Smith, Walker O Jr (2004): Biogenic Silica at niskin bottle station RSBP1995/1996-011496-03 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.140620
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Smith, Walker O Jr; Codispoti, Louis A; Nelson, David M; Manley, T; Buskey, Edward J; Niebauer, H J; Cota, G F (1991): Importance of Phaeocystis blooms in the high-ocean carbon cycle. Nature, 352(6335), 514-516, https://doi.org/10.1038/352514a0
Project(s):
Silicon Cycling in the World Ocean (SINOPS)
Funding:
Coverage:
Latitude: -76.442000 * Longitude: 164.597000
Date/Time Start: 1996-01-14T09:20:00 * Date/Time End: 1996-01-14T09:20:00
Minimum DEPTH, water: 2 m * Maximum DEPTH, water: 150 m
Event(s):
RSBP1995/1996-011496-03 (Station#95-CTD#145) * Latitude: -76.442000 * Longitude: 164.597000 * Date/Time: 1996-01-14T09:20:00 * Location: Ross Sea * Campaign: RossSeaBloomProject1995/1996 (NBP94-06) * Basis: Nathaniel B. Palmer * Method/Device: Bottle, Niskin (NIS)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, water | Depth water | m | Geocode | ||
| 2 | Irradiance | E | % | Smith, Walker O Jr | ||
| 3 | Biogenic silica | bSiO2 | µmol/l | Smith, Walker O Jr | ||
| 4 | Production of biogenic silica | pBSi | nmol/l/h | Smith, Walker O Jr | ||
| 5 | Silicic acid uptake rate, specific | v pSi upt rate | 1/h | Smith, Walker O Jr |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
39 data points
Data
| 1 Depth water [m] | 2 E [%] | 3 bSiO2 [µmol/l] | 4 pBSi [nmol/l/h] | 5 v pSi upt rate [1/h] |
|---|---|---|---|---|
| 2 | 100.0 | 11.627 | 71.793 | 0.006 |
| 4 | 50.0 | 9.949 | 33.918 | 0.003 |
| 9 | 30.0 | 10.175 | 40.553 | 0.004 |
| 13 | 15.0 | 7.695 | 18.315 | 0.002 |
| 22 | 5.0 | 4.141 | 8.912 | 0.002 |
| 31 | 1.0 | 2.601 | 9.536 | 0.004 |
| 47 | 0.1 | 1.319 | 10.809 | 0.008 |
| 60 | 0.0 | 1.481 | 6.478 | 0.004 |
| 80 | 0.0 | 1.083 | 30.383 | 0.028 |
| 100 | 0.944 | |||
| 125 | 0.785 | |||
| 150 | 0.888 |