Minor element geochemistry of Lake Michigan ferromanganese nodules

Fuente: PANGAEA
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Auteurs principaux: Edgington, David N, Callender, Edward
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 1970
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_version_ 1867169106100224000
author Edgington, David N
Callender, Edward
author_facet Edgington, David N
Callender, Edward
collection Datos científicos de ciencias marinas y ambientales
contents Samples of ferromanganese nodules from several localities in Lake Michigan have been analyzed for their minor element content utilizing neutron activation techniques. The thorium and uranium levels in Lake Michigan nodules exhibit marked dissimilarities with marine nodules. The radium content of these freshwater nodules is substantially higher than the reported marine values. The concentrations of barium in the Lake Michigan nodules appear to be abnormally high. Although barium could be present as minute segregations of the mineral barite, patterns obtained using the electron microprobe suggest it is evently dispersed throughout the nodules. The average arsenic content of these freshwater nodules is at least twice as great as that reported for highly oxidized marine sediments. If all this arsenic is dissolved and released into Green Bay as a result of changing environmental conditions (eutrophication), the concentration in the water of Green Bay would be several times the maximum permissible level for drinking water.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_848032
institution PANGAEA
language en
publishDate 1970
publisher PANGAEA
record_format pangaea
spellingShingle Minor element geochemistry of Lake Michigan ferromanganese nodules
Edgington, David N
Callender, Edward
Antimony; Arsenic; Atomic absorption spectrometry (AAS); Barium; Bromine; Cadmium; Cerium; Cobalt; Comment; Copper; Dredge; DRG; EDGI1970_11; EDGI1970_2; EDGI1970_35; EDGI1970_37; EDGI1970_43; EDGI1970_6; Europium; Event label; Gallium; Green Bay - Lake Michigan; Iron; Lake Michigan; Lanthanum; Manganese; Maximum; Neutron activation analysis; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Radium; ROSS1969_25; Samarium; Sample ID; Scandium; Soluble residue; Strontium; Thorium; Uranium; Zinc
Samples of ferromanganese nodules from several localities in Lake Michigan have been analyzed for their minor element content utilizing neutron activation techniques. The thorium and uranium levels in Lake Michigan nodules exhibit marked dissimilarities with marine nodules. The radium content of these freshwater nodules is substantially higher than the reported marine values. The concentrations of barium in the Lake Michigan nodules appear to be abnormally high. Although barium could be present as minute segregations of the mineral barite, patterns obtained using the electron microprobe suggest it is evently dispersed throughout the nodules. The average arsenic content of these freshwater nodules is at least twice as great as that reported for highly oxidized marine sediments. If all this arsenic is dissolved and released into Green Bay as a result of changing environmental conditions (eutrophication), the concentration in the water of Green Bay would be several times the maximum permissible level for drinking water.
title Minor element geochemistry of Lake Michigan ferromanganese nodules
topic Antimony; Arsenic; Atomic absorption spectrometry (AAS); Barium; Bromine; Cadmium; Cerium; Cobalt; Comment; Copper; Dredge; DRG; EDGI1970_11; EDGI1970_2; EDGI1970_35; EDGI1970_37; EDGI1970_43; EDGI1970_6; Europium; Event label; Gallium; Green Bay - Lake Michigan; Iron; Lake Michigan; Lanthanum; Manganese; Maximum; Neutron activation analysis; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Radium; ROSS1969_25; Samarium; Sample ID; Scandium; Soluble residue; Strontium; Thorium; Uranium; Zinc
url https://doi.org/10.1594/PANGAEA.848032