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Effects of sea level rise on Barrier Islands, with examples from Louisiana

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (USA)
OSTI ID:6602443
 [1]
  1. Geological Survey, St. Petersburg, FL (USA)

Conceptually, with sea level constant and no net losses or gains of sediment, a barrier island and shoreface profile would approach an equilibrium configuration. With a rise in sea level, the profile would adjust upward the same amount as the sea level rise, and adjust landward such that the amount of sediment eroded would be equal to the amount accreted. In an early model, the adjustment of the shoreface profile was achieved by nearshore erosion and offshore deposition, a net offshore transport. However, a number of studies have shown that onshore transport through overwash and other processes is very important. To maintain an equilibrium configuration, the quantity of sand overwashed must be balanced by sediment eroded from the shoreface. Barrier islands that have an ample supply of sand may approach an equilibrium configuration as required by the sea level rise models. However, a sand-starved island may not approach equilibrium. Recent field experiments on the Louisiana coast have examined the response of severely sand-starved barriers to rapid sea level rise (1 cm/yr relative to the land) and other processes. These islands are overwash platforms with little to no dune development and consist of a thin (1-2 m) wedge of sand overlying marsh The shoreface is mud that in places is covered by a thin veneer of sand. Low berm elevations allow overwash even during moderate storms. Overwash builds the berm higher during storms, but eolian processes following overwash have been observed to plane the beach to roughly its prestorm elevation. Hence, the beach does not build vertically to limit overwash, and the sand wedge forming the beach rapidly migrates landward over the marsh. The muddy shoreface has the classic exponential shale that has been described for many sandy environments. However, unlike a sandy shoreface, the muddy shoreface does not appear to be evolving to a condition limiting erosion.

OSTI ID:
6602443
Report Number(s):
CONF-900605--
Journal Information:
AAPG Bulletin (American Association of Petroleum Geologists); (USA), Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (USA) Vol. 74:5; ISSN AABUD; ISSN 0149-1423
Country of Publication:
United States
Language:
English

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