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Grid DAP Data | Sub- set | Table DAP Data | Make A Graph | W M S | Source Data Files | Acces- sible | Title | Sum- mary | FGDC, ISO, Metadata | Back- ground Info | RSS | E | Institution | Dataset ID |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
set | data | graph | files | public | [Dissolved Nitrous Oxide] - Dissolved N2O concentration and stable isotope/isotopomer composition measurements from R/V Knorr cruise KN192-05 in the South Atlantic subtropical gyre and Benguela upwelling region in 2007 (CoFeMUG project) (Cobalt, Iron and Micro-organisms from the Upwelling zone to the Gyre) | F I M | background | BCO-DMO | bcodmo_dataset_529599 |
Row Type | Variable Name | Attribute Name | Data Type | Value |
---|---|---|---|---|
attribute | NC_GLOBAL | access_formats | String | .htmlTable,.csv,.json,.mat,.nc,.tsv,.esriCsv,.geoJson |
attribute | NC_GLOBAL | acquisition_description | String | Single water samples for N2O analyses were collected from acid-cleaned, Teflon-coated X-Niskin sampling bottles (OceanTest Equipment) of 8-liter capacity deployed on an epoxy-coated rosette (Sea-Bird Electronics) as described in Noble et al. (2012). Immediately after rosette recovery, water samples were collected by twice overfilling 160 ml glass serum bottles (Wheaton prod. no. 223748) from the bottom up using tygon tubing attached to each niskin bottle. A small headspace was introduced into each sample by pipetting 1 ml of sample off the top. The sample was then poisoned with 100 ul of saturated HgCl2 solution and sealed with gray butyl septa (MicroLiter Analytics prod. no. 20-0025) and aluminum crimps. Poisoned samples were stored for several months in the dark at room temperature before analysis. Isotopic analyses of N2O were made using a Finnigan DELTA PLUS XP IRMS calibrated for isotopomer-specific measurements (see Frame & Casciotti (2010) for details) and referenced against injections of a calibrated N2O reference tank (d15Nbulk = 0.31\u2030, SP = -1.2\u2030, d18O = 40.85\u2030 as calibrated by S. Toyoda, Toykyo Tech) with quality control checks against analyses of tropospheric air samples. Bottles were purged with He and N2O was trapped on- line with a custom-built purge and trap system (McIlvin & Casciotti, 2010). The molar amount of N2O was determined from each bottle using a constant linear relationship of m/z 44 peak area to molar quantity of N2O which is 2.15 Vs per nanomole of N2O, then converted to a concentration by dividing the molar amount by the volume of sample extracted (154 ml). The ratios of sample N2O to reference gas N2O values of m/z 31/30, 45/44, and 46/44 were corrected for a small linear dependence of these values on the sample peak area (see McIlvin and Casciotti 2010), with all ratios corrected to a peak area of 20 Vs. For a 160 ml water sample containing 2.2 nmole of N2O (typical of the lowest concentrations in this dataset), the precision of the d18O = \u00b10.25\u2030, d15Nbulk = \u00b10.09\u2030, and SP = \u00b10.33\u2030. Additional details about measurement precision are included in McIlvin & Casciotti (2010). Triplicate samples of tropospheric N2O from Woods Hole, MA had _d15Na = 15.0 \u00b1 0.1\u2030, _d15Nb = \u22121.9 \u00b1 0.1\u2030, d_18O = 44.4 \u00b1 0.2\u2030, _d15Nbulk = 6.5 \u00b1 0.1\u2030, SP = 16.9 \u00b1 0.1\u2030, and m/z 44 peak area = 15.6 \u00b1 0.2 Vs. All cruise data are included here except two measurements with background interference. |
attribute | NC_GLOBAL | awards_0_award_nid | String | 54681 |
attribute | NC_GLOBAL | awards_0_award_number | String | OCE-0452883 |
attribute | NC_GLOBAL | awards_0_data_url | String | http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=0452883 |
attribute | NC_GLOBAL | awards_0_funder_name | String | NSF Division of Ocean Sciences |
attribute | NC_GLOBAL | awards_0_funding_acronym | String | NSF OCE |
attribute | NC_GLOBAL | awards_0_funding_source_nid | String | 355 |
