Mg. Macklin et al., THE USE OF OVERBANK SEDIMENT FOR GEOCHEMICAL MAPPING AND CONTAMINATION ASSESSMENT - RESULTS FROM SELECTED ENGLISH AND WELSH FLOODPLAINS, Applied geochemistry, 9(6), 1994, pp. 689-700
Overbank sediment profiles from floodplains in England and Wales conta
in a record of both natural geochemical patterns and those showing the
influence of man's activities. It has been suggested that this charac
teristic can be used to allow maps to be compiled which show human imp
act on the fluvial geochemical environment. Studies reviewed in this p
aper, however, show that a single overbank profile very rarely spans t
he period from before anthropogenic disturbance through to the Industr
ial Revolution and later. Significant lateral variations in metal conc
entrations occur also over a relatively small area in overbank sedimen
ts of the same general age. These, and the nature of vertical changes
in chemistry, make the choice of sample sites, and sampling interval w
ithin a profile, difficult. Even sediments which appear uncontaminated
may record anthropogenic influences from activities such as deforesta
tion and agriculture. A means of dating the sediment and an appreciati
on of river erosion and sedimentation histories are shown to be essent
ial in order to ensure that maps intended to depict natural geochemica
l variations are based on material deposited before disturbance of the
cathment by human activity. These considerations and associated costs
may render overbank sediment non-viable as a regional geochemical map
ping medium.