Willis, J P; Ahrens, L H (1962): (Table 1, page 754) Estimated concentrations of various elements in nineteen manganese nodules [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.857790, Supplement to: Willis, JP; Ahrens, LH (1962): Some investigations on the composition of manganese nodules, with particular reference to certain trace elements. Geochimica et Cosmochimica Acta, 26(7), 751-764, https://doi.org/10.1016/0016-7037(62)90037-6
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Abstract:
Using spectrochemical techniques Fe, Si, Mg, Co, Ni, Cu, V, Mo, Ti and Tl have been estimated in nineteen manganese nodules, eight from the Atlantic ocean, seven from the Pacific ocean and four from the Indian ocean. Though data on more samples are required before firm and detailed conclusions can be made about the distribution of elements in manganese nodules, several distinct features appear when the data on the nineteen samples are examined. Certain elements appear to enrich more strongly than others. For example, relative to igneous rocks Mo is much more strongly enriched than V. For several elements (Ni, Cu and particularly Co and Tl) the degree of enrichment in two Fe-low nodules is far smaller than in the other nodules. The magnitude of dispersion of concentration appears to vary considerably for different elements; thus, whereas variation of concentration of V is relatively small, that of Ni, Cu, Co and Tl is far larger. The statistical nature of the distribution of Fe in manganese nodules appears to be characteristic and different from that of the other elements studied so far. Of the possible inter-element relationships examined that of Ni-Cu appears to be the most strongly developed.
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: 2.721926 * Median Longitude: -68.815705 * South-bound Latitude: -49.353300 * West-bound Longitude: -155.916700 * North-bound Latitude: 40.235000 * East-bound Longitude: 67.183333
Date/Time Start: 1904-11-14T00:00:00 * Date/Time End: 1959-05-15T00:00:00
Minimum DEPTH, sediment/rock: 0 m * Maximum DEPTH, sediment/rock: 0 m
Event(s):
AFII-A316 * Latitude: -34.700000 * Longitude: 16.900000 * Elevation: -3200.0 m * Location: Atlantic Ocean * Method/Device: Dredge (DRG) * Comment: Basis: Africana II
AFII-A322 * Latitude: -34.600000 * Longitude: 17.000000 * Elevation: -2743.0 m * Location: Atlantic Ocean * Method/Device: Dredge (DRG) * Comment: Basis: Africana II
ALBTR-13 (ALB-13) * Latitude: 9.950000 * Longitude: -137.783333 * Elevation: -4919.0 m * Location: Pacific Ocean * Campaign: Albatross1899-1900 * Basis: Albatross (1882-1921) * Method/Device: Dredge (DRG)
Comment:
Each powdered sample was dried for 2 hr at 12O°C, weighed and then heated to red heat in a crucible over a bunsen flame for 5 min.
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 | Willis, J P | |||
2 | Campaign of event | Campaign | Willis, J P | |||
3 | Date/Time of event | Date/Time | Willis, J P | |||
4 | Latitude of event | Latitude | Willis, J P | |||
5 | Longitude of event | Longitude | Willis, J P | |||
