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Registro Completo |
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Biblioteca(s): |
Embrapa Meio Norte / UEP-Parnaíba. |
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Data corrente: |
12/02/1996 |
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Data da última atualização: |
12/02/1996 |
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Autoria: |
WHITE, R. E. |
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Afiliação: |
University of Oxford. |
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Título: |
A model for nitratre leaching in undisturbed structured clay soil during unsteady flow. |
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Ano de publicação: |
1985 |
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Fonte/Imprenta: |
Journal of Hydrology, v.79, p.37-51, 1985. |
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Idioma: |
Inglês |
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Conteúdo: |
A two-domain mixing model is described for predicting nitrate leaching during unsteady unsaturated flow through soil. The model assumes that water infiltrating the soil surface mixes incompletely with resident water to form a miscible transport volume, the size of which can vary with time. Changes in solute storage within the transport volume can occur by diffusion and biological transformations. Output from the transport volume is by drainage from a lower surface in the soil. The model's output was tested against the measured amounts of NO3-N leached from large undisturbed cores of structured clay soil during constant flux irrigation with 10 mM CaCl2. The average concentration of NO-3 and Cl- in the soil solution was determined by extraction of smallcores taken around the large cores prior to leaching. The rate of nitrification in the soil was also measured. The change in the transport volume with time was calculated from equations for the mass balance of water and Cl- in the transport volume. Knowing the transport volume, analogous equations in terms of NO-3 were solved to predict the NO-3 concentration in the effluent. Good agreement between predicted and observed NO3-N leached was obtained for cores showing divergent trends in NO-3 leaching. A large difference between cores in the fraction of soil NO3-N leached (0.34 compared to 0.13) was attributed to the difference in the volume of high-nitrate soil water that mixed with infiltrating water to form the transport volume, and to differences in... MenosA two-domain mixing model is described for predicting nitrate leaching during unsteady unsaturated flow through soil. The model assumes that water infiltrating the soil surface mixes incompletely with resident water to form a miscible transport volume, the size of which can vary with time. Changes in solute storage within the transport volume can occur by diffusion and biological transformations. Output from the transport volume is by drainage from a lower surface in the soil. The model's output was tested against the measured amounts of NO3-N leached from large undisturbed cores of structured clay soil during constant flux irrigation with 10 mM CaCl2. The average concentration of NO-3 and Cl- in the soil solution was determined by extraction of smallcores taken around the large cores prior to leaching. The rate of nitrification in the soil was also measured. The change in the transport volume with time was calculated from equations for the mass balance of water and Cl- in the transport volume. Knowing the transport volume, analogous equations in terms of NO-3 were solved to predict the NO-3 concentration in the effluent. Good agreement between predicted and observed NO3-N leached was obtained for cores showing divergent trends in NO-3 leaching. A large difference between cores in the fraction of soil NO3-N leached (0.34 compared to 0.13) was attributed to the difference in the volume of high-nitrate soil water that mixed with infiltrating water to form the transport volume,... Mostrar Tudo |
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Palavras-Chave: |
Chloride; Lixiviacao de nitrato; Nitrate; Nitrate leaching. |
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Thesagro: |
Argila; Cloreto; Drenagem; Lixiviação; Nitrato. |
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Thesaurus Nal: |
clay; drainage; leaching. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 02192naa a2200265 a 4500
001 1075987
005 1996-02-12
008 1985 bl --- 0-- u #d
100 1 $aWHITE, R. E.
245 $aA model for nitratre leaching in undisturbed structured clay soil during unsteady flow.
260 $c1985
520 $aA two-domain mixing model is described for predicting nitrate leaching during unsteady unsaturated flow through soil. The model assumes that water infiltrating the soil surface mixes incompletely with resident water to form a miscible transport volume, the size of which can vary with time. Changes in solute storage within the transport volume can occur by diffusion and biological transformations. Output from the transport volume is by drainage from a lower surface in the soil. The model's output was tested against the measured amounts of NO3-N leached from large undisturbed cores of structured clay soil during constant flux irrigation with 10 mM CaCl2. The average concentration of NO-3 and Cl- in the soil solution was determined by extraction of smallcores taken around the large cores prior to leaching. The rate of nitrification in the soil was also measured. The change in the transport volume with time was calculated from equations for the mass balance of water and Cl- in the transport volume. Knowing the transport volume, analogous equations in terms of NO-3 were solved to predict the NO-3 concentration in the effluent. Good agreement between predicted and observed NO3-N leached was obtained for cores showing divergent trends in NO-3 leaching. A large difference between cores in the fraction of soil NO3-N leached (0.34 compared to 0.13) was attributed to the difference in the volume of high-nitrate soil water that mixed with infiltrating water to form the transport volume, and to differences in...
650 $aclay
650 $adrainage
650 $aleaching
650 $aArgila
650 $aCloreto
650 $aDrenagem
650 $aLixiviação
650 $aNitrato
653 $aChloride
653 $aLixiviacao de nitrato
653 $aNitrate
653 $aNitrate leaching
773 $tJournal of Hydrology$gv.79, p.37-51, 1985.
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Embrapa Meio Norte / UEP-Parnaíba (CPAMN-UEPP) |
