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Effect of pH on the rate of gaseous products of denitrification in a silt loam soil

Journal Article · · Soil Sci. Soc. Am. J.; (United States)
To examine the effect of soil pH on the rate and products of denitrification, a silt loam soil (Typic Arguidoll) was used that had been collected from a field experiment maintained at various pH levels for 18 years. The soil pH ranged from 4.6 to 6.9 and was nearly uniform in organic C (1.15 +/- 0.05%) and texture. Incubation was performed under He in all-glass systems that were sealed throughout the incubation period. The soils were amended with 100 ..mu..g/g of NO/sub 3//sup -/-N before incubation. Denitrification products (N/sub 2/O, NO, and N/sub 2/) and CO/sub 2/ were determined by gas chromatography using an ultrasonic detector. It appears that the rate of organic C mineralization rather than pH controls the rate of denitrification in C-limited systems. At 100 ..mu..g NO/sub 3//sup -/-N added per gram of soil, the overall rates of denitrification correlated with the rates of C mineralization (CO/sub 2/ evolution) but were not consistently related to pH or to total organic C. Soil pH did affect the products of denitrification. Nitrous oxide comprised 83% of the gaseous-N products for pH 4.6 and 5.4 when 90% of the NO/sub 3//sup -/ had been denitrified. The N/sub 2/O was then rapidly reduced to N/sub 2/. The highest amount of NO was observed at pH 4.6 and 5.4. At pH 6.0 the rate of production of N/sub 2/O exceeded the rate of reduction only for the first 2 d of incubation. However, N/sub 2/O was the dominant product until approx.83% of the NO/sub 3//sup -/ had been denitrified. At pH 6.9, N/sub 2/ was the dominant product after the 1st d of incubation. 21 references, 1 figure, 2 tables.
Research Organization:
Univ. of Wisconsin, Madison
OSTI ID:
7018668
Journal Information:
Soil Sci. Soc. Am. J.; (United States), Journal Name: Soil Sci. Soc. Am. J.; (United States) Vol. 46; ISSN SSSJD
Country of Publication:
United States
Language:
English