Academic literature on the topic 'Saxony'

Taking Christianisation as the process by which an entire society can be said to have become Christian, this article examines that phenomenon in ninth-century Saxony. The conversion of Saxony was unwelcome and imposed often by force, especially during the time of Charlemagne. This process of Christianisation is considered through two texts: 'Translato sancti Alexandrii and Translatio sancti Liborii'. The isolationism of the Saxons and the divine triumph over that position through Charlemagne are emphasised in these later accounts of the translation of the remains of saints Alexander and Liborius, whose bodies and the miracles associated with them helped reverse the reintroduction of paganism. At the same time, political necessity had seen the Saxons being granted the right to return to their old way of life in support of the Carolingian rulers. In the end, being Christian was portrayed as the best way to be Saxon and the process of Christianisation hastened.

The 1905 Kalender für das Erzgebirge und Vogtland described an apparently spontaneous shift in the relationship between the German state of Saxony's mountainous southern borderlands and its rapidly urbanizing lowlands. Yet from the 1870s to the 1930s, the Kalender, the Erzgebirgsverein that published it, and a host of similar Heimat (homeland) and tourist organizations pushed, prodded, and cajoled lowlanders into visiting the borderlands. In the process, they repeatedly reframed the ways in which they portrayed the landscapes they championed, rethought their reasons for enticing travelers to the southern regions, and redirected their efforts to new audiences. Saxon Heimatler and tourism promoters succeeded in defining southern Saxony's regions, and eventually Saxony as a whole, in terms of three important characteristics: the interplay of nature and industry in their landscapes; the diversity of those landscapes; and proximity to and interactions with Bohemia. So powerful were these themes that they continue to shape ideas about southern Saxony to the present.

The article deals with the diplomatic struggle for the Duchy of Luxembourg, which unfolded in 1438–1443 between the Duke of Burgundy, Philip III the Good, and the heirs of the House of Luxembourg. Not only representatives of the two dynasties were drawn into the conflict, but also a number of the most influential princes of the empire, such as Frederick III of Habsburg, the Archbishop of Trier, the Dukes of Saxony. Lacking direct rights to inherit Luxembourg, the Duke of Burgundy was able to offer its proprietress, Elisabeth de Görlitz, who held the duchy as a pledge, more favorable terms than William III of Saxony and the Archbishop of Trier, Jacques de Sirk. Philip the Good managed to achieve the neutrality of Emperor Frederick III and and win the trust of part of the Luxembourgish nobility. The entry into the duchy of Saxon contingents under the command of Count von Gleichen prevented the Duke of Burgundy from taking control of Luxembourg in 1442. Negotiations that took place during 1442-1443. did not result in an agreement between the parties. Despite the fact that by 1443 the Saxons controlled most of the duchy, Burgundian diplomacy managed to create the legal preconditions for the conquest of Luxembourg.

The ‘Isenbüttel gold necklace’, now in the Lower Saxony State Museum in Hanover, was found almost a century ago in Lower Saxony, an area with no history of early medieval gold finds or richly furnished burials. As no parallels are known for the object, scholars have long debated the dating, provenance and function of this unique loop-in-loop chain, with its animal-head terminals and garnet cloisonné. Recent excavations of Anglo-Saxon cemeteries dating to the seventh century have, however, added new finds to the small corpus of objects known as ‘pin suites’, consisting of comparatively short pins perhaps designed to fix a veil or a light shawl in the collar area, with ornate pinheads, linked by chains. This paper focuses on Anglo-Saxon pin suites from high-status burials of the second half of the seventh century and seeks to set the finds group in its wider social and historical context, revealing the far-reaching relationships that existed between early medieval elites.

The state election in Lower Saxony on October 9, 2022, was the first election in Germany following the termination of Russian gas supplies to Western Europe . The election campaign was therefore dominated by the energy crisis and the associated conflict over the continued use of German nuclear power plants . Issues of Lower Saxony’s state politics, on the other hand, hardly played a role . The election was won by the SPD, which maintained its position as the strongest party in the Lower Saxony state parliament with slight losses . This was due not least to the high popularity of incumbent Minister President Stephan Weil, whom voters trusted to lead the state through the crisis . The CDU lost a massive number of votes and achieved its worst election result in Lower Saxony since 1955 . The Greens, on the other hand, made significant gains and achieved their best result in Lower Saxony since the party was founded . The AfD also improved significantly, while the FDP dropped out of the state parliament . After the two parties that had previously governed in a grand coalition, the SPD and CDU, had announced already before the election that they did not intend to continue their cooperation, a red-green state government was formed after the election .

