Groundwater station - Ravine Quiock
Water-table level and groundwater temperature measured as a function of time (GMT) in a series of piezometric wells, dug in the Quiock creek catchment. Seven of these wells, denoted from A to G, form a linear array that extends over 30 m, perpendicularly to the Quiock stream, which drains the catchment. Two other boreholes, B_downstream et B_upstream, measure the water table level near the borehole B, but to different depths. All groundwater levels are measured with respect to the elevation of the stream bed. The distance from the wells to the stream are (in meters) : xA=1.13, xB=2.43, xBdownstream=2.65, xBupstream=2.56, xC=4.38, xD=10.04, xE=12.96, xF=21.24, and xG=29.21. Their depth relative to the stream bed are (in meters): zA = -2.1, zB=-2.4, zBdownstream=-4, zBupstream=-5.85, zC=-3.1, zD=-5.03, zE=-4.05, zF=-4.4, and zG=-4.5.
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- Link to Original Record [in-situ.theia-land.fr] This metadata comes from in-situ.theia-land.fr