http://lod.bco-dmo.org/id/dataset/644504
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
2016-05-02
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
Fall 2011 - Water Column Samples
2016-04-20
publication
2016-04-20
revision
BCO-DMO Linked Data URI
2016-04-20
creation
http://lod.bco-dmo.org/id/dataset/644504
Samantha B. Joye
University of Georgia
principalInvestigator
Christof Meile
University of Georgia
principalInvestigator
Vladimir Samarkin
University of Georgia
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: Joye, S. B., Meile, C., Samarkin, V. (2016) Fall 2011 - Water Column Samples. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 20 April 2016) Version Date 2016-04-20 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/644504 [access date]
Fall 2011 - Water Column Samples Dataset Description: <p>Siberia Cruise Porewater Samples Collected Sept-Oct, 2011</p> Methods and Sampling: <p>Fall 2011&nbsp; - Water Column Samples</p>
<p><strong>References:</strong><br />
Joye SB, Bowles M.W., Samarkin V.A., Hunter K.S., Niemann H..&nbsp; 2010.&nbsp; Biogeochemical signatures and microbial activity of different cold seep habitats along the Gulf of Mexico lower slope. Deep Sea Research. 10:doi:10.1016/j.dsr2.2010.06.001.</p>
<p>Joye SB, MacDonald I.R., Leifer I., Asper V..&nbsp; 2011.&nbsp; Magnitude and oxidation potential of hydrocarbon gases released from the BP blowout. Nature Geoscience. 4:160-164.</p>
<p>Orcutt B.N., Samarkin V., Boetius A., Elvert M., Joye SB.&nbsp; 2005.&nbsp; Molecular biogeochemistry of sulfate reduction, methanogenesis and the anaerobic oxidation of methane at Gulf of Mexico methane seeps. Geochimica et Cosmochimica Acta. 69:4267-4281.</p>
Funding provided by NSF Division of Polar Programs (NSF PLR) Award Number: PLR-0908788 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0908788
completed
Samantha B. Joye
University of Georgia
706-542-5893
Dept. of Marine Sciences 325 Sanford Drive
Athens
GA
30602
USA
mjoye@uga.edu
pointOfContact
Christof Meile
University of Georgia
(706) 542-6549
110G Marine Sciences Bldg Department of Marine Sciences University of Georgia
Athens
Georgia
30602
United States
cmeile@uga.edu
pointOfContact
Vladimir Samarkin
University of Georgia
(706) 542-3614
Department of Marine Sciences University of Georgia
Athens
Georgia
30602
United States
samarkin@uga.edu
pointOfContact
asNeeded
Dataset Version: 20 April 2016
Unknown
Sample_No
Water_Column_Sample_ID
Station
Latitude
Longitude
Total_Depth
Sample_Depth
Temp
pH
Salinity
DOC
TDN
NOx
NO2
NH4
TDP
PO4
Si
CH4
CH4_MOX_Sheet
MOX
Drill Core
Lachat Instruments FIA+ 8000 Series
Gravity Core
DIONEX ICS-2000
Scintillation Counter
Shimadzu TOC-V
Shimadzu TOC-V with TN Unit
Shimadzu UV-1601
theme
None, User defined
sample identification
station
latitude
longitude
depth
water temperature at measurement depth
pH
salinity
dissolved organic Carbon
Total Dissolved Nitrogen
nitrate plus nitrite
Nitrite
Ammonium
Total Dissolved Phosphorus
reactive phosphorus (PO4)
Silicon
No BCO-DMO term
featureType
BCO-DMO Standard Parameters
Drill Core
Flow Injection Analyzer
Gravity Corer
Ion Chromatograph
Liquid Scintillation Counter
Shimadzu TOC-V Analyzer
Shimadzu TOC-V Analyzer
UV Spectrophotometer-Shimadzu
instrument
BCO-DMO Standard Instruments
ESAS_Fall_2011
service
Deployment Activity
East Siberian Arctic Shelf
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.
