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Seed cleaning by electrostatic separation

Creator:: Harmond, Jesse E. (Jesse Edward), 1906-, Brandenburg, N. Robert (Norman Robert), 1921-, Booster, Dean E., Oregon State College. Agricultural Experiment Station, and American Society of Agricultural Engineers. Meeting
Abstract:: Published June 1960. Facts and recommendations in this publication may no longer be valid. Please look for up-to-date information in the OSU Extension Catalog: http://extension.oregonstate.edu/catalog
Resource Type:: Technical Report
Full Text:: the American Society of Agricultural Engineers, St. Joseph, Michigan Negative Electrode 0 Postive

Mechanical harvesting of cane fruits

Creator:: Booster, Dean E., Bullock, Richard M. (Richard Melvin), 1918-, and Oregon State University. Agricultural Experiment Station
Abstract:: Published July 1965. Facts and recommendations in this publication may no longer be valid. Please look for up-to-date information in the OSU Extension Catalog: http://extension.oregonstate.edu/catalog
Resource Type:: Technical Report
Full Text:: American Society of Agricultural Engineers, Saint Joseph, Michigan Hand Hand Hand Training systems and

Marine seismic studies near Newport, Oregon

Creator:: Erickson, Barrett H.
Abstract:: In July 1964 three seismic refraction profiles were recorded over Stonewall Bank (44°32'N, 124°24'W) to determine gross sub-bottom geological structure to depths of thousands of feet. In August 1964 a continuous seismic reflection profiler was used to document shallow geological structure within the rocks forming the Bank. Stonewall Bank is...
Resource Type:: Masters Thesis
Full Text:: conducted under the direction of Professor Joseph W. Berg, Jr., Department of Oceanography, Oregon State

Marine geophysical studies offshore: Newport, Oregon

Creator:: Whitcomb, James Hall
Abstract:: A marine geophysical study using shallow seismic reflection, gravity and magnetic methods of investigation was done for an offshore area near Newport, Oregon. The area is bounded by the latitudes 44°1O' to 44°50' N. and longitudes 124°07' to 124°30' W. The interpretation of observational data showed that the geology of...
Resource Type:: Masters Thesis
Full Text:: conducted under the direction of Professor Joseph W. Berg, Jr., Department of Oceanography, Oregon State

Gravity interpretation using the Fourier integral

Creator:: Odegard, Mark Erie
Abstract:: The gravitational anomalies of simple bodies (sphere, cylinder, and fault) were used to develop methods for analyzing gravity data in the frequency domain. The Fourier transforms of the functional representations of the theoretical gravitational anomalies of these bodies were obtained. Mathematical formulations were made between the transform versus frequency relationships...
Resource Type:: Masters Thesis
Full Text:: ACKNOWLEDGMENTS The work presented in this thesis was performed under the direc- tion of Dr. Joseph W. Berg

Transmission and attenuation of the primary seismic wave, [delta]=100 to 600 KM

Creator:: Long, L. T. (Leland Timothy)
Abstract:: The character of the primary seismic wave in the range of distances between 100 and 600 km is affected by such factors as the nature of the source, exponential attenuation, crustal structure, type of wave propagation, recording site geology and instrument response. The first arrivals from the GNOME and SHOAL...
Resource Type:: Dissertation
Full Text:: Redacted for Privacy ACKNOWLEDGEMENTS This research was performed under the direction of Dr. Joseph W

Attenuation of compressional waves in the earth's mantle

Creator:: Sarmah, Suryya Kanta
Abstract:: Fourier transformed amplitudes of the compressional waves recorded between 9° and 91° (about 1000 to 10,000 km) epicentral distance from Gnome, Shoal, Haymaker,and Bilby underground nuclear explosions have been compared with Fourier transformed amplitudes of P waves measured at distances between 9.0 and 1 3. 0 km from the explosions....
Resource Type:: Dissertation
Full Text:: for Privacy ACKNOWLEDGMENT This research was performed under the direction of Dr. Joseph W. Berg

Seismic source characteristics from explosion generated P waves

Creator:: Trembly, Lynn Dale
Resource Type:: Dissertation
Full Text:: SOURCE CHARACTERISTICS FROM EXPLOSION GENERATED P WAVES Abstract approved Joseph W. BergJr The earth

Primary seismic wave (P) at 250-350 km compared to measured wave to 0.3 km from GNOME nuclear explosion

Creator:: Laun, Philip Royal
Abstract:: The first cycle of seismic waves recorded at distances of 45, 300 and 355 km. from the GNOME nuclear explosion was used to determine whether the near source wave characteristics at 0.3 km. could be determined from distance measurements. Both head wave and body wave propagation were considered. First the...
Resource Type:: Masters Thesis
Full Text:: ACKNOWLEDGEMENTS The writer is indebted to Dr. Joseph W. Berg Jr. for guidance in all phases of the research and

Angle of emergence of seismic P waves and its variation with frequency

Creator:: Souders, Robert Hunter
Abstract:: The vertical and radial components of a seismic P wave can be decomposed by a Fourier transform into two sets of nonterminating sinusoidal waves with one set for each component. The tangent of the vertical transform divided by the radial transform gives by definition he apparent angle of emergence for...
Resource Type:: Masters Thesis
Full Text:: ACKNOWLEDGEM ENTS The author gratefully acknowledges Dr. Joseph W. Berg, Jr. for guidance with the work

ScholarsArchive@OSU

Seed cleaning by electrostatic separation

Mechanical harvesting of cane fruits

Marine seismic studies near Newport, Oregon

Marine geophysical studies offshore: Newport, Oregon

Gravity interpretation using the Fourier integral

Transmission and attenuation of the primary seismic wave, [delta]=100 to 600 KM

Attenuation of compressional waves in the earth's mantle

Seismic source characteristics from explosion generated P waves

Primary seismic wave (P) at 250-350 km compared to measured wave to 0.3 km from GNOME nuclear explosion

Angle of emergence of seismic P waves and its variation with frequency

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