Estructura ocupacional de los microemprendimientos de la producción e industrialización del ajo : Mendoza, Argentina

La importancia de la cadena del ajo en Mendoza, Argentina, radica fundamentalmente en la representatividad de la superficie cultivada (82 % del total nacional), en la participación de la producción local con respecto al país (alrededor del 75 %) y en la potencialidad de abastecer mercados internacionales. Este cultivo, tanto en su fase productiva como en la de industrialización, presenta características aptas para su desarrollo en unidades de explotación pequeñas, generando alta participación de microemprendimientos en ambos subsectores funcionales de la cadena. Dicha situación determina particulares y diferenciales condiciones de inserción laboral de sus participantes en relación con el resto de los sectores de la agricultura provincial, por lo que su estudio ofrece datos de interés sobre el impacto de la actividad en las condiciones socio-económicas de la población participante. El trabajo de investigación se efectuó mediante un método combinado de estrategias cuanti y cualitativas. El primer caso se aplicó para caracterizar el sector de producción primaria, mediante una encuesta realizada a una muestra probabilística, representativa y estratificada según tamaño de la unidad productiva. La técnica cualitativa se aplicó al subsector industrializador, entrevistando a informantes clave. Dadas las posibilidades de colocación del producto en mercados internacionales y la importancia cuantitativa de la participación de microempresarios en la cadena del ajo, se puede advertir una tendencia en crecimiento en los niveles de producción y en la participación de microemprendimientos, a pesar de lo cual las unidades productivas más pequeñas no reciben los beneficios de la tendencia ascendente de la cadena, y desarrollan una estructura ocupacional que presenta indicadores de inestabilidad, fluctuación intertemporal y precariedad, con incidencia en las condiciones generales de vida de la población afectada.

Oxygen isotopes from two snow trenches from Kohnen Station, Dronning Maud Land, Antarctica from the 2012/13 field season

In low-accumulation regions, the reliability of d18O-derived temperature signals from ice cores within the Holocene is unclear, primarily due to the small climate changes relative to the intrinsic noise of the isotopic signal. In order to learn about the representativity of single ice cores and to optimise future ice-core-based climate reconstructions, we studied the stable-water isotope composition of firn at Kohnen station, Dronning Maud Land, Antarctica. Analysing d18O in two 50 m long snow trenches allowed us to create an unprecedented, two-dimensional image characterising the isotopic variations from the centimetre to the hundred-metre scale. This data set includes the complete trench oxygen isotope record together with the meta data used in the study.

Storm evolution characterization for analysing stone armour damage progression

Storm evolution is fundamental for analysing the damage progression of the different failure modes and establishing suitable protocols for maintaining and optimally sizing structures. However, this aspect has hardly been studied and practically the whole of the studies dealing with the subject adopt the Equivalent triangle storm. As against this approach, two new ones are proposed. The first is the Equivalent Triangle Magnitude Storm model (ETMS), whose base, the triangular storm duration, D, is established such that its magnitude (area describing the storm history above the reference threshold level which sets the storm condition),HT, equals the real storm magnitude. The other is the Equivalent Triangle Number of Waves Storm (ETNWS), where the base is referred in terms of the real storm's number of waves,Nz. Three approaches are used for estimating the mean period, Tm, associated to each of the sea states defining the storm evolution, which is necessary to determine the full energy flux withstood by the structure in the course of the extreme event. Two are based on the Jonswap spectrum representativity and the other uses the bivariate Gumbel copula (Hs, Tm), resulting from adjusting the storm peaks. The representativity of the approaches proposed and those defined in specialised literature are analysed by comparing the main armour layer's progressive loss of hydraulic stability caused by real storms and that relating to theoretical ones. An empirical maximum energy flux model is used for this purpose. The agreement between the empirical and theoretical results demonstrates that the representativity of the different approaches depends on the storm characteristics and point towards a need to investigate other geometrical shapes to characterise the storm evolution associated with sea states heavily influenced by swell wave components.

