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Metadata Report for BODC Series Reference Number 2244547


Metadata Summary

Data Description

Data Category Water sample data
Instrument Type
NameCategories
Waterproof thermometer  water temperature sensor
Niskin bottle  discrete water samplers
Metrohm 916 Ti Touch compact potentiometric titrator  titrators
Instrument Mounting lowered unmanned submersible
Originating Country United Kingdom
Originator Mr Pablo Trucco Pignata
Originating Organization University of Southampton School of Ocean and Earth Science
Processing Status banked
Online delivery of data Download available - Ocean Data View (ODV) format
Project(s) CUSTARD
 

Data Identifiers

Originator's Identifier DY111_CTD_DOXY_6417:CTD037S
BODC Series Reference 2244547
 

Time Co-ordinates(UT)

Start Time (yyyy-mm-dd hh:mm) 2020-01-03 07:02
End Time (yyyy-mm-dd hh:mm) -
Nominal Cycle Interval -
 

Spatial Co-ordinates

Latitude 54.41130 S ( 54° 24.7' S )
Longitude 89.12820 W ( 89° 7.7' W )
Positional Uncertainty 0.0 to 0.01 n.miles
Minimum Sensor or Sampling Depth 6.3 m
Maximum Sensor or Sampling Depth 756.3 m
Minimum Sensor or Sampling Height 3893.7 m
Maximum Sensor or Sampling Height 4643.7 m
Sea Floor Depth 4650.0 m
Sea Floor Depth Source DATAHEAD
Sensor or Sampling Distribution Variable common depth - All sensors are grouped effectively at the same depth, but this depth varies significantly during the series
Sensor or Sampling Depth Datum Instantaneous - Depth measured below water line or instantaneous water body surface
Sea Floor Depth Datum Approximate - Depth is only approximate
 

Parameters

BODC CODERankUnitsTitle
ADEPZZ011MetresDepth (spatial coordinate) relative to water surface in the water body
BOTTFLAG1Not applicableSampling process quality flag (BODC C22)
DOKGWITX1Micromoles per kilogramConcentration of oxygen {O2 CAS 7782-44-7} per unit mass of the water body [dissolved plus reactive particulate phase] by Winkler titration
DOXMSDXX1Micromoles per kilogramConcentration standard deviation of oxygen {O2 CAS 7782-44-7} per unit mass of the water body [dissolved plus reactive particulate phase]
DOXYWITX1Micromoles per litreConcentration of oxygen {O2 CAS 7782-44-7} per unit volume of the water body [dissolved plus reactive particulate phase] by Winkler titration
FIRSEQID1DimensionlessBottle firing sequence number
OXYTMP011Degrees CelsiusTemperature of oxygen fixation
OXYTMPSD1Degrees CelsiusTemperature standard deviation of oxygen fixation
ROSPOSID1DimensionlessBottle rosette position identifier
SAMPRFNM1DimensionlessSample reference number
SDOXWITX1Micromoles per litreConcentration standard deviation of oxygen {O2 CAS 7782-44-7} per unit volume of the water body [dissolved plus reactive particulate phase] by Winkler titration

Definition of BOTTFLAG

BOTTFLAGDefinition
0The sampling event occurred without any incident being reported to BODC.
1The filter in an in-situ sampling pump physically ruptured during sample resulting in an unquantifiable loss of sampled material.
2Analytical evidence (e.g. surface water salinity measured on a sample collected at depth) indicates that the water sample has been contaminated by water from depths other than the depths of sampling.
3The feedback indicator on the deck unit reported that the bottle closure command had failed. General Oceanics deck units used on NERC vessels in the 80s and 90s were renowned for reporting misfires when the bottle had been closed. This flag is also suitable for when a trigger command is mistakenly sent to a bottle that has previously been fired.
4During the sampling deployment the bottle was fired in an order other than incrementing rosette position. Indicative of the potential for errors in the assignment of bottle firing depth, especially with General Oceanics rosettes.
5Water was reported to be escaping from the bottle as the rosette was being recovered.
6The bottle seals were observed to be incorrectly seated and the bottle was only part full of water on recovery.
7Either the bottle was found to contain no sample on recovery or there was no bottle fitted to the rosette position fired (but SBE35 record may exist).
8There is reason to doubt the accuracy of the sampling depth associated with the sample.
9The bottle air vent had not been closed prior to deployment giving rise to a risk of sample contamination through leakage.

