http://lod.bco-dmo.org/id/dataset/819983
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
2020-08-03
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
Vanadium isotope and elemental concentration analyses of numerous ferromanganese crusts and nodule samples
2020-08-03
publication
2020-08-03
revision
Marine Biological Laboratory/Woods Hole Oceanographic Institution Library (MBLWHOI DLA)
2020-08-13
publication
https://doi.org/10.26008/1912/bco-dmo.819983.1
Jeremy D. Owens
Florida State University
principalInvestigator
Sune G. Nielsen
Woods Hole Oceanographic Institution
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: Owens, J., Nielsen, S. (2020) Vanadium isotope and elemental concentration analyses of numerous ferromanganese crusts and nodule samples. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2020-08-03 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.819983.1 [access date]
Dataset Description: <p>This vanadium isotope and elemental concentration dataset analyzes numerous ferromanganese crusts and nodule samples.</p> Methods and Sampling: <p><strong>Methodology:</strong><br />
Various types of iron (Fe) and manganese (Mn) material, crusts and nodules, were analyzed to determine the fractionation from the starting sewawter value to better understand the oxic sink of vanadium. The Fe-Mn crusts and nodules studied here were collected at 2013 from three seamounts or guyots at the West Pacific Ocean using the Chinese manned submersible Jiaolong during DY125-31 cruise. Samples were from Caiwei Guyot (155°E, 15°N) and Caiqi Guyot (154°E, 15°N) from the Magellan Seamount cluster, and Weiyuan Seamount (154°W, 9°N) from Clarion-Clipperton Fe-Mn Nodule Zone (C-C zone) at water depths of 1720–4420 m, 2000–2400 m, and 5200 m, respectively. The samples studied here were obtained from the surface of the seafloor to avoid the potential diagenetic process that have occurred post burial. Some samples are from the surface The Fe-Mn crusts and nodules studied here were collected at 2013 from three seamounts or guyots at the West Pacific Ocean using the Chinese manned submersible Jiaolong during DY125-31 cruise. Samples were from Caiwei Guyot (155°E, 15°N) and Caiqi Guyot (154°E, 15°N) from the Magellan Seamount cluster, and Weiyuan Seamount (154°W, 9°N) from Clarion-Clipperton Fe-Mn Nodule Zone (C-C zone) at water depths of 1720–4420 m, 2000–2400 m and 5200 m, respectively. The samples studied here were obtained from the surface of the seafloor to avoid the potential diagenetic process that have occurred post burial. All samples from Caiwei Guyot and Caiqi Guyot are Fe-Mn crusts, while samples from Weiyuan Seamount include both Fe-Mn crusts and nodules. Some samples are from the surface layer of the ferromanganese crust to study the spatial variations of V isotope of 'recently' or near modern precipitated ferromanganese crust. Furthermore, some Fe-Mn crust samples were removed perpendicular to growth layers, which best represents a stratigraphic record of ocean chemistry.</p>
<p><strong>Sampling and analytical procedures:</strong><br />
Elemental Quantification: The collected Fe-Mn crust and nodule samples were first cleaned by ultrasonication with deionized water and then dried in an oven at 105°C for six hours. Then samples were powdered using an agate mortar and pestle until the sample passed through a 200 mesh sieve. Prior to powdering, crust samples were cut into layers using a hacksaw with a vertical thickness of 1–3 cm. Nodule samples with diameters of 2–5 cm were cut in half from center prior to powdering. Whole-rock major and trace element measurements of Fe-Mn crusts and nodules were conducted in Guangzhou, China (<a href="http://www.alsglobal.net.cn/" target="_blank">http://www.alsglobal.net.cn/</a>). The sample powders were combined with lithium borate flux and fused in a furnace at 1000°C. The resulting melt was then cooled and dissolved in nitric acid and hydrochloric acid. This solution was then analyzed by Inductively Coupled Plasma Atomic Emission Spectroscopy (ICP-AES) for major elements measurements. For trace element measurements, the powders were digested with a mixture of perchloric, nitric, and hydrofluoric acids, and then dissolved with dilute hydrochloric acid. The prepared solutions were then analyzed by Inductively Coupled Plasma Mass Spectrometry (ICP-MS).</p>
