Contributors | Affiliation | Role |
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Aguilar-Islas, Ana | University of Alaska Fairbanks (UAF) | Principal Investigator, Contact |
Buck, Clifton S. | Skidaway Institute of Oceanography (SkIO) | Co-Principal Investigator |
Landing, William M. | Florida State University EOAS (FSU - EOAS) | Co-Principal Investigator |
Rauch, Shannon | Woods Hole Oceanographic Institution (WHOI BCO-DMO) | BCO-DMO Data Manager |
This dataset contains acetic acid leachable trace metals from bulk aerosol samples collected during the 2013 US GEOTRACES EPZT section cruise, TN303, on R/V Thomas G. Thompson.
Samples were collected using Florida State University's high vol aerosol sampler (Tisch Environmental TSP TE5170V), located on the 03 deck, forward railings. Samples were collected at the rate of 1 cubic meter per minute on Whatman 41, 47 mm discs (cellulose esters; W41) and were acid cleaned. Methods are described in Morton et al. (2013).
Data have been corrected for field and analytical blank. Reported aerosol trace element concentrations values have been normalized to the volume of air filtered during sample collection. Fractional solubility values are relative to total particulate aerosols. Each sample collection period (n = 17) produced 36 replicate filters. Three of those filters were digested to produce three replicate measurements of total particulate aerosols, and a second set of three filters were leached with acetic acid and a reducing agent to produce three replicate measurements of aerosol leachable trace metals. In the majority of cases, the triplicates were above the field blank value and were in good agreement. Data from the three replicates were averaged and reported along with the standard deviation. Outliers and replicate samples that were below the field blank value were not included in the mean.
Quality flag codes:
Codes follow the SeaDataNet scheme (https://www.geotraces.org/geotraces-quality-flag-policy/)
BDL = below detection limit;
0 = No QC performed;
1 = Good data;
2 = Probably good data;
3 = Probably bad data that is potentially correctable;
4 = Bad data;
5 = Value changed;
6 = Sample < blank;
8 = Interpolated value;
9 = Missing value.
BCO-DMO Processing:
- modified parameter names to conform with BCO-DMO naming conventions;
- replaced missing data values of -999 and -9999 with "nd";
- added date-time columns in ISO8601 format.
Version History:
26 May 2020 (current version) - replaced entire dataset using GEOTRACES DOoR format.
19 Jul 2017 - original version.
File |
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acetic_acid_leachable.csv (Comma Separated Values (.csv), 4.70 KB) MD5:a36d168ae7ff40d2592e555ae341bb5b Primary data file for dataset ID 709276 |
Parameter | Description | Units |
Station_ID | Station number | unitless |
Start_Date_UTC | Sampling date; format: DD/MM/YYYY | unitless |
Start_Time_UTC | Sampling start time; format: hh:mm | unitless |
Start_ISO_DateTime_UTC | Sampling start date and time (UTC) formatted to ISO8601 standard: YYYY-MM-DDThh:mmZ | unitless |
End_Date_UTC | Sampling end date; format: DD/MM/YYYY | unitless |
End_Time_UTC | Sampling end time; format: hh:mm | unitless |
End_ISO_DateTime_UTC | Sampling end date and time (UTC) formatted to ISO8601 standard: YYYY-MM-DDThh:mmZ | unitless |
Start_Latitude | Sampling start latitude | degrees North |
Start_Longitude | Sampling start longitude | degrees East |
End_Latitude | Sampling end latitude | degrees North |
End_Longitude | Sampling end longitude | degrees East |
Event_ID | Event number | unitless |
Sample_ID | GEOTRACES sample number | unitless |
Sample_Depth | Sample depth | meters (m) |
air_vol_total | Total volume of air sampled | cubic meters (m3) |
