Validación del método de predicción de direcciones principales de drenaje subterráneo en macizos anisótropos, en los terrenos volcánicos del macizo de Anaga, Tenerife

Actualmente y desde hace ya más de 25 años, el Método de “Predicción de las Direcciones Principales de Drenaje Subterráneo en Macizos Anisótropos”, ha sido utilizado con éxito en diferentes terrenos Kársticos como: calizas, yesos, cuarcitas, pizarras, granitos y criokarst (karst en el hielo glaciar). Sin embargo hasta ahora, nunca se había validado en terrenos volcánicos donde está focalizada esta tesis que lleva por título, Validación de dicho Método en los Terrenos Volcánicos del Macizo de Anaga en Tenerife. Este Método matemático consiste esencialmente en “Predecir y Cuantificar” las direcciones principales de drenaje turbulento subterráneo en macizos anisótropos. Para ello se basa en el estudio realizado en campo de los tectoglifos o deformaciones permanentes del macizo, impresas éstas en la roca, como consecuencia de los esfuerzos tectónicos a los que ha estado sometido dicho macizo. Se consigue de esta manera cubrir el vacío para macizos anisótropos que existe con el modelo matemático de flujo subterráneo laminar (macizos isótropos) definido por Darcy (1856). Para validar el Método se ha elegido el macizo de Anaga, pues es la zona de mayor anisotropía existente en la isla de Tenerife, conformada por una gran y extensa red de diques de diversas formas y tamaños que pertenecen a la familia de diques del eje estructural NE de la isla. En dicho macizo se realizó un exhaustivo trabajo de campo con la toma 331 datos (diques basálticos) y se aplicó el Método, consiguiendo definir las direcciones preferentes de drenaje subterráneo en el macizo de Anaga. Esta predicción obtenida se contrastó con la realidad del drenaje en la zona, conocida gracias a la existencia de cinco galerías ubicadas en la zona trabajo, de las cuales se tiene información sobre sus alumbramientos. En todos los casos se demuestra la bondad de la predicción obtenida con el Método. Queda demostrado que a mayor caos geológico o geotectónico, se ha conseguido mejor predicción del Método, obteniéndose resultados muy satisfactorios para aquellas galerías de agua en las que su rumbo de avance fue coincidente con la dirección perpendicular a la obtenida con la predicción dada por el Método, como dirección preferente de drenaje en la zona en la que se encuentra ubicada cada galería. No cabe duda que la validación de Método en los terrenos volcánicos de Tenerife, supondrá un cambio considerable en el mundo de la hidrogeología en este tipo de terrenos. Es la única herramienta matemática que se dispone para predecir un rumbo acertado en el avance de la perforación de las galerías de aguas, lo que conlleva al mismo tiempo un ahorro importantísimo en la ejecución de las obras. Por otro lado, el Método deja un importante legado a la sociedad canaria, pues con él se abren numerosas vías de trabajo e investigación que generarán un importante desarrollo en el mundo de la hidrogeología volcánica. ABSTRACT Currently and for over 25 years now, the Method of "Prediction of Subsurface Drainage Main Directions in Anisotropic Massifs" has been successfully used in various karstic terrains such as: limestone, gypsum, quartzite, slate, granite and criokarst (karst in the glacier ice). However, until now, it had never been validated in volcanic terrains where is focused this thesis entitled Validation of such Method in the Anaga Massif Volcanic Terrains, in Tenerife. This mathematical method is essentially "predict and quantify" the main directions of groundwater turbulent drainage in anisotropic massifs. This is based on field study of tectoglifes or permanent deformation of the massif, printed on the rocks as a result of previous tectonic stresses. Therefore it is possible to use in anisotropic rock mathematical model instead of the isotropic laminar flow mathematical models defined by Darcy (1856). The Anaga Massif have been chosen to validate the method, because it presents the greatest anisotropy in Tenerife Island, shaped by a large and extensive network of dikes of various shapes and sizes that belong to the family of NE structural axis dikes of the island. An exhaustive field work was carried out in such massif, with 331 collected data (basaltic dikes) and the method was applied, in order to define the preferred direction of the underground drainage in the Anaga massif. This obtained prediction was contrasted to the reality of the drainage in the area, known thanks to the existence of five galleries located in the work area, from which information about their springs was available. In all cases it was possible to demonstrate the fitness of the prediction obtained by the method. It had been demonstrated that a greater geological or geotectonic chaos enhances a better prediction of the method, that predicted very satisfactory results for those water galleries which directions were perpendicular to that predicted by the Method as a drainage preferential direction, for the zone where was located each gallery. No doubt that the validation of the use of the Method in the volcanic terrain of Tenerife, means a considerable change in the world of hydrogeology in this type of terrain. It is the only mathematical tool available to predict a successful drilling direction in advancing water galleries, what also leads to major savings in execution of the drilling works. Furthermore, the method leaves an important legacy to the Canary Islands society, because it opens many lines of work and research to generate a significant development in the world of volcanic hydrogeology.

