Abstract

The acid/base properties of dissolved organic carbon (DOC) are an important feature of soil and surface waters. Large differences in the acid/base properties of DOC found by different studies might be interpreted as spatial and temporal differences in these properties. Different analytical techniques, however, may explain some of the differences. We used a combination of ion-exchange techniques, titration, and surface water chemistry data to evaluate DOC character from two substantially different areas-the relatively pristine boreal zone of Sweden and the heavily acidified temperate zone of the Czech Republic. We found a significantly higher site density (amount of carboxylic groups per milligram of DOC) for the Swedish sites (10.2 muequiv/mg of DOC +/- 0.6) as compared to the Czech sites (8.8 muequiv/mg of DOC +/- 0.5). This suggests a slightly higher buffering capacity for Swedish DOC. A triprotic model of a type commonly incorporated in biogeochemical models was used for estimating the DOC dissociation properties. For Swedish sites, the following constants were calibrated: pK(a1) = 3.04, pK(a2) = 4.51, and pK(a3) = 6.46, while the constants for Czech sites were pK(a1) = 2.5, pK(a2) = 4.42, and pK(a3) = 6.7. Despite differences in site density values, both models predict very similar dissociation and thus pH buffering by DOC in the environmentally important pH range of 3.5-5.0. This can be incorporated into models to make reliable estimates of the effect of organic acids on pH and buffering in different regions

Published in

Environmental Science and Technology
2003, Volume: 37, number: 9, pages: 1726-1730
Publisher: AMER CHEMICAL SOC

SLU Authors

• Bishop, Kevin

  • Department of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences
    

• Laudon, Hjalmar

  • Department of Forest Ecology, Swedish University of Agricultural Sciences
    

UKÄ Subject classification

Environmental Sciences related to Agriculture and Land-use


Publication identifier

DOI: https://doi.org/10.1021/es0201552

Permanent link to this page (URI)

https://res.slu.se/id/publ/80