Water erosion and connectivity analysis during a year with high precipitations in a watershed of Argentina

Soil erosion is a global concern because of its consequences for the environment and the economy of countries. In the Argentine Pampas Region, soil erosion process is a priority issue, although there is little information about sediment concentration (SC) in agricultural catchments. The study aimed...

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Otros Autores: Ares, María Guadalupe, Bongiorno, Fabricio, Holzman, Mauro, Chagas, Celio Ignacio, Varni, Marcelo, Entraigas, Ilda
Formato: Artículo
Lenguaje:Inglés
Materias:
Acceso en línea:http://ri.agro.uba.ar/files/intranet/articulo/2016ares1.pdf
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Aporte de:Registro referencial: Solicitar el recurso aquí
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245 1 0 |a Water erosion and connectivity analysis during a year with high precipitations in a watershed of Argentina 
520 |a Soil erosion is a global concern because of its consequences for the environment and the economy of countries. In the Argentine Pampas Region, soil erosion process is a priority issue, although there is little information about sediment concentration (SC) in agricultural catchments. The study aimed at assessing the factors that have a major influence on SC and discussing the dynamics of hydrological and sedimentological connectivity during 2012, a year with precipitation over the mean and significant erosive events. The study was conducted in a watershed of Buenos Aires province, Argentina. A linear regression model, that considered autocorrelation, was obtained. Maximum rainfall intensity in 30 minutes and peak flow were related to SC. An analysis of satellite images was carried out to discuss the hydrological connectivity, and a connectivity index was calculated to assess changes in sedimentological connectivity. The analyses suggested increments in hydrological and sedimentological connectivity, associated with the drainage area expansion and with water erosion rills. Hydrological connectivity is needed for sedimentological connectivity. However, increments in sedimentological connectivity may have been conditioned by the input of energy to detach and to transport particles. This may have been evidenced when flows exceeded a threshold runoff coefficient. 
653 |a HYDROLOGICAL CONNECTIVITY 
653 |a RILL EROSION 
653 |a RUNOFF 
653 |a SEDIMENT CONCENTRATION 
653 |a SEDIMENTOLOGICAL CONNECTIVITY 
700 1 |9 32717  |a Ares, María Guadalupe  |u CONICET . Buenos Aires, Argentina 
700 1 |a Bongiorno, Fabricio  |u Universidad Nacional del Centro. Facultad de Agronomía. Cátedra de Estadística y Diseño Experimental. Azul, Buenos Aires, Argentina.  |9 37042 
700 1 |a Holzman, Mauro  |u CONICET. Buenos Aires, Argentina.  |u Universidad Nacional del Centro. Facultad de Agronomía. Instituto de Hidrología de Llanuras ‘Dr EJ Usunoff’. Azul, Buenos Aires, Argentina.  |9 67512 
700 1 |a Chagas, Celio Ignacio  |u Universidad de Buenos Aires. Facultad de Agronomía. Laboratorio de Manejo y Conservación de Suelos. Buenos Aires, Argentina.  |9 12919 
700 1 |9 46117  |a Varni, Marcelo  |u Universidad Nacional del Centro. Facultad de Agronomía. Instituto de Hidrología de Llanuras ‘Dr EJ Usunoff’. Azul, Buenos Aires, Argentina. 
700 1 |9 38729  |a Entraigas, Ilda  |u Universidad Nacional del Centro. Facultad de Agronomía. Instituto de Hidrología de Llanuras ‘Dr EJ Usunoff’. Azul, Buenos Aires, Argentina. 
773 |t Hydrology Research  |g Vol.47, no.6 (2016), p.1239-1252, tbls., grafs., mapas, fot. 
856 |f 2016ares1  |i En Reservorio:  |q application/pdf  |u http://ri.agro.uba.ar/files/intranet/articulo/2016ares1.pdf  |x ARTI201807 
856 |u https://iwaponline.com/hr  |z LINK AL EDITOR 
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