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A groyne (in the U.S. groin) is a rigid hydraulic structure built perpendicularly from an ocean shore (in coastal engineering) or a river bank, interrupting water flow and limiting the movement of sediment. It is usually made out of wood, concrete, or stone. In the ocean, groynes create beaches, prevent
beach erosion Coastal erosion is the loss or displacement of land, or the long-term removal of sediment and rocks along the coastline due to the action of waves, currents, tides, wind-driven water, waterborne ice, or other impacts of storms. The landward ...
caused by
longshore drift Longshore drift from longshore current is a geological process that consists of the transportation of sediments (clay, silt, pebbles, sand, shingle) along a coast parallel to the shoreline, which is dependent on the angle incoming wave direction ...
where this is the dominant process and facilitate beach nourishment. There is also often cross-shore movement which if longer than the groyne will limit its effectiveness. In a river, groynes slow down the process of erosion and prevent ice-jamming, which in turn aids navigation. Groynes run generally perpendicular to the shore, extending from the upper foreshore or beach into the water. All of a groyne may be underwater, in which case it is a ''submerged groyne''. They are often used in tandem with seawalls and other coastal engineering features. Groynes, however, may cause a shoreline to be perceived as unnatural. Groynes are generally straight but could be of various plan view shapes, permeable or impermeable, built from various materials such as wood, sand, stone rubble, or gabion, etc.


Background


Etymology

The term ''groyne'' is derived from the Old French , from Late Latin , "
snout A snout is the protruding portion of an animal's face, consisting of its nose, mouth, and jaw. In many animals, the structure is called a muzzle, rostrum, or proboscis. The wet furless surface around the nostrils of the nose of many mammals is c ...
".


History

One of the earliest mentions of groynes is in connection with the planned improvements to the silted-up Dover harbour, by one Fernando Poyntz in 1582. In 1713 the first wooden groyne to protect
Brighton Brighton () is a seaside resort and one of the two main areas of the City of Brighton and Hove in the county of East Sussex, England. It is located south of London. Archaeological evidence of settlement in the area dates back to the Bronze A ...
's seafront and coastline was built, which had been heavily damaged in the Great storm of 1703, and again in 1705. In 1867, the first concrete groyne was built near East Street, Brighton as a 60 m promenade.


Mechanics


Beach evolution and sedimentation accretion

A groyne gradually creates and maintains a wide area of beach on its updrift side by trapping the sediments suspended in the ocean current. This process is called accretion of sand and gravel or beach evolution. It reduces erosion on the other, i.e. downdrift, side by reducing the speed and power of the waves striking the shore. It is a physical barrier to stop
sediment transport Sediment transport is the movement of solid particles (sediment), typically due to a combination of gravity acting on the sediment, and/or the movement of the fluid in which the sediment is entrained. Sediment transport occurs in natural system ...
in the direction of
longshore drift Longshore drift from longshore current is a geological process that consists of the transportation of sediments (clay, silt, pebbles, sand, shingle) along a coast parallel to the shoreline, which is dependent on the angle incoming wave direction ...
(also called longshore transport). If a groyne is correctly designed, then the amount of material it can hold will be limited, and excess sediment will be free to move on through the system. However, if a groyne is too large it may trap too much sediment, which can cause severe beach erosion on the down-drift side.


Groyne fields

Groynes are generally placed in series, generally all perpendicular to the shore. The areas between groups of groynes are groyne fields.


Terminal groyne syndrome

A poorly designed groyne (too long and not suited to the unique features of the coast) can also accelerate the erosion of the downdrift beach, which receives little or no sand from longshore drift. This process is known as terminal groyne syndrome, because in a series of groynes it occurs after the terminal groyne (last groyne on the downdrift side of the beach or coastline).


