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Marine construction

Building structures in or adjacent to large bodies of water

  • 16 min read
  • 12 chapters

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Through Concrete, Temperature and Seawater

Environmental influences

Some aspects of the marine environment that complicate construction:

  • Distance from permanent facilities causes logistical problems for provision of materials, equipment, power supplies, and accommodation.
  • Hydrostatic pressure due to depth in the water column. Hydrostatic pressure is linear with depth and increases at approximately 1 bar for every ten metres of depth.
  • Temperature of the water and the air above it. Sea surface temperature can vary from a minimum of −2 °C (28 °F) to a maximum of about 32 °C (90 °F). Higher surface temperatures decrease rapidly with depth, and generally reach a steady-state of about 2 °C (36 °F) by about 1,000 metres (3,300 ft), though on Australia's Northwest Shelf, water and seabed temperature may exceed 30 °C (86 °F) at a depth of 250 metres (820 ft). Air temperatures may vary much more, and though the water has a moderating effect, the air temperature more variable and may be much more extreme.
  • Seawater and splash zone chemistry
  • Biofouling
  • Currents cause drag loading on structures and equipment. There are several different types of currents in the seas. Categorised by their cause, these include geostrophic, tidal, wind-driven, oceanic circulation and density, as well as those caused by river discharge. River currents are driven mainly by gravity, but differ laterally and vertically. The highest velocity in river currents is usually near the outer bank in a bend, and hey also locally increase around obstructions to their flow. Current may also spin off eddies, and their lateral boundaries may vary considerably over the short term. There may also be short or long term vertical components in some areas, the upwellings and downwellings often associated with bottom topography and winds in coastal areas. Currents may be stratified vertically, even to the extent that they may flow in opposing directions at the surface and at the bottom. Their influence on underwater construction is a consequence of the drag forces induced and the transport of unconsolidated sediment, particularly by scour, both during and after construction. Water passing over an immersed surface can also cause lift forces, proportional to the square of the velocity, which can complicate operations, so the variations of instantaneous velocity induced by waves can further complicate matters.
  • Waves are a further environmental influence near the surface, which cause perturbations in all six degrees of freedom on a floating object, and can exert large forces on a fixed object. They are a major cause of delays and reduced operating efficiency, and may be the major design criterion for fixed structures. Tsunamis are a class of wave which occur relatively seldom but can have a devastating effect due to the large amounts of energy they can carry over long distances at high speeds. The depth to which a wave has significant motion is a function of wave length, and to a lesser extent, on wave height.
  • Wind
  • Tides and storm surges
  • Rain, snow and fog reduce visibility, but with radar and precision positioning systems they are not as serious a hazard as in the past. Nevertheless, they may cause delays in some operations. In heavy rainfall appreciable quantities of water may enter unprotected openings, and must be removed before it has adverse effects on stability due to free-surface. Fog may be of the summer fog type which forms some distance above the water and may leave a narrow band of clear air just above the water, or winter type, where there mat be dense fog just above the water but clear skies a short distance up. Rain, fog and snow may prevent helicopter operations, which generally require good visibility for landing. Snow may present the additional problem of removal to prevent accumulation. Spray caused by wind and waves can also dump large amounts of water which must be drained, and in colder conditions may freeze and build up a burden of ice. Severe spray may prevent people from working on deck. Atmospheric icing, also known as black ice can occur in sub-Arctic regions, when the air is humid and the temperature is low. Ice forms directly on cold surfaces and can accumulate rapidly, adding topside weight and increasing wind drag. Icing and frozen spray may occur in the same regions and in similar conditions. Lightning is generally not a major problem to steel and concrete structure with adequate lightning protection, but is a hazard to personnel working in high exposed areas.
  • Sea ice and icebergs
  • Earthquakes and tsunamis
  • Scour
  • Siltation

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