2005
DOI: 10.1111/j.1747-0765.2005.tb00080.x
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Ion Transport and Permeability in an Allophanic Andisol at Low pH

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 HNO, is percolated in the soil. However, soil permeability does not decrease when dilute &S… Show more

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Cited by 5 publications
(2 citation statements)
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“…The use of surfactants for soil washing to remove low-solubility organic contaminants, such as oils, also changes the inter-particle interactions and can result in a significant change in the hydraulic conductivity of porous media [279,283]. Electrolyte concentration, pH and specific ions that all likely affect the particle-particle interaction may also change the soil permeability [263,[288][289][290][291][292][293][294][295][296][297]. An example of the effect of surfactant adsorption on soil stability is depicted in Fig.…”
Section: Influence Of Surfactant Adsorption On Soil Structure and Permentioning
confidence: 99%
“…The use of surfactants for soil washing to remove low-solubility organic contaminants, such as oils, also changes the inter-particle interactions and can result in a significant change in the hydraulic conductivity of porous media [279,283]. Electrolyte concentration, pH and specific ions that all likely affect the particle-particle interaction may also change the soil permeability [263,[288][289][290][291][292][293][294][295][296][297]. An example of the effect of surfactant adsorption on soil stability is depicted in Fig.…”
Section: Influence Of Surfactant Adsorption On Soil Structure and Permentioning
confidence: 99%
“…The soil dispersed well and the permeability decreased well at pH 9 more than those at pH 6 for the montmorillonitic and the kaolinitic soil (Suarez et al 1984). The allophanic andisol dispersed well and the permeability decreased well at pH < 5 and pH >10 (Nakagawa and Ishiguro 1994;Ishiguro and Nakajima 2000;Ishiguro 2005). Therefore, pH is one of the most important factors when we consider the influence of dispersionflocculation.…”
Section: Introductionmentioning
confidence: 99%