http://lod.bco-dmo.org/id/dataset/2576
eng; USA
utf8
dataset
Highest level of data collection, from a common set of sensors or instrumentation, usually within the same research project
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
2010-08-10
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
Gross and integrated gross oxygen productivity from R/V Atlantis II cruise AII-119-4 in the North Atlantic in 1989 (U.S. JGOFS NABE project)
1995-06-15
publication
1995-06-15
revision
BCO-DMO Linked Data URI
1995-06-15
creation
http://lod.bco-dmo.org/id/dataset/2576
Dr Michael L. Bender
University of Rhode Island
principalInvestigator
Dr J. Kiddon
University of Rhode Island
principalInvestigator
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
publisher
Cite this dataset as: Bender, M. L., Kiddon, J. (1995) Gross and integrated gross oxygen productivity from R/V Atlantis II cruise AII-119-4 in the North Atlantic in 1989 (U.S. JGOFS NABE project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version June 15, 1995) Version Date 1995-06-15 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/2576 [access date]
Gross and Integrated Gross Oxygen Productivity Methods and Sampling: <pre>
<b>PI:</b> Michael Bender and J. Kiddon
<b>of:</b> University of Rhode Island
<b>dataset:</b> Gross and Integrated Gross Oxygen Productivity
<b>dates:</b> April 29, 1989 to May 7, 1989
<b>location:</b> N: 46.8 S: 46.4 W: -20.2 E: -19
<b>project/cruise:</b> North Atlantic Bloom Experiment/Atlantis II 119, leg 4
<b>ship:</b> Atlantis II
sta=station number, each day cycles a new station number
gross_integ_prod=Integrated O-18 Gross O2 Production,
units=mmoles o2/m2/day
depth=sample depth, units=meters
gross_o2=O-18 Gross O2 Production, units=umoles O2/L/14hr
</pre>
<h3>Methodology: J. Kiddon, M.L. Bender; URI O-18 Gross O2 Production</h3>
<b>units: umoles O2/L/14 hr<br>
North Atlantic Bloom Experiment<br>
Atlantis II Cruise 119 Leg 4<br>
<br>
</b>
Seawater samples were spiked with H2O enriched in O-18, such that the
18/16 oxygen mass ratio in the sample water was about twice the natural
level. Gross production during a 14 hour bottle incubation generates O2
with the same enriched ratio, thereby enhancing the 18/16 ratio in the large
original dissolved O2 pool. The tagged O2 mixes with the large O2 pool before
being respired, thereby minimizing changes in the isotopic composition of
the measured O2 pool associated with respiration. Thus, the O-18 enrichment
of the dissolved O2 is taken to be a proportional measure of gross production.<br>
<br>
Water samples were drawn before dawn, spiked with 0.2 ml of H2O(18) and
incubated in 100 ml quartz bottles for 14 daylight hrs at the depth of collection.
A drifting buoy was used for sample deployment. The incubated samples, as
well as unincubated samples from each depth were processed to strip and
collect dissolved gases. This stripping process was accomplished by introducing
approximately 50 ml. of seawater into an evacuated two chamber container;
the degassed water remained in a lower chamber and the stripped gases rose
to an upper glass ampoule. The ampoule was flame sealed and returned to
the lab where the 18/16 ratio of the dissolved O2 was measured with an isotope
ratio mass spectrometer as the per mil difference relative to a laboratory
standard (referred to as 'del' measurements). <br>
<br>
The gross O2 production, denoted [O2]p, was calculated as: [O2]p = {[(del)f
- (del)i]/[(del)p - (del)f]}*[O2]i (eqn 1) The parameters (del)i and (del)f
are the 'del' values of the dissolved O2 measured respectively before and
after incubation. (del)p is the isotopic composition of the O2 produced
during the incubation, calculated knowing the volumes (V) of the H2O(18)
spike and the sample, the mole fraction of O-18 in the spike (0.980) and
the mole fraction of O-18 in natural seawater (0.002). That is, (del)p =
{[(X)incub/(X)ref] - 1}*1000, where (X)incub is the mole fraction of O-18
in the spiked sample water, itself calculated as: (Vspike/Vbottle)*0.978
+ 0.002; and (X)ref is the separately determined O-18 mole fraction in the
laboratory standard. [O2]i in equation 1 is the initial O2 concentration,
determined via Winkler titration by the Oceanographic Data facility. Equation
1 may be derived from a more intuitive equation which expresses the final
isotopic composition (del)f as a weighted average of the isotopic compositions
of the initial O2 and the O2 added during production: (del)f = {[O2]i*(del)i
+ [O2]p*(del)p}/{[O2]i + [O2]p}.
