Caracterização elétrica de túnel-FET em estrutura de nanofio com fontes de SiGe e Ge em função da temperatura.

Este trabalho teve como objetivo estudar os transistores de tunelamento por efeito de campo em estruturas de nanofio (NW-TFET), sendo realizado através de analises com base em explicações teóricas, simulações numéricas e medidas experimentais. A fim de avaliar melhorar o desempenho do NW-TFET, este trabalho utilizou dispositivos com diferentes materiais de fonte, sendo eles: Si, liga SiGe e Ge, além da variação da espessura de HfO2 no material do dielétrico de porta. Com o auxílio de simulações numéricas foram obtidos os diagramas de bandas de energia dos dispositivos NW-TFET com fonte de Si0,73Ge0,27 e foi analisada a influência de cada um dos mecanismos de transporte de portadores para diversas condições de polarização, sendo observado a predominância da influência da recombinação e geração Shockley-Read-Hall (SRH) na corrente de desligamento, do tunelamento induzido por armadilhas (TAT) para baixos valores de tensões de porta (0,5V > VGS > 1,5V) e do tunelamento direto de banda para banda (BTBT) para maiores valores tensões de porta (VGS > 1,5V). A predominância de cada um desses mecanismos de transporte foi posteriormente comprovada com a utilização do método de Arrhenius, sendo este método adotado em todas as análises do trabalho. O comportamento relativamente constante da corrente dos NW-TFETs com a temperatura na região de BTBT tem chamado a atenção e por isso foi realizado o estudo dos parâmetros analógicos em função da temperatura. Este estudo foi realizado comparando a influência dos diferentes materiais de fonte. O uso de Ge na fonte, permitiu a melhora na corrente de tunelamento, devido à sua menor banda proibida, aumentando a corrente de funcionamento (ION) e a transcondutância do dispositivo. Porém, devido à forte dependência de BTBT com o campo elétrico, o uso de Ge na fonte resulta em uma maior degradação da condutância de saída. Entretanto, a redução da espessura de HfO2 no dielétrico de porta resultou no melhor acoplamento eletrostático, também aumentando a corrente de tunelamento, fazendo com que o dispositivo com fonte Ge e menor HfO2 apresentasse melhores resultados analógicos quando comparado ao puramente de Si. O uso de diferentes materiais durante o processo de fabricação induz ao aumento de defeitos nas interfaces do dispositivo. Ao longo deste trabalho foi realizado o estudo da influência da densidade de armadilhas de interface na corrente do dispositivo, demonstrando uma relação direta com o TAT e a formação de uma região de platô nas curvas de IDS x VGS, além de uma forte dependência com a temperatura, aumentando a degradação da corrente para temperaturas mais altas. Além disso, o uso de Ge introduziu maior número de impurezas no óxido, e através do estudo de ruído foi observado que o aumento na densidade de armadilhas no óxido resultou no aumento do ruído flicker em baixa frequência, que para o TFET, ocorre devido ao armadilhamento e desarmadilhamento de elétrons na região do óxido. E mais uma vez, o melhor acoplamento eletrostático devido a redução da espessura de HfO2, resultou na redução desse ruído tornando-se melhor quando comparado à um TFET puramente de Si. Neste trabalho foi proposto um modelo de ruído em baixa frequência para o NW-TFET baseado no modelo para MOSFET. Foram realizadas apenas algumas modificações, e assim, obtendo uma boa concordância com os resultados experimentais na região onde o BTBT é o mecanismo de condução predominante.

Refinery Nonconventional Feedstocks: Influence of the Coprocessing of Vacuum Gas Oil and Low Density Polyethylene in Fluid Catalytic Cracking Unit on Full Range Gasoline Composition

Gasoline coming from refinery fluid catalytic cracking (FCC) unit is a major contributor to the total commercial grade gasoline pool. The contents of the FCC gasoline are primarily paraffins, naphthenes, olefins, aromatics, and undesirables such as sulfur and sulfur containing compounds in low quantities. The proportions of these components in the FCC gasoline invariable determine its quality as well as the performance of the associated downstream units. The increasing demand for cleaner and lighter fuels significantly influences the need not only for novel processing technologies but also for alternative refinery and petrochemical feedstocks. Current and future clean gasoline requirements include increased isoparaffins contents, reduced olefin contents, reduced aromatics, reduced benzene, and reduced sulfur contents. The present study is aimed at investigating the effect of processing an unconventional refinery feedstock, composed of blend of vacuum gas oil (VGO) and low density polyethylene (LDPE) on FCC full range gasoline yields and compositional spectrum including its paraffins, isoparaffins, olefins, napthenes, and aromatics contents distribution within a range of operating variables of temperature (500–700 °C) and catalyst-feed oil ratio (CFR 5–10) using spent equilibrium FCC Y-zeolite based catalyst in a FCC pilot plant operated at the University of Alicante’s Research Institute of Chemical Process Engineering (RICPE). The coprocessing of the oil-polymer blend led to the production of gasoline with very similar yields and compositions as those obtained from the base oil, albeit, in some cases, the contribution of the feed polymer content as well as the processing variables on the gasoline compositional spectrum were appreciated. Carbon content analysis showed a higher fraction of the C9–C12 compounds at all catalyst rates employed and for both feedstocks. The gasoline’s paraffinicity, olefinicity, and degrees of branching of the paraffins and olefins were also affected in various degrees by the scale of operating severity. In the majority of the cases, the gasoline aromatics tended toward the decrease as the reactor temperature was increased. While the paraffins and iso-paraffins gasoline contents were relatively stable at around 5 % wt, the olefin contents on the other hand generally increased with increase in the FCC reactor temperature.

