Phosphogypsum is the by-product of producing phosphoric acid by reacti
ng phosphate rock with sulfuric acid. The phosphoric acid industry in
Florida is the largest in the world and it is estimated that 1 x 10(9)
tonnes of phosphogypsum will soon be stored in 18 subaerial sites, th
e so-called Florida ''gyp-stacks''. Florida phosphate rock samples ana
lyzed in this study have U-238 activities which range from approximate
ly 250 to 2000 Bq kg(-1) with U-234, Th-230, Ra-226, Pb-210 and Po-210
in approximate radioactive equilibrium. During production of phosphor
ic acid, about 990-100% of the Ra-226, Pb-210 and Po-210 in the phosph
ate rock is fractionated to the phosphogypsum. In most cases the activ
ities of Ra-226, Pb-210 and Po-210 in the phosphogypsum are directly a
nd predictably proportional to the activities in the input phosphate r
ock. Studies carried out on the disequilibrium relationships in 74 sam
ples of Florida phosphogypsum show that Ra-226 is relatively immobile
on the unsaturated, aerobic portions of these gyp-stacks. The Pb-210 s
eems to be remobilized preferentially to Po-210 or Ra-226 and solution
s percolating through Florida gyp-stacks have added Pb-210 to some pho
sphogypsum samples. Copyright (C) 1996 Elsevier Science Limited