Collaborative Research: Degrading offshore permafrost as a source of methane on the East Siberian Arctic Shelf
http://www.joyeresearchgroup.uga.edu/research/climate-change/arctic-ecosystems/degrading-offshore-permafrost-source-methane
Collaborative Research: Degrading offshore permafrost as a source of methane on the East Siberian Arctic Shelf
<p><strong>From the NSF Award ABSTRACT</strong><br />
The Arctic region contains a huge amount of organic carbon, referred to as the Arctic Carbon Hyper Pool, within the Arctic Ocean sedimentary basin. This area has the highest documented rates of coastal sedimentation with annual accumulation rates of about 10 million metric tons organic C per year, which approximately equals the amount of sediment accumulated over the entire pelagic zone of the World Ocean. Due to the specific features of sedimentation and lithogenesis in this area, much of this organic carbon survives decomposition, and is buried within seabed sediments. These sediments are frozen annually or seasonally, representing a substantial reservoir of potentially labile organic carbon. Global warming in the arctic region is predicted to be substantial, and possibly rapid, in next few decades. Upon the melting of permafrost, old stored carbon will be reintroduced into the modern carbon biogeochemical cycle, possibly acting as a strong source of methane to the overlying water and potentially the atmosphere. Additionally, extremely large amounts of more ancient (Pleistocene) methane are trapped as gas hydrates within and beneath the permafrost. This research aims to elucidate the present and future methane flux potential of sediments and permafrost in regions of the East Siberian Arctic Shelf. As a result of global warming, seafloor permafrost along the East Siberian Arctic Shelf may experience a pronounced change in thermal regime. Increased temperature may affect permafrost in several ways, ultimately leading to its degradation and enhanced CH4 release. An international, interdisciplinary research team will determine the distribution and stability of permafrost on the East Siberian Arctic Shelf and evaluate this area as a methane source to the arctic region. Cores from eleven locations will be obtained using dry drilling techniques. Rates of biological methane production and consumption (oxidation) will be quantified in permafrost and sediments at in situ and elevated temperatures. Natural abundance stable carbon and hydrogen isotope measurements will be used to quantify the age and source of methane collected from different sites and depths. These data will be used as input to numerical models, which will be developed to describe the thermodynamic and biogeochemical aspects of permafrost methane dynamics. Using field data and modeling, the current and future potential release of methane from offshore permafrost will be determined and a methane budget for the East Siberian Arctic Shelf will be constructed.</p>
<p><strong>BOOKS/ONE TIME PROCEEDING</strong><br />
Joye, S.B., V.A. Samarkin, N. Shakova, I.<br />
Semiletov, and M.W. Bowles. "Methane dynamics along the East Siberian<br />
Arctic Shelf: sources, sinks, and<br />
fluxes to the atmosphere", 09/01/2011-08/31/2012, "<em>Gordon Research Conference on Polar<br />
Marine Science"</em>, 2011, "2011 GRC-PMC Ventura California".</p>
<p>Finke, N., S. Baer, and S.B. Joye. "Methane production in marine sea ice in<br />
the Chukchi Sea, Barrow, Alaska", 09/01/2011-08/31/2012, "<em>Meeting Abstracts"</em>, 2012, "NASA AbSciCon, Atlanta GA April".</p>
<p>Samarkin, V.A., I. Semelitov, N. Finke, N.<br />
Shakhova, and S. B. Joye. "Methane stable isotope signatures in<br />
waters and sediments of the Laptev Sea<br />
Shelf", 09/01/2011-08/31/2012, "<em>Fall AGU meeting 2012"</em>, 2012, "AGU Meeting Abstracts".</p>
<p><strong>Project Summary</strong></p>
<p><strong>Collaborative Research: Degrading offshore permafrost as a current and potential source of atmospheric methane on the East Siberian Arctic Shelf</strong></p>
