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Predictor Equations For Beach Processes And Responses, W. Harrison, N. A. Pore, D. R. Tuck Jr. Dec 1965

Predictor Equations For Beach Processes And Responses, W. Harrison, N. A. Pore, D. R. Tuck Jr.

VIMS Articles

A stepwise (linear) multiple regression procedure is applied to 11 environmental variables (or predictors) in the beach-ocean-atmosphersey stema t Virginia Beach, Virginia, for the following five predictands: mean longshore current velocity, mean bottom slope in the shoaling-wave zone, average mean grain size in the shoaling-wave zone, and beach deposition and beach erosion on the lower foreshore. Predictors consist of variables related to beach geometry, local water properties, local wind conditions, tidal fluctuations, and wave characteristics The resultant equations are tested against a set of independent data and, with one exception, agree reasonably. It is believed that if the data set …


Apparatus For Holding The Individual Oysters Under Equal Water Flows, Dexter S. Haven, Reinaldo Morales-Alamo Apr 1965

Apparatus For Holding The Individual Oysters Under Equal Water Flows, Dexter S. Haven, Reinaldo Morales-Alamo

VIMS Articles

No abstract provided.


Possible Late Pleistocene Uplift, Chesapeake Bay Entrance, W. Harrison, Rj Malloy, Ga Rusnak, J Terasmae Feb 1965

Possible Late Pleistocene Uplift, Chesapeake Bay Entrance, W. Harrison, Rj Malloy, Ga Rusnak, J Terasmae

VIMS Articles

Paleontological and lithological studies of engineering borings and boring logs subaerial erosion surface of Pliocene (?)-Pleistocene age cuts across clastic sediments of pre-Yorktownian Miocene age in the subsurface and subbottom of the lower Chesapeake Bay area. When the bore-hole data are coupled with the results of subbottom echo profiling and piledriving records, it is possible to construct accurate cross sections of the buried Miocene-Pleistocene contact. The cross sections show "lows" in the erosion surface that may be correlated with the buried channels of the Pleistocene Elizabeth, James, York, and Susquehanna river valleys. Probable channel depths below mean low water at …


Frequencies Of Infaunal Invertebrates Related To Water Content Of Chesapeake Bay Sediments, W. Harrison, Marvin L. Wass Jan 1965

Frequencies Of Infaunal Invertebrates Related To Water Content Of Chesapeake Bay Sediments, W. Harrison, Marvin L. Wass

VIMS Articles

The following relationship was investigated for a total of 44 stations, using sequential (linear) multiregression analysis: A = f (D, S a , S i., C, M z, S o , W) 1 z o where A = the frequency of an infaual invertebrate species, D : water depth at the station, Sa = per cent sand, Si =percent silt, C = per cent clay, Mz = mean grain size, S o = sediment Sorting Coefficient, and W = water content. Three animals were chosen for the dependent variable: Ensis directus, Nephtys incisa, and Retusa canaliculata. Results of the least-squares …


Frequencies Of Infaunal Invertebrates Related To Water Content Of Chesapeake Bay Sediments, W. Harrison, Marvin L. Wass Jan 1965

Frequencies Of Infaunal Invertebrates Related To Water Content Of Chesapeake Bay Sediments, W. Harrison, Marvin L. Wass

VIMS Articles

The following relationship was investigated for a total of 44 stations, using sequential (linear) multiregression analysis:

A = f (D, S a , S., C, M , S , W)

where A = the frequency of an infauna! invertebrate species, D : water depth at the station, Sa = per cent sand, Si =percent silt, C = per cent clay, Mz = mean grain size, S o = sediment Sorting Coefficient, and W = water content. Three animals were chosen for the dependent variable: Ensis directus, Nephtys incisa, and Retusa canaliculata.

Results of the least-squares search procedure indicate that if …