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Water source characterization through spatiotemporal patterns of major, minor and trace element stream concentrations in a complex, mesoscale German catchment
by:In: HYDROLOGICAL PROCESSES, Vol. 22, Nr. 12
(2008)
, p. 2028-2043.
Abstract
The link between spatiotemporal patterns of stream water chemistry and
catchment characteristics for the mesoscale Dill catchment 692 km2
in Germany is explored to assess the catchment scale controls on water
quality and to characterize water sources. In order to record the
spatiotemporal pattern, �snapshot sampling� was applied during low,
mean and high flow, including 73 nested sites throughout the catchment.
Water samples were analysed for the elements Li, B, Na, Mg, Al, K, Ca,
V, Cr, Mn, Fe, Co, Ni, Cu, Zn, Rb, Sr, Mo, Ba, Ph and U using
inductively-coupled-plasma mass spectrometry, and for electric
conductivity and pH. Principle component analysis and hierarchical
cluster analysis were used to find typical element associations and to
group water samples according to their hydrochemical fingerprints. This
revealed regional hydrochemical patterns of water quality which were
subsequently related to catchment attributes to draw conclusions about
the controls on stream chemistry. It was found that various lithologic
signals and anthropogenic point source inputs controlled the base flow
hydrochemistry. During increased flows, stream waters were diluted
causing additional hydrochemical variability in response to
heterogeneous precipitation inputs and differences in aquifer storage
capacities. The hydrochemical patterns further displayed in-stream
mixing of waters. This implied, that stream waters could be apportioned
to the identified water sources throughout the catchment. The
basin-wide hydrochemical variability has the potential to outrange the
tracer signatures typically inferred in studies at the hillslope scale
and is able to strongly influence the complexity of the catchment
output. Both have to be considered for further catchment scale tracer
and modelling work. Despite the likelihood of non-conservative
behaviour, the minor and trace elements enhanced the rather qualitative
discrimination of the various groundwater types, as the major cations
were strongly masked by point source inputs. Copyright C 2007 John
Wiley & Sons, Ltd.


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