<p><strong>Intellectual Merit</strong>: The Arctic region contains a huge amount of organic carbon, referred to commonly as the “Arctic Carbon Hyper Pool”, within the Arctic Ocean sedimentary basin. The Russian Arctic shelf acts as an estuary of the Great Siberian Rivers. This area has the highest documented rates of coastal sedimentation with annual accumulation rates of about 10×106 t Corg yr-1, which approximately equals the amount of sediment accumulated over the entire pelagic zone of the World Ocean. Due to the specific features of sedimentation and lithogenesis in this area, much of this organic carbon survives decomposition, and is buried within seabed sediments. Some of these sediments are seasonally or annually frozen (“offshore” permafrost), representing a substantial reservoir of old but potentially labile organic carbon. Global warming in the Arctic region is predicted to be substantial, and possibly rapid, in the next few decades. Upon permafrost melting, the old carbon stored therein will be reintroduced into the modern carbon biogeochemical cycle, possibly acting as a strong source of methane to the overlying water and potentially the atmosphere. Additionally, extremely large amounts of more ancient (Pleistocene) methane are trapped as gas hydrates within and beneath the permafrost. <strong>T</strong>he proposed work aims to elucidate the present and future methane flux potential of sediments and permafrost in regions of the East Siberian Arctic Shelf. As a result of global warming, seafloor permafrost along the East Siberian Arctic Shelf may experience a pronounced change in thermal regime. Increased temperature may affect permafrost in several ways, ultimately leading</p>
<p>to its degradation and enhanced CH4 release. This international, interdisciplinary research team will determine the distribution and stability of permafrost on the East Siberian Arctic Shelf and evaluate this area as a methane source to the Arctic region. Cores from eleven locations will be obtained using dry drilling techniques. Rates of biological methane production and consumption (oxidation) will be quantified in permafrost and sediments at <em>in situ </em>and elevated temperatures.</p>
<p>Natural abundance carbon (13C and 14C) and hydrogen isotope measurements will be used to quantify the age and source of methane collected from different sites and depths. These data will be used as input to numerical models, which will be developed to describe the thermodynamic and biogeochemical aspects of permafrost methane dynamics. Using field data and modeling, the current and future potential release of methane from offshore permafrost will be determined and a methane budget for the East Siberian Arctic Shelf will be constructed.</p>
<p><strong>Broader impacts: </strong>The proposed work will address a key aspect of the “International Polar Year” request for proposals by advancing the understanding of the coupled physical-geological-biological-chemical system of the Arctic Ocean and providing a predictive model of how the system will respond to environmental change. This work will elucidate the impact of global warming on methane dynamics in the Arctic; in particular, the current and potential capacity of sediments and permafrost to act as a methane source to the overlying water column and atmosphere will be quantified. The scientific team includes PIs with experience working in the Arctic (Semiletov, Shakova, Samarkin) as well as PIs new to this area (Joye, Meile). International collaborators (Grigoriev, Rekant, Kholodov) complete the research team by providing extensive expertise in geology and permafrost drilling in the Arctic. Besides supplying crucial data on CH4 fluxes to global change scientists, this proposal will promote training by supporting students at various levels and by reaching the public and interested scientists through a dedicated website. The project will contribute to the active outreach activities coordinated through the multi-agency Northern Eurasia Earth Science Partnership Initiative (NEESPI). This proposal will also contribute to the collaboration between two major Arctic nations, the United States and Russian Federation. All data generated during this project will be submitted to the BCO-DMO database.</p>
East Siberian Arctic Shelf
largerWorkCitation
project
eng; USA
oceans
East Siberian Arctic Shelf
2016-04-20
East Siberian Arctic Shelf
0
BCO-DMO catalogue of parameters from Fall 2011 - Water Column Samples
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/644514.rdf
Name: Sample_No
Units: dimensionless
Description: <p>Sample No</p>
http://lod.bco-dmo.org/id/dataset-parameter/644515.rdf
