Visuell-mediale Landschaftskonstruktionen als Bild-Raum-Diskurse

Durch die massenmediale Zunahme von statischen und bewegten Bilder im Laufe des letzten Jahrhunderts vollzieht sich unsere lebensweltliche Wirklichkeitskonstruktion zu Beginn des 21. Jahrhunderts zunehmend über Visualisierungen, die mit den neuen Formen der Digitalisierung noch an Dynamik zunehmen werden. Mit diesen omnipräsenten visuell-medialen Repräsentationen werden meist räumliche Vorstellungen transportiert, denn Räume werden vor allem über Bilder konstruiert. Diese Bildräume zirkulieren dabei nicht als singuläre Bedeutungszuschreibungen, sondern sind in sprachliche und bildliche Diskurse eingebettet. Visuell-mediale Bild-Raum-Diskurse besitzen zunehmend die Fähigkeit, unser Wissen über und unsere Wahrnehmung von Räumen zu kanalisieren und auf stereotype Raumstrukturen zu reduzieren. Dabei verfestigt sich eine normative Ordnung von bestimmten machtvollen Bildräumen, die nicht genügend kritisch hinterfragt werden. Deshalb ist es für die Geographie von entscheidender Wichtigkeit, mediale Raumkonstruktio- nen, ihre Einbettung in diskursive Bildarchive und ihre essentialistische und handlungspraktische gesellschaftliche Wirkung zu verstehen.rnLandschaften können vor diesem Hintergrund als visuell-medial transportierte Bild-Raum-Diskurse konzeptionalisiert werden, deren gesellschaftliche Wirkmächtigkeit mit Hilfe einer visuell ausgerichteten Diskursanalyse hinterfragt werden sollte. Auf Grundlage einer zeichentheoretischen Ikonologie wurde eine Methodik entwickelt, die visuell ausgerichtete Schrift-Bild-Räume angemessen analysieren kann. Am Beispiel der Inszenierung des Mittelrheintals, wurde, neben einer diachronischen Strukturanalyse der diskursrelevanten Medien (Belletristik, Malerei, Postkarten, Druckgrafiken und Fotografien), eine Feinanalyse der fotografischen „Rheinlandschaften“ von August Sander der 1930er Jahre durchgeführt. Als Ergebnis zeigte sich, dass der Landschaftsdiskurs über das Mittelrheintal immer noch durch die gegenseitige Durchdringung der romantischen Literatur und Malerei in der ersten Hälfte des 19. Jahrhunderts und die historischen Fotografien in den ersten Jahrzehnten des 20. Jahrhunderts bestimmt ist, nicht zuletzt forciert durch die Ernennung zum UNESCO-Welterbe 2002. Der stark visuell ausgerichtete Landschaftsdiskurs trägt somit zum einen positiv konnotierte, romantisch-pittoreske Züge, die die Einheit von Mensch und Natur symbolisieren, zum anderen historisch-konservatorische Züge, die eine Mythifizierung zu einer gewachsenen, authentischen Kulturlandschaft evozieren.

Synthesis and characterization of polyelectrolyte brushes

On the pathway to synthesizing synthetic model systems for human cartilage, macroinitiators for the ATRP of styrene sulfonate esters with different chain lengths and initiation site densities from 10 % to 100 % were synthesized. Polymer brushes from styrene sulfonate ethyl ester and styrene sulfonate dodecyl ester with varying grafting density, backbone length and side chain length were synthesized and characterized by 1H-NMR, AUC, AFM, TEM, and in the case of the ethyl esters, GPC-MALLS. Polyelectrolyte brushes from styrene sulfonate were synthesized from the corresponding esters. These brushes were characterized in solution (GPC-MALLS, static and dynamic light scattering, SANS, 1H-NMR) and on solid interfaces (AFM and TEM). It was shown that these brushes may form extended aggregates in solution. The aggregation behavior and the size and shape of the aggregates depend on the side chain length and the degree of saponification. For samples with identical backbone and side chain length, but varying degrees of ester hydrolysis, marked differences in the aggregation behavior were observed. A functionalized ATRP macroinitiator with a positively charged head group was synthesized and employed for the synthesis of a functionalized polyelectrolyte brush. These brushes were found to form complexes with negatively charged latex particles and are thus suitable as proteoglycan models in the proteoglycan-hyaluronic acid complex.

