Soil Properties of Allophanic and Non-allophanic Horizons of Volcanic Ash Soil in Kyushu District, Japan
Abstract
This study examined the contrasting physical and chemical properties of allophanic and non-allophanic horizons in Japanese volcanic ash soils described in the Soil Survey Data Book before Land Reclamation. A total of 748 investigation points and 1570 soil horizons from the Kyushu District were divided into two groups based on their exchange acidity y1: allophanic horizons y1< 6 and non-allophanic horizons y1> 6. Volcanic ash soils from the Kyushu District were characterized as dark, weakly adherent, soft, dry, humic, and active-Al rich. Soil acidities of the two horizons had significantly different pH, exchange acidity y1, and exchangeable Ca. Mean humus content of LayerⅠ(topsoil), Ⅱ(subsoil), and Ⅲ(deeper subsoil) were 11.1±5.8, 9.7±6.0, and 7.6±6.0%, respectively, for allophanic horizons and 8.2±7.0, 6.7±6.9, and 4.4±5.3%, respectively, for non-allophanic horizons. Humus content of non-allophanic horizon was relatively lower compared to allophanic horizons in the Kyushu District.
Full Text: PDF DOI: 10.15640/jaes.v10n2a5
Abstract
This study examined the contrasting physical and chemical properties of allophanic and non-allophanic horizons in Japanese volcanic ash soils described in the Soil Survey Data Book before Land Reclamation. A total of 748 investigation points and 1570 soil horizons from the Kyushu District were divided into two groups based on their exchange acidity y1: allophanic horizons y1< 6 and non-allophanic horizons y1> 6. Volcanic ash soils from the Kyushu District were characterized as dark, weakly adherent, soft, dry, humic, and active-Al rich. Soil acidities of the two horizons had significantly different pH, exchange acidity y1, and exchangeable Ca. Mean humus content of LayerⅠ(topsoil), Ⅱ(subsoil), and Ⅲ(deeper subsoil) were 11.1±5.8, 9.7±6.0, and 7.6±6.0%, respectively, for allophanic horizons and 8.2±7.0, 6.7±6.9, and 4.4±5.3%, respectively, for non-allophanic horizons. Humus content of non-allophanic horizon was relatively lower compared to allophanic horizons in the Kyushu District.
Full Text: PDF DOI: 10.15640/jaes.v10n2a5
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