 0.9 and 0.6 g N m−2 day−1 (9 and 6 kg N ha−1 day−1), respectively. When DCD was added to the urine, N2O emission rates were significantly lower from 3 to 7 days after urine application onwards. Denitrification was the main source of N2O immediately following each urine application. 14 days after the first application, when soil water contents dropped to 15% (v/v) N2O mainly derived from nitrification. Total denitrification losses during the 14 day periods were 7 g N m−2, or 18% of the urine-N applied. Total N2O emission losses were 6.5 and 3 g N m−2, or 16% and 8% of the urine-N applied for the two periods. The minimum estimations of denitrification and N2O emission losses from urine-affected soil were 45 to 55 kg N ha−1 year−1, and 20 to 50 kg N ha−1 year−1, respectively.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2019-06-27
    Description: The current distribution and impedance of a thin cylindrical antenna with parallel orientation to the static magnetic field of a lossy magnetoplasma is calculated with the method of moments. The electric field produced by an infinitesimal current source is first derived. Results are presented for a wide range of plasma parameters. Reasonable answers are obtained for all cases except for the overdense hyperbolic case. A discussion of the numerical stability is included which not only applies to this problem but other applications of the method of moments.
    Keywords: COMMUNICATIONS
    Type: NASA-CR-128114 , SR-19 , REPT-72-3 , UILU-ENG-72-2546
    Format: application/pdf
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