Flash floods and their effects on the development in El-Qaá plain area in South Sinai, Egypt

The arid regions are dominated to a much larger degree than humid regions by major catastrophic events. Although most of Egypt lies within the great hot desert belt; it experiences especially in the north some torrential rainfall, which causes flash floods all over Sinai Peninsula. Flash floods in hot deserts are characterized by high velocity and low duration with a sharp discharge peak. Large sediment loads may be carried by floods threatening fields and settlements in the wadis and even people who are living there. The extreme spottiness of rare heavy rainfall, well known to desert people everywhere, precludes any efficient forecasting. Thus, although the limitation of data still reflects pre-satellite methods, chances of developing a warning system for floods in the desert seem remote. The relatively short flood-to-peak interval, a characteristic of desert floods, presents an additional impediment to the efficient use of warning systems. The present thesis contains introduction and five chapters, chapter one points out the physical settings of the study area. There are the geological settings such as outcrop lithology of the study area and the deposits. The alluvial deposits of Wadi Moreikh had been analyzed using OSL dating to know deposits and palaeoclimatic conditions. The chapter points out as well the stratigraphy and the structure geology containing main faults and folds. In addition, it manifests the pesent climate conditions such as temperature, humidity, wind and evaporation. Besides, it presents type of soils and natural vegetation cover of the study area using unsupervised classification for ETM+ images. Chapter two points out the morphometric analysis of the main basins and their drainage network in the study area. It is divided into three parts: The first part manifests the morphometric analysis of the drainage networks which had been extracted from two main sources, topographic maps and DEM images. Basins and drainage networks are considered as major influencing factors on the flash floods; Most of elements were studied which affect the network such as stream order, bifurcation ratio, stream lengths, stream frequency, drainage density, and drainage patterns. The second part of this chapter shows the morphometric analysis of basins such as area, dimensions, shape and surface. Whereas, the third part points the morphometric analysis of alluvial fans which form most of El-Qaá plain. Chapter three manifests the surface runoff through rainfall and losses analysis. The main subject in this chapter is rainfall which has been studied in detail; it is the main reason for runoff. Therefore, all rainfall characteristics are regarded here such as rainfall types, distribution, rainfall intensity, duration, frequency, and the relationship between rainfall and runoff. While the second part of this chapter concerns with water losses estimation by evaporation and infiltration which are together the main losses with direct effect on the high of runoff. Finally, chapter three points out the factors influencing desert runoff and runoff generation mechanism. Chapter four is concerned with assessment of flood hazard, it is important to estimate runoff and tocreate a map of affected areas. Therefore, the chapter consists of four main parts; first part manifests the runoff estimation, the different methods to estimate runoff and its variables such as runoff coefficient lag time, time of concentration, runoff volume, and frequency analysis of flash flood. While the second part points out the extreme event analysis. The third part shows the map of affected areas for every basin and the flash floods degrees. In this point, it has been depending on the DEM to extract the drainage networks and to determine the main streams which are normally more dangerous than others. Finally, part four presets the risk zone map of total study area which is of high inerest for planning activities. Chapter five as the last chapter concerns with flash flood Hazard mitigation. It consists of three main parts. First flood prediction and the method which can be used to predict and forecast the flood. The second part aims to determine the best methods which can be helpful to mitigate flood hazard in the arid zone and especially the study area. Whereas, the third part points out the development perspective for the study area indicating the suitable places in El-Qaá plain for using in economic activities.