979 resultados para Color index


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The Continuous Plankton Recorder (CPR) survey has been used to characterize phytoplankton and zooplankton space-time dynamics in the North Sea since 1931 and in the North Atlantic since 1939. Phytoplankton biomass is assessed from these samples by visual assessment of the green color of the silk mesh, the Phytoplankton Color Index (PCI), and the total count of diatoms and dinoflagellates. Species with a frequency of occurrence greater than 1% in the samples are used as indicator species of the community. We investigated (1) long-term fluctuations of phytoplankton biomass, total diatoms, and total dinoflagellates; (2) geographical variation of patterns; (3) the relationship between phytoplankton and climate forcing in the North Atlantic CPR samples; (4) the relative contribution of diatoms and dinoflagellates to the PCI; and (5) the fluctuations of the dominant species over the period of survey to provide more information on the processes linking climate to changes in the phytoplankton community. As a result of the differences in microscopic analysis methods prior to 1958, our analyses were conducted for the period ranging from 1958 to 2002. The North Atlantic was divided into six regions identified through bathymetric criteria and separated along a North-South axis. Based on 12 monthly time series, we demonstrate increasing trends in PCI and total dinoflagellates and a decrease in total diatoms.

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Egg yolk color may be controlled both by the concentration and the type of xanthophylls added to diets, with the aim of meeting consumers demand. The objectives of this work were to study how yellow and red xanthophylls present in laying hens` diets influence yolks colors and find the concentrations of these ingredients that meet the regional consumer desire. A factorial design 5 x 3 with 5 concentrations of yellow xanthophylls (lutein + zeaxantin 40%; 1.0, 1.25, 1.5, 1.75 and 2.0 mg/hen/d) and 3 concentrations of red xanthophylls (canthaxantin 10%; 0, 0.35, 0.7 mg/hen/d) was used. After a 30 d period receiving corn basal diets and water ad libitum, 60 White Dekalbe hens were distributed to receive the 15 dietary treatments in 4 replicates. Diets were provided daily at 110 g, during 21 d under 16 h light/8 h dark. Yolks colors were evaluated daily using the CIE L, a, b color space and the Roche color index. After the color stabilization, data were analyzed by ANOVA, regression analysis and Response Surface Methodology (MRS). Global acceptance for the Roche colors was evaluated with a 5 points hedonic scale and data were analyzed by Friedman and Dunn tests. Significance was established at 95% (P < 0.05). Regression analysis showed that the red xanthophylls content was the most important factor that defined L, a and b values for yolk color (P < 0.0001; square function), although its effect was significantly affected by the yellow xanthophylls contents (P = 0.0277; P < 0.0001; P = 0.0002 for L, a, b, respectively), providing evidence for a synergistic effect and not for a saturation effect. MRS showed that the highest redness of yolks was reached with 1.5 mg/hen/d of yellow and 0.5 mg/hen/d of red xanthophylls. So, higher supplementations aiming at increasing yolk color would bring an unnecessary cost to the ration. The most accepted yolk color scored 9, which corresponded to mean color attributes L = 65; a = 16; and b = 64. MRS showed that these values could be reached with combinations of yellow:red xanthophylls like 1.0:0.15 or 1.5:0.1 mg/ hen/d or simply with the yellow xanthophylls at 2.0 mg/hen/d. So, it was concluded that both yellow and red xanthophylls are important to define yolks color; that high amounts of xanthophylls are unnecessary to bring changes to color; and that Brazilian consumer requires yolks color attainable with few amounts of red xanthophylls or only with the yellow ones.

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El objetivo fue determinar, durante dos años, el contenido de β-caroteno y su relación con el Índice de Color (IC), de ocho cultivares comerciales del tipo 'Flakkee' cultivadas en el INTA La Consulta. El diseño experimental a campo utilizado fue en bloques al azar con 3 repeticiones. Se evaluó β-caroteno (espectrofotometría a 450 nm) y se calculó el IC, mediante captación de imagen digital con PC y escáner, midiendo L, a y b del Sistema CIELAB. Los datos fueron analizados por ACP (análisis de componentes principales), la visualización de la variabilidad, por cartografiado de datos, análisis de varianza, pruebas de diferencia de medias y correlaciones. Los contenidos de β-carotenos y el IC de los cultivares se mantuvieron constantes durante los dos años estudiados, resultando las cultivares Natasha, Flakesse y Colmar las de mayor valor nutricional en cuanto a aporte de β-carotenos. En el rango de valores menores de 18 mg%g de β-carotenos, se observó una correlación positiva significativa en las cultivares Supreme, Spring y Laval. No se encontró una correlación alta lineal entre el IC y el contenido de β-carotenos. El uso del IC resulta adecuado para predecir, en un intervalo de valores, el contenido de β-carotenos en cultivares de zanahoria.

