993 resultados para 207-1258C
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This paper describes some characteristic features of the phytoplankton of Grasmere, one of the smaller of the principal lakes of the English Lake District, and attempts to relate these to distinctive physical and chemical properties of the lake. Quantitative data presented herein are derived from 5-m vertical column samples, collected with a flexible polyethylene hose close to the deepest point of Grasmere, generally at intervals of 14 days ( 7 days from 1972 to 1978, inclusive). The study concludes that although Grasmere has been subject to increased phosphorus-loading and has quickly developed many features associated with eutrophication, the composition of its plankton has retained the characteristics of a mesotrophic, soft-water lake: a vernal diatom maximum, generally dominated by Asterionella, is followed by summer growths of nanoplanktonic species, of various colonial Chlorophyceae, before a substantial return to Asterionella-dominance in the autumn.
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Extensive Rubidium-Strontium age determinations on both mineral and total rock samples of the crystalline rocks of New Zealand, which almost solely crop out in the South Island, indicate widespread plutonic and metamorphic activity occurred during two periods, one about 100-118 million years ago and the other about 340-370 million years ago. The former results date the Rangitata Orogeny as Cretaceous. They associate extensive plutonic activity with this orogeny which uplifted and metamorphosed the rocks of the New Zealand Geosyncline, although no field association between the metamorphosed geosynclinal rocks and plutonic rocks has been found. The Cretaceous plutonic rocks occur to the west in the Foreland Province in Fiordland, Nelson, and Westland, geographically separated from the Geosynclinal Province. Because of this synchronous timing of plutonic and high pressure metamorphic activity in spatially separated belts, the Rangitata Orogeny in New Zealand is very similar to late Mesozoic orogenic activity in many other areas of the circum-Pacific margin (Miyashiro, 1961).
The 340-370 million year rocks, both plutonic and metamorphic, have been found only in that part of the Foreland Province north of the Alpine Fault. There, they are concentrated along the west coast over a distance of 500 km, and appear scattered inland from the coast. Probably this activity marks the outstanding Phanerozoic stratigraphic gap in New Zealand which occurred after the Lower Devonian.
A few crystalline rocks in the Foreland Province north of the Alpine Fault with measured ages intermediate between 340 and 120 million years have been found. Of these, those with more than one mineral examined give discordant results. All of these rocks are tentatively regarded as 340-370 million year old rocks that have been variously disturbed during the Rangitata Orogeny, 100-120 million years ago.
In addition to these two periods, plutonic activity, dominantly basic and ultrabasic, but including the development of some rocks of intermediate and acidic composition, occurred along the margin of the Geosynclinal Province at its border with the Foreland Province during Permian times about 245 million years ago, and this activity possibly extended into the Mesozoic.
Evidence from rubidium-strontium analyses of minerals and a total rock, and from uranium, thorium, and lead analyses of uniform euhedral zircons from a meta-igneous portion of the Charleston Gneiss, previously mapped as Precambrian, indicate that this rock is a 350-370 million year old plutonic rock metamorphosed 100 million yea rs ago during the Rangitata Orogeny. No crystalline rocks with primary Precambrian ages have been found in New Zealand. However, Pb207/Pb206 ages of 1360 million years and 1370 million years have been determined for rounded detrital zircons separated from each of two hornfels samples of one of New Zealand's olde st sedimentary units, the Greenland Series. These two samples were metamorphosed 345- 370 million years ago. They occur along the west coast, north of the Alpine Fault, at Waitaha River and Moeraki River, separated by 135 km. The Precambrian measured ages are most likely minimum ages for the oldest source area which provided the detrital zircons because the uranium, thorium and lead data are highly discordant. These results are of fundamental importance for the tectonic picture of the Southwest Pacific margin and demonstrate the existence of relatively old continental crust of some lateral extent in the neighborhood of New Zealand.
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Isotope shifts of Kα1 x-ray transitions were measured for the Neodymium isotopes Nd 142, 143, 144, 145, 146, 148 and 150, the Samarium isotopes Sm 147, 148, 149, 150, 152 and 154, the Gadolinium isotopes Gd 154, 155, 156, 157, 158 and 160, the Dysprosium isotopes Dy 162 and 164, the Erbium isotopes Er 166, 168 and 170, the Hafnium isotopes Hf 178 and 180 and the Lead isotopes Pb 204, 206, 207 and 208. A curved crystal Cauchois spectrometer was used. The analysis of the measurement furnished the variation of the mean square charge radius of the nucleus, δ˂r2˃, for 23 isotope pairs. The experimental results were compared with theoretical values from nuclear models. Combining the x-ray shifts and the optical shifts in Nd and Sm yielded the optical mass shifts. An anomaly was observed in the odd-even shifts when the optical and the x-ray shifts were plotted against each other.
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A despeito de suas limitações, os dados do SIHSUS são os mais sistemáticos e abrangentes sobre as Reações Adversas e Intoxicações a medicamentos que provocam hospitalização. Eles demonstram a importância das ações de educação e investigação de casos do Programa Nacional de Farmacovigilância para possibilitar o diagnóstico mais acurado e superação do quadro atual de ocorrência desses agravos, além da possibilidade de o SIH/SUS ser utilizado sistematicamente como fonte de dados na detecção e análise dos problemas relacionados a medicamentos. No período de 1999 a 2007, foram emitidas 6.670.609 AIH (tipo 1), entre as quais 3.611 foram classificadas como internações devidas a RAM e 4.675 como Intoxicações, correspondendo, respectivamente, às taxas médias de 5,41 casos por 104 AIH e 7,2 casos por 104 AIH. Ocorreram 137 óbitos (3,79% das AIH) por RAM e 207 (4,43% das AIH) por Intoxicações na população internada. Tanto as RAM como as Intoxicações tiveram menor chance de levar ao óbito quando comparados às outras causas. Uma característica da distribuição dos RAM foi concentrar 62% das AIH nas faixas etárias de 20 a 59 anos de idade (grupo adulto). Nas Intoxicações merece destaque a elevada proporção de AIH na faixa etária de 0-4 anos (14,29%). As AIH registradas com causas básicas relacionados a RAM foram principalmente de pacientes do sexo masculino, já as Intoxicações foram principalmente de pacientes do sexo feminino. Em ambos tipos de agravos estes pacientes foram internados em hospitais que não faziam parte da Rede de Hospitais Sentinelas do Programa Nacional de Farmacovigilância. No entanto, a probabilidade destes hospitais registrarem as AIH com códigos CID-10 referentes às RAM é maior, o que ocorre provavelmente por estarem mais capacitados em diagnosticar este tipo de agravo. Porém este fato não foi observado para as Intoxicações. Os fármacos que causaram os agravos estudados são psicoativos. Este estudo apresentou algumas evidências sobre a distribuição da morbi-mortalidade provocada por medicamentos entre pacientes internados em hospitais conveniados ao SUS no período de 1999-2007, baseadas nas informações das AIH, que podem ser úteis ao Programa de Farmacovigilância no Estado do Rio de Janeiro.
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170 p.
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207 p.
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由于放电结构及谐振腔的限制,准分子激光光斑呈现不均的分布。介绍了各种均匀器的工作原理,从衡量光束均匀性的各项指标出发,评述分析了各种均匀方法的优缺点及适用范围。
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207 p.