Detalhes bibliográficos
Título da fonte: Repositório Institucional da UFMG
id UFMG_fbbf13d63950d9952d47b10c7cd3f151
oai_identifier_str oai:repositorio.ufmg.br:1843/52423
network_acronym_str UFMG
network_name_str Repositório Institucional da UFMG
repository_id_str
reponame_str Repositório Institucional da UFMG
instacron_str UFMG
institution Universidade Federal de Minas Gerais (UFMG)
instname_str Universidade Federal de Minas Gerais (UFMG)
spelling 2023-04-24T21:11:00Z2023-04-24T21:11:00Z2017-06-2717Especial259267https://doi.org/10.11606/rdg.v0ispe.1327212236-2878http://hdl.handle.net/1843/52423https://orcid.org/0000-0003-3336-7397https://orcid.org/0000-0001-7060-1598As baixas disponibilidade de água líquida e temperatura na Antártica condicionam a formação de solos incipientes. Condições climáticas menos severas na Antártica Marítima permitem o maior desenvolvimento de solos, com maior cobertura vegetal e intemperismo químico mais significativo. A Península Barton, localizada na Ilha Rei George (Antártica Marítima), possui solos derivados de litologias diversas, com destaque para o basalto/andesito piritizado, representando a área de maior extensão de materias sulfídicos na região. O objetivo deste trabalho foi analisar o papel do relevo na gênese de solos sulfatados e sua relação com a evolução da paisagem. Os solos foram classificados de acordo com a Soil Taxonomy e WRB/FAO. Foram descritos três perfis em toposequência e analisados seus atributos morfológicos, físicos, químicos e mineralógicos. A crioclastia está presente como um processo pedogenético, mas o que se destaca é o grau evolutivo dos solos associado à acidificação pela oxidação dos sulfetos. Esse processo promove a liberação de elementos como o Fe, que são mobilizados por influência do relevo. Consequentemente, formam-se niveis encouraçados, isto é, horizontes petroplínticos, caracterizando uma transformação da cobertura pedológica. A gênese destes solos demonstra que a paisagem periglacial é dinâmica e de profundo interesse das investigações pedogeomorfológicas.Antarctic soils are characterized by low development degree due to low liquid water content. Compared to mainland, Maritime Antactica has a mild climate. These milder conditions allow a much greater development of soils and more significant chemical weathering. The study area is Barton Peninsula, the second largest ice-free area of King George Island (Maritime Antarctica). The Barton Peninsula has soils derived from different lithologies, with basalt / andesite (with pyrite) standing out. This study aimed to evaluate the role of relief in the genesis of sulfated soils. Three pedons were selected, described, sampled, and classified according to Soil Taxonomy and WRB/FAO. Morphological, physical, mineralogical and chemical analysis were performed. The Barton soils present polygenic evolution. The rock shattering caused by freezing and thawing is present as a pedogenetic process. However, the evolution degree of the soils is substantially associated with the acidification by sulphide oxidation. This process promotes the release of elements, such as Fe, which are mobilized by the relief. Consequently, duricrusts (i.e. petroplintic horizons) are formed, characterizing a transformation of the pedological cover. The genesis of these soils shows that the peri-glacial landscape is dynamic and of deep interest in soil-geomorphological investigations.porUniversidade Federal de Minas GeraisUFMGBrasilIGC - DEPARTAMENTO DE GEOGRAFIARevista do Departamento de GeografiaOxidaçãoSulfetosCiência do soloOxidaçãoSulfetosPedogêneseConcreçõesPedogeomorfologiaSolos e evolução da paisagem em ambiente periglacial na Península Barton, Antártica marítimaSoils and landscape evolution in periglacial environment on the Barton Peninsula, maritime Antarcticainfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttps://www.revistas.usp.br/rdg/article/view/132721Davi do Vale LopesJosé João Lelis Leal de SouzaFábio Soares de OliveiraCarlos Ernesto Gonçalves Reynaud Schaeferapplication/pdfinfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UFMGinstname:Universidade Federal de Minas Gerais (UFMG)instacron:UFMGLICENSELicense.txtLicense.txttext/plain; charset=utf-82042https://repositorio.ufmg.br/bitstream/1843/52423/1/License.txtfa505098d172de0bc8864fc1287ffe22MD51ORIGINALsoloseevoluçãodapaisagem.pdfsoloseevoluçãodapaisagem.pdfapplication/pdf652413https://repositorio.ufmg.br/bitstream/1843/52423/2/soloseevolu%c3%a7%c3%a3odapaisagem.pdf80b8632fcbd1f7d3fcb1344b5efc6657MD521843/524232023-04-24 18:11:00.82oai:repositorio.ufmg.br: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Repositório InstitucionalPUBhttps://repositorio.ufmg.br/oaiopendoar:2023-04-24T21:11Repositório Institucional da UFMG - Universidade Federal de Minas Gerais (UFMG)false
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