Definition of Rank

  • Rank 1 is a one-dimensional parameter
  • Rank 2 is a two-dimensional parameter
  • Rank 0 is a one-dimensional parameter describing the second dimension of a two-dimensional parameter (e.g. bin depths for moored ADCP data)

Problem Reports

No Problem Report Found in the Database


Data Access Policy

Open Data

These data have no specific confidentiality restrictions for users. However, users must acknowledge data sources as it is not ethical to publish data without proper attribution. Any publication or other output resulting from usage of the data should include an acknowledgment.

If the Information Provider does not provide a specific attribution statement, or if you are using Information from several Information Providers and multiple attributions are not practical in your product or application, you may consider using the following:

"Contains public sector information licensed under the Open Government Licence v1.0."


Narrative Documents

Metrohm 916 Ti-Touch compact potentiometric titrator

The Metrohm 916 Ti-Touch is a stand-alone potentiometric titrator for dynamic (DET), monotonic (MET), set endpoint (SET) and manual titrations (MAT). The instrument consists of an intergrated buret, rod stirrer (or magnetic stirrer) and dosing system with a live touch control display.

Specifications

Dosing element with intelligent exchange unit 2 x 800 Dosino or 2 x 805 Dosimat
Dosing steps per cylinder content 800 Dosino: 10,000 pulses; 805 Dosimat: 20,000 pulses
Stirrers/Titration stands

Included - 802 rod stirrer

Additional - 1 x 801 magnetic stirrer or 1 x 802 rod stirrer or 1 x 803 KF titration stand

Attachments 2 MSB connectors, 1 sample changer (814, 815) via USB
Temperature sensor Pt1000 or NTC

More information can be found in the manufacturer's product description.

Niskin Bottle

The Niskin bottle is a device used by oceanographers to collect subsurface seawater samples. It is a plastic bottle with caps and rubber seals at each end and is deployed with the caps held open, allowing free-flushing of the bottle as it moves through the water column.

Standard Niskin

The standard version of the bottle includes a plastic-coated metal spring or elastic cord running through the interior of the bottle that joins the two caps, and the caps are held open against the spring by plastic lanyards. When the bottle reaches the desired depth the lanyards are released by a pressure-actuated switch, command signal or messenger weight and the caps are forced shut and sealed, trapping the seawater sample.

Lever Action Niskin

The Lever Action Niskin Bottle differs from the standard version, in that the caps are held open during deployment by externally mounted stainless steel springs rather than an internal spring or cord. Lever Action Niskins are recommended for applications where a completely clear sample chamber is critical or for use in deep cold water.

Clean Sampling

A modified version of the standard Niskin bottle has been developed for clean sampling. This is teflon-coated and uses a latex cord to close the caps rather than a metal spring. The clean version of the Levered Action Niskin bottle is also teflon-coated and uses epoxy covered springs in place of the stainless steel springs. These bottles are specifically designed to minimise metal contamination when sampling trace metals.

Deployment

Bottles may be deployed singly clamped to a wire or in groups of up to 48 on a rosette. Standard bottles and Lever Action bottles have a capacity between 1.7 and 30 L. Reversing thermometers may be attached to a spring-loaded disk that rotates through 180° on bottle closure.

