Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Interaction of surface gravity waves with vertical permeable breakwaters

View through CrossRef
The protection of the coastline, objects of vital activity, hydrotechnical structures, marine flora and fauna require constant modernization of coastal protection structures, which is due to climate changes and an increase in wave energy of the sea. In recent years, in the development of coastal protection structures, a trend has emerged to use permeable structures, the advantage of which is to improve the ecology of the protected water area, saving construction materials. The article presents the results of experimental researches on the study of the characteristics of the interaction of surface gravity waves with coastal defense structures in the form of permeable vertical breakwaters. The research was conducted in laboratory conditions on models of single-row penetrating breakwaters, which were located in a wave tray. Visual studies were conducted to record the interaction of wave motion with breakwater models, and instrumental studies of the wave field were also conducted. Parameters of wave movement were recorded by specially developed wave height sensors, which were made on the basis of piezoresistive pressure sensitive elements. Photos and video footage allowed us to evaluate the features of the interaction of the wave field with the studied models of permeable breakwaters. Permeable breakwaters of different permeability were used in the experiments. In addition, the vertical permeable breakwaters were closed by impermeable shields at the top of the breakwaters in the area of the water cut. At the same time, impermeable shields were installed at different depths relative to the water level. Hydrodynamic parameters of the wave field in the vicinity of permeable breakwaters (wave heights, periods and lengths, reflection and transformation coefficients, dissipation coefficient of the wave energy) were measured by a group of wave height sensors, which were located in different places in front of the breakwater models, as well as behind them. Integral and spectral characteristics of the wave field were obtained, the dependences of changes in the hydrodynamic parameters of the wave field were determined, depending on the permeability of the breakwater, the relative depth of the water in the wave tray, and the length of the gravitational wave. The degree of protection of the coastline by permeable vertical breakwaters was determined and the maximum values of wave energy dissipation were obtained depending on the shape, size and permeability of the studied models of vertical single-row breakwaters.
Title: Interaction of surface gravity waves with vertical permeable breakwaters
Description:
The protection of the coastline, objects of vital activity, hydrotechnical structures, marine flora and fauna require constant modernization of coastal protection structures, which is due to climate changes and an increase in wave energy of the sea.
In recent years, in the development of coastal protection structures, a trend has emerged to use permeable structures, the advantage of which is to improve the ecology of the protected water area, saving construction materials.
The article presents the results of experimental researches on the study of the characteristics of the interaction of surface gravity waves with coastal defense structures in the form of permeable vertical breakwaters.
The research was conducted in laboratory conditions on models of single-row penetrating breakwaters, which were located in a wave tray.
Visual studies were conducted to record the interaction of wave motion with breakwater models, and instrumental studies of the wave field were also conducted.
Parameters of wave movement were recorded by specially developed wave height sensors, which were made on the basis of piezoresistive pressure sensitive elements.
Photos and video footage allowed us to evaluate the features of the interaction of the wave field with the studied models of permeable breakwaters.
Permeable breakwaters of different permeability were used in the experiments.
In addition, the vertical permeable breakwaters were closed by impermeable shields at the top of the breakwaters in the area of the water cut.
At the same time, impermeable shields were installed at different depths relative to the water level.
Hydrodynamic parameters of the wave field in the vicinity of permeable breakwaters (wave heights, periods and lengths, reflection and transformation coefficients, dissipation coefficient of the wave energy) were measured by a group of wave height sensors, which were located in different places in front of the breakwater models, as well as behind them.
Integral and spectral characteristics of the wave field were obtained, the dependences of changes in the hydrodynamic parameters of the wave field were determined, depending on the permeability of the breakwater, the relative depth of the water in the wave tray, and the length of the gravitational wave.
The degree of protection of the coastline by permeable vertical breakwaters was determined and the maximum values of wave energy dissipation were obtained depending on the shape, size and permeability of the studied models of vertical single-row breakwaters.

Related Results

Gravity data reduction, Bouguer anomaly, and gravity disturbance
Gravity data reduction, Bouguer anomaly, and gravity disturbance
Each point on the earth has a gravity and gravity potential value. Surfaces formed by connecting points with equal gravity potential values are called equipotential surfaces or lev...
Interaction of gravitational waves with permeable breakwater
Interaction of gravitational waves with permeable breakwater
A method for calculating the parameters of gravitational waves that interact with vertical permeable breakwaters, based on potential theory, has been developed and presented. The w...
Transformation of wave field by permeable vertical wall
Transformation of wave field by permeable vertical wall
Laboratory experimental studies were conducted to study the interaction of gravity waves with models of permeable vertical walls, which are formed by piles of circular cross-sectio...
Using spherical scaling functions in scalar and vector airborne gravimetry
Using spherical scaling functions in scalar and vector airborne gravimetry
<p>Airborne gravimetry is capable to provide Earth’s gravity data of high accuracy and spatial resolution for any area of interest, in particular for ha...
Exploring the Venusian Clouds: Dayside Atmospheric Gravity Waves with Akatsuki UVI instrument
Exploring the Venusian Clouds: Dayside Atmospheric Gravity Waves with Akatsuki UVI instrument
As our neighbouring world, Venus stands as a pivotal planet in the study of planetary evolution. Its dense atmosphere, mostly composed of carbon dioxide makes it a unique laborator...
Planetary wave‐gravity wave interactions during mesospheric inversion layer events
Planetary wave‐gravity wave interactions during mesospheric inversion layer events
AbstractRayleigh lidar temperature observations over Gadanki (13.5°N, 79.2°E) show a few mesospheric inversion layer (MIL) events during 20–25 January 2007. The zonal mean removed ...
Sinking or bouncing in low gravity environments?
Sinking or bouncing in low gravity environments?
Understanding the physics of granular materials in a low gravity and vacuum environment is essential to predict the regolith behavior on the Moon and asteroids. Cohesive forces - i...

Back to Top