<p>Vanadium Purification: Approximately 10–20 mg of sample powders containing 5–10 mg of V were digested for V isotope analysis. Samples were first treated with aqua regia. After evaporation to dryness, samples were dissolved with a 3:1 (v/v) mixture of concentrated HF and HNO₃ to digest the remaining oxide and silicate phases. Then, samples were dried and further treated with aqua regia and concentrated HNO₃ and dried down in between each step. All the samples were finally dissolved in 1 mL of 1 M HNO₃ for ion-exchange chromatography. Briefly, V was purified with a multistep ion-exchange procedure by coupling cation- and anion-exchange columns. The cation resin AG50W-X12 (200–400 mesh) was applied to remove Fe, Ti, and other main matrix elements (e.g., Al, Ca, Mn, and Cr). Then AG1-X8 (200–400 mesh) chloride-form anion resin was used to further remove residual matrix and isobaric elements (e.g., K, Na, Mg, and trace amount of Cr). The total procedural blank was less than 2 ng, thus is negligible compared with the loaded amount of V (5–10 mg). The V yields of the total chemical procedures are &gt;99%.</p>
<p>Isotope Instrumental Configuration: Vanadium isotopic ratios were measured using a sample-standard bracketing method on a Thermo Scientific Neptune plus MultiCollector Inductively Coupled Plasma-Mass Spectrometer (MC-ICP-MS). Measurements were performed on the flat-topped shoulder on the lower mass side of the overlapping V and molecular interference peaks in medium-resolution mode (resolution &gt; 4000) to resolve all interfering molecular species representing combinations of C, N, O, S, Ar and Cl (such as ³⁶Ar¹⁴N+, ³⁶Ar¹⁶O+, and ³⁸Ar¹⁴N+). Jet sample and Ni X-skimmer cones were used to obtain the highest possible V transmission efficiency. In addition, the amplifiers with 10¹⁰Ω and 10¹¹Ω resistor were applied to monitor ⁵¹V and ⁵⁰V signal, respectively. We applied dry plasma inlet system with Aridus II desolvator (CETAC Technologies).</p>
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1434785 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1434785
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1624895 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1624895
completed
Jeremy D. Owens
Florida State University
850-644-5018
1800 E. Paul Dirac Drive
Tallahassee
FL
32310
USA
jdowens@fsu.edu
pointOfContact
Sune G. Nielsen
Woods Hole Oceanographic Institution
CRPG, CNRS, Université de Lorraine 15 rue Notre Dame des Pauvres
54501 Vandoeuvre lès Nancy
France
sune.nielsen@univ-lorraine.fr
pointOfContact
asNeeded
Dataset Version: 1
Unknown
Site
Location_Name
Latitude
Longitude
Water_Depth
Type
Depth
d51V
two_sd
n
Si_pcnt
Al_pcnt
Mn_pcnt
Fe_pcnt
P_pcnt
Li_ppm
V_ppm
Co_ppm
Ni_ppm
Cu_ppm
Zn_ppm
Mn_Fe_ratio
Thermo Element II Inductively Coupled Plasma Mass Spectrometry ICP-MS
Thermo Neptune multi-collector ICP-MS
Inductively Coupled Plasma Atomic Emission Spectroscopy
theme
None, User defined
site
latitude
longitude
depth
sample type
Vanadium
numb_obs
Silicon
Aluminum
Manganese
Iron
Phosphorus
Lithium
Cobalt
Nickel
Copper
Zinc
weight
featureType
BCO-DMO Standard Parameters
Inductively Coupled Plasma Mass Spectrometer
Inductively Coupled Plasma Mass Spectrometer
Inductively Coupled Plasma Optical Emission Spectrometer
instrument
BCO-DMO Standard Instruments
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.
