Zur Darstellung und Interpretation archäologischer und geowissenschaftlicher Untersuchungen anhand einer Auswahl römischer Gebrauchskeramik aus dem Limeskastell Saalburg

Die vorliegende Arbeit gliedert sich in drei Kapitel. Das erste Kapitel umfasst dabei die Darstellung von Methoden, die zum gegenwärtigen Zeitpunkt unter anderem in der provinzialrömischen Archäologie zur Untersuchung von Gefäßkeramik üblich sind, wobei die Einzelergebnisse des im Rahmen dieser Arbeit untersuchten gebrauchskeramischen Materials (Randfragmente) der Saalburg (bei Bad Homburg) am Ende des Kapitels zusammengefasst werden. Im zweiten Kapitel werden anhand des gleichen Materials einige naturwissenschaftliche Methoden dargestellt, die zur Materialanalyse sowohl in den Geowissenschaften (Materialwissenschaft), als auch in der Archäometrie häufig Anwendung finden und deren Ergebnisse am Ende des Kapitels zusammengefasst. In einer Gesamtbetrachtung (drittes Kapitel) werden schließlich diese hinsichtlich ihrer Aussagekraft in archäologischem Kontext evaluiert. Neben der im Anhang festgehaltenen Original-dokumentation der Dünnschliff-Untersuchungen (Ramanspektroskopie, „RS“), werden im Abbildungsteil die Kopien der Originaldaten aus der Röntgendiffraktometrie („XRD“) und der Röntgenfluoreszenzanalyse („RFA“, chemische Analyse), Abbildungen einiger Festkörper, als auch Zeichnungen, Photos und Dünnschliffe der Randfragmente aufgeführt. Während die Darstellung der angewandten Methoden einer Verständniserleichterung vor allem der komplexen chemisch-physikalischen Zusammenhänge dienen soll - nicht zuletzt auch, um die künftige Methodenwahl zu optimieren - soll mittels der Evaluation, vor allem für die Keramikforschung, die Entwicklung neuer Forschungsmethoden unterstützt werden. Aus dem Vergleich der Ergebnisse beider Kapitel erhebt sich nicht allein für die Keramikforschung die Frage, inwieweit die Anwendungen bestimmter Untersuchungen überhaupt sinnvoll sind, wenn sie nicht nur der Bestätigung dienen sollen, sondern welche Konsequenzen daraus auch für die Untersuchung anderer historisch-kultureller Materialgruppen resultieren könnten.

Historisches Grabenreißen im Wassereinzugsgebiet der Aar zwischen Wiesbaden und Limburg

Im Wassereinzugsgebiet der Aar zwischen Taunuskamm und Limburger Becken wurden 242 Erosionsschluchten, so genannte Runsen kartiert. Die vorgefundenen geomorphologischen Formen sind zum Teil mehr als 15 Meter tief, kerben- oder kastenförmig. Einige führen ein zeitweise oder ständig fließendes Gerinne. Die Untersuchung acht verschiedener Einzelbeispiele mit geomorphologischen, bodenkundlichen und kulturhistorischen Methoden ergab, dass die Erosionsschluchten in geschichtlicher Zeit entstanden sind. Damit wurden die Ergebnisse von BORK 1988, 1985, BORK et al. 1998, BAUER 1995, 1993, SEMMEL 1963, HEMPEL 1954, 1954 und HARD 1970 weitgehend bestätigt. Die Runsen an der Aar und ihrer Nebenbäche sind das Ergebnis exzessiver Erosionsprozesse, die in Folge einer erheblichen Übernutzung der Landschaft durch Köhlerei, Eisenerzverhüttung und Landwirtschaft hauptsächlich im 17. und 18. Jahrhundert ausgelöst wurden. Dabei kommt der seit 1656 betriebenen Michelbacher Hütte als landesherrliches Eisenwerk eine besondere Rolle zu. Ein weiterer Einfluss geht auf die spezifische Geofaktorenkonstellation im Untertaunus zurück. Die dort verbreiteten stark tonig verwitterten Schiefer und erodierten Parabraunerden fördern den Oberflächenabfluss, der während zeitweise auftretender Starkregenereignisse an den Hängen zum Einreißen von Erosionsschluchten führen kann . Zur Untersuchung des Phänomens wurden sowohl geomorphologische und bodenkundliche als auch historisch-kulturlandschaftgenetische Methoden herangezogen. Neben der bodenkundlichen Beprobung zahlreicher Aufschlüsse wurden auch Analysen mittels der Radiokarbonmethode, Schwermineralanalysen, Kohlholzspektren historischer Meilerplätze und die Auswertung von Archivunterlagen als Methoden herangezogen. Als grundlegendes Ergebnis liefert die vorliegende Arbeit einen umfassenden Abriss der Nutzungsgeschichte im Wassereinzugsgebiet der Aar von vorgeschichtlicher Zeit bis zum heutigen Tage. Zudem werden die naturräumlichen Einflussfaktoren, die die Entstehung von Erosionsschluchten erst ermöglichen, auf umfassende Weise dargestellt. Zwei Exkurse behandeln die Bedeutung der spätmittelalterlichen Landwehr bei Hennethal, die während der Geländearbeiten entdeckt wurde sowie die Entstehung und zeitliche Einordnung der Auelehme im Aartal.

