Elementos visuales determinantes del Paisaje Litoral. El potencial presente y endógeno en la Confluencia del Tajo con el Atlántico

El objeto de esta tesis es analizar la calidad del paisaje litoral como realidad espacial captada e interpretada por el hombre, a partir de la elección de elementos descriptibles y valorables, que ayudan a encuadrar y relacionar los principales aspectos, componentes, variables y parámetros asociados a la apreciación visual del territorio costero. Resumo Este trabalho tem como objecto de estudo a análise da qualidade da paisagem litoral, enquanto realidade espacial percepcionada e interpretada pelo homem a partir de elementos descritíveis e valoráveis, enquadrando, relacionando e caracterizando os principais aspectos, componentes, variáveis e parâmetros relacionados com a apreciação visual do território costeiro. Résumé Cette thèse a pour objet l'analyse du paysage littoral en tant que réalité spatiale perçue et traduite à partir d'éléments qui peuvent être décrits et mesurés pour servir ensuite à interpréter, caractériser et mettre en relation les principaux aspects, composants, variables et paramètres liés à l'interprétation visuelle du territoire côtier. Abstract The object of this project is to analyse the littoral landscape as a spatial reality perceived and interpreted by mankind, with reference to those elements that can be described and measured, thereby categorizing, connecting and characterizing the principal aspects, components, variables and parameters which relate to the visual interpretation of the coastal territory. Riassunto Questo lavoro ha come obbiettivo di studio l'analisi della qualità del paesaggio litoraneo, inteso come realtà particolare percepita ed interpretata dall'uomo a partire da elementi descrittivi e di valutazione, inquadrando, mettendo in relazione e distinguendo i principali aspetti, componenti, variabili e parametri relativi all'interpretazione visiva del territorio costiero. Zusammenfassung Ziel dieses Projekts ist es, die Eigenschaften der Küstenlandschaft, wie sie vom Menschen als räumliche Wirklichkeit wahrgenommen und gedeutet wird, unter Verwendung der beschreibbaren und messbaren Elemente zu analysieren, und die Hauptaspekte, Bestandteile, Variablen und Parameter der visuellen Interpretation des Küstengebiets einzubeziehen und zu charakterisieren. Samenvatting Het doel van dit project is het analyseren van de kwaliteit van het kustlandschap, zoals dit landschap door mensen als realiteit waargenomen en geïnterpreteerd, geinterpreteerd wordt, daarbij gebruik makende van beschrijfbare en meetbare elementen en tegelijkertijd daarbij in te passen, te verbinden en te karakteriseren de hoofdaspecten, componenten, variabelen en parameters die betrekking hebben op op visuele interpretatie van het kustlandschap.

Age determination of sediment core M1_251, Persian Gulf (Table 1)

Sediments from a 3.40 m core out of the Persian Gulf were investigated for their content of straight chain paraffins and fatty acids. The samples range in age between 2000 and 9000 years (C-14-age of organic C). They contain 100-300 ppm of extractable fatcompounds and 20-70 ppm of hydrocarbons. There is no connection between the original distribution of the homologous series of n-fatty acids and n-paraffins. However, there is evidence that part of the n-fatty acids was reduced to n-paraffins, although the sediment itself does not look as if it were deposited under reducing conditions.

Quantitative composition and distribution of the silt fraction in surface sediments of the North-West African continental margin

Surface sediments from the continental slope and rise of North-West Africa between the Canary lslands and the Cape Verde Islands are mainly composed of silt-sized material (2-63 µm). A number of sampling profiles were run normal to the coast and the composition of the silt fraction was determined quantitatively by scanning electron microscope analysis. The carbonate portion of the sediment was found to be nearly exclusively of biogenic origin. The most important contributors are planktonic foraminifers and coccoliths with minor contributions derived from pteropods. Plankton-produced biogenic opal such as diatoms and radiolarians play a very minor role. The high production rates of opal-silica plankton which exists in the surface waters of the NW-African upwelling system does not give rise to corresponding increases of opal accumulation in the bottom sediment. Benthic producers consist mainly of foraminifers and molluscs but the entire input from benthic producers is extremely small. An exception to this occurs in the prodelta sediments of the Senegal river. Downslope particle transport is indicated by the occurrence of shallow-water coralline algae, ascidian sclerites and cliona boring chips and can be traced as far down as the continental rise. The non-carbonate silt fraction mostly consists of quartz which is derived as eolian dust from the Sahara desert by the Harmattan and the NE-Trade-wind system. The percentage of carbonate in the surface sediments directly indicates the relative proportions of autochthonous biogenic components and terrigenous allochthonous quartz particles.

Tab. 1: Längenänderungen der Gletscherenden 1980/81

Im österreichischen Alpenanteil gibt es 925 Gletscher, die zusammen eine Fläche von 542 km**2 bedecken. Die Längenmessungen werden derzeit an 118 Gletschern mit einer Gesamtfläche von 310 km**2 durchgeführt, das sind 13 % der Anzahl und 57 % der Fläche aller österreichischen Gletscher. Diese ungleiche Verteilung kommt daher, weil das Beobachtungsnetz alle großen Talgletscher (>5 km**2) enthält, während die kleinen Kargletscher zu gering vertreten sind. Von den insgesamt 110 österreichischen Gletschern, die größer als 1 km**2 sind, werden die Längenänderungen an 75 Gletscherenden (=68 %) gemessen; von den 815 Gletschern, die weniger als 1 km**2 Fläche bedecken, liegen nur 44 (=5,4 %) im Beobachtungsnetz. Diese Tatsache muß bei der Interpretation von Ergebnissen der Längenmessungen und ihrer Wertung im Auge behalten werden. Im Berichtsjahr wurden von den ehrenamtlichen Mitarbeitern des Meßdienstes 16 Gebietsberichte mit 167 Seiten und 230 Fotos abgegeben, die im Gletschermeßarchiv des Österreichischen Alpenvereines aufbewahrt werden. Aus diesen Berichten wurde der vorliegende Sammelbericht zusammengestellt.

