19:I[42426,["/_next/static/immutable/chunks/1xctgzqre-wsy.js","/_next/static/immutable/chunks/06_-wz6pdtp2b.js","/_next/static/immutable/chunks/30e52g49hg40p.js","/_next/static/immutable/chunks/02yq6tul2z-oh.js","/_next/static/immutable/chunks/10bx_ec2vj7n_.js","/_next/static/immutable/chunks/33bfn03fo8xnt.js","/_next/static/immutable/chunks/0tfjf78scu61b.js","/_next/static/immutable/chunks/31xnvej4n1bi9.js"],"default"] 1a:Tc39,

Sampling was conducted during day trips on Pleasant (Maine, USA) and St. John (New Brunswick, CA) estuaries in May and October 2018 and 2019.

* See "Related Datasets" section for access to the related organic alkalinity data described below.

Sample Collection:

Four surveys were conducted of both the Pleasant and St. John estuaries, in May and October 2018, and again in May and October 2019 in order to assess potential differences in estuary conditions between spring and fall seasons. Estuary samples were collected during single-day surveys on small vessels in each system, departing from Addison Maine for Pleasant estuary surveys and from St. John, New Brunswick, for St. John surveys. Estuary water was continuously pumped to an underway measurement system, which recorded location, salinity(Seabird SBE-45), water temperature (Seabird SBE-45), and the partial pressure of carbon dioxide (pCO₂) among other parameters. Surveys were started on the incoming tide and lasted through high tide and into the ebb tide. At intervals determined from the underway salinity, surface water was captured for discrete sample collection. During the October 2017 and May 2018 surveys a Niskin bottle was lowered overboard by hand; during the later surveys a 10-liter high-density polyethylene (HDPE) carboy was rinsed and filled from the outflow of the underway system, then tightly capped until samples were drawn from a spout at the bottom of the carboy. River endmember samples were collected from above the final downstream dam on each river. For the Pleasant, this dam formed a physical tidal barrier, and the transition from river to estuary was immediate. For the St. John the closest site was in Fredericton New Brunswick, a location over 120 km from the estuary mouth along the river’s course. For both endmember sites, a plastic bucket was lowered from the center of a bridge over the river, rinsed three times with river water, and samples were collected as described above. The temperature and conductivity of samples were measured directly from the bucket with a handheld meter (YSI, Yellow Springs, Ohio).

Water from the Niskin or carboy was transferred without bubbling into individual, previously-flushed borosilicate glass BOD bottles: 500 mL for alkalinity and pH_T analyses, and 300 mL for inorganic carbon (DIC) analysis. All bottles had greased stoppers and positive closure mechanisms, were filled to leave less than 1% headspace in the bottle, and were preserved with saturated mercuric chloride solution. Samples for silicate and phosphate analysis were filtered using a plastic syringe and 0.2 µm cartridge filter into acid-washed and previously-rinsed 50 mL HDPE vials and preserved with chloroform. Samples for DOC were filtered as was done for the nutrients into acid-washed and previously-rinsed 30 mL HDPE bottles. All samples were immediately placed on ice. Alkalinity, pH, and DIC samples were refrigerated until analysis; nutrient and DOC samples were frozen until analysis.

