Distribution of charred plant fragments in particle size fractions of Japanese volcanic ash soils(Soil Chemistry and Mineralogy)
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概要
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To gain a better understanding of the distribution of charred plant fragment C (CPFC) and its contribution to organic C (OC) in the particle size fractions of Japanese volcanic ash soils, each of four soil samples was divided into six particle size fractions, namely three sand-sized aggregate (20-53, 53-212 and 212-2,000μm) fractions, one silt-sized aggregate (2-20μm) fraction, and two clay-sized aggregate (<0.2 and 0.2-2μm) fractions. Furthermore, after HCl-HF treatment of these aggregate fractions, sub-fractions of less than specific gravity (s.g.) 1.6gcm^<-3> (<1.6 fraction) were isolated using s.g. 1.6gcm^<-3> sodium polytungstate solution. Microscopic observation indicated that the charred plant fragments, which are black or blackish brown, were the main components in the <1.6 fractions. Therefore, the OC in this fraction was designated as CPFC. In all the soils studied, the quantitative distribution of the CPFC of the silt-sized aggregate fractions to total CPFC of whole soils, ranging from 59 to 84%, was greatest among the aggregate fractions. The sum of the distribution (%) values of the CPFC in the three sand-sized aggregate fractions varied from 6.9 to 33%, while that in the two clay-sized aggregate fractions ranged from 1.1 to 9.4%. Similar to the CPFC, in all soils, the quantitative distribution of the OC in the aggregate fractions was greater in the silt-sized aggregate fractions (52-76%) than in the other aggregate fractions (0.1-20%). In all soils, the quantitative contribution of total CPFC to total OC of whole soils ranged from 10 to 28%. The CPFC/OC values in the aggregate fractions were 21% or more in 10 samples from a total of 24 fractions, with a maximum value of 34%. On the basis of the findings obtained in the present study, it is assumed that in Japanese volcanic ash soils the silt-sized fraction is an important reservoir of CPFC and OC, and CPFC merits attention as one of the constituents of OC in particle size fractions.
- 社団法人日本土壌肥料学会の論文
著者
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Shindo Haruo
Faculty of Agriculture, Yamaguchi University
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NISHIMURA Syusaku
Faculty of Agriculture, Yamaguchi University
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Shindo Haruo
Faculty Of Agriculture Yamaguchi University
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NOGUCHI Takashi
Faculty of Agriculture, Yamaguchi University
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Nishimura Syusaku
Faculty Of Agriculture Yamaguchi University
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Shindo Haruo
Faculty Of Agriculture Nagoya University
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Noguchi Takashi
Faculty Of Agriculture Yamaguchi University
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