CLIMATE AND ZONAL SOIL DISTRIBUTION IN RIO GRANDE DO SUL - BRAZIL
Autor(a) principal: | |
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Data de Publicação: | 2017 |
Outros Autores: | , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Revista Geografar |
Texto Completo: | https://revistas.ufpr.br/geografar/article/view/44633 |
Resumo: | The weather has great influence on the soils formation, besides the integrated action of factors as source material, relief, organisms and time. The zonal soils are formed when the weather is a major factor in weathering. This study aimed to highlight the zonal soils of Rio Grande do Sul and determine its location. The spatial distribution of climate resources for the development of zonal soils was performed using the annual averages, the annual average of total pluvial precipitation and the annual average of air temperature, between 1931 and 1960 of 41 weather stations of the 8th Meteorology District (8 DISME). It was found that the zonal soils of Rio Grande do Sul comprehend Lateritic soils and Pedalférricos soils. Soils of very humid climate are located in the northern half of the state with annual average of total pluvial precipitation above 1,500 mm and are represented by Lateritic soils predominantly Oxisols. The Pedalférricos occur preferentially in temperate regions and are described as soils with pronounced leaching occurring in chemical weathering conditions with annual average of total pluvial precipitation above 600mm. In Rio Grande do Sul the ideal climatic conditions for the formation of these soils are recorded at meteorological stations located in Central Depression (with the exception of stations of Santa Maria and Santa Cruz do Sul), in South-Riograndense Shield (with the exception of Cacapava do Sul), in the coastal plain and in the North of Rio Grande Plateau just Vacaria region and are represented predominantly by Neossolos and Cambisols.Keywords: Laterites; Pedalfers; Latossols. |
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CLIMATE AND ZONAL SOIL DISTRIBUTION IN RIO GRANDE DO SUL - BRAZILCLIMA E DISTRIBUIÇÃO DOS SOLOS ZONAIS NO RIO GRANDE DO SUL – BRASILLateríticos; Pedalférricos; Latossolos.Keywords: Laterites; Pedalfers; LatossolsThe weather has great influence on the soils formation, besides the integrated action of factors as source material, relief, organisms and time. The zonal soils are formed when the weather is a major factor in weathering. This study aimed to highlight the zonal soils of Rio Grande do Sul and determine its location. The spatial distribution of climate resources for the development of zonal soils was performed using the annual averages, the annual average of total pluvial precipitation and the annual average of air temperature, between 1931 and 1960 of 41 weather stations of the 8th Meteorology District (8 DISME). It was found that the zonal soils of Rio Grande do Sul comprehend Lateritic soils and Pedalférricos soils. Soils of very humid climate are located in the northern half of the state with annual average of total pluvial precipitation above 1,500 mm and are represented by Lateritic soils predominantly Oxisols. The Pedalférricos occur preferentially in temperate regions and are described as soils with pronounced leaching occurring in chemical weathering conditions with annual average of total pluvial precipitation above 600mm. In Rio Grande do Sul the ideal climatic conditions for the formation of these soils are recorded at meteorological stations located in Central Depression (with the exception of stations of Santa Maria and Santa Cruz do Sul), in South-Riograndense Shield (with the exception of Cacapava do Sul), in the coastal plain and in the North of Rio Grande Plateau just Vacaria region and are represented predominantly by Neossolos and Cambisols.Keywords: Laterites; Pedalfers; Latossols.O clima tem grande influência na formação dos solos, além da ação integrada de fatores como material de origem, relevo, organismos e tempo. Os solos zonais são formados quando o clima é o fator preponderante no intemperismo. Neste estudo objetivou-se evidenciar os solos zonais do Rio Grande do Sul e determinar sua localização. A espacialização das disponibilidades climáticas para o desenvolvimento de solos zonais foi realizada utilizando-se as médias anuais, as médias dos totais anuais de precipitação pluvial e as médias anuais de temperatura do ar, entre 1931 e 1960, de 41 estações meteorológicas do 8° Distrito de Meteorologia (8º DISME). Constatou-se que os solos zonais do Rio Grande do Sul compreendem solos Lateríticos e solos Pedalférricos. Solos de clima muito úmido situam-se na metade norte do Estado com médias anuais de precipitação pluvial acima de 1.500mm e são representados pelos solos Lateríticos, predominantemente, os Latossolos. Os Pedalférricos ocorrem, preferencialmente, em regiões de clima temperado e são descritos como solos com pronunciada lixiviação, que ocorrem em condições de intemperismo químico com índices de precipitação anual acima de 600mm. No Rio Grande do Sul as condições climáticas ideais para a formação desses solos são registradas nas estações meteorológicas localizadas na Depressão Central (com exceção das estações de Santa Maria e Santa Cruz do Sul), no Escudo Sul-Riograndense (com exceção de Caçapava do Sul), na Planície Costeira e no Planalto Norte-rio-grandense (apenas a região de Vacaria). São