“…The isolation of highly aromatic humic acids from SOM has long been considered an indicator of BC inputs (Haumaier and Zech, 1995;Golchin et al, 1997;Zech et al, 1997;Almendros et al, 2003;Benites et al, 2005), as is development of stable humus forms highly resistant to decomposition (Almendros et al, 2003;Benites et al, 2005). Highly aromatic humic acids (Shindo et al, 1986;Hiradate et al, 2004) and charred plant fragments constituting 3-33% of SOC (Shindo et al, , 2005 were found in volcanic ash soils from Japanese grasslands subject to frequent burning.…”