Open Access. Powered by Scholars. Published by Universities.®

Physical Sciences and Mathematics Commons

Open Access. Powered by Scholars. Published by Universities.®

Oceanography and Atmospheric Sciences and Meteorology

1992

Center for Coastal and Ocean Mapping

Articles 1 - 3 of 3

Full-Text Articles in Physical Sciences and Mathematics

Downhole Logging As A Paeoceanographic Tool On Ocean Drilling Program Leg 138: Interface Between High-Resolution Stratigraphy And Regional Syntheses, Mitchell Lyle, Larry A. Mayer, Nicklas G. Pisias, T. K. Hagelberg, Kathleen A. Dadey, Stephen F. Bloomer Dec 1992

Downhole Logging As A Paeoceanographic Tool On Ocean Drilling Program Leg 138: Interface Between High-Resolution Stratigraphy And Regional Syntheses, Mitchell Lyle, Larry A. Mayer, Nicklas G. Pisias, T. K. Hagelberg, Kathleen A. Dadey, Stephen F. Bloomer

Center for Coastal and Ocean Mapping

On Ocean Drilling Program (ODP) Leg 138, standard shipboard procedures were modified to allow for the real-time monitoring of several laboratory core-scanning systems that provide centimeter-scale measurements of saturated bulk density, magnetic susceptibility and digital color reflectance. These continuous, high-resolution data sets were used to ensure the proper offset of multiple holes and to splice together complete sedimentary sections. Typically, the spliced, continuousediment sections were found to be about 10% longer than the section drilled, as measured by the length of the drill string. While the source of this elongation is not yet fully understood, it must be compensated for …


Differential Phase Estimation With The Seamarc Ii Bathymetric Sidescan Sonar System, M A. Masnadi-Shirazi, Christian De Moustier, Pierre Cervenka, Stanley H. Zisk Jul 1992

Differential Phase Estimation With The Seamarc Ii Bathymetric Sidescan Sonar System, M A. Masnadi-Shirazi, Christian De Moustier, Pierre Cervenka, Stanley H. Zisk

Center for Coastal and Ocean Mapping

A maximum-likelihood estimator is used to extract differential phase measurements from noisy seafloor echoes received at pairs of transducers mounted on either side of the SeaMARC II bathymetricsidescan sonar system. Carrier frequencies for each side are about 1 kHz apart, and echoes from a transmitted pulse 2 ms long are analyzed. For each side, phase difference sequences are derived from the full complex data consisting of base-banded and digitized quadrature components of the received echoes. With less bias and a lower variance, this method is shown to be more efficient than a uniform mean estimator. It also does not exhibit …


Evaluation And Verification Of Bottom Acoustic Reverberation Statistics Predicted By The Point Scattering Model, Dimitri Alexandrou, Christian De Moustier, G Haralabus Mar 1992

Evaluation And Verification Of Bottom Acoustic Reverberation Statistics Predicted By The Point Scattering Model, Dimitri Alexandrou, Christian De Moustier, G Haralabus

Center for Coastal and Ocean Mapping

The point scatteringmodel offers a parameterization of the reverberation probability density function (pdf) in terms of the coefficient of excess (kurtosis) and a coherent component represented by a harmonic process with random phase. In this paper the potential utility of this parametrization is investigated in the context of seafloor characterization. The problem of separating out the effect of each parameter is discussed. Computer simulations are used to verify model predictions on the reverberation quadrature, envelope, and phase pdf. As part of the verification study, the scatterer density was determined from the kurtosis of the reverberation quadrature pdf. A statistical analysis …