THE EFFECT OF TEMPERATURE, pH, AND AERATION ON THE PRODUCTION OF NITROUS OXIDE AND GASEOUS NITROGEN—A ZERO-ORDER KINETIC MODEL

Focht, D. D.

doi:10.1097/00010694-197409000-00007

Cited by 153 publications

(82 citation statements)

References 0 publications

Supporting

Mentioning

Contrasting

Unclassified

Order By: Relevance

“…A similar observation was described by Focht (1974), who found that as the denitrification rate increased, the quantity of N 2 O evolved decreased, due to the greater increase in N 2 O reduction rate than in its formation rate. Their results also support and further develop the hypothesis proposed by Bailey & Beauchamp (1973) that account for the change in relative proportion of denitrification gases produced as temperature changes.…”

Section: Resultssupporting

confidence: 85%

N2O emissions from a cultivated mollisol: optimal time of day for sampling and the role of soil temperature

Cosentino

Fernández

Aureggi

et al. 2012

Rev. Bras. Ciênc. Solo

View full text Add to dashboard Cite

show abstract

Section: Resultssupporting

confidence: 85%

N2O emissions from a cultivated mollisol: optimal time of day for sampling and the role of soil temperature

Cosentino

Fernández

Aureggi

et al. 2012

Rev. Bras. Ciênc. Solo

View full text Add to dashboard Cite

show abstract

“…As noted in many earlier reports (78), there is considerable range in these values. For wetlands, including stream and lake sediments, the values are always low; N 2 dominates the efflux in anerobic environments (79)(80)(81). For upland ecosystems, a significant percentage of the efflux occurs as N 2 O, with an unknown proportion of this derived from nitrification rather than denitrification.…”

Section: Runoff and Fluvial Lossesmentioning

confidence: 99%

On the fate of anthropogenic nitrogen

Schlesinger

2009

Proc. Natl. Acad. Sci. U.S.A.

836

545

View full text Add to dashboard Cite

This article provides a synthesis of literature values to trace the fate of 150 Tg/yr anthropogenic nitrogen applied by humans to the Earth's land surface. Approximately 9 TgN/yr may be accumulating in the terrestrial biosphere in pools with residence times of ten to several hundred years. Enhanced fluvial transport of nitrogen in rivers and percolation to groundwater accounts for Ϸ35 and 15 TgN/yr, respectively. Greater denitrification in terrestrial soils and wetlands may account for the loss of Ϸ17 TgN/yr from the land surface, calculated by a compilation of data on the fraction of N2O emitted to the atmosphere and the current global rise of this gas in the atmosphere. A recent estimate of atmospheric transport of reactive nitrogen from land to sea (NOx and NHx) accounts for 48 TgN/yr. The total of these enhanced sinks, 124 TgN/yr, is less than the human-enhanced inputs to the land surface, indicating areas of needed additional attention to global nitrogen biogeochemistry. Policy makers should focus on increasing nitrogen-use efficiency in fertilization, reducing transport of reactive N to rivers and groundwater, and maximizing denitrification to its N2 endproduct.biogeochemistry ͉ denitrification ͉ nitrogen cycle

show abstract

“…Soil oxygenation status, usually inversely proportional to the amount of water in soil, is in many studies considered to be the key factor affecting the production of N 2 O. That inverse relation between the rate of denitrification and the content of oxygen is described in numerous publications (Bailey & Beauchamp 1971;Focht 1974;Burton & Beauchamp 1985).…”

Section: Redox Potential Versus Nitrate Content In Soilsmentioning

confidence: 99%

Redox potential, nitrate content and pH in flooded Eutric Cambisol during nitrate reduction

Włodarczyk¹,

Szarlip²,

Brzezińska³

et al. 2007

Res. Agric. Eng.

View full text Add to dashboard Cite

Topsoils from 16 arable Cambisols developed from sand, loam and silt were used to study soil ability to nitrate reduction under flooding conditions. The strongest drop of redox potential (Eh) was observed during the first day of soil flooding. Decreasing tendency in pH values was observed of alkaline and neutral soils, and an increase in pH of acid and strongly acid soils, accompanied by a fall in Eh values.

show abstract

THE EFFECT OF TEMPERATURE, pH, AND AERATION ON THE PRODUCTION OF NITROUS OXIDE AND GASEOUS NITROGEN—A ZERO-ORDER KINETIC MODEL

Cited by 153 publications

References 0 publications

N2O emissions from a cultivated mollisol: optimal time of day for sampling and the role of soil temperature

N2O emissions from a cultivated mollisol: optimal time of day for sampling and the role of soil temperature

On the fate of anthropogenic nitrogen

Redox potential, nitrate content and pH in flooded Eutric Cambisol during nitrate reduction

Contact Info

Product

Resources

About