Agrupamentos de amostras circulares em função das unidades de solo

The objective of the study was to analyze the features of the relief through the variables: maximum altitude (HM); mean altitude (Hmd); minimum altitude (Hm); altitude range (H); average slope length (CVm); minimum length of run-off (Cd) and average steepness of circular samples (I) of the Capivara...

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Detalhes bibliográficos
Autores: Campos, Sérgio [UNESP], Pissarra, Teresa Cristina Tarlé [UNESP], Traficante, Daniela Polizeli [UNESP], Carrega, Ellen Fittipaldi Brasílio [UNESP], Zanata, Marcelo [UNESP], Reis, Fabiana Camargo dos [UNESP]
Formato: artículo
Estado:Versión publicada
Fecha de publicación:2014
País:Brasil
Recursos:Universidade Estadual Paulista (UNESP)
Repositorio:Repositório Institucional da UNESP
Idioma:portugués
OAI Identifier:oai:repositorio.unesp.br:11449/137467
Acesso em linha:http://dx.doi.org/10.15809/irriga.2014v19n2p174
http://hdl.handle.net/11449/137467
Access Level:acceso abierto
Palavra-chave:Multivariable analysis
Watershed
Relief
Análise multivariada
Bacia hidrográfica
Relevo
Descrição
Resumo:The objective of the study was to analyze the features of the relief through the variables: maximum altitude (HM); mean altitude (Hmd); minimum altitude (Hm); altitude range (H); average slope length (CVm); minimum length of run-off (Cd) and average steepness of circular samples (I) of the Capivara River Watershed – Botucatu (SP). A total of 4 circular samples were obtained per unit of soil (Quartzipsamment alfisol oxisol - RQ, Udox - LVA and Udorthent - RL). Multivariable analysis and aerial color photographs of 2000, Brazilian Chart and Soil Chart of Botucatu city-SP were used for data analyses. Soil differentiation was performed using the Student-t Test for analyzes of orthogonal contrasts among means of the three soils and analysis of groupings and major components. The grouping analysis of the variables of relief differentiated 75% of LVA and 100% of RL and RQ soil circular samples. The most efficient parameters of relief for differentiation of soils according to their order of importance were as follows: HM, Hm, Hmd and H.