1b:T564,* Underway data files were provided as SeaBASS format .sb files. These were loaded into matlab using the sbread.m file provided by the submitter (included in supplemental package on this dataset underway_data_sb_format.zip). Data were then converted to matlab table and exported as .csv format. * .csv form of the data were imported into BCO-DMO's data system and concatenated into one table. Additional column ISO_DateTime_UTC added. Data imported with missing data identifier designated as -9999 ** Missing data values are displayed differently based on the file format you download. They are blank in csv files, "NaN" in MatLab files, etc. * Column names adjusted to conform to BCO-DMO naming conventions designed to support broad re-use by a variety of research tools and scripting languages. [Only numbers, letters, and underscores. Can not start with a number] * sbread() loads and performs some reformatting of the data (for example, extraneous trailing .000000 on integers like year were removed). * commands used to convert .sb to .csv files = dir('*.sb') ; % you are in the folder where mat files are present N = length(files) ; for i = 1:N [data,fields,units,header]=sbread(files(i).name) T = array2table(data,'VariableNames',fields) outfile = regexprep(files(i).name,'sb$','csv') writetable(T,outfile); end 1c:T431,This dataset contains underway data from four organic alkalinity estuary transects, in May and October of 2018 and 2019, completed in the Pleasant (Maine, USA) and St. John (New Brunswick, Canada) estuaries. See "Related Datasets" section for alkalinity data. Discrete samples were collected at intervals of salinity along each estuary. An underway measurements system was also operated during each transect. Discrete samples were analyzed via a number of methods described below. Underway measurements were collected using the procedures described in Hunt et al. (2013). Organic alkalinity is a poorly understood component of the estuarine and coastal ocean acid-base system. This lack of understanding makes assessment of ocean acidification vulnerability and inorganic carbon dynamics more difficult. However, the methods used to quantify organic alkalinity and its effects on the acid-base system are not standardized. In this work we examined several approaches for the measurement of organic alkalinity, and their application to inorganic carbon dynamics. 1d:T490,Underway data system file for each estuary survey in SeaBASS (.sb) format which includes header lines and comment lines preceding the data. files named: FLO_L3_yyyymmdd_yyyy_2sec.sb = underway data system file for each estuary survey. Matlab m-file (sbread.m) is also contained in this package which reads data and metadata from the .sb files and performs reformatting (for example trailing decimal .000000 values stripped from integers like year). function [data,fields,units,header]=sbread(sbfile); % [data,fields,units,header,fieldwvln]=sbread(sbfile); % Reads in data from SeaBASS files and assigns field names to 'fields', units % to 'units', data to 'data', and header parameters to 'header'. List of % header parameters is in 'header.parameters' and all of the header text is in % 'header.all'. Time in the format hh:mm:ss is reformated to decimal hours and % inserted in place of the orignal. Uses function NEAREST.M The primary data table for this dataset was produced by loading .sb files using sbread(), converting to table type, and exporting as csv files. All subtables were concatenated into one table. See "BCO-DMO Processing Notes" section.1e:T894,NSF Award Abstact: Estuaries are bodies of water formed where rivers meet the ocean, and are important ecosystems that provide protected environments and abundant food for fish and shellfish to reproduce. Many estuary systems are under pressure by changing atmospheric and oceanic conditions, as well as impacts on the rivers that empty into them. Scientists from the University of New Hampshire and the University of South Florida propose that the total alkalinity of some coastal systems, influenced by river runoff, may contain a large fraction of organic acids that have been previously ignored and may play a role in the acid-base chemistry of the estuary. This project would focus on understanding the organic and inorganic acid-base chemistry in estuaries. The project will support a PhD student and several undergraduate students, as well as high school interns from minority communities, broadening participation in the ocean sciences. Also, the monitoring and outreach capacity of a regional wild fishery conservation group will be enhanced, allowing the public to be more fully informed on the effect of ongoing estuarine changes on fisheries. This project will be a comparison study of two estuary-plume systems to examine the exact buffering impact of organic alkalinity on the acid-base properties of coastal systems. The Pleasant (Maine) and St. John (Canada) estuaries represent extremes of river acid-base systems, where the Pleasant is comprised mostly of organic alkalinity and the St. John has a small organic alkalinity fraction. It is hypothesized by these scientists that some coastal regions may experience organic alkalinity as the dominant alkalinity factor in the total alkalinity distribution. This would mean that organic alkalinity would be the dominant factor affecting system pH, pCO2 (partial pressure of carbon dioxide), and the saturation index of aragonite. By doing this river endmember study into organic alkalinity of these two systems, these scientists will provide the tools for the entire oceanographic community to assess the buffering capability of organic alkalinity in other coastal systems and how the systems are likely to respond to acidification.6:["$","$L19",null,{"dataset":{"_id":"918590","description":"

This project was a collaboration between Dr. Christopher W. Hunt and Dr. Joseph Salisbury (of the University of New Hampshire) and Dr. Xuewu Liu and Dr. Robert H. Byrne (of the University of South Florida).

