Gromov, V V (1975): (Table 1) Composition of bottom sediments from the East Pacific [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.758721, Supplement to: Gromov, VV (1975): Adsorption of elements of the iron group by bottom sediments of the Pacific Ocean. Oceanology, 15(1), 40-44
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Abstract:
Adsorption of ion, nickel, cobalt, and manganese from ocean water by calcareous sediments, diatomaceous ooze, hydrogenous sediments, and red clay was studied under close to natural conditions using a tracer method. It was found that hydrogenous sediments selectively remove manganese from seawater. This may be associated with formation of chemical compounds between manganese and sediment material. It was also found that nickel, manganese, and iron exist in the ocean in several ionic and neutral forms. Cobalt typically present in only one ionic form Co(2+).
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 6.044175 * Median Longitude: -113.069583 * South-bound Latitude: -13.650000 * West-bound Longitude: -122.050000 * North-bound Latitude: 23.966700 * East-bound Longitude: -101.200000
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 0.55 m
Event(s):
DM8-515 * Latitude: 23.966700 * Longitude: -121.500000 * Elevation: -4140.0 m * Location: Southeast Pacific * Campaign: DM8 * Basis: Dmitry Mendeleev * Method/Device: Gravity corer (GC)
DM8-521 * Latitude: 8.650000 * Longitude: -122.050000 * Elevation: -5020.0 m * Location: Southeast Pacific * Campaign: DM8 * Basis: Dmitry Mendeleev * Method/Device: Grab (GRAB)
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
68 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Depth sed [m] | 6 Depth top [m] | 7 Depth bot [m] | 8 Sediment | 9 SiO2 [%] | 10 Al2O3 [%] | 11 CaCO3 [%] | 12 MgO [%] | 13 Fe [%] | 14 Mn [%] | 15 Ti [%] | 16 Ni [mg/kg] | 17 Co [mg/kg] | 18 Cu [mg/kg] | 19 Zn [mg/kg] | 20 Cr [mg/kg] | 21 Pb [mg/kg] | 22 V [mg/kg] | 23 SSA [m2/g] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
DM8-570 | -13.6500 | -101.2000 | -4040 | 0.55 | 0.50 | 0.60 | hydrogenous sediment composed mainly of iron-clay aggregates; grains of iron hydroxide present (10%); calcareous material consists largely of foraminifers and coccoliths | 22.0 | 3.7 | 17.0 | 13.5 | 5.40 | 0.25 | 1300 | 100 | 900 | 200 | <10 | <10 | 108 | ||
DM8-524 | 5.2100 | -107.5283 | -3883 | 0.05 | 0.00 | 0.10 | calcareous sediment containing coccoliths and foraminifers, low siliceous (mainly diatoms and radiolarians); about 70% of size fraction <0.01 mm | 6.4 | 0.6 | 83.7 | 0.7 | 0.3 | 0.30 | 0.01 | <100 | <10 | 70 | 20 | <10 | <10 | 20 | |
DM8-521 | 8.6500 | -122.0500 | -5020 | 0.05 | 0.00 | 0.10 | diatomaceous radiolarian clayey ooze with admixture of fine silty iron-managnese grains | 64.0 | 12.0 | 1.4 | 3.6 | 3.9 | 0.35 | 0.40 | 200 | 60 | 500 | 200 | 60 | <10 | 79 | |
DM8-515 | 23.9667 | -121.5000 | -4140 | 0.30 | 0.10 | 0.50 | red clay with nodules and admixture of mica, hornblende, pyroxene, etc. | 58.0 | 25.0 | 2.0 | 3.4 | 5.5 | 0.50 | 0.85 | 200 | 70 | 200 | 100 | 70 | 50 | 120 | 64 |