Upper Saxon (Obersächsisch/ɵːpoˁˈsɛksʃ/) refers to a group of dialects spoken by over two million people in the Free State of Saxony in eastern Germany. It is considered one of the eastern branches of Central German (Wiesinger 1983, Lewis 2009), with major phonological, morphological, and lexical differences from Standard German and other regional dialects.

Abstract Orchard meadows are appreciated as an integrated land use of high cultural and biological value. While such meadows are typical habitats for temperate Europe, they experienced a decline in their total area during the second half of the 20th century, both in Western and Eastern Europe. In this contribution, we compare their current area and status in terms of semantics, law, public support in general, and the efficiency of public support in both Saxony and the Czech Republic. We estimated the area in Saxony on the basis of three public mapping projects. In the Czech Republic, where no recent mapping included orchard meadows as a specific land-use type, we carried out our own mapping. Hence, we mapped 124 randomly selected plots of 1 km2. To cross-reference results from both countries, we used the pan-EU project LUCAS (Land Use/Cover Area frame Survey). According to various different sources, the orchard meadows cover 0.09–0.55% of Saxony and 0.01–0.72% of the Czech Republic. Interestingly, the results of the three mapping projects conducted in Saxony vary from each other. Although orchard meadows are supported by financial incentives of the respective governments in both countries, the Saxon approach concentrating more on individual activities (sanitation of old trees, planting, grassland management), seems more focused than the single measure practised in the Czech Republic. One key to a greater public awareness of the orchard meadow problematic can lie in the promotion of a simple expression referring to this specific landscape feature in Czech, similar to the phrase common in the German language: ‘Streuobstwiese’. Our suggestion for the Czech language is: ‘luční sad’.

Abstract The regime change in the former German Democratic Republic and its reunification with the Federal Republic of Germany at the beginning of 1990s launched significant social and economic changes which resulted i.a. in high out-migration rate and secondary also rapid demographic ageing of the populations of the states of former Eastern Germany including Saxony. As a consequence, there is a lack of health professionals in Saxon hospitals which is going to be solved by the in-migration of medical staff from abroad. The geographical location of the Federal state of Saxony predetermines representatives of Saxon hospitals to look for missing health care labour in Czechia and latest statistics demonstrate that this could be a successful way to stabilize or even increase the personnel numbers of Saxon health care providers. The aim of this article is not only to bring some basic data about the migration of Czech health professionals to Germany, but especially to focus on processes which facilitate or hinder such kind of mobility, influence the rate of success of their integration both into the work team and German society and form the prospects of their permanent stay in Germany. Ten interviews with Czech health professionals were conducted in order to fulfill these ambitions. As a result, crucial barriers and recommendations for improvements concerning the migration decision making, their integration and sustaining in the migratory destination are presented.

A jurisdictional dispute over the burial of suicides in Electoral Saxony in the years 1702–1706 brought into sharp contrast conflicting views of the body in popular belief and Lutheran pastoral theology, and in the secularizing project of the early Enlightenment. The dispute centred on the practical, local implications of territorialism, a theory of church subordination to the state developed in the 1690s by the Saxon jurist Christian Thomasius (1655–1728), the most influential German political philosopher of the early Enlightenment. Considered in its intellectual and institutional contexts, the Saxon dispute illustrates the importance of the body to an understanding of secularization, the early Enlightenment and the history of suicide.

African swine fever (ASF) emerged in Latvia in 2014. In 2020, the virus has been detected in the German federal state, Saxony. In both regions, the virus was probably introduced by infected wild boar coming from affected neighboring countries. As the current ASF control strategy at EU level had not yet been developed at the time of ASF introduction into Latvia, disease control measures in both study areas differed over time. Assessing the course of ASF in Saxony and the implemented control strategies, the first 18 months of the ASF epidemic were epidemiologically compared between Saxony and Latvia. ASF wild boar surveillance data were analyzed and the prevalence of ASF virus-positive wild boar was estimated. For estimating the wild boar density, the numbers of wild boar per km² were calculated for the respective geographical areas. The number of samples collected from hunted wild boar and wild boar found dead was higher in Saxony. The ASF virus prevalence in Latvia was significantly higher than in Saxony, indicating that Saxony has had more time for getting prepared for dealing with an ASF incursion. Experience from other countries and the rapid implementation of new control strategies may have helped Saxony deal with ASF.

