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Institute
- Mathematisch-Naturwissenschaftliche Fakultät (80)
- Institut für Slavistik (75)
- Institut für Geowissenschaften (41)
- Humanwissenschaftliche Fakultät (39)
- Institut für Chemie (39)
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- Institut für Biochemie und Biologie (30)
- Vereinigung für Jüdische Studien e. V. (29)
- Bürgerliches Recht (28)
- Department Linguistik (23)
Der Jüdische Friedhof in Potsdam ist der einzige authentische Gedächtnisort, der vom Lebenszyklus der jüdischen Bevölkerung in der ehemaligen preußischen Residenz- und Garnisonstadt zeugt. Er ist zudem Ausdruck des unterschiedlichen Umgangs der Nachgeborenen mit ihrem Kulturgut. Außerdem ist dieser Jüdische Friedhof zurzeit als einziger in Deutschland durch die UNESCO als Welterbe anerkannt.
Da die jüdische Geschichte Potsdams bislang nur wenig bekannt ist, entstand ein durch die Stiftung „Erinnerung, Verantwortung und Zukunft“ gefördertes Projekt, in dem sich Schüler*innen des Potsdamer Humboldt-Gymnasiums im Rahmen eines Seminarkurses mit dem jüdischen Erbe ihrer Stadt intensiv auseinandersetzten. Neben einer Annäherung an das Thema über verschiedene, den Friedhof betreffende Sachthemen beschäftigten sich die Jugendlichen mit einzelnen jüdischen Potsdamern, ihren Familienschicksalen und Lebenskonzepten. Ergänzend wurden Aspekte des religiösen Verständnisses von Tod und Trauer im Judentum vorgestellt.
Die Ergebnisse all dieser Ausarbeitungen sind im vorliegenden Lehrmaterial vereinigt und dienen als Anregung für Lehrende und Lernende, die jüdische Geschichte ihrer jeweiligen Heimatorte zu thematisieren.
LifE
(2016)
Die LifE-Studie (Lebensverläufe ins fortgeschrittene Erwachsenenalter) ist eine der wenigen Studien weltweit, in der Lebensläufe vom 12. bis zum 45. Lebensjahr nachgezeichnet werden. Es wird bislang eine Spanne von über 30 Jahren betrachtet. Im Mittelpunkt steht die Frage nach den Bedingungen produktiver Lebensbewältigung im jungen und mittleren Lebensalter. Damit wird auch die Frage nach den Risiken nicht gelingender Lebensbewältigung thematisiert. Insbesondere ist von Interesse, welche herkunftsbezogenen, persönlichen und sozialen Ressourcen zu einer gelingenden Lebensbewältigung beitragen. Wie entwickeln und verändern sich bereichsspezifische Domänen, wie etwa Partnerschaft und Familie, die Erwerbstätigkeit oder auch die Identität im Leben? Welche Faktoren haben eine prädikative Wirkung über mehrere Jahrzehnte, welche Faktoren haben nur temporäre Bedeutung?
Der erste Teil dieses Berichts stellt die Durchführung und das Konzept der LifE-Studie vor. Der zweite Teil betrachtet das Teilnahmeverhalten seit Beginn der Jugendstudie 1979 über die erste Follow-Up-Studie im Jahre 2002 bis zur letzten Erhebung 2012. Ausfälle sind bei einem Untersuchungszeitraum von über 30 Jahren unvermeidbar. Eine Herausforderung von langangelegten Panelstudien stellt das Wiederauffinden und Motivieren der Teilnehmer dar, dass sie langfristig – über Jahrzehnte – an der Studie partizipieren. Insbesondere wird daher nach den Ausfallgründen gefragt.
Um eine untersuchte Alterskohorte als repräsentativ für einen Jahrgang betrachten zu können, ist es notwendig zu überprüfen, ob und in welchem Ausmaß die Personen, die über einen solchen langen Zeitraum an einer Studie teilgenommen haben, eine herausragend selektive Gruppe darstellen. Um dies zu überprüfen, werden ausgewählte soziodemografische Merkmale der Stichprobe der Erhebung 2012 (1.359 Teilnehmende) mit den entsprechenden Verteilungen des SOEP 2012 und des Mikrozensus 2012 verglichen. Durch diese externe Validierung werden mögliche Verzerrungen der Datengrundlage der Studie sichtbar.
