Physical and mineralogical changes of Hungarian monumental stones exposed to different conditions: stone-testing in-situ and under laboratory conditions

The Székesfehérvár Ruin Garden is a unique assemblage of monuments belonging to the cultural heritage of Hungary due to its important role in the Middle Ages as the coronation and burial church of the Kings of the Hungarian Christian Kingdom. It has been nominated for “National Monument” and as a consequence, its protection in the present and future is required. Moreover, it was reconstructed and expanded several times throughout Hungarian history. By a quick overview of the current state of the monument, the presence of several lithotypes can be found among the remained building and decorative stones. Therefore, the research related to the materials is crucial not only for the conservation of that specific monument but also for other historic structures in Central Europe. The current research is divided in three main parts: i) description of lithologies and their provenance, ii) physical properties testing of historic material and iii) durability tests of analogous stones obtained from active quarries. The survey of the National Monument of Székesfehérvár, focuses on the historical importance and the architecture of the monument, the different construction periods, the identification of the different building stones and their distribution in the remaining parts of the monument and it also included provenance analyses. The second one was the in situ and laboratory testing of physical properties of historic material. As a final phase samples were taken from local quarries with similar physical and mineralogical characteristics to the ones used in the monument. The three studied lithologies are: fine oolitic limestone, a coarse oolitic limestone and a red compact limestone. These stones were used for rock mechanical and durability tests under laboratory conditions. The following techniques were used: a) in-situ: Schmidt Hammer Values, moisture content measurements, DRMS, mapping (construction ages, lithotypes, weathering forms) b) laboratory: petrographic analysis, XRD, determination of real density by means of helium pycnometer and bulk density by means of mercury pycnometer, pore size distribution by mercury intrusion porosimetry and by nitrogen adsorption, water absorption, determination of open porosity, DRMS, frost resistance, ultrasonic pulse velocity test, uniaxial compressive strength test and dynamic modulus of elasticity. The results show that initial uniaxial compressive strength is not necessarily a clear indicator of the stone durability. Bedding and other lithological heterogeneities can influence the strength and durability of individual specimens. In addition, long-term behaviour is influenced by exposure conditions, fabric and, especially, the pore size distribution of each sample. Therefore, a statistic evaluation of the results is highly recommended and they should be evaluated in combination with other investigations on internal structure and micro-scale heterogeneities of the material, such as petrographic observation, ultrasound pulse velocity and porosimetry. Laboratory tests used to estimate the durability of natural stone may give a good guidance to its short-term performance but they should not be taken as an ultimate indication of the long-term behaviour of the stone. The interdisciplinary study of the results confirms that stones in the monument show deterioration in terms of mineralogy, fabric and physical properties in comparison with quarried stones. Moreover stone-testing proves compatibility between quarried and historical stones. Good correlation is observed between the non-destructive-techniques and laboratory tests results which allow us to minimize sampling and assessing the condition of the materials. Concluding, this research can contribute to the diagnostic knowledge for further studies that are needed in order to evaluate the effect of recent and future protective measures.

Study of the building and decorative materials and techniques used in Hungarian Roman sites

