Soil samples taken from excavated pits on traverses across New Zealand's Sc
ott Base, Antarctica,were leached with water and 0.01 M HNO3 and the leacha
tes analysed for Ag, Al, As, Cd, Cr, Cu, Fe, Mn, Ni, Pb and Zn. The soils h
ad high conductivity and pH values generally increasing with depth and in t
he range 8.3-10.1. The water leachate generally contained most of the extra
ctable metals except Mn and Cd, and As. Linear relationships were observed
between some metals leached into alkaline solution and the Fe in those solu
tions. The ratios to Fe were comparable to those of the host basanite, and
this observation is interpreted as showing that these metals are incorporat
ed in fine mineral particulates derived directly from the rock mass. Outlie
rs in leachable metal concentrations in the soils indicated appreciable con
tamination of the soil from anthropogenic sources with Ag, Cd, Cu, Pb and Z
n as well as As. In some locations high concentrations of Ag and Cd corresp
ond to specific sources and drainage channels. High concentrations of Pb we
re widely spread and in the top soil layers whereas the elevated concentrat
ions of Zn were distributed throughout the soil profiles indicating atmosph
eric sources and different mobilities within the soils. Transport within th
e soils is evident for some metals, as is lateral movement over and through
the soils. (C) 2000 Elsevier Science Ltd. All rights reserved.