Headland groyne / Headland breakwater

A ''
breakwater Breakwater may refer to: * Breakwater (structure), a structure for protecting a beach or harbour Places * Breakwater, Victoria, a suburb of Geelong, Victoria, Australia * Breakwater Island Breakwater Island () is a small island in the Palme ...
'' is an artificial offshore structure built parallel to the shore -- similar to naturally formed barrier islands -- that normally remains unattached to the shore. When a groyne is built to attach the breakwater to the shore, it is called a "
headland A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John ...
groyne", also known as "bulkhead groyne", "headland breakwater", "T-head groyne", or "T-shaped groyne".


Usage


Coastal management

A groyne's length and elevation, and the spacing between groynes is determined according to local wave energy and beach slope. Groynes that are too long or too high tend to accelerate downdrift erosion, and are ineffective because they trap too much sediment. Groynes that are too short, too low, or too permeable are ineffective because they trap too little sediment. If a groyne does not extend far enough landward, water (for example at a high tide combined with a storm surge) may flow past the landward end and erode a channel bypassing the groyne, a process known as ''flanking''.


River management

River groynes (spur dykes, wing dykes, or wing dams) are often constructed nearly perpendicular to the riverbanks, beginning at a riverbank with a root and ending at the regulation line with a head. They maintain a channel to prevent ice jamming, and more generally improve navigation and control over lateral erosion, that would form from meanders. Groynes have a major impact on the river morphology: they cause autonomous degradation of the river. They are also used around bridges to prevent bridge scour. Groynes can be distinguished by how they are constructed, whether they are submerged, their effect on stream flow or by shape.Przedwojski ''et al.'' (1995)


By their planview shape

Groynes can be built with different planview shapes. Some examples include straight groynes, hockey stick or curved, inverted hockey stick groynes, tail or checkmark shaped groynes, L head, straight groynes with pier head (seaward end raised on the stilts, since the pier head is raised on the stilts it does not act as the breakwater), T-head ( headland groyne, breakwater attached to the shore with straight groyne, the head/breakwater itself could be shaped straight, Y-shaped, arrow or wing shaped head).


By cross-section based on material used

Wooden groynes, sheetpile groynes, sandbag groynes, rubble mound or gabion groynes, etc.


By permeability

Groynes can be permeable, allowing the water to flow through at reduced velocities, or impermeable, blocking and deflecting the current. * Permeable groynes are large rocks, bamboo or timber * impermeable groynes (solid groynes or rock armour groynes) are constructed using rock, gravel, gabions.


By whether they are submerged

Groynes can be submerged or not under normal conditions. Usually impermeable groynes are non-submerged, since flow over the top of solid groynes may cause severe erosion along the shanks. Submerged groynes, on the other hand, may be permeable depending on the degree of flow disturbance needed.


By their effect on stream flow

Groynes can be attracting, deflecting or repelling. * Attracting groynes point downstream, serving to attract the stream flow toward themselves and not repel the flow toward the opposite bank. They tend to maintain deep current close to the bank. * Deflecting groynes change the direction of flow without repelling it. They are generally short and used for limited, local protection. * Repelling groynes point upstream; they force the flow away from themselves. A single groyne may have one section, for example, attracting, and another section deflecting.


Gallery

File:Duisburg, Mündelheim, Rheinbogen, 2020-04 CN-02.jpg, Groynes on the Rhine, Germany File:GROYNES in the Dutch Rhine.jpg, Groynes in the Waal, part of the Rhine in the Netherlands File:Beach with groynes.JPG, Groyne on the east coast of England File:Cresbeach-groyne.jpg, Groyne in Crescent Beach, British Columbia, Canada File:Ennore Expressway gyrones.JPG, Groynes off the Ennore Expressway near Chennai, India File:Ostrogi Wisła Warszawa 001.jpg, Groynes on the Vistula, Warsaw, Poland File:Estuary in Pozhikara, Paravur.jpg, Groynes on the Arabian Sea at Pozhikara on the Malabar Coast of India File:2017 Sarasota Cortez Beach Sea Wall Groyne at Sunset 1 FRD 7204.jpg, A groyne at Cortez Beach on Anna Maria Island, Florida at sunset File:Silver_Beach_Sydney.jpg, Groyne at Silver Beach, Sydney, Australia File:Otago Harbour entrance, Otago, New Zealand, 12th. Dec. 2010 - Flickr - PhillipC.jpg, A 1200-metre-long mole at Aramoana (centre left of image), protects the mouth of New Zealand's Otago Harbour


