995 resultados para Gramatica comparada e geral - Sintaxe
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Partindo da experiência na enfermaria de um hospital-escola1, do confronto com o status-quo do trabalho dos psicólogos em hospitais e da avaliação da literatura sobre a clínica psicanalítica em hospital, esta pesquisa se propôs a buscar avanços frente a uma questão específica: a escuta psicanalítica no trabalho em enfermarias de hospital geral e as implicações dessa prática com o desejo do psicanalista. Foram entrevistados quinze psicólogos declaradamente de orientação psicanalítica, vinculados a unidades de internação e com experiência mínima de dois anos de trabalho em hospital geral. As entrevistas foram abertas e semi-estruturadas, com o intuito de contemplar de maneira uniforme a coleta de informações de cunho mais objetivo, assim como de facilitar a pertinência ao tema de estudo. A interpretação dos dados foi realizada à luz do referencial clínico psicanalítico (freud-lacaniano), sendo que tal interpretação nos permitiu identificar uma importante interação entre os impasses, presentes na instituição hospitalar, da prática clínica psicanalítica com questões pessoais e de formação do profissional, interação que se vincula à postura de trabalho adotada no hospital. Reafirmamos, através desta pesquisa, a possibilidade de fazer uso de uma escuta analítica no trabalho com pacientes internados, a qual está sempre voltada para as manifestações do inconsciente ao longo da fala, e na qual a direção do tratamento é a emergência do sujeito do inconsciente.
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Palaeomagnetic results from 20 volcanic sequences and 11 intrusive bodies (sills and dykes) of the Serra Geral Formation (Paraná Basin) are reported in this paper. The sequences are widespread all over the basin, while sills and dykes (Ponta Grossa arch) come from the northeastern portion. Three mean palaeomagnetic poles were computed for the Serra Geral Formation, which account for a time interval of ∼ 15 Ma. Pole SG1 is located at 85°S,108°E (α95 = 1.1°, N = 18) and represents the main phase of the magmatic activity in the basin, with a mean age of ∼ 135 Ma. Pole SG2 is located at 82°S,38°E (α95 = 7.8°, N = 2) and represents a younger magmatic phase, with an associated age of ∼ 130 Ma. Pole SG3 (72°S,37°E; α95 = 6.8°, N = 10) is the youngest pole. It is computed from the intrusive rocks and its age is assumed to be not younger than 118 Ma, the lower limit of the 'Cretaceous normal magnetic interval'. These three poles describe a shifting path, which suggest that the South American platform moved ∼ 5° southwards and rotated ∼ 10° clockwise during the Lower Cretaceous, preceding the South Atlantic opening. © 1990.
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This work defines the main volcanic types of Central-Southern Parana State (Serra Geral Formation), their stratigraphic relations, and which petrological process are able to explain the observed volcanic associations. -from English summary
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The objective of this study was to evaluate the in vitro activity of cefepime, cefpirome and amikacin against the most prevalent nosocomial bacteria. Initially a prospective study was designed to compare the bacterial susceptibility to the three drugs using 1,022 pathogenic strains. The strains were isolated from hospitalized patients of the Hospital das Clinicas - Faculdade de Medicina de Botucatu, SP, from March to December of 1996, by using the Bauer-Kirby susceptibility diffusion controlled method. The activity of cefepime by the Kirby-Bauer method was significantly higher (χ2, p ≤ 0.05) than cefpirome and amikacin for the following bacteria: P. aeruginosa (72% x 56% x 64%, respectively), Enterobacter cloacae (98% x 88% x 80%) and total strains (79.5% x 74.3% x 76.8%). Cefpirome exhibited higher activity than cefepime only to Enterococcus faecalis (42% x 23%). In the 12 other bacterial groups studied the sensibility of the three drugs was similar (χ2, p ≥ 0.05). The minimal inhibitory concentration (MIC) for 127 bacterial strains - Enterobacter cloacae (12), Citrobacter sp (15), Pseudomonas aeruginosa (50), Acinetobacter baumannii (12), BGNF others (22) and Enterococcus faecalis (16)-from the same origin previously described and isolated during 1997, was determined by E-test. Ranges of MIC intervals, MIC(50%), MIC(90%) and the proportion of the sensitive bacterial strains were determined and permitted the following analysis: the activity of cefepime against Gram-negative bacteria was 2 or more times higher than that of cefpirome and amikacin, specially when CIM(90%) was considered; the activity of cefpirome was higher only against E. faecalis. This information must be considered in the rational use of antibiotic, specially in patients with nosocomial infections.
