1000 resultados para Resultados negativos
Resumo:
El éxito en la difusión de los estándares de gestión ha llevado a las organizaciones a tratar de avanzar en su integración. Paralelamente, en el ámbito académico se han comenzado a publicar las primeras investigaciones que analizan dichos aspectos. En este sentido, la literatura existente sobre la integración de sistemas de gestión se basa, principalmente, en estudios teóricos en los que se describe qué es un sistema integrado de gestión, la metodología de integración, los niveles de integración de la empresa y sus ventajas y desventajas, como principales aspectos a tener en cuenta en el proceso. Ene ste artículo se resumen los primeros resultados descriptivos de un trabajo de campo cuantitativo finalizado recientemente en las empresas de la Comunidad Autónoma del País Vasco, con el objetivo de obtener algún tipo de evidencia empírica sobre cuál es el grado de integración de los diferentes estándares de sistemas de gestión en las empresas vascas, así como de recoger la opinión de las empresas que ya han implantado algún estándar internacional de sistemas de gestión sobre la dirección que ha de tomar el proceso de creación de estos estándares
Resumo:
Los docentes de los distintos ciclos del sistema educativo que están comenzando su vida profesional,si permanecen en esta actividad, trabajarán durante los próximos treinta o cuarentaaños con personas que vivirán parte de su vida en el siglo XXII. Este hecho constituye un puntode reflexión para los educadores quienes recibimos nuestra formación básica en el sigloXX, estamos desarrollando nuestro trabajo en el XXI, y tenemos la responsabilidad de preparara individuos para que puedan construir un mañana que ya es hoy (Millán y Sancho, 1995).Aquí comienza el interés de nuestros grupos de investigación por explorar cómo los hombresy las mujeres que han salido en los últimos años de las facultades de formación del profesorado,con las especialidades de educación infantil y primaria, aprenden a ser docentes. Cómose han ido constituyendo y posicionando como maestros y maestras durante la formación inicial y los primeros años de su vida profesional...
Resumo:
Los docentes de los distintos ciclos del sistema educativo que están comenzando su vida profesional,si permanecen en esta actividad, trabajarán durante los próximos treinta o cuarentaaños con personas que vivirán parte de su vida en el siglo XXII. Este hecho constituye un puntode reflexión para los educadores quienes recibimos nuestra formación básica en el sigloXX, estamos desarrollando nuestro trabajo en el XXI, y tenemos la responsabilidad de preparara individuos para que puedan construir un mañana que ya es hoy (Millán y Sancho, 1995).Aquí comienza el interés de nuestros grupos de investigación por explorar cómo los hombresy las mujeres que han salido en los últimos años de las facultades de formación del profesorado,con las especialidades de educación infantil y primaria, aprenden a ser docentes. Cómose han ido constituyendo y posicionando como maestros y maestras durante la formación inicial y los primeros años de su vida profesional...
Resumo:
Los docentes de los distintos ciclos del sistema educativo que están comenzando su vida profesional,si permanecen en esta actividad, trabajarán durante los próximos treinta o cuarentaaños con personas que vivirán parte de su vida en el siglo XXII. Este hecho constituye un puntode reflexión para los educadores quienes recibimos nuestra formación básica en el sigloXX, estamos desarrollando nuestro trabajo en el XXI, y tenemos la responsabilidad de preparara individuos para que puedan construir un mañana que ya es hoy (Millán y Sancho, 1995).Aquí comienza el interés de nuestros grupos de investigación por explorar cómo los hombresy las mujeres que han salido en los últimos años de las facultades de formación del profesorado,con las especialidades de educación infantil y primaria, aprenden a ser docentes. Cómose han ido constituyendo y posicionando como maestros y maestras durante la formación inicial y los primeros años de su vida profesional...
Resumo:
Los docentes de los distintos ciclos del sistema educativo que están comenzando su vida profesional,si permanecen en esta actividad, trabajarán durante los próximos treinta o cuarentaaños con personas que vivirán parte de su vida en el siglo XXII. Este hecho constituye un puntode reflexión para los educadores quienes recibimos nuestra formación básica en el sigloXX, estamos desarrollando nuestro trabajo en el XXI, y tenemos la responsabilidad de preparara individuos para que puedan construir un mañana que ya es hoy (Millán y Sancho, 1995).Aquí comienza el interés de nuestros grupos de investigación por explorar cómo los hombresy las mujeres que han salido en los últimos años de las facultades de formación del profesorado,con las especialidades de educación infantil y primaria, aprenden a ser docentes. Cómose han ido constituyendo y posicionando como maestros y maestras durante la formación inicial y los primeros años de su vida profesional...
