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Johnson, Kenneth S; Martin, John (2004): Chemistry measured on water bottle samples at station DrakePassage1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.194727

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Related to:
Johnson, Kenneth S; Gordon, R Michael; Coale, Kenneth H (1997): What controls dissolved iron in the world ocean? Marine Chemistry, 57(3-4), 137-162, https://doi.org/10.1016/S0304-4203(97)00043-1
Martin, J H; Gordon, R Michael; Fitzwater, Steve (1990): Iron in Antarctic waters. Nature, 345(6271), 156-158, https://doi.org/10.1038/345156a0
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3970141: Silicon Cycling in the World Ocean
Coverage:
Latitude: -60.800000 * Longitude: -63.400000
Date/Time Start: 1989-03-28T00:00:00 * Date/Time End: 1989-03-28T00:00:00
Minimum DEPTH, water: 30 m * Maximum DEPTH, water: 1400 m
Event(s):
DrakePassage1 * Latitude: -60.800000 * Longitude: -63.400000 * Date/Time: 1989-03-28T00:00:00 * Location: World Ocean * Campaign: compiled data * Method/Device: Go-Flo bottles (GOFLO)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, waterDepth watermGeocode
Temperature, waterTemp°CMartin, John
SalinitySalMartin, John
Iron, dissolvedFe dissnmol/lMartin, JohnElement analyser AAS, graphite furnace, Perkin-Elmer 5000
OxygenO2µmol/lMartin, John
Oxygen, apparent utilizationAOUµmol/lMartin, John
Phosphate[PO4]3-µmol/lMartin, John
Nitrate[NO3]-µmol/lMartin, John
SilicateSi(OH)4µmol/lMartin, John
Size:
40 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Depth water [m]

Temp [°C]

Sal

Fe diss [nmol/l]

O2 [µmol/l]

AOU [µmol/l]

[PO4]3- [µmol/l]

[NO3]- [µmol/l]

Si(OH)4 [µmol/l]
302.9733.800.164314131.7824.89
110-0.3433.930.102341152.1229.326
3001.9134.400.267253812.5435.165
5502.1434.590.4101102222.5535.490
14001.6534.720.7791122242.2830.3101