Dubinin, Alexander V (2006): (Table 53) Chemical compositions of residues after different leaching treatments of bottom sediment from Core AKO26-35 [dataset]. P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, PANGAEA, https://doi.org/10.1594/PANGAEA.743894, In supplement to: Dubinin, AV (2006): Geochemistry of Rare-Earth Elements in the Ocean. Nauka Publ. (Moscow): in Russian, 360 pp
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: -29.600000 * Longitude: -149.966700
Minimum DEPTH, sediment/rock: 0.135 m * Maximum DEPTH, sediment/rock: 1.850 m
Event(s):
AKO26-35 * Latitude: -29.600000 * Longitude: -149.966700 * Elevation: -3880.0 m * Campaign: AKO_1970-1982_USSR * Basis: Akademik Korolev * Method/Device: Gravity corer (GC)
Comment:
The method developed and described by R. Chester and M.J. Hughes (1967) can be found here: doi:10.1016/0009-2541(67)90025-3).
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
228 data points
Data
1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Exp treat | 5 La [mg/kg] | 6 Ce [mg/kg] | 7 Pr [mg/kg] | 8 Nd [mg/kg] | 9 Sm [mg/kg] | 10 Eu [mg/kg] | 11 Gd [mg/kg] | 12 Tb [mg/kg] | 13 Dy [mg/kg] | 14 Ho [mg/kg] | 15 Er [mg/kg] | 16 Tm [mg/kg] | 17 Yb [mg/kg] | 18 Lu [mg/kg] | 19 P [%] | 20 Fe [%] | 21 Mn [%] | 22 Al [%] | 23 Ni [%] | 24 Co [%] | 25 Cu [%] | 26 Mn/Fe | 27 Ce/Ce* |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.135 | 0.12 | 0.15 | by 3.5N H2SO4 | 9.15 | 33.0 | 1.43 | 5.48 | 0.97 | 0.34 | 1.02 | 0.14 | 0.97 | 0.17 | 0.46 | 0.07 | 0.52 | 0.06 | 0.024 | 4.97 | 2.00 | 4.13 | 0.045 | 0.035 | 0.024 | 0.400 | 1.93 |
0.135 | 0.12 | 0.15 | according to Chester and Hughes (1967) | 12.70 | 34.5 | 2.86 | 12.00 | 2.62 | 0.78 | 2.68 | 0.42 | 2.50 | 0.54 | 1.55 | 0.26 | 1.38 | 0.21 | 0.067 | 5.07 | 0.03 | 6.12 | <0.001 | 0.009 | 0.018 | 0.006 | 1.25 |
0.225 | 0.20 | 0.25 | by 3.5N H2SO4 | 7.60 | 34.8 | 1.52 | 5.80 | 1.10 | 0.30 | 1.10 | 0.15 | 0.99 | 0.20 | 0.55 | 0.09 | 0.50 | 0.09 | 2.21 | ||||||||
0.225 | 0.20 | 0.25 | according to Chester and Hughes (1967) | 12.50 | 35.2 | 3.17 | 13.00 | 2.98 | 0.86 | 2.83 | 0.39 | 2.24 | 0.45 | 1.25 | 0.21 | 1.68 | 0.20 | 1.22 | ||||||||
0.660 | 0.64 | 0.68 | by 3.5N H2SO4 | 9.32 | 36.0 | 1.91 | 7.16 | 1.39 | 0.35 | 1.53 | 0.22 | 1.40 | 0.28 | 0.84 | 0.10 | 0.79 | 0.12 | 0.042 | 5.65 | 2.67 | 3.63 | 0.048 | 0.044 | 0.028 | 0.470 | 1.85 |
0.660 | 0.64 | 0.68 | according to Chester and Hughes (1967) | 14.30 | 28.4 | 3.77 | 16.10 | 3.31 | 0.93 | 3.76 | 0.49 | 3.41 | 0.76 | 2.25 | 0.30 | 1.82 | 0.32 | 0.117 | 5.78 | 0.03 | 5.21 | 0.010 | 0.003 | 0.018 | 0.005 | 0.84 |
1.625 | 1.60 | 1.65 | by 3.5N H2SO4 | 11.20 | 47.0 | 2.69 | 10.50 | 2.02 | 0.55 | 2.35 | 0.28 | 1.60 | 0.35 | 1.02 | 0.15 | 1.15 | 0.15 | 1.87 | ||||||||
1.625 | 1.60 | 1.65 | according to Chester and Hughes (1967) | 28.10 | 38.4 | 6.95 | 27.90 | 6.49 | 1.58 | 6.77 | 0.93 | 5.52 | 1.19 | 3.43 | 0.49 | 3.47 | 0.45 | 0.60 | ||||||||
1.850 | 1.80 | 1.90 | by 3.5N H2SO4 | 11.00 | 54.1 | 2.51 | 10.80 | 1.88 | 0.48 | 2.29 | 0.36 | 2.05 | 0.37 | 1.30 | 0.20 | 1.37 | 0.19 | 0.129 | 11.00 | 3.15 | 3.35 | 0.057 | 0.048 | 0.043 | 0.290 | 2.24 |
1.850 | 1.80 | 1.90 | according to Chester and Hughes (1967) | 19.10 | 28.4 | 5.22 | 23.00 | 5.33 | 1.49 | 5.95 | 0.90 | 5.57 | 1.14 | 3.64 | 0.47 | 3.31 | 0.45 | 0.334 | 10.60 | 0.04 | 3.63 | 0.019 | 0.008 | 0.037 | 0.004 | 0.62 |