\n","problem":"","acquisition":"$1a","processing":"","bcodmoProcessing":"$1b","title":"Underway data from estuary transects in Coastal Gulf of Maine (Pleasant, Maine; St. John, New Brunswick) in May and October of 2018 and 2019","nickname":"Underway Data","dataUrl":"","currentState":"Final no updates expected","currentStateId":"7","validated":true,"restricted":false,"version":"1","version_date":"2024-01-26T05:00:00.000Z","abstract":"$1c","citation":"Hunt, C. (2024) Underway data from estuary transects in Coastal Gulf of Maine (Pleasant, Maine; St. John, New Brunswick) in May and October of 2018 and 2019. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2024-01-26 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.918590.1 [access date]","citationParts":{"identifier":"doi:10.26008/1912/bco-dmo.918590.1","versionDate":"2024-01-26","versionId":"1","year":"2024","title":"Underway data from estuary transects in Coastal Gulf of Maine (Pleasant, Maine; St. John, New Brunswick) in May and October of 2018 and 2019","authors":"Hunt, C.","publisher":"Biological and Chemical Oceanography Data Management Office (BCO-DMO)."},"doi":"10.26008/1912/bco-dmo.918590.1","release_date":null,"field_dataset_location":"Coastal Gulf of Maine: Pleasant (Maine, USA) and St. John (New Brunswick, CA) ","temporal_extent":{"start":"2018-05-15T04:00:00.000Z","end":"2019-10-24T04:00:00.000Z"},"temporal":{"resolution":"time:unitDay","type":"time:Interval","start":{"value":"1526356800","label":"2018-05-15"},"end":{"value":"1571889600","label":"2019-10-24"}},"spatial_extent":{"shape":"polygon","center":{"latitude":45.210500000003,"longitude":-66.882500000005},"wkt":"POLYGON ((-67.764 44.48, -66.001 44.48, -66.001 45.941, -67.764 45.941, -67.764 44.48))","north":45.941,"east":-66.001,"south":44.48,"west":-67.764},"dataset_type":["Other Field Results"],"keywords":["oceans"],"data_files":[{"id":"918792","title":"918590_v1_underway-data.csv","url":"https://datadocs.bco-dmo.org/dataset/918590/file/A8OWzZDC9KnN7R/918590_v1_underway-data.csv","showTableUrl":"https://www.bco-dmo.org/dataset/918590/data/view/918792","description":"Primary data file for dataset ID 918590, version 1. \n\nSee \"BCO-DMO Data Processing\" section for more information about how this table was created from source files contained in underway_data_sb_format.zip","filename":"918590_v1_underway-data.csv","bytesize":17840785,"checksum":{"value":"810bf5ae706cce63c3c15dcab03bdb61","Algorithm":{"_id":"190","name":"MD5"}},"mimetype":"text/csv","fileType":{"_id":"192","name":"Comma Separated Values (.csv)"},"isErddap":"bcodmo_dataset_918590_v1","date":"","isPublicDuringEmbargo":false,"primaryDataFile":true,"showTable":true,"restricted":false}],"supplemental_files":[{"id":"918791","title":"Underway data system files (.sb) [Alternate data format]","url":"https://datadocs.bco-dmo.org/dataset/918590/file/QALjlEZsJXX8BX/underway_data_sb_format.zip","showTableUrl":"","description":"$1d","filename":"underway_data_sb_format.zip","bytesize":4967831,"checksum":{"value":"de8e991c6ee08051a2a6f83456516f0b","Algorithm":{"_id":"190","name":"MD5"}},"mimetype":"application/zip","fileType":{"_id":"196","name":"ZIP Archive (ZIP)"},"isErddap":"","date":"","isPublicDuringEmbargo":false,"primaryDataFile":false,"showTable":false,"restricted":false}],"roles":[{"role":{"_id":"138","name":"Principal Investigator"},"performedBy":{"_id":"876898","name":"Christopher Hunt"},"performedAtOrganization":{"_id":"33","name":"University of New Hampshire"}},{"role":{"_id":"145","name":"BCO-DMO Data Manager"},"performedBy":{"_id":"643627","name":"Amber D. York"},"performedAtOrganization":{"_id":"191","name":"Woods Hole Oceanographic Institution"}}],"deployments":[],"funding":[{"_id":"876890","name":"OCE-1658321","fundingSource":{"_id":"355","name":"NSF Division of Ocean Sciences"},"url":"https://www.nsf.gov/awardsearch/show-award?AWD_ID=1658321"},{"_id":"876896","name":"OCE-1658377","fundingSource":{"_id":"355","name":"NSF Division of Ocean Sciences"},"url":"https://www.nsf.gov/awardsearch/show-award?AWD_ID=1658377"}],"instruments":[{"_id":"918613","name":"","description":". Estuary water was continuously pumped to an underway measurement system, which recorded location, salinity(Seabird SBE-45), water temperature (Seabird SBE-45), and the partial pressure of carbon dioxide (pCO2) among other parameters. ","type_id":"528063","type_name":"Sea-Bird SBE 45 MicroTSG Thermosalinograph","type_desc":"A small externally powered, high-accuracy instrument, designed for shipboard determination of sea surface (pumped-water) conductivity and temperature. It is constructed of plastic and titanium to ensure long life with minimum maintenance. It may optionally be interfaced to an external SBE 38 hull temperature sensor.\r\n\r\nSea Bird SBE 45 MicroTSG (Thermosalinograph)","type_acronym":"SBE 45 MicroTSG"}],"parameters":[{"_id":"918753","name":"year","format":"","frictionlessType":"string","description":"

