The vertical distribution of main soil hydroxyanthraquinones (HAQs) in the soil profiles of five Japanese Andosols, one Japanese Gambisol, and one Nepalese Gambisol was analyzed quantitatively, using high performance liquid chromatography and thin Bayer chromatography with a two stage development accompanied by scanning densitormetry. The results were as follows: The vertical distribution patterns of chrysophanol (CIPL) and its dimers in Andosols profiles shewed maximum contents in the middle past of the surface horizon. The vertical distribution of physcion (PYS) and its dimers in soil profiles showed various patterns in each profile. AdditionaBPy, we investigated the vertical distribution of HAQs in AndosoPs under a Miscanthus sinensis grassland, and in an adjacent successional red pine (Pinus densiflora) forest at Sugadaira, Central Japan. En the surface soil (0–15 cm), the contents of the dimers of CPL (microcarpin and chrysotalunin) slightly increased and those of the dimers of PPS (7,7′-biphyscion and Rinakurian) showed a remarkable increase in the succession, whereas the contents of monomeric HAQs (CBL and PYS) slightly decreased suggesting preferential production of dimeric HAQs below a depth of 15 em in the forest Andosol. The dimers of CPL and the dimers sf PPS exhibited diRerent structures, vertical distribution patterns, and changes in the contents in Andosols in the secondary succession. Therefore, it was assumed that dimeric reaction processes of CPL may be different from those of PYS, if dimeric reactions had occurred in soil.
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