“…Weathering reactions proceed naturally in incinerator BA upon contact with atmospheric agents including water, O 2 and CO 2 , and basically mimic the mineralogical alteration processes documented for soils of volcanic origin (Zevenbergen and Comans, 1994;Zevenbergen et al, 1998). Although it is well established that natural weathering leads to the formation of thermodynamically stable phases or phase assemblages Johnson et al, 1995;Meima and Comans, 1997;Zevenbergen et al, 1996Zevenbergen et al, , 1998Zevenbergen and Comans, 1994;Comans and Meima, 1994;Pfrang-Stotz et al, 2000), completion of the chemical and mineralogical transformations is expected to occur within time frames on the order of hundreds to thousands of years. Nevertheless, it has been shown that a certain degree of BA stabilization can be attained when the material is stockpiled for periods ranging from some weeks to a few months.…”