Sample year (yyyy)

","units":{"_id":"","name":"unitless"},"type":{"_id":"1062","name":"year","description":"

year, reported as YYYY, e.g. 1995

"}},{"_id":"918754","name":"month","format":"","frictionlessType":"integer","description":"

Sample month (mm)

","units":{"_id":"","name":"unitless"},"type":{"_id":"1115","name":"month","description":"

Month of year; numeric 1 to 12.

"}},{"_id":"918755","name":"day","format":"","frictionlessType":"integer","description":"

Sample day (dd)

","units":{"_id":"","name":"unitless"},"type":{"_id":"1113","name":"day","description":"

day of month; numeric 1 to 31

"}},{"_id":"918756","name":"hour","format":"","frictionlessType":"integer","description":"

Sample hour (HH)

","units":{"_id":"","name":"unitless"},"type":{"_id":"858","name":"hour_gmt","description":"

hours of time, GMT

"}},{"_id":"918757","name":"minute","format":"","frictionlessType":"integer","description":"

Sample minute (MM)

","units":{"_id":"","name":"unitless"},"type":{"_id":"891","name":"minute_gmt","description":"

minutes of time, GMT

"}},{"_id":"918758","name":"second","format":"","frictionlessType":"integer","description":"

Sample second (SS)

","units":{"_id":"","name":"unitless"},"type":{"_id":"965","name":"seconds_gmt","description":"

seconds of time, GMT

"}},{"_id":"918759","name":"ISO_DateTime_UTC","format":"%Y-%m-%dT%H:%M:%SZ","frictionlessType":"datetime","description":"

Sample datetime (UTC) in ISO 8601 format

","units":{"_id":"","name":"unitless"},"type":{"_id":"1908","name":"ISO_DateTime_UTC","description":"

Date/Time (UTC) ISO formatted
\nThis standard is based on ISO 8601:2004(E) and takes on any of the following forms:
\n2009-08-30T09:05:00[.xx] (local time)
\n2009-08-30T14:05:00[.xx]Z (UTC time)
\n2009-08-30T14:05:00[.xx]-05:00
\nThe dashes and the colons can be dropped.
\nThe T can also be dropped \"by mutual agreement\", but one needs the trailing Z if the time is UTC.

Sample ISO_datetime_utc:
\n2009-08-30T14:05:00[.xx]Z (UTC time)

Format: YYYY-mm-ddTHH:MM:SS[.xx]Z (UTC time)

"}},{"_id":"918760","name":"Julian_Day","format":"","frictionlessType":"integer","description":"

Days since January 1

","units":{"_id":"","name":"unitless"},"type":{"_id":"866","name":"julian_day","description":"

Julian day as a decimal. Julian date which is the time elapsed in days from 00:00 on January 1st 4713 BC. Julian Date (chronological).

For reference: Julian day 2440000 begins at 0000 hours, May 23, 1968.

