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Ion Transport and Permeability in an Allophanic Andisol at Low pH
Title: | Ion Transport and Permeability in an Allophanic Andisol at Low pH |
Authors: | Ishiguro, Munehide Browse this author →KAKEN DB |
Keywords: | allophanic Andisol | flocculation | ion transport | permeability | soil dispersion |
Issue Date: | 2005 |
Publisher: | Taylor & Francis |
Journal Title: | Soil Science and Plant Nutrition |
Volume: | 51 |
Issue: | 5 |
Start Page: | 637 |
End Page: | 640 |
Publisher DOI: | 10.1111/j.1747-0765.2005.tb00080.x |
Abstract: | Allophanic Andisols have a significant pH-dependent charge. The positive charge increases and the negative charge decreases as pH decreases; therefore, anion movement becomes slower and cation movement becomes faster as pH decreases in the soil. At low pH, soil dispersion occurs easily due to electric repulsive force. The permeability of the soil then decreases because of structural changes that occur when dilute HCl or HNO3 is percolated in the soil. However, soil permeability does not decrease when dilute H2SO4 is percolated in the soil. This is because SO4 2- strongly adsorbs on the soil surface at low pH and the soil remains flocculated. |
Rights: | This is an Accepted Manuscript of an article published by Taylor & Francis in Soil Science and Plant Nutrition on 2005, available online: https://www.tandfonline.com/doi/abs/10.1111/j.1747-0765.2005.tb00080.x |
Type: | article (author version) |
URI: | http://hdl.handle.net/2115/70738 |
Appears in Collections: | 農学院・農学研究院 (Graduate School of Agriculture / Faculty of Agriculture) > 雑誌発表論文等 (Peer-reviewed Journal Articles, etc)
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Submitter: 石黒 宗秀
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