<p>
</p><h3>Integrated gross O2 production</h3>
<b>units: mmoles O2/m2/day<br>
Leg 4<br>
<br>
</b>Integrated values of productivity were calculated using the histogram
method. The euphotic region (surface to the 1% light level, Knudson et al.)
was divided into intervals of uniform productivity associated with O-18
gross production measurements. The summation interval was defined as the
depth interval bounded by the two mid points of three adjacent sampling
depths. For example, if depths 4, 12, 20 and 30 meters were sampled, the
productivity measured at 20m was taken to represent the interval 16 to 25
meters. The productivity of the shallowest sample represents the interval
from the surface to the mid point with the next deepest sample, i.e., from
0 to 8 meters. The deepest sample represents the interval from the last
mid point to the 1% light level.
<p>
</p><h3>Net O2 Production</h3>
<b>units: umoles O2/L/24 hr<br>
Leg 4<br>
<br>
</b>Net O2 production was determined as the difference in the measured dissolved
O2 concentrations of sea water, measured before and after a 24 hour light/dark
incubation by Winkler titrations. High precision in the Winkler determinations,
+/- 0.1% umole O2/L, was achieved both by using an automated titrator (Radiometer,
model ABU93) and by averaging four replicate measurements for each water
sample.<br>
<br>
Eight replicate water samples were drawn into quartz bottles from a Go-Flo
flask containing water collected from the euphotic region before dawn (sample
volumes about 100 ml, known to 0.01ml). Winkler titrations were performed
on four of the replicates immediately, and the results averaged to establish
the initial O2 concentration. The remaining four samples were incubated
for 14 daylight hours at the depth of collection (attached to a drifting
buoy), and further incubated for 10 night hours in a darkened, ship board
incubator, maintained at constant temperature by flowing surface water.
Winkler titrations were then performed on the incubated samples and the
results averaged. Net production was calculated as the difference between
the final and initial O2 concentrations.
<p>
</p><h3>Integrated net O2 production</h3>
<b>units: mmoles O2/m2/day<br>
Leg 4<br>
<br>
</b>Integrated values of net O2 productivity were calculated using the histogram
method. The summation intervals were defined as described above for the
integrated gross production, e.g., with boundaries set midway between sampled
depths. Productivity was integrated over the euphotic region, to the 1%
light level (Knudson et al.). In cases where data was sparse (stations 19
and 20 and, in general, for depths near the 1% light level), the net productivity
was augmented using computed values of respiration rates and extrapolated
gross O2 productivities: net prod = gross prod - 24 * resp rate.
<p>
</p><dl> Reference:
<dt> Knudson, C. W.S. Chamberlin and J. Marra (1989)
</dt><dd>Primary production and irradiance data for U.S. JGOFS (Leg 4) Atlantis
II (Cruise 112.4) Technical report LDGO-89.4. Lamont-Doherty Geological
Observatory, Palisades, N.Y.