Name: Water_Column_Sample_ID
Units: dimensionless
Description: <p>Water Column Sample ID</p>
http://lod.bco-dmo.org/id/dataset-parameter/644516.rdf
Name: Station
Units: dimensionless
Description: <p>Station</p>
http://lod.bco-dmo.org/id/dataset-parameter/644517.rdf
Name: Latitude
Units: decimal degrees
Description: <p>Station latitude (South is negative)</p>
http://lod.bco-dmo.org/id/dataset-parameter/644518.rdf
Name: Longitude
Units: decimal degrees
Description: <p>Station longitude (West is negative)</p>
http://lod.bco-dmo.org/id/dataset-parameter/644519.rdf
Name: Total_Depth
Units: meters
Description: <p>Total_Depth</p>
http://lod.bco-dmo.org/id/dataset-parameter/644520.rdf
Name: Sample_Depth
Units: meters
Description: <p>Sample_Depth</p>
http://lod.bco-dmo.org/id/dataset-parameter/644521.rdf
Name: Temp
Units: °C
Description: <p>Temp</p>
http://lod.bco-dmo.org/id/dataset-parameter/644522.rdf
Name: pH
Units: pH units
Description: <p>pH</p>
http://lod.bco-dmo.org/id/dataset-parameter/644523.rdf
Name: Salinity
Units: PSU
Description: <p>Salinity</p>
http://lod.bco-dmo.org/id/dataset-parameter/644524.rdf
Name: DOC
Units: uM
Description: <p>DOC</p>
http://lod.bco-dmo.org/id/dataset-parameter/644525.rdf
Name: TDN
Units: uM
Description: <p>TDN</p>
http://lod.bco-dmo.org/id/dataset-parameter/644526.rdf
Name: NOx
Units: uM
Description: <p>NOx (Nitrate + Nitrite)</p>
http://lod.bco-dmo.org/id/dataset-parameter/644527.rdf
Name: NO2
Units: uM
Description: <p>NO2</p>
http://lod.bco-dmo.org/id/dataset-parameter/644528.rdf
Name: NH4
Units: uM
Description: <p>NH4</p>
http://lod.bco-dmo.org/id/dataset-parameter/644529.rdf
Name: TDP
Units: uM
Description: <p>TDP</p>
http://lod.bco-dmo.org/id/dataset-parameter/644530.rdf
Name: PO4
Units: uM
Description: <p>PO4</p>
http://lod.bco-dmo.org/id/dataset-parameter/644531.rdf
Name: Si
Units: uM
Description: <p>Si</p>
http://lod.bco-dmo.org/id/dataset-parameter/644532.rdf
Name: CH4
Units: nM
Description: <p>CH4</p>
http://lod.bco-dmo.org/id/dataset-parameter/644533.rdf
Name: CH4_MOX_Sheet
Units: nM
Description: <p>CH4 (MOX Sheet)</p>
http://lod.bco-dmo.org/id/dataset-parameter/644534.rdf
Name: MOX
Units: (tbd)
Description: <p>MOX</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
11776
https://datadocs.bco-dmo.org/file/XYYPGjmIMyqvw2/Fall2011_Water_Column.csv
Fall2011_Water_Column.csv
Primary data file for dataset ID 644504
download
https://osprey.bco-dmo.org/dataset/644504/data/download
download
onLine
dataset
<p>Fall 2011&nbsp; - Water Column Samples</p>
<p><strong>References:</strong><br />
Joye SB, Bowles M.W., Samarkin V.A., Hunter K.S., Niemann H..&nbsp; 2010.&nbsp; Biogeochemical signatures and microbial activity of different cold seep habitats along the Gulf of Mexico lower slope. Deep Sea Research. 10:doi:10.1016/j.dsr2.2010.06.001.</p>
<p>Joye SB, MacDonald I.R., Leifer I., Asper V..&nbsp; 2011.&nbsp; Magnitude and oxidation potential of hydrocarbon gases released from the BP blowout. Nature Geoscience. 4:160-164.</p>
<p>Orcutt B.N., Samarkin V., Boetius A., Elvert M., Joye SB.&nbsp; 2005.&nbsp; Molecular biogeochemistry of sulfate reduction, methanogenesis and the anaerobic oxidation of methane at Gulf of Mexico methane seeps. Geochimica et Cosmochimica Acta. 69:4267-4281.</p>
Specified by the Principal Investigator(s)
<p><strong>BCO-DMO Processing Notes</strong><br />
- Generated from original file "00908788_Joye_Fall-2011_Data-Summary.xlsx", Sheet: "Water Column" contributed by Samantha Joye<br />
- Parameter names edited to conform to BCO-DMO naming convention found at <a href="http://usjgofs.whoi.edu/naming-guidelines.html" target="_blank">Choosing Parameter Name</a><br />
- "nd" (no data) inserted into blank cells<br />
- blank rows removed<br />
- "B.D.L." converted to "BDL" (periods removed) to avoid potential data errors downstream<br />
- "N.S." converted to "NS" (periods removed) to avoid potential data errors downstream and for consistency</p>
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
Drill Core
Drill Core
PI Supplied Instrument Name: Drill Core Instrument Name: Drill Core Instrument Short Name:Drill Core Instrument Description: A core drill is a drill specifically designed to remove a cylinder of material, much like a hole saw. The material left inside the drill bit is referred to as the core.
