Land use and landscape position influence soil organic phosphorus speciation in a mixed land‐use watershed
- Autores
- Perillo, Vanesa Liliana; Cade Menun, Barbara; Ivancic, Monika; Ross, Donald S.; Wemple, Beverley C.
- Año de publicación
- 2021
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Land use can significantly alter soil P forms, which will influence P loss in runoff. Organic P (Po) compounds are an important component of soil P, but their forms and cycling in soils with different land uses are still poorly understood. In addition, streambanks are potential sources of P loss; P forms and concentrations in streambank soils may vary with land use, affecting potential P loss to water. This study used solution 31P nuclear magnetic resonance spectroscopy (P-NMR) to characterize and quantify P in interior and streambank soils (0-10 cm) under duplicate sites from four different land uses along streams in the Missisquoi River Basin (VT, USA) ? silage corn, hay meadow, emergent wetlands and forest. Orthophosphate monoesters were the dominant P compound class regardless of land use or landscape position. Forest soils had the lowest Po concentrations, less labile P forms than other soils, and significantly lower concentrations of total inositol hexakisphosphates and total orthophosphate monoesters compared to corn soils. Riparian buffer zones for agricultural soils lower P concentrations in streambank soils for many soil P pools relative to interior soils. The wetland soils of this study had P concentrations and P forms that were similar to those for interior agricultural soils, and generally showed no reduction in P concentrations in streambank soils relative to interior soils. This is consistent with the role of wetlands as P sinks in the landscape, but also suggests these wetlands should be carefully monitored to minimize P accumulation, especially in streambank soils.
Fil: Perillo, Vanesa Liliana. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Argentino de Oceanografía. Universidad Nacional del Sur. Instituto Argentino de Oceanografía; Argentina. Universidad Nacional del Sur. Departamento de Biología, Bioquímica y Farmacia; Argentina. University of Vermont; Estados Unidos
Fil: Cade Menun, Barbara. Swift Current Research And Development Centre.; Canadá
Fil: Ivancic, Monika. University of Vermont; Estados Unidos
Fil: Ross, Donald S.. University of Vermont; Estados Unidos
Fil: Wemple, Beverley C.. University of Vermont; Estados Unidos - Materia
-
ORGANIC PHOSPHORUS
LAND USE
RIPARIAN SOIL
STREAMBANK SOIL - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by/2.5/ar/
- Repositorio
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/158129
Ver los metadatos del registro completo
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Land use and landscape position influence soil organic phosphorus speciation in a mixed land‐use watershedPerillo, Vanesa LilianaCade Menun, BarbaraIvancic, MonikaRoss, Donald S.Wemple, Beverley C.ORGANIC PHOSPHORUSLAND USERIPARIAN SOILSTREAMBANK SOILhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Land use can significantly alter soil P forms, which will influence P loss in runoff. Organic P (Po) compounds are an important component of soil P, but their forms and cycling in soils with different land uses are still poorly understood. In addition, streambanks are potential sources of P loss; P forms and concentrations in streambank soils may vary with land use, affecting potential P loss to water. This study used solution 31P nuclear magnetic resonance spectroscopy (P-NMR) to characterize and quantify P in interior and streambank soils (0-10 cm) under duplicate sites from four different land uses along streams in the Missisquoi River Basin (VT, USA) ? silage corn, hay meadow, emergent wetlands and forest. Orthophosphate monoesters were the dominant P compound class regardless of land use or landscape position. Forest soils had the lowest Po concentrations, less labile P forms than other soils, and significantly lower concentrations of total inositol hexakisphosphates and total orthophosphate monoesters compared to corn soils. Riparian buffer zones for agricultural soils lower P concentrations in streambank soils for many soil P pools relative to interior soils. The wetland soils of this study had P concentrations and P forms that were similar to those for interior agricultural soils, and generally showed no reduction in P concentrations in streambank soils relative to interior soils. This is consistent with the role of wetlands as P sinks in the landscape, but also suggests these wetlands should be carefully monitored to minimize P accumulation, especially in streambank soils.Fil: Perillo, Vanesa Liliana. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Argentino de Oceanografía. Universidad Nacional del Sur. Instituto Argentino de Oceanografía; Argentina. Universidad Nacional del Sur. Departamento de Biología, Bioquímica y Farmacia; Argentina. University of Vermont; Estados UnidosFil: Cade Menun, Barbara. Swift Current Research And Development Centre.; CanadáFil: Ivancic, Monika. University of Vermont; Estados UnidosFil: Ross, Donald S.. University of Vermont; Estados UnidosFil: Wemple, Beverley C.. University of Vermont; Estados UnidosAmerican Society of Agronomy2021-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/158129Perillo, Vanesa Liliana; Cade Menun, Barbara; Ivancic, Monika; Ross, Donald S.; Wemple, Beverley C.; Land use and landscape position influence soil organic phosphorus speciation in a mixed land‐use watershed; American Society of Agronomy; Journal of Environmental Quality; 50; 5-2021; 967-9780047-2425CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/10.1002/jeq2.20237info:eu-repo/semantics/altIdentifier/doi/10.1002/jeq2.20237info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-11-12T09:55:53Zoai:ri.conicet.gov.ar:11336/158129instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-11-12 09:55:53.857CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
| dc.title.none.fl_str_mv |
Land use and landscape position influence soil organic phosphorus speciation in a mixed land‐use watershed |
| title |
Land use and landscape position influence soil organic phosphorus speciation in a mixed land‐use watershed |
| spellingShingle |
Land use and landscape position influence soil organic phosphorus speciation in a mixed land‐use watershed Perillo, Vanesa Liliana ORGANIC PHOSPHORUS LAND USE RIPARIAN SOIL STREAMBANK SOIL |
| title_short |