Integrated studies for the evaluation of conservation treatments on stone material from archaeological sites. Application to the case of Mérida (Spain)

In recent decades archaeological sites have been subject of many interventions. The application of conservation treatments, such us consolidation and protection ones by means of using, for instance, synthetic resins or organosilicic compounds, has been demonstrated inadequate in many cases, and even harmful for the heritage materials [1]. Evaluation studies should be a mandatory task, ideally before and after the intervention, but both tasks are complex and unusual in the case of archaeological heritage. Moreover, there is a general lack of knowledge in the mid and long term effects of these treatments, and how to act when these have resulted in deterioration of the original material. Remains of Roman Augusta Emerita, located in Merida (Spain), have gone through many interventions since the first archaeological campaign, in 1910. Some of them have demonstrated already to be harmful [2], others, more recent, must be evaluated in order to determine its effectiveness and durability, considering that many of these treatments are currently still applied. For this purpose a range of parameters has been measured such as color, surface hardness and roughness, mechanical or hydric properties, porosity, etc. on the original material (granite, marble and mortars mainly), and then the transformations of those same parameters analyzed after treatment, both in situ, in places where a intervention is documented, and in the laboratory, in samples. The study is being conducted both in the laboratory (Petrophysics Laboratory within IGEO) and in situ, on selected archaeological sites of Mérida (Theater and House of Mitreo). The comparison of results in untreated and treated areas of the site, and in treated-untreated samples, allows the distinction of variables that affect the interaction between products and stone material, issues such us effectiveness and durability of treatment and its validation or dismissal.

Concesión de explotación de granitos derivada del permiso de investigación “Honor de Miengo”

Este proyecto tiene por objeto el estudio de la viabilidad, tanto económica como técnica, de la apertura y explotación de una cantera de granito para su uso como roca ornamental. Para ello se ha seleccionado una zona de potencial interés en Santa Olalla del Cala (Huelva) debido a los afloramientos y la tonalidad de los mismos. En esta zona se ha realizado un estudio del medio físico y una investigación sobre los tipos de roca existentes en la superficie que comprende el Permiso de Investigación de la compañía minera Canteras Extremeñas S.L. Con todo ello, se han determinado varias áreas de interés en las que se podría realizar el emplazamiento de la cantera. Desde el punto de vista técnico, se ha definido el diseño de la cantera optando por un método de explotación combinando el Método Finlandés con el corte con hilo diamantado, proyectando a su vez una zona de emplazamiento para la futura escombrera temporal, teniendo en cuenta la realización de un estudio de impacto ambiental, plan de restauración, plan de vigilancia ambiental, explosivos y previsión de ejecución de las labores. El estudio realizado de los indicadores económicos nos muestra que el proyecto es rentable, con todo ello se concluye que, tanto técnica como económicamente, la explotación del recurso minero es viable. ABSTRACT This project aims to study the feasibility, both economic and technical, to the opening and operation of a granite quarry for use as an ornamental stone. For this we have selected an area of potential interest in Santa Olalla del Cala (Huelva) due to upwelling and tonality of these. In this area, it has made a study of the physical environment and an investigation into the types of rock on the surface comprising the Research Permit of the mining company Canteras Extremeñas SL. With all this, we have identified several areas of interest in which they could make the location of the quarry. From the technical point of view, we have defined the design of the quarry opting for a mining method combining the Finnish Method with the diamond wire cutting, projecting turn an area of the site for future temporal tip, taking into account the completion of an environmental impact, restoration plan, environmental monitoring plan, explosives and forecasting operations execution. The study of economic indicators shows that the project is profitable, yet it can be concluded that, both technically and economically, exploitation of mineral resources is viable.