Bottle Dissolved Oxygen for Cruise DY111

Originator's Protocol for Data Acquisition and Analysis

Sampling methodology

Seawater samples for dissolved oxygen concentration were directly collected from the Niskin bottles on deck for the stainless steel CTD casts and in the clean laboratory to avoid their contamination for the titanium CTD casts. Seawater was siphoned into 100 mL borosilicate glass bottles (nominal volume, actual volume was determined gravimetrically prior to the cruise), using silicone tubing and overflowing 2 times the bottle volume, and samples were immediately fixed. Oxygen in the samples was fixed with Manganese Sulphate and Alkaline Iodide solutions dispensed from calibrated pipettes. The fixing temperature was recorded on a hand-held thermometer. Immediately after fixing, the samples were stored until analysis.

Analytical methodology

Titrations for dissolved oxygen determination were made within the following 12 h. The concentration of thiosulphate was calibrated prior to starting oxygen analyses as well as blank determination. Dissolved Oxygen (DO) was determined by automated Winkler titration with potentiometric end-point (Williams and Jenkinson 1982) using a Metrohm 916 Ti-Touch controller and 2 Metrohm Dosino 800 units for dispensing Thiosulphate and Iodate solutions. A Metrohm Pt-Titrode electrode was used for detecting the potentiometric end-point of the titration. The titration sequence and data acquisition were controlled by Metrohm Tiamo software. Oxygen saturation was calculated from the equations for solubility in seawater of Benson and Krause (1984).

Instrument Description

Metrohm 916 Ti-Touch

References Cited

Benson B.B. & Krause D.Jr. (1984). The concentration and isotopic fractionation of oxygen dissolved in freshwater and seawater in equilibrium with the atmosphere. Limnology and Oceanography, 29(3), 620-632.

Williams P.J.leB. & Jenkinson N.W. (1982). A transportable microprocessor-controlled precise Winkler titration suitable for field station and shipboard use. Limnology and Oceanography, 27(3), 576-584.

DY111 Cruise report

Further information can be found in the DY111 Cruise report.

BODC Data Processing Procedures

Data received were loaded into the BODC database using established BODC data banking procedures. Where data were provided by the originator as replicates the data were averaged and standard deviations calculated. A parameter mapping table is provided below:

Originator's Variable Originator's Units BODC Parameter Code BODC Unit Comments
Winkler DO_[µmol kg-1] µmol kg-1 DOKGWITX µmol/kg -
Temp_fix [°C] deg C OXYTMP01 deg C -
Winkler DO [µmol l-1] µmol l-1 DOXYWITX µmol/L -
wDO_dupl_stdev µmol l-1 SDOXWITX µmol/L -
- - DOXMSDXX µmol/kg Calculated by BODC
- - OXYTMPSD deg C Calculated by BODC

Data Quality Report

Flags were added to oxygen samples that were taken from Niskin bottles that had been reported as leaking or that had misfired after discussion with the originator.


Project Information

Carbon Uptake and Seasonal Traits of Antarctic Remineralisation Depth (CUSTARD)

Carbon Uptake and Seasonal Traits of Antarctic Remineralisation Depth (CUSTARD) is a £1.8 million, four-year (2018-2022) research project funded by the Natural Environment Research Council (NERC).

The main aim of the CUSTARD project is to quantify the seasonal drivers of carbon fluxes in a region of the Southern Ocean upper limb, and estimate how long different quantities of carbon are kept out of the atmosphere based on the water flow routes at the observed remineralisation depths. Please visit the CUSTARD web page for more information

CUSTARD is one of three projects funded as part of the Role of the Southern Ocean in the Earth System (RoSES) programme, also known as the Southern Ocean programme. Please see the RoSES project document for more information on the wider programme and the research projects associated with it.

Background

The upper limb of the Antarctic Circumpolar Current (ACC) represents an important junction in the marine carbon cycle, as the fate of carbon fixed by surface phytoplankton will differ according to how deep it penetrates before being remineralised. If shallow remineralisation occurs, carbon will follow the upper limb circulation and upwell further north, escaping into the atmosphere within decades. On the other hand, deep remineralisation will result in carbon entering the lower limb circulation, with the potential of being retained in the ocean for hundreds of years. Seasonality in plankton dynamics play an important role in remineralisation depth, and CUSTARD aims to resolve all factors contributing to the carbon export out of the region.

