CMAR Measurements

This page provides an overview of where and how dissolved oxygen is measured through the CMAR’s Coastal Monitoring Program.

These figures and values include data collected up to the end of the 2022 field season and subjected to preliminary Quality Control.

Locations

CMAR has collected dissolved oxygen data from 63 stations in 13 counties (Figure 1).

Figure 1: Approximate location of stations with dissolved oxygen data. At most stations, dissolved oxygen is measured in units of percent saturation. For several stations in Halifax and Lunenburg counties, dissolved oxygen is now recorded in units of concentration.

Number of Observations

A large proportion of dissolved oxygen records are from Guysborough County (23.37 %) and Shelburne County (20.58 %), while a small proportion are from Antigonish (0.53 %) and Pictou (1.1 %) Counties (Figure 2).

Most observations to date have been measured in units of percent saturation. In 2021, CMAR began deploying several sensors that record in concentration (mg / L), and there are a growing number of observations recorded in these units (Figure 2).

Figure 2: The number of dissolved oxygen observations in each county.

Depth

There is typically one dissolved oxygen sensor on each sensor string, usually attached 5 m below the surface (Figure 3). This choice of depth reflects the original Coastal Monitoring Program objective, which was to provide data to inform aquaculture site selection1. As the Program and mandate expands, DO sensors continue to be deployed at this depth for consistency and longevity of the time series.

Dissolved oxygen has also been measured at other depths for specific research projects, particularly in Whycocomagh Basin, Inverness County (Figure 3).

Figure 3: Number of dissolved oxygen observations at each depth (rounded to nearest whole number).

Sensors

CMAR uses two types of sensors to measure dissolved oxygen: the aquaMeasure DOT (InnovaSea 2021) and Onset HOBO U26 (Onset 2012).

aquaMeasure DOT

CMAR has a large inventory of DOTs (71 in April 2023), which are used for most deployments with dissolved oxygen. The DOT measures temperature and partial pressure of oxygen, providing dissolved oxygen values in units of percent saturation. Partial pressure values are not affected by salinity (Bittig et al. 2018), and so no correction factor is required for these measurements. For CMAR deployments, each DOT is programmed to measure and internally log at 10 minute intervals. CMAR typically retrieves sensors after ~1 year for data offload, cleaning, and calibration/validation.

HOBO U26

CMAR added 13 HOBO U26 sensors to the inventory in 2021, and purchased an additional 10 in January 2023. The HOBO U26 measures temperature the concentration of dissolved oxygen (in units of mg / L). For CMAR deployments, each HOBO U26 is programmed to measure and internally log at 10 minute intervals. These sensors have a sensor cap that needs to be replaced every 6 months. They are deployed in St. Margaret’s Bay and Mahone Bay rather than more remote locations so that they can be serviced twice a year with minimal travel requirements (Figure 1).

The HOBO U26 sensor does not account for salinity, so the measurements should be adjusted based on a salinity correction factor before analysis. The HOBOware software can apply this salinity correction if salinity conditions are provided. The software can also convert measured concentration values to percent saturation if salinity and pressure conditions are provided. CMAR does not have consistent salinity or pressure measurements, and so the uncorrected data are provided.

Biofouling

The DOT and HOBO U26 do not have any anti-fouling mechanisms, and so measurements are susceptible to biofouling. Ideally, sensors would be cleaned every 2 - 4 weeks to remove fouling, but this is not feasible due to logistical and financial constraints. Significant effort was made to flag possible biofouling signals, and CMAR is evaluating potential anti-fouling strategies.

References

Bittig, Henry C., Arne Körtzinger, Craig Neill, Eikbert van Ooijen, Joshua N. Plant, Johannes Hahn, Kenneth S. Johnson, Bo Yang, and Steven R. Emerson. 2018. “Oxygen Optode Sensors: Principle, Characterization, Calibration, and Application in the Ocean.” Journal Article. Frontiers in Marine Science 4 (429). https://doi.org/10.3389/fmars.2017.00429.
InnovaSea. 2021. “Realtime Monitoring Product Manual.” https://rsaqua.co.uk/wp-content/uploads/2021/03/Innovasea_UserManual-2021_V1.5.pdf.
Onset. 2012. “HOBO® Water Temp Pro V2 (U22-001) Manual.” https://www.onsetcomp.com/files/manual_pdfs/10366-F-MAN-U22-001.pdf.

Footnotes

  1. 5 m is approximately mid-cage depth for net pens in the region.↩︎