Changes in Petrophysical Properties of the Stone Surface due to Past Conservation Treatments in Archaeological Sites of Merida (Spain)

Petrophysical properties, such as porosity, permeability, density or anisotropy de-termine the alterability of stone surfaces from archaeological sites, and therefore, the future preservation of the material. Others, like superficial roughness or color, may point out changes due to alteration processes, natural or man-induced, for ex-ample, by conservation treatments. The application of conservation treatments may vary some of these properties forcing the stone surface to a re-adaptation to the new conditions, which could generate new processes of deterioration. In this study changes resulting from the application of consolidating and hydrophobic treatments on stone materials from the Roman Theatre (marble and granite) and the Mitreo’s House (mural painting and mosaics), both archaeological sites from Merida (Spain), are analyzed. The use of portable field devices allows us to perform analyses both on site and in la-boratory, comparing treated and untreated samples. Treatments consisted of syn-thetic resins, consolidating (such as tetraethoxysilane TEOS) and hydrophobic products. Results confirm that undesirable changes may occur, with consequences ranging from purely aesthetic variations to physical, chemical and mechanical damages. This also permits us to check limitations in the use of these techniques for the evaluation of conservation treatments.

NDT for the detection and characterization of superficial treatments on stone material from archaeological sites of Merida (Spain)

Different treatments (consolidation and water-repellent) were applied on samples of marble and granite from the Front stage of the Roman Theatre of Merida (Spain). The main goal is to study the effects of these treatments on archaeological stone material, by analyzing the surface changes. X-Ray Fluorescence and Laser-Induced Breakdown Spectroscopy techniques, as well as Nuclear Magnetic Resonance have been used in order to study changes in the surface properties of the material, comparing treated and untreated specimens. The results confirm that silicon (Si) marker tracking allows the detection of applied treatments, increasing the peak signal in treated specimens. Furthermore, it is also possible to prove changes both within the pore system of the materialand in the distribution of surface water, resulting from the application of these products

Entre el Binomio Arte / Técnica. El cemento y el granito en el paisaje del Duero Internacional

Between Art and Tecnology. Concrete and granite in landscape of International Douro

