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The NewSTHEPS MetaData catalogue gives an overview of all persons and institutes involved and lists all created datasets and publications coming out of the project.

 

Persons Institutes Publications Datasets

 

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pH modelling in aquatic systems with time-variable acid-base dissociation constants applied to the turbid, tidal Scheldt estuary
Hofmann, A.F.; Middelburg, J.J.; Soetaert, K.; Meysman, F.J.R. (2009). pH modelling in aquatic systems with time-variable acid-base dissociation constants applied to the turbid, tidal Scheldt estuary. Biogeosciences 6(8): 1539-1561. http://dx.doi.org/10.5194/bg-6-1539-2009
In: Gattuso, J.P.; Kesselmeier, J. (Ed.) Biogeosciences. Copernicus Publications: Göttingen. ISSN 1726-4170; e-ISSN 1726-4189
Peer reviewed article  
Beschikbaar in  Auteurs 
Trefwoorden
    Belgium: Schelde
    Cycles > Chemical cycles > Geochemical cycle > Biogeochemical cycle
    Netherlands: Schelde
    Water bodies > Coastal waters > Coastal landforms > Coastal inlets > Estuaries
    Marien/Kust; Brak water
Auteurs  Top 
  • Hofmann, A.F.
  • Middelburg, J.J.
  • Soetaert, K.
  • Meysman, F.J.R.
Abstract
    A new pH modelling approach is presented that explicitly quantifies the influence of biogeochemical processes on proton cycling and pH in an aquatic ecosystem, and which accounts for time variable acid-base dissociation constants. As a case study, the method is applied to investigate proton cycling and long-term pH trends in the Scheldt estuary (SW Netherlands, N Belgium). This analysis identifies the dominant biogeochemical processes involved in proton cycling in this heterotrophic, turbid estuary. Furthermore, information on the factors controlling the longitudinal pH profile along the estuary as well as long-term pH changes are obtained. Proton is mainly counteracted by proton consumption due to CO2 degassing. Overall, CO2 degassing generates the largest proton turnover in the whole estuary on a yearly basis. The main driver of long-term changes in the mean estuarine pH over the period 2001 to 2004 is the decreasing freshwater flow, which influences the pH directly via a decreasing supply of dissolved inorganic carbon and alkalinity, and also indirectly, via decreasing ammonia loadings and lower nitrification rates.
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