Investigations on maar-diatreme volcanoes by inversion of magnetic and gravity data from the Eifel area, Germany

A study of maar-diatreme volcanoes has been perfomed by inversion of gravity and magnetic data. The geophysical inverse problem has been solved by means of the damped nonlinear least-squares method. To ensure stability and convergence of the solution of the inverse problem, a mathematical tool, consisting in data weighting and model scaling, has been worked out. Theoretical gravity and magnetic modeling of maar-diatreme volcanoes has been conducted in order to get information, which is used for a simple rough qualitative and/or quantitative interpretation. The information also serves as a priori information to design models for the inversion and/or to assist the interpretation of inversion results. The results of theoretical modeling have been used to roughly estimate the heights and the dip angles of the walls of eight Eifel maar-diatremes — each taken as a whole. Inversemodeling has been conducted for the Schönfeld Maar (magnetics) and the Hausten-Morswiesen Maar (gravity and magnetics). The geometrical parameters of these maars, as well as the density and magnetic properties of the rocks filling them, have been estimated. For a reliable interpretation of the inversion results, beside the knowledge from theoretical modeling, it was resorted to other tools such like field transformations and spectral analysis for complementary information. Geologic models, based on thesynthesis of the respective interpretation results, are presented for the two maars mentioned above. The results gave more insight into the genesis, physics and posteruptive development of the maar-diatreme volcanoes. A classification of the maar-diatreme volcanoes into three main types has been elaborated. Relatively high magnetic anomalies are indicative of scoria cones embeded within maar-diatremes if they are not caused by a strong remanent component of the magnetization. Smaller (weaker) secondary gravity and magnetic anomalies on the background of the main anomaly of a maar-diatreme — especially in the boundary areas — are indicative for subsidence processes, which probably occurred in the late sedimentation phase of the posteruptive development. Contrary to postulates referring to kimberlite pipes, there exists no generalized systematics between diameter and height nor between geophysical anomaly and the dimensions of the maar-diatreme volcanoes. Although both maar-diatreme volcanoes and kimberlite pipes are products of phreatomagmatism, they probably formed in different thermodynamic and hydrogeological environments. In the case of kimberlite pipes, large amounts of magma and groundwater, certainly supplied by deep and large reservoirs, interacted under high pressure and temperature conditions. This led to a long period phreatomagmatic process and hence to the formation of large structures. Concerning the maar-diatreme and tuff-ring-diatreme volcanoes, the phreatomagmatic process takes place due to an interaction between magma from small and shallow magma chambers (probably segregated magmas) and small amounts of near-surface groundwater under low pressure and temperature conditions. This leads to shorter time eruptions and consequently to structures of smaller size in comparison with kimberlite pipes. Nevertheless, the results show that the diameter to height ratio for 50% of the studied maar-diatremes is around 1, whereby the dip angle of the diatreme walls is similar to that of the kimberlite pipes and lies between 70 and 85°. Note that these numerical characteristics, especially the dip angle, hold for the maars the diatremes of which — estimated by modeling — have the shape of a truncated cone. This indicates that the diatreme can not be completely resolved by inversion.