See also

* Similar **
Training (civil) Training or entrance training refers to coastal structures built to constrain a river discharging across a littoral coast so that it discharges only where desired. Untrained entrances on sandy coasts tend to move widely and violently to discharge i ...
**
Breakwater Breakwater may refer to: * Breakwater (structure), a structure for protecting a beach or harbour Places * Breakwater, Victoria, a suburb of Geelong, Victoria, Australia * Breakwater Island Breakwater Island () is a small island in the Palme ...
** Drop structure ** Jetty * Beach erosion and accretion ** Beach nourishment ** Modern recession of beaches ** Raised beach **
Strand plain A strand plain or strandplain is a broad belt of sand along a shoreline with a surface exhibiting well-defined parallel or semi-parallel sand ridges separated by shallow swales. A strand plain differs from a barrier island in that it lacks eit ...
*
Integrated coastal zone management Integrated coastal zone management (ICZM), integrated coastal management (ICM), or integrated coastal planning is a coastal management process for the management of the coast using an integrated approach, regarding all aspects of the coastal zone ...
** Coastal management, to prevent coastal erosion and creation of beach **
Coastal and oceanic landforms The coast, also known as the coastline or seashore, is defined as the area where land meets the ocean, or as a line that forms the boundary between the land and the coastline. The Earth has around of coastline. Coasts are important zones in n ...
** Coastal development hazards ** Coastal erosion **
Coastal geography Coastal geography is the study of the constantly changing region between the ocean and the land, incorporating both the physical geography (i.e. coastal geomorphology, climatology and oceanography) and the human geography (sociology and history) ...
** Coastal engineering ** Coastal morphodynamics **
Coastal and Estuarine Research Federation The Coastal and Estuarine Research Federation (CERF) is a private, nonprofit organization that was created in 1971. At that time, the members of two regionally based organizations, the Atlantic Estuarine Research Society (AERS) and the New England ...
(CERF) * Erosion **
Bioerosion Bioerosion describes the breakdown of hard ocean substrates – and less often terrestrial substrates – by living organisms. Marine bioerosion can be caused by mollusks, polychaete worms, phoronids, sponges, crustaceans, echinoids, and ...
**
Blowhole Blowhole may refer to: * Blowhole (anatomy), the hole at the top of a whale's or other cetacean's head *Blowhole (geology), a hole at the inland end of a sea cave **Kiama Blowhole in Kiama, Australia **The Blow Hole, a marine passage between Minst ...
** Natural arch ** Wave-cut platform *
Longshore drift Longshore drift from longshore current is a geological process that consists of the transportation of sediments (clay, silt, pebbles, sand, shingle) along a coast parallel to the shoreline, which is dependent on the angle incoming wave direction ...
** Deposition (sediment) ** Coastal sediment supply ** Sand dune stabilization ** Submersion


References


Notes

* Construction Industry Research and Information Association (1990) ''Groynes in coastal engineering : data on performance of existing groyne systems'', CIRIA technical note 135, London : CIRIA, * Crossman, M. and Simm, J. (2004)
Manual on the use of timber in coastal and river engineering
', HR Wallingford, London : Thomas Telford, * French, P.W. (2001) ''Coastal defences : processes, problems and solutions'', London : Routledge, * Hoyle, J.W. and King, J.T. (1971) ''The principles of coast protection'', Lyndhurst : the authors, * Przedwojski, B., Błażejewski, R and Pilarczyk, K.W. (1995) ''River training techniques : fundamentals, design and applications'', Rotterdam : Balkema, * Walker, D.J. (1987) ''Nearshore hydrodynamics and the behaviour of groynes on sandy beaches'', PhD thesis, Imperial College London, 277 p. * Also published in the ''Delft Hydraulics Select Series'' (No. 7/2005).


External links


Groynes in the Netherlands
*
Coastal Wiki portal
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