1964
DOI: 10.1038/201951a0
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Ammonium Production in Soil under Waterlogged Conditions as an Index of Nitrogen Availability

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Cited by 548 publications
(231 citation statements)
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“…The short-term anaerobic soil incubation method, developed by Waring & Bremner (1964) and modified by Keeney & Bremner (1966), involves the determination of NH 4 + -N in incubated and nonincubated soil and water suspensions. Five-gram soil samples were placed in test tubes (length 15 cm, inner diameter 1.6 cm) with 12.5 mL of deionized water.…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…The short-term anaerobic soil incubation method, developed by Waring & Bremner (1964) and modified by Keeney & Bremner (1966), involves the determination of NH 4 + -N in incubated and nonincubated soil and water suspensions. Five-gram soil samples were placed in test tubes (length 15 cm, inner diameter 1.6 cm) with 12.5 mL of deionized water.…”
Section: Methodsmentioning
confidence: 99%
“…The short-term (waterlogged) anaerobic incubation method developed by Waring & Bremner (1964) and modified by Keeney & Bremner (1966) involves the determination of available NH 4 + after soil samples were incubated under anaerobic conditions for seven or 14 days. Compared to aerobic incubation, the advantages of this short-term method include the following: only the available NH 4 + -N needs to be determined; appropriate moisture and water levels during incubation are easily stabilized; and a higher amount of N is mineralized (Keeney, 1982).…”
Section: Introductionmentioning
confidence: 99%
“…This was done using the waterlogged procedure of Waring and Bremner (1964), and total-N (<0.25 mm size) by modified Kjeldahl method (Dalal et al . 1984).…”
Section: Soil Sampling and Analysismentioning
confidence: 99%
“…On the other hand, the faster replacement of nitrate by ammonium in the soil in the tidally treated agricultural grassland monoliths compared to stagnant treatments does not support the alternative explanation directly. It can be seen as an argument in favour of the original hypothesis as it suggests an overall lower oxygen availability in the tidal treatments, with accumulation of ammonium as a consequence (e.g., Waring and Bremner 1964;Buresh and Patrick Jr. 1981;Bowden 1986). However, the apparent lower activity of ammonia-oxidizing bacteria in more oxygen-rich tidal treatments could be subscribed to the fact that they are poorer competitors for oxygen compared to the relatively large population of aerobic decomposers in these soils (Bodelier and Laanbroek 1997).…”
Section: Effects Of Tidementioning
confidence: 96%