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Registro Completo |
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Biblioteca(s): |
Embrapa Instrumentação. |
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Data corrente: |
27/12/2022 |
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Data da última atualização: |
25/01/2023 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
FERNANDES, G. de J. C.; SILVA, K. F.; MARQUES, C. S.; BENEDITO, L. Z.; CABRAL, B. R.; CAMPELO, P. H.; BORGES, S. V.; MARCONCINI, J. M.; MAGRIOTIS, Z. M.; CLARO, P. I. C.; DIAS, M. V. |
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Afiliação: |
JOSE MANOEL MARCONCINI, CNPDIA. |
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Título: |
Development of an SO2 indicator label applied to shrimp. |
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Ano de publicação: |
2022 |
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Fonte/Imprenta: |
Polímeros, v. 32, n. 3, e2022035, 2022 |
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Páginas: |
1 - 9 |
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DOI: |
https://doi.org/10.1590/0104-1428.20220033 |
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Idioma: |
Inglês |
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Palavras-Chave: |
Colorimetric indicator; Crustaceans; Smart label. |
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Categoria do assunto: |
-- |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/1150373/1/P-Development-of-an-SO2.pdf
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Marc: |
LEADER 00825naa a2200289 a 4500
001 2150373
005 2023-01-25
008 2022 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1590/0104-1428.20220033$2DOI
100 1 $aFERNANDES, G. de J. C.
245 $aDevelopment of an SO2 indicator label applied to shrimp.$h[electronic resource]
260 $c2022
300 $a1 - 9
653 $aColorimetric indicator
653 $aCrustaceans
653 $aSmart label
700 1 $aSILVA, K. F.
700 1 $aMARQUES, C. S.
700 1 $aBENEDITO, L. Z.
700 1 $aCABRAL, B. R.
700 1 $aCAMPELO, P. H.
700 1 $aBORGES, S. V.
700 1 $aMARCONCINI, J. M.
700 1 $aMAGRIOTIS, Z. M.
700 1 $aCLARO, P. I. C.
700 1 $aDIAS, M. V.
773 $tPolímeros$gv. 32, n. 3, e2022035, 2022
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Registro original: |
Embrapa Instrumentação (CNPDIA) |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Cerrados. Para informações adicionais entre em contato com cpac.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Cerrados. |
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Data corrente: |
25/03/2002 |
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Data da última atualização: |
25/03/2002 |
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Autoria: |
MATTHIAS, A. D.; FIMBRES, A.; SANO, E. E.; POST, D. F.; ACCIOLY, A.; BATCHILY, A. K.; FERREIRA, L. G. |
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Título: |
Surface roughness effects on soil albedo. |
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Ano de publicação: |
2000 |
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Fonte/Imprenta: |
Soil Science Society of America Journal, Madison, v. 64, n. 3, p. 1035-1041, 2000. |
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Idioma: |
Inglês |
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Conteúdo: |
Knowledge of how surface roughness influences the reflectance of sunlight from cultivated soils in useful in various applications such as estimating albedo values used as inputs to soil temperature models and erosion models. The albedos of two soils were studied for dry and wet surfaces with four different roughness conditions, changed from a reference smooth soil surface. The soils were the Gila fine sandy loam (coarse-loamy,mixed calcareous , thermic typic torrifluvent ap horizon, 10YR 6.0/3.2 dry and 10YR 4.1/3.3 wet, and the pima clay loam fine silty, mixed calcareous, thermic tipic torrifluvent ap horizon, 10YR 5.2/2.3 dry and 10YR 3.3/2.3 wet. Albedo measurements were made during selected mornings with clear skies in 1995 and 1996. The mean albedos of reference smooth surfaces ( menor 2 mm sieved soil) were 0.279 and 0.155 for dry and wet gila soil and 0.221 and 0.114 for dry and wet pima soil. Tillage directionh was north-soult in 1995 and east west in 1996. The goodness of fit of linear relationships determined between mean albedo and surface roughness, measured with a roughness meter and reported as the root mean square deviation, were relatively high however, the slops for the regression equations were different for the two soils and the two moisture conditions. The different slopes indicate that the sensitivity of albeto to surface roughness was highest for yhe most reflective surface (dry gila soil) and lowest for the least reflective