Please note, Seabird processing software includes a \"julianday\" which is day of year. That is categorized as a separate term \"yrday\" at BCO-DMO.
\nSeabird permalink: https://blog.seabird.com/ufaqs/in-sea-bird-software-is-noon-on-january-1-julian-day-0-5-or-julian-day-1-5/

"}},{"_id":"918761","name":"secDay","format":"","frictionlessType":"integer","description":"

Cumulative seconds of the day since 00:00:00 GMT

","units":{"_id":"","name":"sssss"},"type":{"_id":"1838","name":"time_elapsed","description":"

Elapsed time. Units can be seconds, minutes, etc.

"}},{"_id":"918762","name":"lat","format":"","frictionlessType":"number","description":"

Latitude

","units":{"_id":"","name":"decimal degrees"},"type":{"_id":"730","name":"latitude","description":"

latitude, in decimal degrees, North is positive, negative denotes South; Reported in some datasets as degrees, minutes

"}},{"_id":"918763","name":"lon","format":"","frictionlessType":"number","description":"

Longitude

","units":{"_id":"","name":"decimal degrees"},"type":{"_id":"731","name":"longitude","description":"

longitude, in decimal degrees, East is positive, negative denotes West; Reported in some datasets as degrees, minutes

"}},{"_id":"918764","name":"heading","format":"","frictionlessType":"integer","description":"

Heading of vessel

","units":{"_id":"","name":"degrees"},"type":{"_id":"853","name":"heading","description":"

heading of ship or platform

"}},{"_id":"918765","name":"speed","format":"","frictionlessType":"number","description":"

Speed of Vessel

","units":{"_id":"","name":"meters per second (m/s)"},"type":{"_id":"895950","name":"speed","description":"

Speed is a scalar measure of the rate of movement of an object, typically expressed either as the distance traveled divided by the time taken (average speed) or the rate of change of position with respect to time at a particular point (instantaneous speed).

"}},{"_id":"918766","name":"Wt","format":"","frictionlessType":"number","description":"

Water temperature

","units":{"_id":"","name":"degreesC"},"type":{"_id":"733","name":"temperature","description":"

water temperature at measurement depth

"}},{"_id":"918767","name":"cond","format":"","frictionlessType":"number","description":"

Water conductivity

","units":{"_id":"","name":"millimho per centimeter (mmho/cm)"},"type":{"_id":"779","name":"conductivity","description":"

Conductivity. Units and collection methods may vary. Often reported in Siemens/meter.

When used in a JGOFS/GLOBEC project this is the conductivity in Siemens/meter for the primary conductivity sensor on a CTD.

"}},{"_id":"918768","name":"sal","format":"","frictionlessType":"number","description":"

Water salinity

","units":{"_id":"","name":"Practical Salinity Units (PSU)"},"type":{"_id":"955","name":"sal","description":"

Salinity: The amount (mass or quantity of matter) of salt per amount (volume or mass) of a body of water.

"}},{"_id":"918769","name":"stimfCDOM","format":"","frictionlessType":"number","description":"

Stimulated fluorescence of chromophoric dissolved organic matter

","units":{"_id":"","name":"parts per billion (ppb)"},"type":{"_id":"1891","name":"CDOM","description":"

Colored dissolved organic matter (CDOM): The optically measurable component of the dissolved organic matter in water

"}},{"_id":"918770","name":"stimf","format":"","frictionlessType":"number","description":"

Stimulated fluorescence of chlorophyll

","units":{"_id":"","name":"milligrams per meter cubed (mg/m^3)"},"type":{"_id":"766","name":"chlorophyll a","description":"

Total chlorophyll a pigment. See dataset for units of measurement; often reported in: milligrams per cubic meter (mg/m3); micrograms/liter (ug/L); nanograms/liter (ng/L).

CAUTION Within JGOFS MERGED water column products: this parameter is derived from HPLC methodology and the units are nanograms/liter; however; this parameter name is also used for a variety of water and nonwater column sampling; derived via the fluorometric method; units will also vary.

"}},{"_id":"918771","name":"c660","format":"","frictionlessType":"number","description":"

Bean transmittance at 600 nm

","units":{"_id":"","name":"per meter (1/m)"},"type":{"_id":"1013","name":"transmission","description":"

light transmission, as percent

"}},{"_id":"918772","name":"SBE43_oxygen","format":"","frictionlessType":"number","description":"

Dissolved oxygen concentration

","units":{"_id":"","name":"micromoles per liter (umol/L)"},"type":{"_id":"910","name":"dissolved Oxygen","description":"

dissolved oxygen concentration

"}},{"_id":"918773","name":"SBE43_oxygen_percent_sat","format":"","frictionlessType":"number","description":"

Dissolved oxygen saturation

","units":{"_id":"","name":"percent (%)"},"type":{"_id":"911","name":"O2sat","description":"

oxygen saturation, in milliliters/liters or sometimes milligrams per liter.

