Dataset Edition

Présentation générale
Nom du jeu de donnéesCE.Gwat_Odc - Ground water, catena, Oueme meso-site
Créé le2005-12-02
Projet(s)AMMA > AMMA-EOP
Date de début (yyyy-mm-dd)2004-03-21Date de fin (yyyy-mm-dd)2008-09-25
Accès aux données Dataset as provided by the Principal Investigator
Description du jeu de données
RésuméDocumentation of the processes of ground water recharge-discharge. Documentation of the ground-water river connections. Contribution to the water budget at the hillslope scale in relation with soil water, runoff measurements. The identified processes will be used to improve hydrological modelling at the super site scale (Donga).
Strategie d'observationAccording with electrical geophysical surveys, sites of drilling along the hillslope are selected. On each site, multi-level piezometers (<1m, 2m, 10m, 20m depth) are put in. Automatic measurements of water level and electrical conductivity (1 hour) for the most superficial piezometers and manual measurements every two days for the others.
Description de l'instrument
No information available
Information géographique
Site 1
SiteOueme meso-site
Type de plateformeIn Situ Land-based Platforms > GROUND STATIONS
Longitude minimale (°)1.6048Longitude maximale (°)1.6064
Latitude maximale (°)9.7469Latitude minimale (°)9.743
Altitude min427.41Altitude max446.32
Paramètre mesuré
Nom du paramètreWater Table
Mot-clé du paramètreTerrestrial Hydrosphere > Ground Water > Ground Water Features > Water Table
Date de début (yyyy-mm-dd)2004-03-21Date de fin (yyyy-mm-dd)2008-09-25
Précision du capteur / Incertitude
Information sur l'utilisation des données
Conditions d'utilisation des donnéesPermission is granted to use these data in research and publications when accompanied by the following statement: "The AMMA-CATCH regional observing system was set up thanks to an incentive funding of the French Ministry of Research that allowed pooling together various pre-existing small scale observing setups. The continuity and long term perenity of the measurements are made possible by an undisrupted IRD funding since 1990 and by a continuous CNRS-INSU funding since 2005."
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