Water table depth - Groundwater - Kamech Site

The water table depth from the soil surface is measured at different points in the Kamech catchment. In Kamech site, the groundwater is shallow with a free surface water table rising and falling in the soil and subsoil layers. The measurements are made at different points in the catchment with piezometers. A piezometer is a perforated PVC tube at its base installed in the soil through a borehole. In every piezometer, the water table depth is measured by manual piezometric probe or monitored at high frequency (~15') with autonomous and automatic probe integrating acquisition units.

revisionJan 20, 2025creationOct 26, 2007publicationDec 9, 2024

Temporal CoverageOct 26, 2007Dec 18, 2024

Overview

Lineage

Dataset acquired during OMERE program.The dataset is broadcasted unmodified to Theia/OZCAR information system

Links

Downloads

• Download this dataset from producer dataportal

Geolinks

• No links available

Others

• Link to Original Record [in-situ.theia-land.fr]
  This metadata comes from in-situ.theia-land.fr
• Theia/OZCAR dataset description

Contacts

OZCAR-RI OMERE

• coordination@obs-omere.org

Observatoire Mediteranéen de l'Environnement Rural et de l'Eau

• coordination@obs-omere.org

Institut de recherche pour le développement

• victoria.agazzi@ird.fr

Keywords

data acquisition

observable property

manual observation

hydrological cycle

Water table depth

FIXED OBSERVATION STATIONS

Environmental monitoring facilities

Sedimentary rocks or undifferentiated facies

Temperate, dry summer, hot summer

CDS THEIA-OZCAR

Constraints

License

Other restrictions

Use limitations

Free use subject to compliance with the OMERE Observatory data use charter available on this form and also digitally signed when downloading data via the OMERE portal.

Other restrictions

no limitations to public access

CC BY 4.0: https://creativecommons.org/licenses

https://www.obs-omere.org/sites/obs-omere.org/files/Charte_OMERE.pdf