Land use and landscape position influence soil organic phosphorus speciation in a mixed land‐use watershed |
| title_full |
Land use and landscape position influence soil organic phosphorus speciation in a mixed land‐use watershed |
| title_fullStr |
Land use and landscape position influence soil organic phosphorus speciation in a mixed land‐use watershed |
| title_full_unstemmed |
Land use and landscape position influence soil organic phosphorus speciation in a mixed land‐use watershed |
| title_sort |
Land use and landscape position influence soil organic phosphorus speciation in a mixed land‐use watershed |
| dc.creator.none.fl_str_mv |
Perillo, Vanesa Liliana Cade Menun, Barbara Ivancic, Monika Ross, Donald S. Wemple, Beverley C. |
| author |
Perillo, Vanesa Liliana |
| author_facet |
Perillo, Vanesa Liliana Cade Menun, Barbara Ivancic, Monika Ross, Donald S. Wemple, Beverley C. |
| author_role |
author |
| author2 |
Cade Menun, Barbara Ivancic, Monika Ross, Donald S. Wemple, Beverley C. |
| author2_role |
author author author author |
| dc.subject.none.fl_str_mv |
ORGANIC PHOSPHORUS LAND USE RIPARIAN SOIL STREAMBANK SOIL |
| topic |
ORGANIC PHOSPHORUS LAND USE RIPARIAN SOIL STREAMBANK SOIL |
| purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| dc.description.none.fl_txt_mv |
Land use can significantly alter soil P forms, which will influence P loss in runoff. Organic P (Po) compounds are an important component of soil P, but their forms and cycling in soils with different land uses are still poorly understood. In addition, streambanks are potential sources of P loss; P forms and concentrations in streambank soils may vary with land use, affecting potential P loss to water. This study used solution 31P nuclear magnetic resonance spectroscopy (P-NMR) to characterize and quantify P in interior and streambank soils (0-10 cm) under duplicate sites from four different land uses along streams in the Missisquoi River Basin (VT, USA) ? silage corn, hay meadow, emergent wetlands and forest. Orthophosphate monoesters were the dominant P compound class regardless of land use or landscape position. Forest soils had the lowest Po concentrations, less labile P forms than other soils, and significantly lower concentrations of total inositol hexakisphosphates and total orthophosphate monoesters compared to corn soils. Riparian buffer zones for agricultural soils lower P concentrations in streambank soils for many soil P pools relative to interior soils. The wetland soils of this study had P concentrations and P forms that were similar to those for interior agricultural soils, and generally showed no reduction in P concentrations in streambank soils relative to interior soils. This is consistent with the role of wetlands as P sinks in the landscape, but also suggests these wetlands should be carefully monitored to minimize P accumulation, especially in streambank soils. Fil: Perillo, Vanesa Liliana. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Argentino de Oceanografía. Universidad Nacional del Sur. Instituto Argentino de Oceanografía; Argentina. Universidad Nacional del Sur. Departamento de Biología, Bioquímica y Farmacia; Argentina. University of Vermont; Estados Unidos Fil: Cade Menun, Barbara. Swift Current Research And Development Centre.; Canadá Fil: Ivancic, Monika. University of Vermont; Estados Unidos Fil: Ross, Donald S.. University of Vermont; Estados Unidos Fil: Wemple, Beverley C.. University of Vermont; Estados Unidos |
| description |
Land use can significantly alter soil P forms, which will influence P loss in runoff. Organic P (Po) compounds are an important component of soil P, but their forms and cycling in soils with different land uses are still poorly understood. In addition, streambanks are potential sources of P loss; P forms and concentrations in streambank soils may vary with land use, affecting potential P loss to water. This study used solution 31P nuclear magnetic resonance spectroscopy (P-NMR) to characterize and quantify P in interior and streambank soils (0-10 cm) under duplicate sites from four different land uses along streams in the Missisquoi River Basin (VT, USA) ? silage corn, hay meadow, emergent wetlands and forest. Orthophosphate monoesters were the dominant P compound class regardless of land use or landscape position. Forest soils had the lowest Po concentrations, less labile P forms than other soils, and significantly lower concentrations of total inositol hexakisphosphates and total orthophosphate monoesters compared to corn soils. Riparian buffer zones for agricultural soils lower P concentrations in streambank soils for many soil P pools relative to interior soils. The wetland soils of this study had P concentrations and P forms that were similar to those for interior agricultural soils, and generally showed no reduction in P concentrations in streambank soils relative to interior soils. This is consistent with the role of wetlands as P sinks in the landscape, but also suggests these wetlands should be carefully monitored to minimize P accumulation, especially in streambank soils. |
| publishDate |
2021 |
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2021-05 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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article |
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publishedVersion |
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http://hdl.handle.net/11336/158129 Perillo, Vanesa Liliana; Cade Menun, Barbara; Ivancic, Monika; Ross, Donald S.; Wemple, Beverley C.; Land use and landscape position influence soil organic phosphorus speciation in a mixed land‐use watershed; American Society of Agronomy; Journal of Environmental Quality; 50; 5-2021; 967-978 0047-2425 CONICET Digital CONICET |
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http://hdl.handle.net/11336/158129 |
| identifier_str_mv |
Perillo, Vanesa Liliana; Cade Menun, Barbara; Ivancic, Monika; Ross, Donald S.; Wemple, Beverley C.; Land use and landscape position influence soil organic phosphorus speciation in a mixed land‐use watershed; American Society of Agronomy; Journal of Environmental Quality; 50; 5-2021; 967-978 0047-2425 CONICET Digital CONICET |
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eng |
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eng |
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American Society of Agronomy |
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American Society of Agronomy |
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