Hydroelastic interaction between ocean waves and large floating structures in the inhomogeneous ocean environment : Υδροελαστική αλληλεπίδραση θαλάσσιων κυματισμών με μεγάλες πλωτές κατασκευές σε ανομοιογενές περιβάλλον

Interaction of waves with Very Large Floating Structures (VLFS) and sea ice formations present similarities permitting a common mathematical treatment and numerical modelling. Wave-induced structural response and its underlying effect on the hydrodynamic field are fundamental to the in-depth underst...

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Main Author: Karperaki, Angeliki
Format: Article in Journal/Newspaper
Language:unknown
Published: National Technological University of Athens 2021
Subjects:
Online Access:https://dx.doi.org/10.26240/heal.ntua.20888
https://dspace.lib.ntua.gr/xmlui/handle/123456789/53190
id ftdatacite:10.26240/heal.ntua.20888
record_format openpolar
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Υδροελαστικότητα
Μεγάλες πλωτές κατασκευές
Μέθοδος πεπερασμένων στοιχείων
Σύστημα συζευγμένων ιδιομορφών
Μείωση διάστασης
Hydroelasticity
Large floating structures
Finite element method
Coupled mode system
Dimensionality reduction
spellingShingle Υδροελαστικότητα
Μεγάλες πλωτές κατασκευές
Μέθοδος πεπερασμένων στοιχείων
Σύστημα συζευγμένων ιδιομορφών
Μείωση διάστασης
Hydroelasticity
Large floating structures
Finite element method
Coupled mode system
Dimensionality reduction
Karperaki, Angeliki
Hydroelastic interaction between ocean waves and large floating structures in the inhomogeneous ocean environment : Υδροελαστική αλληλεπίδραση θαλάσσιων κυματισμών με μεγάλες πλωτές κατασκευές σε ανομοιογενές περιβάλλον
topic_facet Υδροελαστικότητα
Μεγάλες πλωτές κατασκευές
Μέθοδος πεπερασμένων στοιχείων
Σύστημα συζευγμένων ιδιομορφών
Μείωση διάστασης
Hydroelasticity
Large floating structures
Finite element method
Coupled mode system
Dimensionality reduction
description Interaction of waves with Very Large Floating Structures (VLFS) and sea ice formations present similarities permitting a common mathematical treatment and numerical modelling. Wave-induced structural response and its underlying effect on the hydrodynamic field are fundamental to the in-depth understanding of physical processes like ice shelf calving as well as the design of marine structures operating nearshore. The common features of the aforementioned systems are: (a) their low bending rigidity, (b) their inherently complex geometries and material inhomogeneity and (c) their extent over large horizontal domains, dictating the need to address the effects of bathymetric variations. The common ground allows for the development of joint computational tools for the treatment of the above coupled wave-structure-seabed interaction problems. Intricacies lay on the very same features, namely the large horizontal domains along with geometric and material inhomogeneity. In this work a novel methodology is proposed based on finite elements, in conjunction with coupled-mode system formulation, which is derived by appropriate local-mode representations of the vertical structure of the wave field. Confined in the linear regime, potential theory is employed. The floating body is assumed to be thin in the vertical direction within the limits of reduced elastic plate models. Depending on the structure slenderness and the excitation wavelength-to-plate thickness ratio, the structure is modelled using either Classical Thin or Reissner-Mindlin Plate theory to account for first order shear deformation effects. The wave field is decomposed in the propagating component over the variable bathymetry (in the absense of the body) and the diffraction and radiation parts both due to the rigid motions and the elastic plate deflection. An in vacuo modal expansion for the plate deflection is employed to partially decouple the hydrodynamics from structural mechanics. The employed decomposition allows for the formulation of a propagating wave field and a series of radiation-type sub-problems, formulated by following a domain decomposition approach using different vertical local-mode expansions enabling the consistent satisfaction of the boundary conditions on the free-surface and elastic body subdomains. The formulation is supplemented by introducing matching conditions on the interfaces separating the above subdomains. A weighted residual approach is employed to derive a permissive form of the latter facilitating a FEM-based scheme. To this end, radiation-type problems are re-cast into a mixed weak form by means of Lagrange multipliers defined on the interface between the plate-covered and the free surface regions, aiming at the weak satisfaction of the essential continuity requirement across the transmission interface. This approach circumvents the complexity of constructing appropriate finite element subspaces that would ab initio satisfy the Dirichlet type constraint. Subsequently, the dimensionality reduction of the problems at hand is achieved by the introduction of suitable local-mode vertical representations for the velocity potential in each sub-region, ultimately yielding the variational form of coupled-mode systems on the horizontal plane. The reduced weak forms allow the development of a FEM scheme that employs conventional Lagrange elements, capable of h-p refinement. Finally, the numerical tool incorporates a Perfectly Matched Layer, featuring an unbounded absorbing function, for the numerical domain truncation. Numerical results for a number of configurations are presented in both the 2D and 3D examples. Extensive comparisons are presented against results and data from the literature illustrating the accuracy of the method and showcasing its capabilities in modelling inhomogeneity.
