Efeito da suplementação de vitamina D no desenvolvimento de lesões pré-neoplásicas quimicamente induzidas em ratos Wistar macho

Pós-graduação em Biologia Geral e Aplicada - IBB

Efeitos da sobrecarga calórica em ratos machos submetidos ou não a restrição protéica in útero

Pós-graduação em Biologia Geral e Aplicada - IBB

Tintas pretas e papéis brancos: educadoras negras e emancipação

Pós-graduação em Serviço Social - FCHS

Le minoranze religiose durante il fascismo

La volontà di ritornare a un'Italia completamente unita sotto un'unica fede religiosa, quella cattolica, costituisce uno degli elementi che caratterizzarono il regime fascista. Sorge spontaneo chiedersi quali furono le sorti delle altre denominazioni religiose, insediatesi relativamente da poco tempo sul suolo italiano, e come esse reagirono di fronte a questo nuovo potere che cercò di screditarle e limitarle fino a farle scomparire. Si parla spesso della religione ebraica, la minoranza più colpita dalla dittatura: essa dovette subire numerosi provvedimenti che finirono per sfociare in un'aperta persecuzione. Tuttavia, parlare della realtà ebraica durante il regime fascista di Benito Mussolini sarebbe un argomento decisamente troppo esteso per questo mio breve elaborato finale. Mi concentrerò quindi sulle altre minoranze religiose esistenti all'epoca in Italia, tutte riconducibili al protestantesimo, per riflettere sui loro rapporti con il regime e sulle conseguenze che derivarono da determinati provvedimenti presi dal governo. Le mie considerazioni sulle minoranze religiose durante il fascismo inizieranno dai primi atti del nuovo regime, come gli episodi della marcia su Roma e l'attentato all'onorevole Matteotti, fino ad arrivare ad analizzare gli effetti di alcune azioni messe in atto dal governo in ambito religioso e la posizione assunta dalle diverse fedi. Infine, non potendomi soffermare su ogni singola denominazione e sul loro comportamento alla fine della Seconda guerra mondiale, osserverò in linea generale la realtà della Chiesa avventista, indicando i cambiamenti salienti che avvennero nel secondo dopoguerra.

Ecological effects of an artificial island, Rincon Island, Punta Gorda, California /

This study documents marine ecological conditions at Rincon Island, located approximately 0.8 kilometer offshore between Ventura and Santa Barbara, California, in a depth of 14 meters. The island, which was constructed between 1957 and 1958 to serve as a permanent platform for oil and gas production, is particularly suitable for ecological study. Habitat features associated with the armor rock and concrete tetrapods surrounding the island support a 'microecosystem' which differs in biotic composition from surrounding natural bottom areas. A major part of the study was devoted to analysis of seasonal dynamics in biotic composition. Permanent transects extending from the high intertidal to natural bottom were established normal to each of the four cardinal sides of the island. All macrobiota were censused in duplicate 1-square meter quadrats along each transect during each of the four seasons. Data analysis indicated that many species exhibit significant variability in abundance from one season to the next. In general, the findings indicate a rich and varied fauna and flora associated with the high-relief solid substrate of Rincon Island which differs substantially from the more depauperate natural bottom habitats in the area.

Beach changes at Long Beach Island, New Jersey, 1962-73 /

Beach profile line data collected from 32 profile sites along Long Beach Island, New Jersey. A total of 2,158 profile line surveys were examined, using empirical eigenfunction analysis and other measures of beach variability. Most profile lines have shown an accretionary trend since 1962 with rates between 2.3 and 0.24 meter per year in spite of erosion estimates due to sea level rise on the order of 0.68 meter per year. A great deal of variability in profile line change takes place along the beach, increasing from north to south, due to the location of profile lines relative to structures and offshore linear shoals. Detailed closely spaced profile lines taken over a year in a groin field near the north end of the island indicate littoral transport directions shift from north to south. Evidence of a littoral transport node near the north end of the groin field has been found. Net transport of the node is toward the south, but the rate could not be established due to lack of adequate wave data. Profile line variability within groin cells shows that single profile lines are not sufficient to determine the net change within a cell. The design of future beach monitoring studies should consider coastal structures, offshore bathymetry, the method of analysis, and the scales of processes under study. A coastal storm in November 1968 moved the MSL back as much as 22 meters; however, the beach recovered without artificial measures. The offshore bathymetry shows a series of shoreface-connected linear shoals at several locations along the island. Limited data show that these have remained stable and that most beach variability takes place in water shallower than 3 meters.

Field experiences with floating breakwaters in the eastern United States /

In the past 10 years, the use of floating breakwaters as temporary coastal structures has become increasingly widespread in the United States as an inexpensive means for suppressing waves. However, as with any new technology, there have been many failures and a substantial number of imaginative, successful innovations. One of the chief problems contributing to the failure rate has been a lack of awareness by designers of reliable, up-to-date technical information. As part of a large research effort to remedy this problem, a survey was conducted on field experience with floating breakwaters in the Eastern United States. Results of the survey confirmed that state-of-the-art technical literature is not being properly disseminated. Structures built according to early design manuals were shown to have failed before the completion of their design life. Conversely, floating breakwaters built to the standards set by recent research have fared well and show promise of meeting their design golas. The weakest areas of the present technology are flotation and the anchoring systems. It is recommended that a concentrated research effort be directed toward these problem areas; it is also recommended that the monitoring of state-of-the-art projects continue. (Author).

Long-term changes in beach fauna at Duck, North Carolina /

Long-term changes in the beach fauna at Duck, North Carolina, were investigated. Twenty-one stations located on three transects on the oceanside and twenty-four stations located on three transects on the sound side were sampled seasonally from November 1980 to July 1981. The data collected in this study were compared to a previous study conducted in 1976 (Matta, 1977) to investigate the potential effects of the construction of the CERC Field Research Facility pier on the adjacent beaches. No effects on the benthic fauna were found. Changes observed in the benthic macrofauna on the ocean beaches were well within the range attributable to the natural variation of an open coast system. The ocean beach macrofauna was observed to form a single community migrating on an off the beach with the seasons. On the sound beaches, changes were detected in the benthic macrofauna; however, these were attributed to a salinity increase during the 1981 sampling year. (Author).

Dune stabilization with Panicum amarum along the North Carolina coast /

"February 1976."

Reflection and transmission characteristics of porous rubble-mound breakwaters /

"March 1976."

Vegetative study at the Duck Field Research Facility, Duck, North Carolina /

"April 1976."

A positive displacement oscillatory water tunnel /

"February 1977."

The development of a numerical solution to transport equation /

"Prepared for U.S. Army Engineer District, Mobile."

Sand ripple growth in an oscillatory-flow water tunnel /

The development of sand ripples in an oscillatory-flow water tunnel was observed in 104 laboratory experiments approximating conditions at the seabed under steady progressive surface waves. The period, T, and amplitude, a, of the water motion were varied over wide ranges. Three quartz sands were used, with mean grain diameters, D = 0.55, 0.21, and 0.18 millimeter. In 24 experiments, with the bed initially leveled, T was reduced until ripples appeared, and their development to final equilibrium form was observed without further change in T. The remaining 80 experiments investigated the response of previously established bed forms to changes in T or a or both. The ripple length, lambda, and height, eta, were measured from photos, except when bed forms were three dimensional.