Antonio Vallejo Álvarez: arquitectura de la sensatez

La presente tesis doctoral desarrolla la obra del arquitecto Antonio Vallejo Álvarez (n. 1903, t. 1928, f. 2002) cuya larga carrera profesional permite observar una evolución que tiene como fondo la de la arquitectura española desde los planteamientos academicistas de principios del siglo XX, pasando por el primer racionalismo, hasta la influencia del Movimiento Moderno. Antonio Vallejo nació en Almonacid de Zorita, un pueblo de la provincia de Guadalajara pequeño pero singular ya que entonces se construía el Salto de Bolarque, instalación energética crucial en la época que albergaba además elementos de arquitectura culta. La familia le envió a Madrid a estudiar en las Escuelas Pías de San Fernando y luego en la vieja escuela de arquitectura de la calle Escritorios perteneciente a la Real Academia de Bellas Artes de San Fernando. Terminada la carrera realizó unas primeras edificaciones de corte historicista con relativa abundancia de estilemas academicista que van desapareciendo paulatinamente a la vez que evolucionan hacia el “decó”. De esta depuración, que puede observarse muy bien en los números 69,73 y 62 de la calle Viriato de Madrid, resulta un primer racionalismo en el que las balconadas y cuerpos volados se apoyan sobre una trama racionalista ortogonal cada vez más rígida. Simultáneamente trabajó en esta época en la Oficina de Información sobre la Ciudad del Ayuntamiento de Madrid junto a Bernardo Giner de los Ríos y Fernando García Mercadal, entre otros. Más tarde se incorporó a las órdenes del primero a la Oficina de Construcciones escolares donde se mantuvo hasta el estallido de la guerra civil. Al amparo de la Ley Salmón fundó la empresa promotora de viviendas Ar-In donde realizó una arquitectura en la que la trama racionalista cobra una gran fuerza expresiva, matizada y potenciada por grandes balcones aterrazados de corte higienista. Sus exponentes máximos son el conjunto en la calle Narváez esquina a Alcalde Sáinz de Baranda, y la manzana de Guzmán el Bueno, 75 de Madrid. La guerra civil interrumpe el proceso y tras ella nuestro autor ensaya la supervivencia del racionalismo mediante la superposición de la trama en grandes cuerpos de alzado de ladrillo ocupando las plantas de pisos, sobre un basamento de granito en la planta baja y una especie de pórtico enmarcando los huecos del ático a modo de remate. En las ventanas se colocan embocaduras de caliza de diversas formas. Esta arquitectura, muy en la línea del gusto de la época, será sublimada mediante un magnífico ejemplo de manierismo en su gran obra de la Residencia de los Agustinos Recoletos y la Iglesia de Santa Rita de Madrid. Superados los al menos tres lustros de postguerra, Vallejo inicia un proceso que podríamos llamar estructuralista en la medida en que la asunción de la situación de la estructura en el edificio y el módulo por ella creada definen sus características formales. Aquí, tras trabajar el hormigón armado en algunos edificios como los del Residencial Bellas Vistas de Madrid, lo hace con mucho más convencimiento en edificios con estructuras de acero como el colegio del Sagrado Corazón de Guadalajara. Es también importante hablar de la provincia de Almería, a cuya capital llega nuestro arquitecto inmediatamente después de la guerra civil para alejarse de las indeseables consecuencias que hubiera podido tener su fidelidad al gobierno de la República con el que colaboró hasta el último momento. En la ciudad desarrolló una extensa labor como constructor a través de Duarín SA, que se había formado sobre los restos de su promotora. También como arquitecto, con una labor paralela a la madrileña pero con menor presión ambiental, lo que contribuyó a que en cierta medida el proceso de afloramiento de su arquitectura estructuralista, heredera lejana de su primer racionalismo, fuese más rápido, como prueban realizaciones como los edificios de la calle Juan Pérez, 18 y del Paseo de la Estación, 19. ABSTRACT This thesis deals with the works in architecture from Antonio Vallejo Álvarez (b. 1903, g. 1928, d. 2002) whose long career enables us to concentrate on the evolution of the Spanish Architecture from the Academicism taking place at the beginning of XXth century , until the influence of the Modern Movement, taking also into account Racionalism. Antonio Vallejo was born in Almonacid de Zorita, a village in the province of Guadalajara small but unique because then Salto de Bolarque the crucial energy facility at the time also housed elements of classical architecture is built. His family sent him to study to Madrid in Escuelas Pías de San Fernando first, and then he attended lessons in the old Architecture school from Escritorios street belonging this last one to la Real Academia de Bellas Artes de San Fernando. Once he finished his degree on Architecture, he worked on some historicist buildings with a great use of academicist stylemes which will be disappearing little by little, turning into “deco”. From this depurationn, whose traces can be found in 69, 73, 62 at Viriato street in Madrid, our architect ends up with a first racionalism in which balconies and flown bodies are suspended on a racionalist and orthogonal more and more rigid. At that time, he was also working in the Information Office in Madrid Town Hall together with Bernardo Giner de los Ríos y Fernando García Mercadal, among others. Later, he worked for Bernardo Giner de los Ríos in the School Building Offices until the breaking out of the Civil War. Under Salmón law, he founded a developer for buildings named Ar-In, where he developed a type of Architecture in which racionalism develops a magnificent expressive force, empowered by great terraced balconies with higienistain court. His great masterpieces at this time are the buildings from Narvaez opposite to Alcalde Sáinz de Baranda and the block in 75 Guzmán El Bueno, in Madrid. Civil war interrupts somehow his process and once the war is over, our architect works on the survival of racionalism by overlapping on large bodies of brick elevation occupying different floor plants, on a base of granite on the ground floor and a sort of portico framing the gaps in the attic by way of auction. On the Windows he se colocan embocaduras de caliza de diversas formas. This type of architecture, very much enjoyed at that time, will be sublimed as a great example of manierism in his great work such as the case of Agustinos Recoletos Residence and Santa Rita Church in Madrid. About fifteen years after the war, in the post-war era, Vallejo starts a process which we could call structuralist, as lons as the asumption from the situation of the structure in the building and the created module define his main features. Here, once our architect works with reinforce concrete in some of his buildings such as Residencial Bellas Vistas de Madrid, he improves his technique with steel strucutres such as the on in the school Sagrado Corazón in Guadalajara. It is also remarkable to speak about the province of Almería, where our architect arrives inmediately after the civil war, to get rid of the consequences of his loyalty to the Republic movement to which he collaborated until his death. He developed a great career as a builder there through Duarín SA, which was launched though his former enterprise. Similary as the way he worked in Madrid,he, also as an arquitect, did his work in Almería with less environmental pressure though, fact which contributed to the flourishing of the structuralist architecture, as an heir from his first racionalism, as it can be shown from buildings in streets such as 18 Juan Pérez, and 19 Paseo de la Estación.