format Article in Journal/Newspaper
author Karperaki, Angeliki
author_facet Karperaki, Angeliki
author_sort Karperaki, Angeliki
title Hydroelastic interaction between ocean waves and large floating structures in the inhomogeneous ocean environment : Υδροελαστική αλληλεπίδραση θαλάσσιων κυματισμών με μεγάλες πλωτές κατασκευές σε ανομοιογενές περιβάλλον
title_short Hydroelastic interaction between ocean waves and large floating structures in the inhomogeneous ocean environment : Υδροελαστική αλληλεπίδραση θαλάσσιων κυματισμών με μεγάλες πλωτές κατασκευές σε ανομοιογενές περιβάλλον
title_full Hydroelastic interaction between ocean waves and large floating structures in the inhomogeneous ocean environment : Υδροελαστική αλληλεπίδραση θαλάσσιων κυματισμών με μεγάλες πλωτές κατασκευές σε ανομοιογενές περιβάλλον
title_fullStr Hydroelastic interaction between ocean waves and large floating structures in the inhomogeneous ocean environment : Υδροελαστική αλληλεπίδραση θαλάσσιων κυματισμών με μεγάλες πλωτές κατασκευές σε ανομοιογενές περιβάλλον
title_full_unstemmed Hydroelastic interaction between ocean waves and large floating structures in the inhomogeneous ocean environment : Υδροελαστική αλληλεπίδραση θαλάσσιων κυματισμών με μεγάλες πλωτές κατασκευές σε ανομοιογενές περιβάλλον
title_sort hydroelastic interaction between ocean waves and large floating structures in the inhomogeneous ocean environment : υδροελαστική αλληλεπίδραση θαλάσσιων κυματισμών με μεγάλες πλωτές κατασκευές σε ανομοιογενές περιβάλλον
publisher National Technological University of Athens
publishDate 2021
url https://dx.doi.org/10.26240/heal.ntua.20888
https://dspace.lib.ntua.gr/xmlui/handle/123456789/53190
long_lat ENVELOPE(-62.597,-62.597,-64.529,-64.529)
geographic Lagrange
geographic_facet Lagrange
genre Ice Shelf
Sea ice
genre_facet Ice Shelf
Sea ice
op_rights Αναφορά Δημιουργού - Μη Εμπορική Χρήση - Παρόμοια Διανομή 3.0 Ελλάδα
http://creativecommons.org/licenses/by-nc-sa/3.0/gr/
op_rightsnorm CC-BY-NC-SA
op_doi https://doi.org/10.26240/heal.ntua.20888
_version_ 1766032404632305664
spelling ftdatacite:10.26240/heal.ntua.20888 2023-05-15T16:41:56+02:00 Hydroelastic interaction between ocean waves and large floating structures in the inhomogeneous ocean environment : Υδροελαστική αλληλεπίδραση θαλάσσιων κυματισμών με μεγάλες πλωτές κατασκευές σε ανομοιογενές περιβάλλον Karperaki, Angeliki 2021 https://dx.doi.org/10.26240/heal.ntua.20888 https://dspace.lib.ntua.gr/xmlui/handle/123456789/53190 unknown National Technological University of Athens Αναφορά Δημιουργού - Μη Εμπορική Χρήση - Παρόμοια Διανομή 3.0 Ελλάδα http://creativecommons.org/licenses/by-nc-sa/3.0/gr/ CC-BY-NC-SA Υδροελαστικότητα Μεγάλες πλωτές κατασκευές Μέθοδος πεπερασμένων στοιχείων Σύστημα συζευγμένων ιδιομορφών Μείωση διάστασης Hydroelasticity Large floating structures Finite element method Coupled mode system Dimensionality reduction CreativeWork article 2021 ftdatacite https://doi.org/10.26240/heal.ntua.20888 2021-11-05T12:55:41Z Interaction of waves with Very Large Floating Structures (VLFS) and sea ice formations present similarities permitting a common mathematical treatment and numerical modelling. Wave-induced structural response and its underlying effect on the hydrodynamic field are fundamental to the in-depth understanding of physical processes like ice shelf calving as well as the design of marine structures operating nearshore. The common features of the aforementioned systems are: (a) their low bending