Smith, Walker O Jr (2004): Biogenic Silica at niskin bottle station RSBP1995/1996-011296-03 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.140624
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: -76.519000 * Longitude: 167.228000
Date/Time Start: 1996-01-12T05:02:00 * Date/Time End: 1996-01-12T05:02:00
Minimum DEPTH, water: 0 m * Maximum DEPTH, water: 150 m
Event(s):
RSBP1995/1996-011296-03 (Station#86-CTD#132) * Latitude: -76.519000 * Longitude: 167.228000 * Date/Time: 1996-01-12T05:02:00 * 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] |
---|---|---|---|---|
0 | 100.0 | 4.545 | 22.527 | 0.005 |
3 | 50.0 | 5.208 | 28.113 | 0.005 |
5 | 30.0 | 5.309 | 18.779 | 0.004 |
8 | 15.0 | 7.919 | 31.650 | 0.004 |
13 | 5.0 | 10.250 | 34.618 | 0.003 |
20 | 1.0 | 9.863 | 28.396 | 0.003 |
30 | 0.1 | 3.927 | 5.631 | 0.001 |
50 | 0.0 | 1.392 | 0.147 | 0.000 |
75 | 0.0 | 0.729 | 0.005 | 0.000 |
100 | 0.449 | |||
125 | 0.404 | |||
150 | 0.364 |