Biochemical evolution II: Origin of life in tubular microstructures on weathered feldspar surfaces

Mineral surfaces were important during the emergence of life on Earth because the assembly of the necessary complex biomolecules by random collisions in dilute aqueous solutions is implausible. Most silicate mineral surfaces are hydrophilic and organophobic and unsuitable for catalytic reactions, but some silica-rich surfaces of partly dealuminated feldspars and zeolites are organophilic and potentially catalytic. Weathered alkali feldspar crystals from granitic rocks at Shap, north west England, contain abundant tubular etch pits, typically 0.4–0.6 μm wide, forming an orthogonal honeycomb network in a surface zone 50 μm thick, with 2–3 × 106 intersections per mm2 of crystal surface. Surviving metamorphic rocks demonstrate that granites and acidic surface water were present on the Earth’s surface by ∼3.8 Ga. By analogy with Shap granite, honeycombed feldspar has considerable potential as a natural catalytic surface for the start of biochemical evolution. Biomolecules should have become available by catalysis of amino acids, etc. The honeycomb would have provided access to various mineral inclusions in the feldspar, particularly apatite and oxides, which contain phosphorus and transition metals necessary for energetic life. The organized environment would have protected complex molecules from dispersion into dilute solutions, from hydrolysis, and from UV radiation. Sub-micrometer tubes in the honeycomb might have acted as rudimentary cell walls for proto-organisms, which ultimately evolved a lipid lid giving further shelter from the hostile outside environment. A lid would finally have become a complete cell wall permitting detachment and flotation in primordial “soup.” Etch features on weathered alkali feldspar from Shap match the shape of overlying soil bacteria.

Biochemical evolution III: Polymerization on organophilic silica-rich surfaces, crystal–chemical modeling, formation of first cells, and geological clues

Catalysis at organophilic silica-rich surfaces of zeolites and feldspars might generate replicating biopolymers from simple chemicals supplied by meteorites, volcanic gases, and other geological sources. Crystal–chemical modeling yielded packings for amino acids neatly encapsulated in 10-ring channels of the molecular sieve silicalite-ZSM-5-(mutinaite). Calculation of binding and activation energies for catalytic assembly into polymers is progressing for a chemical composition with one catalytic Al–OH site per 25 neutral Si tetrahedral sites. Internal channel intersections and external terminations provide special stereochemical features suitable for complex organic species. Polymer migration along nano/micrometer channels of ancient weathered feldspars, plus exploitation of phosphorus and various transition metals in entrapped apatite and other microminerals, might have generated complexes of replicating catalytic biomolecules, leading to primitive cellular organisms. The first cell wall might have been an internal mineral surface, from which the cell developed a protective biological cap emerging into a nutrient-rich “soup.” Ultimately, the biological cap might have expanded into a complete cell wall, allowing mobility and colonization of energy-rich challenging environments. Electron microscopy of honeycomb channels inside weathered feldspars of the Shap granite (northwest England) has revealed modern bacteria, perhaps indicative of Archean ones. All known early rocks were metamorphosed too highly during geologic time to permit simple survival of large-pore zeolites, honeycombed feldspar, and encapsulated species. Possible microscopic clues to the proposed mineral adsorbents/catalysts are discussed for planning of systematic study of black cherts from weakly metamorphosed Archaean sediments.

