Titlebook: Rational Transmitting Boundaries for Time-Domain Analysis of Dam-Reservoir Interaction; Benedikt Weber Book 1994 Springer Basel AG 1994 ea

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Time-Domain Implementation, repeating the essential equations from previous chapters. In the last part, several examples are given ranging from simple two-dimensional geometries to three-dimensional arch dam models. The results are compared to analytical results and to results from the literature to confirm the accuracy and efficiency of the procedure.

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Book 1994n examples of arch dams which have been seriously damaged by earthquakes, the need for more realistic seismic analyses is now well recognized, not only for new dams but especially in the context of the safety evaluation of existing dams. Fortunately, with the finite element method, engineers have a

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Introduction,t for the analysis reasonable, only the . consisting of the structure and a small portion of the surrounding media can be modeled directly while the rest, the ., has to be captured by an appropriate boundary condition at the .. The setup for a dam-reservoir problem is schematically shown in Figure 1.1

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Model Problems,ple as possible but general enough to allow a conclusive discussion. In the following chapters they will be used to investigate some commonly used numerical solutions and some new methods which are the main contribution of this work. A similar collection of example problems for wave propagation can be found in [Gra75].

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Scalar Systems, Signal Processing,elationship described by a differential or difference equation, an impulse response function or a transfer function. The internal structure is usually of minor interest and has generally no physical significance but general attributes such as stability, and minimal realization have to be investigated.

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Renedikt Webern. Im Erdmittelpunkt herrscht eine Temperatur von ca 6.000 °C. Durch W?rmeleitung, W?rme aus radioaktiven Zerf?llen und durch hei?e magmatische Gebiete wird in der Erdkruste ein Temperaturgradient erzeugt, der an der Erdoberfl?che 3 °C pro 100 m ausmacht (die normale geothermische Tiefenstufe wird m

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