The aim of this work is to present a discussion on the concept of baseline and to compare the
natural variations in inorganic water quality present in a selection of British and Norwegian
groundwaters. The use of boxplots and cumulative frequency plots facilitates comparison
between individual rock aquifers, different regions with divergent geological and climatic
records, and between various elements and parameters. The range of baseline concentrations is
often large; e.g. uranium concentrations in Precambrian granitic groundwaters in Norway spans
almost 4 orders of magnitude.
Baseline values are useful as a means to assess pollution or to set a realistic base for remediation.
The EU Maximum Admissible Concentrations (MAC values) of drinking water should be set on
toxicological criteria only, as natural unpolluted groundwater sometimes contain elements in
concentrations deemed to be harmful.
Most of the hard rock groundwaters in Norway have relatively high pH compared with those of
the UK. Na-HCO3 type waters seem to be much more common in Norway than in the UK where
Ca-HCO3 type water dominate. High F, U and Rn concentrations are found in many granitic and
sedimentary groundwaters in Norway, while Ba concentrations tend to be higher in the UK
sedimentary aquifers.
Universal baseline values do not exist for any element and statistical representative sampling
from all aquifers is necessary to establish reliable knowledge about the natural groundwater
quality in each area. A suggested series of methodologies are suggested which can be applied to
aquifers where the effects of anthropogenic pollution are present. There is a strong need for timeseries
data on a wide range of parameters to ascertain the long-term effects of human activity on
groundwater quality. The trends of groundwater quality with depth should also be studied more
thoroughly.
In order for a European wide policy to be implemented it is necessary to establish protocols for
criteria related to data quality, sampling and analytical wor
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