Geologia e petrologia da ilha de São Sebastião (Estado de São Paulo)

A ilha de São Sebastião consta principalmente de rochas alcalinas que formam um maciço de 300 km2 aproximadamente, constituindo o terceiro em área no Brasil. Apresenta-se em um "stock" alongado segundo NE-SW, encaixado em estruturas de gnais. As formações geológicas encontradas consistem em 1 - Granitos e Gnais (ARQUEANO), 2 - Eruptivas básicas (RÉTICO), 3 - Eruptivas alcalinas (JURÁSSICO) e 4 - Depósitos recentes (HOLOCENO). O método de estudo empregado foi o petrográfico e a coluna geológica estabelecida em base de dados petrográficos, tectônicos e fisiográficos. O arqueano é determinado por definição dos seus tipos petrográficos (1- gnais facoidal, 2- oligoclásio-gnais, 3- hornblenda-gnais, 4- biotita-gnais e 5- microlina-granito) idênticos aos concorrentes no considerado arqueano do Brasil meridional. O triássico (rético) é conferido às rochas básicas (diabásios e basaltos) pela sua semelhança tectônica e petrográfica com as congêneres que cortam de maneira semelhante o arqueano no continente. A "mise-en-place" das eruptivas alcalinas (1- Nordmarkito, 2- Biotita-pulaskito, 3- Pulaskito, 4- Nefelina-sienito, 5- Foiaito, 6- Essexito-foiaito, 7- Essexito e 8- Teralito) pode ser considerada jurássica devido suas relações com as eruptivas básicas referidas réticas, pois na praia do Bonete (foto 14) observa-se um dique de nordmarkito cortando outro de diabásio. As eruptivas quartzo-dioríticas (quartzo-microdiorito e quartzo-andesito) cortam as alcalinas no cume do Zabumba, indicando sua idade mais moderna que estas. Além deste fato, preenchem linhas de fraturas tectônicas recentes, como as falhas ao longo do canal de São Sebastião, indicando que a topografia deveria ser a mesma que a atual para permitir rios efusivos ao nível do canal ou que pelo menos toda a zona de extrusão estivesse, como hoje está, em superfície. Os depósitos aluviais marinhos e continentais são considerados recentes, (holocênicos) pelo favor da topografia onde se dispõe, ocupando o fundo os vales e os bordos do atual modelado costeiro, idade esta conferida em base fisiográfica. A tectônica que afetou a ilha de São Sebastião participa da que atuou em todo o litoral meridional brasileiro. Pode-se distinguir duas fases distintas: na primeira ocorreram as erupções básicas e as alcalinas subsidiárias e na segunda deram-se os falhamentos escalonados em blocos basculados para NW, com as fraturas de tensão preenchidas pelas eruptivas quartzo-dioríticas. Toda a atividade tectônica foi regulada pela direção NE-SW privilegiada da estrutura do arqueano, correspondente a antigos eixos dos dobramentos laurencianos e huronianos. A geomorfologia da ilha consta de uma antiga superfície de erosão rematada até a senilidade, - o peneplano cretáceo, hoje reduzida às cristas culminares do maciço alcalino e às satélites das estruturas gnáissicas, desnivelada pelo falhamento em blocos e ligeiramente adernada para NW devido ao basculamento. Ao lado desta topografia vestigial existe o modelado atual da ilha caracterizado por uma juventude do estágio evolutivo. Esta escultura foi inaugurada com os últimos levantamentos epirogênicos que ascenderam as eruptivas alcalinas plutônicas a mais de 1.300 m sobre o nível do mar. O modelado costeiro apresenta uma costa típica de submergência com esculturas em rias, no estágio da juventude. A presença de terraceamentos marinhos de abrasão, atualmente elevados cerca de 20 a 30 m, lembra as oscilações epirogênicas ou eustáticas do litoral.