attribute | NC_GLOBAL | awards_0_program_manager | String | Donald L. Rice |
attribute | NC_GLOBAL | awards_0_program_manager_nid | String | 51467 |
attribute | NC_GLOBAL | awards_1_award_nid | String | 55017 |
attribute | NC_GLOBAL | awards_1_award_number | String | OCE-1031271 |
attribute | NC_GLOBAL | awards_1_data_url | String | http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=1031271 |
attribute | NC_GLOBAL | awards_1_funder_name | String | NSF Division of Ocean Sciences |
attribute | NC_GLOBAL | awards_1_funding_acronym | String | NSF OCE |
attribute | NC_GLOBAL | awards_1_funding_source_nid | String | 355 |
attribute | NC_GLOBAL | awards_1_program_manager | String | Donald L. Rice |
attribute | NC_GLOBAL | awards_1_program_manager_nid | String | 51467 |
attribute | NC_GLOBAL | awards_2_award_nid | String | 55159 |
attribute | NC_GLOBAL | awards_2_award_number | String | OCE-0928414 |
attribute | NC_GLOBAL | awards_2_data_url | String | http://nsf.gov/awardsearch/showAward?AWD_ID=0928414&HistoricalAwards=false |
attribute | NC_GLOBAL | awards_2_funder_name | String | NSF Division of Ocean Sciences |
attribute | NC_GLOBAL | awards_2_funding_acronym | String | NSF OCE |
attribute | NC_GLOBAL | awards_2_funding_source_nid | String | 355 |
attribute | NC_GLOBAL | awards_2_program_manager | String | Donald L. Rice |
attribute | NC_GLOBAL | awards_2_program_manager_nid | String | 51467 |
attribute | NC_GLOBAL | awards_3_award_nid | String | 529604 |
attribute | NC_GLOBAL | awards_3_award_number | String | OCE-0752291 |
attribute | NC_GLOBAL | awards_3_data_url | String | http://www.nsf.gov/awardsearch/showAward?AWD_ID=0752291 |
attribute | NC_GLOBAL | awards_3_funder_name | String | NSF Division of Ocean Sciences |
attribute | NC_GLOBAL | awards_3_funding_acronym | String | NSF OCE |
attribute | NC_GLOBAL | awards_3_funding_source_nid | String | 355 |
attribute | NC_GLOBAL | awards_3_program_manager | String | Donald L. Rice |
attribute | NC_GLOBAL | awards_3_program_manager_nid | String | 51467 |
attribute | NC_GLOBAL | cdm_data_type | String | Other |
attribute | NC_GLOBAL | comment | String | Dissolved nitrous oxide and stable isotopes/isotopomers CoFeMUG cruise KN192-05 PI: Karen Casciotti (Stanford) Co-PI: Caitlin Frame (University of Basel) Version: 17 Sept 2014 |
attribute | NC_GLOBAL | Conventions | String | COARDS, CF-1.6, ACDD-1.3 |
attribute | NC_GLOBAL | creator_email | String | info at bco-dmo.org |
attribute | NC_GLOBAL | creator_name | String | BCO-DMO |
attribute | NC_GLOBAL | creator_type | String | institution |
attribute | NC_GLOBAL | creator_url | String | https://www.bco-dmo.org/ |
attribute | NC_GLOBAL | data_source | String | extract_data_as_tsv version 2.3 19 Dec 2019 |
attribute | NC_GLOBAL | date_created | String | 2014-10-03T15:33:32Z |
attribute | NC_GLOBAL | date_modified | String | 2020-03-31T17:27:18Z |
attribute | NC_GLOBAL | defaultDataQuery | String | &time<now |
attribute | NC_GLOBAL | doi | String | 10.26008/1912/bco-dmo.529599.1 |
attribute | NC_GLOBAL | Easternmost_Easting | double | 14.5 |
attribute | NC_GLOBAL | geospatial_lat_max | double | -12.0 |
attribute | NC_GLOBAL | geospatial_lat_min | double | -25.0 |
attribute | NC_GLOBAL | geospatial_lat_units | String | degrees_north |
attribute | NC_GLOBAL | geospatial_lon_max | double | 14.5 |
attribute | NC_GLOBAL | geospatial_lon_min | double | -20.0 |
attribute | NC_GLOBAL | geospatial_lon_units | String | degrees_east |
attribute | NC_GLOBAL | infoUrl | String | https://www.bco-dmo.org/dataset/529599 |
attribute | NC_GLOBAL | institution | String | BCO-DMO |
attribute | NC_GLOBAL | instruments_0_acronym | String | IR Mass Spec |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_description | String | Isotopic analyses of N2O were made using a Finnigan DELTA PLUS XP IRMS calibrated for isotopomer-specific measurements; see Frame & Casciotti (2010) for details. |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_nid | String | 529615 |