Im Verlauf dieser Arbeit sind Blockcopolymere verschiedener Ladung auf Basis von PEO mit hohen Molekulargewichten durch lebendende freie radikalische Polymerisation hergestellt worden. Die Polymere sind einfach im Grammmaßstab herstellbar. Sie zeigen sowohl einen großen Einfluss auf die Nukleation als auch auf die Auflösung von Calciumphosphat. Gleichwohl scheint das Vorhandensein von positiven Gruppen (Kationen, Ampholyten und Betainen) keinen dramatischen Einfluss auf die Nukleation zu haben.
So verursachen Polymere mit positiven Ladungen die gleiche Retentionwirkung wie solche, die ausschließlich anionische Gruppen enthalten. Aus der Verwendung der kationischen, ampholytischen und betainischen Copolymere resultiert allerdings eine andersartige Morphologie der Niederschläge, als aus der Verwendung der Anionischen hervorgeht. Bei der Stabilisierung einer HAP-Oberfläche setzt sich dieser Trend fort, das heißt, rein anionische Copolymere wirken stärker stabilisierend als solche, die positive Ladungen enthalten. Durch Inkubation von menschlichem Zahnschmelz mit anionischen Copolymeren konnte gezeigt werden, dass die Biofilmbildung verglichen mit einer unbehandelten Zahnoberfläche eingeschränkt abläuft. All dies macht die Polymere zu interessanten Additiven für Zahnpflegeprodukte.
Zusätzlich konnten auf Basis dieser rein anionischen Copolymere Polymerbürsten, ebenfalls über lebendende freie radikalische Polymerisation, hergestellt werden. Diese zeichnen sich durch einen großen Einfluss auf die Kristallphase aus und bilden mit dem CHAP des AB-Types das Material, welches auch in Knochen und Zähnen vorkommt. Erste Cytotoxizitätstests lassen auf das große Potential dieser Polymerbürsten für Beschichtungen in der Medizintechnik schließen.
The aim of this work is the evaluation of the geothermal potential of Luxembourg. The approach consists in a joint interpretation of different types of information necessary for a first rather qualitative assessment of deep geothermal reservoirs in Luxembourg and the adjoining regions in the surrounding countries of Belgium, France and Germany. For the identification of geothermal reservoirs by exploration, geological, thermal, hydrogeological and structural data are necessary. Until recently, however, reliable information about the thermal field and the regional geology, and thus about potential geothermal reservoirs, was lacking. Before a proper evaluation of the geothermal potential can be performed, a comprehensive survey of the geology and an assessment of the thermal field are required.
As a first step, the geology and basin structure of the Mesozoic Trier–Luxembourg Basin (TLB) is reviewed and updated using recently published information on the geology and structures as well as borehole data available in Luxembourg and the adjoining regions. A Bouguer map is used to get insight in the depth, morphology and structures in the Variscan basement buried beneath the Trier–Luxembourg Basin. The geological section of the old Cessange borehole is reinterpreted and provides, in combination with the available borehole data, consistent information for the production of isopach maps. The latter visualize the synsedimentary evolution of the Trier–Luxembourg Basin. Complementary, basin-wide cross sections illustrate the evolution and structure of the Trier–Luxembourg Basin. The knowledge gained does not support the old concept of the Weilerbach Mulde. The basin-wide cross sections, as well as the structural and sedimentological observations in the Trier–Luxembourg Basin suggest that the latter probably formed above a zone of weakness related to a buried Rotliegend graben. The inferred graben structure designated by SE-Luxembourg Graben (SELG) is located in direct southwestern continuation of the Wittlicher Rotliegend-Senke.
The lack of deep boreholes and subsurface temperature prognosis at depth is circumnavigated by using thermal modelling for inferring the geothermal resource at depth. For this approach, profound structural, geological and petrophysical input data are required. Conceptual geological cross sections encompassing the entire crust are constructed and further simplified and extended to lithospheric scale for their utilization as thermal models. The 2-D steady state and conductive models are parameterized by means of measured petrophysical properties including thermal conductivity, radiogenic heat production and density. A surface heat flow of 75 ∓ 7 (2δ) mW m–2 for verification of the thermal models could be determined in the area. The models are further constrained by the geophysically-estimated depth of the lithosphere–asthenosphere boundary (LAB) defined by the 1300 °C isotherm. A LAB depth of 100 km, as seismically derived for the Ardennes, provides the best fit with the measured surface heat flow. The resulting mantle heat flow amounts to ∼40 mW m–2. Modelled temperatures are in the range of 120–125 °C at 5 km depth and of 600–650 °C at the crust/mantle discontinuity (Moho). Possible thermal consequences of the 10–20 Ma old Eifel plume, which apparently caused upwelling of the asthenospheric mantle to 50–60 km depth, were modelled in a steady-state thermal scenario resulting in a surface heat flow of at least 91 mW m–2 (for the plume top at 60 km) in the Eifel region. Available surface heat-flow values are significantly lower (65–80 mW m–2) and indicate that the plume-related heating has not yet entirely reached the surface.
