Diffusion of Inorganic Materials in Soil

Long-established theory concerning the diffusion of solutes in soil is described, with particular reference to the means by which pH changes are propagated through soil by acid-base transfer. The application of the theory is then demonstrated by way of models of the reaction with soil or two importa...

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Autor principal: Kirk, G.J.D.
Formato: Journal Article
Lenguaje:Inglés
Publicado: Royal Society 1990
Materias:
Acceso en línea:https://hdl.handle.net/10568/167270
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author Kirk, G.J.D.
author_browse Kirk, G.J.D.
author_facet Kirk, G.J.D.
author_sort Kirk, G.J.D.
collection Repository of Agricultural Research Outputs (CGSpace)
description Long-established theory concerning the diffusion of solutes in soil is described, with particular reference to the means by which pH changes are propagated through soil by acid-base transfer. The application of the theory is then demonstrated by way of models of the reaction with soil or two important fertilizer materials (urea and rock phosphate) and a model of the diffusion and oxidation of ferrous iron in the rhizosphere of lowland rice. Experimental verifications of the urea and rock phosphate models are given, in which reactant concentration profiles in the soil are compared with model predictions based on independently measured parameter values. No parameter-fitting is used. A sensitivity analysis of the urea model shows how loss of urea-derived nitrogen by ammonia volatilization depends on fertilizer, soil and atmospheric parameters. A sensitivity analysis of the rock phosphate model shows how the rate of rockphosphate dissolution and the amount of dissolved phosphorus taken up by plant roots depend on fertilizer, soil and plant parameters including acid-base release by roots. A sensitivity analysis of the iron diffusion and oxidation model shows how rice roots may greatly alter chemical, conditions in the soil near them, with major implications for nutrient and toxin transformations.
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spelling CGSpace1672702025-12-08T10:29:22Z Diffusion of Inorganic Materials in Soil Kirk, G.J.D. inorganic materials soil Long-established theory concerning the diffusion of solutes in soil is described, with particular reference to the means by which pH changes are propagated through soil by acid-base transfer. The application of the theory is then demonstrated by way of models of the reaction with soil or two important fertilizer materials (urea and rock phosphate) and a model of the diffusion and oxidation of ferrous iron in the rhizosphere of lowland rice. Experimental verifications of the urea and rock phosphate models are given, in which reactant concentration profiles in the soil are compared with model predictions based on independently measured parameter values. No parameter-fitting is used. A sensitivity analysis of the urea model shows how loss of urea-derived nitrogen by ammonia volatilization depends on fertilizer, soil and atmospheric parameters. A sensitivity analysis of the rock phosphate model shows how the rate of rockphosphate dissolution and the amount of dissolved phosphorus taken up by plant roots depend on fertilizer, soil and plant parameters including acid-base release by roots. A sensitivity analysis of the iron diffusion and oxidation model shows how rice roots may greatly alter chemical, conditions in the soil near them, with major implications for nutrient and toxin transformations. 1990-09-29 2024-12-19T12:57:11Z 2024-12-19T12:57:11Z Journal Article https://hdl.handle.net/10568/167270 en Royal Society Kirk, G. J. D.. 1990. Diffusion of Inorganic Materials in Soil. Phil. Trans. R. Soc. Lond. B, Volume 329 no. 1255 p. 331-342
spellingShingle inorganic materials
soil
Kirk, G.J.D.
Diffusion of Inorganic Materials in Soil
title Diffusion of Inorganic Materials in Soil
title_full Diffusion of Inorganic Materials in Soil
title_fullStr Diffusion of Inorganic Materials in Soil
title_full_unstemmed Diffusion of Inorganic Materials in Soil
title_short Diffusion of Inorganic Materials in Soil
title_sort diffusion of inorganic materials in soil
topic inorganic materials
soil
url https://hdl.handle.net/10568/167270
work_keys_str_mv AT kirkgjd diffusionofinorganicmaterialsinsoil