attribute | NC_GLOBAL | instruments_0_description | String | 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). |
attribute | NC_GLOBAL | instruments_0_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB16/ |
attribute | NC_GLOBAL | instruments_0_instrument_name | String | Isotope-ratio Mass Spectrometer |
attribute | NC_GLOBAL | instruments_0_instrument_nid | String | 469 |
attribute | NC_GLOBAL | instruments_0_supplied_name | String | Finnigan DELTA PLUS XP IRMS |
attribute | NC_GLOBAL | instruments_1_acronym | String | TM Bottle |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_description | String | Single water samples for N2O analyses were collected from acid-cleaned, Teflon-coated X-Niskin sampling bottles (OceanTest Equipment) of 8-liter capacity deployed on an epoxy-coated rosette (Sea-Bird Electronics). |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_nid | String | 529614 |
attribute | NC_GLOBAL | instruments_1_description | String | Trace metal (TM) clean rosette bottle used for collecting trace metal clean seawater samples. |
attribute | NC_GLOBAL | instruments_1_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/30/ |
attribute | NC_GLOBAL | instruments_1_instrument_name | String | Trace Metal Bottle |
attribute | NC_GLOBAL | instruments_1_instrument_nid | String | 493 |
attribute | NC_GLOBAL | instruments_1_supplied_name | String | Teflon-coated X-Niskin sampling bottles (Ocean Test Equipment) |
attribute | NC_GLOBAL | keywords | String | bco, bco-dmo, biological, chemical, code, cruise, cruise_id, d15, d15Na_N2O, d15Nb_N2O, d15Nbulk_N2O, d18, d18O_N2O, data, dataset, date, date_event, dmo, erddap, ev_code, event, latitude, lon_360, longitude, management, N2O, nbulk, oceanography, office, preliminary, press, SP_N2O, sta |
attribute | NC_GLOBAL | license | String | https://www.bco-dmo.org/dataset/529599/license |
attribute | NC_GLOBAL | metadata_source | String | https://www.bco-dmo.org/api/dataset/529599 |
attribute | NC_GLOBAL | Northernmost_Northing | double | -12.0 |
attribute | NC_GLOBAL | param_mapping | String | {'529599': {'lat': 'flag - latitude', 'press': 'flag - depth', 'lon': 'flag - longitude'}} |
attribute | NC_GLOBAL | parameter_source | String | https://www.bco-dmo.org/mapserver/dataset/529599/parameters |
attribute | NC_GLOBAL | people_0_affiliation | String | Stanford University |
attribute | NC_GLOBAL | people_0_person_name | String | Karen L. Casciotti |
attribute | NC_GLOBAL | people_0_person_nid | String | 50980 |
attribute | NC_GLOBAL | people_0_role | String | Principal Investigator |
attribute | NC_GLOBAL | people_0_role_type | String | originator |
attribute | NC_GLOBAL | people_1_affiliation | String | University of Basel (Universitat Basel) |
attribute | NC_GLOBAL | people_1_person_name | String | Caitlin Frame |
attribute | NC_GLOBAL | people_1_person_nid | String | 529608 |
attribute | NC_GLOBAL | people_1_role | String | Co-Principal Investigator |
attribute | NC_GLOBAL | people_1_role_type | String | originator |
attribute | NC_GLOBAL | people_2_affiliation | String | Stanford University |
attribute | NC_GLOBAL | people_2_person_name | String | Karen L. Casciotti |
attribute | NC_GLOBAL | people_2_person_nid | String | 50980 |
attribute | NC_GLOBAL | people_2_role | String | Contact |
attribute | NC_GLOBAL | people_2_role_type | String | related |
attribute | NC_GLOBAL | people_3_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_3_affiliation_acronym | String | WHOI BCO-DMO |
attribute | NC_GLOBAL | people_3_person_name | String | Shannon Rauch |
attribute | NC_GLOBAL | people_3_person_nid | String | 51498 |
attribute | NC_GLOBAL | people_3_role | String | BCO-DMO Data Manager |
attribute | NC_GLOBAL | people_3_role_type | String | related |
attribute | NC_GLOBAL | project | String | CoFeMUG |
attribute | NC_GLOBAL | projects_0_acronym | String | CoFeMUG |
