Regular Article
River Discharge of Humic Substances and Humic-bound Metals to the Gulf of Bothnia

https://doi.org/10.1006/ecss.1996.0159Get rights and content

Abstract

Water from 24 Swedish and Finnish rivers running to the Gulf of Bothnia (comprising the Bothnian Sea and Bothnian Bay) was sampled on five occasions in 1991–93, and analysed for concentrations of total organic carbon (TOC), humic substances and metals (Fe, Al, Cu, Zn). In general, TOC is higher in the Finnish rivers, which drain forest and peatlands, than in the Swedish rivers, which drain vast mountainous and forested areas. The pH is slightly lower in the Finnish rivers. Humic substances comprise approximately 80% of the total amount of organic matter. Calculations of the specific transport of organic matter (i.e. the total transport per catchment area) showed that the average release from the Finnish catchments is more than twice the release from the Swedish catchments. Fe and Al exhibit the same concentration pattern as TOC. To estimate the humic fraction of some metals (Fe, Cu and Zn), a speciation study, utilizing a weak anion-exchange resin, was performed on water from rivers with different hydrochemical properties. The humic fractions of Fe, Cu and Zn were 20–40, 40–60 and <10%, respectively, of the total metal content. The total load to the Gulf of Bothnia of humic substances and Fe, Cu and Zn associated with the humic matter was calculated. It was found that the discharge of humic substances to Bothnian Bay originates primarily from the Finnish rivers, and the largest amounts contributed to the Bothnian Sea come from the Swedish rivers.

References (0)

Cited by (63)

  • Drivers of phytoplankton production and community structure in nutrient-poor estuaries receiving terrestrial organic inflow

    2019, Marine Environmental Research
    Citation Excerpt :

    Seasonal variations in river discharge and characteristic differences in the properties of the catchment areas are major factors affecting the supply of organic matter to the sea (Skoog et al., 2011; Asmala et al., 2013). The inflow of tDOM to coastal areas is highest during spring when snowmelt in forest and peatland dominated areas takes place (Pettersson et al., 1997; Räike et al., 2012; Reader et al., 2014). Climate change scenarios indicate that precipitation and thus the inflow of tDOM to the northern Baltic Sea will increase in the future (Meier, 2006).

  • Seasonal variation and mixing behaviour of glutathione, thioacetamide and fulvic acids in a temperate macrotidal estuary (Aulne, NW France)

    2017, Estuarine, Coastal and Shelf Science
    Citation Excerpt :

    Note that this comparison, based on the few reports on humic substances in estuaries, must not be considered representative of all system types. Indeed humic substances concentrations in natural waters can vary from tens of μgC L−1 in alpine systems to tens of mgC L−1 in peat systems (Pettersson et al., 1997; Chanudet et al., 2006). In coastal and oceanic waters, the presence of GSH-like and thiol compounds has been attributed to in situ primary production (Le Gall and van den Berg, 1998; Al-Farawati and van den Berg, 2001).

View all citing articles on Scopus
View full text