Ferralitic soils from Brazil : formation and evolution of structure

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Date

1983

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Persée

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MESR

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Copyright PERSEE 2003-2023. Works reproduced on the PERSEE website are protected by the general rules of the Code of Intellectual Property. For strictly private, scientific or teaching purposes excluding all commercial use, reproduction and communication to the public of this document is permitted on condition that its origin and copyright are clearly mentionned.



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Armand Chauvel et al., « Ferralitic soils from Brazil : formation and evolution of structure », Sciences Géologiques, bulletins et mémoires, ID : 10670/1.17zuxh


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The stucfy of three ferrallitic soil sequences from Brazil, developed upon basalt, granite-rhyolite and detrital sedimentary rocks respectively, under different types of climate, confirms the mainly "pedoplasmic" nature of the question of the formation of the structure of these soils. The study also points out the existence of possibly different lineages leading to different "faciès" according to the nature of the parent material and pedobioclimatic conditions.

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