attribute | NC_GLOBAL | projects_0_description | String | The geochemistries of dissolved cobalt (Co) and iron (Fe) in the oceanic water column share several characteristics such as extremely low concentrations, redox chemistry, low solubility,and utilization as micronutrients by marine microbes. Iron has been the subject of considerable research focus in recent years due to its role in limiting phytoplankton productivity in oceanic and coastal upwelling environments. Cobalt has been much less studied, but recent data show it may be important in influencing primary productivity or phytoplankton community composition in certain geographical areas. The CoFeMUG project predated GEOTRACES, so while it is not formally recognized as a GEOTRACES section, it is considered a GEOTRACES-related project and the CoFeMUG data are GEOTRACES compliant. State-of-the-art geochemical and molecular biological techniques were used to address biogeochemical questions in the South Atlantic, and focus especially on the two trace metals, cobalt and iron. The 27-day cruise in November and December 2007 to the South Atlantic was designed to study cobalt and iron biogeochemistry and focus on four major hypotheses. (1) Large fluxes of labile cobalt are associated with upwelling systems even in Aeolian dominated environments. (2) Cobalt and phosphate show correlations in (and only in) surface waters due to micronutrient utilization and rapid remineralization. The slope of the correlation is dependent on the chemical speciation of cobalt. (3) The absence of Trichodesmium populations in the subtropical and tropical South Atlantic is caused by iron limitation. (4) Based on work from the California and Peru Upwelling regimes, primary productivity in the Benguela upwelling regime off of South West Africa may be iron limited or iron-cobalt colimited. A combination of geochemical and biological/molecular analyses were made across an oligotrophic-upwelling transition to examine how changing metal regimes affect the physiology and growth of the important primary producers Trichodesmium and Synechococcus. CoFeMUG project results are published in: Noble, Abigail E., Carl H. Lamborg, Dan C. Ohnemus, Phoebe J. Lam, Tyler J. Goepfert, Chris I. Measures, Caitlin H. Frame, Karen L. Casciotti, Giacomo R. DiTullio, Joe Jennings, and Mak A. Saito (2012) Basin-scale inputs of cobalt, iron, and manganese from the Benguela-Angola front to the South Atlantic Ocean. Limnology & Oceanography. Vol. 57(4), July 2012. pgs 989-1010. doi:10.4319/lo.2012.57.4.0989 (www.aslo.org/lo/toc/vol_57/issue_4/0989.pdf) |
attribute | NC_GLOBAL | projects_0_end_date | String | 2008-03 |
attribute | NC_GLOBAL | projects_0_geolocation | String | South Atlantic subtropical gyre and Benguela upwelling region |
attribute | NC_GLOBAL | projects_0_name | String | Cobalt, Iron and Micro-organisms from the Upwelling zone to the Gyre |
attribute | NC_GLOBAL | projects_0_project_nid | String | 2067 |
attribute | NC_GLOBAL | projects_0_start_date | String | 2005-03 |
attribute | NC_GLOBAL | publisher_name | String | Biological and Chemical Oceanographic Data Management Office (BCO-DMO) |
attribute | NC_GLOBAL | publisher_type | String | institution |
attribute | NC_GLOBAL | sourceUrl | String | (local files) |
attribute | NC_GLOBAL | Southernmost_Northing | double | -25.0 |
attribute | NC_GLOBAL | standard_name_vocabulary | String | CF Standard Name Table v55 |
attribute | NC_GLOBAL | subsetVariables | String | cruise_id |
attribute | NC_GLOBAL | summary | String | Dissolved N2O concentration and stable isotope/isotopomer composition measurements made from samples from acid-cleaned, Teflon-coated X-Niskin sampling bottles on the CoFeMUG cruise (KN192-05). |
attribute | NC_GLOBAL | title | String | [Dissolved Nitrous Oxide] - Dissolved N2O concentration and stable isotope/isotopomer composition measurements from R/V Knorr cruise KN192-05 in the South Atlantic subtropical gyre and Benguela upwelling region in 2007 (CoFeMUG project) (Cobalt, Iron and Micro-organisms from the Upwelling zone to the Gyre) |
attribute | NC_GLOBAL | version | String | 1 |