Transatlantic negotiations on "hell"?: W. E. B. Du Bois's visit to fascist Germany and Theodor W. Adorno's exile in the land of the culture industry

In 1936, the African-American intellectual W.E.B. Du Bois visited Nazi Germany for a period of five months. Two years later, the eleven-year-long American exile of the German philosopher Theodor W. Adorno began. From the latter’s perspective, the United States was the “home” of the Culture Industry. One intuitively assumes that these sojourns abroad must have amounted to “hell on earth” for both the civil rights activist W.E.B. Du Bois and the subtle intellectual Adorno. But was this really the case? Or did they perhaps arrive at totally different conclusions? This thesis deals with these questions and attempts to make sense of the experiences of both men. By way of a systematic and comparative analysis of published texts, hitherto unpublished documents and secondary literature, this dissertation first contextualizes Du Bois’s and Adorno’s transatlantic negotiations and then depicts them. The panoply of topics with which both men concerned themselves was diverse. In Du Bois’s case it encompassed Europe, science and technology, Wagner operas, the Olympics, industrial education, race relations, National Socialism and the German Africanist Diedrich Westermann. The opinion pieces which Du Bois wrote for the newspaper “Pittsburgh Courier” during his stay in Germany serve as a major source for this thesis. In his writings on America, Adorno concentrated on what he regarded as the universally victorious Enlightenment and the predominance of mass culture. This investigation also sheds light on the correspondences between the philosopher and Max Horkheimer, Thomas Mann, Walter Benjamin, Siegfried Kracauer and Oskar and Maria Wiesengrund. In these autobiographical texts, Adorno’s thoughts revolve around such diverse topics as the American landscape, his fears as German, Jew and Left-Hegelian as well as the loneliness of the refugee. This dissertation has to refute the intuitive assumption that Du Bois’s and Adorno’s experiences abroad were horrible events for them. Both men judged the foreign countries in which they were staying in an extremely differentiated and subtle manner. Du Bois, for example, was not racially discriminated against in Germany. He was also delighted by the country’s rich cultural offerings. Adorno, for his part, praised the U.S.’s humanity of everyday life and democratic spirit. In short: Although both men partly did have to deal with utterly negative experiences, the metaphor of “hell on earth” is simply untenable as an overall conclusion.

The reconstruction of paleoclimate variability in Northern Germany, during marine isotope stage 5

In order to obtain a better understanding about the influence of post-depositional diagenesis on speleothem 230Th/U-ages and paleoclimate variability during Marine Isotope Stage (MIS) 5 in northern Germany, four stalagmites from the Riesenberghöhle (RBH) were investigated by thin section analysis, 230Th/U-dating as well as stable oxygen and carbon isotope and laser ablation inductively coupled mass spectrometry (LA-ICPMS) trace element analysis. The RBH is located in the Weser Hills and is one of the northernmost limestone caves in Germany.rnMulti collector (MC) ICPMS 230Th/U-ages and thin section analysis of the RBH stalagmites shows that some growth phases of the stalagmites were diagenetically altered after their deposition. The impact of post-depositional diagenesis (PDD) on the 230Th/U-ages is modeled, and potential processes leading to PDD are discussed. In this context, it is suggested that PDD may be induced by rapid climate change at the inception of the GIS.rnDespite of the dating uncertainties resulting from PDD, 230Th/U-dating shows that the RBH stalagmites grew during the Eemian and most of the Greenland Interstadials (GIS) during MIS 5. Thus, the growth phases of the RBH stalagmites might be related to a reorganization of the Atlantic Meridional Overturning Circulation (AMOC). The stable isotope (δ13C and δ18O) and the trace element variability of the stalagmites reflects rapid changes of past temperature and precipitation on millennial and sub-millennial timescales. These past climate changes can be amplified by orbitally forced variations of the July solar insolation at 65°N.

