Nitrogen dynamics in a feedlot soil

The feedlot system (FL) generates a high input of sewage causing imbalances in the cycling process of nitrogen (N) as well as a potential negative impact on the environment. The objective of this study was to deepen into the dynamics of N in a FL's soil so as to provide tools to reduce its envi...

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Autores principales: Wyngaard,N, Videla,C, Picone,L, Zamuner,E, Maceira,N
Lenguaje:English
Publicado: Chilean Society of Soil Science / Sociedad Chilena de la Ciencia del Suelo 2012
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Acceso en línea:http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-95162012000300016
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spelling oai:scielo:S0718-951620120003000162014-03-10Nitrogen dynamics in a feedlot soilWyngaard,NVidela,CPicone,LZamuner,EMaceira,N feedlot system mineral nitrogen urea nitrogen urease activity The feedlot system (FL) generates a high input of sewage causing imbalances in the cycling process of nitrogen (N) as well as a potential negative impact on the environment. The objective of this study was to deepen into the dynamics of N in a FL's soil so as to provide tools to reduce its environmental impact. The study was conducted in a FL, located in Balcarce County (Buenos Aires, Argentina). Soil samples were taken between November 2006 and May 2007 in a control Pasture, in the FL-High (Upper Slope position) and FL-Low (Lower Slope position) of the FL, and in the runoff area (RA). Urease activity and concentrations of Ammonium-N, Nitrate-N and urea-N were evaluated in the soil up to 60 cm depth. Urea-N values were always low (6 mg kg-1), due to the high urease activity measured (438 mg kg-1). Ammonium-N concentration was highest in FL-Low, reaching a value of 65.5 mg kg-1 at 40-60 cm soil depth. Nitrate-N concentration was highest in FL-High for all depths, with a maximum concentration of 97.4 mg kg-1 in the 0-10 cm layer; at 40-60 cm depth, Nitrate-N concentration in FL was 31.98 mg kg-1, higher than that in Pasture (1.21 mg kg-1). There were no differences in Nitrate-N concentration between Pasture and RA; hence, it can be inferred that there was no transport of nitrate by surface water flow from the FL to RA. However, the potential for groundwater contamination via nitrate, a mobile soil constituent, should be studied.info:eu-repo/semantics/openAccessChilean Society of Soil Science / Sociedad Chilena de la Ciencia del SueloJournal of soil science and plant nutrition v.12 n.3 20122012-09-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-95162012000300016en10.4067/S0718-95162012005000016
institution Scielo Chile
collection Scielo Chile
language English
topic feedlot system
mineral nitrogen
urea nitrogen
urease activity
spellingShingle feedlot system
mineral nitrogen
urea nitrogen
urease activity
Wyngaard,N
Videla,C
Picone,L
Zamuner,E
Maceira,N
Nitrogen dynamics in a feedlot soil
description The feedlot system (FL) generates a high input of sewage causing imbalances in the cycling process of nitrogen (N) as well as a potential negative impact on the environment. The objective of this study was to deepen into the dynamics of N in a FL's soil so as to provide tools to reduce its environmental impact. The study was conducted in a FL, located in Balcarce County (Buenos Aires, Argentina). Soil samples were taken between November 2006 and May 2007 in a control Pasture, in the FL-High (Upper Slope position) and FL-Low (Lower Slope position) of the FL, and in the runoff area (RA). Urease activity and concentrations of Ammonium-N, Nitrate-N and urea-N were evaluated in the soil up to 60 cm depth. Urea-N values were always low (6 mg kg-1), due to the high urease activity measured (438 mg kg-1). Ammonium-N concentration was highest in FL-Low, reaching a value of 65.5 mg kg-1 at 40-60 cm soil depth. Nitrate-N concentration was highest in FL-High for all depths, with a maximum concentration of 97.4 mg kg-1 in the 0-10 cm layer; at 40-60 cm depth, Nitrate-N concentration in FL was 31.98 mg kg-1, higher than that in Pasture (1.21 mg kg-1). There were no differences in Nitrate-N concentration between Pasture and RA; hence, it can be inferred that there was no transport of nitrate by surface water flow from the FL to RA. However, the potential for groundwater contamination via nitrate, a mobile soil constituent, should be studied.
author Wyngaard,N
Videla,C
Picone,L
Zamuner,E
Maceira,N
author_facet Wyngaard,N
Videla,C
Picone,L
Zamuner,E
Maceira,N
author_sort Wyngaard,N
title Nitrogen dynamics in a feedlot soil
title_short Nitrogen dynamics in a feedlot soil
title_full Nitrogen dynamics in a feedlot soil
title_fullStr Nitrogen dynamics in a feedlot soil
title_full_unstemmed Nitrogen dynamics in a feedlot soil
title_sort nitrogen dynamics in a feedlot soil
publisher Chilean Society of Soil Science / Sociedad Chilena de la Ciencia del Suelo
publishDate 2012
url http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-95162012000300016
work_keys_str_mv AT wyngaardn nitrogendynamicsinafeedlotsoil
AT videlac nitrogendynamicsinafeedlotsoil
AT piconel nitrogendynamicsinafeedlotsoil
AT zamunere nitrogendynamicsinafeedlotsoil
AT maceiran nitrogendynamicsinafeedlotsoil
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