This study concerns the humic-like polymeric compounds formed by D-glu
cose plus L-tryptophan and by L-tryptophan alone, both on Cu-saturated
nontronite, montmorillonite and kaolinite and on quartz in the presen
ce of Cu(II) ions. These mineral-organic systems were kept in thermost
at at 70 degrees C for 30 days and submitted to alternate wetting-dryi
ng cycles. Higher amounts of humic-like compounds were extracted from
quartz-organic than from clay-organic systems, showing the remarkable
action of Cu(II), which even overcame the high catalytic power of clay
s. (C) 1997 Elsevier Science Ltd.