Participants

Six different UK-based organisations are directly involved in research for CUSTARD:

  • National Oceanography Centre (NOC)
  • NERC British Antarctic Survey (BAS)
  • University of Southampton
  • University of Oxford
  • Plymouth University
  • University of East Anglia (UEA)

CUSTARD collaborates closely with the US Ocean Observatories Initiative (OOI) program through sharing of instruments and platforms at and around the Global Southern Ocean Array. OOI is funded by the National Science Foundation (NSF) and is managed by the Woods Hole Oceanographic Institution. Rutgers University maintains the cyberinfrastructure component, working alongside CUSTARD scientists in the handling and distribution of shared observational data.

Research details

Four Work Packages have been funded by the CUSTARD project, each addressing a separate project objective within the region of study in the south eastern Pacific ocean. These are described briefly below:

  • Work Package 1: Obtain an accurate picture of the seasonal air-sea flux and macronutrient drawdown.
    This work package aims at determining the magnitude and variability of air-sea CO2 fluxes and their physical and biogeochemical drivers. High-resolution carbon measurements in the water column, CO2 flux estimates and daily resolved nitrate and silicate observations are combined to better understand the link between seasonal changes in CO2 fluxes and biological variability.

  • Work Package 2: Quantify the link between iron and silicate availability and remineralisation depth.
    This work package investigates the annual cycle of phytoplankton dynamics, net production and export of organic material in conjunction with iron availability.

  • Work Package 3: Observationally determine the seasonal cycle in remineralisation depth.
    This work package assesses remineralisation depth and its variability using marine snow catchers deployed during the process cruise, and backscatter measurements carried out year-round by gliders.

  • Work Package 4: Examine the link between seasonality and remineralisation depth and the trajectory of carbon from the surface out of the upper limb.
    This work package aims to ingest all CUSTARD observational data into models to determine whether seasonal variability in phytoplankton composition is reflected in changes in remineralisation depth, which in turn leads to seasonal variability in the fate of organic carbon leaving the Southern Ocean via the upper limb.

Fieldwork and data collection

All the observational data from the project is collected at and south of the Ocean Observatories Initiative (OOI) Global Southern Ocean Array, located south-west of Chile. Data collection activities span from November 2018 to January 2020, and include three cruises, four glider missions, and one mooring.

Cruises

All cruises depart from and return to Punta Arenas (Chile). Cruise activities include deployments and recovery of gliders and a mooring, Conductivity, Temperature and Depth (CTD), trace metal clean GoFlo bottle sampling, Red Camera Frame, Marine Snow Catcher and Underwater Vision Profiler deployments, as well as laboratory incubations with sea water samples. See cruise details below:

Cruise identifier Research ship Cruise dates Comments
DY096 RRS Discovery November - December 2018 Deployment cruise
DY111 RRS Discovery December 2019 - January 2020 Process cruise
DY112 RRS Discovery January 2020 Mooring recovery cruise
Gliders

Two Slocum 1000 MARS gliders (Pancake and Churchill) are deployed from DY096, to collect data continuously for one year until recovery on DY111. The gliders are mounted with CTD sensors, an optode, a fluorometer, and twin backscatter sensors. Pancake failed and its mission ended early in February 2019.

One Rutgers University glider is deployed from DY111, to collect data until recovery at the end of the same cruise. The glider is owned by Rutgers University and the data is shared with CUSTARD. It carries CTD sensors, an optode, a fluorometer, a backscatter sensor and a particle size analyser.

Mooring

Deployment of Global Surface Mooring GS01SUMO-00004 (SUMO-4) during DY096, to take continuous measurements for approximately one year until recovery during DY112. Its location is roughly 54 28 S, 89 02 W. This is an OOI mooring provided and deployed by WHOI, and adapted to integrate NOC lab-on-chip nitrate and silicate sensors.