A number of studies have been published in the last few decades on Pleistocene palaeo-temperature reconstruction based on isotopic studies on deep sea cores and ice core records from Greenland. Such temporal high-resolution data represents northern hemispheric circulations and has to be reconfirmed through the study of terrestrial archives in order to recognise the character of such fluctuations in different regions. Loess-palaeosol sequences (LPSs) are suitable to interpret them as palaeoenvironmental archives, because loess is a widely distributed terrestrial deposit and is datable using luminescence techniques. The Saxon loess region (SLR) is characterised by a loess cover of ca. 8 m thickness, mainly representing deposits of the last glacial cycle. Over the past 35 years, Saxon loess remains under-researched wherefore a reactivation with the objective of contributing to the European loess research is important. There is a clear need to re-examine Saxon LPSs and close this gap of knowledge, because in recent years much work has been done on important and European-wide known loess sections as well as in adjacent loess areas. In this study, LPSs from Saxony were investigated and a regional palaeoenvironmental reconstruction of the last Glacial/Interglacial cycle was developed. The established stratigraphical scheme has to be advanced by results of optically stimulated luminescence (OSL) dating. The stratigraphical results should be compared with previous work from Saxony and with results from adjacent loess areas, to verify if our results have to be interpreted as singularities or if they are in accordance with known European conceptions. Therefore, 8 sections, mostly never investigated before, were described and correlated with each other to finally generate an independent standard stratigraphy for this area. Carbonate content, pH-value, soil organic matter, total and pedogenic iron, magnetic susceptibility and classical grain size analyses were obtained from every section. Furthermore, rare earth elements concentrations were measured from selected positions in order to prove if there are variations in the deposit composition during the glaciation. The OSL dating results were processed by Kreutzer (2012). As previously noted, the first step towards a regional palaeoenvironmental reconstruction was to establish a standard stratigraphic scheme where all found units are involved. Based on features regarding grain size distribution, the found palaeosols and the magnetic susceptibility Baumgart et al. (2013), 5 units could be defined. Unit V reflects the pre-Weichselian sediments modified by the Eemian soil formation. Unit IV contains deposits from the beginning of the Weichselian glaciation. Typically, this unit starts with the first Weichselian deposit, a bright-greyish Mn- and Fe-precipitates enriched layer which shows an aggregation of charcoal at its top. This layer is covered by a greyish, humus-enriched and reworked relict of a Chernozem-like soil. After a Gelic Gleysol and a reddish-brownish soil sediment, a loess package with an embedded interstadial Cambisol-like soil is preserved. The top of the unit is represented by another brownish soil sediment which forms the lower part of the Gleina complex. Typically, unit IV is characterised by stronger reworked layers and soil sediments but at the Rottewitz section an older loess package is preserved. Unit III represents the reactivation of aeolian sedimentation. The base of this unit is made up of a strong Gelic Gleysol (upper part of the Gleina complex). The deposits of this unit are mostly pedogenically overprinted and show features of at least two Gelic Gleysols. Unit II is dominated by unweathered loess. Its lower part (unit IIb) is built of a more stratified loess facies whereas the upper part (unit IIa) is built of a homogeneous loess facies. They are separated by a strong Gelic Gleysol. Unit I represent the upper part of the loess section, which is modified by the Holocene and Late Pleistocene soil development. Within this succession, a huge hiatus is found between unit III and IV of ca. 35 ka. It is labelled as the Gleina complex according to Lieberoth (1963). Furthermore, we demonstrate how combined analyses of high-resolution grain size distributions and microscopic analysis can be used to discriminate depositional and pedogenetic features of loess-palaeosol profiles from the SLR. Generally, it was observed that an increase of coarse material is linked with an increase of the mineralogical components which refers to slope processes. Rounded shapes of Mn- and Fe-precipitates, mostly found in Early Weichselian humus layers, indicate strong interstadial soil development modified by subsequent redeposition. Further observations suggest that the class of medium sand is dominated by secondary precipitates. The varying amount of very fine sand shows that sequences are cyclically built up of pure loess comparable to the Nussloch section. Studying coarse grain size fractions by microscopic analysis, a differentiation between loessic layers formed by periglacial slope processes and layers overprinted by pedogenetic