C. Pettersson et al., RIVER DISCHARGE OF HUMIC SUBSTANCES AND HUMIC-BOUND METALS TO THE GULF OF BOTHNIA, Estuarine, coastal and shelf science, 44(5), 1997, pp. 533-541
Water from 24 Swedish and Finnish rivers running to the Gulf of Bothni
a (comprising the Bothnian Sea and Bothnian Bay) was sampled on five o
ccasions 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 peatland
s, than in the Swedish rivers, which drain vast mountainous and forest
ed areas. The pH is slightly lower in the Finnish rivers. Humic substa
nces comprise approximately 80% of the total amount of organic matter.
Calculations of the specific transport of organic matter (i.e. the to
tal transport per catchment area) showed that the average release from
the Finnish catchments is more than twice the release 14 om the Swedi
sh catchments. Fe and Al exhibit the same concentration pattern as TOC
. To estimate the humic fraction of some metals (Fe, Cu and Zn), a spe
ciation 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, o
f the total metal content. The total load to the Gulf of Bothnia of hu
mic substances and Fe, Cu and Zn associated with the humic matter was
calculated. It was found that the discharge of humic substances to Bot
hnian Bay originates primarily from the Finnish rivers, and the larges
t amounts contributed to the Bothnian Sea come from the Swedish rivers
. (C) 1997 Academic Press Limited.