Techniques de l’eau et calcul des réseaux
description
Transcript of Techniques de l’eau et calcul des réseaux
Velocity determination: Float Method
Inexpensive and simple
Measures surface velocity
Mean velocity obtained using a correction factor
Basic idea: measure the time that it takes an object to float a specified distance downstream
The electromagnetic sensors use the Faraday Principle to measure the water speed.
As a conductor (water) moves through an electromagnetic field (produced by the sensor),
it generates a voltage that is measured by the sensor electrodes.
ou GPRS
Etablissement des relations de tarage hauteurs-débits
Rating curve hysteresis loop in Zenne river (Lot), 15-16 July 2012 event: blue triangles – rising stage, green squares – falling stage
1 Membrane (formant diaphragme)2 Brasage en verre (matériau agglomérant soudé)3 Corps de base
L'élément de mesure de ce capteur de pression est une cellule céramique capacitive sèche. Le corps de base et la membrane sont en céramique de grande pureté (Al2O3 99.9 % )
Capteur à effet capacitif
-la capacité électrique varie en fonction de la déformation de la membrane -mesure des très faibles pressions -excellent temps de réponse
•12
In the illustrated configuration (rio Parapeti), the immersed pressure transducer is hanged in the internal part of a (perforated) protection tube.
water depth on 11-March-2010
1.06
1.08
1.10
1.12
1.14
1.16
1.18
1.20
1.22
06:00 09:00 12:00 15:00 18:00
Time
Water depth changes in rio Parapeti under constant discharge. Sensor sensitivity is sufficient to follow the progression of a sand dune.
Principe du limnimètre bulle-à-bulle
La chaîne de mesures
Phénomène physique Capteur Conditionneur
Instrument(carte d’acquisition)
Logiciel(ex. Labview)
méthode d’injection de traceur à
débit constant q et
concentration C1
méthode par intégration (injection
instantanée)
Tube de Pitot
Il est constitué de deux tubes coudés concentriques dont les orifices, en communication avec le fluide dont on veut mesurer la vitesse, sont disposés de façon particulière.•L'un, placé orthogonalement, a une vitesse relative v égale à la vitesse du fluide et une pression statique ps égale à la pression ambiante.•L'autre, placé dans le sens de l'écoulement, a une vitesse relative nulle et une pression totale pt, somme de la pression dynamique et de la pression statique.
La différence entre ces pressions donne la vitesse
v = vitessep = pression dans la conduite (ps est la pression
statique, pt est la pression totale)
ρ = masse volumique du fluide
The radar flow-meter is also based on the principle of the frequency shift due to the Doppler
effect. The radar sensor is installed pointing in a defined angle on the water surface. Via the
sending antenna, a constant frequency of 24 GHz is emitted. This signal is partly reflected at the
water surface (minimum 3 mm waves) and returns with a specific frequency shift to the receiving
antenna. With support of spectral analysis, filters and statistical methods, the surface velocity is
obtained. Significant progress has been reached recently in these data processing techniques,
improving the applicability of this non-intrusive measurement method.
The Acoustic Doppler Current Profiler (ADCP) is a kind of sonar: it operates by transmitting acoustic pulses into the water column. These acoustic pulses propagate through the water column and are “reflected” by suspended particles which are carried by water currents. The reflected signals (echoes) are received by the ADCP. Echoes arriving later, from deeper in the water column, are assigned greater depths in the velocity profile. This allows the ADCP to form vertical profiles of current velocity.
Particles within the current flow moving towards the instrument exhibit higher frequencies while those moving away exhibit lower frequencies. This is the well-known Doppler shift, which enables precise measurement of current speed and direction, allowing to reconstitute the full velocity field.
side-looking ADCP
(around 15 kEuros HTVA)