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Johnson, Kenneth S; Martin, John (2004): Chemistry measured on water bottle samples at station VertexVStation1. PANGAEA, https://doi.org/10.1594/PANGAEA.194739

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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 (1988): Northeast Pacific iron distributions in relation to phytoplankton productivity. Deep-Sea Research Part A. Oceanographic Research Papers, 35(2), 177-196, https://doi.org/10.1016/0198-0149(88)90035-0
Coverage:
Latitude: 35.810000 * Longitude: -122.560000
Date/Time Start: 1984-06-13T00:00:00 * Date/Time End: 1984-06-13T00:00:00
Minimum DEPTH, water: m * Maximum DEPTH, water: 2000 m
Event(s):
VertexVStation1 * Latitude: 35.810000 * Longitude: -122.560000 * Date/Time: 1984-06-13T00:00:00 * Location: World Ocean * Campaign: compiled data * Method/Device: Go-Flo bottles (GOFLO)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, waterDepth watermGeocode
2Temperature, waterTemp°CMartin, John
3SalinitySalMartin, John
4Iron, dissolvedFe dissnmol/lMartin, JohnElement analyser AAS, graphite furnace, Perkin-Elmer 5000
5Iron, particulateFe partnmol/lMartin, JohnElement analyser AAS, graphite furnace, Perkin-Elmer 5000
6OxygenO2µmol/lMartin, John
7Oxygen, apparent utilizationAOUµmol/lMartin, John
8Phosphate[PO4]3-µmol/lMartin, John
9Nitrate[NO3]-µmol/lMartin, John
10SilicateSi(OH)4µmol/lMartin, John
Size:
167 data points

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