attribute | NC_GLOBAL | Westernmost_Easting | double | -20.0 |
attribute | NC_GLOBAL | xml_source | String | osprey2erddap.update_xml() v1.3 |
variable | cruise_id | String | ||
attribute | cruise_id | bcodmo_name | String | cruise_id |
attribute | cruise_id | description | String | Official cruise identifier. |
attribute | cruise_id | long_name | String | Cruise Id |
attribute | cruise_id | units | String | dimensionless |
variable | sta | byte | ||
attribute | sta | _FillValue | byte | 127 |
attribute | sta | actual_range | byte | 5, 27 |
attribute | sta | bcodmo_name | String | sta |
attribute | sta | description | String | Station number. |
attribute | sta | long_name | String | Sta |
attribute | sta | units | String | dimensionless |
variable | latitude | double | ||
attribute | latitude | _CoordinateAxisType | String | Lat |
attribute | latitude | _FillValue | double | NaN |
attribute | latitude | actual_range | double | -25.0, -12.0 |
attribute | latitude | axis | String | Y |
attribute | latitude | bcodmo_name | String | latitude |
attribute | latitude | colorBarMaximum | double | 90.0 |
attribute | latitude | colorBarMinimum | double | -90.0 |
attribute | latitude | description | String | Latitude; North is positive. |
attribute | latitude | ioos_category | String | Location |
attribute | latitude | long_name | String | Latitude |
attribute | latitude | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P09/current/LATX/ |
attribute | latitude | standard_name | String | latitude |
attribute | latitude | units | String | degrees_north |
variable | longitude | double | ||
attribute | longitude | _CoordinateAxisType | String | Lon |
attribute | longitude | _FillValue | double | NaN |
attribute | longitude | actual_range | double | -20.0, 14.5 |
attribute | longitude | axis | String | X |
attribute | longitude | bcodmo_name | String | longitude |
attribute | longitude | colorBarMaximum | double | 180.0 |
attribute | longitude | colorBarMinimum | double | -180.0 |
attribute | longitude | description | String | Longitude; East is positive. Calculated by BCO-DMO from the original PI-provided lon_360 values. |
attribute | longitude | ioos_category | String | Location |
attribute | longitude | long_name | String | Longitude |
attribute | longitude | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P09/current/LONX/ |
attribute | longitude | standard_name | String | longitude |
attribute | longitude | units | String | degrees_east |
variable | lon_360 | float | ||
attribute | lon_360 | _FillValue | float | NaN |
attribute | lon_360 | actual_range | float | 0.0, 357.5 |
attribute | lon_360 | bcodmo_name | String | lon_360 |
attribute | lon_360 | colorBarMaximum | double | 180.0 |
attribute | lon_360 | colorBarMinimum | double | -180.0 |
attribute | lon_360 | description | String | Longitude measured from 0 to 360 degrees. |
attribute | lon_360 | long_name | String | Longitude |
attribute | lon_360 | standard_name | String | longitude |
attribute | lon_360 | units | String | decimal degrees |
variable | press | double | ||
attribute | press | _FillValue | double | NaN |
attribute | press | actual_range | double | 9.0, 5106.0 |
attribute | press | bcodmo_name | String | pressure |
attribute | press | description | String | Pressure. |
attribute | press | long_name | String | Press |
attribute | press | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/PRESPR01/ |
attribute | press | units | String | decibars (db) |
variable | ev_code | String | ||
attribute | ev_code | bcodmo_name | String | event code |
attribute | ev_code | description | String | Event code; type and number of sampling event; matches cruise event log. |
attribute | ev_code | long_name | String | Ev Code |
attribute | ev_code | units | String | dimensionless |
variable | event | int | ||
attribute | event | _FillValue | int | 2147483647 |
attribute | event | actual_range | int | 11220908, 12111150 |
attribute | event | bcodmo_name | String | event |