The aims of this research were: - To identify the characteristics, properties and provenance of the building and decorative material found in three Hungarian Roman sites: Nagyharsány, Nemesvámos-Balácapuszta and Aquincum - To provide a database of information on the different sites - To have an overview of main conservation strategies applied in Hungary. Geological studies, macroscopical and microscopical observations, XRD investigations, physical and chemical analyses allowed us to define the characteristics and properties of the different kinds of collected materials. Building stones sampled from Nagyharsány site showed two different kinds of massive limestone belonging to the areas surrounding the villa. Also Building stones sampled from Nemesvámos-Balácapuszta Roman villa proved to be compatible with limestone belonging to local sources. Mural painting fragments show that all samples are units composed of multilayered structures. Mosaic tesserae can be classified as following: -Pale yellow , blackish and pink tesserae are comparable with local limestone; -White tessera, composed of marble, was probably imported from distant regions of the Empire, as the usual practice of Romans. Mortars present different characteristics according to the age, the site and the functions: -Building mortars are generally lime based, white or pale yellow in colour, present a high percentage of aggregates represented by fine sand; -Supporting mortars from both mosaics and mural paintings are reddish or pinkish in colour, due to the presence of high percentage of brick dust and tiles fragments, and present a higher content of MgO. Although the condition of the sites, there is an insignificant content of soluble salts. Database The whole study has allowed us to provide work sheets for each samples, including all characteristics and properties. Furthermore, all sites included in the frame of the research have been described and illustrated on the base of their floor plans, material and construction methodologies. It can be concluded that: 1. In Nagyharsány Archaeological site, it is possible to define a sequence of different construction phases on the base of the study of building material and mortars. The results are comparable with the chronology of the site provided by the archaeologists 2. The material used for construction was of local origin while the more precious ones, used for decorative elements, were probably imported from long distance 3. Construction techniques in Hungary mainly refer to the usual Roman knowledge and practice (Vitruvius); few differences have been found 4. The database will represent an archive for Archaeologists, Historians and Conservators dealing with Roman period in Hungary.

"Weil eine Fremd’ ich bin, aus fernem Land ...“ – Fremdheit und Fremde im dramatischen Werk Franz Grillparzers und Friedrich Hebbels

Große Dramendichtung kann nur in historischen Umbruchszeiten wie der Antike, der Reformationszeit und im 19. Jahrhundert, also zu Lebzeiten Friedrich Hebbels, entstehen. Das schreibt Hebbel im Vorwort zu seinem bürgerlichen Trauerspiel „Maria Magdalena“. Die großen Zeiten der Tragödien sind Zeiten umwälzender Veränderungen. Im langen 19. Jahrhundert, zwischen Revolution und Restauration, zwischen Reformen und Reaktion, zwischen Hoffnungen auf Demokratie, Nationalstaatlichkeit, zwischen Josephinismus und Ära Metternich, waren die Voraussetzungen für ein Jahrhundert der Tragödie gegeben. Zwei der bedeutendsten Dramatiker des 19. Jahrhunderts, Franz Grillparzer und Friedrich Hebbel, sind Thema der Dissertation. Dabei hat die Arbeit mit der Diskursivierung von Fremdheit und Fremde eine Neuperspektivierung ausgewählter Dramen geleistet, die so in der Forschung noch nicht existiert, wobei diese Perspektive in der Forschung bereits angelegt war. Die hier vorliegende Arbeit hat das „Phänomen der Fremde“, wie Günther Häntzschel es in einem Aufsatz nennt, in den Dramen „Judith“, „Gyges und sein Ring“ und „Die Nibelungen“ von Hebbel und in den Dramen „Das goldene Vließ“, „Die Jüdin von Toledo“ und „Libussa“ von Grillparzer untersucht. Die zentralen Begriffe „Fremde“ und „Fremdheit“ wurden dabei als literarische Topoi, um methodisch besser mit ihnen operieren zu können, in verschiedene Dimensionen der Fremdheit unterteilt: Dabei wurde neben der „Fremdheit der Kulturen“ und der „Fremdheit zwischen den Geschlechtern“ auch die Fremdheit zwischen dem „mythischen Rand der Welt“ und dem „Horizont der Vernunft“ untersucht. Ferner widmete sich ein Kapitel dem Thema Entfremdung und Selbstentfremdung, eine Dimension der Fremdheit, die ebenfalls für die Dramenanalyse relevant ist.

