C. Johns, CONTAMINATION OF RIPARIAN WETLANDS FROM PAST COPPER MINING AND SMELTING IN THE HEADWATERS REGION OF THE CLARK-FORK RIVER, MONTANA, USA, Journal of geochemical exploration, 52(1-2), 1995, pp. 193-203
The headwaters region of the Clark Fork River in western Montana, U.S.
A., has been the center of copper mining and smelting activities for a
pproximately 120 years. Poor control of waste materials led to widespr
ead contamination. High metal concentrations have been found in bed se
diments of the river 381 km downstream and in reservoir sediments 500
km downstream. Fish and aquatic insects have been influenced by metal
contamination, but little has been published about metal influences on
riparian wetland areas, either sediments or plant species. In this st
udy sediment and a dominant emergent macrophyte species (Typha latifol
ia) were sampled from eight small riparian wetlands along the upper 19
0 km of the Clark Fork and from one site on an uncontaminated tributar
y to the Clark Fork River. Elevated concentrations of copper, zinc, an
d frequently, lead were found in plant tissues and sediments of 8 Clar
k Fork sites compared to the local reference site. Total and HCI-extra
ctable copper and zinc concentrations in unsieved and sieved (<60 micr
on) sediment were strong and highly significant predictors of the meta
l concentrations in Typha latifolia root tissues.