Sustainable improvement of water networks : to achieve best decisions for rehabilitation plans using advanced GIS and statistical techniques

Many of developing countries are facing crisis in water management due to increasing of population, water scarcity, water contaminations and effects of world economic crisis. Water distribution systems in developing countries are facing many challenges of efficient repair and rehabilitation since the information of water network is very limited, which makes the rehabilitation assessment plans very difficult. Sufficient information with high technology in developed countries makes the assessment for rehabilitation easy. Developing countries have many difficulties to assess the water network causing system failure, deterioration of mains and bad water quality in the network due to pipe corrosion and deterioration. The limited information brought into focus the urgent need to develop economical assessment for rehabilitation of water distribution systems adapted to water utilities. Gaza Strip is subject to a first case study, suffering from severe shortage in the water supply and environmental problems and contamination of underground water resources. This research focuses on improvement of water supply network to reduce the water losses in water network based on limited database using techniques of ArcGIS and commercial water network software (WaterCAD). A new approach for rehabilitation water pipes has been presented in Gaza city case study. Integrated rehabilitation assessment model has been developed for rehabilitation water pipes including three components; hydraulic assessment model, Physical assessment model and Structural assessment model. WaterCAD model has been developed with integrated in ArcGIS to produce the hydraulic assessment model for water network. The model have been designed based on pipe condition assessment with 100 score points as a maximum points for pipe condition. As results from this model, we can indicate that 40% of water pipeline have score points less than 50 points and about 10% of total pipes length have less than 30 score points. By using this model, the rehabilitation plans for each region in Gaza city can be achieved based on available budget and condition of pipes. The second case study is Kuala Lumpur Case from semi-developed countries, which has been used to develop an approach to improve the water network under crucial conditions using, advanced statistical and GIS techniques. Kuala Lumpur (KL) has water losses about 40% and high failure rate, which make severe problem. This case can represent cases in South Asia countries. Kuala Lumpur faced big challenges to reduce the water losses in water network during last 5 years. One of these challenges is high deterioration of asbestos cement (AC) pipes. They need to replace more than 6500 km of AC pipes, which need a huge budget to be achieved. Asbestos cement is subject to deterioration due to various chemical processes that either leach out the cement material or penetrate the concrete to form products that weaken the cement matrix. This case presents an approach for geo-statistical model for modelling pipe failures in a water distribution network. Database of Syabas Company (Kuala Lumpur water company) has been used in developing the model. The statistical models have been calibrated, verified and used to predict failures for both networks and individual pipes. The mathematical formulation developed for failure frequency in Kuala Lumpur was based on different pipeline characteristics, reflecting several factors such as pipe diameter, length, pressure and failure history. Generalized linear model have been applied to predict pipe failures based on District Meter Zone (DMZ) and individual pipe levels. Based on Kuala Lumpur case study, several outputs and implications have been achieved. Correlations between spatial and temporal intervals of pipe failures also have been done using ArcGIS software. Water Pipe Assessment Model (WPAM) has been developed using the analysis of historical pipe failure in Kuala Lumpur which prioritizing the pipe rehabilitation candidates based on ranking system. Frankfurt Water Network in Germany is the third main case study. This case makes an overview for Survival analysis and neural network methods used in water network. Rehabilitation strategies of water pipes have been developed for Frankfurt water network in cooperation with Mainova (Frankfurt Water Company). This thesis also presents a methodology of technical condition assessment of plastic pipes based on simple analysis. This thesis aims to make contribution to improve the prediction of pipe failures in water networks using Geographic Information System (GIS) and Decision Support System (DSS). The output from the technical condition assessment model can be used to estimate future budget needs for rehabilitation and to define pipes with high priority for replacement based on poor condition. rn

Anthropology in the twenty-first century : a view of, and from, Germany

The article explores the developments in German-language anthropology in the past decades, focussing on the period after the 1970s. It argues that the recent history of German-language Ethnologie (social and cultural anthropology) is one of catching-up modernization. German-speaking anthropologists are increasingly involved in, and contribute to, broader theoretical debates, publish in English and in international journals, and are actively engaged in international academic networks. The paper discusses how and under what conditions of knowledge production these transformations have taken place. It analyses the changing institutional environment in which German anthropologists have worked and work today, as well as the theoretical impulses from within and outside the discipline that have given rise to the contemporary orientation of German-language anthropology as an anthropology of the 'present'. Finally, and beyond the focus on Germany, the article offers some ideas on the future of anthropology as a symmetrical social science, characterized by a continued strong reliance on field work and a high level of 'worldliness', a basic attitude of systematically shifting perspectives, the critical reflection of the social and political embeddedness of knowledge production, and an engagement with social theory across disciplinary boundaries.