Relationship between mineral composition or soil texture and available silicon in alluvial paddy soils on the Shounai Plain, Japan(Soil Fertility)

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概要

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• To evaluate the relationship between the amount of available Silicon (Si) in paddy soils and their mineral properties on the Shounai Plain in Japan, which is formed from several parent materials, we evaluated the amount of available Si, the particle size distribution, the oxide composition of crystalline minerals and the amount of oxalate-extractable Si (Si_o), iron (Fe_o) and aluminum (Al_o) in the soil. The amount of available Si in the soil and the oxide content of the crystalline minerals differed among four soil groups that were distinguished by their clay mineral composition. There was no difference in the particle size distribution among the soil groups. The amount of available Si was positively related to the SiO_2/Al_2O_3 ratio of clay, the CaO concentration of silt and fine sand, and the amounts of Si_o, Fe_o and Al_o in the soil. The amount of available Si in the soils was negative correlated with the Na_2O and K_2O concentrations of silt, the K_2O concentration of fine sand, and the coarse sand content. These results suggest that the amount of available Si in soils is affected by the weathering resistivity of their minerals and that the particle size distribution and mineral composition are related to the available Si of the soils. Mineralogical properties, including the particle size distribution and mineral composition such as the SiO_2/Al_2O_3 ratio × clay fraction content and the amounts of CaO and MgO in silt-sized particles, were positively correlated with the amount of available Si in the soil, but these correlations were not found for fine sand-sized particles. The Si_o, Fe_o and SiO_2/Al_2O_3 ratio × clay fraction contents contributed approximately 50% to the amount of available Si in the soils. The amount of available Si in the soil was divided into two groups according to the location of the paddy field. The amount of soil-available Si in the alluvial plain was affected by the geology upstream through the mineral composition.

著者

• Fujii Hiroshi

  Dep. Of Bioscience And Biotechnology Shinshu Univ.

• Kakuda Ken-ichi

  Faculty of Agriculture, Yamagata University

• Ando Ho

  Faculty of Agriculture, Yamagata University

• Ando H

  Faculty Of Agriculture Yamagata University

• Ando Ho

  Faculty Of Agriculture Kagawa University

• Sasaki Yuka

  Faculty Of Agriculture Yamagata University

• Ando Tadashi

  Yamagata Agricultural Experimental Station Shounai Branch:(present Office)industrial And Economic Af

• Kakuda K

  Faculty Of Agriculture Yamagata University

• Kakuda Ken-ichi

  Faculty Of Agriculture Yamagata University

• MAKABE Shuhei

  The United Graduate School of Agricultural Sciences, Iwate University

• FUJII Hiroshi

  Yamagata Agricultural Experimental Station, Shounai Branch

• Fujii H

  Yamagata Agricultural Experimental Station Shounai Branch

• Makabe Shuhei

  The United Graduate School Of Agricultural Sciences Iwate University

• Fujii Hiroshi

  Interdisciplinary Graduate School Of Science And Technology Shinshu University

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