surface (wet pima soil). The albedos were on average 27,18, 10, and 8% lower for dry and wet rough plow, disk, disk-disk and seedbed treatments, respectively, as compared with the albedo of the reference smooth soil. Thesze reduction percentages can be used as a general guide to estimate the albedos of tilled soils similar to the gila and pima soils studied here. MenosKnowledge of how surface roughness influences the reflectance of sunlight from cultivated soils in useful in various applications such as estimating albedo values used as inputs to soil temperature models and erosion models. The albedos of two soils were studied for dry and wet surfaces with four different roughness conditions, changed from a reference smooth soil surface. The soils were the Gila fine sandy loam (coarse-loamy,mixed calcareous , thermic typic torrifluvent ap horizon, 10YR 6.0/3.2 dry and 10YR 4.1/3.3 wet, and the pima clay loam fine silty, mixed calcareous, thermic tipic torrifluvent ap horizon, 10YR 5.2/2.3 dry and 10YR 3.3/2.3 wet. Albedo measurements were made during selected mornings with clear skies in 1995 and 1996. The mean albedos of reference smooth surfaces ( menor 2 mm sieved soil) were 0.279 and 0.155 for dry and wet gila soil and 0.221 and 0.114 for dry and wet pima soil. Tillage directionh was north-soult in 1995 and east west in 1996. The goodness of fit of linear relationships determined between mean albedo and surface roughness, measured with a roughness meter and reported as the root mean square deviation, were relatively high however, the slops for the regression equations were different for the two soils and the two moisture conditions. The different slopes indicate that the sensitivity of albeto to surface roughness was highest for yhe most reflective surface (dry gila soil) and lowest for the least reflective surface (wet pima soil). T... Mostrar Tudo |
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Palavras-Chave: |
Propriedade fisico-quimica do solo; Soil chemicophysical properties. |
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Thesagro: |
Sensoriamento Remoto; Textura do Solo. |
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Thesaurus NAL: |
remote sensing; soil texture. |
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Categoria do assunto: |
-- |
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Marc: |
LEADER 02591naa a2200265 a 4500
001 1564556
005 2002-03-25
008 2000 bl --- 0-- u #d
100 1 $aMATTHIAS, A. D.
245 $aSurface roughness effects on soil albedo.
260 $c2000
520 $aKnowledge of how surface roughness influences the reflectance of sunlight from cultivated soils in useful in various applications such as estimating albedo values used as inputs to soil temperature models and erosion models. The albedos of two soils were studied for dry and wet surfaces with four different roughness conditions, changed from a reference smooth soil surface. The soils were the Gila fine sandy loam (coarse-loamy,mixed calcareous , thermic typic torrifluvent ap horizon, 10YR 6.0/3.2 dry and 10YR 4.1/3.3 wet, and the pima clay loam fine silty, mixed calcareous, thermic tipic torrifluvent ap horizon, 10YR 5.2/2.3 dry and 10YR 3.3/2.3 wet. Albedo measurements were made during selected mornings with clear skies in 1995 and 1996. The mean albedos of reference smooth surfaces ( menor 2 mm sieved soil) were 0.279 and 0.155 for dry and wet gila soil and 0.221 and 0.114 for dry and wet pima soil. Tillage directionh was north-soult in 1995 and east west in 1996. The goodness of fit of linear relationships determined between mean albedo and surface roughness, measured with a roughness meter and reported as the root mean square deviation, were relatively high however, the slops for the regression equations were different for the two soils and the two moisture conditions. The different slopes indicate that the sensitivity of albeto to surface roughness was highest for yhe most reflective surface (dry gila soil) and lowest for the least reflective surface (wet pima soil). The albedos were on average 27,18, 10, and 8% lower for dry and wet rough plow, disk, disk-disk and seedbed treatments, respectively, as compared with the albedo of the reference smooth soil. Thesze reduction percentages can be used as a general guide to estimate the albedos of tilled soils similar to the gila and pima soils studied here.
650 $aremote sensing
650 $asoil texture
650 $aSensoriamento Remoto
650 $aTextura do Solo
653 $aPropriedade fisico-quimica do solo
653 $aSoil chemicophysical properties
700 1 $aFIMBRES, A.
700 1 $aSANO, E. E.
700 1 $aPOST, D. F.
700 1 $aACCIOLY, A.
700 1 $aBATCHILY, A. K.
700 1 $aFERREIRA, L. G.
773 $tSoil Science Society of America Journal, Madison$gv. 64, n. 3, p. 1035-1041, 2000.
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