representados, predominantemente pelos Neossolos e Cambissolos. Palavras-Chave: Lateríticos; Pedalférricos; Latossolos.UFPRBecker, Elsbeth Léia SpodeBuriol, Galileo AdeliStreck, Nereu Augusto2017-11-06info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionimage/jpegapplication/pdfhttps://revistas.ufpr.br/geografar/article/view/4463310.5380/geografar.v12i1.44633REVISTA GEOGRAFAR; v. 12, n. 1 (2017); 112-1291981-089X10.5380/geografar.v12i1reponame:Revista Geografarinstname:Universidade Federal do Paraná (UFPR)instacron:UFPRporhttps://revistas.ufpr.br/geografar/article/view/44633/33815https://revistas.ufpr.br/geografar/article/view/44633/33814Direitos autorais 2017 Revista Geografarinfo:eu-repo/semantics/openAccess2018-01-21T04:06:52Zoai:revistas.ufpr.br:article/44633Revistahttps://revistas.ufpr.br/geografarPUBhttps://revistas.ufpr.br/geografar/oai||geografar@ufpr.br1981-089X1981-089Xopendoar:2018-01-21T04:06:52Revista Geografar - Universidade Federal do Paraná (UFPR)false |
dc.title.none.fl_str_mv |
CLIMATE AND ZONAL SOIL DISTRIBUTION IN RIO GRANDE DO SUL - BRAZIL CLIMA E DISTRIBUIÇÃO DOS SOLOS ZONAIS NO RIO GRANDE DO SUL – BRASIL |
title |
CLIMATE AND ZONAL SOIL DISTRIBUTION IN RIO GRANDE DO SUL - BRAZIL |
spellingShingle |
CLIMATE AND ZONAL SOIL DISTRIBUTION IN RIO GRANDE DO SUL - BRAZIL Becker, Elsbeth Léia Spode Lateríticos; Pedalférricos; Latossolos. Keywords: Laterites; Pedalfers; Latossols |
title_short |
CLIMATE AND ZONAL SOIL DISTRIBUTION IN RIO GRANDE DO SUL - BRAZIL |
title_full |
CLIMATE AND ZONAL SOIL DISTRIBUTION IN RIO GRANDE DO SUL - BRAZIL |
title_fullStr |
CLIMATE AND ZONAL SOIL DISTRIBUTION IN RIO GRANDE DO SUL - BRAZIL |
title_full_unstemmed |
CLIMATE AND ZONAL SOIL DISTRIBUTION IN RIO GRANDE DO SUL - BRAZIL |
title_sort |
CLIMATE AND ZONAL SOIL DISTRIBUTION IN RIO GRANDE DO SUL - BRAZIL |
author |
Becker, Elsbeth Léia Spode |
author_facet |
Becker, Elsbeth Léia Spode Buriol, Galileo Adeli Streck, Nereu Augusto |
author_role |
author |
author2 |
Buriol, Galileo Adeli Streck, Nereu Augusto |
author2_role |
author author |
dc.contributor.none.fl_str_mv |
|
dc.contributor.author.fl_str_mv |
Becker, Elsbeth Léia Spode Buriol, Galileo Adeli Streck, Nereu Augusto |
dc.subject.por.fl_str_mv |
Lateríticos; Pedalférricos; Latossolos. Keywords: Laterites; Pedalfers; Latossols |
topic |
Lateríticos; Pedalférricos; Latossolos. Keywords: Laterites; Pedalfers; Latossols |
description |
The weather has great influence on the soils formation, besides the integrated action of factors as source material, relief, organisms and time. The zonal soils are formed when the weather is a major factor in weathering. This study aimed to highlight the zonal soils of Rio Grande do Sul and determine its location. The spatial distribution of climate resources for the development of zonal soils was performed using the annual averages, the annual average of total pluvial precipitation and the annual average of air temperature, between 1931 and 1960 of 41 weather stations of the 8th Meteorology District (8 DISME). It was found that the zonal soils of Rio Grande do Sul comprehend Lateritic soils and Pedalférricos soils. Soils of very humid climate are located in the northern half of the state with annual average of total pluvial precipitation above 1,500 mm and are represented by Lateritic soils predominantly Oxisols. The Pedalférricos occur preferentially in temperate regions and are described as soils with pronounced leaching occurring in chemical weathering conditions with annual average of total pluvial precipitation above 600mm. In Rio Grande do Sul the ideal climatic conditions for the formation of these soils are recorded at meteorological stations located in Central Depression (with the exception of stations of Santa Maria and Santa Cruz do Sul), in South-Riograndense Shield (with the exception of Cacapava do Sul), in the coastal plain and in the North of Rio Grande Plateau just Vacaria region and are represented predominantly by Neossolos and Cambisols.Keywords: Laterites; Pedalfers; Latossols. |
publishDate |
2017 |
dc.date.none.fl_str_mv |
2017-11-06 |
dc.type.none.fl_str_mv |
|
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://revistas.ufpr.br/geografar/article/view/44633 10.5380/geografar.v12i1.44633 |
url |
https://revistas.ufpr.br/geografar/article/view/44633 |
identifier_str_mv |
10.5380/geografar.v12i1.44633 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://revistas.ufpr.br/geografar/article/view/44633/33815 https://revistas.ufpr.br/geografar/article/view/44633/33814 |
dc.rights.driver.fl_str_mv |
Direitos autorais 2017 Revista Geografar info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Direitos autorais 2017 Revista Geografar |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
image/jpeg application/pdf |
dc.publisher.none.fl_str_mv |
UFPR |
publisher.none.fl_str_mv |
UFPR |
dc.source.none.fl_str_mv |
REVISTA GEOGRAFAR; v. 12, n. 1 (2017); 112-129 1981-089X 10.5380/geografar.v12i1 reponame:Revista Geografar instname:Universidade Federal do Paraná (UFPR) instacron:UFPR |
instname_str |
Universidade Federal do Paraná (UFPR) |
instacron_str |
UFPR |
institution |
UFPR |
reponame_str |
Revista Geografar |
collection |
Revista Geografar |
repository.name.fl_str_mv |
Revista Geografar - Universidade Federal do Paraná (UFPR) |
repository.mail.fl_str_mv |
||geografar@ufpr.br |
_version_ |
1788990019396960256 |