Core drills are used frequently in mineral exploration where the coring may be several hundred to several thousand feet in length. The core samples are recovered and examined by geologists for mineral percentages and stratigraphic contact points. This gives exploration companies the information necessary to begin or abandon mining operations in a particular area.
Lachat Instruments FIA+ 8000 Series
Lachat Instruments FIA+ 8000 Series
PI Supplied Instrument Name: Lachat Instruments FIA+ 8000 Series PI Supplied Instrument Description:Porewater samples collected for:
NOx (Nitrate + Nitrite)
Nitrite
Orthophosphate
Reactive Silicate
Analytical Method: Flow Injection Autoanalyzer
Instrument: Lachat Instruments FIA+ 8000 Series
Method Reference(s):
Lachat Instruments FIA 8000 Autoanalyzer Method 31-107-04-1-A
Lachat Instruments FIA 8000 Autoanalyzer Method 31-115-01-1-H
Lachat Instruments FIA 8000 Autoanalyzer Method 31-114-27-1-D Instrument Name: Flow Injection Analyzer Instrument Short Name:FIA Instrument Description: An instrument that performs flow injection analysis. Flow injection analysis (FIA) is an approach to chemical analysis that is accomplished by injecting a plug of sample into a flowing carrier stream. FIA is an automated method in which a sample is injected into a continuous flow of a carrier solution that mixes with other continuously flowing solutions before reaching a detector. Precision is dramatically increased when FIA is used instead of manual injections and as a result very specific FIA systems have been developed for a wide array of analytical techniques. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB36/
Gravity Core
Gravity Core
PI Supplied Instrument Name: Gravity Core Instrument Name: Gravity Corer Instrument Short Name:Gravity Corer Instrument Description: The gravity corer allows researchers to sample sediment layers at the bottom of lakes or oceans. The coring device is deployed from the ship and gravity carries it to the seafloor. (http://www.whoi.edu/instruments/viewInstrument.do?id=1079). Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/51/
DIONEX ICS-2000
DIONEX ICS-2000
PI Supplied Instrument Name: DIONEX ICS-2000 PI Supplied Instrument Description:Porewater samples collected for: Anions (Sulfate + Chloride)
Analytical Method: Ion Chromatography
Instrument: DIONEX ICS-2000
Method Reference: DIONEX Application Note 154: Determination of Inorganic Anions in Environmental Waters Using a Hydroxide-Selective Column Instrument Name: Ion Chromatograph Instrument Short Name:Ion Chromatograph Instrument Description: Ion chromatography is a form of liquid chromatography that measures concentrations of ionic species by separating them based on their interaction with a resin. Ionic species separate differently depending on species type and size. Ion chromatographs are able to measure concentrations of major anions, such as fluoride, chloride, nitrate, nitrite, and sulfate, as well as major cations such as lithium, sodium, ammonium, potassium, calcium, and magnesium in the parts-per-billion (ppb) range. (from http://serc.carleton.edu/microbelife/research_methods/biogeochemical/ic.html)
Scintillation Counter
Scintillation Counter
PI Supplied Instrument Name: Scintillation Counter PI Supplied Instrument Description:Porewater samples collected for: Anaerobic Methane Oxidation
Analytical Method: Sediment incubations with 14CH4
Instrument: Scintillation Counter
Method Reference: Orcutt, B., et al. 2005. Molecular biogeochemistry of sulfate reduction, methanogenesis and the anaerobic oxidation of methane at Gulf of Mexico methane seeps. GCA Vol. 69, No. 17, pp. 4267–4281 Instrument Name: Liquid Scintillation Counter Instrument Short Name:LSC Instrument Description: Liquid scintillation counting is an analytical technique which is defined by the incorporation of the radiolabeled analyte into uniform distribution with a liquid chemical medium capable of converting the kinetic energy of nuclear emissions into light energy. Although the liquid scintillation counter is a sophisticated laboratory counting system used to quantify the activity of particulate emitting (ß and a) radioactive samples, it can also detect the auger electrons emitted from 51Cr and 125I samples.
