Carbon and net nitrogen mineralisation in two forest soils amended with different concentrations of biuret

• Published in: Soil biology & biochemistry Vol. 35; no. 6; pp. 855 - 866
• Main Authors: Xue, J.M., Sands, R., Clinton, P.W., Payn, T.W., Skinner, M.F.
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier Ltd 01-06-2003; New York, NY Elsevier Science
• Subjects: Agronomy. Soil science and plant productions; Biological and medical sciences; Biuret; C and net N mineralisation; Fundamental and applied biological sciences. Psychology; General agronomy. Plant production; Microbial biomass; Nitrogen fertilization; Nitrogen, phosphorus, potassium fertilizations; Priming effect; Soil-plant relationships. Soil fertility. Fertilization. Amendments; Microbial biomass; Biuret; Priming effect; C and net N mineralisation; Carbon cycle; Nitrogen cycle; Mineralization; Ureas; Forest soil; Nitrogen fertilizer
• ISSN: 0038-0717; 1879-3428
• DOI: 10.1016/S0038-0717(03)00141-X

Biuret is a known contaminant of urea fertilisers that might be useful as a slow release N fertiliser for forestry. We studied carbon (C), net nitrogen (N) mineralisation and soil microbial biomass C and N dynamics in two forest soils (a sandy loam and a silt loam) during a 16-week long incubation following application of biuret (C 23.3%, N 40.8%, O 30.0% and H 4.9%) at concentrations of 0, 2, 10, 100 and 1000 mg kg
−1 (oven-dried) soil to assess the potential of biuret as a slow-release N fertiliser. Lower concentrations of biuret specifically increased C mineralisation and soil microbial biomass C in the sandy loam soil, but not in the silt loam soil. A significant decrease of microbial biomass C was found in both soils at week 16 after biuret was applied at higher concentrations. C mineralisation declined with duration of incubation in both soils due to decreased C availability. Biuret at concentrations from 10 to 100 mg kg
−1 soil had a significantly positive priming effect on soil organic N mineralisation in both soils. The causes for the priming effects were related to the stimulation of microbial growth and activity at an early stage of the incubation and/or the death of microbes at a later stage, which was biuret-concentration-dependent. The patterns in NH
4
+-N accumulation differed markedly between the two soils. Net N mineralisation and nitrification were much greater in the sandy loam soil than in the silt loam soil. However, the onset of net nitrification was earlier in the silt loam soil. Biuret might be a potential slow-release N source in the silt loam soil.