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Tatyana Khabakhpasheva

Researcher at University of East Anglia

Publications -  67
Citations -  747

Tatyana Khabakhpasheva is an academic researcher from University of East Anglia. The author has contributed to research in topics: Hydroelasticity & Deflection (engineering). The author has an hindex of 13, co-authored 60 publications receiving 567 citations. Previous affiliations of Tatyana Khabakhpasheva include Novosibirsk State University & Russian Academy of Sciences.

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Hydroelastic behaviour of compound floating plate in waves

TL;DR: In this article, the authors deal with the plane problem of the hydroelastic behavior of floating plates under the influence of periodic surface water waves, in which the coupled hydrodynamics and structural dynamics problems are solved simultaneously.
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Elastic wedge impact onto a liquid surface: Wagner's solution and approximate models

TL;DR: In this article, the problem of elastic wedge impact onto the free surface of an ideal incompressible liquid of infinite depth is considered, and three approximate models of water impact are examined and their predictions are tested against the present numerical solution obtained by the normal mode method within the Wagner theory.
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Regular wave impact onto an elastic plate

TL;DR: In this paper, a computational analysis of an elastic plate dropped against regular long waves is presented within the linear potential-flow theory and the contributions of kinetic and potential energies to the total energy are analyzed.
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Waves propagating along a channel with ice cover

TL;DR: In this paper, the dispersion relation of one-dimensional hydroelastic waves in an unbounded ice sheet is investigated and the wave profiles across the channel and the distributions of strains in the ice sheet are investigated.
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The response of ice cover to a load moving along a frozen channel

TL;DR: In this paper, the effects of the load speed, width and depth of the channel on the hydroelastic response of the ice cover were studied in detail, and it was shown that the models of ice response without hydrodynamic component of the pressure provided correct stresses in the ice sheet only for very low speeds of the moving load.