1984
DOI: 10.1080/10643388409381709
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Nitrogen transformations and loss in flooded soils and sediments

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Cited by 421 publications
(255 citation statements)
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References 151 publications
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“…This would be especially true for the alkaline soils due to their high pH and the presence of calcite (Singh and Nye 1986). Indeed, floodwater pH in the pot trials (pH 7.5-10.5) was high enough to support substantial NH 3 volatilization losses (Reddy and Patrick 1984). We observed consistently higher NH 4 + concentrations in the floodwater of C treatments, which confirmed the suppression of volatilization (Chen et al 1998) and underlined the importance of volatilization losses on the alkaline soils.…”
Section: Discussionsupporting
confidence: 72%
“…This would be especially true for the alkaline soils due to their high pH and the presence of calcite (Singh and Nye 1986). Indeed, floodwater pH in the pot trials (pH 7.5-10.5) was high enough to support substantial NH 3 volatilization losses (Reddy and Patrick 1984). We observed consistently higher NH 4 + concentrations in the floodwater of C treatments, which confirmed the suppression of volatilization (Chen et al 1998) and underlined the importance of volatilization losses on the alkaline soils.…”
Section: Discussionsupporting
confidence: 72%
“…Furthermore, from the stepwise regression analyses it can be deduced that, within this mesocosm experiment, there is an overall control of potential DEA by soil nitrate concentrations with respect to the agricultural grassland soils. This is in line with earlier studies (e.g., Reddy and Patrick Jr. 1984;Groffman and Tiedje 1989;Schipper et al 1993). Additional analyses revealed that indeed in both soil types nitrate and/ or carbon addition increased DEA (not shown).…”
Section: Mesocosm Application Considerationssupporting
confidence: 81%
“…However, wetland vegetation transports atmospheric oxygen through the stem, to the root, and into adjacent soil, which may oxidize the reduced microzone around the root surface (Armstrong, 1964;Brix & Schierup, 1990). Two distinct layers are formed around a root surface favoring nitrification-denitrification (Reddy & Patrick, 1984). Trapped sediments provide ammonification sites; nitrification can utilize ammonification product in the aerobic water, surface sediments and root surface; and denitrification occurs in the underlying sediment, releasing dinitrogen or nitrous oxide.…”
Section: External Sources Of Nitrogen In the Littoral Zonementioning
confidence: 99%