Fingerprinting and Calibrating Low Oxygen Conditions Using Vanadium Isotopes
https://osprey.bco-dmo.org/project/775701
Fingerprinting and Calibrating Low Oxygen Conditions Using Vanadium Isotopes
<p><em>NSF Award Abstract:</em><br />
Discovering, testing, and developing chemical proxies (relic materials) in marine sediments that reveal how strongly or weakly oxidizing near-surface environmental conditions were in the Earth's geological past are immensely important for understanding interactions between ocean chemistry, biological evolution and extinctions, and climate. To date scientists do not have a proxy for low but non-zero oxygen conditions -- the sort of conditions that are likely to have dominated in biologically important periods of Earth history. In this project, researchers will study the relationship between bottom water oxygen concentration and the isotopes of the trace metal vanadium (V) in a range of oxygen conditions in the modern ocean. Based on pilot data, theoretical calculations and dissolved seawater V concentrations they believe that stable V isotope ratios of core top sediments will correlate systematically over a range of bottom water oxygen conditions. By analyzing these materials, the research team expects to establish the relationship between V isotopes and bottom water oxygen concentrations. Given the importance of chemical proxies to quantify past climate change, the results of this study will be of great importance to the modern and paleoceanographic community, as well as for modelers to better understand a broad range of oxygen variability in Earth history.</p>
<p>Although recent investigations have provided a wealth of information about the redox conditions of the ancient oceans, there is a significant gap in understanding low oxygen conditions throughout Earth history. Therefore, it is important to develop new paleoredox proxies that can provide additional and complementary knowledge about ocean redox conditions during these important periods of Earth history. In this study, scientists will analyze bulk sediments and their organic and ferromanganese mineral fractions to investigate the V isotopic variability within the various sedimentary components. (These samples comprise organic rich to ferromanganese rich sediments due to a range in bottom water oxygen concentrations.) Reconstructing marine low oxygen conditions using vanadium isotopes would fill a void in the paleoredox proxy toolbox. Developing, calibrating, and fingerprinting the V isotopic variability in modern sediments is required to be able to apply vanadium isotopes as an accurate paleoredox proxy.</p>
Vanadium Isotopes
largerWorkCitation
project
eng; USA
oceans
-154
155
9
31.033
2020-08-03
0
BCO-DMO catalogue of parameters from Vanadium isotope and elemental concentration analyses of numerous ferromanganese crusts and nodule 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/819996.rdf
Name: Site
Units: unitless
Description: <p>Site name</p>
http://lod.bco-dmo.org/id/dataset-parameter/819997.rdf
Name: Location_Name
Units: unitless
Description: <p>Location name</p>
http://lod.bco-dmo.org/id/dataset-parameter/819998.rdf
Name: Latitude
Units: decimal degrees North
Description: <p>Latitude</p>
http://lod.bco-dmo.org/id/dataset-parameter/819999.rdf
Name: Longitude
Units: decimal degrees East
Description: <p>Longitude</p>
http://lod.bco-dmo.org/id/dataset-parameter/820000.rdf
Name: Water_Depth
Units: meters (m)
Description: <p>Water depth to the sediment where the sample was collected</p>
http://lod.bco-dmo.org/id/dataset-parameter/820001.rdf
Name: Type
Units: unitless
Description: <p>Material type</p>
http://lod.bco-dmo.org/id/dataset-parameter/820002.rdf
Name: Depth
Units: centimeters (cm)
Description: <p>Bulk is a homogenized sample and numbers are the depth from top</p>
http://lod.bco-dmo.org/id/dataset-parameter/820003.rdf
Name: d51V
Units: per mil (‰)
Description: <p>Measured V isotope value</p>
http://lod.bco-dmo.org/id/dataset-parameter/820004.rdf
Name: two_sd
Units: per mil (‰)
Description: <p>2 standard deviation error from all analyses</p>