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Background and Objectives - The decision to perform anesthetic and surgical procedures in children with upper airway infeccious disease, due to the possibility of intraoperative respiratory morbidity, has been a dilemma for anesthesiologists. This study aimed at evaluating the incidence of respiratory complications in children submitted to general anesthesia and correlate them to preoperative signs and symptoms related to the respiratory tract, thus determining anesthetic-surgical morbidity. Methods - Participated in this study 284 children, physical status ASA I or II, submitted to general anesthesia. During preoperative evaluation, respiratory signs and symptoms were recorded, as well as types of diseases and corresponding diagnoses. Respiratory complications during anesthesia and in the recovery room were also recorded and analyzed taking into account age, elective or urgent procedure, airway management and presence or absence of signs, symptoms or history of respiratory tract diseases. Results - We found 38% of patients with preoperative respiratory disease history. The most common respiratory disease was upper airway infection. Intraoperative respiratory complications were present in 26.4% of patients. Children under 12 months of age and those with preoperative respiratory disease history had more intraoperative and PACU complications. Conclusions - We concluded that children, specially younger, with respiratory system involvement, like upper airway infections, are at a higher risk of intra and postoperative respiratory complications, thus with an increased incidence of anesthetic-surgical morbidity.
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With the development of greenhouse grown crops, the whitefly Trialeurodes vaporariorum (West.) has become an important pest. Aiming at verifying the effect of host on the development of this species, the biology of the whitefly was studied on bean (Phaseolus vulgaris L.) cultivars IAC-Carioca Pyatã, IAPAR-57, Jalo Precoce, IAC-Bico de Ouro, IAC-Maravilha and on soybean (Glycine max L.) cultivar Cristalina. The study was conducted at the Laboratório de Entomologia Agrícola - FCA-UNESP, at 25 ± 3°C temperature, 80 ± 10% RH and 14h photophase. The biological parameters assessed were duration, viability and number of nymphal instars; male and female longevity, oviposition period, number of eggs per female and sex ratio; egg viability and incubation period and the life cycle duration. Based on data obtained, fertility life tables were constructed to allow a comparative analysis of the effect of cultivars on the biological development and consequent population growth of this species. The bean cultivars IAC-Maravilha and Jalo Precoce negatively influenced T. vaporariorum development, whereas, the other bean cultivars studied, as well as the soybean cultivar Cristalina, provided good conditions for development of this pest.
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The salivary system of the Hymenoptera consists of the mandible, hypopharynx and thoracic salivary glands. It is very important because it is related to various aspects of the life of the insects, such as pheromone production, feeding the young, food digestion and nest building. Adult Polistes versicolor (Olivier) individuals were dissected, the thoracic salivary glands removed and processed for scanning electronic microscopy and histological examination. The P. versicolor thoracic salivary gland presents alveolar secretory units, consists of pseudoacines and does not have a reservoir. Four types of cells are present in the gland. The T1 and T2 cells make up the pseudoacines and differ mainly by the many secretory vessels in T2. There is a cluster of T3 cells at the base of the gland duct collectors, also with secretory characteristics. The secretion produced in the pseudoacines is conducted by canals and ducts to the outside, and the latter are made of T4 cells. The comparison of these characteristics with those of different Hymenoptera species, already studied, showed that the thoracic salivary gland cannot be used as a single comparison factor in evolutionary studies.
