Vershinin, Andrey V; Egorov, Alexander V; Rozanov, Alexander G (2009): (Table 1a) Dissolved forms of chemical elements in near-bottom waters and interstitial waters from sediments at Station PSh-6208 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.755607, In supplement to: Vershinin, AV et al. (2009): The fluxes of dissolved forms of chemical elements in Gdansk Bay of the Baltic Sea: Measurements by means of a lander. Oceanologv (Translated ftom Okeanologiya, 2009, 49(4), 501-507), 49(4), 459-465, https://doi.org/10.1134/S0001437009040031
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Published: 2009 (exact date unknown) • DOI registered: 2011-02-09
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: 55.457433 * Longitude: 19.535117
Minimum DEPTH, sediment/rock: 0.0000 m * Maximum DEPTH, sediment/rock: 0.1750 m
Event(s):
PSh-6208 * Latitude: 55.457433 * Longitude: 19.535117 * Location: Baltic Sea * Campaign: AKU26A * Basis: Akademik Kurchatov * Method/Device: Multiple investigations (MULT)
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
145 data points
Data
| 1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Comment | 5 Mn diva [nmol/l] | 6 Mn std dev [±] | 7 Fe diva [nmol/l] | 8 Fe std dev [±] (ferrous) | 9 Fe3+ [µmol/l] | 10 Fe std dev [±] (ferric) | 11 Si(OH)4 [µmol/l] | 12 Si(OH)4 std dev [±] | 13 [PO4]3- [µmol/l] | 14 [PO4]3- std dev [±] |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 0.0000 | 0.000 | 0.000 | near-bottom water | 4200 | 200 | 2010 | 100 | 0.45 | 0.02 | 28.3 | 1.4 | 3.80 | 0.20 |
| 0.0050 | 0.000 | 0.010 | 5000 | 1000 | 610 | 120 | 0.48 | 0.10 | 141.0 | 25.0 | 4.60 | 0.90 | |
| 0.0150 | 0.010 | 0.020 | 5000 | 1000 | 20 | 5 | 0.04 | 0.01 | 148.0 | 25.0 | 8.30 | 1.70 | |
| 0.0250 | 0.020 | 0.030 | 5400 | 1100 | 20 | 5 | 0.04 | 0.01 | 149.0 | 25.0 | 8.10 | 1.60 | |
| 0.0350 | 0.030 | 0.040 | 6100 | 1200 | 150 | 30 | 0.06 | 0.01 | 147.0 | 25.0 | 2.80 | 0.60 | |
| 0.0450 | 0.040 | 0.050 | 6600 | 1300 | 20 | 5 | 0.04 | 0.01 | 152.0 | 25.0 | 5.70 | 1.10 | |
| 0.0600 | 0.050 | 0.070 | 6600 | 1300 | 460 | 90 | 0.05 | 0.01 | 152.0 | 25.0 | 16.40 | 3.30 | |
| 0.0800 | 0.070 | 0.090 | 6600 | 1300 | 20 | 5 | 0.04 | 0.01 | 152.0 | 25.0 | 17.20 | 3.40 | |
| 0.1000 | 0.090 | 0.110 | 5800 | 1200 | 20 | 5 | 0.04 | 0.01 | 152.0 | 25.0 | 6.60 | 1.30 | |
| 0.1200 | 0.110 | 0.130 | 7400 | 1500 | 20 | 5 | 0.04 | 0.01 | 152.0 | 25.0 | 16.40 | 3.30 | |
| 0.1400 | 0.130 | 0.150 | 9700 | 1900 | 150 | 30 | 0.63 | 0.13 | 151.0 | 25.0 | 16.60 | 3.30 | |
| 0.1750 | 0.150 | 0.200 | 8500 | 1700 | 20 | 5 | 0.04 | 0.01 | 152.0 | 25.0 | 26.00 | 5.20 |