http://lod.bco-dmo.org/id/dataset-parameter/820005.rdf
Name: n
Units: unitless
Description: <p>Number of isotope analyses</p>
http://lod.bco-dmo.org/id/dataset-parameter/820006.rdf
Name: Si_pcnt
Units: weight percent
Description: <p>Quantified silicon concentration in weight percent</p>
http://lod.bco-dmo.org/id/dataset-parameter/820007.rdf
Name: Al_pcnt
Units: weight percent
Description: <p>Quantified aluminum concentration in weight percent</p>
http://lod.bco-dmo.org/id/dataset-parameter/820008.rdf
Name: Mn_pcnt
Units: weight percent
Description: <p>Quantified manganese concentration in weight percent</p>
http://lod.bco-dmo.org/id/dataset-parameter/820009.rdf
Name: Fe_pcnt
Units: weight percent
Description: <p>Quantified iron concentration in weight percent</p>
http://lod.bco-dmo.org/id/dataset-parameter/820010.rdf
Name: P_pcnt
Units: weight percent
Description: <p>Quantified phosphorus concentration in weight percent</p>
http://lod.bco-dmo.org/id/dataset-parameter/820011.rdf
Name: Li_ppm
Units: parts per million (ppm)
Description: <p>Quantified lithium concentration in weight percent</p>
http://lod.bco-dmo.org/id/dataset-parameter/820012.rdf
Name: V_ppm
Units: parts per million (ppm)
Description: <p>Quantified vanadium concentration in weight percent</p>
http://lod.bco-dmo.org/id/dataset-parameter/820013.rdf
Name: Co_ppm
Units: parts per million (ppm)
Description: <p>Quantified cobalt concentration in weight percent</p>
http://lod.bco-dmo.org/id/dataset-parameter/820014.rdf
Name: Ni_ppm
Units: parts per million (ppm)
Description: <p>Quantified nickel concentration in weight percent</p>
http://lod.bco-dmo.org/id/dataset-parameter/820015.rdf
Name: Cu_ppm
Units: parts per million (ppm)
Description: <p>Quantified copper concentration in weight percent</p>
http://lod.bco-dmo.org/id/dataset-parameter/820016.rdf
Name: Zn_ppm
Units: parts per million (ppm)
Description: <p>Quantified zinc concentration in weight percent</p>
http://lod.bco-dmo.org/id/dataset-parameter/820017.rdf
Name: Mn_Fe_ratio
Units: unitless (ratio)
Description: <p>Elemental ratio of manganese and iron; both in weight percent</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
5087
https://darchive.mblwhoilibrary.org/bitstream/1912/26066/1/dataset-819983_oxic-sediment-v-isotope-signature__v1.tsv
download
https://doi.org/10.26008/1912/bco-dmo.819983.1
download
onLine
dataset
<p><strong>Methodology:</strong><br />
Various types of iron (Fe) and manganese (Mn) material, crusts and nodules, were analyzed to determine the fractionation from the starting sewawter value to better understand the oxic sink of vanadium. The Fe-Mn crusts and nodules studied here were collected at 2013 from three seamounts or guyots at the West Pacific Ocean using the Chinese manned submersible Jiaolong during DY125-31 cruise. Samples were from Caiwei Guyot (155°E, 15°N) and Caiqi Guyot (154°E, 15°N) from the Magellan Seamount cluster, and Weiyuan Seamount (154°W, 9°N) from Clarion-Clipperton Fe-Mn Nodule Zone (C-C zone) at water depths of 1720–4420 m, 2000–2400 m, and 5200 m, respectively. The samples studied here were obtained from the surface of the seafloor to avoid the potential diagenetic process that have occurred post burial. Some samples are from the surface The Fe-Mn crusts and nodules studied here were collected at 2013 from three seamounts or guyots at the West Pacific Ocean using the Chinese manned submersible Jiaolong during DY125-31 cruise. Samples were from Caiwei Guyot (155°E, 15°N) and Caiqi Guyot (154°E, 15°N) from the Magellan Seamount cluster, and Weiyuan Seamount (154°W, 9°N) from Clarion-Clipperton Fe-Mn Nodule Zone (C-C zone) at water depths of 1720–4420 m, 2000–2400 m and 5200 m, respectively. The samples studied here were obtained from the surface of the seafloor to avoid the potential diagenetic process that have occurred post burial. All samples from Caiwei Guyot and Caiqi Guyot are Fe-Mn crusts, while samples from Weiyuan Seamount include both Fe-Mn crusts and nodules. Some samples are from the surface layer of the ferromanganese crust to study the spatial variations of V isotope of 'recently' or near modern precipitated ferromanganese crust. Furthermore, some Fe-Mn crust samples were removed perpendicular to growth layers, which best represents a stratigraphic record of ocean chemistry.</p>
