Pedogenesis and relict properties of soils with columnar structure from Roraima, north Amazonia

Detalhes bibliográficos
Autor(a) principal: Schaefer, Carlos E.R.
Data de Publicação: 1996
Outros Autores: Dalrymple, John
Tipo de documento: Artigo
Idioma: eng
Título da fonte: LOCUS Repositório Institucional da UFV
Texto Completo: https://doi.org/10.1016/0016-7061(95)00073-9
http://www.locus.ufv.br/handle/123456789/21669
Resumo: A toposequence of soils with columnar structure in the Paricarana catchment (Roraima State, north Amazonia) was studied. The soils occur within the driest part of tropical Amazonia. The two soils in the lower positions are magnesic, as well as sodic, displaying columnar structural peds. The upper slope position is calcium-saturated, associated with dry forest, whilst the the Mg/Na affected soils are associated with xerophytic savanna. The whole toposequence is being progressively acidified and leached (the solodization process), from the upper slope position to a maximum at the bottom of the toposequence. In spite of the high amounts of total Na,O in all three soils due to the presence of Na-plagioclase, the exchangeable level is concentrated in the lower slope positions, thus creating abrupt changes between the columnar Bt and the overlying A and E horizons. Morphologically, the resulting structural patterns of columnar peds are thought to reflect the effects of exchangeable magnesium plus sodium, more than sodium itself. The little variability in total amounts combined with large variability in the exchange levels suggest that differential redistribution of Na and Mg by overland-flow, throughflow and groundwater fluctuations is responsible for such Na/Mg accumulation in the bottom of the landscape. The present climatic regime, although seasonal, ought not to favour the presence of sodium/magnesium affected soils in this part of Amazonia. They possibly represent relict soils from former semiarid climates in north Amazonia, showing features of the degradation process currently underway.
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spelling Schaefer, Carlos E.R.Dalrymple, John2018-09-06T11:12:04Z2018-09-06T11:12:04Z1996-050016-7061https://doi.org/10.1016/0016-7061(95)00073-9http://www.locus.ufv.br/handle/123456789/21669A toposequence of soils with columnar structure in the Paricarana catchment (Roraima State, north Amazonia) was studied. The soils occur within the driest part of tropical Amazonia. The two soils in the lower positions are magnesic, as well as sodic, displaying columnar structural peds. The upper slope position is calcium-saturated, associated with dry forest, whilst the the Mg/Na affected soils are associated with xerophytic savanna. The whole toposequence is being progressively acidified and leached (the solodization process), from the upper slope position to a maximum at the bottom of the toposequence. In spite of the high amounts of total Na,O in all three soils due to the presence of Na-plagioclase, the exchangeable level is concentrated in the lower slope positions, thus creating abrupt changes between the columnar Bt and the overlying A and E horizons. Morphologically, the resulting structural patterns of columnar peds are thought to reflect the effects of exchangeable magnesium plus sodium, more than sodium itself. The little variability in total amounts combined with large variability in the exchange levels suggest that differential redistribution of Na and Mg by overland-flow, throughflow and groundwater fluctuations is responsible for such Na/Mg accumulation in the bottom of the landscape. The present climatic regime, although seasonal, ought not to favour the presence of sodium/magnesium affected soils in this part of Amazonia. They possibly represent relict soils from former semiarid climates in north Amazonia, showing features of the degradation process currently underway.engGeodermaVolume 71, Issues 1–2, Pages 1-17, May 1996Elsevier B.V.info:eu-repo/semantics/openAccessPedogenesisSoilsRoraimaNorth AmazoniaPedogenesis and relict properties of soils with columnar structure from Roraima, north Amazoniainfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfreponame:LOCUS Repositório Institucional da UFVinstname:Universidade Federal de Viçosa (UFV)instacron:UFVORIGINALartigo.pdfartigo.pdfTexto completoapplication/pdf1211796https://locus.ufv.br//bitstream/123456789/21669/1/artigo.pdf0886e74bdc096f658f5ad84d4529ea52MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://locus.ufv.br//bitstream/123456789/21669/2/license.txt8a4605be74aa9ea9d79846c1fba20a33MD52THUMBNAILartigo.pdf.jpgartigo.pdf.jpgIM Thumbnailimage/jpeg4785https://locus.ufv.br//bitstream/123456789/21669/3/artigo.pdf.jpg00f5587c63213ff5ee8e13fc4c0978e5MD53123456789/216692018-09-06 23:00:55.29oai:locus.ufv.br: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Repositório InstitucionalPUBhttps://www.locus.ufv.br/oai/requestfabiojreis@ufv.bropendoar:21452018-09-07T02:00:55LOCUS Repositório Institucional da UFV - Universidade Federal de Viçosa (UFV)false
dc.title.en.fl_str_mv Pedogenesis and relict properties of soils with columnar structure from Roraima, north Amazonia
title Pedogenesis and relict properties of soils with columnar structure from Roraima, north Amazonia
spellingShingle Pedogenesis and relict properties of soils with columnar structure from Roraima, north Amazonia
Schaefer, Carlos E.R.