</dd></dl>
Funding provided by National Science Foundation (NSF) Award Number: unknown NABE NSF
completed
Dr Michael L. Bender
University of Rhode Island
M48 Guyot Hall
Princeton
NJ
08544
USA
bender@princeton.edu
pointOfContact
Dr J. Kiddon
University of Rhode Island
USA
pointOfContact
asNeeded
Dataset Version: June 15, 1995
Unknown
year
date
sta
lat
lon
gross_integ_prod
depth
gross_o2
Drifter Buoy
GO-FLO Bottle
Isotope-ratio Mass Spectrometer
Quartz Bottle
Winkler Oxygen Titrator
theme
None, User defined
year
No BCO-DMO term
latitude
longitude
depth
featureType
BCO-DMO Standard Parameters
Drifter Buoy
GO-FLO Bottle
Isotope-ratio Mass Spectrometer
Light-Dark Bottle
Winkler Oxygen Titrator
instrument
BCO-DMO Standard Instruments
AII-119-4
service
Deployment Activity
U.S. JGOFS North Atlantic
place
Locations
otherRestrictions
otherRestrictions
Access Constraints: none. Use Constraints: Please follow guidelines at: http://www.bco-dmo.org/terms-use Distribution liability: Under no circumstances shall BCO-DMO be liable for any direct, incidental, special, consequential, indirect, or punitive damages that result from the use of, or the inability to use, the materials in this data submission. If you are dissatisfied with any materials in this data submission your sole and exclusive remedy is to discontinue use.
U.S. Joint Global Ocean Flux Study
http://usjgofs.whoi.edu/
U.S. Joint Global Ocean Flux Study
The United States Joint Global Ocean Flux Study was a national component of international JGOFS and an integral part of global climate change research.
The U.S. launched the Joint Global Ocean Flux Study (JGOFS) in the late 1980s to study the ocean carbon cycle. An ambitious goal was set to understand the controls on the concentrations and fluxes of carbon and associated nutrients in the ocean. A new field of ocean biogeochemistry emerged with an emphasis on quality measurements of carbon system parameters and interdisciplinary field studies of the biological, chemical and physical process which control the ocean carbon cycle. As we studied ocean biogeochemistry, we learned that our simple views of carbon uptake and transport were severely limited, and a new "wave" of ocean science was born. U.S. JGOFS has been supported primarily by the U.S. National Science Foundation in collaboration with the National Oceanic and Atmospheric Administration, the National Aeronautics and Space Administration, the Department of Energy and the Office of Naval Research. U.S. JGOFS, ended in 2005 with the conclusion of the Synthesis and Modeling Project (SMP).
U.S. JGOFS
largerWorkCitation
program
U.S. JGOFS North Atlantic Bloom Experiment
http://usjgofs.whoi.edu/research/nabe.html
U.S. JGOFS North Atlantic Bloom Experiment
<p>One of the first major activities of JGOFS was a multinational pilot project, North Atlantic Bloom Experiment (NABE), carried out along longitude 20° West in 1989 through 1991. The United States participated in 1989 only, with the April deployment of two sediment trap arrays at 48° and 34° North. Three process-oriented cruises where conducted, April through July 1989, from R/V <em>Atlantis II</em> and R/V <em>Endeavor</em> focusing on sites at 46° and 59° North. Coordination of the NABE process-study cruises was supported by NSF-OCE award # 8814229. Ancillary sea surface mapping and AXBT profiling data were collected from NASA's P3 aircraft for a series of one day flights, April through June 1989.</p>
<p>A detailed description of NABE and the initial synthesis of the complete program data collection efforts appear in: Topical Studies in Oceanography, JGOFS: The North Atlantic Bloom Experiment (1993), Deep-Sea Research II, Volume 40 No. 1/2.</p>
