Expedition 347 Scientists (2014): Calculated salinity and elemental ratios of interstitial water of IODP Hole 347-M0061C [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.839773
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Andrén, Thomas; Jørgensen, Bo Barker; Cotterill, Carol; Expedition 347 Scientists (2015): Baltic Sea Paleoenvironment. Proceedings of the IODP, Integrated Ocean Drilling Program, https://doi.org/10.2204/iodp.proc.347.2015
Further details:
Project(s):
Coverage:
Latitude: 62.778700 * Longitude: 18.049700
Date/Time Start: 2013-10-05T07:40:00 * Date/Time End: 2013-10-05T12:00:00
Minimum DEPTH, sediment/rock: 1.35 m * Maximum DEPTH, sediment/rock: 21.15 m
Event(s):
347-M0061C (BSB-10) * Latitude: 62.778700 * Longitude: 18.049700 * Date/Time Start: 2013-10-05T07:40:00 * Date/Time End: 2013-10-05T12:00:00 * Elevation: -87.9 m * IGSN: IBCR0347EHK0001 * Recovery: 23.12 m * Location: Baltic Sea, Angermanaelven River Estuary * Campaign: Exp347 (Baltic Sea Paleoenvironment) * Basis: Greatship Manisha * Comment: Drilling Depth Method (DSF): tag sea floor; Core Depth Method (CSF): let overlap if long. 7 cores, 23.1m drilled
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Expedition 347 Scientists | DSDP/ODP/IODP sample designation | ||
| 2 | Sample type | Samp type | Expedition 347 Scientists | |||
| 3 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 4 | Salinity | Sal | Expedition 347 Scientists | Calculated | Cl-based | |
| 5 | Salinity | Sal | Expedition 347 Scientists | Calculated | Anion-based | |
| 6 | Sodium/Chlorine ratio | Na/Cl | mmol/mol | Expedition 347 Scientists | Calculated | |
| 7 | Calcium/Chlorine ratio | Ca/Cl | mmol/mol | Expedition 347 Scientists | Calculated | |
| 8 | Magnesium/Chlorine ratio | Mg/Cl | mmol/mol | Expedition 347 Scientists | Calculated | |
| 9 | Potassium/Chlorine ratio | K/Cl | mmol/mol | Expedition 347 Scientists | Calculated | |
| 10 | Bromide/Chlorine ratio | Br/Cl | µmol/mol | Expedition 347 Scientists | Calculated | |
| 11 | Boron/Chlorine ratio | B/Cl | µmol/mol | Expedition 347 Scientists | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
120 data points
Data
| 1 Sample label (DSDP/ODP/IODP sample designation) | 2 Samp type | 3 Depth sed [m] | 4 Sal (Cl-based, Calculated) | 5 Sal (Anion-based, Calculated) | 6 Na/Cl [mmol/mol] (Calculated) | 7 Ca/Cl [mmol/mol] (Calculated) | 8 Mg/Cl [mmol/mol] (Calculated) | 9 K/Cl [mmol/mol] (Calculated) | 10 Br/Cl [µmol/mol] (Calculated) | 11 B/Cl [µmol/mol] (Calculated) |
|---|---|---|---|---|---|---|---|---|---|---|
| 347-M0061C-1H-1,135-140 | Rhizon sample | 1.35 | 6.22 | 7.57 | 0.80 | 0.02 | 0.09 | 0.02 | 1.610 | 0.990 |
| 347-M0061C-1H-2,135-140 | Rhizon sample | 2.85 | 6.58 | 9.43 | 0.82 | 0.03 | 0.10 | 0.02 | 1.640 | 1.220 |
| 347-M0061C-2H-1,135-140 | Rhizon sample | 4.65 | 7.42 | 12.07 | 0.99 | 0.04 | 0.13 | 0.03 | 1.640 | 1.440 |
| 347-M0061C-2H-2,135-140 | Rhizon sample | 6.15 | 7.51 | 13.66 | 0.92 | 0.04 | 0.12 | 0.02 | 1.640 | 1.160 |
| 347-M0061C-3H-1,135-140 | Rhizon sample | 9.45 | 7.59 | 17.04 | 0.91 | 0.05 | 0.11 | 0.02 | 1.620 | 1.000 |
| 347-M0061C-4H-1,135-140 | Rhizon sample | 11.25 | 7.85 | 19.10 | 0.92 | 0.10 | 0.12 | 0.02 | 1.590 | 0.500 |
| 347-M0061C-4H-2,125-130 | Rhizon sample | 12.65 | 7.81 | 20.46 | 0.87 | 0.13 | 0.12 | 0.02 | 1.580 | 0.300 |
| 347-M0061C-5H-1,135-140 | Rhizon sample | 14.55 | 7.71 | 22.26 | 0.77 | 0.15 | 0.12 | 0.01 | 1.580 | 0.160 |
| 347-M0061C-5H-2,135-140 | Rhizon sample | 16.05 | 7.78 | 23.83 | 0.72 | 0.16 | 0.12 | 0.01 | 1.590 | 0.110 |
| 347-M0061C-6H-1,135-140 | Rhizon sample | 17.85 | 7.76 | 25.61 | 0.71 | 0.20 | 0.14 | 0.01 | 1.580 | 0.050 |
| 347-M0061C-6H-2,125-130 | Rhizon sample | 19.25 | 7.80 | 27.05 | 0.55 | 0.16 | 0.11 | 0.01 | 1.580 | 0.020 |
| 347-M0061C-7H-1,135-140 | Rhizon sample | 21.15 | 7.90 | 29.05 | 0.59 | 0.21 | 0.13 | 0.01 | 1.570 | 0.020 |