Fechar

@MastersThesis{Pizarro:1999:SeReHi,
               author = "Pizarro, Marco Antonio",
                title = "Sensoriamento remoto hiperespectral para a 
                         caracteriza{\c{c}}{\~a}o e identifica{\c{c}}{\~a}o mineral em 
                         solos tropicais",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "1999",
              address = "Sao Jose dos Campos",
                month = "1999-06-21",
             keywords = "Espectr{\^o}metro de imageamento, sensoriamento remoto, 
                         espectr{\^o}metro imageador aerotransportado no vis{\'{\i}}vel 
                         e infravermelho (AVIRIS), solos, identifica{\c{c}}{\~a}o 
                         mineral, reflect{\^a}ncia, an{\'a}lise por componente principal, 
                         imaging spectrometer, remote sensing, airborne visible/infrared 
                         imaging spectrometer (AVIRIS), soils, mineral indetification, 
                         reflectance, Principal Components Analysis (PCA).",
             abstract = "O objetivo do presente trabalho foi avaliar o uso dos dados 
                         gerados pelo espectr{\^o}metro imageador Airborne 
                         Visible/InfraRed Imaging Spectrometer (AVIRIS) durante a 
                         miss{\~a}o Smoke, Sulfate, Clouds, and Radiation - Brazil 
                         (SCAR-B), no per{\'{\i}}odo de agosto a setembro de 1995, para a 
                         caracteriza{\c{c}}{\~a}o espectral e identifica{\c{c}}{\~a}o 
                         mineral em solos de uma area de estudo localizada pr{\'o}ximo a 
                         cidade de Campo Grande (MS). As imagens foram convertidas de 
                         valores de radi{\^a}ncia para reflect{\^a}ncia de 
                         superf{\'{\i}}cie, atrav{\'e}s de um m{\'e}todo de 
                         corre{\c{c}}{\~a}o atmosf{\'e}rica baseado no modelo MODTRAN. 
                         Para facilitar a an{\'a}lise das caracter{\'{\i}}sticas 
                         espectrais da {\'a}rea de estudo e da discrimina{\c{c}}{\~a}o 
                         dos principais tipos de solos presentes, a An{\'a}lise por 
                         Componentes Principais (ACP) foi aplicada sobre as imagens 
                         Airborne Visible InfraRed Imaging Spectrometer (AVIRIS) para 
                         reduzir a alta dimensionalidade de seu conjunto de bandas. As 
                         rela{\c{c}}{\~o}es entre as curvas espectrais obtidas para 18 
                         amostras de solos em laborat{\'o}rio pelo sensor InfraRed 
                         Intelligent Spectrometer (IRIS) e os espectros AVIRIS de pixels 
                         aproximadamente correspondentes aos locais de amostragem em campo 
                         foram estudadas. Para tal finalidade, a an{\'a}lise de 
                         correla{\c{c}}{\~a}o, a an{\'a}lise derivativa e o calculo do 
                         Normalized Difference Vegetation Index (NDVI), a partir dos 
                         espectros dos pixels e das amostras de solo, foram sequencialmente 
                         aplicados. Finalmente, a t{\'e}cnica Spectral Feature Fitting 
                         (SFF) foi usada para a identifica{\c{c}}{\~a}o na cena de alguns 
                         minerais do grupo dos {\'o}xidos de ferro (apetita e hematita) e 
                         do grupo das argilas (caulinita, montmorilonita e gibbsita). Os 
                         resultados obtidos indicaram que: (a) as classes de solo Podzolico 
                         Vermelho-Amarelo (PV), Latossolo Vermelho-Escuro (LE) e Latossolo 
                         Roxo (LR) podem ser discriminadas, principalmente, em 
                         fun{\c{c}}{\~a}o de seu albedo (primeira Componente Principal - 
                         CP1). A varia{\c{c}}{\~a}o na forma dos espectros, associada a 
                         CP2 e CP3, propicia a discrimina{\c{c}}{\~a}o da PV em relacao 
                         aos LR e LE, (b) as rela{\c{c}}{\~o}es entre os espectros de 
                         laborat{\'o}rio (IRIS) e de aeronave (AVIRIS) refletem as 
                         diferen{\c{c}}as inerentes aos dois ambientes de 
                         aquisi{\c{c}}{\~a}o de dados. A contamina{\c{c}}{\~a}o de 
                         pixel por res{\'{\i}}duos de vegeta{\c{c}}{\~a}o 
                         fotossinteticamente ativa ou inativa afeta as 
                         correla{\c{c}}{\~o}es entre os dois conjuntos de todos, 
                         especialmente, na faixa entre 500 e 1.200 nm; (c) os solos da 
                         {\'a}rea de estudo s{\~a}o espectralmente dominados pela 
