Use of a flowing helium atmosphere incubation technique to measure the effects of denitrification controls applied to intact cores of a clay soil

• Published in: Soil biology & biochemistry 1997-09, Vol.29 (9), p.1337-1344
• Main Authors: Scholefield, D., Hawkins, J.M.B., Jackson, S.M.
• Format: Article
• Language: English
• Subjects: Agronomy. Soil science and plant productions; Biological and medical sciences; Chemical, physicochemical, biochemical and biological properties; Fundamental and applied biological sciences. Psychology; Organic matter; Physics, chemistry, biochemistry and biology of agricultural and forest soils; Soil science
• ISSN: 0038-0717; 1879-3428
• DOI: 10.1016/S0038-0717(97)00059-X

Patterns of evolution of N 2O and N 2 due to denitrification in intact cores of a clay loam soil were measured using a He O 2 atmosphere “flow-over” incubation system housed in a temperature-controlled room. Square section cores were taken from a grassland site in SW England under extensive grazing management and assembled into composite turves, each comprising 25 cores in a 5 × 5 array, which were placed in each of six incubation vessels. After replacement of N 2 in the soil pores with He, the headspace gas above each turf was continuously flushed with a stream of 20% O 2 in He, which was directed to either waste or dual gas chromatographs. The effects of the major controls on denitrification were investigated while simulating the application of NO 3 − fertilizer to the sward made via a N 2-free irrigation assembly placed above each incubation vessel. Denitrification increased with increasing NO 3 added within the range equivalent to 0–150 kg ha −1, and with increasing water-filled pore space within the range 70–90%. The denitrification response to variation in the other controls did not agree well with the results of previous studies: although the initial rate of denitrification increased with a Q 10 of 2 within the range 5–30°C, there was no clear trend in the total N denitrified at temperatures above 10°C; denitrification decreased with increasing soil pH within the range 5.1–9.4. The N 2O-to-N 2 ratio increased with increasing NO 3 −, and with decreasing water content, pH and temperature. Antecedent soil aerobicity also had a large effect on the N 2O-to-N 2 ratio: after 7 d of either aerobic or anaerobic conditioning, the ratio was 1.74 or 0.15, respectively. In most of the experimental runs, less than 100%, and sometimes less than 50%, of the added N could be accounted for in gaseous products. The results indicate the need to develop and apply techniques that enable concurrent measurement of all relevant processes of N transformation, such as assimilatory NO 3 − reduction, nitrification and plant uptake, if prediction of denitrification in field soils is to be improved.