skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Partitioning of sediments among shoreface transport paths: analysis of sediment dispersal patterns using empirical orthogonal functions

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:5848670

Recent geomorphic evidence from the inner shelf and shoreface to the east of Long Island's barrier island system indicates that reworking of glacial outwash deposits at the inner shelf-shoreface transition, as sea level rises, may be supplying much of the sediment needed to maintain barrier island to the west. A conceptual model describing sediment dispersal from outwash source areas was developed from this hypothesis. It was reasoned that outwash sediments ranging from silts to coarse gravels would be subject to differential transport paths across and along the shoreface upon reworking. Coarser grain sizes would move onshore toward the intertidal beach, whereas finer sediments would move offshore. Sand of intermediate grain size would be concentrated in the surf zone and move alongshore in wave-generated longshore currents. To test this model, 400 samples from the beach and shoreface of Long Island were analyzed for grain-size frequency distribution and each grain-size class was examined for frequency of occurrence in the cross-shore and alongshore directions. On a spatially averaged basis, grain-size classes displayed peak abundance in specific zones across the shoreface as predicted by the model, but alongshore trends could not be recognized among the noisy data. Therefore, empirical orthogonal functions (EOF) were used to examine uncorrelated modes of variability in the occurrence of each grain-size class in the alongshore direction. The first function, representing more than 60% of the variability among the data, showed that grain sizes subject to longshore transport in the surf zone increase in frequency in the alongshore direction relative to coarser grain sizes. Results also show that peak concentrations of coarse sediments correspond to zones subject to frequent overwashing. It is concluded that EOF analysis of individual grain-size classes holds promise for extracting trends from noisy data sets.

Research Organization:
State Univ. of New York, Stony Brook
OSTI ID:
5848670
Report Number(s):
CONF-850322-
Journal Information:
Am. Assoc. Pet. Geol., Bull.; (United States), Vol. 69:2; Conference: American Association of Petroleum Geologists annual meeting, New Orleans, LA, USA, 25 Mar 1985
Country of Publication:
United States
Language:
English

Similar Records

Barrier/lagoon and shoreface Holocene stratigraphy: Masonboro Island, N. C
Conference · Mon Mar 01 00:00:00 EST 1993 · Geological Society of America, Abstracts with Programs; (United States) · OSTI ID:5848670

Recent carbonate sedimentation on Balearic platform: model for temperate-climate carbonate shelves
Conference · Wed Mar 01 00:00:00 EST 1989 · AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States) · OSTI ID:5848670

Sequence stratigraphic analysis of individual depositional successions: Effects of marine/nonmarine sediment partitioning and longitudinal sediment transport, Mannville Group, Alberta Foreland Basin, Canada
Journal Article · Mon May 01 00:00:00 EDT 1995 · AAPG Bulletin · OSTI ID:5848670