Contacts

Dr. Adrian Marin (National Oceanography Centre, UK) - Lead Principal Investigator and lead of Work Package 4
Dr. Dorothee Bakker (University of East Anglia, UK) - Lead of Work Package 1
Prof. Mark Moore (University of Southampton, UK) - Lead of Work Package 2
Dr. Stephanie Henson (National Oceanography Centre / University of Southampton, UK) - Lead of Work Package 3


Data Activity or Cruise Information

Data Activity

Start Date (yyyy-mm-dd) 2020-01-03
End Date (yyyy-mm-dd) 2020-01-03
Organization Undertaking ActivityNational Oceanography Centre, Southampton
Country of OrganizationUnited Kingdom
Originator's Data Activity IdentifierDY111_CTD_CTD037S
Platform Categorylowered unmanned submersible

BODC Sample Metadata Report for DY111_CTD_CTD037S

Sample reference number Nominal collection volume(l) Bottle rosette position Bottle firing sequence number Minimum pressure sampled (dbar) Maximum pressure sampled (dbar) Depth of sampling point (m) Bottle type Sample quality flag Bottle reference Comments
1781108   20.00 24 24    5.80    6.80    6.20 Niskin bottle No problem reported    
1781111   20.00 23 23    5.90    6.90    6.30 Niskin bottle No problem reported    
1781114   20.00 22 22    9.70   10.70   10.10 Niskin bottle No problem reported    
1781117   20.00 21 21   16.00   17.00   16.40 Niskin bottle No problem reported    
1781120   20.00 20 20   20.60   21.60   20.90 Niskin bottle No problem reported    
1781123   20.00 19 19   20.70   21.70   21.00 Niskin bottle No problem reported    
1781126   20.00 18 18   30.00   31.00   30.20 Niskin bottle No problem reported    
1781129   20.00 17 17   39.90   40.90   40.00 Niskin bottle No problem reported    
1781132   20.00 16 16   40.10   41.10   40.20 Niskin bottle Bottle misfire   did not fire
1781135   20.00 15 15   50.20   51.20   50.20 Niskin bottle No problem reported    
1781138   20.00 14 14   60.00   61.00   59.90 Niskin bottle No problem reported    
1781141   20.00 13 13   75.60   76.60   75.40 Niskin bottle No problem reported    
1781144   20.00 12 12   76.10   77.10   75.90 Niskin bottle No problem reported    
1781147   20.00 11 11  100.60  101.60  100.20 Niskin bottle No problem reported    
1781150   20.00 10 10  100.50  101.50  100.10 Niskin bottle No problem reported    
1781153   20.00 9 9  124.80  125.80  124.10 Niskin bottle No problem reported    
1781156   20.00 8 8  149.20  150.20  148.30 Niskin bottle No problem reported    
1781159   20.00 7 7  200.10  201.10  198.70 Niskin bottle No problem reported    
1781162   20.00 6 6  200.20  201.20  198.80 Niskin bottle No problem reported    
1781165   20.00 5 5  302.00  303.00  299.60 Niskin bottle No problem reported    
1781168   20.00 4 4  402.90  403.90  399.40 Niskin bottle No problem reported    
1781171   20.00 3 3  505.00  506.00  500.40 Niskin bottle No problem reported    
1781174   20.00 2 2  764.00  765.00  756.30 Niskin bottle No problem reported    
1781177   20.00 1 1 1016.60 1017.60 1005.50 Niskin bottle No problem reported    

Please note:the supplied parameters may not have been sampled from all the bottle firings described in the table above. Cross-match the Sample Reference Number above against the SAMPRFNM value in the data file to identify the relevant metadata.

