By Stella et Jacques Choque
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7) For both experiments the Stokes number is of order O(10−4 ) which means that the particles used indeed perfectly follow the flow. 6). The idea of 3D-PTV was introduced by Chang and Taterson (1983), and was further developed by Racca and Dewey (1988), Maas (1991, 1992a, 1992b, 1993, 1995, 1996) and Malik et al. (1993). The technique has a history of development for more than a decade at the Institute of Geodesy and Photogrammetry (IGP) and at the Institute for Hydromechanics and Water Resources Management (IHW) both at the Swiss Federal Institute (ETH) Zürich.
16: The joint PDFs of ∂u ∂xi versus ∂xj + ∂xk (here no summation over i, j, k) for three cases, 60Hz with full numerical processing, 60Hz, not using the polynomials and 30Hz with full numerical processing. The superior behaviour of the 60Hz experiment with full numerical processing can be seen both in amount of data - as compared to 30Hz - and alignment to the diagonal - as compared to 60Hz, not using the polynomials. have resulted in much too small data sets especially for the 30Hz data and the material volumes.
14 a) that k2 has a range from roughly 4 · 10−5 to 8 · 10−5 m2 /s2 . 5 times less ® likely than the most probable events. For accelerations the situation is quite diﬀerent. 15 b) we see that this mean is governed by extremely rare events which have a probability to occur that is two to three orders of magnitude smaller than the most probable events. In other words, the current 3D-PTV system is able to capture a set of points for long trajectories with only half as many ’strong’ but highly unlikely events as for short trajectories.