Condutividade térmica de rochas: uma aplicação para granitos ornamentais

This dissertation focuses on rock thermal conductivity and its correlations with petrographic, textural, and geochemical aspects, especially in granite rocks. It aims at demonstrating the relations of these variables in an attempt to enlighten the behavior of thermal effect on rocks. Results can be useful for several applications, such as understanding and conferring regional thermal flow results, predicting the behavior of thermal effect on rocks based upon macroscopic evaluation (texture and mineralogy), in the building construction field in order to provide more precise information on data refinement on thermal properties emphasizing a rocky material thermal conductivity, and especially in the dimension stone industry in order to open a discussion on the use of these variables as a new technological parameter directly related to thermal comfort. Thermal conductivity data were obtained by using Anter Corporation s QuicklineTM -30 a thermal property measuring equipment. Measurements were conducted at temperatures ranging between 25 to 38 OC in samples with 2cm in length and an area of at least 6cm of diameter. As to petrography data, results demonstrated good correlations with quartz and mafics. Linear correlation between mineralogy and thermal conductivity revealed a positive relation of a quartz percentage increase in relation to a thermal conductivity increase and its decrease with mafic minerals increase. As to feldspates (K-feldspate and plagioclase) they show dispersion. Quartz relation gets more evident when compared to sample sets with >20% and <20%. Sets with more than 20% quartz (sienogranites, monzogranites, granodiorites, etc.), exhibit to a great extent conductivity values which vary from 2,5 W/mK and the set with less than 20% (sienites, monzonites, gabbros, diorites, etc.) have an average thermal conductivity below 2,5 W/mK. As to textures it has been verified that rocks considered thick/porphyry demonstrated in general better correlations when compared to rocks considered thin/medium. In the case of quartz, thick rocks/porphyry showed greater correlation factors when compared to the thin/medium ones. As to feldspates (K-feldspate and plagioclase) again there was dispersion. As to mafics, both thick/porphyry and thin/medium showed negative correlations with correlation factor smaller than those obtained in relation to the quartz. As to rocks related to the Streckeisen s QAP diagram (1976), they tend to fall from alcali-feldspates granites to tonalites, and from sienites to gabbros, diorites, etc. Thermal conductivity data correlation with geochemistry confirmed to a great extent mineralogy results. It has been seen that correlation is linear if there is any. Such behavior could be seen especially with the SiO2. In this case similar correlation can be observed with the quartz, that is, thermal conductivity increases as SiO2 is incremented. Another aspect observed is that basic to intermediate rocks presented values always below 2,5 W/mK, a similar behavior to that observed in rocks with quartz <20%. Acid rocks presented values above 2,5 W/mK, a similar behavior to that observed in rocks with quartz >20% (granites). For all the other cases, correlation factors are always low and present opposite behavior to Fe2O3, CaO, MgO, and TiO2. As to Al2O3, K2O, and Na2O results are not conclusive and are statistically disperse. Thermal property knowledge especially thermal conductivity and its application in the building construction field appeared to be very satisfactory for it involves both technological and thermal comfort aspects, which favored in all cases fast, cheap, and precise results. The relation between thermal conductivity and linear thermal dilatation have also shown satisfactory results especially when it comes to the quartz role as a common, determining phase between the two variables. Thermal conductivity studies together with rocky material density can function as an additional tool for choosing materials when considering structural calculation aspects and thermal comfort, for in the dimension stone case there is a small density variation in relation to a thermal conductivity considerable variation

Caracterização Morfodinâmica e Sedimentologia da Plataforma Continental Rasa na APA Estadual dos Recifes de Corais - RN

This study had to aimed to characterize the sediments of shallow continental shelf and realize the mapping of features visible for satellite images by using remote sensing techniques, digital image processing and analysis of bathymetry between Maxaranguape and Touros - RN. The study s area is located in the continental shallow shelf of Rio Grande do Norte, Brazil, and is part of the Environmental Protection Area (APA) of Coral Reefs. A total of 1186 sediment samples were collected using a dredge type van veen and positioning of the vessel was made out with the aid of a Garmin 520s. The samples were treated In the laboratory to analyze particle size of the sediment, concentration of calcium carbonate and biogenic composition. The digital images from the Landsat-5 TM were used to mapping of features. This stage was used the band 1 (0,45-1,52 μm) where the image were georeferenced, and then adjusting the histogram, giving a better view of feature bottom and contacts between different types of bottom. The results obtained from analysis of the sediment showed that the sediments of the continental shelf east of RN have a dominance of carbonate facies and a sand-gravelly bottom because the region is dominated by biogenic sediments, that are made mainly of calcareous algae. The bedform types identified and morphological features found were validated by bathymetric data and sediment samples examined. From the results obtained a division for the shelf under study is suggested, these regions being subdivided, in well characterized: (1) Turbid Zone, (2) Coral Patch Reefs Zone, (3) Mixed Sediments Carbonates Zone, ( 4) Algae Fouling Zone, (5) Alignment Rocky Zone, (6) Sand Waves Field (7) Deposit siliciclastic sands

