A. Miltner et W. Zech, EFFECTS OF MINERALS ON THE TRANSFORMATION OF ORGANIC-MATTER DURING SIMULATED FIRE-INDUCED PYROLYSIS, Organic geochemistry, 26(3-4), 1997, pp. 175-182
The effect of Fe(OH)(3), Al(OH)(3), birnessite, montmorillonite, and s
ea sand on changes in the composition of organic matter during heating
was investigated. CO2 was released in all treatments, although the ex
periments were conducted in the absence of oxygen. In the presence of
Fe(OH)3, Al(OH)(3), and birnessite, more CO2 was evolved than in the o
ther treatments. Birnessite and Fe(OH)3 enhance the thermal decomposit
ion of polysaccharides and lignin more than Al(OH)(3). Changes in the
lignin signature resembled the alterations during aerobic litter decom
position and humification in humus profiles. DRIFT spectra indicate th
at the formation of aromatic compounds was favoured, especially in the
presence of birnessite. (C) 1997 Elsevier Science Ltd.