Vershinin, Andrey V; Egorov, Alexander V; Rozanov, Alexander G (2009): (Table 1b) Dissolved forms of chemical elements in near-bottom waters and interstitial waters from sediments at Station PSh-6214 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.755608, 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: 55.037783 * Longitude: 19.714033
Minimum DEPTH, sediment/rock: 0.0000 m * Maximum DEPTH, sediment/rock: 0.2150 m
Event(s):
PSh-6214 * Latitude: 55.037783 * Longitude: 19.714033 * Elevation: -72.0 m * 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:
73 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 | 770 | 40 | 150 | 10 | 0.13 | 0.02 | 25.4 | 1.3 | 1.91 | 0.10 |
| 0.0125 | 0.000 | 0.025 | 13800 | 2800 | 300 | 50 | 1.26 | 0.25 | 129.0 | 25.0 | 2.34 | 0.47 | |
| 0.0375 | 0.025 | 0.050 | 13400 | 2700 | 760 | 150 | 0.95 | 0.19 | 247.0 | 49.0 | 25.50 | 5.10 | |
| 0.0750 | 0.050 | 0.100 | 11200 | 2200 | 610 | 120 | 0.79 | 0.16 | 139.0 | 28.0 | 36.40 | 7.30 | |
| 0.1500 | 0.100 | 0.200 | 13200 | 2600 | 2600 | 500 | 1.15 | 0.23 | 139.0 | 28.0 | 5.70 | 1.10 | |
| 0.2150 | 0.200 | 0.230 | 15800 | 3100 | 3000 | 600 | 0.39 | 0.08 | 139.0 | 28.0 | 2.10 | 0.40 |