Conversion of a digital camera into a non-contact colorimeter for use in stone cultural heritage: The application case to Spanish granites

In this study, a digital CMOS camera was calibrated for use as a non-contact colorimeter for measuring the color of granite artworks. The low chroma values of the granite, which yield similar stimulation of the three color channels of the camera, proved to be the most challenging aspect of the task. The appropriate parameters for converting the device-dependent RGB color space into a device-independent color space were established. For this purpose, the color of a large number of Munsell samples (corresponding to the previously defined color gamut of granite) was measured with a digital camera and with a spectrophotometer (reference instrument). The color data were then compared using the CIELAB color formulae. The best correlations between measurements were obtained when the camera works to 10-bits and the spectrophotometric measures in SCI mode. Finally, the calibrated instrument was used successfully to measure the color of six commercial varieties of Spanish granite.

Artefatos funerários como fontes para a história de ofícios urbanos artesanais

Este artigo descreve o uso de artefatos funerários na reconstituição histórica do processo de trabalho em marmorarias instaladas no município de São Carlos (São Paulo, Brasil), no período 1890-1950. Observação direta e registro fotográfico de artefatos funerários, exame de ferramentas de trabalho e utilização de fontes orais permitiram a reconstituição do processo de trabalho. A composição química de fragmentos de artefatos funerários foi determinada por Difração de Raios X e Microscopia Eletrônica de Varredura, evidenciando matérias-primas e sua combinação e uso no processo de trabalho. Considerando-se as etapas produtivas da indústria de rochas ornamentais (extração, serragem e beneficiamento final), os artefatos funerários indicam que as marmorarias inseriam-se na etapa de beneficiamento final. As marmorarias integravam os setores de base técnica artesanal da indústria brasileira, apresentando: baixo grau de concentração de capital e de operários; predomínio da habilidade do ofício especializado; separação pouco nítida entre trabalhadores e instrumentos de trabalho; identificação do trabalhador com o produto. Artefatos de mármore e granito eram destinados a brasileiros de segmentos sociais abastados, durante o início da imigração na cidade de São Carlos (final do século XIX). A partir de 1920, italianos incorporam-se a clientela dos marmoristas, indicando a mobilidade social do imigrante na cidade.

Experimental research on the residual mechanical properties of an ordinary concretes after fire

This paper summarizes the results of an experimental research to assess the residual mechanical properties of an ordinary concrete after fire. It was studied the influence of the cooling process, the maximum temperature that the concrete was subjected to and the loading level on the residual mechanical properties of calcareous and granite aggregate concretes. The properties studied were the residual compressive, tensile, splitting and flexural strengths and modulus of elasticity. Four levels of temperature; 20, 300, 500 and 700ºC; two loading levels (0.3f and 0.7fcd) and two cooling processes (cooling in the air and by water jet) were tested. The high temperatures attained and the sudden cooling down process on the concrete showed a negative effect on its residual mechanical properties. This effect was more notorious on the residual compression strength than in the other mechanical properties

Influência das elevadas temperaturas e as propriedades mecânicas residuais do concreto normal

O concreto, de um modo geral, apresenta um bom comportamento em situação de incêndio quando comparado com o aço, todavia em função da temperatura ocorrem algumas transformações químicas e físicas que podem comprometer esse desempenho. Apesar das alterações das propriedades mecânicas e térmicas do concreto quando sujeito a temperaturas elevadas e após situação de incêndio já terem sido avaliadas em vários estudos, ainda é um campo aberto onde é necessário muita investigação. O presente artigo apresenta os resultados de um estudo experimental sobre a avaliação das propriedades mecânicas residuais de concretos normais após incêndio. Para o efeito foram selecionados agregados graníticos e agregados calcários, dado serem os agregados mais utilizados na construção civil em Portugal e em muitos outros países. Os parâmetros testados foram: o nível de carregamento (0,3fcd e 0,7fcd); o processo de arrefecimento (arrefecimento ao ar e arrefecimento por jato de água) e o nível máximo de temperatura atingida (20, 300, 500 e 700ºC). As propriedades mecânicas estudadas foram a resistência à compressão residual, resistência à tração direta e resistência à tração por compressão diametral, resistência à flexão, módulo de elasticidade e coeficiente de Poisson. As temperaturas atingidas e o arrefecimento rápido do concreto apresentaram um efeito negativo sobre as propriedades mecânicas residuais. Este efeito foi mais notório na resistência à compressão residual do que nas restantes propriedades mecânicas estudadas.