SOIL PROPERTY COMPARISON BETWEEN ALLOPHANIC AND NON-ALLOPHANIC HORIZONS IN VOLCANIC ASH SOILS OF KYUSHU, JAPAN

Andosols, volcanic ash-derived soils, play a vital role in upland farming in Japan, with distinct categorization into allophanic and non-allophanic types. Allophanic Andosols, constituting 69.9% of the total Andosol land area in Japan, are prevalent in regions with significant Holocene tephra deposition. In contrast, non-allophanic Andosols, accounting for 30.1% of the total Andosol area, occur in areas with minor tephra deposition. Both categories exhibit distinctive characteristics such as a thick black A-horizon, high phosphate fixation, superior water retention, and low bulk density. Despite similarities in morphology, chemistry, and physical attributes, non-allophanic Andosols possess unique features due to the presence of 2:1 minerals. Notably, non-allophanic Andosols, characterized by substantial exchangeable aluminum (represented by exchangeable acidity y1), pose a significant challenge by inducing severe aluminum toxicity in common agricultural crops. Hence, distinguishing between allophanic and non-allophanic Andosols is crucial for effective agricultural management.

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2025-05-26
DOI
https://doi.org/10.5281/zenodo.15518062
Primary Topic
Clay minerals and soil interactions
Type
article
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article

SOIL PROPERTY COMPARISON BETWEEN ALLOPHANIC AND NON-ALLOPHANIC HORIZONS IN VOLCANIC ASH SOILS OF KYUSHU, JAPAN

Zenodo (CERN European Organization for Nuclear Research)
Clay minerals and soil interactions
article

SOIL PROPERTY COMPARISON BETWEEN ALLOPHANIC AND NON-ALLOPHANIC HORIZONS IN VOLCANIC ASH SOILS OF KYUSHU, JAPAN

article en

Abstract

Andosols, volcanic ash-derived soils, play a vital role in upland farming in Japan, with distinct categorization into allophanic and non-allophanic types. Allophanic Andosols, constituting 69.9% of the total Andosol land area in Japan, are prevalent in regions with significant Holocene tephra deposition. In contrast, non-allophanic Andosols, accounting for 30.1% of the total Andosol area, occur in areas with minor tephra deposition. Both categories exhibit distinctive characteristics such as a thick black A-horizon, high phosphate fixation, superior water retention, and low bulk density. Despite similarities in morphology, chemistry, and physical attributes, non-allophanic Andosols possess unique features due to the presence of 2:1 minerals. Notably, non-allophanic Andosols, characterized by substantial exchangeable aluminum (represented by exchangeable acidity y1), pose a significant challenge by inducing severe aluminum toxicity in common agricultural crops. Hence, distinguishing between allophanic and non-allophanic Andosols is crucial for effective agricultural management.

Zenodo (CERN European Organization for Nuclear Research)
Hirosaki University (JP), Tohoku University (JP), Aomori Prefectural Industrial Technology Center (JP)
Zero hunger
Openalex Percentile: Top 59%
Clay minerals and soil interactions
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SOIL PROPERTY COMPARISON BETWEEN ALLOPHANIC AND NON-ALLOPHANIC HORIZONS IN VOLCANIC ASH SOILS OF KYUSHU, JAPAN · Zenodo (CERN European Organization for Nuclear Research) (2025) | TGRS Research Map | TGRS