OPTIMIZACION DEL USO DE LA VEGETACION EN VAGUADAS DE AREAS CULTIVADAS PARA MINIMIZAR LA EROSION Y CONTAMINACION DIFUSA Y MEJORAR EL PAISAJE Y LA BIODIVERSIDAD
AGL2015-65036-C3-1-R
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Nombre agencia financiadora Ministerio de Economía y Competitividad
Acrónimo agencia financiadora MINECO
Programa Programa Estatal de I+D+I Orientada a los Retos de la Sociedad
Subprograma Todos los retos
Convocatoria Proyectos de I+D+I dentro del Programa Estatal Retos de la Sociedad (2015)
Año convocatoria 2015
Unidad de gestión Dirección General de Investigación Científica y Técnica
Centro beneficiario AGENCIA ESTATAL CONSEJO SUPERIOR DE INVESTIGACIONES CIENTIFICAS (CSIC)
Centro realización DPTO. DE AGRONOMIA
Identificador persistente http://dx.doi.org/10.13039/501100003329
Resultados relacionados
Resultados totales (Incluyendo duplicados): 1Encontrada(s) 1 página(s)
Set de datos (Dataset). 2020
Underlaying data for paper "Autonomous shallow flow runoff detector for hillslope hydrological studies", Datos correspondientes al artículo "Autonomous shallow flow runoff detector for hillslope hydrological studies"
DIGITAL.CSIC. Repositorio Institucional del CSIC
- Chamber, Enrique
- Pérez Alcántara, Rafael
- Gómez Calero, José Alfonso
Data corresponding to the calibration and validation of overland flow detectors presented in
in paper "Autonomous shallow flow runoff detector for hillslope hydrological studies".-- Datos de calibración y validación de detectores de escorrentía presentados en el artículo "Autonomous shallow flow runoff detector for hillslope hydrological studies"., This is the underlaying data for the manuscript which describes the development, calibration and validation of an autonomous overland flow detector (OFD) for the measurement and recording of shallow runoff depth at varying recording intervals based on measurement of runoff water electrical conductivity (EC). Using electronic components easily available and of moderate cost, approximately367€ per unit, the proposed device can operate for a broad range of surface overland flow with EC from 0 to 435 µS cm-1 with a regular charge using a small built-in cell panel. It was originally intended for use in experiments related to runoff connectivity and efficiency of vegetated buffer strips at hillslope scale. Results show how, once calibrated for the expected range of runoff EC, the proposed device can provide reliable and replicable measurements among different units with an average root mean square error of 3mm. When deployed in the validation test under rainfall simulation with water of high EC (435 µS cm-1)it allowed the determination of the evolution of the change in runoff starting time and the duration of the hydrograph after the end of rainfall in individual points as a function of slope length. In this test the differences in depth among OFD was not significant, since being lower than 4 mm overlaps with the average measurement error among units. This result highlights the need for careful interpretation of the measured depth in relation to the equipment measurement error in spatial variability of shallow flow. Further improvements will concentrate on remote communication for downloading data via a cell phone network, and additional ruggedness and autonomy for long-term deployment in the field under very cloudy conditions., AGL2015-65036-C3-1-R (Spanish Government), Peer reviewed
in paper "Autonomous shallow flow runoff detector for hillslope hydrological studies".-- Datos de calibración y validación de detectores de escorrentía presentados en el artículo "Autonomous shallow flow runoff detector for hillslope hydrological studies"., This is the underlaying data for the manuscript which describes the development, calibration and validation of an autonomous overland flow detector (OFD) for the measurement and recording of shallow runoff depth at varying recording intervals based on measurement of runoff water electrical conductivity (EC). Using electronic components easily available and of moderate cost, approximately367€ per unit, the proposed device can operate for a broad range of surface overland flow with EC from 0 to 435 µS cm-1 with a regular charge using a small built-in cell panel. It was originally intended for use in experiments related to runoff connectivity and efficiency of vegetated buffer strips at hillslope scale. Results show how, once calibrated for the expected range of runoff EC, the proposed device can provide reliable and replicable measurements among different units with an average root mean square error of 3mm. When deployed in the validation test under rainfall simulation with water of high EC (435 µS cm-1)it allowed the determination of the evolution of the change in runoff starting time and the duration of the hydrograph after the end of rainfall in individual points as a function of slope length. In this test the differences in depth among OFD was not significant, since being lower than 4 mm overlaps with the average measurement error among units. This result highlights the need for careful interpretation of the measured depth in relation to the equipment measurement error in spatial variability of shallow flow. Further improvements will concentrate on remote communication for downloading data via a cell phone network, and additional ruggedness and autonomy for long-term deployment in the field under very cloudy conditions., AGL2015-65036-C3-1-R (Spanish Government), Peer reviewed