<p><strong>Sampling and analytical procedures:</strong><br />
Elemental Quantification: The collected Fe-Mn crust and nodule samples were first cleaned by ultrasonication with deionized water and then dried in an oven at 105°C for six hours. Then samples were powdered using an agate mortar and pestle until the sample passed through a 200 mesh sieve. Prior to powdering, crust samples were cut into layers using a hacksaw with a vertical thickness of 1–3 cm. Nodule samples with diameters of 2–5 cm were cut in half from center prior to powdering. Whole-rock major and trace element measurements of Fe-Mn crusts and nodules were conducted in Guangzhou, China (<a href="http://www.alsglobal.net.cn/" target="_blank">http://www.alsglobal.net.cn/</a>). The sample powders were combined with lithium borate flux and fused in a furnace at 1000°C. The resulting melt was then cooled and dissolved in nitric acid and hydrochloric acid. This solution was then analyzed by Inductively Coupled Plasma Atomic Emission Spectroscopy (ICP-AES) for major elements measurements. For trace element measurements, the powders were digested with a mixture of perchloric, nitric, and hydrofluoric acids, and then dissolved with dilute hydrochloric acid. The prepared solutions were then analyzed by Inductively Coupled Plasma Mass Spectrometry (ICP-MS).</p>
<p>Vanadium Purification: Approximately 10–20 mg of sample powders containing 5–10 mg of V were digested for V isotope analysis. Samples were first treated with aqua regia. After evaporation to dryness, samples were dissolved with a 3:1 (v/v) mixture of concentrated HF and HNO₃ to digest the remaining oxide and silicate phases. Then, samples were dried and further treated with aqua regia and concentrated HNO₃ and dried down in between each step. All the samples were finally dissolved in 1 mL of 1 M HNO₃ for ion-exchange chromatography. Briefly, V was purified with a multistep ion-exchange procedure by coupling cation- and anion-exchange columns. The cation resin AG50W-X12 (200–400 mesh) was applied to remove Fe, Ti, and other main matrix elements (e.g., Al, Ca, Mn, and Cr). Then AG1-X8 (200–400 mesh) chloride-form anion resin was used to further remove residual matrix and isobaric elements (e.g., K, Na, Mg, and trace amount of Cr). The total procedural blank was less than 2 ng, thus is negligible compared with the loaded amount of V (5–10 mg). The V yields of the total chemical procedures are &gt;99%.</p>
<p>Isotope Instrumental Configuration: Vanadium isotopic ratios were measured using a sample-standard bracketing method on a Thermo Scientific Neptune plus MultiCollector Inductively Coupled Plasma-Mass Spectrometer (MC-ICP-MS). Measurements were performed on the flat-topped shoulder on the lower mass side of the overlapping V and molecular interference peaks in medium-resolution mode (resolution &gt; 4000) to resolve all interfering molecular species representing combinations of C, N, O, S, Ar and Cl (such as ³⁶Ar¹⁴N+, ³⁶Ar¹⁶O+, and ³⁸Ar¹⁴N+). Jet sample and Ni X-skimmer cones were used to obtain the highest possible V transmission efficiency. In addition, the amplifiers with 10¹⁰Ω and 10¹¹Ω resistor were applied to monitor ⁵¹V and ⁵⁰V signal, respectively. We applied dry plasma inlet system with Aridus II desolvator (CETAC Technologies).</p>
Specified by the Principal Investigator(s)
<p><strong>Data processing:</strong><br />