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Foram aplicadas as técnicas de petrografia orgânica e palinologia no testemunho do poço TMB-01-SP, localizado na porção central da Bacia de Taubaté. A análise visual de 41 lâminas organopalinológicas e palinológicas permitiu individualizar três palinofácies e posicionar temporalmente a seção. A partir dos resultados das análises quantitativas do conteúdo orgânico, observou-se o predomínio de matéria orgânica amorfa de origem lacustre determinada pela presença de algas Botryococcus braunii e Pediastrum sp. Subordinadamente, verificou-se também a presença de grãos de pólen, esporos, fitoclastos e tecidos cutículares. Devido ao predomínio de matéria orgânica amorfa e algas lacustres com contribuições menores de material proveniente de vegetais superiores, foi possível classificar o querogênio como sendo dos tipos I e III. A matéria orgânica amorfa apresentou fluorescência moderada a alta na maior parte da seção (palinofácies 1 e 3) indicando um ambiente de sedimentação redutor predominante. Os resultados do índice de coloração de esporos (ICE) entre 1,5 e 2,5 indicaram zona imatura de geração de hidrocarbonetos. A partir das análises palinológicas foi possível observar uma rica e diversificada associação com 49 espécies identificadas, incluindo grãos de pólen, esporos, algas e fungos. Os resultados palinoestratigráficos permitiram correlacionar a seção analisada à palinozona Parvisaccites? sp. (Regali et al., 1974) que corresponde ao Oligoceno. Entre os palinomorfos diagnósticos de idade e ambiente deposicional foram identificados: Catinipollis geiseltalensis, Cicatricosisporites dorogensis, Dacrydiumites florinii, Echitriletes muelleri, Ephedripites tertiarius, Perisyncolporites pokornyi, Podocarpidites marwickii, Polypodiaceiosporites potoniei, Psilatricolporites operculatus, Quadraplanus sp., Ulmodeipites krempii e Verrucatosporites usmensis. Os sedimentos estudados foram depositados em um paleoambiente lacustre raso sob condições redutoras ao longo de praticamente toda a seção.

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O presente estudo baseou-se na análise do conteúdo orgânico do furo de sondagem rasa do poço 9-FBA-69-BA localizado na Bacia do Recôncavo. Foram utilizadas 126 amostras para análise de COT e 35 pares de lâminas para as análises palinológicas e palinofaciológicas. As análises palinofaciológicas mostraram que os componentes orgânicos particulados são dominados por material orgânico amorfo em praticamente toda a seção. Representantes alóctones estão pontualmente presentes e representados por fitoclastos, grãos de pólen e esporos. Os resultados de COT mostram valores percentuais acima de 1% em praticamente todo o intervalo estudado. Através da observação à luz de microscopia branca transmitida e luz incidente, foi possível individualizar três palinofácies distintas para a seção, levando-se em conta os tipos e o grau de preservação da matéria orgânica. A análise do ICE (Índice de Coloração dos Esporos) apresenta valores de maturação entre 4,5 a 5, caracterizando um grau de maturação térmica próximo da janela de geração de hidrocarbonetos. A associação palinoflorística mostra uma baixa diversidade de representantes, onde dentre os 292 palinomorfos com 28 gêneros e 11 espécies de grãos de pólen e esporos, 167 são representados somente pela espécie Classopollis classoides. Baseado na associação palinoflorística presente e na análise litológica do poço podemos inferir que a sedimentação ocorreu em um paleoambiente fluvial deltaico- lacustre, sob um clima árido a semiárido visto a abundante presença de formas Rimuladas. Apesar da não detecção das formas guias diagnósticas de idade, que definem as palinozonas do arcabouço palinoestratigráfico válido para seções cretáceas brasileiras, a associação palinológica recuperada, com formas típicas do eocretáceo (Classopollis classoides, Araucariacites australis, Equisetosporites sp.), aliado a presença da espécie Vitreisporites pallidus, e ausência de formas do neocretáceo, nos permitiu posicionar a seção na palinozona Vitreisporites pallidus considerada de idade Aratu

