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dc.contributor.authorHART EDen_US
dc.contributor.otheren_US
dc.date.accessioned2010-02-15T17:16:01Z
dc.date.available2010-02-15T17:16:01Z
dc.date.issued1969en_US
dc.identifier.urihttp://hdl.handle.net/1969.3/23291
dc.description33-en_US
dc.description.abstractRadioactive sediment tracer tests were conducted to determine qualitatively sediment movement in channel; about 5 C of isotope, Au-198 was thoroughly mixed with sediment samples from channel, and activated sediment was then deposited along bottom at two locations; results of tracing deposits indicated that activated sediment moved upstream for several miles; activity was recorded downstream for only short distance; very little lateral movement out of channel was detecteden_US
dc.description.urihttp://gbic.tamug.edu/request.htmen_US
dc.publisheren_US
dc.relation.ispartofseries50886.00en_US
dc.relation.urien_US
dc.subjectONAen_US
dc.subjectRADIOACTIVE MATERIALS,TRACERSen_US
dc.subjectRIVERSen_US
dc.subjectSedimentationen_US
dc.subjectTexasen_US
dc.titleRadioactive sediment tracer tests Houston ship channel, Houston, Texasen_US
dc.typeJournalen_US
dc.placeen_US
dc.seriesen_US
dc.vol-issue()en_US
dc.locationen_US
dc.scaleen_US
dc.latitudeen_US
dc.longitudeen_US
dc.contract-noen_US
dc.notesCompilation and indexing terms, Copyright 2004 Elsevier Engineering Information, Incen_US
dc.degreeen_US
dc.acquisition-srcDownloaded from-Engineering Village 2en_US
dc.description-otheren_US
dc.universityen_US
dc.historyen_US
dc.call-noen_US


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