processes is possible. Furthermore, an increase of fine material and secondary Mn- and Fe-precipitates can be attributed to soil forming processes (clay formation, redoximorphic processes, and illuviation). Additionally, a palaeoenvironmental reconstruction for the Late Pleistocene is proposed. As palaeo-temperature proxies ice wedges, pure loess sedimentation or the platy soil structure due to former ice lensing for cold periods and soil formations or vegetation remnants for warmer periods were used. A reconstruction of wind speed is directly deduced from the very fine sand content. The stability/instability of the landscape surface could be indicated by soil formation (stable) or through an increase of coarse sand (active). The type of soil development for the reconstruction is of major importance. For example, a humus enriched soil indicates warmer and dryer conditions than a Gelic Gleysol. The results of grain size analyses reveal a similar temporal and lithogenic pattern of Weichselian aeolian dynamics of the study area and other records from Europe. Furthermore, grain size results independently confirm the luminescence chronology of the studied sections. Reworked loess-like sediments show varying OSL age estimates; aeolian loess shows a systematic change of OSL ages. Generally, the findings of this study agree with observations from other loess areas. In most areas, a similar hiatus between Middle and Upper Weichselians is documented. Additionally, OSL dating suggests that we found an older loess package with an age between ca. 60 and 70 ka and a younger loess package with an age of ca. 15 and 30 ka. These periods of aeolian deposition are in accordance with MIS 4 and MIS 2 as well as with dust concentrations results derived from lake sediments and from ice cores. A major finding of this study is that we uncover the internal differences of loess-palaeosol sequences regarding their temporal resolution. In periods of loess sedimentation, a temporally high-resolution record is preserved. In contrast, in periods dominated by interstadial soil development or redeposition, a temporal low-resolution record is preserved and a reconstruction of palaeoenvironment is almost impossible
In den vergangenen Jahrzehnten wurden viele Studien über die Rekonstruktion der pleistozänen Temperaturentwicklung veröffentlicht, welche anhand von Isotopenanalysen aus Tiefsee- und Eisbohrkernen des grönländischen Eises abgeleitet werden konnten. In solchen zeitlich hochaufgelösten Daten sind nordhemisphärische Klimaschwankungen repräsentiert und diese sollten durch Untersuchungen terrestrischer Archive validiert und deren regionale Ausprägung in verschiedenen Räumen abgeschätzt werden. Löss-Paläobodensequenzen eignen sich hervorragend als Paläoumweltarchiv, da der Löss ein weit verbreitetes Sediment und mittels Lumineszenzverfahren datierbar ist. Die Sächsische Lössregion ist durch eine ca. 8 m mächtige Lössdecke charakterisiert, welche vornehmlich aus Ablagerungen des letzten glazialen Zyklus besteht. In den vergangenen 35 Jahren wurde die Lössforschung in diesem Raum vernachlässigt, sodass eine Wiederbelebung wichtig ist, um einen Beitrag zur europäischen Lössforschung zu leisten. Da in den letzten Jahren an wichtigen europäischen Lössprofilen, wie auch in angrenzenden Lössregionen, intensiv geforscht wurde besteht der dringende Bedarf, die Forschungen an sächsischen Löss-Paläobodensequenzen wieder aufzunehmen und die entstandene Wissenslücke zu schließen. In dieser Studie werden sächsische Löss-Paläobodensequenzen untersucht und eine regionale Umweltrekonstruktion für den letzten glazialen Zyklus vorgestellt. Die Standardstratigraphie wird dabei durch optisch stimulierte Lumineszenz (OSL)-Alter erweitert. Die Ergebnisse werden mit älteren Arbeiten aus diesem Raum verglichen, um abzuschätzen, ob es sich hierbei um Einzelbefunde handelt oder ob sich die Ergebnisse in schon bekannte europäische Konzepte einordnen lassen. Es werden 8, meist noch nie bearbeitete Profile beschrieben und miteinander korreliert, um schließlich eine unabhängige Standardstratigraphie für diesen Raum zu erarbeiten. Von jedem Profil wurde der Kalkgehalt, der pH-Wert, der Anteil der organischen Substanz, das pedogene und Gesamteisen, die magnetische Suszeptibilität und die Korngrößenverteilung (klassisch) bestimmt. Zudem wurde die Konzentration der Seltene Erden Elemente an ausgewählten Positionen bestimmt, um zu prüfen, ob es Verschiebungen in der mineralogischen Zusammensetzungen über das letzte Glazial hinweg gab. Die OSL-Datierungen wurden dabei von Kreutzer (2012) realisiert. Wie schon erläutert wurde, bestand der erste Arbeitsschritt darin, eine Standardstratigraphie zu erarbeiten, worin alle Befunde integriert werden können. Auf Grundlage der Korngrößenverteilung, der gefundenen Paläoböden und der magnetischen Suszeptibilität Baumgart et al. (2013) konnten 5 Einheiten ausgewiesen werden. Die Einheit V stellt die prä-weichselzeitlichen Sedimente dar, welche von der eemzeitlichen Bodenbildung überprägt wurden. Einheit IV beinhaltet die Sedimente vom Beginn der Weichselkaltzeit. Typischerweise befindet sich