"}},{"_id":"918774","name":"pressure_atm","format":"","frictionlessType":"number","description":"

Atmospheric pressure

","units":{"_id":"","name":"hectopascal (hPa)"},"type":{"_id":"732","name":"pressure","description":"

water pressure at measurement; depth reported as pressure; positive number increasing with water depth

"}},{"_id":"918775","name":"L1_pCO2","format":"","frictionlessType":"number","description":"

In-water partial pressure of carbon dioxide

","units":{"_id":"","name":"microatmospheres. (uatm)"},"type":{"_id":"1991","name":"pCO2","description":"

Partial pressure of carbon dioxide {pCO2} in the water body by computation from pH and alkalinity.

"}},{"_id":"918776","name":"L1_fCO2","format":"","frictionlessType":"number","description":"

In-water fugacity of carbon dioxide

","units":{"_id":"","name":"microatmospheres. (uatm)"},"type":{"_id":"1747","name":"fugacity of CO2","description":"

Fugacity of carbon dioxide (CO2) in sea water

"}},{"_id":"918777","name":"L2_pCO2","format":"","frictionlessType":"number","description":"

In-air partial pressure of carbon dioxide

","units":{"_id":"","name":"microatmospheres. (uatm)"},"type":{"_id":"1991","name":"pCO2","description":"

Partial pressure of carbon dioxide {pCO2} in the water body by computation from pH and alkalinity.

"}},{"_id":"918778","name":"L2_fCO2","format":"","frictionlessType":"number","description":"

In-air fugacity of carbon dioxide

","units":{"_id":"","name":"microatmospheres. (uatm)"},"type":{"_id":"1747","name":"fugacity of CO2","description":"

Fugacity of carbon dioxide (CO2) in sea water

"}},{"_id":"918779","name":"bottom_flag","format":"","frictionlessType":"integer","description":"

Data from surface (1) or bottom water (2)

","units":{"_id":"","name":"unitless"},"type":{"_id":"1741","name":"sample_descrip","description":"

text description or other traits of the sample collected

"}},{"_id":"918780","name":"source_data_file","format":"","frictionlessType":"string","description":"

Filename of input data file

","units":{"_id":"","name":"unitless"},"type":{"_id":"659543","name":"file_name","description":"

File name

"}}],"related_publications":[{"id":"794173","citation":"Cai, W.-J., Wang, Y., & Hodson, R. E. (1998). Acid-Base Properties of Dissolved Organic Matter in the Estuarine Waters of Georgia, USA. Geochimica et Cosmochimica Acta, 62(3), 473–483. doi:10.1016/s0016-7037(97)00363-3\r\n","relation_type":["Methods"],"relation_desc":""},{"id":"918610","citation":"Hinckley, Jessica A., "The Non-Conservative Behavior of Organic Alkalinity in Simulated Gulf of Maine Estuary Mixing" (2021). Master's Theses and Capstones. 1512.\r\nhttps://scholars.unh.edu/thesis/1512","relation_type":["Results"],"relation_desc":""},{"id":"918607","citation":"Hunt, C. W., Salisbury, J. E., & Vandemark, D. (2013). CO2 Input Dynamics and Air–Sea Exchange in a Large New England Estuary. Estuaries and Coasts, 37(5), 1078–1091. https://doi.org/10.1007/s12237-013-9749-2\r\n","relation_type":["Methods"],"relation_desc":""},{"id":"918612","citation":"Hunt, C.W., Salisbury, J.E., Liu, X., and R.H. Byrne. 2023. Estuary Organic Alkalinity Distributions, Characteristics, and Application to Carbonate System Calculations (in prep). ","relation_type":["Results"],"relation_desc":""},{"id":"918611","citation":"Hunt, Christopher, "Alkalinity and Buffering in Estuarine, Coastal and Shelf Waters" (2021). Doctoral Dissertations. 2623.\r\nhttps://scholars.unh.edu/dissertation/2623","relation_type":["Results"],"relation_desc":""},{"id":"918608","citation":"Kerr, D. E., Turner, C., Grey, A., Keogh, J., Brown, P. J., & Kelleher, B. P. (2023). OrgAlkCalc: Estimation of organic alkalinity quantities and acid-base properties with proof of concept in Dublin Bay. Marine Chemistry, 251, 104234. https://doi.org/10.1016/j.marchem.2023.104234\r\n","relation_type":["Methods"],"relation_desc":""},{"id":"794171","citation":"Song, S., Wang, Z. A., Gonneea, M. E., Kroeger, K. D., Chu, S. N., Li, D., & Liang, H. (2020). An Important Biogeochemical Link between Organic and Inorganic Carbon Cycling: Effects of Organic Alkalinity on Carbonate Chemistry in Coastal Waters Influenced by Intertidal Salt Marshes. Geochimica et Cosmochimica Acta. doi:10.1016/j.gca.2020.02.013","relation_type":["Results"],"relation_desc":""}],"related_datasets":[{"_id":"918545","name":"Organic Alkalinity Discrete Data","url":"","relation_type":"IsRelatedTo","type_desc":"

