TY - JOUR
T1 - Prolonged testing of metal mobility in mining-impacted soils amended with phosphate fertilisers
AU - Munksgaard, Niels
AU - Lottermoser, Bernd G.
AU - Blake, Kevin
PY - 2012/6
Y1 - 2012/6
N2 - The aim of the study was to determine whether the
application of superphosphate fertiliser to soils contaminated with mine wastes
can inhibit metal and metalloid mobility (Cu, Pb, Zn, Cd, Fe, Mn, As, Sb) in
the long term. Contaminated soils contained sulfide- and sulfate-rich waste
materials from the Broken Hill and Mt Isa mining centres. Results of long-term
(10 months) column experiments demonstrate that fertiliser amendment had highly
variable effects on the degree of metal and metalloid mobilisation and capture.
Rapid release of metals from a sulfate-rich soil showed that phosphate
amendment was ineffective in stabilising highly soluble metal-bearing phases.
In a sulfide-rich soil with abundant organic matter, complexing of metals with
soluble organic acids led to pronounced metal (mainly Cd, Cu and Zn) release
from fertiliser-amended soils. The abundance of pyrite, as well as the addition
of fertiliser, caused persistent acid production over time, which prevented the
formation of insoluble metal phosphate phases and instead fostered an increased
mobility of both metals and metalloids (As, Cd, Cu, Sb, Zn). By contrast,
fertiliser application to a sulfide-rich soil with low organic carbon content
and a sufficient acid buffering capacity to maintain near-neutral pH resulted
in the immobilisation of Pb in the form of newly precipitated Pb phosphate
phases. Thus, phosphate stabilisation was ineffective in suppressing metal and
metalloid mobility from soils that were rich in organic matter, contained
abundant pyrite and had a low acid buffering capacity. Phosphate stabilisation
appears to be more effective for the in situ treatment of sulfide-rich soils
that are distinctly enriched in Pb and contain insignificant concentrations of
organic matter and other metals and metalloids.
AB - The aim of the study was to determine whether the
application of superphosphate fertiliser to soils contaminated with mine wastes
can inhibit metal and metalloid mobility (Cu, Pb, Zn, Cd, Fe, Mn, As, Sb) in
the long term. Contaminated soils contained sulfide- and sulfate-rich waste
materials from the Broken Hill and Mt Isa mining centres. Results of long-term
(10 months) column experiments demonstrate that fertiliser amendment had highly
variable effects on the degree of metal and metalloid mobilisation and capture.
Rapid release of metals from a sulfate-rich soil showed that phosphate
amendment was ineffective in stabilising highly soluble metal-bearing phases.
In a sulfide-rich soil with abundant organic matter, complexing of metals with
soluble organic acids led to pronounced metal (mainly Cd, Cu and Zn) release
from fertiliser-amended soils. The abundance of pyrite, as well as the addition
of fertiliser, caused persistent acid production over time, which prevented the
formation of insoluble metal phosphate phases and instead fostered an increased
mobility of both metals and metalloids (As, Cd, Cu, Sb, Zn). By contrast,
fertiliser application to a sulfide-rich soil with low organic carbon content
and a sufficient acid buffering capacity to maintain near-neutral pH resulted
in the immobilisation of Pb in the form of newly precipitated Pb phosphate
phases. Thus, phosphate stabilisation was ineffective in suppressing metal and
metalloid mobility from soils that were rich in organic matter, contained
abundant pyrite and had a low acid buffering capacity. Phosphate stabilisation
appears to be more effective for the in situ treatment of sulfide-rich soils
that are distinctly enriched in Pb and contain insignificant concentrations of
organic matter and other metals and metalloids.
UR - http://www.scopus.com/inward/record.url?scp=84862228901&partnerID=8YFLogxK
U2 - 10.1007/s11270-011-1019-y
DO - 10.1007/s11270-011-1019-y
M3 - Article
SN - 0049-6979
VL - 223
SP - 2237
EP - 2255
JO - Water, Air, and Soil Pollution
JF - Water, Air, and Soil Pollution
IS - 5
ER -