Al_A_SSLHAC_CONC_HIVOL_88qmbp | Acetic Acid Leachable particulate aerosol Al concentration, average of 3 replicates. Detection limit = 0.19 ng/m3. | nanograms per cubic meter (ng/m3) |
SD1_Al_A_SSLHAC_CONC_HIVOL_88qmbp | One standard deviation of Al_A_SSLHAC_CONC_HIVOL_88qmbp | nanograms per cubic meter (ng/m3) |
Flag_Al_A_SSLHAC_CONC_HIVOL_88qmbp | Quality flag for Al_A_SSLHAC_CONC_HIVOL_88qmbp | unitless |
Cd_A_SSLHAC_CONC_HIVOL_9mt6ne | Acetic Acid Leachable particulate aerosol Cd concentration, average of 3 replicates. Detection limit = 0.0026 ng/m3. | nanograms per cubic meter (ng/m3) |
SD1_Cd_A_SSLHAC_CONC_HIVOL_9mt6ne | One standard deviation of Cd_A_SSLHAC_CONC_HIVOL_9mt6ne | nanograms per cubic meter (ng/m3) |
Flag_Cd_A_SSLHAC_CONC_HIVOL_9mt6ne | Quality flag for Cd_A_SSLHAC_CONC_HIVOL_9mt6ne | unitless |
Cu_A_SSLHAC_CONC_HIVOL_zmurzd | Acetic Acid Leachable particulate aerosol Cu concentration, average of 3 replicates. Detection limit = 0.001 ng/m3. | nanograms per cubic meter (ng/m3) |
SD1_Cu_A_SSLHAC_CONC_HIVOL_zmurzd | One standard deviation of Cu_A_SSLHAC_CONC_HIVOL_zmurzd | nanograms per cubic meter (ng/m3) |
Flag_Cu_A_SSLHAC_CONC_HIVOL_zmurzd | Quality flag for Cu_A_SSLHAC_CONC_HIVOL_zmurzd | unitless |
Fe_A_SSLHAC_CONC_HIVOL_9ytn8o | Acetic Acid Leachable particulate aerosol Fe concentration, average of 3 replicates. Detection limit = 0.72 ng/m3. | nanograms per cubic meter (ng/m3) |
SD1_Fe_A_SSLHAC_CONC_HIVOL_9ytn8o | One standard deviation of Fe_A_SSLHAC_CONC_HIVOL_9ytn8o | nanograms per cubic meter (ng/m3) |
Flag_Fe_A_SSLHAC_CONC_HIVOL_9ytn8o | Quality flag for Fe_A_SSLHAC_CONC_HIVOL_9ytn8o | unitless |
Mn_A_SSLHAC_CONC_HIVOL_wq15vx | Acetic Acid Leachable particulate aerosol Mn concentration, average of 3 replicates. Detection limit = 0.004 ng/m3. | nanograms per cubic meter (ng/m3) |
SD1_Mn_A_SSLHAC_CONC_HIVOL_wq15vx | One standard deviation of Mn_A_SSLHAC_CONC_HIVOL_wq15vx | nanograms per cubic meter (ng/m3) |
Flag_Mn_A_SSLHAC_CONC_HIVOL_wq15vx | Quality flag for Mn_A_SSLHAC_CONC_HIVOL_wq15vx | unitless |
Pb_A_SSLHAC_CONC_HIVOL_nr31qu | Acetic Acid Leachable particulate aerosol Pb concentration, average of 3 replicates. Detection limit = 0.091 ng/m3. | nanograms per cubic meter (ng/m3) |
SD1_Pb_A_SSLHAC_CONC_HIVOL_nr31qu | One standard deviation of Pb_A_SSLHAC_CONC_HIVOL_nr31qu | nanograms per cubic meter (ng/m3) |
Flag_Pb_A_SSLHAC_CONC_HIVOL_nr31qu | Quality flag for Pb_A_SSLHAC_CONC_HIVOL_nr31qu | unitless |
Ti_A_SSLHAC_CONC_HIVOL_bdezwf | Acetic Acid Leachable particulate aerosol Ti concentration, average of 3 replicates. Detection limit = 0.003 ng/m3. | nanograms per cubic meter (ng/m3) |
SD1_Ti_A_SSLHAC_CONC_HIVOL_bdezwf | One standard deviation of Ti_A_SSLHAC_CONC_HIVOL_bdezwf | nanograms per cubic meter (ng/m3) |
Flag_Ti_A_SSLHAC_CONC_HIVOL_bdezwf | Quality flag for Ti_A_SSLHAC_CONC_HIVOL_bdezwf | unitless |
V_A_SSLHAC_CONC_HIVOL_bsytua | Acetic Acid Leachable particulate aerosol V concentration, average of 3 replicates. Detection limit = 0.0002 ng/m3. | nanograms per cubic meter (ng/m3) |
SD1_V_A_SSLHAC_CONC_HIVOL_bsytua | One standard deviation of V_A_SSLHAC_CONC_HIVOL_bsytua | nanograms per cubic meter (ng/m3) |
Flag_V_A_SSLHAC_CONC_HIVOL_bsytua | Quality flag for V_A_SSLHAC_CONC_HIVOL_bsytua | unitless |
Dataset-specific Instrument Name | Tisch Environmental TSP TE5170V |
Generic Instrument Name | Aerosol Sampler |
Generic Instrument Description | A device that collects a sample of aerosol (dry particles or liquid droplets) from the atmosphere. |
Website | |
Platform | R/V Thomas G. Thompson |
Report | |
Start Date | 2013-10-25 |
End Date | 2013-12-20 |
