The interaction of Ge-containing solutions with solid fossil fuel samples confirm its organic mode of occurrence. Based on the maximum sorption capacities, the samples follow the order: vitrain and xylain > peat (Romania) > bituminous coal > peat (Belarus) > lignite > semifusain. The results show the dependence between the sorption capacity of the studied samples and the pH medium, as well as the time of soaking. It was found that Ge is strongly associated with organic matter.
Sorption, germanium, pH dependence, peat, coal, coal lithotypes