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The combination of chemical and biological water treatment processes is a promising technique to reduce recalcitrant wastewater loads. The key to the efficiency of such a system is a better understanding of the mechanisms involved during the degradation processes. Ozonation has been applied to many fields in water and wastewater treatment. Especially for effluents of textile finishing industry ozonation can achieve high color removal, enhance biodegradability, destroy phenols and reduce the COD. However, little is known about the reaction intermediates and products formed during ozonation. This work focuses on the oxidative degradation of purified (>90%), hydrolyzed Reactive Red 120 (Color Index), a widely used azo dye in the textile finishing processes with two monochlorotriazine anchor groups. Ozonation of the dye in ultra pure water was performed in a laboratory scale cylindrical batch reactor. Decolorization, determined by measuring the light absorbance at the maximum wavelength in the visible range (53 5 nm), was almost complete after 150 min with an ozone concentration of 12.8 mg/l. The TOC/TOC0 ratio was about 74% and the COD was diminished to 46% of the initial value. The BOD5/COD ratio increased from 0.01 to 0.14. To obtain detailed information on the reaction processes during ozonation and the resulting oxidation products organic and inorganic anions were analyzed. Oxidation and cleavage of the azo group yielded nitrate. Cleavage of the sulfonic acid groups of aromatic rings caused an increase in the amount of sulfate. Formic acid and oxalic acid were identified as main oxidation products by high performance ion chromatography (HPIC). The concentrations of these major products were monitored at defined time intervals during ozonation.

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Inter-annual variability in the timing of phytoplankton spring bloom and phytoplankton community structure in the central North Atlantic Ocean was quantified using ocean color data and continuous plankton recorder (CPR) data. This variability was related to the North Atlantic Oscillation using correlation analysis and multivariate auto-regression models. The initiation of the spring bloom derived from CPR phytoplankton color index data is similar to that derived from satellite chlorophyll, and exhibits a nominal correlation with the sea surface temperature (SST) and the North Atlantic Oscillation (NAO). The extrapolated spring bloom timing suggested later initiation of blooms in the mid-1980s and earlier initiation of blooms in the 1990s. The climatological phytoplankton community structure in the central North Atlantic is dominated by diatoms, except for a shift in community composition favoring dinoflagellates in August. The ratio of diatoms to total phytoplankton abundance and the ratio of dinoflagellates to total phytoplankton abundance are both closely correlated with the NAO and SST. The extended time series of phytoplankton community structure between 1985 and 2009, deduced from the time series of SST and NAO over the same interval, showed a decadal shift away from diatoms towards dinoflagellates. The linkages between the NAO, and changes in stratification and phytoplankton processes occur over a larger scale than previously observed.

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Studies relating biodiversity to ecosystem processes typically do not take into account changes in biodiversity through time. Marine systems are highly dynamic, with biodiversity changing at diel, seasonal and inter-decadal timescales. We examined the dynamics of biodiversity in the Gulf of Maine pelagic zooplankton community. Taxonomic data came from the Gulf of Maine continuous plankton recorder (CPR) transect, spanning the years 1961–2006. The CPR transect also contains coincident information on temperature and phytoplankton biomass (measured by the phytoplankton color index). Taxonomic richness varied at all timescales considered. The relationships between temperature and richness, and between phytoplankton and richness, also depended on temporal scale. The temperature–richness relationship was monotonic at the multi-decadal scale, and tended to be hump-shaped at finer scales; the productivity–richness relationship was hump-shaped at the multi-decadal scale, and tended to be monotonic at finer scales. Seasonal biodiversity dynamics were linked to temperature; inter-decadal biodiversity dynamics were linked to phytoplankton.

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A reflectância da folha em determinados comprimentos de onda pode ser uma alternativa para estimar a concentração de nitrogênio (N) na planta, devido à relação entre o teor de clorofila e de N no tecido foliar. Este trabalho teve por objetivo avaliar índices da cor verde em grama-bermuda para predizer o nível de N na planta. O experimento foi conduzido em área comercial de produção de grama-bermuda, localizada na cidade de Capela do Alto/SP. O delineamento experimental utilizado foi de blocos ao acaso, com cinco tratamentos (0, 150, 300, 450 e 600kg de N ha-1) e quatro repetições. Foi avaliada a reflectância das folhas pelo uso de medidor de cor de grama, clorofilômetro, e por meio de análise da imagem digital. O matiz (H) e índice de cor verde escuro (ICVE), calculados com base nos índices de reflectância da imagem digital, o ICVE, obtido com medidor de cor de grama, e a intensidade de coloração verde (ICV), obtida com o clorofilômetro, apresentaram forte correlação positiva com a concentração de N e a taxa de cobertura do solo (TCS) da grama-bermuda, podendo ser utilizados como índices auxiliares na recomendação de adubação nitrogenada para a cultura. Os valores obtidos que podem servir como primeiros índices para avaliação do estado nutricional em N na grama-bermuda Celebration são: H de 88 a 109o e ICVE de 0,54 a 0,66 (imagem digital); H de 67 a 76o e ICVE de 0,41 a 0,44 (medidor de cor da grama TCM 500); e ICV de 374 a 471 (clorofilômetro CM 1000).

