_version_ 1867170987939725312
author Varentsov, Igor M
Michailova, R M
author_facet Varentsov, Igor M
Michailova, R M
collection Datos científicos de ciencias marinas y ambientales
contents The distribution of Mn and Fe in water, sediments, hydroxide nodules and crusts of Eningi-Lampi ore-bearing lake is regular, and concordant from the source to the areas of accumulation of these components. Mn-Fe hydroxide nodules and crusts occur at the water-sediment interface, and more rarely in the upper (0-5 cm) film of brown watery mud. The leading role in the formation of Mn-Fe nodules and crusts is played by the chemosorption and auto-catalytic oxidation in the course of interaction of component-bearing solutions with active surfaces. This is considered to be the basic process for the model of ferromanganese ore formation in recent basins. Despite the differences in the physico-geographical and geochemical characteristics of lakes, mediterranean seas and oceans, the formation of ferromanganese hydroxide nodules and crusts in these basins may be explained by this model.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_855186
institution PANGAEA
language en
publishDate 1972
publisher PANGAEA
record_format pangaea
spellingShingle (Fig 2, page 399), Distribution of Fe and Mn in ferromanganese nodules of the Eningi-Lampi Lake, Russia
Varentsov, Igor M
Michailova, R M
DEPTH, sediment/rock; Dredge; DRG; Elevation of event; EningiLampi_104; EningiLampi_116; EningiLampi_117; EningiLampi_118; EningiLampi_119; EningiLampi_121; EningiLampi_123; EningiLampi_127; EningiLampi_128; EningiLampi_133; EningiLampi_137; EningiLampi_141; EningiLampi_150; EningiLampi_152; EningiLampi_154; EningiLampi_158; EningiLampi_99; Event label; Iron; Lake Eningi-Lampi, Russia; Latitude of event; Longitude of event; Manganese; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Spectrophotometric
The distribution of Mn and Fe in water, sediments, hydroxide nodules and crusts of Eningi-Lampi ore-bearing lake is regular, and concordant from the source to the areas of accumulation of these components. Mn-Fe hydroxide nodules and crusts occur at the water-sediment interface, and more rarely in the upper (0-5 cm) film of brown watery mud. The leading role in the formation of Mn-Fe nodules and crusts is played by the chemosorption and auto-catalytic oxidation in the course of interaction of component-bearing solutions with active surfaces. This is considered to be the basic process for the model of ferromanganese ore formation in recent basins. Despite the differences in the physico-geographical and geochemical characteristics of lakes, mediterranean seas and oceans, the formation of ferromanganese hydroxide nodules and crusts in these basins may be explained by this model.
title (Fig 2, page 399), Distribution of Fe and Mn in ferromanganese nodules of the Eningi-Lampi Lake, Russia
topic DEPTH, sediment/rock; Dredge; DRG; Elevation of event; EningiLampi_104; EningiLampi_116; EningiLampi_117; EningiLampi_118; EningiLampi_119; EningiLampi_121; EningiLampi_123; EningiLampi_127; EningiLampi_128; EningiLampi_133; EningiLampi_137; EningiLampi_141; EningiLampi_150; EningiLampi_152; EningiLampi_154; EningiLampi_158; EningiLampi_99; Event label; Iron; Lake Eningi-Lampi, Russia; Latitude of event; Longitude of event; Manganese; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Spectrophotometric
url https://doi.org/10.1594/PANGAEA.855186