Multidecadal variability of the continental precipitation annual amplitude driven by AMO and ENSO

As the water vapor content in the atmosphere scales with temperature, a warmer world is expected to feature an intensification of the hydrological cycle. Work to date has mainly focused on mean precipitation changes, whose connection to climatic modes is elusive at a global scale. Here we show that continental precipitation annual amplitude, which represents the annual range between minimum and maximum (monthly) rainfall, covaries with a linear combination of the Atlantic Multidecadal Oscillation and low-frequency variations in the El Niño–Southern Oscillation on a decadal to multidecadal scale with a correlation coefficient of 0.92 (P<0.01). The teleconnection is a result of changes in moisture transport in key regions. Reported trends in the annual amplitude of global precipitation in recent decades need to be assessed in light of this substantial low-frequency variability, which could mask or enhance an anthropogenic signal in hydrological cycle changes.

The SAAS-R: A New Instrument to Assess the School Attitudes of Students with High and Low Academic Achievement in Spain

We examined the psychometric properties of the School Attitude Assessment Survey–Revised in a Spanish population (n = 1,398). Confirmatory factor analysis procedures supported the instrument’s five-factor structure. The results of discriminant analysis demonstrated the predictive power of the School Attitude Assessment Survey–Revised scales as regards academic performance. Implications for education and assessment are discussed.

Satisfying Labour Demands in Mid- and Low-Skilled Occupations through Immigration

The purpose of this article is to explain the importance and necessity of satisfying labour demands through the migration of less-skilled workers. It will also argue that more work is needed to anticipate labour and skill shortages and will examine ways of better identifying the role of mid- and low-skilled migration in filling such shortages.

(Appendix) Oxygen isotope record and carbonate mineralogy of the top part of ODP Hole 101-633A

Hole 633A was drilled in the southern part of Exuma Sound on the toe-of-slope of the southeastern part of Great Bahama Bank during ODP Leg 101. The top 55 m, collected as a suite of six approximately 9.5-m-long hydraulic piston cores, represents a Pliocene-Pleistocene sequence of periplatform carbonate ooze, a mixture of pelagic calcite (foraminifer and coccolith tests), some pelagic aragonite (pteropod tests), and bank-derived fine aragonite and magnesian calcite. A 1.6-m.y.-long hiatus was identified at 43.75 mbsf using calcareous nannofossil biostratigraphy and magnetostratigraphy. The 43.75-m-thick periplatform sequence above the hiatus is a complete late Pliocene-Quaternary record of the past 2.15 m.y. The d18O curve, primarily based on Globigerinoides sacculifera, clearly displays high-frequency/low-amplitude cycles during the early Pleistocene and low-frequency/high-amplitude cycles during the middle and late Pleistocene. Variations in aragonite content in the fine fraction of the periplatform ooze show a cyclic pattern throughout the Pleistocene, as previously observed in piston cores of the upper Pleistocene. These variations correlate well with the d18O record: high aragonite corresponds to light interglacial d18O values, and vice versa. Comparison of the d18O record and the aragonite curve helps to identify 23 interglacial and glacial oxygen-isotope stages, corresponding to 10.5 aragonite cycles (labeled A to K) commonly established during the middle and late Pleistocene (0.9 Ma-present). Strictly based on the aragonite curve, another 11 aragonite cycles, labeled L to V, were identified for the early Pleistocene (0.9 to 1.6 Ma). Mismatches between the d18O record and the aragonite curve occur mainly at some of the glacial-to-interglacial transitions, where aragonite increases usually lag behind d18O depletion. When one visually connects the minima on the Pleistocene aragonite curve, low-frequency (0.4 to 0.5 m.y.) supercycles seem to be superimposed on the high-frequency cycles. The timing of this supercycle roughly matches the timing of the Pleistocene carbonate preservation supercycles described in the Pacific, Indian, and Atlantic oceans. Mismatches between aragonite and d18O cycles are even more obvious for the late Pliocene (1.6 to 2.15 Ma). Irregular aragonite variations are observed for the late Pliocene, although after the onset of late Pleistocene-like glaciations in the North Atlantic Ocean 2.4 m.y. ago the d18O record has shown a mode of high-frequency/low-amplitude cycles. Initiation of climatically induced aragonite cycles occurs only at the Pliocene-Pleistocene transition, 1.6 m.y. ago. After that time, aragonite cycles are fully developed throughout the Quaternary. The 11-m-thick periplatform sequence below the hiatus represents a lower Pliocene interval between 3.75 and 4.45 Ma. The bottom half (4.25-4.45 Ma) has a fairly constant, high aragonite content (averaging 60%) and high sedimentation rates (28 m/m.y.) and corresponds to the end of the prolonged early Pliocene interglacial interval (4.1-5.0 Ma), established as a worldwide high sea-level stand. The second half (3.75-4.25 Ma), in which aragonite content decreases by successive steps, paralleled by a gradual 5180 enrichment in Globigerinoides sacculifera and low sedimentation rates (10 m/m.y), corresponds to the climatic deterioration established worldwide between 4.1 and 3.8 Ma, to a decrease of carbonate preservation observed in the equatorial Pacific Ocean, and to a global sea-level decline. Dolomite, a ubiquitous secondary component in the lower Pliocene, is interpreted as being authigenic and possibly related to diagenetic transformation of primary bank-derived fine magnesian calcite. Transformation of the primary mineralogical composition of the periplatform ooze was evidently minor, as the sediments have retained a detailed record of the Pliocene-Pleistocene climatic evolution. Clear evidence of diagenetic transformations in the periplatform ooze includes (1) the disappearance of magnesian calcite in the upper 20 m of Hole 633A, (2) the occurrence of calcite overgrowths on foraminiferal tests and microclasts at intermittent chalky core levels, and (3) the ubiquitous presence of authigenic dolomite in the lower Pliocene.