Description | A zonal transect in the eastern tropical South Pacific (ETSP) from Peru to Tahiti as the second cruise of the U.S.GEOTRACES Program. This Pacific section includes a large area characterized by high rates of primary production and particle export in the eastern boundary associated with the Peru Upwelling, a large oxygen minimum zone that is a major global sink for fixed nitrogen, and a large hydrothermal plume arising from the East Pacific Rise. This particular section was selected as a result of open planning workshops in 2007 and 2008, with a final recommendation made by the U.S.GEOTRACES Steering Committee in 2009. It is the first part of a two-stage plan that will include a meridional section of the Pacific from Tahiti to Alaska as a subsequent expedition.
Figure 1. The 2013 GEOTRACES EPZT Cruise Track. [click on the image to view a larger version]
Additional cruise information is available from the Rolling Deck to Repository (R2R): http://www.rvdata.us/catalog/TN303 |
From the NSF Award Abstract
The mission of the International GEOTRACES Program (https://www.geotraces.org/), of which the U.S. chemical oceanography research community is a founding member, is "to identify processes and quantify fluxes that control the distributions of key trace elements and isotopes in the ocean, and to establish the sensitivity of these distributions to changing environmental conditions" (GEOTRACES Science Plan, 2006). In the United States, ocean chemists are currently in the process of organizing a zonal transect in the eastern tropical South Pacific (ETSP) from Peru to Tahiti as the second cruise of the U.S.GEOTRACES Program. This Pacific section includes a large area characterized by high rates of primary production and particle export in the eastern boundary associated with the Peru Upwelling, a large oxygen minimum zone that is a major global sink for fixed nitrogen, and a large hydrothermal plume arising from the East Pacific Rise. This particular section was selected as a result of open planning workshops in 2007 and 2008, with a final recommendation made by the U.S.GEOTRACES Steering Committee in 2009. It is the first part of a two-stage plan that will include a meridional section of the Pacific from Tahiti to Alaska as a subsequent expedition.
This award provides funding for management of the U.S.GEOTRACES Pacific campaign to a team of scientists from the University of Southern California, Old Dominion University, and the Woods Hole Oceanographic Institution. The three co-leaders will provide mission leadership, essential support services, and management structure for acquiring the trace elements and isotopes samples listed as core parameters in the International GEOTRACES Science Plan, plus hydrographic and nutrient data needed by participating investigators. With this support from NSF, the management team will (1) plan and coordinate the 52-day Pacific research cruise described above; (2) obtain representative samples for a wide variety of trace metals of interest using conventional CTD/rosette and GEOTRACES Sampling Systems; (3) acquire conventional JGOFS/WOCE-quality hydrographic data (CTD, transmissometer, fluorometer, oxygen sensor, etc) along with discrete samples for salinity, dissolved oxygen (to 1 uM detection limits), plant pigments, redox tracers such as ammonium and nitrite, and dissolved nutrients at micro- and nanomolar levels; (4) ensure that proper QA/QC protocols are followed and reported, as well as fulfilling all GEOTRACES Intercalibration protocols; (5) prepare and deliver all hydrographic-type data to the GEOTRACES Data Center (and US data centers); and (6) coordinate cruise communications between all participating investigators, including preparation of a hydrographic report/publication.
