Bat
ch equilibrations were performed to investigate theability of hydroxyapatite (Ca
5(PO
4)
3OH) to
chemi
cally immobilizeU in two
contaminated sediment samples having differentorgani
c carbon
contents (123 and 49 g kg
-1, respe
ctively).Apatite additions lowered aqueous U to near proposed drinkingwater standards in bat
ch equilibrations of two distin
ctsediment strata having total U
con
centrations of 1703 and2100 mg kg
-1, respe
ctively. Apatite addition of 50 g kg
-1redu
ced the solubility of U to values less than would beexpe
cted if autunite (Ca(UO
2)
2(PO
4)
2·10H
2O) was the
controlling solid phase. A
comparison of the two sedimenttypes suggests that aqueous phase U may be
controlledby both the DOC
content through
complexation andthe equilibrium pH for a given apatite appli
cation rate.Sequential
chemi
cal extra
ctions demonstrated that apatiteamendment transfers U from more
chemi
cally labilefra
ctions, in
cluding water-soluble, ex
changeable, and a
cid-soluble (pH
![](/images/entities/ap.gif)
2.55) fra
ctions, to the Mn-o
ccluded fra
ction(pH
![](/images/entities/ap.gif)
1.26). This suggests that apatite amendmentredire
cts solid-phase spe
ciation with se
condary U phosphatesbeing solubilized due to the lower pH of the Mn-o
ccluded extra
ctant, despite the la
ck of signifi
cantquantities of Mn oxides within these sediments. Energydispersive X-ray (EDX) analysis
condu
cted in a transmissionele
ctron mi
cros
cope (TEM)
confirmed that apatiteamendment sequesters some U in se
condary Al/Fephosphate phases.