Batch equilibration experiments using a low calcium (similar to 1 wt.% as C
aO), acidic (pH similar to 4.5) Type F fly ash demonstrated phosphate immob
ilization on the order of 100% to 75% for 50 and 100 me; P/1 solutions, res
pectively. A loosely compacted column of fly ash similarly removed 10 mg P/
1 for over 85 pore volumes, While the interactions between phosphate and ca
lcium-rich (Type C) ashes are relatively well understood, insight into the
mechanisms of phosphate immobilization in Type F ash necessitated a review
of the phosphate chemistry and interactions with acidic geomedia. Phosphate
adsorption was subsequently modeled using a constant capacitance model app
roach (CCM) excluding precipitation reactions. Our CCM predictions of total
phosphate immobilization (20%) were substantially less than the results of
the batch equilibration experiments and phosphate adsorption predicted by
other researchers examining near pure natural and synthetic geomedia due to
the compositional heterogeneity of the fly ash. Nevertheless, for the amor
phous and crystalline phases studied, the immobilization of phosphate in th
e Type F fly ash is attributed to the formation of insoluble aluminum and i
ron phosphates at low to medium values of pH. (C) 2000 Elsevier Science B.V
. All rights reserved.