2012
DOI: 10.1590/s0006-87052012005000005
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Espectrorradiometria de solos e comparação com sensores orbitais

Abstract: ResumoEste trabalho teve por objetivo caracterizar e comparar o comportamento espectral de diferentes classes de solo obtidos de sensores orbitais e terrestres. Para tanto, em Rafard (SP), uma área de 184 ha foi estaqueada em grade regular de 100 x 100 m e amostras de solo foram coletadas e seus pontos georreferenciados. Posteriormente, foram obtidas as curvas espectrais das amostras com o sensor IRIS e os pontos amostrais, sobrepostos às imagens Landsat e ASTER da área para coleta dos dados espectrais orbitai… Show more

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Cited by 7 publications
(5 citation statements)
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References 12 publications
(6 reference statements)
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“…This, however, does not interfere in soil classification but in its discrimination. Interpretation of surface curves allows initial inference of probable soil characteristics, agreeing with Genú and Demattê (2012). Data on soil surface may be related to altitude, relief and affect soil classes.…”
Section: Comparison Between the Rs Techniques Used In Soil Mappingmentioning
confidence: 66%
“…This, however, does not interfere in soil classification but in its discrimination. Interpretation of surface curves allows initial inference of probable soil characteristics, agreeing with Genú and Demattê (2012). Data on soil surface may be related to altitude, relief and affect soil classes.…”
Section: Comparison Between the Rs Techniques Used In Soil Mappingmentioning
confidence: 66%
“…This fact was related to the large soil area still exposed during data collection; in these phenological stages, the soil was only partially covered by the crambe canopy. The soil of the experimental area was rich in iron oxide, causing the red tonality, which may have contributed to this behaviour (Sousa Jr., Demattê, & Genú, 2008;Genú & Demattê, 2012).…”
Section: Harvestmentioning
confidence: 99%
“…Para esta investigación, en esta región del espectro se manifiesta la caolinita. Según Genú & Demattê (2012), la caolinita se manifiesta en los picos ubicados a 1900 y 2200 nm para diferentes clases de suelo. Para los suelos de Carimagua, este es el mineral predominante en la fracción arcilla.…”
Section: Colombia Forestalunclassified