Abstract
Abstract Lithological grouping of rock and soil samples was performed using the Fe2O3/Al2O3 and Al2O3/TiO2 ratios, in one attempt, and Fe2O3/Al2O3 and ZrO2/TiO2 ratios, in anotner. By and large, the two groupings were suitable for the rock samples, and the soil samples were often assigned to the same groups as those of the respective parent rocks. Hence, the lithological features of the parent rocks were considered to be well preserved in the course of profile development. The uniformity of the parent material within the profile was confirmed by the lithology index (LI) and TiO2/ZrO2 ratio except for the Yakuno, Niimi-1, Niimi-2, Sekinomiya-1, and Sekinomiya-2 soils. The value of the weathering index (WI) often increased from the C to the B horizon within the profile. But the WI value decreased from the B to the A horizon in eight of the sampled soils. The rejuvenation in the surface soil was ascribed either to the surface accumulation of bases associated with the biological cycling under the forest, or t...
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