attribute | event | description | String | Event number from the cruise event log. |
attribute | event | long_name | String | Event |
attribute | event | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/EVTAGFL/ |
attribute | event | units | String | dimensionless |
variable | date_event | int | ||
attribute | date_event | _FillValue | int | 2147483647 |
attribute | date_event | actual_range | int | 20071122, 20071211 |
attribute | date_event | bcodmo_name | String | date |
attribute | date_event | description | String | Year-month-day of the event; added by BCO-DMO from the cruise event log. in the format YYYYmmdd |
attribute | date_event | long_name | String | Date Event |
attribute | date_event | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/ADATAA01/ |
attribute | date_event | units | String | unitless |
variable | N2O | float | ||
attribute | N2O | _FillValue | float | NaN |
attribute | N2O | actual_range | float | 6.8, 49.3 |
attribute | N2O | bcodmo_name | String | Nitrous Oxide |
attribute | N2O | description | String | Dissolved N2O concentration. |
attribute | N2O | long_name | String | N2 O |
attribute | N2O | units | String | nanomoles per liter (nm/L) |
variable | d15Nbulk_N2O | float | ||
attribute | d15Nbulk_N2O | _FillValue | float | NaN |
attribute | d15Nbulk_N2O | actual_range | float | -0.1, 9.1 |
attribute | d15Nbulk_N2O | bcodmo_name | String | unknown |
attribute | d15Nbulk_N2O | description | String | d15Nbulk-N2O = average (bulk) isotope ratio (15N/14N) of both nitrogen atoms in N2O. Calculated as d15Nbulk-N2O = (d15Na-N2O + d15Nb-N2O)/2; referenced to atmospheric N2. |
attribute | d15Nbulk_N2O | long_name | String | D15 Nbulk N2 O |
attribute | d15Nbulk_N2O | units | String | per mil (‰) |
variable | SP_N2O | float | ||
attribute | SP_N2O | _FillValue | float | NaN |
attribute | SP_N2O | actual_range | float | 5.3, 25.2 |
attribute | SP_N2O | bcodmo_name | String | unknown |
attribute | SP_N2O | description | String | SP-N2O = site preference of 15N in N2O. Calculated as (d15Na-N2O - d15Nb-N2O); the difference between d15Na-N2O and d15Nb-N2O. |
attribute | SP_N2O | long_name | String | SP N2 O |
attribute | SP_N2O | units | String | per mil (‰) |
variable | d18O_N2O | float | ||
attribute | d18O_N2O | _FillValue | float | NaN |
attribute | d18O_N2O | actual_range | float | 37.5, 52.2 |
attribute | d18O_N2O | bcodmo_name | String | unknown |
attribute | d18O_N2O | description | String | d18O-N2O = isotope ratio (18O/16O) of oxygen in N2O. Calculated as d18O = ({[18O]/[16O]sample}/{[18O]/[16O]standard} -1) x 1000‰; referenced to VSMOW. |
attribute | d18O_N2O | long_name | String | D18 O N2 O |
attribute | d18O_N2O | units | String | per mil (‰) |
variable | d15Na_N2O | float | ||
attribute | d15Na_N2O | _FillValue | float | NaN |
attribute | d15Na_N2O | actual_range | float | 6.1, 19.8 |
attribute | d15Na_N2O | bcodmo_name | String | unknown |
attribute | d15Na_N2O | description | String | d15Na-N2O = isotope ratio (15N/14N) in the internal nitrogen of N2O; d15Na-N2O = ({[15N]/[14N]a,sample}/{[15N]/[14N]a,standard} -1) x 1000‰; referenced to atmospheric N2 as the standard. |
attribute | d15Na_N2O | long_name | String | D15 Na N2 O |
attribute | d15Na_N2O | units | String | per mil (‰) |
variable | d15Nb_N2O | float | ||
attribute | d15Nb_N2O | _FillValue | float | NaN |
attribute | d15Nb_N2O | actual_range | float | -9.5, 2.1 |
attribute | d15Nb_N2O | bcodmo_name | String | unknown |
attribute | d15Nb_N2O | description | String | d15Nb-N2O = isotope ratio (15N/14N) in the external nitrogen of N2O; d15Nb-N2O = ({[15N]/[14N]b,sample}/{[15N]/[14N]b,standard} -1) x 1000‰; referenced to atmospheric N2 as the standard. |
attribute | d15Nb_N2O | long_name | String | D15 Nb N2 O |
attribute | d15Nb_N2O | units | String | per mil (‰) |
The information in the table above is also available in other file formats (.csv, .htmlTable, .itx, .json, .jsonlCSV1, .jsonlCSV, .jsonlKVP, .mat, .nc, .nccsv, .tsv, .xhtml) via a RESTful web service.