Cantate dialogiche e serenate (1706-1710) di Georg Friedrich Händel

La dissertazione è uno studio monografico delle cantate dialogiche e delle serenate a più voci e strumenti composte da Händel in Italia negli anni 1706-1710. Insieme ai drammi per musica e agli oratori coevi, le quattro cantate "Aminta e Fillide" HWV 83, "Clori, Tirsi e Fileno" HWV 96, "Il duello amoroso" HWV 82, "Apollo e Dafne" HWV 122 e le due serenate "Aci, Galatea e Polifemo" HWV 72 e "Olinto pastore arcade alle glorie del Tebro" HWV 143 costituiscono le prime importanti affermazioni di Händel come compositore di musica vocale. Le sei composizioni sono state studiate sotto l’aspetto storico-letterario, drammaturgico-musicale e della committenza, con l’obiettivo di individuare intersecazioni fra questi piani. I testi poetici, di cui si è curata l’edizione, sono stati analizzati da un punto di vista storico e stilistico e collocati nel particolare contesto romano del primo Settecento, in cui la proibizione di ogni spettacolo teatrale determinò, sotto la spinta di una raffinata committenza, un ‘drammatizzazione’ dei generi della cantata e della serenata. L’analisi musicale di ciascuna composizione è stata dunque finalizzata a una lettura ‘drammaturgica’, che ha portato alla individuazione dei dispositivi di ascendenza teatrale nella scelte compositive di Händel. Lo studio si conclude con un selettivo confronto con le cantate e le serenate scritte negli stessi anni a Roma da Alessandro Scarlatti.

A river runs through it - ancient DNA data on the neolithic populations of the Great Hungarian Plain

This thesis was part of a multidisciplinary research project funded by the German Research Foundation (“Bevölkerungsgeschichte des Karpatenbeckens in der Jungsteinzeit und ihr Einfluss auf die Besiedlung Mitteleuropas”, grant no. Al 287/10-1) aimed at elucidating the population history of the Carpathian Basin during the Neolithic. The Carpathian Basin was an important waypoint on the spread of the Neolithic from southeastern to central Europe. On the Great Hungarian Plain (Alföld), the first farming communities appeared around 6000 cal BC. They belonged to the Körös culture, which derived from the Starčevo-Körös-Criş complex in the northern Balkans. Around 5600 cal BC the Alföld-Linearbandkeramik (ALBK), so called due to its stylistic similarities with the Transdanubian and central European LBK, emerged in the northwestern Alföld. Following a short “classical phase”, the ALBK split into several regional subgroups during its later stages, but did not expand beyond the Great Hungarian Plain. Marking the beginning of the late Neolithic period, the Tisza culture first appeared in the southern Alföld around 5000 cal BC and subsequently spread into the central and northern Alföld. Together with the Herpály and Csőszhalom groups it was an integral part of the late Neolithic cultural landscape of the Alföld. Up until now, the Neolithic cultural succession on the Alföld has been almost exclusively studied from an archaeological point of view, while very little is known about the population genetic processes during this time period. The aim of this thesis was to perform ancient DNA (aDNA) analyses on human samples from the Alföld Neolithic and analyse the resulting mitochondrial population data to address the following questions: is there population continuity between the Central European Mesolithic hunter-gatherer metapopulation and the first farming communities on the Alföld? Is there genetic continuity from the early to the late Neolithic? Are there genetic as well as cultural differences between the regional groups of the ALBK? Additionally, the relationships between the Alföld and the neighbouring Transdanubian Neolithic as well as other European early farming communities were evaluated to gain insights into the genetic affinities of the Alföld Neolithic in a larger geographic context. 320 individuals were analysed for this study; reproducible mitochondrial haplogroup information (HVS-I and/or SNP data) could be obtained from 242 Neolithic individuals. According to the analyses, population continuity between hunter-gatherers and the Neolithic cultures of the Alföld can be excluded at any stage of the Neolithic. In contrast, there is strong evidence for population continuity from the early to the late Neolithic. All cultural groups on the Alföld were heavily shaped by the genetic substrate introduced into the Carpathian Basin during the early Neolithic by the Körös and Starčevo cultures. Accordingly, genetic differentiation between regional groups of the ALBK is not very pronounced. The Alföld cultures are furthermore genetically highly similar to the Transdanubian Neolithic cultures, probably due to common ancestry. In the wider European context, the Alföld Neolithic cultures also highly similar to the central European LBK, while they differ markedly from contemporaneous populations of the Iberian Peninsula and the Ukraine. Thus, the Körös culture, the ALBK and the Tisza culture can be regarded as part of a “genetic continuum” that links the Neolithic Carpathian Basin to central Europe and likely has its roots in the Starčevo -Körös-Criş complex of the northern Balkans.