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Registro Completo |
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
22/11/2002 |
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Data da última atualização: |
22/11/2002 |
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Autoria: |
SMECK, N. E.; THOMPSON, M. L.; NORTON, L. D.; SHIPITALO, M. J. |
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Título: |
Weathering discontinuities: a key to fragipan formation |
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Ano de publicação: |
1989 |
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Fonte/Imprenta: |
In: SMECK, N.E.; CIOLKOSZ, E.J. Fragipans: their occurrence, classificacao and genesis. Madison: Soil Science Society of America, 1989. (SSSA. Special Publication, 24). |
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Páginas: |
p.99-112 |
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Idioma: |
Inglês |
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Conteúdo: |
Recently, numerous studies of soils with fragipans have been conducted in Ohio.This chapter is an attempt to collale the Ohio data with that available in the literature in order to formulate a general theory applicable to the formation of fragipans. Six pedons were selected to illustrate various pedogenetic scenarios in Ohio resulting in fragipan development and contributing to the development of our theory. Based on data for these pedons, it is concluded that fragipans form at weathering discontinuities originating either as a result of a wethering front or due to the occurrence of a lithologic or chronologic discontinuities due to an interaction between acid weathering products and components present in relatively unweathered material to form a bonding agentThis theory is presented for additional testing and evaluation |
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Palavras-Chave: |
Estados Unidos; Solos. |
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Thesaurus Nal: |
fragipans. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 01477naa a2200205 a 4500
001 1327882
005 2002-11-22
008 1989 bl uuuu u00u1 u #d
100 1 $aSMECK, N. E.
245 $aWeathering discontinuities$ba key to fragipan formation
260 $c1989
300 $ap.99-112
520 $aRecently, numerous studies of soils with fragipans have been conducted in Ohio.This chapter is an attempt to collale the Ohio data with that available in the literature in order to formulate a general theory applicable to the formation of fragipans. Six pedons were selected to illustrate various pedogenetic scenarios in Ohio resulting in fragipan development and contributing to the development of our theory. Based on data for these pedons, it is concluded that fragipans form at weathering discontinuities originating either as a result of a wethering front or due to the occurrence of a lithologic or chronologic discontinuities due to an interaction between acid weathering products and components present in relatively unweathered material to form a bonding agentThis theory is presented for additional testing and evaluation
650 $afragipans
653 $aEstados Unidos
653 $aSolos
700 1 $aTHOMPSON, M. L.
700 1 $aNORTON, L. D.
700 1 $aSHIPITALO, M. J.
773 $tIn: SMECK, N.E.; CIOLKOSZ, E.J. Fragipans: their occurrence, classificacao and genesis. Madison: Soil Science Society of America, 1989. (SSSA. Special Publication, 24).
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Registro original: |
Embrapa Solos (CNPS) |
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