Temporal stability of magnetic parameters of anthropogenic ferrimagnetics i
n model soil conditions was studied. Fly ash from a power plant was used as
original contaminant material, while soil reactive medium was modeled by d
ifferent soil solutions. Changes in mass-specific magnetic susceptibility (
chi), percentage frequency dependent magnetic susceptibility (chi(FD)%), hy
steresis parameters and thermomagnetic curves were measured for samples whi
ch underwent different leaching time periods. Virtually constant magnetic s
usceptibility values were obtained, independently on the soil medium (acid,
neutral). On the other hand, the original highly non-stoichiometric maghem
ite phase rapidly transformed to stable magnetite. In some cases (model of
free-draining soils) further decrease of Curie temperature (T-c) to 550-560
degrees C is observed. (C) 2000 Elsevier Science Ltd. All rights reserved.