<p>The U.S. JGOFS Data management office compiled a preliminary NABE data report of U.S. activities: Slagle, R. and G. Heimerdinger, 1991. U.S. Joint Global Ocean Flux Study, North Atlantic Bloom Experiment, Process Study Data Report P-1, April-July 1989. NODC/U.S. JGOFS Data Management Office, Woods Hole Oceanographic Institution, 315 pp. (out of print).</p>
NABE
largerWorkCitation
project
eng; USA
oceans
U.S. JGOFS North Atlantic
1995-06-15
North Atlantic
0
BCO-DMO catalogue of parameters from Gross and integrated gross oxygen productivity from R/V Atlantis II cruise AII-119-4 in the North Atlantic in 1989 (U.S. JGOFS NABE project)
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
http://lod.bco-dmo.org/id/dataset-parameter/10552.rdf
Name: year
Units: YYYY
Description: <p>year, reported as YYYY</p>
http://lod.bco-dmo.org/id/dataset-parameter/10553.rdf
Name: date
Units: MMDD
Description: <p>date, reported as MMDD</p>
http://lod.bco-dmo.org/id/dataset-parameter/10554.rdf
Name: sta
Units: dimensionless
Description: <p>station number, from event log</p>
http://lod.bco-dmo.org/id/dataset-parameter/10555.rdf
Name: lat
Units: decimal degrees
Description: <p>latitude, minus = south</p>
http://lod.bco-dmo.org/id/dataset-parameter/10556.rdf
Name: lon
Units: decimal degrees
Description: <p>longitude, minus = west</p>
http://lod.bco-dmo.org/id/dataset-parameter/10557.rdf
Name: gross_integ_prod
Units: millimoles O2/m2/day
Description: <p>integrated O-18 gross O2 production to the 1% light level</p>
http://lod.bco-dmo.org/id/dataset-parameter/10558.rdf
Name: depth
Units: meters
Description: <p>sample depth</p>
http://lod.bco-dmo.org/id/dataset-parameter/10559.rdf
Name: gross_o2
Units: micromoles O2/liter/14hours
Description: <p>O-18 gross O2 production</p>
GB/NERC/BODC > British Oceanographic Data Centre, Natural Environment Research Council, United Kingdom
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
2083
https://datadocs.bco-dmo.org/file/l880yozszzLmKy/ox18.csv
ox18.csv
Primary data file for dataset ID 2576
download
https://osprey.bco-dmo.org/dataset/2576/data/download
download
onLine
dataset
<pre>
<b>PI:</b> Michael Bender and J. Kiddon
<b>of:</b> University of Rhode Island
<b>dataset:</b> Gross and Integrated Gross Oxygen Productivity
<b>dates:</b> April 29, 1989 to May 7, 1989
<b>location:</b> N: 46.8 S: 46.4 W: -20.2 E: -19
<b>project/cruise:</b> North Atlantic Bloom Experiment/Atlantis II 119, leg 4
<b>ship:</b> Atlantis II
sta=station number, each day cycles a new station number
gross_integ_prod=Integrated O-18 Gross O2 Production,
units=mmoles o2/m2/day
depth=sample depth, units=meters
gross_o2=O-18 Gross O2 Production, units=umoles O2/L/14hr
</pre>
<h3>Methodology: J. Kiddon, M.L. Bender; URI O-18 Gross O2 Production</h3>
<b>units: umoles O2/L/14 hr<br>
North Atlantic Bloom Experiment<br>
Atlantis II Cruise 119 Leg 4<br>
<br>
</b>
Seawater samples were spiked with H2O enriched in O-18, such that the
18/16 oxygen mass ratio in the sample water was about twice the natural
level. Gross production during a 14 hour bottle incubation generates O2
with the same enriched ratio, thereby enhancing the 18/16 ratio in the large
original dissolved O2 pool. The tagged O2 mixes with the large O2 pool before
being respired, thereby minimizing changes in the isotopic composition of
the measured O2 pool associated with respiration. Thus, the O-18 enrichment
of the dissolved O2 is taken to be a proportional measure of gross production.<br>
<br>
Water samples were drawn before dawn, spiked with 0.2 ml of H2O(18) and
incubated in 100 ml quartz bottles for 14 daylight hrs at the depth of collection.
