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dc.contributor.authorHart, E.D.en_US
dc.contributor.editoren_US
dc.contributor.otheren_US
dc.date.accessioned2010-02-15T16:53:22Z
dc.date.available2010-02-15T16:53:22Z
dc.date.issued1969en_US
dc.identifier.urihttp://hdl.handle.net/1969.3/19704
dc.description37 p.en_US
dc.description.abstractRadioactive sediment tracer tests were conducted in the Houston Ship Channel to determine qualitatively the sediment movement in the channel. About 5 curies of the isotope gold 198 was thoroughly mixed with sediment samples from the channel, and the activated sediment was then deposited along the bottom at two locations. The results of tracing the deposits indicated that the activated sediment moved up-stream for several miles. Activity was recorded down-stream for only a short distance. Very little lateral movement out of the channel was detected.en_US
dc.description.urihttp://gbic.tamug.edu/request.htmen_US
dc.publisherU.S. Army Corps of Engineers, Waterways Experiment Stationen_US
dc.relation.ispartofseries1944.00en_US
dc.relation.urien_US
dc.subjectradioactive labeling; sediment movement; navigational channels; sediment transport; radioactive tracersen_US
dc.titleRadioactive sediment tracer tests, Houston Ship Channel, Houston, Texas.en_US
dc.typeBooken_US
dc.placeVicksburg, Mississippien_US
dc.seriesReport No. AEWES-Misc.-Pap.-H-69-2en_US
dc.vol-issueen_US
dc.geo-codeHouston Ship Channelen_US
dc.locationNOT AVAILABLE IN-HOUSE.en_US
dc.scaleen_US
dc.latitudeen_US
dc.longitudeen_US
dc.contract-noen_US
dc.notesen_US
dc.degreeen_US
dc.acquisition-srcen_US
dc.description-otheren_US
dc.universityen_US
dc.historyen_US
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