Related Data Activity activities are detailed in Appendix 1

Cruise

Cruise Name DY111
Departure Date 2019-12-02
Arrival Date 2020-01-09
Principal Scientist(s)Adrian P Martin (National Oceanography Centre, Southampton)
Ship RRS Discovery

Complete Cruise Metadata Report is available here


Fixed Station Information

Fixed Station Information

Station NameOOI-Southern Ocean
CategoryOffshore location
Latitude54° 4.88' S
Longitude89° 39.91' W
Water depth below MSL4800.0 m

Fixed Station - Ocean Observatories Initiative (OOI) Global Southern Ocean Array

OOI Southern Ocean Array is an offshore site situated in the South Pacific to the south west of Chile, in an area of large scale thermohaline circulation, intermediate water formation, and CO2 sequestration. The array originally comprised four moorings and a combination of Open Ocean and Profiling Gliders. All of the moorings were successfully recovered for the last time in January 2020.

Central Location of Fixed Station Average Water Depth (m)
54.0814 °S 89.6652 °W 4800

The following is a list of the cruises involved in recovery and deployment of the moorings:

Cruise Date Funding Body
R/V Atlantis AT 26-30 March 2015 NSF
R/V Nathaniel B. Palmer NPB 15-11 December 2015 NSF
R/V Nathaniel B. Palmer NPB 16-10 November-December 2016 NSF
R/V Nathaniel B. Palmer NPB 17-09 November-December 2017 NSF
RRS Discovery DY096 November-December 2018 NERC
RRS Discovery DY112 January 2020 NERC

More information can be found at: https://oceanobservatories.org/array/global-southern-ocean-array/

Related Fixed Station activities are detailed in Appendix 2


BODC Quality Control Flags

The following single character qualifying flags may be associated with one or more individual parameters with a data cycle:

Flag Description
Blank Unqualified
< Below detection limit
> In excess of quoted value
A Taxonomic flag for affinis (aff.)
B Beginning of CTD Down/Up Cast
C Taxonomic flag for confer (cf.)
D Thermometric depth
E End of CTD Down/Up Cast
G Non-taxonomic biological characteristic uncertainty
H Extrapolated value
I Taxonomic flag for single species (sp.)
K Improbable value - unknown quality control source
L Improbable value - originator's quality control
M Improbable value - BODC quality control
N Null value
O Improbable value - user quality control
P Trace/calm
Q Indeterminate
R Replacement value
S Estimated value
T Interpolated value
U Uncalibrated
W Control value
X Excessive difference

SeaDataNet Quality Control Flags

The following single character qualifying flags may be associated with one or more individual parameters with a data cycle:

Flag Description
0 no quality control
1 good value
2 probably good value
3 probably bad value
4 bad value
5 changed value
6 value below detection
7 value in excess
8 interpolated value
9 missing value
A value phenomenon uncertain
B nominal value
Q value below limit of quantification

Appendix 1: DY111_CTD_CTD037S

Related series for this Data Activity are presented in the table below. Further information can be found by following the appropriate links.

If you are interested in these series, please be aware we offer a multiple file download service. Should your credentials be insufficient for automatic download, the service also offers a referral to our Enquiries Officer who may be able to negotiate access.

Series IdentifierData CategoryStart date/timeStart positionCruise
2121953Water sample data2020-01-03 07:02:0054.4113 S, 89.1282 WRRS Discovery DY111

Appendix 2: OOI-Southern Ocean

Related series for this Fixed Station are presented in the table below. Further information can be found by following the appropriate links.

If you are interested in these series, please be aware we offer a multiple file download service. Should your credentials be insufficient for automatic download, the service also offers a referral to our Enquiries Officer who may be able to negotiate access.