Benthic foraminiferal assemblages and paleoproductivity reconstructions for the last 550 kyr of the Ontong Java Plateau, western equatorial Pacific

We analyzed foraminiferal and nannofossil assemblages and stable isotopes in samples from ODP Hole 807A on the Ontong Java Plateau in order to evaluate productivity and carbonate dissolution cycles over the last 550 kyr (kilo year) in the western equatorial Pacific. Our results indicate that productivity was generally higher in glacials than during interglacials, and gradually increased since MIS 13. Carbonate dissolution was weak in deglacial intervals, but often reached a maximum during interglacial to glacial transitions. Carbonate cycles in the western equatorial Pacific were mainly influenced by changes of deep-water properties rather than by local primary productivity. Fluctuations of the estimated thermocline depth were not related to glacial to interglacial alternations, but changed distinctly at ~280 kyr. Before that time the thermocline was relatively shallow and its depth fluctuated at a comparatively high amplitude and low frequency. After 280 kyr, the thermocline was deeper, and its fluctuations were at lower amplitude and higher frequency. These different patterns in productivity and thermocline variability suggest that thermocline dynamics probably were not a controlling factor of biological productivity in the western equatorial Pacific Ocean. In this region, upwelling, the influx of cool, nutrient-rich waters from the eastern equatorial Pacific or of fresh waters from rivers have probably never been important, and their influence on productivity has been negligible over the studied period. Variations in the inferred productivity in general are well correlated with fluctuations in the eolian flux as recorded in the northwestern Pacific, a proxy for the late Quaternary history of the central East Asian dust flux into the Pacific. Therefore, we suggest that the dust flux from the central East Asian continent may have been an important driver of productivity in the western Pacific.

Differential educational attainment among "at-risk" youth : a case study of language minority youth of Mexican descent and low socioeconomic status /

"August 1982."

Some performance effects of age and low blood alcohol levels on a computerized neuropsychological test.

Federal Aviation Administration, Office of Aviation Medicine, Washington, D.C.

Effects of age and low doses of alcohol on compensatory tracking during angular acceleration.

Federal Aviation Administration, Office of Aviation Medicine, Washington, D.C.

Drivers survey on unreported and low-damage accidents involving bumpers. Final report.

National Highway Traffic Safety Administration, Washington, D.C.

Health status of minorities and low-income groups.

Shipping list no.: 91-296-P.

A treatise of the law of waters; including the law relating to rights in the sea, and rights concerning rivers, canals, dock companies, fisheries, mills, water-courses, &c. with a note concerning the rights of the Crown to the land between high and low water mark.

"The law of sewers has been separately published in a second edition, and is, therefore, withdrawn from this second edition of the Law of waters."--2d prelim. leaf.

Potential means of cost reduction in grade crossing automatic gate systems. Volume I: overview and low cost railroad/highway grade crossing gate systems. Final report.

Transportation Systems Center, Cambridge, Mass.