Pedogenesis
Soils
Roraima
North Amazonia
title_short Pedogenesis and relict properties of soils with columnar structure from Roraima, north Amazonia
title_full Pedogenesis and relict properties of soils with columnar structure from Roraima, north Amazonia
title_fullStr Pedogenesis and relict properties of soils with columnar structure from Roraima, north Amazonia
title_full_unstemmed Pedogenesis and relict properties of soils with columnar structure from Roraima, north Amazonia
title_sort Pedogenesis and relict properties of soils with columnar structure from Roraima, north Amazonia
author Schaefer, Carlos E.R.
author_facet Schaefer, Carlos E.R.
Dalrymple, John
author_role author
author2 Dalrymple, John
author2_role author
dc.contributor.author.fl_str_mv Schaefer, Carlos E.R.
Dalrymple, John
dc.subject.pt-BR.fl_str_mv Pedogenesis
Soils
Roraima
North Amazonia
topic Pedogenesis
Soils
Roraima
North Amazonia
description A toposequence of soils with columnar structure in the Paricarana catchment (Roraima State, north Amazonia) was studied. The soils occur within the driest part of tropical Amazonia. The two soils in the lower positions are magnesic, as well as sodic, displaying columnar structural peds. The upper slope position is calcium-saturated, associated with dry forest, whilst the the Mg/Na affected soils are associated with xerophytic savanna. The whole toposequence is being progressively acidified and leached (the solodization process), from the upper slope position to a maximum at the bottom of the toposequence. In spite of the high amounts of total Na,O in all three soils due to the presence of Na-plagioclase, the exchangeable level is concentrated in the lower slope positions, thus creating abrupt changes between the columnar Bt and the overlying A and E horizons. Morphologically, the resulting structural patterns of columnar peds are thought to reflect the effects of exchangeable magnesium plus sodium, more than sodium itself. The little variability in total amounts combined with large variability in the exchange levels suggest that differential redistribution of Na and Mg by overland-flow, throughflow and groundwater fluctuations is responsible for such Na/Mg accumulation in the bottom of the landscape. The present climatic regime, although seasonal, ought not to favour the presence of sodium/magnesium affected soils in this part of Amazonia. They possibly represent relict soils from former semiarid climates in north Amazonia, showing features of the degradation process currently underway.
publishDate 1996
dc.date.issued.fl_str_mv 1996-05
dc.date.accessioned.fl_str_mv 2018-09-06T11:12:04Z
dc.date.available.fl_str_mv 2018-09-06T11:12:04Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.uri.fl_str_mv https://doi.org/10.1016/0016-7061(95)00073-9
http://www.locus.ufv.br/handle/123456789/21669
dc.identifier.issn.none.fl_str_mv 0016-7061
identifier_str_mv 0016-7061
url https://doi.org/10.1016/0016-7061(95)00073-9
http://www.locus.ufv.br/handle/123456789/21669
dc.language.iso.fl_str_mv eng
language eng
dc.relation.ispartofseries.pt-BR.fl_str_mv Volume 71, Issues 1–2, Pages 1-17, May 1996
dc.rights.driver.fl_str_mv Elsevier B.V.
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