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Earth Observing Laboratory
Field Data Archive

Sediment pore-water dissolved oxygen

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Summary

These data were collected from several Bering Sea Ecosystem Study-Bering Sea Integrated Ecosystem Research Program (BEST-BSIERP) cruises. BEST-BSIERP together are the Bering Sea project. Sediment pore-water dissolved oxygen concentrations were measured using a clark-type oxygen microelectrode (Unisense, Denmark). Depth in the sediment was determined using a micromanipulator. Negative depth indicates the sensor was in the water column. Zero is the sediment-water interface. Positive depth is downward.

The data in this collection were collected during the following cruises: HLY0701, HLY0802, HLY0803, HLY0902, KN195-10, TN249, and TN250 aboard the U.S. Coast Guard Cutter Healy (HLY), UNOLS R/V Knorr (KN), and R/V Thompson (TN).

Data access

  • ORDER data to made available for download

Additional information

Identifier
Versions
  • 1.0 (2011-06-25)
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Related projects
Frequency no set schedule
Language English
Grant Code 0612380
ISO Topic Categories
  • oceans
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Temporal coverage

Begin datetime 2007-04-10 09:00:00
End datetime 2010-07-14 17:00:00

Spatial coverage


Map data from IBCSO, IBCAO, and Global Topography.

Maximum (North) Latitude: 63.00, Minimum (South) Latitude: 55.00
Minimum (West) Longitude: -180.00, Maximum (East) Longitude: -164.00

Primary point of contact information

David H. Shull <david.shull@wwu.edu>

Additional contact information

Citation

Shull, D., Devol, A. 2011. Sediment pore-water dissolved oxygen. Version 1.0. UCAR/NCAR - Earth Observing Laboratory. https://doi.org/10.5065/D6MC8X1Z. Accessed 25 Apr 2025.

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NSF

This material is based upon work supported by the NSF National Center for Atmospheric Research, a major facility sponsored by the U.S. National Science Foundation and managed by the University Corporation for Atmospheric Research. Any opinions, findings and conclusions or recommendations expressed in this material do not necessarily reflect the views of the U.S. National Science Foundation.