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The purpose of this paper is to present preliminary aspects of the petrography and chemistry of intrusive rocks (sills and dykes) from the eastern portion of the Parana Basin in the State of Säo Paulo. Data from 80 samples of the region show a subaphyric and subophitic nature and have plagioclase (25-50%), augite (3-39%), pigeonite (0-10%) and magnetite (4-20%) as an essential minerals. Apatite and quartz are present as accessory minerals. The geochemical data of intrusive rocks show a basic to intermediate composition (48% < SiO 2 < 56%) and a high Ti nature (TiO 2 > 2%). Based on the minor and trace composition of the intrusive rocks, two different magma types were recognized, named Paranapanema and Pitanga. The spatial distribution of these magma types is not alleatory in the studied region. The intrusive rocks of Pitanga magma type are displayed in the Campinas-Paulinia region, while the Paranapanema magma type cover a large region above that one, between Rio Claro and Cajuru. Furthermore, the chemical composition of the lava flows of the Serra Geral Formation, sampled in this work, reveals a magma of Urubici type. So, the intrusive rocks of the eastern portion of the of State Säo Paulo are not the extension of the lava flows, or they aren't a portions which don't reach the surface.
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This study correlated the solid preoperative fasting periods with plasma glycemia, serum cortisol, condition clinic and acid-base balance in dogs submitted to inhalation of general anaesthesia. Eight adults, animals were distributed into three groups in accordance with solid preoperative fasting: group 1 (12 hours), group 2 (18 hours) and group 3 (24 hours). Gastric emptying was observed and following this animals were submitted to the same anesthetic procedure. Heart and respiratory rate, rectal temperature, capillary refill time, percent hydration and noninvasive arterial pressure determined before and after Acepromazine and every 10 minutes during anaesthesia, included ETCO 2; values blood gas (pH, PaCO 2, PaO 2, HCO 3, TCO 2, SaO 2, BE), glycemic and serum cortisol were analyzed before MPA and each 30 minutes during anaesthesia. In recovery anaesthetic, glycemia and serum cortisol were repeated. During anaesthesia there were little cardiovascular and respiratory alteration not having interference of the preoperative fasting periods. Animals with 12 hours of the preoperative fasting showed a higher rise in glycemia levels than others groups in recovery anaesthetic. Serum cortisol wasn't influenced by fasting. Solid preoperative fasting independent of the duration describe a discreet respiratory alkalosis. All animals showed good clinical condition in all three groups. Solid preoperative fasting of the 18 hours is recommended to ensure a complete absence of the solid food contents in stomach.
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The basalts of the Formação Serra Geral in Parana Basin in the Mato Grosso do Sul and Mato Grosso states cover an area of 180,000 km2. They rest on the Botucatu sandstones and they are recovered by the sedimentary rocks of Bauru and Caiuá Groups. The mineralogical composition of these rocks are plagioclase (40%-55%), clinopyroxenes (19%-40%; augite and pigeonite), opaque minerals (2%-10%; magnetite and ilmenite) and olivine (1.5%). Geochemical data show two different types of basalts, named ATi-Pitanga (2.6% < TiO2 < 4.2%; 396 ppm < Sr < 438 ppm) and BTi-Ribeira (1.7% TiO2 <2.4%, 246 ppm < Sr < 286 ppm). In general, ATi-Pitanga have gently higher La/Yb(n) (6,1 ± 1,5ppm) than those BTi-Ribeira (5.6 ± 1,7ppm). The geochemical differences between ATi-Pitanga and BTi-Ribeira probably are related to different degrees of partial melt of a same mantle source, or to different mantle sources. The field relations show that BTi-Ribeira is displaced towards the north-western margin of the Paraná Basin and the thickness of lava flows increases towards the Paraná Graben, suggesting that ATi-Pitaga overlies BTi-Ribeira.
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