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- W2130766243 abstract "Enumeration of populations of nitrate respiring bacteria in estuarine sediments of the River Tay, Scotland, showed that bacteria capable of dissimilating NO−3 to NH+4 predominated over those denitrifying NO−3 to N2. On the other hand, seasonal data and depth profile studies, using 15NO−3, showed that denitrification was the principal route of dissimilatory NO−3 reduction (78-90% of NO−3 respired), with maximum rates of both processes occurring in the summer. Population densities of both populations of NO−3 respiring bacteria were highest in the 0-2 cm horizon in Tay estuary mud-flats where maximum rates of NO−3 respiration were also recorded [28-56 μg N d−1 (g dry wt sediment)−1]. Autotrophic nitrification rates in Tay estuary sediments showed a distinct seasonality, highest rates [0.93 μg N d−1 (g dry wt sediment)−1] occurring during the summer. Nitrification rates declined rapidly with sediment depth and were not detectable below the oxidized zone (3 cm). Population densities of autotrophic NH+4 and NO−2 oxidizing bacteria followed a similar pattern of distribution. Heterotrophic nitrification appears to play an insignificant role in Tay estuary sediments." @default.
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- W2130766243 date "1984-09-01" @default.
- W2130766243 modified "2023-10-14" @default.
- W2130766243 title "Dissimilatory Nitrate Reduction and Nitrification in Estuarine Sediments" @default.
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- W2130766243 doi "https://doi.org/10.1099/00221287-130-9-2301" @default.
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