Resumo:
The understanding of false belief is one of the most important milestones in the development of social cognition in children. Many studies have been conducted on this kind of cognition in children with a typical development. Despite being a key point for improving their welfare and quality of life, there are few studies in children with Down's syndrome. The aim of the present work is to carry out an in-depth study of social cognition in children with Down's syndrome. For this purpose, we used 6 tasks, with 3 levels of difficulty, in a group of 9 children aged between 4 and 14 years. Six of these children had a genetic diagnosis of Down's syndrome. The results of our research corroborate previous studies suggesting difficulties in the development of social cognition in children with Down's syndrome, and more specifically in tasks involving false beliefs
Resumo:
A hydrometallurgical method for the recovery of rare earth metals, cobalt, nickel, iron, and manganese from the negative electrodes of spent Ni - MH mobile phone batteries was developed. The rare earth compounds were obtained by chemical precipitation at pH 1.5, with sodium cerium sulfate (NaCe(SO4)2.H2O) and lanthanum sulfate (La2(SO4)3.H2O) as the major recovered components. Iron was recovered as Fe(OH)3 and FeO. Manganese was obtained as Mn3O4.The recovered Ni(OH)2 and Co(OH)2 were subsequently used to synthesize LiCoO2, LiNiO2 and CoO, for use as cathodes in ion-Li batteries. The anodes and recycled materials were characterized by analytical techniques.
Resumo:
Electrodegradation of atrazine in water was performed using homemade (PA and PB) and purchased (PC) boron-doped diamond anodes. The degradation was monitored off-line by analyzing total organic carbon and high performance liquid chromatography with diode array detector (HPLC-DAD) and at-line by UV spectroscopy. The spectra were recorded every 2 min. The rank deficiency problem was resolved by assembling an augmented column-wise matrix. HPLC was employed to separate the original and byproducts degradation components. Aiming the same goal, multivariate curve resolution - alternating least squares (MCR-ALS) was applied to resolve the UV spectroscopic data. Comparison between HPLC and MCR-ALS separations is presented. By using MCR-ALS the spectra of atrazine and two byproducts were successfully resolved and the resulted concentration profiles properly represented the system studied. The ALS explained variance (R2) for PA, PB and PC was equal to 99.99% for all of them and the lack of fit for PA, PB and PC were 0.39, 0.34 and 0.54 respectively. The correlation (R) between the recovered and pure spectra were calculate for each electrodegradation, validating the MCR-ALS results. The average R was equal to 0.997. The spectral and concentration profiles described with this new approach are in agreement with HPLC-DAD results. The proposed method is an alternative to classical analyses for monitoring of the degradation process, mainly due to the simplicity, fast results and economy.
Resumo:
O gênero Erigeron (Asteraceae), de plantas da vegetação espontânea, encontra-se amplamente disseminado nas regiões Sul e Sudeste do Brasil, sendo freqüentemente encontrado em lavouras perenes e anuais. Plantas de E. bonariensis com sintoma de mosaico, típico do induzido por vírus, foram coletadas no município de São Paulo e submetidas a análises ao microscópio eletrônico de transmissão, testes biológicos, sorológicos e moleculares. Em cortes ultrafinos do tecido foliar original, observaram-se inclusões tubulares e cata-ventos dispersos no citoplasma. Através de inoculação mecânica, somente Chenopodium amaranticolor, C. quinoa, Nicotiana benthamiana e N. clevelandii foram infetadas. Os resultados obtidos em ELISA foram negativos quando se utilizaram antissoros contra o Turnip mosaic vírus (TuMV) e diferentes estirpes do Potato virus Y (PVY), constatando-se relacionamento sorológico com o Lettuce mosaic virus (LMV). Com a utilização de oligonucleotídeos específicos para LMV amplificaram-se fragmentos esperados de aproximadamente 280 pb, que seqüênciados confirmaram a identidade do vírus. A ocorrência do LMV em E. bonariensis, gênero da mesma família botânica da alface (Lactuca sativa), é de grande importância, pois talvez possa atuar como reservatório para infecção de campos de produção de alface. Este é o primeiro relato, no Brasil, de vírus infetando Erigeron sp., o qual só havia sido reportado como hospedeira natural do Bidens mottle virus (BiMoV) e do Tomato spotted wilt virus (TSWV) nos Estados Unidos.