an der Basis dieser Einheit eine hellgraue, an Mn- und Fe-Konkretionen angereicherte Schicht, welche eine Häufung von Holzkohlebruchstücken im oberen Bereich zeigt. Diese Schicht ist wiederum von einem Rest einer schwarzerdeähnlichen Bodenbildung überlagert und zeigt eine Anreicherung an organischer Substanz. Über einem Nassboden und einem rotbraunen Bodensediment ist ein Lösspaket, mit einem zwischengelagerten interstadialen braunerdeartigen Boden, erhalten. Der obere Bereich der Einheit IV ist durch ein weiteres rötlichbraunes Bodensediment geprägt, welches dem unteren Teil des Gleinaer Komplexes entspricht. Normalerweise ist die Einheit IV in Sachsen durch stark umgelagerte Schichten charakterisiert, jedoch ist im Profil Rottewitz in dieser Einheit ein älteres Lösspaket erhalten. Die Einheit III repräsentiert eine Reaktivierung der äolischen Sedimentation. Ihre Basis bildet ein kräftiger Nassboden (oberer Teil des Gleinaer Komplex). Die Sedimente dieser Einheit sind meist pedogen überprägt und es können mindestens zwei separate Nassböden ausgewiesen werden. Die Einheit II besteht vornehmlich aus unverwittertem kalkhaltigen Löss. Ihr unterer Abschnitt (Einheit IIb) wird durch eine streifige Löss-Fazies gebildet, wohingegen der obere Teil von einer homogenen Löss-Fazies dominiert wird. Diese sind durch einen kräftigen Nassboden voneinander getrennt. Die Einheit I bildet den oberen Teil des Lössprofiles und ist durch die pedogene Überprägung der spätpleistozänen und holozänen Bodenentwicklung geprägt. In dieser Abfolge ist ein Alterssprung von ca. 35 ka zwischen der Einheit IV und III nachgewiesen. Dieser Hiatus befindet sich im durch Lieberoth (1963) definierten Gleinaer Komplex. Weiterhin konnte gezeigt werden, dass mit Hilfe einer kombinierten Untersuchung aus Korngrößenanalyse und Mikroskopieren es möglich ist, eine durch Bodenbildung bedingte und eine durch Umlagerung hervorgerufenen Überformung von Lösssedimenten voneinander zu unterscheiden. Generell wurde festgestellt, dass ein Anstieg der groben Kornfraktionen oft mit einer Erhöhung der mineralischen Komponente einhergeht und dies auf laterale Umlagerungsprozesse hindeutet. Abgerundete Mn- und Fe-Konkretionen aus humosen frühweichselzeitlichen Schichten lassen eine kräftige interstadiale Bodenentwicklung mit anschließender Umlagerung vermuten. Es wurde zudem festgestellt, dass die Mittelsandfraktion durch sekundäre Fe- und Mn-Konkretionen dominiert wird. Der variierende Feinstsandanteil zeigt, dass die Sequenzen in verschiedenen Zyklen aus unverwittertem Löss aufgebaut wurden, wie es auch aus dem Profil Nussloch beschrieben wird. Bodenbildungsprozesse bedingen demgegenüber ein Anstieg der Feinkomponenten und der Mn- und Fe-Konkretionen in den Sandfraktionen. Weiterhin wird eine Paläoumweltrekonstruktion für das Spätpleistozän vorgeschlagen. Hierbei werden verschiedenste Indikatoren als Paläotemperaturzeiger herangezogen. Für kalte Phasen stehen zum Beispiel Eiskeilpseudomorphosen, Pakete aus unverwittertem Löss oder plattige Strukturen infolge von Schichteisbildung. Für wärmere Phasen sprechen Paläoböden oder Pflanzenreste. Eine Rekonstruktion der Paläowindgeschwindigkeiten wird direkt über die Feinstsandanteile abgeleitet. Die Stabilität einer Landschaftoberfläche wird durch Bodenbildungen (stabil) oder einem Anstieg der groben Sandkomponenten (aktiv) repräsentiert. Den Paläoböden kommt bei einer solchen Rekonstruktion eine Schlüsselstellung zugute. Zum Beispiel signalisiert ein Steppenboden wärmere und trockenere Bedingungen im Vergleich mit einem Nassboden. Die Ergebnisse der Korngrößenuntersuchungen zeigen, dass hinsichtlich ihres Aufbaues und ihrer chronologischen Einordnung die äolisch dominierten Phasen der sächsischen Lössprofile bekannten Mustern aus anderen Archiven in Europa folgen. Zudem zeigt sich, dass die Ergebnisse der Korngrößenverteilung die mittels OSL bestimmten Alter untermauern. Umgelagerte Sedimente zeigen größere Altersschwankungen, wohingegen äolische Sedimente eine kontinuierliche Altersentwicklung haben. Die Ergebnisse dieser Untersuchungen stimmen mit Beobachtungen aus anderen Lössgebieten überein. In den meisten Regionen wird ein ähnlicher Hiatus zwischen der mittleren und oberen Weichselkaltzeit beschrieben. Zudem deuten die OSL-Ergebnisse an, dass in Sachsen ein älteres Lösspaket mit einem Alter von ca. 60 bis 70 ka und ein jüngeres Lösspaket mit einem Alter von ca. 15 bis 30 ka existiert. Die beiden äolischen Phasen korrelieren mit der marinen Isotopenstufe 4 (MIS) beziehungsweise der MIS 2, sowie mit Ergebnissen pleistozäner Staubkonzentration der Atmosphäre, abgeleitet aus Seesedimenten oder Eisbohrkernen. Eine wichtige Erkenntnis dieser Untersuchungen ist, dass wir innerhalb eines Lössprofiles Pakete unterschiedlicher zeitlicher Auflösung identifizieren konnten. Aus Phasen kräftiger Lösssedimentation sind zeitlich hoch aufgelöste Sequenzen erhalten. Demgegenüber ist aus Phasen, dominiert durch Bodenbildungen oder Umlagerungen, ein zeitlich nur sehr schlecht aufgelöstes Archiv erhalten, weshalb anhand dieser Abschnitte eine Paläoumweltrekonstruktion nur bedingt möglich ist