Liquid scintillation counters are instruments assaying alpha and beta radiation by quantitative detection of visible light produced by the passage of rays or particles through a suitable scintillant incorporated into the sample. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB21/
Shimadzu TOC-V
Shimadzu TOC-V
PI Supplied Instrument Name: Shimadzu TOC-V PI Supplied Instrument Description:Porewater samples collected for: Dissolved Organic Carbon
Analytical Method: High temperature combustion
Instrument: Shimadzu TOC-V
Method Reference: http://www.pangaea.de/Projects/JGOFS/Methods/chap16.html Instrument Name: Shimadzu TOC-V Analyzer Instrument Short Name:Shimadzu TOC-V Instrument Description: A Shimadzu TOC-V Analyzer measures DOC by high temperature combustion method. Community Standard Description: http://onto.nerc.ac.uk/CAST/124
Shimadzu TOC-V with TN Unit
Shimadzu TOC-V with TN Unit
PI Supplied Instrument Name: Shimadzu TOC-V with TN Unit PI Supplied Instrument Description:Porewater samples collected for: Total Dissolved Nitrogen
Analytical Method: High temperature combustion/Chemiluminescence
Instrument: Shimadzu TOC-V with TN Unit
Method Reference: Pan et al., Simultaneous Determination of Dissolved Organic Carbon and Total Dissolved Nitrogen on a Coupled High-Temperature Combustion Total Organic Carbon-Nitrogen Chemiluminescence Detection (HTC TOC-NCD) System. Journal of Automated Methods & Management in Chemistry, 2005 (2005), no. 4, 240–246 Instrument Name: Shimadzu TOC-V Analyzer Instrument Short Name:Shimadzu TOC-V Instrument Description: A Shimadzu TOC-V Analyzer measures DOC by high temperature combustion method. Community Standard Description: http://onto.nerc.ac.uk/CAST/124
Shimadzu UV-1601
Shimadzu UV-1601
PI Supplied Instrument Name: Shimadzu UV-1601 PI Supplied Instrument Description:Porewater samples collected for: Total Dissolved Phosphorus and Ammonium
Analytical Method: Spectrophotometry
Instrument: Shimadzu UV-1601
Method Reference:
Solorzano, L., and Sharp, J. H. 1980. Determination of total dissolved phosphorus and particulate phosphorus in natural waters. Limnol. Oceanogr. 25: 754-758.
Solorzano, L. 1969. Determination of ammonia in natural waters by the phenolhypochlorite method. Limnol. Oceanogr. 14: 799-801 Instrument Name: UV Spectrophotometer-Shimadzu Instrument Short Name:UV Spectrophotometer-Shimadzu Instrument Description: The Shimadzu UV Spectrophotometer is manufactured by Shimadzu Scientific Instruments (ssi.shimadzu.com). Shimadzu manufacturers several models of spectrophotometer; refer to dataset for make/model information. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB20/
Deployment: ESAS_Fall_2011
ESAS_Fall_2011
shoreside East Siberian Arctic Shelf
shoreside
ESAS_Fall_2011
Samantha B. Joye
University of Georgia
shoreside East Siberian Arctic Shelf
shoreside