“…Up to date, there are no direct evidences of the mode of occurrence of Be in coals, and in many coal deposits it has been deduced by the following indirect evidences: -A negative correlation between Be content in ash and ash implies organic association (Jedwab, 1960;Danchev and Lapinskaja, 1968;Kortenski and Sotirov, 2002), while positive correlation indicates the domination of inorganic affinity (Ren et al, 2004;Dai et al, 2005). -A positive correlation of Be with Al and Si in coal and peat points to major (Querol et al, 1997;Zhuang et al, 2000;Kalaitzidis et al, 2002) or an intermediate (Querol et al, 2001a) aluminosilicate affinity. On this basis in another deposit, partial organic and partial Al-Si affinity for Be has been suggested (Querol et al, 1999).…”