Skip to main content
Skip table of contents

O2 saturation derived from concentration

Consider an RBRconcerto³ with an integrated RBRcoda³ T.ODO or Aanderaa Optode DO sensor. The dissolved oxygen sensor transfers both the foil temperature and the dissolved oxygen concentration (not compensated for salinity). The RBRconcerto³ calculates the concentration compensated for salinity first, then the air saturation (in %) via the following equation:



where

  • Cc is the concentration in uMol/L, compensated for salinity,
  • Patm is atmospheric pressure, and
  • Pav is air vapour pressure.


Solubility is calculated via Gordon and Garcia as:



where S is the salinity in PSU and Ts is defined as:



with T being the water temperature in °C and:




Air vapour pressure (in dbar) is calculated as:



JavaScript errors detected

Please note, these errors can depend on your browser setup.

If this problem persists, please contact our support.