Open Access steht für den freien Zugang zu wissenschaftlichen Publikationen über das Internet. Die Open-Access-Tage, kurz OA-Tage, sind die zentrale jährliche Konferenz zu diesem Thema im deutschsprachigen Raum. In diesem Jahr findet die Tagung erstmals in Dresden statt.

Die sächsischen Hochschulbibliotheken verfügten bisher nur über eigene, auf die jeweilige Einrichtung beschränkte Hochschulschriftenserver. Qucosa, das der kostenlosen Publikation und dauerhaften Archivierung von elektronischen Diplomarbeiten, Dissertationen und anderen Veröffentlichungen dient, eröffnet den sächsischen Hochschulbibliotheken neue Perspektiven und bildet eines der Elemente einer „Digitalen Bibliothek“ in Sachsen. Bereits mehrere sächsische Hochschulen und Forschungsinstitute benutzen Qucosa zur Publizierung der eigenen Forschungsergebnisse. Auch nichtwissenschaftliche, staatliche Einrichtungen werden zukünftig ihre Schriften auf Qucosa im Volltext anbieten.

Massive Open Online Courses, sogenannte MOOCs sind offene und über das Internet für jeden kostenfrei zugängliche Kurse, die hierdurch oft eine Vielzahl an Teilnehmenden erreichen. Alle Beteiligten lernen gemeinsam, jedoch mit verschiedensten persönlichen Zielen. Die Inhalte werden nicht ausschließlich von den Veranstalter/inne/n vorgegeben, sondern können zudem auch von den Teilnehmenden erweitert und geteilt werden. Mit dem SOOC13, dem Saxon Open Online Course, wurde einer der aktuellsten und vieldiskutierten Trends [1] im E-Learning im Sommersemester 2013 von den Technischen Universitäten in Chemnitz und Dresden sowie der Universität Siegen aufgegriffen, praktisch erprobt und evaluiert. Der Kreis der Teilnehmenden bestand dabei nicht nur aus Studierenden, vielmehr waren mit dem Kurs explizit auch Lehrende sowie andere Hochschulmitarbeiter/innen angesprochen. Als konnektivistischer Open Online Course war der SOOC13 zudem offen für alle Interessierten innerhalb der Netz-Community. Als Methode der Leistungserbringung und -bewertung kamen E-Portfolios zum Einsatz, welche formative Feedback- und Beurteilungsprozesse zulassen. Lernende erstellen Lernprodukte (Artefakte), reflektieren über Lernziele, -verhalten und -fortschritte und teilen die Ergebnisse mit anderen Teilnehmenden in Form von Blogeinträgen, Tweets oder Facebook-Posts. Gegenseitiges Feedback und Hinweise durch die Veranstalter/innen führen zu ausgiebigen Diskussionen und kritischen Auseinandersetzungen.

The curriculum has set new courses, and sparked discussions about educational issues and teaching attitudes. Many parents have made positive comments about it. You too are of course welcome to have a look at the curriculum. The most important factor here is that you maintain good contact with the facility or childminder. Exercise your legal right to help the day-care centres and childminding facilities complete their tasks. The full version of the curriculum is available at www.kita-bildungsserver.de. Redaktionsschluss: 21.12.2017

Der Verein „Silicon Saxony e.V.“ und seine Mitglieder verfolgen die Vision, durch gezielte Bündelung von Erfahrungen und Know-how zur Unterstützung von Unternehmen und Forschungseinrichtungen der Halbleiterbranche und deren Zulieferer die Region Sachsen zu einem weltweit anerkannten Mikroelektronikstandort zu entwickeln.