Resumo:
In Anis paper are listed 19 different species of Hydrozca collected during a trip to the oceanic island of Trindade, located at lat. 20º 30' 00" S. and long. 29º 22' 00" W., 600 miles off the brazilian coast. During the trip hawls and dredges were done at different points of the island and of banks that exist between the coast and the island. Of the 19 listed species one is here considered new to science: Hebellopsis besnardi (p. 83), characterized by having thecae with a single curvature and a strongly everted margin. Its measures are intermediate between those os H. hartmeyeri and H. sinuosa, which are its closest allies. H. besnardi was found epizoic on D. quadridentata. Of the remainder 18, 14 were already known from the brazilian coast. Of these 14, 4 were previously known only from the coast south of Cabo Frio, and 10 are at present known only from the region north of Cabo Frio. Five species are found both north and south of this Cape. As a whole, 5 species are recorded now for the first time on the brazilian coast, of these are given a full description and figures. This paper has the purpose of increasing the faunistical knowledge of this region of the Atlantic Ocean as a first step towards the understanding of the zoogeographical relationships with the other oceans and the establishment of the zoogeographical regions of this coast.
Resumo:
Trata o presente trabalho de uma coleção de peixes obtida em Cabo Frio, em São João da Barra, no Banco de São Tomé, no Banco Jaseur e na Ilha da Trindade. Considerando-se a ocorrência das espécies, por localidade, chega-se ao seguinte resultado: Cabo Frio ........................................... 13 espécies. São João da Barra ............................... 8 " " " Banco São Tomé ................................. 16 " " " Banco Jaseur ...................................... 2 " " " Ilha da Trindade .................................. 32 " " " Examinando-se as espécies da Ilha da Trindade, verifica-se que as frequentadoras da região representam, na realidade, 37,5% do total capturado, cifra obtida nessa primeira viagem de estudo. A maioria é encontratada tanto na região pelágica como nas proximidades da costa. Analisando-se a fauna da região estudada pelo Museu Americano de Nova Iorque, pelo Museu Nacional, do Rio de Janeiro e pelo Instituto Paulista de Oceanografia, constata-se que sobe a 66 o número de espécies lá encontradas entre 1912 e 1950. É de se presumir que ulteriores observações, levadas a efeito em várias épocas do ano, possam ainda acrescer esse número. A contribuição do Instituto Paulista de Oceanografia foi de 24 espécies que, incorporadas às 42 já constatadas per outras expedições, dão o total das até agora conhecidas no local.
Resumo:
This preliminary paper gives new informations concerning occurrence and geographical dispersal of some Chlorophyceae collected at TRINDADE ISLAND (20º 30' Lat. S. and 29º 22' Long. W. Gw.). The following species are considered: Halimeda Opuntia (L.) Lamx. Penicillus Lamourouxii Dcne. Udotea Flabellum (E. & Sol.) Howe. Dictyosphaeria favulosa (Ag.) Dcne. Anadyomene stellata (W.) J. Ag.
Resumo:
The oceanographic work realized during 10 days in the surroundings of the eruptive island of Trindade, 20º30'36" lat. S - 29º19'26" long. W, had as principal aim the determination of the insular plateau, whose knowledge was very insufficient. Thus were established some oceanographic stations and sounding lines were realized by means of an echobathymeter whose responses were initially verified with mechanical soundings obtaneid by means of a Thomson sounder. The insular plateau is very narrow and exhibits a sudden fall between the 100 and 120 m. depth line at 740 m. - 2950 m. from the coast. Its greatest depth is of 108,30 m. and its mean inclination is of 8,12%. The plateau of the island of Trindade is separated from that of the neighbouring group of Martim Yaz by great depths. The bottoms are rocky near the coast, the blocks having been produced by the rupture of the magmatic mass of the island. Further away from the coast, the size of the rocks gradually diminishes up to the fine sand thickness. In the litoral zone there are abundant tufts of living Lithothamnion with a rich associated flora and fauna, which partly covers the rocks themselves. Further off at sea, the spheres of the dead alga with its commensals are cimented together by sedimentation. The spheres are further broken up and become an integrating part of the sand. The results of the physical and chemical analyses of the sand bottoms are shown in tables 2 and 3. The coast is either of abrupt rocky walls falling down to sea level, or of shores, made of pebbles or of sand. Anyhow, there are frequently Lithothamnion terraces slightly inclinated towards the bottom (chemical analysis table 1).