6 | Elevation of event | Elevation | m | Willis, J P | ||
7 | Sample ID | Sample ID | Willis, J P | |||
8 | DEPTH, sediment/rock | Depth sed | m | Willis, J P | Geocode | |
9 | Loss on ignition | LOI | % | Willis, J P | Spectrography (Hilger E 478) | |
10 | Iron | Fe | % | Willis, J P | Spectrography (Hilger E 478) | |
11 | Silicon | Si | % | Willis, J P | Spectrography (Hilger E 478) | |
12 | Magnesium | Mg | % | Willis, J P | Spectrography (Hilger E 478) | |
13 | Cobalt | Co | % | Willis, J P | Spectrography (Hilger E 478) | |
14 | Nickel | Ni | % | Willis, J P | Spectrography (Hilger E 478) | |
15 | Copper | Cu | % | Willis, J P | Spectrography (Hilger E 478) | |
16 | Molybdenum | Mo | % | Willis, J P | Spectrography (Hilger E 478) | |
17 | Vanadium | V | % | Willis, J P | Spectrography (Hilger E 478) | |
18 | Titanium | Ti | % | Willis, J P | Spectrography (Hilger E 478) | |
19 | Thallium | Tl | mg/kg | Willis, J P | Indirect determination by reference to Ni | |
20 | Manganese | Mn | % | Willis, J P | Indirect determination by Mn/Pd intensity ratio | |
21 | Sample code/label | Sample label | Willis, J P | Index of sample in the collections of NHM, London (British Museum) | ||
22 | Description | Description | Willis, J P |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
271 data points
Data
1 Event | 2 Campaign | 3 Date/Time | 4 Latitude | 5 Longitude | 6 Elevation [m] | 7 Sample ID | 8 Depth sed [m] | 9 LOI [%] | 10 Fe [%] | 11 Si [%] | 12 Mg [%] | 13 Co [%] | 14 Ni [%] | 15 Cu [%] | 16 Mo [%] | 17 V [%] | 18 Ti [%] | 19 Tl [mg/kg] | 20 Mn [%] | 21 Sample label | 22 Description |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
AFII-A322 | -34.6000 | 17.0000 | -2743 | A322-1-W11 | 0 | 13.6 | 9.30 | 5.3 | 0.92 | 0.2000 | 0.710 | 0.083 | 0.033 | 0.045 | 0.053 | 30 | 0.38 | Sample 4 x 2 x 2 cm | |||
AFII-A322 | -34.6000 | 17.0000 | -2743 | A322-1-W12 | 0 | 12.4 | 8.40 | 8.7 | 1.20 | 0.2600 | 0.820 | 0.093 | 0.032 | 0.032 | 0.076 | 15 | 0.37 | Sample taken from layer 7 x 5 x 0.5 cm on vertebra1 disk of a whale | |||
AFII-A316 | -34.7000 | 16.9000 | -3200 | A316-1-W13 | 0 | 13.4 | 15.50 | 7.9 | 1.70 | 0.2000 | 0.750 | 0.095 | 0.044 | 0.049 | 0.093 | 90 | 0.47 | Sample 1 x 3 x 3 cm taken off a fossilized whale bone | |||
AT150-008D | AT150 | 1947-07 | 31.8166 | -43.4166 | -3700 | AT150-1-W16 | 0 | 12.9 | 24.30 | 4.3 | 1.00 | 0.4800 | 0.190 | 0.100 | 0.032 | 0.085 | 0.910 | 65 | 0.34 | BM 1960,197 | Dredge, Manganese nodule. 1 nodule app. mass 100 g. Received in powder form |
TH1-TR4 | TH1 | 1956-09 | 29.3000 | -57.3333 | -5400 | TH1-TR4-1-W17 | 0 | 12.5 | 17.50 | 8.2 | 1.70 | 0.3000 | 0.360 | 0.200 | 0.047 | 0.055 | 0.480 | 135 | 0.40 | BM 1960.198a | The 49g nodule was cut in half for geochemical determinations (17/3/1961) and one half is retained. Of the powder, a sample was sent to Dr J.P. Willis in March 1961. |
V15-125SBT | V15 | 1959-03 | -49.3533 | -47.7433 | -5040 | V15-125SBT-1-W18 | 0 | 10.2 | 11.20 | 13.7 | 1.20 | 0.0580 | 0.630 | 0.190 | 0.042 | 0.034 | 0.320 | 40 | 0.40 | BM 1959,550a | Received in powder form |