Der Verein „Silicon Saxony e.V.“ und seine Mitglieder verfolgen die Vision, durch gezielte Bündelung von Erfahrungen und Know-how zur Unterstützung von Unternehmen und Forschungseinrichtungen der Halbleiterbranche und deren Zulieferer die Region Sachsen zu einem weltweit anerkannten Mikroelektronikstandort zu entwickeln.

In August 2002 a heavy rainfall event lasting more than two days occurred in Saxony/Germany. This led to extreme flash floods and extreme high water levels in some left tributaries of the river Elbe in the Ore mountains (Erzgebirge). Much damage occurred: houses and bridges were destroyed, much sediment moved and a dam broke. About 20 people died. Immediately after the event a mapping exercise of all damages arising from the flood was compiled. The hydrologic and hydraulic processes during the flood were analysed. This analysis included the genesis of the flood, the flood routing, the erosion, plain bed load transport and the sedimentation. The analysis of such an extraordinary event can help us learn how to prevent flood damages in the future.

<p>Since the 1830s, the railway network has grown rapidly, connecting all regions of the German country. In order to overcome topographical obstacles such as valleys, rivers etc., many railway bridges were built in different construction periods. The individual structures are understood as elements of the dynamic development of the complex "railway" network. Railway bridges are constantly changing structures, as their functionality and preservation value must be secured through maintenance, repair and replacement due to increased requirements. During the beginning of railway expansion, especially in Saxony, a dense network was developed. The topography of a low mountain region led to a high number of arch bridges. This type of construction still makes up a high proportion of the existing bridges in Saxony today. The history of selected railway arch bridges from representative parts of the railway network in Saxony is shown and analysed.</p>

The article presents the interdisciplinary and general education courses in Studium fundamentale. In doing so, a way of the university for more interdisciplinary teaching offers for listeners of all faculties is described. It describes a way of integrating intercultural education into bachelor's programs (engineering, social sciences, natural sciences and economics). A number of sources provide further information on the state of general education at universities and colleges in Saxony.

Halle-Neustadt, built as a new city for the workers of the chemical industry, was recently celebrating its 50 years of existence. The former pride of socialism is now facing dramatic shrinkage, with the population drop of 46%. The paper presents the history of the city – its growth and fall. It discusses the demolitions which took place in the city and the simultaneous 2002-2010 IBA Saxony-Anhalt revitalisation programme, including the post-evaluation facts. The Kompetenzzentrum Stadtumbau workshop conducted in 2014 by HTW Dresden, TU Delft, CUT Krakow, Gent University and UT Chalmers – a project carried out under the auspices of the City of Halle and the Land of Saxony-Anhalt offers a new perspective onto the problem. The final results and strategies developed within the framework of the project raise the question of relations between an urban form and the community. The problem manifests itself by uneven distribution of population between the modern Neustadt and the traditional Altstadt – the latter still featuring the authentic historic block structure. Serving for over millennium as the centre of Halle – Altstadt, saved from the ravages of wars, now renovated and vibrant with life, exemplifies the return of people to their identity - to the traditional sense of the city.

Abstract Summary In the high risk Managed Pressure Drilling operations, increased certainty given by Mud Logging is a critical deliverable to guarantee a safe drilling environment even under challenging conditions and, to provide the first indications for reservoir evaluation. This paper describes a novel product application that successfully obtains advanced mud gas data from a Managed Pressure Drilling environment, proven in flow-loop and field applications (in Lower Saxony, Germany), by reducing service footprint as well as power consumption.

