The vertical distribution of main soil hydroxyanthraquinones (HAQs) in the
soil profiles of five Japanese Andosols, one Japanese Cambisol, and one Nep
alese Cambisol was analyzed quantitatively, using high performance liquid c
hromatography and thin layer chromatography with a two stage development ac
companied by scanning densitometry. The results were as follows: The vertic
al distribution patterns of chrysophanol (CPL) and its dimers in Andosols p
rofiles showed maximum contents in the middle part of the surface horizon.
The vertical distribution of physcion (PYS) and its dimers in soil profiles
showed various patterns in each profile. Additionally, we investigated the
vertical distribution of HAQs in Andosols under a Miscanthus sinensis gras
sland, and in an adjacent successional red pine (Pinus densiflora) forest a
t Sugadaira, Central Japan. In the surface soil (0-15 cm), the contents of
the dimers of CPL (microcarpin and chrysotalunin) slightly increased and th
ose of the dimers of PYS (7,7'-biphyscion and hinakurin) showed a remarkabl
e increase in the succession, whereas the contents of monomeric HAQs (CPL a
nd PYS) slightly decreased suggesting preferential production of dimeric HA
Qs below a depth of 15 cm in the forest Andosol. The dimers of CPL and the
dimers of PYS exhibited different structures, vertical distribution pattern
s, and changes in the contents in Andosols in the secondary succession. The
refore, it was assumed that dimeric reaction processes of CPL may be differ
ent from those of PYS, if dimeric reactions had occurred in soil.