A drifting buoy was used for sample deployment. The incubated samples, as
well as unincubated samples from each depth were processed to strip and
collect dissolved gases. This stripping process was accomplished by introducing
approximately 50 ml. of seawater into an evacuated two chamber container;
the degassed water remained in a lower chamber and the stripped gases rose
to an upper glass ampoule. The ampoule was flame sealed and returned to
the lab where the 18/16 ratio of the dissolved O2 was measured with an isotope
ratio mass spectrometer as the per mil difference relative to a laboratory
standard (referred to as 'del' measurements). <br>
<br>
The gross O2 production, denoted [O2]p, was calculated as: [O2]p = {[(del)f
- (del)i]/[(del)p - (del)f]}*[O2]i (eqn 1) The parameters (del)i and (del)f
are the 'del' values of the dissolved O2 measured respectively before and
after incubation. (del)p is the isotopic composition of the O2 produced
during the incubation, calculated knowing the volumes (V) of the H2O(18)
spike and the sample, the mole fraction of O-18 in the spike (0.980) and
the mole fraction of O-18 in natural seawater (0.002). That is, (del)p =
{[(X)incub/(X)ref] - 1}*1000, where (X)incub is the mole fraction of O-18
in the spiked sample water, itself calculated as: (Vspike/Vbottle)*0.978
+ 0.002; and (X)ref is the separately determined O-18 mole fraction in the
laboratory standard. [O2]i in equation 1 is the initial O2 concentration,
determined via Winkler titration by the Oceanographic Data facility. Equation
1 may be derived from a more intuitive equation which expresses the final
isotopic composition (del)f as a weighted average of the isotopic compositions
of the initial O2 and the O2 added during production: (del)f = {[O2]i*(del)i
+ [O2]p*(del)p}/{[O2]i + [O2]p}.
<p>
</p><h3>Integrated gross O2 production</h3>
<b>units: mmoles O2/m2/day<br>
Leg 4<br>
<br>
</b>Integrated values of productivity were calculated using the histogram
method. The euphotic region (surface to the 1% light level, Knudson et al.)
was divided into intervals of uniform productivity associated with O-18
gross production measurements. The summation interval was defined as the
depth interval bounded by the two mid points of three adjacent sampling
depths. For example, if depths 4, 12, 20 and 30 meters were sampled, the
productivity measured at 20m was taken to represent the interval 16 to 25
meters. The productivity of the shallowest sample represents the interval
from the surface to the mid point with the next deepest sample, i.e., from
0 to 8 meters. The deepest sample represents the interval from the last
mid point to the 1% light level.
<p>
</p><h3>Net O2 Production</h3>
<b>units: umoles O2/L/24 hr<br>
Leg 4<br>
<br>
</b>Net O2 production was determined as the difference in the measured dissolved
O2 concentrations of sea water, measured before and after a 24 hour light/dark
incubation by Winkler titrations. High precision in the Winkler determinations,
+/- 0.1% umole O2/L, was achieved both by using an automated titrator (Radiometer,
model ABU93) and by averaging four replicate measurements for each water
sample.<br>
<br>
Eight replicate water samples were drawn into quartz bottles from a Go-Flo
flask containing water collected from the euphotic region before dawn (sample
volumes about 100 ml, known to 0.01ml). Winkler titrations were performed
on four of the replicates immediately, and the results averaged to establish
the initial O2 concentration. The remaining four samples were incubated
for 14 daylight hours at the depth of collection (attached to a drifting
buoy), and further incubated for 10 night hours in a darkened, ship board
incubator, maintained at constant temperature by flowing surface water.
Winkler titrations were then performed on the incubated samples and the
results averaged. Net production was calculated as the difference between
the final and initial O2 concentrations.
<p>
</p><h3>Integrated net O2 production</h3>
<b>units: mmoles O2/m2/day<br>
Leg 4<br>
<br>
</b>Integrated values of net O2 productivity were calculated using the histogram
method. The summation intervals were defined as described above for the
integrated gross production, e.g., with boundaries set midway between sampled
depths. Productivity was integrated over the euphotic region, to the 1%
light level (Knudson et al.). In cases where data was sparse (stations 19
and 20 and, in general, for depths near the 1% light level), the net productivity
was augmented using computed values of respiration rates and extrapolated
gross O2 productivities: net prod = gross prod - 24 * resp rate.
<p>
</p><dl> Reference:
<dt> Knudson, C. W.S. Chamberlin and J. Marra (1989)
</dt><dd>Primary production and irradiance data for U.S. JGOFS (Leg 4) Atlantis
II (Cruise 112.4) Technical report LDGO-89.4. Lamont-Doherty Geological
Observatory, Palisades, N.Y.