Resumo:
From the Jaseur Bank, off the Brazilian coast at 20º 30' S - 35º 50' W, were collected a few specimens of one of the less known species of the Heteropoda: Firoloida lesueuri (d'Orbigny). A detailed anatomical description follows aiming at the elucidation of some obscure points in the litterature on the subject and at showing the identity of most of the previously described "species" of the genus Firoloida. Special care was taken with the study of the nervous system of which most of the descriptions found were discordant. The author arrived at the conclusion that the pleural ganglia are either missing of fused to the cerebral ganglia, that the supraintestinal ganglion (left parietal ganglion) is present in the posterior region and is close to the subintestinal or right parietal ganglion, being both located near the rear end of the body. The innervations are described and discussed as well as the fusion of extensive tracts of the connectives. The present material is shown to be identical to F. kowalewskyi, well described by Vayssière and Tesch; F. desmaresti (Lesueur 1817) is shown to be undistinguishable from F. blainvilleana and F. gracilis. F. aculeata and F. gaimardi are here considered as "nomina nuda". F. liguriae Issel 1907 is admitted as separate species in spite of its insufficient description and, finally, F. vigilans (Troschel 1855), unsatisfactorily described from only one specimen is perhaps a valid species. A table is presented to show the slight differences between the 4 species which are undoubtedly very similar. F. desmaresti is found only in the Atlantic north of the line and a few points south and close to it as well as in dependent seas, while F. lesueuri is common to the south Atlantic, south Indie and south Pacific oceans, extending north only up to the Azores Islands. F. liguriae is from the south western Atlantic. ?F. vigilans would be an endemic species from Messina (Mediterranean).
Resumo:
In May 1950 a trip was undertaken by the ships "Baependi" and "Vega" to the Trindade Island - 20º30'S and 29º20'W - Approximately 1200 km off the coast of Espirito Santo State. This scientific expedition was realized by the iniciative of the Minister J. A. Lins de Barros. In this expedition the supervisor of the oceanographic works was Prof. W. Besnard, the director of the São Paulo Oceanographic Institute. He brougth home 42 samples of water for study, collected upon the insular terrace of the island, referring to the 15 established stations - see table I - with depths varying between 0 m and 115 m. The physical and chemical properties of them are to be seen on table II. The results obtained were compared with those of the German Expedition to the South Atlantic, 1925/27 ("Meteor"), observed at the stations 157-158-159-163 of profile VI and 168-169-170 of profile VII. The mean results obtaneid by the boats "Baependi" and "Vega" are represented on table IV. We constructed vertical sections - I to VI - of each group of Stations, showing the slope of the insular shelves and, in a general manner, the distribution of salinity. We made also longitudinal section - E, M, I - involving the island and corresponding, respectively, to the groups of stations, the farthest, nearest and intermediary ones. As the number of samples received is reduced and consequently the data obtained are few, no conclusions could be deduced. We made only a commentary supposing that the predominating waters surrounding the island are the same as those coming from the mentioned stations on Profile VI, marked by the "Meteor". No indication authorizes the supposition that waters of the Brazil Current or those of Profile VII of the "Meteor" reach the Trindade Island. On the contrary, its waters must be warm and salted to which Albert Defant (Die Troposphaere, Wiss. Erg. D. Atl. Exp. "Meteor" Band VI, 1 Tel Lief. 3, Berlin, 1936) has referred, as the island is located very near to the limits of the perspective diagram of warm water circulation pointed out. (Kieler Meeresforschungen, Inst. Meereskunde, Universit. Kiel, Band VII, Heft 1, S 24, 1950).