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The impact of agricultural erosion processes upon δ15N, δ13C, and C/N signatures of eroded-soil

Producción científica: Conference contributionrevisión exhaustiva

3 Citas (Scopus)

Resumen

The objective here is to show the ability of δ15N, δ13C, and C/N to capture the response of morphologic erosion processes. Analyses of δ15N, δ13C, and C/N of suspended eroded-soils, upland soils, and floodplain soils illustrate that an early event on March 7th 2003 was indicative of non-equilibrium sediment transport conditions. Later events on March 14th and 22nd produce eroded-soil in quasi-equilibrium conditions that may be predicted using rill erosion and headcut erosion models. It is expected that the sensitivity of δ15N, δ13C, and C/N will serve the purpose of sediment transport model calibration for further studying morphologic erosion processes.

Idioma originalEnglish
Título de la publicación alojadaRiver, Coastal and Estuarine Morphodynamics
Subtítulo de la publicación alojadaRCEM 2005 - Proceedings of the 4th IAHR Symposium on River, Coastal and Estuarine Morphodynamics
Páginas1147-1151
Número de páginas5
EstadoPublished - 2006
Evento4th IAHR Symposium on River, Coastal and Estuarine Morphodynamics, RCEM 2005 - Urbana, IL, United States
Duración: oct 4 2005oct 7 2005

Serie de la publicación

NombreRiver, Coastal and Estuarine Morphodynamics: RCEM 2005 - Proceedings of the 4th IAHR Symposium on River, Coastal and Estuarine Morphodynamics
Volumen2

Conference

Conference4th IAHR Symposium on River, Coastal and Estuarine Morphodynamics, RCEM 2005
País/TerritorioUnited States
CiudadUrbana, IL
Período10/4/0510/7/05

ASJC Scopus subject areas

  • Ecological Modeling
  • Environmental Chemistry

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