The addition of hydrated lime and dolomite to fly ash
slurries results in the development of anionic clays.
These
minerals are comprised of stacked sequences of double-metal hydroxide layers. Unlike most clays, the
hydroxide
layers have a net positive charge. As a result,
anionic-form elements in fly ash leachate waters are scavenged into
the interlayer positions to neutralize the positive
charge.
In our experiments, leachate borate, sulfate, and
arsenate
concentrations were reduced by up to 2 orders of
magnitude.
High leachable boron is the chief limitation on the
agricultural use of fly ash in soil remediation, and in
this
study lime treatment reduced leachable boron to levels
below those toxic to plants. Under the oxygenated
conditions
of surface and near-surface waters, many elements of
environmental concern occur as oxyanions, such as borate,
arsenate, chromate, selenate, and molybdate. Anions
are
typically mobile under the neutral to alkaline pH
conditions typical of most groundwaters, and little
reliance
can be given to the geosphere for their attenuation.
The
design of geochemical conditions to precipitate anionic
clay minerals is a promising means to sequester and
immobilize
anionic-form elements from wastewaters. However, it
is not known whether high pH conditions, which promote
the formation of these anionic clays, will also be
necessary
to ensure their stability and thus the long-term
immobilization
of sequestered anions.