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Decomposition of methyl nitrite in solutions and soils

Journal Article · · Soil Sci. Soc. Am. J.; (United States)
OSTI ID:6938393

The role of hydrolysis as a process affecting the concentration of CH/sub 3/ONO in the soil atmosphere was investigated by measuring the sorption of CH/sub 3/ONO and the formation of NO/sub 2//sup -/ and NO/sub 3//sup -/ in two soils (-33-kPa soil water potential) and three solutions in the dark at 20/sup 0/C for 10 h. Soil pH and the pH of distilled H/sub 2/O decreased on absorption of CH/sub 3/ONO. In acidic solutions (distilled H/sub 2/O and 0.1MH/sub 2/SO/sub 4/), >90% of CH/sub 3/ONO was recovered as NO/sub 3//sup -/, whereas to an alkaline soil and 0.2 M NaOH, >80% was recovered as NO/sub 2//sup -/. Only 0 to 7% of CH/sub 3/ONO remained in the atmosphere. In an acid soil only 50% of CH/sub 3/ONO was recovered as (CH/sub 3/ONO + NO/sub 2//sup -/ + NO/sub 3//sup -/-N. Recoveries of N in ..gamma..-irradiated and nonirradiated soils did not differ significantly. The data indicate that CH/sub 3/ONO was rapidly hydrolysed in solutions and in soils (CH/sub 3/ONO + H/sub 2/O in equilibrium CH/sub 3/OH + HNO/sub 2/), and that NO/sub 3//sup -/ formed via the self-decomposition of HNO/sub 2/. The low recovery of N in the acid soil may have been due to the participation of HNO/sub 2/ in chemodenitrification reactions. The rapid hydrolysis of CH/sub 3/ONO is likely to inhibit the emission of CH/sub 3/ONO formed in soils, and to cause the sorption of CH/sub 3/ONO evolved from soils in closed systems.

Research Organization:
Univ. of Melbourne, Parkville, Australia
OSTI ID:
6938393
Journal Information:
Soil Sci. Soc. Am. J.; (United States), Journal Name: Soil Sci. Soc. Am. J.; (United States) Vol. 50:1; ISSN SSSJD
Country of Publication:
United States
Language:
English