Series IdentifierData CategoryStart date/timeStart positionCruise
2053339Water sample data2018-12-04 20:19:0054.408 S, 89.27967 WRRS Discovery DY096
2080221Water sample data2018-12-04 20:19:0054.408 S, 89.27967 WRRS Discovery DY096
2053340Water sample data2018-12-09 12:54:0054.408 S, 89.27767 WRRS Discovery DY096
2080233Water sample data2018-12-09 12:54:0054.408 S, 89.27767 WRRS Discovery DY096
2053352Water sample data2018-12-10 04:06:3054.40863 S, 89.27947 WRRS Discovery DY096
2080245Water sample data2018-12-10 04:06:3054.40863 S, 89.27947 WRRS Discovery DY096
2053364Water sample data2018-12-11 06:16:0054.42297 S, 89.25102 WRRS Discovery DY096
2080257Water sample data2018-12-11 06:16:0054.42297 S, 89.25102 WRRS Discovery DY096
2121719Water sample data2019-12-06 07:05:3054.4213 S, 89.1285 WRRS Discovery DY111
2243808Water sample data2019-12-06 07:05:3054.4213 S, 89.1285 WRRS Discovery DY111
2244210Water sample data2019-12-06 07:05:3054.4213 S, 89.1285 WRRS Discovery DY111
2053118Water sample data2019-12-06 16:15:0054.4213 S, 89.1285 WRRS Discovery DY111
2206982Water sample data2019-12-06 16:15:0054.4213 S, 89.1285 WRRS Discovery DY111
2244596Water sample data2019-12-06 16:15:0054.4213 S, 89.1285 WRRS Discovery DY111
2121720Water sample data2019-12-06 22:35:3054.4213 S, 89.1285 WRRS Discovery DY111
2244222Water sample data2019-12-06 22:35:3054.4213 S, 89.1285 WRRS Discovery DY111
2244302Water sample data2019-12-14 04:41:3554.42467 S, 89.10633 WRRS Discovery DY111
2053180Water sample data2019-12-14 11:55:3054.4273 S, 89.1062 WRRS Discovery DY111
2207057Water sample data2019-12-14 11:55:3054.4273 S, 89.1062 WRRS Discovery DY111
2244652Water sample data2019-12-14 11:55:3054.4273 S, 89.1062 WRRS Discovery DY111
2121793Water sample data2019-12-14 19:11:3054.4168 S, 89.135 WRRS Discovery DY111
2243869Water sample data2019-12-14 19:11:3054.4168 S, 89.135 WRRS Discovery DY111
2244314Water sample data2019-12-14 19:11:3054.4168 S, 89.135 WRRS Discovery DY111
2053192Water sample data2019-12-15 07:43:0054.4163 S, 89.1348 WRRS Discovery DY111
2207069Water sample data2019-12-15 07:43:0054.4163 S, 89.1348 WRRS Discovery DY111
2244664Water sample data2019-12-15 07:43:0054.4163 S, 89.1348 WRRS Discovery DY111
2121800Water sample data2019-12-15 11:48:0054.4163 S, 89.1348 WRRS Discovery DY111
2243870Water sample data2019-12-15 11:48:0054.4163 S, 89.1348 WRRS Discovery DY111
2244326Water sample data2019-12-15 11:48:0054.4163 S, 89.1348 WRRS Discovery DY111
2244431Water sample data2019-12-22 04:39:2854.4165 S, 89.13233 WRRS Discovery DY111
2053260Water sample data2019-12-22 10:47:3054.4162 S, 89.1328 WRRS Discovery DY111
2207125Water sample data2019-12-22 10:47:3054.4162 S, 89.1328 WRRS Discovery DY111
2244732Water sample data2019-12-22 10:47:3054.4162 S, 89.1328 WRRS Discovery DY111
2121885Water sample data2019-12-22 17:23:0054.419 S, 89.1462 WRRS Discovery DY111
2243949Water sample data2019-12-22 17:23:0054.419 S, 89.1462 WRRS Discovery DY111
2244443Water sample data2019-12-22 17:23:0054.419 S, 89.1462 WRRS Discovery DY111
2053315Water sample data2020-01-02 20:24:0054.4153 S, 89.126 WRRS Discovery DY111
2207174Water sample data2020-01-02 20:24:0054.4153 S, 89.126 WRRS Discovery DY111
