Filmes finos ferroelétricos do tipo PBCT, PBST e PCST: estudo experimental e teórico

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Age determination of sediment cores from the continental shelf and slope off North-West Africa

Three sediment cores from the continental shelf and slope off NW Africa (Banc d'Arguin; 52 m, 665 m and 973 m water depth) have been investigated by means of a coarse fraction analysis. The two shallower cores have been deposited during less than 10,000 years, the deeper one during the last 36,000 years. The Holocene sedimentation ( 4000 years) in the deeper part of core 79 the edge of the Banc d'Arguin is strongly influenced by reworking of Late Glacial dune sands and biogenic particles from shallower ware (<40 m), as well as eroding current influence. A decrease in grain size of silicate material and a decrease in lateral supply, correlated to a doubling of accumulation rates in the upper part of the core, indicates a more autochthonous sedimentation with less sorting influence in the youngest Holocene. The depth of provenance of the allochttonous material can be assumed in 100-300 m water depth as indicated by various biogenous particles. Small amounts of shallow water particles in the autochthonous layers indicate a supplay from shallow water, which probably occured b ythe mechanism of "particle by particle supply". None of the three cores indicates upwelling influence, although occanographers found intense upwelling in the area of the Banc d'Arguin. The Holocene climate in that area probably has been arid, small variations in terrigenous matter composition and grain size in the Early Holocene might be due to decreased wind strength or to an increase in rain fall. The Peak Glacial section (14,000-22,000 y. B.P.) of the deepest core 88 indicates a very much intensified eolian silt supply and an additional bottom supply of quartz sand In the interval 22,000-36,000 y. B.P. wind strength decreased, but probably no increase in humidity occurred. So this area in about 19° 40' N had an arid climate in the Late Holocene and in the Peak Glacial. The fragmentation of planktonic foraminifers and the abundance of aragonitic tests of pteropods in core 88 indicate an Early Holocene (8330 y. B.P.) preservation spike. Two minima in fragmentation correlated to maxima in pteropod content at about 15,700 and 21,000 y. B.P. are correlated to maxima in shallow water supply and thus do not reflect preservation conditions, but only lateral supply from the carbonate dissolution minimum zone in about 300 m water depth.

Alegación por la casa-banco conocida bajo la razon de Rothschild hermanos, de Paris, en el pleito ... de quiebra de la sociedad metalúrgica La Británica establecida en Alicante que ... pende ... de esta Audiencia territorial entre los herederos del ... señor Don Pio Pita Pizarro, los Síndicos de la quiebra, y la referida casa de Rothschild sobre liquidacion de la cuenta de plata núm. 1º presentada á la junta de acreedores por ésta

Las h. pleg. contienen: Testimonios de la cuentas de Rothschild

La formació d'una cooperativa de segon grau en la Vall de Guadalest. Un instrument agrari de desenvolupament rural

El camp valencià es troba immers en un procés de subsistència que any rere any empitjora, lligat a la falta de rendibilitat i que afecta sobretot a zones que han conservat el seu model agrari tradicional, condicionades doncs al seu abandonament. Aquesta situació recau en les nostres mans, tenint l’oportunitat de cercar projectes i iniciatives per tal de posar en valor els recursos propis de cada lloc i que a més, siguen atractives per a anar tant a viure com treballar. Per tant la finalitat d’aquest treball és realitzar un estudi aplicat a la Vall de Guadalest, per a estimar si la creació d’un instrument què cohesione els agents implicats en l’activitat agrària, com en aquest cas, una cooperativa de segon grau, pot servir com eina de desenvolupament territorial sostenible que reactive l’activitat agrària i ature el procés d’abandonament del camp.

(Tab. XIII.1) TOC content, carbonate content, carbonate mineralogy, percentage of total carbonate, aragonite, low magnesium calcium, and high magnesium calcium, and grain-size contents from samples from the Golfe d'Arguin and from the Western Sahara

Modern carbonate sedimentation takes place on the northern Mauritanian shelf (20°N), where typical tropical components (e.g. hermatypic reefs, calcareous green algae) are absent. Such deposits are reminiscent of extratropical sediment in the geological record. The tropical open shelf of Mauritania is influenced by large siliciclastic dust input and upwelling, highly fertilizing the ocean, as well as strongly limiting the light penetration. In this context, temperature does not appear to be the steering factor of carbonate production. This thesis describes the depositional system of the Golfe d'Arguin off Mauritania and focuses on environmental conditions that control the depositional pattern, in particular carbonate production. The description of this modern analogue provides a tool for paleoenvironmental interpretation of ancient counterparts. The Golfe d'Arguin is a broad shallow shelf comprising extensive shoals (<10 m water depth; i.e. the Banc d'Arguin) on the inner shelf where waters warm up. The sediments collected in water depths between 4 and 600 m are characterized by mixed carbonate and siliciclastic (dust) deposits. They vary from clean coarse-grained, almost pure carbonate loose sediments to siliciclastic-dominated fine-grained sediments. The carbonate content and sediment grain size show a north-south decreasing pattern through the Golfe d'Arguin and are controlled by the hydraulic regime influenced by wind-driven surface currents, swell, and tidal currents. The carbonate grain association is heterozoan. Components include abundant molluscs, foraminifers, and worm tubes, as well as barnacles and echinoderms, elements that are also abundant in extratropical sediments. The spatial distribution of the sedimentary facies of the Golfe d'Arguin does not display a depth zonation but rather a mosaic (i.e. patchy distribution). The depth and climatic signatures of the different sedimentary facies are determined by taxonomic and ecological investigations of the carbonate-secreting biota (molluscs and foraminifers). While certain planktonic foraminifers and molluscs represent upwelling elements, other components (e.g. mollusc and benthic foraminifer taxa) demonstrate the tropical origin of the sediment. The nutrient-rich (and thus also low light-penetration) conditions are reflected in the fact that symbiotic and photosynthetic carbonate-producing organisms (e.g. hermatypic corals) are absent. The Mauritanian deposits represent an environment that is rare in the modern world but might have been more common in the geological past when global temperatures were higher. Taxonomic and ecological studies allow for distinguishing carbonate sediments formed under either tropical high-nutrient or extratropical conditions, thus improving paleoclimate reconstruction.

Nachertanie statistiki rossĭskago gosudarstva /

Mode of access: Internet.

Bilder des griechischen Alterthums, oder, Darstellung der berühmtesten Gegenden und der wichtigsten Kunstwerke des alten Griechenlandes /

Includes a plan mapped by Kauffer, plans lithographed by J. Brodtmann and other illustrations drawn by L.F. Cassas, Schulthess, and Brehm and lithographed by J. Brodtmann and Scheuchzer.

Art by the way /

One of 750 copies.

The twelve moneths and Christmas Day, from 'Fantastickes.'

Printed at the Thistle Press to designs executed by Bruce Rogers.

Reminiscences of outdoor life /

Farquhar

Prince Lucien Campbell /

Mode of access: Internet.

Half-hours with Jimmieboy /

Mode of access: Internet.

A house dividing; Lincoln as president elect,

"Originally written as a doctoral dissertation."--Pref.

Chilula texts /

Chilula text with English translation.

What you ought to know about your baby /

All ghost-written by H.L. Mencken except the questions and answers. cf. Schrader.