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A intensidade da cor verde da folha pode ser alternativa para estimar a concentração de N na planta, devido à relação entre o teor de clorofila e o de N no tecido foliar. Objetivou-se neste trabalho avaliar índices da cor verde da grama esmeralda obtidos da análise da imagem digital e pelo uso do clorofilômetro para predizer o estado nutricional em N fornecido pelo lodo de esgoto. O experimento foi instalado e desenvolvido em uma propriedade comercial de grama esmeralda, localizada na cidade de Itapetininga (SP). O delineamento experimental foi em blocos casualizados, com quatro repetições e cinco doses de lodo de esgoto: 0, 10, 20, 30 e 40 Mg ha-1, base seca. As doses de lodo aplicadas correspondem a 100, 200, 300 e 400 kg ha-1 de nitrogênio disponível. Foram avaliadas as concentrações de N e a intensidade de coloração verde da folha pelo uso do clorofilômetro (ICV) e por meio da análise da imagem digital (G, H e ICVE) aos 45, 105 e 165 dias após a aplicação do lodo. Os valores de intensidade obtidos foram correlacionados com a concentração de N na lâmina foliar e com a taxa de cobertura do solo determinada nas mesmas épocas. A aplicação de doses de lodo de esgoto proporcionou aumento dos índices de cor verde e da concentração de N nas folhas da grama esmeralda. A concentração de N na lâmina foliar pode auxiliar a adubação nitrogenada em cobertura, pois proporcionou altas correlações com a taxa de cobertura do solo. O matiz (H) obtido com a imagem digital e a intensidade de cor verde da folha (ICV) obtida com o clorofilômetro correlacionaram-se com a concentração de N e com a taxa de cobertura do solo e, dessa forma, podem servir como índices na recomendação da adubação nitrogenada.

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The interest in the systematic analysis of astronomical time series data, as well as development in astronomical instrumentation and automation over the past two decades has given rise to several questions of how to analyze and synthesize the growing amount of data. These data have led to many discoveries in the areas of modern astronomy asteroseismology, exoplanets and stellar evolution. However, treatment methods and data analysis have failed to follow the development of the instruments themselves, although much effort has been done. In present thesis, we propose new methods of data analysis and two catalogs of the variable stars that allowed the study of rotational modulation and stellar variability. Were analyzed the photometric databases fromtwo distinctmissions: CoRoT (Convection Rotation and planetary Transits) and WFCAM (Wide Field Camera). Furthermore the present work describes several methods for the analysis of photometric data besides propose and refine selection techniques of data using indices of variability. Preliminary results show that variability indices have an efficiency greater than the indices most often used in the literature. An efficient selection of variable stars is essential to improve the efficiency of all subsequent steps. Fromthese analyses were obtained two catalogs; first, fromtheWFCAMdatabase we achieve a catalog with 319 variable stars observed in the photometric bands Y ZJHK. These stars show periods ranging between ∼ 0, 2 to ∼ 560 days whose the variability signatures present RR-Lyrae, Cepheids , LPVs, cataclysmic variables, among many others. Second, from the CoRoT database we selected 4, 206 stars with typical signatures of rotationalmodulation, using a supervised process. These stars show periods ranging between ∼ 0, 33 to ∼ 92 days, amplitude variability between ∼ 0, 001 to ∼ 0, 5 mag, color index (J - H) between ∼ 0, 0 to ∼ 1, 4 mag and spectral type CoRoT FGKM. The WFCAM variable stars catalog is being used to compose a database of light curves to be used as template in an automatic classifier for variable stars observed by the project VVV (Visible and Infrared Survey Telescope for Astronomy) moreover it are a fundamental start point to study different scientific cases. For example, a set of 12 young stars who are in a star formation region and the study of RR Lyrae-whose properties are not well established in the infrared. Based on CoRoT results we were able to show, for the first time, the rotational modulation evolution for an wide homogeneous sample of field stars. The results are inagreement with those expected by the stellar evolution theory. Furthermore, we identified 4 solar-type stars ( with color indices, spectral type, luminosity class and rotation period close to the Sun) besides 400 M-giant stars that we have a special interest to forthcoming studies. From the solar-type stars we can describe the future and past of the Sun while properties of M-stars are not well known. Our results allow concluded that there is a high dependence of the color-period diagram with the reddening in which increase the uncertainties of the age-period realized by previous works using CoRoT data. This thesis provides a large data-set for different scientific works, such as; magnetic activity, cataclysmic variables, brown dwarfs, RR-Lyrae, solar analogous, giant stars, among others. For instance, these data will allow us to study the relationship of magnetic activitywith stellar evolution. Besides these aspects, this thesis presents an improved classification for a significant number of stars in the CoRoT database and introduces a new set of tools that can be used to improve the entire process of the photometric databases analysis

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Pós-graduação em Agronomia (Produção Vegetal) - FCAV

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Pós-graduação em Ciência Florestal - FCA

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Pós-graduação em Ciência Florestal - FCA