Goldberg, Edward D (1954): (Table 2, Page 252) Average chemical composition of 11 manganese nodules and crust from the Pacific Ocean [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.858479, Supplement to: Goldberg, ED (1954): Marine Geochemistry 1. Chemical Scavengers of the Sea. The Journal of Geology, 62(3), 249-265, http://www.jstor.org/stable/30080120
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Abstract:
The ability of the hydrated oxides of manganese and iron to adsorb ions from solution (scavenging) is considered in relation to some problems in marine geology, chemistry, and biology. In the ferruginous sediments of the Pacific Ocean, iron oxides are accompanied by titanium, cobalt, and zirconium in amounts proportional to the iron content. Similarly, copper and nickel are linearly related to the manganese content. These observations are explained on the basis of scavenging. An electrochemical theory for the formation of manganese nodules is presented. Marine sediments are classified on the basis of the geosphere in which the solid phases originate. The distribution of certain ionic species in sea water between the solid and aqueous phases is considered on the basis of scavenging and co-ordination compound theory. The concentration of minor elements by members of the marine biosphere is explained either by the direct uptake of the element or by the uptake of iron or manganese oxides with the accompanying scavenged element.
Source:
Grant, John Bruce; Moore, Carla J; Alameddin, George; Chen, Kuiying; Barton, Mark (1992): The NOAA and MMS Marine Minerals Geochemical Database. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V52Z13FT
Further details:
Warnken, Robin R; Virden, William T; Moore, Carla J (1992): The NOAA and MMS Marine Minerals Bibliography. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V53X84KN
Project(s):
Coverage:
Median Latitude: 22.471245 * Median Longitude: -169.188094 * South-bound Latitude: -42.700000 * West-bound Longitude: 134.166667 * North-bound Latitude: 56.166000 * East-bound Longitude: -116.166000
Date/Time Start: 1874-03-13T00:00:00 * Date/Time End: 1955-01-01T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 0.070 m
Event(s):
CHA-160 * Latitude: -42.700000 * Longitude: 134.166667 * Date/Time: 1874-03-13T00:00:00 * Elevation: -4269.0 m * Campaign: Challenger1872 * Basis: H.M.S. Challenger (1872) * Method/Device: Grab (GRAB)
Comment:
Samples have been dried and digested in an HCl acid solution. Only the soluble part was analysed. Except for AL, Ti and Zr, analyses have been averaged over the 3 analyses per sample presented by the author.
From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | Goldberg, Edward D | |||
2 | Identification | ID | Goldberg, Edward D | |||
3 | DEPTH, sediment/rock | Depth sed | m | Goldberg, Edward D | Geocode | |
4 | Iron | Fe | % | Goldberg, Edward D | Spectrophotometer, Beckmann DU | |
5 | Manganese | Mn | % | Goldberg, Edward D | Spectrophotometer, Beckmann DU | |
6 | Nickel | Ni | % | Goldberg, Edward D | Spectrophotometer, Beckmann DU | |
7 | Cobalt | Co | % | Goldberg, Edward D | Spectrophotometer, Beckmann DU | |
8 | Copper | Cu | % | Goldberg, Edward D | Spectrophotometer, Beckmann DU | |
9 | Phosphorus | P | % | Goldberg, Edward D | Spectrophotometer, Beckmann DU | |
10 | Aluminium | Al | % | Goldberg, Edward D | Spectrophotometer, Beckmann DU | |
11 | Titanium | Ti | % | Goldberg, Edward D | Spectrophotometer, Beckmann DU | |
12 | Zirconium | Zr | % | Goldberg, Edward D | Spectrophotometer, Beckmann DU | |
13 | Deposit type | Deposit type | Goldberg, Edward D |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
118 data points
Data
1 Event | 2 ID | 3 Depth sed [m] | 4 Fe [%] | 5 Mn [%] | 6 Ni [%] | 7 Co [%] | 8 Cu [%] | 9 P [%] | 10 Al [%] | 11 Ti [%] | 12 Zr [%] | 13 Deposit type |
---|---|---|---|---|---|---|---|---|---|---|---|---|
NTHL-10 | NTHL-10-1-11 | 0.000 | 11.12 | 12.53 | 0.20 | 0.11 | 0.50 | 0.38 | 0.94 | 0.89 | 0.0130 | Mn crust |
GOLDHW1 | GOLDHW1-1 | 0.000 | 17.00 | 14.53 | 0.27 | 0.19 | 0.50 | 0.42 | 1.24 | 1.24 | 0.0140 | Mn nodule |
MPC-43K | MPC-43K -1-14-16 | 0.070 | 15.77 | 17.13 | 0.38 | 0.21 | 0.63 | 0.29 | Mn nodule | |||
MPC-26A-3 | MPC-26A-3-2-26 | 0.000 | 16.77 | 16.90 | 0.31 | 0.46 | 0.19 | 1.23 | 0.27 | 1.25 | 0.0057 | Mn nodule |
NTHL-D1 | NTHL-D1-1-4 | 0.000 | 14.80 | 19.40 | 0.32 | 0.31 | 0.21 | 0.56 | 0.27 | 0.77 | 0.0060 | Mn nodule |
NTHL-D7 | NTHL-D7-1-17 | 0.000 | 13.07 | 20.20 | 0.45 | 0.26 | 0.40 | 0.54 | 0.67 | 0.59 | 0.0018 | Mn nodule |
NEL-HEND | NEL-HEND-23 | 0.000 | 20.10 | 21.30 | 0.30 | 0.32 | 0.22 | 0.80 | 0.39 | 0.74 | 0.0038 | Mn nodule |
MPC-37A | MPC-37A-1-7 | 0.000 | 13.40 | 21.03 | 0.58 | 0.54 | 0.47 | 0.54 | 0.39 | 0.81 | 0.0056 | Mn crust |
PAS-19121 | PAS-19121-20 | 0.000 | 6.90 | 22.40 | 0.61 | 0.02 | 0.82 | 0.38 | 1.70 | 0.27 | 0.0021 | Mn nodule |
MPC-43J | MPC-43J-1-29-31 | 0.000 | 15.60 | 23.63 | 0.61 | 0.61 | 0.47 | 0.41 | 0.29 | 1.18 | 0.0082 | Mn nodule |
CHA-160 | CHA-160-2-32 | 0.000 | 9.34 | 19.93 | 1.05 | 0.08 | 1.65 | 0.34 | 1.17 | 0.31 | 0.0038 | Mn nodule |