Caracterização sonográfica e sismoestratigráfica de alta resolução do estuário do Rio Potengi, Natal - RN

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior

Trabalhadores de verão : políticas públicas, turismo e emprego no litoral potiguar

El turismo en el Estado de Rio Grande do Norte (RN) se presenta constantemente por los medios de comunicación de massa como fuente de desarrollo regional y local , delante de las inversiones generadas y la posibilidad verdadera/potencial de trabajos en sus diversos sectores. Las políticas públicas del sector fueran y son responsables por la captación de inversiones privadas y su generación consiguiente de puestos de trabajo. En los años 90, el gobierno del RN puso el Programa de Desarrollo del Turismo en Rio Grande do Norte PRODETUR/RN I, con vistas a la competitividad local como destinación regional y nacional. El programa relacionado fue responsable por las inversiones diversas en infraestructura en los espacios implicados, aunque de forma asimétrica. Tales inversiones han contribuido para consolidar los discursos positivos con respecto al binomio turismo y trabajo . Con respecto a los discursos acríticos relacionados a este tema, mientras generador de trabajos y del desarrollo local es que se ha planteado esta investigación, puesto que la calidad de los trabajos generados por la actividad turística no se questiona y, de forma análoga, los costes sociales de la política pública, es decir, la importancia de su modelo de desarrollo , tampoco es questionado. Desde la problematica que se ha delineado arriba las questones que han norteado la investigación fueran: ¿de que forma la política pública del turismo llamada de PRODETUR/RN fue eficaz para generar empleo y renta a las ciudades en que se ha llavado a cabo? ¿Cuales son las características de estos trabajos? ¿ como estos trabajos se dividen en el espacio de las ciudades? Así el área delimitada para el estudio englobou las seis ciudades apoyadas por este Programa: Natal, Parnamirim, Ceará-Mirim, Nísia Floresta, Extremoz y Tibau do Sul. El recorte temporal de la pesquisa corresponde a la implantación de este programa (1996) hasta los dias actuales. La investigación de campo fue basada en el uso de 186 encuestas con los trabajadores en la actividad del turismo de litoral sur de Rio Grande do Norte, más allá de la realización (secundaria) de ocho entrevistas con agentes sociales que tienen relación con el tema. Como consideraciones finales de la investigación, se creer que hay una asimetría en el espacio turístico potiguar, donde Natal es la zona que más ha recibido las ventajas más grandes proporcionadas por la actividad, mientras que el restante de las ciudades son el eje para la sustentación de la actividad turística de Natal. De esta forma, las ciudades periféricas (todas, excepto Natal) incluidas en PRODETUR/RN ejercen el papel del subproducto de la ciudad capital, donde la precarización de las relaciones de trabajo se evidencian, todavía más en estas ciudades secundarias . La política pública en vez de intentar ecualizar las ventajas de la actividad en las seis ciudades, contribuye más, todavía para consolidar el nivel de centralizad de Natal. El PRODETUR/RN I fue capaz de generar, indirectamente, trabajos significativos, sin embargo la mayoría de éstos si presentan en los niveles operacionales de la actividad, con las características puestas en esta investigación (baja escolaridad, bajas rentas, falta de formalidad, levantadas horas de trabajo, bajo grado de sindicación y otros más); los puestos de trabajos creados si hallan sobretodo en Natal; y las demás ciudades sirven como elementos de apoyo para la capital mientras producto central de las decisiones sobre el turismo en el Estado del RN

Florística e fitossociologia do componente arbóreo da transição Floresta Ombrófila Densa das Terras Baixas - Floresta Ombrófila Densa Submontana do Núcleo Picinguaba/PESM, Ubatuba, sudeste do Brasil

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Description of the tadpole of Scinax auratus (Wied-Neuwied) (Anura, Hylidae)

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Stream fish, water and habitat quality in a pasture dominated basin, southeastern Brazil

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Anatomia de escapos de Tillandsia L. (Bromeliaceae) dos Campos Gerais do Paraná, Brasil

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Influência da estrutura do hábitat sobre a ictiofauna de um riacho em uma micro-bacia de pastagem, São Paulo, Brasil

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Análisis económico de externalidades ambientales. Guía para decisores

Incluye Bibliografía

Política fiscal y crecimiento económico: consideraciones microeconómicas y relaciones macroeconómicas

Incluye bibliografia

Comunidades de peixes e integridade biótica do Córrego da Água Limpa na fase de pré-recuperação de matas ciliares

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Influência relativa de parâmetros ambientais e espaciais na diversidade de anuros (Amphibia: Anura) dos Campos Gerais, Paraná, Brasil

Pós-graduação em Biologia Animal - IBILCE

Revisitação de Bromeliaceae na APA Santuário ecológico da Pedra Branca Caldas, MG

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Mapeamento de sensibilidade a derramamentos de petróleo do Parque Estadual da Ilha do Cardoso - PEIC e áreas do entorno

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)