WHOI-A-105 | 30.8500 | -78.4500 | -732 | WHOI-A-105-1-W27 | 0 | 18.9 | 18.70 | 2.0 | 3.70 | 0.5500 | 0.520 | 0.069 | 0.068 | 0.084 | 0.490 | 55 | 0.47 | Sample 1 x2 x3cm | |||
TH1-TR6 | TH1 | 1956-09 | 29.2833 | -57.3833 | -5840 | TH1-TR6-1-W28 | 0 | 12.7 | 18.40 | 7.7 | 2.40 | 0.3700 | 0.480 | 0.170 | 0.055 | 0.066 | 0.590 | 130 | 0.45 | Small nodules: 0.5 - 1 cm. diam., 2.6 g. | |
ALBTR-173 | Albatross1899-1900 | -18.9167 | -146.5333 | -4462 | ALBTR-173-2-W23m | 0 | 12.7 | 21.40 | 9.9 | 1.50 | 0.3600 | 0.300 | 0.160 | 0.039 | 0.055 | 0.930 | 80 | 0.42 | Middle layer (0.5 cm) of nodule having a nucleus of yellow clay | ||
ALBTR-173 | Albatross1899-1900 | -18.9167 | -146.5333 | -4462 | ALBTR-173-2-W23o | 0 | 13.1 | 18.50 | 8.7 | 1.70 | 0.4700 | 0.290 | 0.140 | 0.035 | 0.052 | 1.300 | 110 | 0.44 | Outer layer (0.5 cm) | ||
ALBTR-4658 | Albatross1904-1905 | 1904-11 | -8.4917 | -85.5933 | -4334 | ALBTR-4658-1-W24 | 0 | 10.0 | 0.38 | 2.7 | 2.00 | 0.0074 | 0.029 | 0.043 | 0.081 | 0.042 | 0.030 | 0.85 | |||
NTHL-10 | Northern_Holiday | 1951-09 | 40.2350 | -155.9167 | -5100 | W-25 | 0 | 11.6 | 15.80 | 14.2 | 1.70 | 0.3400 | 0.390 | 0.510 | 0.036 | 0.039 | 0.840 | 40 | 0.41 | Sample analysed was half a nodule (2 cm dia.) taken from manganese crust that constituted the main sample | |
DWHD16 | DOWNWIND-H | 1957-11 | -16.4830 | -146.5500 | -1270 | DWHD16-1-W-26 | 0 | 13.6 | 15.90 | 2.4 | 2.30 | 1.3000 | 0.750 | 0.140 | 0.072 | 0.075 | 1.100 | 180 | 0.62 | Sample 3 x 1.5 x 2.5 cm | |
VSS35D | VERMILION_SEA | 1959-05 | 22.3000 | -107.8000 | -3000 | VSS35D-1-W-29 | 0 | 8.2 | 1.80 | 25.9 | 1.10 | 0.0087 | 0.075 | 0.016 | 0.019 | 0.056 | 0.072 | 1 | 0.40 | Sample analysed was homogeneous core (1 cm dia.) of this nodule and contained less clay material than the outer parts | |
ALBTR-13 | Albatross1899-1900 | 9.9500 | -137.7833 | -4919 | ALBTR-13-2-W30 | 0 | 10.7 | 6.20 | 6.2 | 2.70 | 0.2600 | 1.600 | 1.770 | 0.110 | 0.052 | 1.400 | 85 | 0.70 | Sample analysed was the inner part containing less clay material than the rest of the nodule | ||
MABAH-166 | John_Murray_Expedition | 1934-04 | 6.9167 | 67.1833 | -4793 | MABAH-166-1-W19 | 0 | 13.8 | 18.90 | 8.3 | 1.20 | 0.2100 | 0.230 | 0.120 | 0.048 | 0.058 | 0.360 | 55 | 0.38 | 96626 F (1-81) | Central core. Received in powder form |
MABAH-166 | John_Murray_Expedition | 1934-04 | 6.9167 | 67.1833 | -4793 | MABAH-166-1-W20 | 0 | 13.2 | 17.70 | 7.7 | 1.90 | 0.1600 | 0.730 | 0.270 | 0.059 | 0.060 | 0.360 | 80 | 0.46 | 96626 F (1-81) | Third from outer layer. Received in powder form |
MABAH-166 | John_Murray_Expedition | 1934-04 | 6.9167 | 67.1833 | -4793 | MABAH-166-1-W21 | 0 | 14.7 | 17.00 | 8.4 | 2.10 | 17.0000 | 0.810 | 0.380 | 0.057 | 0.064 | 0.410 | 80 | 0.48 | 96626 F (1-81) | Second outer layer. Received in powder form |
MABAH-166 | John_Murray_Expedition | 1934-04 | 6.9167 | 67.1833 | -4793 | MABAH-166-1-W22 | 0 | 14.2 | 14.30 | 9.5 | 2.20 | 0.1500 | 0.950 | 0.400 | 0.054 | 0.060 | 0.360 | 80 | 0.50 | 96626 F (1-81) | Outer layer. Received in powder form |