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Quantifying the fluxes of
inorganic carbon and alkalinity
through UK estuaries
Ruth Matthews, Dorothee Bakker, Naomi Greenwood,
Matthew Humphreys, Silke Kroeger, Richard Sanders
Why do we care?
• Large uncertainty of estuarine outgassing estimate
• 0.25 ± 0.25 Pg C yr-1
• Estimates of estuarine CO2 emission and transport to coastal ocean
probably within 50%-100% of true value
• Estimates rely on extrapolation
• UK accounts for ~1/4 of NW European estuarine surface area
A bit of chemistry…
• Dissolved Inorganic Carbon (DIC)
• CT = [CO2*] + [HCO3
−] + [CO3
2−]
• (Total) Alkalinity
• AT = [HCO3
-] + 2[CO3
2-] + [B(OH)4
-] + [OH-] + [HPO4
2-] + 2[PO4
3-] + [SiO(OH)3
-] +
[HS-] + 2[S2-] + [NH3] - [H+] - [HSO4
-] - [HF] - [H3 PO4]
• Carbonate weathering:
• CaCO3+ CO2+ H2O ⇌Ca2++ 2HCO3
−
• Dissolved Inorganic Carbon (DIC)
• CT = [CO2*] + [HCO3
−] + [CO3
2−]
• (Total) Alkalinity
• AT = [HCO3
-] + 2[CO3
2-] + [B(OH)4
-] + [OH-] + [HPO4
2-] + 2[PO4
3-] + [SiO(OH)3
-] +
[HS-] + 2[S2-] + [NH3] - [H+] - [HSO4
-] - [HF] - [H3 PO4]
• Carbonate weathering:
• CaCO3+ CO2+ H2O ⇌Ca2++ 2HCO3
−
Could limestone weathering be important?
• McGrath et al., 2019:
Samples
• LOCATE sampling campaign
2017-18
• 16 of ~90 estuaries in UK
sampled
• 14 estuaries sampled on 5
occasions, seasonally
• We analysed samples for DIC
and alkalinity
Analysis
• Versatile INstrument for the
Determination of Total dissolved
inorganic carbon and Alkalinity
(VINDTA 3C)
• Adapted method for large
salinity range using different
electrode setup and adapted
alkalinity calculation
Results
Let’s focus in a bit…
Conclusions
• Heterogeneity in DIC and Alkalinity concentrations between estuaries
in the UK
• Some estuaries seasonally shift in gradient of DIC and Alkalinity
change with salinity
• Geology appears to affect Alkalinity concentrations at low salinity
Any questions?
References
• Regnier, P., Friedlingstein, P., Ciais, P., Mackenzie, F.T., Gruber, N.,
Janssens, I.A., Laruelle, G.G., Lauerwald, R., Luyssaert, S., Andersson,
A.J. and Arndt, S., 2013. Anthropogenic perturbation of the carbon
fluxes from land to ocean. Nature geoscience, 6(8), pp.597-607.
• Bauer, J.E., Cai, W.J., Raymond, P.A., Bianchi, T.S., Hopkinson, C.S. and
Regnier, P.A., 2013. The changing carbon cycle of the coastal ocean.
Nature, 504(7478), pp.61-70.
• https://jncc.gov.uk/
• https://nrfa.ceh.ac.uk/

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Matthews, Ruth: Quantifying the fluxes of inorganic carbon and alkalinity through UK estuaries

  • 1. Quantifying the fluxes of inorganic carbon and alkalinity through UK estuaries Ruth Matthews, Dorothee Bakker, Naomi Greenwood, Matthew Humphreys, Silke Kroeger, Richard Sanders
  • 2. Why do we care? • Large uncertainty of estuarine outgassing estimate • 0.25 ± 0.25 Pg C yr-1 • Estimates of estuarine CO2 emission and transport to coastal ocean probably within 50%-100% of true value • Estimates rely on extrapolation • UK accounts for ~1/4 of NW European estuarine surface area
  • 3. A bit of chemistry… • Dissolved Inorganic Carbon (DIC) • CT = [CO2*] + [HCO3 −] + [CO3 2−] • (Total) Alkalinity • AT = [HCO3 -] + 2[CO3 2-] + [B(OH)4 -] + [OH-] + [HPO4 2-] + 2[PO4 3-] + [SiO(OH)3 -] + [HS-] + 2[S2-] + [NH3] - [H+] - [HSO4 -] - [HF] - [H3 PO4] • Carbonate weathering: • CaCO3+ CO2+ H2O ⇌Ca2++ 2HCO3 − • Dissolved Inorganic Carbon (DIC) • CT = [CO2*] + [HCO3 −] + [CO3 2−] • (Total) Alkalinity • AT = [HCO3 -] + 2[CO3 2-] + [B(OH)4 -] + [OH-] + [HPO4 2-] + 2[PO4 3-] + [SiO(OH)3 -] + [HS-] + 2[S2-] + [NH3] - [H+] - [HSO4 -] - [HF] - [H3 PO4] • Carbonate weathering: • CaCO3+ CO2+ H2O ⇌Ca2++ 2HCO3 −
  • 4. Could limestone weathering be important? • McGrath et al., 2019:
  • 5. Samples • LOCATE sampling campaign 2017-18 • 16 of ~90 estuaries in UK sampled • 14 estuaries sampled on 5 occasions, seasonally • We analysed samples for DIC and alkalinity
  • 6. Analysis • Versatile INstrument for the Determination of Total dissolved inorganic carbon and Alkalinity (VINDTA 3C) • Adapted method for large salinity range using different electrode setup and adapted alkalinity calculation
  • 8.
  • 9. Let’s focus in a bit…
  • 10.
  • 11.
  • 12. Conclusions • Heterogeneity in DIC and Alkalinity concentrations between estuaries in the UK • Some estuaries seasonally shift in gradient of DIC and Alkalinity change with salinity • Geology appears to affect Alkalinity concentrations at low salinity
  • 14. References • Regnier, P., Friedlingstein, P., Ciais, P., Mackenzie, F.T., Gruber, N., Janssens, I.A., Laruelle, G.G., Lauerwald, R., Luyssaert, S., Andersson, A.J. and Arndt, S., 2013. Anthropogenic perturbation of the carbon fluxes from land to ocean. Nature geoscience, 6(8), pp.597-607. • Bauer, J.E., Cai, W.J., Raymond, P.A., Bianchi, T.S., Hopkinson, C.S. and Regnier, P.A., 2013. The changing carbon cycle of the coastal ocean. Nature, 504(7478), pp.61-70. • https://jncc.gov.uk/ • https://nrfa.ceh.ac.uk/