HLY-04-03 Sedimentary Water Fluxes of O2, TCO2 and Dissolved Silica [Christensen, J. P.]

Sediment water fluxes of dissolved oxygen, nitrogen gas, total carbon dioxide (TCO2), and dissolved silicate were measured on incubated sediment cores collected on the northern Alaskan outer continental shelf and continental slope during July 2004 and August 2004. The methods are described, and the resulting fluxes are presented.

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Temporal Range

  • Begin:  2004-07-16T00:00:00Z
    End:  2004-08-26T23:59:59Z

Keywords

Resource Type dataset
Temporal Range Begin 2004-07-16T00:00:00Z
Temporal Range End 2004-08-26T23:59:59Z
Temporal Resolution N/A
Bounding Box North Lat 80.00000
Bounding Box South Lat 60.00000
Bounding Box West Long -180.00000
Bounding Box East Long -130.00000
Spatial Representation grid
Spatial Resolution N/A
Related Links N/A
Additional Information N/A
Resource Format PDF: Portable Document Format (application/pdf)
Standardized Resource Format PDF
Asset Size 1 MB
Legal Constraints

none
Access Constraints none
Software Implementation Language N/A

Resource Support Name EOL Data Support
Resource Support Email datahelp@eol.ucar.edu
Resource Support Organization UCAR/NCAR - Earth Observing Laboratory
Distributor UCAR/NCAR - Earth Observing Laboratory
Metadata Contact Name EOL Data Support
Metadata Contact Email datahelp@eol.ucar.edu
Metadata Contact Organization UCAR/NCAR - Earth Observing Laboratory

Author John P. Christensen
Publisher UCAR/NCAR - Earth Observing Laboratory
Publication Date 2007-11-05T14:54:55
Digital Object Identifier (DOI) https://doi.org/10.5065/D6XK8CN8
Alternate Identifier 62.258
Resource Version 1.0
Topic Category oceans
Progress completed
Metadata Date 2024-12-26T23:52:39Z
Metadata Record Identifier edu.ucar.eol::62.258
Metadata Language eng; USA
Suggested Citation John P. Christensen. (2007). HLY-04-03 Sedimentary Water Fluxes of O2, TCO2 and Dissolved Silica [Christensen, J. P.]. 1.0. UCAR/NCAR - Earth Observing Laboratory. https://doi.org/10.5065/D6XK8CN8. Accessed 13 February 2025.

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