2244781Water sample data2020-01-02 20:24:0054.4153 S, 89.126 WRRS Discovery DY111
2121953Water sample data2020-01-03 07:02:0054.4113 S, 89.1282 WRRS Discovery DY111
2053327Water sample data2020-01-03 15:15:3054.415 S, 89.1262 WRRS Discovery DY111
2207186Water sample data2020-01-03 15:15:3054.415 S, 89.1262 WRRS Discovery DY111
2244793Water sample data2020-01-03 15:15:3054.415 S, 89.1262 WRRS Discovery DY111
2121965Water sample data2020-01-03 18:14:0054.4152 S, 89.1262 WRRS Discovery DY111
2244001Water sample data2020-01-03 18:14:0054.4152 S, 89.1262 WRRS Discovery DY111
2244559Water sample data2020-01-03 18:14:0054.4152 S, 89.1262 WRRS Discovery DY111
2053886Water sample data2020-01-21 12:22:0054.419 S, 89.138 WRRS Discovery DY112
2244037Water sample data2020-01-21 12:22:0054.419 S, 89.138 WRRS Discovery DY112
2244117Water sample data2020-01-21 12:22:0054.419 S, 89.138 WRRS Discovery DY112
2244800Water sample data2020-01-21 12:22:0054.419 S, 89.138 WRRS Discovery DY112
2053898Water sample data2020-01-21 13:05:0054.42 S, 89.137 WRRS Discovery DY112
2244049Water sample data2020-01-21 13:05:0054.42 S, 89.137 WRRS Discovery DY112
2244129Water sample data2020-01-21 13:05:0054.42 S, 89.137 WRRS Discovery DY112
2244812Water sample data2020-01-21 13:05:0054.42 S, 89.137 WRRS Discovery DY112
2053905Water sample data2020-01-21 13:26:0054.42 S, 89.136 WRRS Discovery DY112
2244050Water sample data2020-01-21 13:26:0054.42 S, 89.136 WRRS Discovery DY112
2244130Water sample data2020-01-21 13:26:0054.42 S, 89.136 WRRS Discovery DY112
2244824Water sample data2020-01-21 13:26:0054.42 S, 89.136 WRRS Discovery DY112
2053917Water sample data2020-01-21 13:42:0054.421 S, 89.136 WRRS Discovery DY112
2244062Water sample data2020-01-21 13:42:0054.421 S, 89.136 WRRS Discovery DY112
2244142Water sample data2020-01-21 13:42:0054.421 S, 89.136 WRRS Discovery DY112
2244836Water sample data2020-01-21 13:42:0054.421 S, 89.136 WRRS Discovery DY112
2053929Water sample data2020-01-21 16:21:0054.421 S, 89.136 WRRS Discovery DY112
2244074Water sample data2020-01-21 16:21:0054.421 S, 89.136 WRRS Discovery DY112
2244154Water sample data2020-01-21 16:21:0054.421 S, 89.136 WRRS Discovery DY112
2244848Water sample data2020-01-21 16:21:0054.421 S, 89.136 WRRS Discovery DY112
2053930Water sample data2020-01-21 16:43:0054.423 S, 89.135 WRRS Discovery DY112
2244086Water sample data2020-01-21 16:43:0054.423 S, 89.135 WRRS Discovery DY112
2244166Water sample data2020-01-21 16:43:0054.423 S, 89.135 WRRS Discovery DY112
2244861Water sample data2020-01-21 16:43:0054.423 S, 89.135 WRRS Discovery DY112
2053942Water sample data2020-01-21 17:03:0054.424 S, 89.134 WRRS Discovery DY112
2244098Water sample data2020-01-21 17:03:0054.424 S, 89.134 WRRS Discovery DY112
2244178Water sample data2020-01-21 17:03:0054.424 S, 89.134 WRRS Discovery DY112
2244873Water sample data2020-01-21 17:03:0054.424 S, 89.134 WRRS Discovery DY112
2053954Water sample data2020-01-21 17:20:0054.424 S, 89.134 WRRS Discovery DY112
2244105Water sample data2020-01-21 17:20:0054.424 S, 89.134 WRRS Discovery DY112
2244191Water sample data2020-01-21 17:20:0054.424 S, 89.134 WRRS Discovery DY112
2244885Water sample data2020-01-21 17:20:0054.424 S, 89.134 WRRS Discovery DY112