1960
DOI: 10.1038/1881048a0
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Diffusion of Ions in Soils

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1963
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Cited by 21 publications
(6 citation statements)
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“…Two processes of mass-flow in the water absorbed by plant and diffusion of ions were involved, which could act differently across spatial and temporal scales. Factors, such as soil water content (Danielson and Russell 1957;Mederski and Wilson 1960), transpiration ratio (Brouwer 1954), relative extent of root system, concentration gradient at root interface (Barber 1962) and soil texture (Schofield and Graham 1960), could strongly affect the uptake of nutrients by plants.…”
Section: Introductionmentioning
confidence: 99%
“…Two processes of mass-flow in the water absorbed by plant and diffusion of ions were involved, which could act differently across spatial and temporal scales. Factors, such as soil water content (Danielson and Russell 1957;Mederski and Wilson 1960), transpiration ratio (Brouwer 1954), relative extent of root system, concentration gradient at root interface (Barber 1962) and soil texture (Schofield and Graham 1960), could strongly affect the uptake of nutrients by plants.…”
Section: Introductionmentioning
confidence: 99%
“…On the other hand, precise measurement of the dimensions of the system and of the quantities of ions transferred becomes much more difficult for a small apparatus. The method used for this work has been described previously (Schofield & Graham-Bryce, 1960;Graham-Bryce, 1963) and makes use of the fact tliat if a layer of soil containing radioactive tracer of the ion under investigation is placed in contact with an exactly similar layer without tracer, the radioactive concentration at the boundary immediately falls to half that of the initially active soil and remains at this value as a result of the diffusion of the tracer. If a thin permeable ion-exchange membrane which has previously been prepared in equilibrium with half the initial tracer concentration in the radioactive section is used to separate the two layers, the movement of ions in the soil is affected to a negligible extent provided the rate of diffusion in the membrane is fast enough relative to that in the soil, and provided the exchange capacity of the membrane is higher than that of the soil.…”
Section: Methodsmentioning
confidence: 99%
“…The values of the 'apparent' bulk diffusion coefficients, D', presented in Table z were calculated from the equation of Schofield and Graham-Bryce (1965) D' = ( r / t ) .…”
Section: Bulk Digusion Coeflcientsmentioning
confidence: 99%