Abstract

Abstract In surface horizons (4 samples) and buried humic horizons (14 samples) derived from volcanic ash, the contents of total, fulvic acid. humic acid and humin carbon and nitrogen were determined. The C/N ratios and the percentage of carbon and nitrogen of each fraction in total carbon and nitrogen were calculated. These values varied with each soil profile and horizon. In the surface horizons and the buried humic horizons with age younger than 3,000 yrs. B.P., C/N ratios of soil samples, fulvic acid, and humic acid were low, and those of humin were distributed over a wide range. The C/N ratios increased in the order of fulvic acid, humic acid, humin among these soil samples. Among soil samples which have been buried from 3,000 to 28,000 yrs. B.P., the more were the total carbon contents of soil and also the fulvic acid, humic acid and humin carbon contents, the greater was the tendency of the C/N ratios to rise. The C/N ratios increased in the order of fulvic acid, humin, humic acid among these soil ...

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