There are about 83 000 lakes in Sweden; about 40 000 lakes have fish (
here = 1 kg pike) with Hg-concentrations above the guideline of 0.5 mg
Hg/kg ww; about 10 000 lakes have pike with Hg-concentrations higher
than the 'blacklisting' limit of 1.0 mg Hg/kg ww. How long will this s
ituation last? The answer to that question involves many complex proce
sses and assumptions about future developments, and is, thus, a very i
nteresting area for modelling. The basic aim of this work has been to
present a dynamic model to address this question, and critically evalu
ate the rates and environmental factors regulating the recovery proces
s, so that quantitative predictions concerning the duration of the mer
cury problem in Sweden may be obtained. This modelling approach sugges
ts that it would take very long, till about year 2360, until the mean
Hg-concentration in pike would fall from the present of about 1 below
the guideline value of 0.5. This model is based on certain assumptions
about the future Swedish and European Hg-emissions. Sensitivity and u
ncertainty tests indicate that the most important rates regulating the
uncertainties in the model predictions, and hence the duration of the
mercury problem, are the processes governing the transport of mercury
from land to water, and not lake processes. These land to lake fluxes
, are, in turn, regulated by the atmospheric emissions and the deposit
ion of mercury via wet and dry deposition. The only way to remediate t
he mercury problem (i.e., high concentrations of Hg in fish used for h
uman consumption) is to reduce the basic cause of the problem, i.e., t
he anthropogenic emissions related to, e.,g., the burning of fossil fu
els, and the industrial use of Hg in the technosphere.