The dataset is related to another dataset.

\n","relation_desc":"Data collected from the same estuary transects, in May and October of 2018 and 2019, completed in the Pleasant (Maine, USA) and St. John (New Brunswick, Canada) estuaries.","citation":"Hunt, C. (2024) Organic alkalinity data from estuary transects in Coastal Gulf of Maine (Pleasant, Maine; St. John, New Brunswick) in May and October of 2018 and 2019. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2024-01-25 doi:10.26008/1912/bco-dmo.918545.1"}],"services":[{"grouping":"","items":[{"name":"View Data","description":"An in-browser view of the primary tabular data file","url":"https://www.bco-dmo.org/dataset/918590/data/view","contentType":"text/html","actionType":"view"}]},{"grouping":"ERDDAP","items":[{"name":"SUBSET DATA","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_918590_v1.html","contentType":"text/html","actionType":"tool"},{"name":"VIEW TABLE","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_918590_v1.htmlTable","contentType":"text/html","actionType":"view"},{"name":"CSV","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_918590_v1.csv","contentType":"text/csv","actionType":"download"},{"name":"TSV","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_918590_v1.tsv","contentType":"text/tsv","actionType":"download"},{"name":"MATLAB","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_918590_v1.mat","contentType":"text/x-matlab","actionType":"download"},{"name":"netCDF","description":"","url":"https://erddap.bco-dmo.org/erddap/tabledap/bcodmo_dataset_918590_v1.nc","contentType":"application/x-netcdf","actionType":"download"}]},{"grouping":"Metadata","items":[{"name":"HTML","description":"A simple HTML page of the dataset metadata","url":"https://www.bco-dmo.org/dataset/918590/description","contentType":"text/html","actionType":"view"},{"name":"PDF","description":"A PDF of the HTML dataset metadata","url":"https://www.bco-dmo.org/dataset/918590/Dataset_description.pdf","contentType":"application/pdf","actionType":"download"},{"name":"ISO 19115-2 (NOAA Profile)","description":"","url":"https://www.bco-dmo.org/dataset/918590/iso","contentType":"application/xml","actionType":"download"}]}],"programs":[],"projects":[{"_id":"876891","name":"Collaborative Research: Organic Alkalinity: Impacts of the [OTHER] Alkalinity on Estuary and Coastal Ocean Chemistry","acronym":"organic alkalinity","description":"$1e"}],"archives":[{"id_value":"10.26008/1912/bco-dmo.918590.1","url":"https://doi.org/10.26008/1912/bco-dmo.918590.1","date_assigned":"2024-01-29","version_date":"2024-01-26","archiver":"Marine Biological Laboratory/Woods Hole Oceanographic Institution Library (MBLWHOI DLA)","archiver_id":"272"}],"license":{"name":"Creative Commons Attribution 4.0","id":"CC-BY-4.0","uri":"https://creativecommons.org/licenses/by/4.0/","spdxUri":"https://spdx.org/licenses/CC-BY-4.0"},"metrics":{"views":{"count":271},"downloads":{"count":412}}}}]