Once conceptual geological models are established and the thermal regime is assessed, the geothermal potential of Luxembourg and the surrounding areas is evaluated by additional consideration of the hydrogeology, the stress field and tectonically active regions. On the one hand, low-enthalpy hydrothermal reservoirs in Mesozoic reservoirs in the Trier–Luxembourg Embayment (TLE) are considered. On the other hand, petrothermal reservoirs in the Lower Devonian basement of the Ardennes and Eifel regions are considered for exploitation by Enhanced/Engineered Geothermal Systems (EGS). Among the Mesozoic aquifers, the Buntsandstein aquifer characterized by temperatures of up to 50 °C is a suitable hydrothermal reservoir that may be exploited by means of heat pumps or provide direct heat for various applications. The most promising area is the zone of the SE–Luxembourg Graben. The aquifer is warmest underneath the upper Alzette River valley and the limestone plateau in Lorraine, where the Buntsandstein aquifer lies below a thick Mesozoic cover. At the base of an inferred Rotliegend graben in the same area, temperatures of up to 75 °C are expected. However, geological and hydraulic conditions are uncertain. In the Lower Devonian basement, thick sandstone-/quartzite-rich formations with temperatures >90 °C are expected at depths >3.5 km and likely offer the possibility of direct heat use. The setting of the Südeifel (South Eifel) region, including the Müllerthal region near Echternach, as a tectonically active zone may offer the possibility of deep hydrothermal reservoirs in the fractured Lower Devonian basement. Based on the recent findings about the structure of the Trier–Luxembourg Basin, the new concept presents the Müllerthal–Südeifel Depression (MSD) as a Cenozoic structure that remains tectonically active and subsiding, and therefore is relevant for geothermal exploration. Beyond direct use of geothermal heat, the expected modest temperatures at 5 km depth (about 120 °C) and increased permeability by EGS in the quartzite-rich Lochkovian could prospectively enable combined geothermal heat production and power generation in Luxembourg and the western realm of the Eifel region.
Das vorliegende Werk ist das Ergebnis der 3. Woche des Russischen Rechts an der Juristischen Fakultät der Universität Potsdam. Namhafte Wissenschaftlerinnen und Wissenschaftler der Moskauer Staatlichen Juristischen Universität O. E. Kutafin hielten Vorträge zum Völkerrecht, Verfassungs- und Staatsangehörigkeitsrecht, Bürgerlichen Recht, Unternehmens- und Gesellschaftsrecht, Finanzrecht und Bankrecht. Das russische Recht befindet sich nach dem Ende der Sowjetunion im Wandel. Die Beiträge zeugen vom hohen Stand der Jurisprudenz an der Moskauer Staatlichen Juristischen Universität O. E. Kutafin. Die Wochen des Russischen Rechts tragen dazu bei, das Recht der Russischen Föderation bei uns in Deutschland bekannt zu machen und rechtsvergleichend zur Diskussion zu stellen.
The aim of this paper is to bring together two areas which are of great importance for the study of overdetermined boundary value problems. The first area is homological algebra which is the main tool in constructing the formal theory of overdetermined problems. And the second area is the global calculus of pseudodifferential operators which allows one to develop explicit analysis.
This article assesses the distance between the laws of stochastic differential equations with multiplicative Lévy noise on path space in terms of their characteristics. The notion of transportation distance on the set of Lévy kernels introduced by Kosenkova and Kulik yields a natural and statistically tractable upper bound on the noise sensitivity. This extends recent results for the additive case in terms of coupling distances to the multiplicative case. The strength of this notion is shown in a statistical implementation for simulations and the example of a benchmark time series in paleoclimate.
Grenzräume – Grenzbewegungen
(2016)
Der vorliegende Sammelband vereinigt die Beiträge der 12. und 13. Tagung des Jungen Forums Slavistische Literaturwissenschaft (JFSL) in Basel 2013 und Frankfurt (Oder) und Słubice 2014. Unter den thematischen Leitbegriffen Grenzräume – Grenzbewegungen präsentiert er Einblicke in die Arbeit von Nachwuchswissenschaftlerinnen und -wissenschaftlern der deutschsprachigen slavischen Literatur- und Kulturwissenschaft.