Using δ15N values to characterise the nitrogen nutrient pathways from intensive animal units
Author(s)
Skinner, RA
Ineson, P
Jones, H
Sleep, D
Rank, R
Griffith University Author(s)
Year published
2006
Metadata
Show full item recordAbstract
Previous studies on foliar δ 15N values, in certain bryophytes, have indicated signature similarities to source pollutants. The object of this study was to investigate the effect further, by examining the mechanisms whereby isotopic fractionation occurs in systems such as atmospheric ammonia (NH3), throughfall, vegetation and soil. Measurements taken in and around point emission sources will then be used to characterise the various fractionation effects associated with these N transformations, as well as to demonstrate some of the issues associated with using δ 15N values as pollution indicators. The atmospheric dispersion ...
View more >Previous studies on foliar δ 15N values, in certain bryophytes, have indicated signature similarities to source pollutants. The object of this study was to investigate the effect further, by examining the mechanisms whereby isotopic fractionation occurs in systems such as atmospheric ammonia (NH3), throughfall, vegetation and soil. Measurements taken in and around point emission sources will then be used to characterise the various fractionation effects associated with these N transformations, as well as to demonstrate some of the issues associated with using δ 15N values as pollution indicators. The atmospheric dispersion model UK‐ADMS has also been used to model atmospheric δ 15NH3 emissions, with signatures exhibiting marked negative shifts immediately downwind of an agricultural NH3 source. Similar dispersion patterns were mapped for NH3 concentration data illustrating the link between these two forms of measurement.
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View more >Previous studies on foliar δ 15N values, in certain bryophytes, have indicated signature similarities to source pollutants. The object of this study was to investigate the effect further, by examining the mechanisms whereby isotopic fractionation occurs in systems such as atmospheric ammonia (NH3), throughfall, vegetation and soil. Measurements taken in and around point emission sources will then be used to characterise the various fractionation effects associated with these N transformations, as well as to demonstrate some of the issues associated with using δ 15N values as pollution indicators. The atmospheric dispersion model UK‐ADMS has also been used to model atmospheric δ 15NH3 emissions, with signatures exhibiting marked negative shifts immediately downwind of an agricultural NH3 source. Similar dispersion patterns were mapped for NH3 concentration data illustrating the link between these two forms of measurement.
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Journal Title
Rapid Communications in Mass Spectrometry
Volume
20
Issue
19
Subject
Chemical sciences
Earth sciences
Biological sciences