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Title: Effect of acidity on nitrate reduction and denitrification in lower Coastal Plain soils. [North Carolina]

Journal Article · · Soil Sci. Soc. Am. J.; (United States)

Denitrification and nitrate reduction to NH/sub 4//sup +/-N and organic N were investigated in the laboratory using surface samples of Histosols and Ultisols. A wide range of pH (3.4 to 7.3) was obtained by liming acidic virgin soils and by selecting a range of field-limed soils. When incubated under waterlogged conditions in the presence of glucose for 2 d at 25/sup 0/C, there was a very low loss of NO/sub 3//sup -/-N below a pH of 4.0 and an increase in NO/sub 3//sup -/-N loss with pH up to a pH of 6.0. After 12 d of incubation, NO/sub 3//sup -/-N loss (105-115 mg L/sup -1/) was complete from soils at all pH values. Laboratory and field-limed soils behaved as expected from their pHs. For soils incubated for 2 d without glucose, there was a moderate effect of soil pH upon NO/sub 3//sup -/-N loss. For incubations longer than 2 d soluble C appeared to be more important than pH in controlling loss of NO/sub 3//sup -/-N. Soils with pH <4.0 showed unexpectedly high NO/sub 3//sup -/-N loss when incubated for periods >12 d without glucose. Experiments with /sup 15/NO/sub 3//sup -/-N showed that 16 to 20% of the NO/sub 3//sup -/-N loss in soils with pH <4.0 was due to reduction to NH/sub 4//sup +/-N and orgainc N but only 1 to 2% for soils with pH >4.0. Evidence indicates that the reduction was dissimilatory and unrelated to levels of soluble C. Denitrification was substantial in the soils with pH <4.0 and of a similar level to that for moderately acidic soils (pH 4.4-5.4). In the neutral soils (pH 6.9-7.3) denitrification was much higher but much of the increase appeared due to the higher level of soluble C.

Research Organization:
North Carolina State Univ., Raleigh
OSTI ID:
6750363
Journal Information:
Soil Sci. Soc. Am. J.; (United States), Vol. 47
Country of Publication:
United States
Language:
English