                         presen{\c{c}}a de hematita e caulinita, de acordo com os 
                         resultados obtidos com o uso da t{\'e}cnica SFF. ABSTRACT: The 
                         objective of this work was to evaluate the use of the data 
                         generated by the imaging spectrometer Airborne Visible/InfraRed 
                         Imaging Spectrometer (AVIRIS) during the mission Smoke, Sulfate, 
                         Clouds, And Radiation Brazil (SCAR-B), in the period of August to 
                         September of 1995, for the spectral characterization and mineral 
                         identification in soils. The study area was near Campo Grande (MS) 
                         city, Brazil. The AVIRIS data were converted from radiance values 
                         to surface reflectance through a method of atmospheric correction 
                         based on the MODTRAN radiative transfer model. In order to make 
                         the spectral analysis of the soil characteristics and to 
                         discriminate the main types of soils present in the area, 
                         Principal Components Analysis (PCA) was applied on the AVIRIS 
                         data. PCA reduced the high dimensionality of AVIRIS data. AVIRIS 
                         spectral data were compared to laboratory IRIS (InfraRed 
                         Intelligent Spectroradiometer) data of 18 soil samples. 
                         Correlation analysis, derivative analysis and the calculation of 
                         Normalized Difference Vegetation Index (NDVI), were applied for 
                         both laboratory and AVIRIS data. Finally, the Spectral Feature 
                         Fitting (SFF) technique was used for the identification of some 
                         minerals in the AVIRIS scene. The main minerals studied were from 
                         the group of the iron oxides (hematite and goethite) and from the 
                         group of the clays (kaolinite, montmorillonite and gibbsite). The 
                         main results were: (a) the soil classes Podz{\'o}lico 
                         Vermelho-Amarelo (PV, Arenica Abruptic Paleudult), Latossolo 
                         Vermelho-Escuro (LE, Typic Haplorthox) and Latossolo Roxo (LR, 
                         Typic Acrorthox ) could be discriminated, mainly, in function of 
                         their albedo (first Principal Component - PC1). The variation in 
                         the shape of the spectra, associated with PC2 and PC3, allowed the 
                         discrimination of PV in relation to LR and LE; (b) the 
                         relationships among the laboratory (IRIS) and field (AVIRIS) 
                         spectra reflected the inherent differences between both data 
                         sources mainly due to the influence of the atmosphere; c) the 
                         pixel contamination by residues of photosynthetic or 
                         non-photosynthetic vegetation affected the correlations between 
                         the two groups of data, especially in the 500-1,220 nm spectral 
                         region; (d) the soils in the studied area are spectrally dominated 
                         by the presence of hematite and kaolinite, according to the 
                         results obtained from the use of the SFF technique. The results 
                         showed the potential of imaging spectroscopy in characterizing the 
                         albedo variations, shapes of the spectra and mineral absorption. 
                         Thus, by using this approach, it was possible to discriminate 
                         different tropical soil classes and to identify surface materials 
                         on a pixel basis.",
            committee = "Epiphanio, Jos{\'e} Carlos Neves (presidente/orientador) and 
                         Galvao, L{\^e}nio Soares (orientador) and Novo, Evlyn Le{\~a}o 
                         de Moraes and Antunes, Mauro Ant{\^o}nio Homem and Accioly, 
                         Luciano Jos{\'e} de Oliveira",
           copyholder = "SID/SCD",
         englishtitle = "Hyperspectral remote sensing for mineral characterization and 
                         identification in tropical soils",
                label = "8602",
             language = "pt",
                pages = "194",
                  ibi = "6qtX3pFwXQZ4PKzA/iQQHK",
                  url = "http://urlib.net/ibi/6qtX3pFwXQZ4PKzA/iQQHK",
           targetfile = "publicacao.PDF",
        urlaccessdate = "08 maio 2024"
}


Fechar