(Tables 1-3, pages 14-15) Radionuclide determinations on cores from the DOMES Site B and MANOP Site S in the Pacific Ocean

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Autor principal: Kadko, David
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 1983
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_version_ 1867170078183653376
author Kadko, David
author_facet Kadko, David
collection Datos científicos de ciencias marinas y ambientales
contents Erosion of sediment at two sites within the siliceous-clay province of the northeast equatorial Pacific is investigated by examining radionuclide, radiolarian and percent smectite profiles of three cores. A numerical model of the sediment is presented that examines the effect of various particle rain rates, erosion rates and biological mixing parameters on these profiles. 230Th, because of its longer half-life, is a more sensitive tracer of erosion than231Pa. Because the input of these radionuclides into the sediment is not well defined however, conservative tracers, such as the percent smectite of the clay fraction and fossil radiolarians are used to constrain the rate of sediment recycling. Dissolution of radiolarians though can greatly affect the interpretation of the observed biostratigraphy.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_881163
institution PANGAEA
language en
publishDate 1983
publisher PANGAEA
record_format pangaea
spellingShingle (Tables 1-3, pages 14-15) Radionuclide determinations on cores from the DOMES Site B and MANOP Site S in the Pacific Ocean
Kadko, David
BC; Box corer; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DOMES Site B, Pacific Ocean; Event label; Identification; Inductively coupled plasma - mass spectrometry (ICP-MS); K7905; K7905-047BC; K7905-106BC; Knorr; Lead-210 excess; Lead-210 excess, standard deviation; MANOP; MANOP Site S, Pacific Ocean; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; Protactinium-231; Protactinium-231, standard deviation; RP-8-OC-75; RP8OC7503; RP8OC75-55-56; Thorium-230; Thorium-230, standard deviation; Uranium-234; Uranium-234, standard deviation; Uranium-238; Uranium-238, standard deviation
Erosion of sediment at two sites within the siliceous-clay province of the northeast equatorial Pacific is investigated by examining radionuclide, radiolarian and percent smectite profiles of three cores. A numerical model of the sediment is presented that examines the effect of various particle rain rates, erosion rates and biological mixing parameters on these profiles. 230Th, because of its longer half-life, is a more sensitive tracer of erosion than231Pa. Because the input of these radionuclides into the sediment is not well defined however, conservative tracers, such as the percent smectite of the clay fraction and fossil radiolarians are used to constrain the rate of sediment recycling. Dissolution of radiolarians though can greatly affect the interpretation of the observed biostratigraphy.
title (Tables 1-3, pages 14-15) Radionuclide determinations on cores from the DOMES Site B and MANOP Site S in the Pacific Ocean
topic BC; Box corer; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DOMES Site B, Pacific Ocean; Event label; Identification; Inductively coupled plasma - mass spectrometry (ICP-MS); K7905; K7905-047BC; K7905-106BC; Knorr; Lead-210 excess; Lead-210 excess, standard deviation; MANOP; MANOP Site S, Pacific Ocean; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; Protactinium-231; Protactinium-231, standard deviation; RP-8-OC-75; RP8OC7503; RP8OC75-55-56; Thorium-230; Thorium-230, standard deviation; Uranium-234; Uranium-234, standard deviation; Uranium-238; Uranium-238, standard deviation
url https://doi.org/10.1594/PANGAEA.881163