http://lod.bco-dmo.org/id/dataset/905278
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
2023-07-31
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
Total alkalinity and dissolved inorganic carbon data measured during the pH internal consistency experiment.
2023-07-31
publication
2023-07-31
revision
Marine Biological Laboratory/Woods Hole Oceanographic Institution Library (MBLWHOI DLA)
2023-08-02
publication
https://doi.org/10.26008/1912/bco-dmo.905278.1
Ryan Woosley
Massachusetts Institute of Technology
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: Woosley, R. (2023) Total alkalinity and dissolved inorganic carbon data measured during the pH internal consistency experiment. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2023-07-31 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.905278.1 [access date]
Experimental total alkalinity and disolved inorganic carbon data Dataset Description: Methods and Sampling: <p>Oligotrophic Atlantic surface seawater was collected from 39° 46.406′ N and 70° 53.065′ W on October 10, 2019.</p>
<p>The surface seawater was modified to five different salinities and 5 different pCO2 values for a total of 25 batches. Salinity was modified through dilution or evaporation. pCO2 was modified by bubbling CO2 gas of different pCO2 concentrations (balance air).</p>
<p>The water was then bottled and sealed into 250 mL borosilicate glass bottles following SOPs (Dickson et al. 2007). Each batch consisted of 44 bottles.</p>
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1923312 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1923312
completed
Ryan Woosley
Massachusetts Institute of Technology
617-253-1984
77 Massachusetts Ave Bldg. 54-1414
Cambridge
MA
02139
USA
rwoosley@mit.edu
pointOfContact
asNeeded
Dataset Version: 1
Unknown
Batch
Practical_Salinity
meas_TA
meas_DIC
theme
None, User defined
sample identification
salinity
total alkalinity (TA)
dissolved inorganic Carbon
featureType
BCO-DMO Standard Parameters
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.
Improving Accuracy and Precision of Marine Inorganic Carbon Measurements
https://osprey.bco-dmo.org/project/813194
Improving Accuracy and Precision of Marine Inorganic Carbon Measurements
<p><em>NSF Award Abstract:</em><br />
The oceans absorb about one third of the CO2 humans release into the atmosphere from the burning of fossil fuels and other activities. While ocean uptake of CO2 slows its rate of increase in the atmosphere, it comes with costs for the oceans and the organisms that live there. Once in seawater, CO2 reacts with water to produce bicarbonate and hydrogen ions. The increase in hydrogen ions lowers the pH in a process called ocean acidification. Not all areas of the ocean are affected equally. The solubility of CO2 is greater in the cold waters of the Arctic making them more prone to ocean acidification. However, due to the low temperatures and low salinities in the Arctic, the uncertainties in pH values are much larger there than for the other oceans. This project evaluates pH at low temperatures and salinities, and develops best practice recommendations to improve the ability to compare measurements among laboratory groups and studies and reduce overall uncertainty in the measurements. The project provides training for an undergraduate student and promotes awareness of ocean acidification through public outreach.</p>
<p>Having highly accurate and precise measurements are important for monitoring changes to pH and CO2 uptake through time and the effects on marine life. In order to improve pH measurements for polar waters, several different experiments will be conducted. The temperature dependence of pH will be determined from 30˚C to near freezing for low salinity waters. The results will be compared to current chemical models to quantify offsets and biases. Recommendations will be made for the best physical chemical model to use for low temperature and salinity seawater. Moreover, pH is measured spectrophotometrically using an indicator dye. Preparation and calibration of the indictor is important to standardize studies across space and time and ensure comparability. Indicator quality is essential for detecting ocean acidification, but its stability is currently unknown. If the dye degrades after production, biases or artifacts in pH measurements may result as the dye ages. Experiments will be undertaken using batches of dyes from weeks to over 10 years old to resolve its degradation characteristics. The experiments will establish how long a batch of dye remains valid once it is prepared without biasing the measurements. This is particularly important for long term studies such as extended research expeditions and autonomous systems where a batch of dye may be used over a year. Together, by both investigating the validity of chemical models for seawater pH at low temperature and salinity and examining the stability of the pH indicator dye, methodological uncertainties can be reduced to permit better monitoring of changes in global ocean pH.</p>
<p>This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.</p>
Inorganic Carbon Meaurements
largerWorkCitation
project
eng; USA
oceans
-70.884417
-70.884417
39.773433
39.773433
2019-10-10
2019-10-10
Lab studies
0
BCO-DMO catalogue of parameters from Total alkalinity and dissolved inorganic carbon data measured during the pH internal consistency experiment.
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/905302.rdf
Name: Batch
Units: unitless
Description: <p>Seawater batch number</p>
http://lod.bco-dmo.org/id/dataset-parameter/905303.rdf
Name: Practical_Salinity
Units: unitless
Description: <p>Salinity</p>
http://lod.bco-dmo.org/id/dataset-parameter/905304.rdf
Name: meas_TA
Units: micromoles per kilogram (µmol/kg)
Description: <p>measured total alkalinity</p>
http://lod.bco-dmo.org/id/dataset-parameter/905305.rdf
Name: meas_DIC
Units: micromoles per kilogram (µmol/kg)
Description: <p>measured dissolved inorganic carbon</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
2465
https://darchive.mblwhoilibrary.org/server/api/core/bitstreams/825c6b41-7606-46ff-aedf-86d7354b42eb/content
download
https://doi.org/10.26008/1912/bco-dmo.905278.1
download
onLine
dataset
<p>Oligotrophic Atlantic surface seawater was collected from 39° 46.406′ N and 70° 53.065′ W on October 10, 2019.</p>
<p>The surface seawater was modified to five different salinities and 5 different pCO2 values for a total of 25 batches. Salinity was modified through dilution or evaporation. pCO2 was modified by bubbling CO2 gas of different pCO2 concentrations (balance air).</p>
<p>The water was then bottled and sealed into 250 mL borosilicate glass bottles following SOPs (Dickson et al. 2007). Each batch consisted of 44 bottles.</p>
Specified by the Principal Investigator(s)
<p>Total Alkalinity was measured by open cell HCl titration following SOP (Dickson et al. 2007)</p>
<p>Dissolved inorganic carbon was measured by coulometry following SOP (Dickson et al. 2007)</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