Nigeria Journal of Science, 1. Study of soil surface causts in the loess plain soils of Northen Nigeria / Kowal, J.

Public ISBD Titre de série : Nigeria Journal of Science, 1 Titre : Study of soil surface causts in the loess plain soils of Northen Nigeria Type de document : texte imprimé Auteurs : Kowal, J. Année de publication : July 1972 ISBN/ISSN/EAN : CI-04506 Note générale : Surface crusting in the cultivated loessic soils at Samaru, Nigeria, resultats from the breakdown of soil agregates due to rainfall impact and slaking. The surface crusts or caps consist of horizontal beddings and laminae of soil particules in a dispersed and compact condition. The macroporosity of crusts is reduced from about 17 to about 10 per cent with a consequent decrease in infiltration and increase in run-off. In spite of increased run-off surface crust are very effective in protecting soil against accelerated erosion. Drycrusts are unlikely to interfere with soil aeration, but under wet conditions diffusion of gases across the surface soil is reducd and this may have an adverse efect on crops. Langues : Anglais (eng) Mots-clés : Sol  Pédologie  Occupation du sol  Système de culture  Infiltration  Ruissellement  Croûte superficielle  Calcul hydraulique Index. décimale : 631.4 Pédologie, science et préservation des sols : chimie, physique, fertilité Résumé : Surface crusting in the cultivated loessic soils at Samaru, Nigeria, resultats from the breakdown of soil agregates due to rainfall impact and slaking. The surface crusts or caps consist of horizontal beddings and laminae of soil particules in a dispersed and compact condition. The macroporosity of crusts is reduced from about 17 to about 10 per cent with a consequent decrease in infiltration and increase in run-off. In spite of increased run-off surface crust are very effective in protecting soil against accelerated erosion. Drycrusts are unlikely to interfere with soil aeration, but under wet conditions diffusion of gases across the surface soil is reducd and this may have an adverse efect on crops. Note de contenu : Surface crusting in the cultivated loessic soils at Samaru, Nigeria, resultats from the breakdown of soil agregates due to rainfall impact and slaking. The surface crusts or caps consist of horizontal beddings and laminae of soil particules in a dispersed and compact condition. The macroporosity of crusts is reduced from about 17 to about 10 per cent with a consequent decrease in infiltration and increase in run-off. In spite of increased run-off surface crust are very effective in protecting soil against accelerated erosion. Drycrusts are unlikely to interfere with soil aeration, but under wet conditions diffusion of gases across the surface soil is reducd and this may have an adverse efect on crops. Nigeria Journal of Science, 1. Study of soil surface causts in the loess plain soils of Northen Nigeria [texte imprimé] / Kowal, J. . - July 1972. ISSN : CI-04506 Surface crusting in the cultivated loessic soils at Samaru, Nigeria, resultats from the breakdown of soil agregates due to rainfall impact and slaking. The surface crusts or caps consist of horizontal beddings and laminae of soil particules in a dispersed and compact condition. The macroporosity of crusts is reduced from about 17 to about 10 per cent with a consequent decrease in infiltration and increase in run-off. In spite of increased run-off surface crust are very effective in protecting soil against accelerated erosion. Drycrusts are unlikely to interfere with soil aeration, but under wet conditions diffusion of gases across the surface soil is reducd and this may have an adverse efect on crops. Langues : Anglais (eng) Mots-clés : Sol  Pédologie  Occupation du sol  Système de culture  Infiltration  Ruissellement  Croûte superficielle  Calcul hydraulique Index. décimale : 631.4 Pédologie, science et préservation des sols : chimie, physique, fertilité Résumé : Surface crusting in the cultivated loessic soils at Samaru, Nigeria, resultats from the breakdown of soil agregates due to rainfall impact and slaking. The surface crusts or caps consist of horizontal beddings and laminae of soil particules in a dispersed and compact condition. The macroporosity of crusts is reduced from about 17 to about 10 per cent with a consequent decrease in infiltration and increase in run-off. In spite of increased run-off surface crust are very effective in protecting soil against accelerated erosion. Drycrusts are unlikely to interfere with soil aeration, but under wet conditions diffusion of gases across the surface soil is reducd and this may have an adverse efect on crops. Note de contenu : Surface crusting in the cultivated loessic soils at Samaru, Nigeria, resultats from the breakdown of soil agregates due to rainfall impact and slaking. The surface crusts or caps consist of horizontal beddings and laminae of soil particules in a dispersed and compact condition. The macroporosity of crusts is reduced from about 17 to about 10 per cent with a consequent decrease in infiltration and increase in run-off. In spite of increased run-off surface crust are very effective in protecting soil against accelerated erosion. Drycrusts are unlikely to interfere with soil aeration, but under wet conditions diffusion of gases across the surface soil is reducd and this may have an adverse efect on crops.

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