Reaching the goals of the Kunming-Montreal Global Biodiversity Framework requires commitment at all political levels and in all sectors. The State of Saxony also has to contribute its share. Saxony has a great potential, but also faces particular challenges. Almost half of the land area is used for agriculture, mainly for arable farming. However, only around eight percent of the land is farmed ecologically4. Intensification and monotonization of agriculture, as well as the use of pesticides and fertilizers, significantly contribute to the loss of biodiversity. Agriculture plays a crucial role as a habitat for biodiversity5. It is indispensable to promote biodiversity-friendly use, increase the proportion of land under organic farming, and establish corresponding methods in conventional agriculture. As a producer of fossil fuels, especially by the Lusatian and Central German lignite mining regions, Saxony is also strongly affected by the energy transition. The expansion of renewable energies needs to be nature-compatible and in harmony with the protection of biodiversity. Approaches to multifunctional landuse may provide support in this regard. Prof. Dr. Edeltraud Günther, Director of UNU-FLORES, emphasizes the need to consider biodiversity in the resource nexus. Saxony has good prerequisites to meet these challenges. With its Saxony Biodiversity 2030 Program, it has a revised biodiversity strategy to meet the global targets. In addition, Saxony is home to major research institutions that intensively focus on biodiversity. Research, education, and science communication play a central role in this context. Prof. Tshilidzi Marwala, Rector of UNU and Under-Secretary- General of the UN, emphasized the key role of education in his opening address of the DNCi 2023: 'Education is the key to unlock our potential. It empowers us to become stewards of our environment by providing us with a deep appreciation for biodiversity and inspiring sustainable practices in every aspect of our lives. By integrating transformative education at the international, national, and local levels, we can create profound change in attitudes, knowledge, and behaviors.' The DNCi 2023 participants had a hands-on experience of the importance of education and science communication on biodiversity thanks to a guided tour of the Botanical Garden. Many thanks to Prof. Dr. Christoph Neinhuis, Director of the Botanical Garden, and Dr. Barbara Dietsch, Scientific Director of the Botanical Garden, for these valuable insights. As part of the DNCi 2023, co-organized by UNU-FLORES, the IOER, and TU Dresden, we succeeded in bringing together different stakeholders from science, government, civil society, and the private sector to create a dynamic platform for exchange and collaboration on the topic of biodiversity. We would like to express our sincere gratitude to all participants for their commitment during the event and beyond, and to the Saxon State Ministry of Energy, Climate Protection, Environment and Agriculture for supporting the event within the framework of its cooperation with UNU-FLORES.

La gestion des risques industriels soulève de nombreuses questions auxquelles on ne peut pas répondre par un simple «oui» ou «non»: (1) quels critères la société devrait-elle utiliser pour décider que les risques d'une installation industrielle ont été réduits aussi bas que raisonnablement praticable? (2) comment arbitrer entre des considérations qui relèvent de «dimensions» différentes: morts et blessés potentiels en cas d'accident industriel, impacts potentiels sur l'environnement, enjeux financiers, développement de l'emploi, déménagements forcés en cas d'expropriation d'habitations, etc. et ayant des impacts sur de multiples parties prenantes (riverains des installations industrielles, exploitants et employés des sites, élus locaux et régionaux, etc.)? L'analyse coût-bénéfices (ACB) est un outil d'aide à la décision qui peut faciliter la discussion entre parties prenantes. Elle fournit un cadre structuré permettant de présenter l'ensemble des éléments de la décision et discuter de leur pondération respective, favorisant ainsi la transparence du processus décisionnel. Cet outil est largement utilisé dans les pays anglo-saxons en matière de réglementation environnementale et de décisions concernant la sécurité industrielle. Le présent document vise à aider des analystes qui souhaiteraient conduire une ACB d'un projet d'investissement en matière de sécurité ou une analyse d'impact d'une réglementation liée à la prévention. Il vise également à éclairer les lecteurs de telles études et les aider à évaluer la qualité de l'analyse. Le document présente les concepts économiques qui sous-tendent l'ACB, et décrit les principales étapes pratiques d'une étude. Il fournit des indications sur les sources de données permettant de monétiser différentes conséquences hors-marché de l'activité industrielle (impact sur la santé et la sécurité des personnes, pollutions environnementales et nuisances sonores). Le document propose également une check-list des questions qu'il peut être utile de se poser lors de la lecture critique d'une étude ACB.

This report is adapted from the forthcoming Climate Instruments for the Transport Sector (CITS) report written by Cornie Huizenga, convener of the Partnership for Sustainable Low Carbon Transport (SLoCaT), and Stefan Bakker, from the Energy Research Center of the Netherlands. Under the CITS project, studies were carried out in two Asian and two Latin American cities to explore how NAMAs, a new financial mechanism being developed under the UNFCCC, may support emissions reductions from urban transport policies and programs. The authors received valuable input from: Dario Hidalgo, from EMBARQ/World Resources Institute, for the Belo Horizonte case study; Frederic Rudolph, Urda Eichhorst and Wolfgang Sterk, from Wuppertal Institute, for the Hefei case study; Holger Dalkmann and Ko Sakamoto, from Transport Research Laboratory, for the Jakarta case study; and Martina Jung and Christian Ellermann, from ECOFYS, for the Mexico case study. This report was edited by Peter Shifter. The CITS project was guided by Rafael Acevedo-Daunas, Maria Cordeiro, Vera Lucia Vicentini, Maria Netto and Francisco Arango at the Inter-American Development Bank (IDB), and by Jamie Leather and Sharad Saxena at the Asian Development Bank (ADB). The two case studies in Asian cities were financed by the ADB, and the two Latin American studies by the IDB. The combined report was financed by the ADB and the publication financed by the IDB as part of a combined effort within an MOU signed by both institutions and their participation in the SLoCaT partnership.