Digital image processing techniques as a tool for evaluating and mapping patinas on granite monuments

Monument conservation is related to the interaction between the original petrological parameters of the rock and external factors in the area where the building is sited, such as weather conditions, pollution, and so on. Depending on the environmental conditions and the characteristics of the materials used, different types of weathering predominate. In all, the appearance of surface crusts constitutes a first stage, whose origin can often be traced to the properties of the material itself. In the present study, different colours of “patinas” were distinguished by defining the threshold levels of greys associated with “pathology” in the histogram. These data were compared to background information and other parameters, such as mineralogical composition, porosity, and so on, as well as other visual signs of deterioration. The result is a map of the pathologies associated with “cover films” on monuments, which generate images by relating colour characteristics to desired properties or zones of interest.

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.