Sedimentology of surface sediments from the continental shelf and slope off West Africa (Table 1)

Samples from sutface sediments of the shell, continental slope, and adjacent deep sea regions off West Africa between 27° N and 15° N were investigated with respect to grain size distribution of the total samples, sand contents of the acid insoluble residues, carbonate content of the total samples, and the separate grain size fractions, specific surfaces, colours and mineralogical composition of the clay fractions. The grain size distributions of the total samples of the sediments of the shelf and the continental slope off Spanish-Sahara are controlled mainly by biogenic components. The supply of terrigeneous material in this area is very low. At deeper parts of the continental slope and in the deep sea areas, the relative amounts of carbonate minerals in the sediments are considerably reduced. The prevailing sand contents of the upper slope changes into clay dominance. On the shelf of Mauritania - represented by profiles extending down to 200 m water depth - the grain size is also controlled mainly by biogenic carbonates. Nevertheless, the admixture of fossil silicate components is important, too. The southern parts of the area is investigated are located in a region influenced by sediments of the Senegal River, which especially control the contents of silt and clay. The silicate sands, predominately of quartz, are fossil and form a mixed sediment with younger deposits. The carbonate contents of the different grain size fractions are formed either by sedimentation of carbonate and silicate particles of the respective grain size or by autochtonous disintegration of coarser sediment particles, as shown by the occurence of Mg-rich calcite and especially aragonite in the clay sized fraction. In the northern parts of the area investigated, which have very minute terrigeneous supply, the latter mechanism is the dominant factor, controlling the carbonate contents of the fine grain sized fractions. In the vicinity of the mouth of the Senegal the carbonate contents are influenced by extremely high dilution with terrigencous silicates. Mg-rich calcite and aragonite are produced preferentially in shallow slope and shelf areas up to 500 m of water depth. The specific surfaces of the carbonate-free clay fractions indicate that the clay fractions of the shelfareas with little terrigenous supply consits of relatively coarser particles. Very fine particles are removed and transported towards the deep sea. Lateral differentiation of this kind was not observed in the area off Senegal. The high surface areas, characterizing the clay fractions of this region, are thought to be due to high montmorillonite contents as was found for deep seas sediments. The mineralogical composition of the clay fraction from the southern parts of the area is characterized by high kaolinite and montmorillonite contents, while in the northern illite is predominating. At least two types of montmorillionites are present: in areas influenced by the Senegal mostly one type was found, which could swell to 17; on the shelves and slopes of the other regions the montmorillonite-group is represented by a montmorillonite-mica-type mixed-layer mineral. A "glauconite", found in the sand fraction, which had very similar properties to those of the montmorillonite-mica mixed-layer, is believed to be the source of this mixed-layer-type mineral. Palygorskite is present in all samples out of range of the Senegal supply. It may be an indicator of eolian transported material. The occurence of rich palygorskit deposits in the arid hinterlands emphasizes the terrestrial origin.

German Bight bedform reconstructions

Bodenformen an der Sohle von Flüssen, Küstenzonen und flachen Schelfen sind wichtige skalenübergreifende Elemente der Küstendynamik in ihren Eigenschaften als Transportkörper von Sedimenten und ihrer Wirkung auf die Strömungsdynamik als Rauheitselemente. Neben vielen neueren Studien über die Entstehung, Gestalt und Dynamik von Bodenformen in vergleichsweise kleinen Untersuchungsgebieten ist die Arbeit von ULRICH (1973) über die Verteilung von Bodenformen in der Deutschen Bucht bis heute die einzige verfügbare zusammenhängende Darstellung für die deutsche Nordseeküste. Die analogen Karten und die Darstellung der Klassifizierung in Buchstabenkürzeln macht sie für heutige quantitative Analysen schwer zugänglich. Hier wurden diese Karten digitalisiert und Eigenschaften der Bodenformen rekonstruiert und interpretiert. Das Ergebnis ist eine Zusammenstellung digitaler Karten eines vollständigen - und eines auf steile, hydrodynamisch wirksame Bodenformen reduzierten Datensatzes der Minimal, Maximalund Mittelwerte von Höhen, Längen und Steilheiten von Bodenformen in der Deutschen Bucht. Die Datensätze stehen der Allgemeinheit in der Datenbank Pangaea zur Verfügung. Bedforms in rivers, coastal zones and shallow shelf seas are important cross-scale elements of coastal dynamics in their function as sediment transport agent and in their effect on the flow dynamics as roughness elements. In addition to many recent studies on the origin, shape and dynamics of bedforms in relatively small study areas the work of ULRICH (1973) on the classification of bedform types in the German Bight is until today the only available coherent representation of the spatial distribution of bedforms for the whole German coastal sea. The analogue maps and the coded classification makes them difficult to access for quantitative analyses. Here these maps were digitized and properties of the bedforms were reconstructed and interpreted. Resulting digital maps of the whole and a reduced dataset on steep bedforms contain minimum, maximum and average values of heights, lengths and steepness of bedform types in the German Bight. The data sets are available to the public in the database Pangaea.

Festschrift zum 50-jähr. jubiläum der Realschule mit progymnasium zu Reichenbach i. V. 1899.

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