Broader Impacts: The project is part of an international collaborative program that has forged strong partnerships in the intercalibration and implementation phases that are unprecedented in chemical oceanography. The science product of these collective missions will enhance our ability to understand how to interpret the chemical composition of the ocean, and interpret how climate change will affect ocean chemistry. Partnerships include contributions to the infrastructure of developing nations with overlapping interests in the study area, in this case Peru. There is a strong educational component to the program, with many Ph.D. students carrying out thesis research within the program.
Figure 1. The 2013 GEOTRACES EPZT Cruise Track. [click on the image to view a larger version]
During the 2013 GEOTRACES Eastern Pacific zonal transect, a gradient in aerosol inputs to surface waters will be encountered with higher inputs near Peru and decreasing offshore. This zonal section contrasts sharply to the high aerosol deposition areas found and sampled during the GEOTRACES North Atlantic Zonal Section in the fall of 2010 and 2011. As such, this Pacific section represents a unique opportunity to characterize aerosol and rainfall chemistry in a low deposition environment. Scientists from the University of Alaska and Florida State University plan to collect and characterize aerosol and rainfall samples along this transect, as well as distribute samples to the community. Bulk and size-fractionated aerosol samples collected on a 24 to 48-hour integrated basis and event-based rain samples will be analyzed for trace elements and isotopes (TEIs) to quantify their atmospheric input. The TEIs to be analyzed will be aluminum, vanadium, chromium, manganese, iron, cobalt, nickel, copper, zinc, cadmium, lead, and thorium, as well as the major ions sodium, magnesium, potassium, calcium, nitrate, phosphate, chlorine, and fluorine. Other efforts to be carried out as part of this study include (1) aerosol leaches to determine seawater-soluble and ultrapure-water-soluble TEI fractions: (2) determine the size fractionation and redox speciation of seawater-soluble iron: (3) obtain subsamples of water column samples from other GEOTRACES scientists for the analysis of the TEIs of interest to help interpret the atmospheric deposition data; and (4) collaborate with researchers from other institutions to characterize and constrain estimates of atmospheric deposition. This project will contribute towards the overall goal of the GEOTRACES Program by establishing the range of fractional aerosol solubility and better quantify deposition across the global ocean.
One graduate student from the University of Alaska would be supported and trained as part of this project. Relying on a cruise blog, email, and project website updates, the scientist from the University of Alaska plans to continue her interactions with students in Alaska, Arizona, and Florida and results from the study would be incorporated into class curricula, as well as disseminated via public outreach and web dissemination.
GEOTRACES is a SCOR sponsored program; and funding for program infrastructure development is provided by the U.S. National Science Foundation.
GEOTRACES gained momentum following a special symposium, S02: Biogeochemical cycling of trace elements and isotopes in the ocean and applications to constrain contemporary marine processes (GEOSECS II), at a 2003 Goldschmidt meeting convened in Japan. The GEOSECS II acronym referred to the Geochemical Ocean Section Studies To determine full water column distributions of selected trace elements and isotopes, including their concentration, chemical speciation, and physical form, along a sufficient number of sections in each ocean basin to establish the principal relationships between these distributions and with more traditional hydrographic parameters;
* To evaluate the sources, sinks, and internal cycling of these species and thereby characterize more completely the physical, chemical and biological processes regulating their distributions, and the sensitivity of these processes to global change; and
* To understand the processes that control the concentrations of geochemical species used for proxies of the past environment, both in the water column and in the substrates that reflect the water column.
GEOTRACES will be global in scope, consisting of ocean sections complemented by regional process studies. Sections and process studies will combine fieldwork, laboratory experiments and modelling. Beyond realizing the scientific objectives identified above, a natural outcome of this work will be to build a community of marine scientists who understand the processes regulating trace element cycles sufficiently well to exploit this knowledge reliably in future interdisciplinary studies.
Expand "Projects" below for information about and data resulting from individual US GEOTRACES research projects.
Funding Source | Award |
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NSF Division of Ocean Sciences (NSF OCE) | |
NSF Division of Ocean Sciences (NSF OCE) |