During the period 1975-1979, 45 of these centrifugal tests were undertaken for Rijkswaterstaat, most of which were for the parametric studies for the piers of the Oosterschelde barrier. Predictions were also made regarding the outcome of physical tests on a scale of 1:10 at Kats. One of the other forms of research is the physical model-test. By this means, the shear stress on the horizontal displacement of the piers was investigated in a physical model at Schelphoek. The friction co-efficient proved to be 0.67, whereas 0.3 would have been sufficient. Waves at the mouth of the Oosterschelde The waves along the Dutch coast are mostly caused by winds on the North Sea or on the Norwegian Sea. The height of the waves is strongly influenced by the direction of the wind: coming from the North the wind-shear can affect the waves over a distance of 2,500 km. The higher the water-levels, the higher the waves that are generated. The coastal area, however, acts as a filter, limiting the wave-heights and causing small changes in the wave-direction. On the other hand, the local wind will add energy to the wave-pattern. The factors concerned and the relations between them are being studied in the mathematical FILTER model. The prediction of the waves forms an essential part of the boundary conditions set for the Oosterschelde barrier. Drainage of the construction-pit for the 'Krammer' locks When a structure is built in a construction-pit, which is itself surrounded by water, it has to be pumped dry and kept dry. To this end a pumping-station must be installed and kept working during the entire operation. In addition, other drainage equipment must be available when, in the initial stages, the construction-pit is still completely full of water. In advance, instructions for the pumping procedures and an estimate of the costs will be prepared. The construction-pit for the push-tow locks in the Philips Dam has been equipped with more than the normal number of level gauges and discharge meters in order to study in general the peculiarities of a pumping operation. The location on the Plaat van de Vliet displays a peculiar soil mechanical phenomenon: there are two layers of water-bearing soil sandwiching an almost impermeable layer. Sand piles had to be driven through the intermediate layer because only the lowest layer was drained. 40 percent of the water that was drained was done by filter-pumping and the remaining 60 percent by the normal de-watering process. Improvement of the Kanaal door Zuid-Beveland The Canal through South-Beveland will be improved, in conjunction with the other hydraulic engineering works in the Oosterschelde. The sluice on the northern side near Wemeldinge will no longer be used, thus enabling the reduced tidal action to penetrate the Canal. The shipping route will be made suitable for a train of four push-tow barges. As a consequence and also because of the tidal action, the Canal will have to be widened and deepened. The dikes along the Canal will be raised. The southern sluice, near Hansweert, will be rebuilt completely at a different location and be of the same dimensions as the sluices in the Krammer and the Philips dam; the height of the dam walls will be in accordance with the stipulations laid down in the Delta Law. A scouring test near the discharge-sluice in the Brouwers-dam Up till now, for the solution of problems regarding scourings near structures, one has depended entirely on hydraulic model tests. Not only the fact that the translation of a test into the actual situation offers some uncertainty, also the fact that the data used in model tests are only abstracted from the actual situation causes uncertainty about the question of the intrinsic value of the test. Recently a physical scouring test has been performed on the inside of the discharge-sluice in the Brouwersdam, i.e. a test on the scale of 1:1, which was later repeated in the model. In fact, the physical test was divided into two parts i.e. a test with the natural bed-soil, followed by a test performed with artificial homogenous sediment. Only the results of the first test and of the model are discussed here. The outcome is not unfavourable for the model. 403

Tijdschriftenbank Zeeland

Driemaandelijks bericht Deltawerken | 1981 | | pagina 53