While the chemical purification quantitatively separates Ti and Cr from V, minor amounts of Ti and Cr in solution can dramatically affect the isotopic value especially for low V concentration measurements. Therefore, analysis of the ⁴⁹Ti/⁵¹V and ⁵³Cr/⁵¹V ratios are needed and should be less than 0.00005 to properly correct for interferences of ⁵⁰Cr and ⁵⁰Ti. We used the procedure described by Nielsen et al. (2011) and Wu et al. (2016) to correct the raw data for any potential interferences. Briefly, 100 ppb Cr and 100 ppb Ti standard solutions were analyzed before each sequence analysis. These were used to correct for the instrumental mass bias factor (β) for Cr and Ti which are calculated with the assumption of the natural abundances of ⁴⁹Ti, ⁵⁰Ti, ⁵⁰Cr and ⁵³Cr in the standard solutions (de Laeter et al., 2003). The ion beam intensities of ⁵⁰Ti and ⁵⁰Cr were then subtracted from the signal mass 50 from the measured ⁴⁹Ti and ⁵³Cr ion beams for each sample with the calculated b values. Samples were measured using sample-standard bracketing. All V isotope measurements from different labs mentioned in this study used the aliquots of the Alfa Aesar (AA) V standard primary made and distributed by Nielsen et al. (2011) and Prytulak et al. (2011) as the bracketing solution, and V isotopic data are reported in standard d notation in per mil relative to AA(δ⁵¹V = ((⁵¹V/⁵⁰V)<sub>sample </sub>/⁵¹V/⁵⁰V)<sub>AA</sub> – 1) × 1,000). The AA V standard solution is defined as δ⁵¹V = 0‰ (Nielsen et al., 2011). Each sample analysis consists of 40 cycles of 4.194 s integrations and was bracketed by double measurements of AA solution on each side to obtain an average value and stability of the instrument for the highest quality control. After evaluation of two samples a solution standard, BDH, was measured to ensure the performance and stability of the analysis on the MC-ICP-MS. The δ⁵¹V values of the nodule standards are -1.57 ± 0.09‰ (2 SD, n = 4, NOD-P) and -0.98 ± 0.01‰ (2 SD, n = 3, NOD-A), within analytical error of previously reported values (NOD-P: -1.65 ± 0.06‰, n = 10 and NOD-A: -0.99 ± 0.10‰, n = 19). The reproducibility of in-house standards and duplicated samples for V isotope analyses are always better than 0.10‰ (2 SD).</p>
<p><strong>BCO-DMO Processing:</strong><br />
- moved site names into a column;<br />
- modified parameter names;<br />
- replaced empty values with 'nd' (no data);<br />
- converted latitude and longitude from degrees and decimal minutes to decimal degrees.</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
Thermo Element II Inductively Coupled Plasma Mass Spectrometry ICP-MS
Thermo Element II Inductively Coupled Plasma Mass Spectrometry ICP-MS
PI Supplied Instrument Name: Thermo Element II Inductively Coupled Plasma Mass Spectrometry ICP-MS Instrument Name: Inductively Coupled Plasma Mass Spectrometer Instrument Short Name:ICP Mass Spec Instrument Description: An ICP Mass Spec is an instrument that passes nebulized samples into an inductively-coupled gas plasma (8-10000 K) where they are atomized and ionized. Ions of specific mass-to-charge ratios are quantified in a quadrupole mass spectrometer. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB15/
Thermo Neptune multi-collector ICP-MS
Thermo Neptune multi-collector ICP-MS
PI Supplied Instrument Name: Thermo Neptune multi-collector ICP-MS Instrument Name: Inductively Coupled Plasma Mass Spectrometer Instrument Short Name:ICP Mass Spec Instrument Description: An ICP Mass Spec is an instrument that passes nebulized samples into an inductively-coupled gas plasma (8-10000 K) where they are atomized and ionized. Ions of specific mass-to-charge ratios are quantified in a quadrupole mass spectrometer. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB15/
Inductively Coupled Plasma Atomic Emission Spectroscopy
Inductively Coupled Plasma Atomic Emission Spectroscopy
PI Supplied Instrument Name: Inductively Coupled Plasma Atomic Emission Spectroscopy Instrument Name: Inductively Coupled Plasma Optical Emission Spectrometer Instrument Short Name:ICP-OES or ICP-AES Instrument Description: Also referred to as an Inductively coupled plasma atomic emission spectroscope (ICP-AES). These instruments pass nebulised samples into an inductively-coupled gas plasma (8-10000 K) where they are atomised and excited. The de-excitation optical emissions at characteristic wavelengths are spectroscopically analysed. It is often used in the detection of trace metals.