Concentrations of Fe, Mn, Cu, Zn, Co, Ni, Pb, Cd, B, and SiO2 in interstitial waters from bottom sediments of the Atlantis II and Discovery Deeps, Red Sea rift zone

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Main Authors: Pushkina, Zinaida V, Stepanets, M I, Orlova, L P, Sinani, T I
Format: Dataset Open Access
Language:en
Published: PANGAEA 1981
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author Pushkina, Zinaida V
Stepanets, M I
Orlova, L P
Sinani, T I
author_facet Pushkina, Zinaida V
Stepanets, M I
Orlova, L P
Sinani, T I
collection Datos científicos de ciencias marinas y ambientales
contents Chemical analyzes show that interstitial waters from ore-bearing bottom sediments of the Atlantis II and Discovery Deeps are enriched in Fe, Mn, Cu, Ni, Co, Zn, Pb, and Cd compared to sea water. Enrichment factors of these trace elements in the interstitial waters of the Atlantis II Deep relative to the sea water vary within the following ranges: for Fe from 100 to 7000, for Mn from 19047 to 32738, for Zn from 500 to 1600, for Pb from 78333 to 190000, for Cu from 107 to 654. Comparison of average weighted concentrations of Fe, Mn, Zn, Pb, Cu, Ni in the bottom sediments and the interstitial waters of the Atlantis II Deep indicates common regularities and good relationship in distribution of these elements along sediment cores. Differences in concentrations and distribution of the studied trace elements in the interstitial waters of the Atlantis II and Discovery Deeps result from different chemical compositions of hydrothermal fluids entering these deeps.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_777804
institution PANGAEA
language en
publishDate 1981
publisher PANGAEA
record_format pangaea
spellingShingle Concentrations of Fe, Mn, Cu, Zn, Co, Ni, Pb, Cd, B, and SiO2 in interstitial waters from bottom sediments of the Atlantis II and Discovery Deeps, Red Sea rift zone
Pushkina, Zinaida V
Stepanets, M I
Orlova, L P
Sinani, T I
AK22-1905/4; AK22-1905/5; AK22-1995/1; Akademik Kurchatov; AKU22; Archive of Ocean Data; ARCOD; GC; Gravity corer; MULT; Multiple investigations; Red Sea
Chemical analyzes show that interstitial waters from ore-bearing bottom sediments of the Atlantis II and Discovery Deeps are enriched in Fe, Mn, Cu, Ni, Co, Zn, Pb, and Cd compared to sea water. Enrichment factors of these trace elements in the interstitial waters of the Atlantis II Deep relative to the sea water vary within the following ranges: for Fe from 100 to 7000, for Mn from 19047 to 32738, for Zn from 500 to 1600, for Pb from 78333 to 190000, for Cu from 107 to 654. Comparison of average weighted concentrations of Fe, Mn, Zn, Pb, Cu, Ni in the bottom sediments and the interstitial waters of the Atlantis II Deep indicates common regularities and good relationship in distribution of these elements along sediment cores. Differences in concentrations and distribution of the studied trace elements in the interstitial waters of the Atlantis II and Discovery Deeps result from different chemical compositions of hydrothermal fluids entering these deeps.
title Concentrations of Fe, Mn, Cu, Zn, Co, Ni, Pb, Cd, B, and SiO2 in interstitial waters from bottom sediments of the Atlantis II and Discovery Deeps, Red Sea rift zone
topic AK22-1905/4; AK22-1905/5; AK22-1995/1; Akademik Kurchatov; AKU22; Archive of Ocean Data; ARCOD; GC; Gravity corer; MULT; Multiple investigations; Red Sea
url https://doi.org/10.1594/PANGAEA.777804