</dd></dl>
Specified by the Principal Investigator(s)
asNeeded
7.x-1.1
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
Drifter Buoy
Drifter Buoy
PI Supplied Instrument Name: Drifter Buoy PI Supplied Instrument Description:Used to obtain samples. Instrument Name: Drifter Buoy Instrument Short Name: Instrument Description: Drifting buoys are free drifting platforms with a float or buoy that keep the drifter at the surface and underwater sails or socks that catch the current. These instruments sit at the surface of the ocean and are transported via near-surface ocean currents. They are not fixed to the ocean bottom, therefore they "drift" with the currents. For this reason, these instruments are referred to as drifters, or drifting buoys.
The surface float contains sensors that measure different parameters, such as sea surface temperature, barometric pressure, salinity, wave height, etc. Data collected from these sensors are transmitted to satellites passing overhead, which are then relayed to land-based data centers.
definition sources: https://mmisw.org/ont/ioos/platform/drifting_buoy and https://www.aoml.noaa.gov/phod/gdp/faq.php#drifter1
GO-FLO Bottle
GO-FLO Bottle
PI Supplied Instrument Name: GO-FLO Bottle PI Supplied Instrument Description:samples were drawn from GO-FLO bottles, fixed and then redeployed on a drifter buoy for incubation Instrument Name: GO-FLO Bottle Instrument Short Name:GO-FLO Instrument Description: GO-FLO bottle cast used to collect water samples for pigment, nutrient, plankton, etc. The GO-FLO sampling bottle is specially designed to avoid sample contamination at the surface, internal spring contamination, loss of sample on deck (internal seals), and exchange of water from different depths. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/30/
Isotope-ratio Mass Spectrometer
Isotope-ratio Mass Spectrometer
PI Supplied Instrument Name: Isotope-ratio Mass Spectrometer PI Supplied Instrument Description:An isotope ratio mass spectrometer was used to measure the 18/16 ratio of the dissolved O2. Instrument Name: Isotope-ratio Mass Spectrometer Instrument Short Name:IR Mass Spec; IRMS Instrument Description: The Isotope-ratio Mass Spectrometer is a particular type of mass spectrometer used to measure the relative abundance of isotopes in a given sample (e.g. VG Prism II Isotope Ratio Mass-Spectrometer). Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB16/
Quartz Bottle
Quartz Bottle
PI Supplied Instrument Name: Quartz Bottle PI Supplied Instrument Description:100 ml quartz bottles were used to store samples which spiked with 0.2 ml of H2O(18) for 14 daylight hrs at the depth of collection. Instrument Name: Light-Dark Bottle Instrument Short Name:Light-Dark Bottle Instrument Description: The light/dark bottle is a way of measuring primary production by comparing before and after concentrations of dissolved oxygen. Bottles containing seawater samples with phytoplankton are incubated for a predetermined period of time under light and dark conditions. Incubation is preferably carried out in situ, at the depth from which the samples were collected. Alternatively, the light and dark bottles are incubated in a water trough on deck, and neutral density filters are used to approximate the light conditions at the collection depth.Rates of net and gross photosynthesis and respiration can be determined from measurements of dissolved oxygen concentration in the sample bottles. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/82/
Winkler Oxygen Titrator
Winkler Oxygen Titrator
PI Supplied Instrument Name: Winkler Oxygen Titrator Instrument Name: Winkler Oxygen Titrator Instrument Short Name:Winkler Titrator Instrument Description: A Winkler Oxygen Titration system is used for determining concentration of dissolved oxygen in seawater. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB12/
Cruise: AII-119-4
AII-119-4
Community Standard Description
International Council for the Exploration of the Sea
R/V Atlantis II
vessel
AII-119-4
John F. Marra
Lamont-Doherty Earth Observatory
Community Standard Description
International Council for the Exploration of the Sea
R/V Atlantis II
vessel