Nam Ton Watershed

Knowledge Platform

The water level in the stream is actually a useful parameter to show trends and set up warnings. It is nevertheless necessary to be able to convert the water level to the water flow (in m3/s). This will allow quantifying base flow and run off as part of the hydrological balance. This will be used mainly for evaluate the water available and evaluate flood risks. Actually, a statistical curve H-Q (Water Level versus Flow) must be established in each of the stations where the water level is measured.

To proceed to this measurement, SUMALOM Nam Ton is now equipped with a Doppler Sensor, namely “Qliner” that allows automatic measurement of the stream cross-section and water velocity at different heights of the stream. The integration of the surface by the velocity gives us the flow for the water level observed at the time of the measurement. For very low flows, the traditional flow meter is used. For the time being, the Qliner faced technical problems that needed to be fixed in OTT, Germany. Only low flow could be measured.

Flow Measurement - References