rigidity, (b) their inherently complex geometries and material inhomogeneity and (c) their extent over large horizontal domains, dictating the need to address the effects of bathymetric variations. The common ground allows for the development of joint computational tools for the treatment of the above coupled wave-structure-seabed interaction problems. Intricacies lay on the very same features, namely the large horizontal domains along with geometric and material inhomogeneity. In this work a novel methodology is proposed based on finite elements, in conjunction with coupled-mode system formulation, which is derived by appropriate local-mode representations of the vertical structure of the wave field. Confined in the linear regime, potential theory is employed. The floating body is assumed to be thin in the vertical direction within the limits of reduced elastic plate models. Depending on the structure slenderness and the excitation wavelength-to-plate thickness ratio, the structure is modelled using either Classical Thin or Reissner-Mindlin Plate theory to account for first order shear deformation effects. The wave field is decomposed in the propagating component over the variable bathymetry (in the absense of the body) and the diffraction and radiation parts both due to the rigid motions and the elastic plate deflection. An in vacuo modal expansion for the plate deflection is employed to partially decouple the hydrodynamics from structural mechanics. The employed decomposition allows for the formulation of a propagating wave field and a series of radiation-type sub-problems, formulated by following a domain decomposition approach using different vertical local-mode expansions enabling the consistent satisfaction of the boundary conditions on the free-surface and elastic body subdomains. The formulation is supplemented by introducing matching conditions on the interfaces separating the above subdomains. A weighted residual approach is employed to derive a permissive form of the latter facilitating a FEM-based scheme. To this end, radiation-type problems are re-cast into a mixed weak form by means of Lagrange multipliers defined on the interface between the plate-covered and the free surface regions, aiming at the weak satisfaction of the essential continuity requirement across the transmission interface. This approach circumvents the complexity of constructing appropriate finite element subspaces that would ab initio satisfy the Dirichlet type constraint. Subsequently, the dimensionality reduction of the problems at hand is achieved by the introduction of suitable local-mode vertical representations for the velocity potential in each sub-region, ultimately yielding the variational form of coupled-mode systems on the horizontal plane. The reduced weak forms allow the development of a FEM scheme that employs conventional Lagrange elements, capable of h-p refinement. Finally, the numerical tool incorporates a Perfectly Matched Layer, featuring an unbounded absorbing function, for the numerical domain truncation. Numerical results for a number of configurations are presented in both the 2D and 3D examples. Extensive comparisons are presented against results and data from the literature illustrating the accuracy of the method and showcasing its capabilities in modelling inhomogeneity. Article in Journal/Newspaper Ice Shelf Sea ice DataCite Metadata Store (German National Library of Science and Technology) Lagrange ENVELOPE(-62.597,-62.597,-64.529,-64.529)