Storm characterization for analyzing stone armour damage progression

Storm evolution is fundamental for analysing the damage progression of the different failure modes and establishing suitable protocols for maintaining and optimally sizing structures. However, this aspect has hardly been studied and practically the whole of the studies dealing with the subject adopt the Equivalent triangle storm. As against this approach, two new ones are proposed. The first is the Equivalent Triangle Magnitude Storm model (ETMS), whose base, the triangular storm duration, D, is established such that its magnitude (area describing the storm history above the reference threshold level which sets the storm condition),HT, equals the real storm magnitude. The other is the Equivalent Triangle Number of Waves Storm (ETNWS), where the base is referred in terms of the real storm's number of waves,Nz. Three approaches are used for estimating the mean period, Tm, associated to each of the sea states defining the storm evolution, which is necessary to determine the full energy flux withstood by the structure in the course of the extreme event. Two are based on the Jonswap spectrum representativity and the other uses the bivariate Gumbel copula (Hs, Tm), resulting from adjusting the storm peaks. The representativity of the approaches proposed and those defined in specialised literature are analysed by comparing the main armour layer's progressive loss of hydraulic stability caused by real storms and that relating to theoretical ones. An empirical maximum energy flux model is used for this purpose. The agreement between the empirical and theoretical results demonstrates that the representativity of the different approaches depends on the storm characteristics and point towards a need to investigate other geometrical shapes to characterise the storm evolution associated with sea states heavily influenced by swell wave components.

Anatomofisiologia da sucção e deglutição do bebê em computação gráfica 3D como instrumento educacional

A eficiência da amamentação exige uma complexa coordenação entre sucção, deglutição e respiração, sendo que a tecnologia tem possibilitado importantes avanços na compreensão desse processo. Porém, não foram encontrados vídeos disponíveis na internet que demonstrassem a anatomia e fisiologia da amamentação, de modo didático e fidedigno à ciência atual. Este trabalho teve por objetivo descrever o desenvolvimento de uma sequência em computação gráfica sobre a sucção e a deglutição, resultante da produção digital do Bebê Virtual, bem como validar tal produção quanto ao conteúdo e prover adequações necessárias ao material educacional. Para a produção das iconografias em 3D da sucção e deglutição no Bebê Virtual, inicialmente foi elaborado um mapa conceitual e uma matriz de conteúdos, objetivos e competências voltadas ao material educacional. Posteriormente foi elaborado um roteiro científico que abordou a anatomia do crânio, face, cavidade oral, faringe, laringe e esôfago do recém-nascido, bem como, a descrição dos mecanismos fisiológicos relacionados à sucção e às fases oral e faríngea da deglutição no bebê. Para isso foram utilizadas 14 publicações do período de 1998 a 2008, que continham informações relevantes para demonstrar a amamentação. Os conteúdos teóricos foram organizados em cenas principais, possibilitando a criação de previews das sequências dinâmicas, as quais foram avaliadas por profissionais de anatomia, fonoaudiologia e medicina, possibilitando os ajustes necessários e a construção das imagens em computação gráfica 3D. Para análise da validade de conteúdo dessas imagens foi verificada a representatividade dos itens que o compõe, por meio de consulta à literatura. Foram incluídos estudos que utilizaram auxílio tecnológico e abordaram o tema proposto em bebês a termo e saudáveis, sem alterações neurológicas ou anomalias craniofaciais. Foram excluídas as publicações realizadas com bebês pré-termo, sindrômicos, com anomalias, doenças neurológicas ou qualquer alteração que pudesse interferir na amamentação, revisões de literatura e relatos de caso. Os artigos selecionados foram analisados e classificados quanto ao nível de evidência científica, predominando o nível três de evidência. A análise de conteúdo demonstrou a necessidade de adequações nas iconografias 3D, para que o processo de sucção e deglutição demonstrado no bebê virtual pudesse corresponder ao conhecimento científico atual. Tais adequações foram propostas a partir dos achados de 9 estudos, publicados entre 2008 e 2014, que utilizaram ultrassonografia para demonstrar como ocorre o processo de amamentação. Desta forma, foram modificados os aspectos da pega, da movimentação de língua, mandíbula, palato mole e laringe, além da sincronização da sucção/deglutição/respiração e deslocamento do mamilo, num processo desenvolvido em cinco etapas. Assim, o presente estudo descreveu o processo de desenvolvimento das iconografias em 3D sobre a anatomia e fisiologia da sucção e deglutição no recém-nascido a termo, sendo que a validade de conteúdo permitiu atualizar vários aspectos da amamentação do Bebê Virtual, quebrando velhos paradigmas e possibilitando ilustrar didaticamente as evidências científicas relacionadas.

Circumpolar Landscape Units, links to GeoTIFFs

Requirements for space based monitoring of permafrost features had been already defined within the IGOS Cryosphere Theme Report at the start of the IPY in 2007 (IGOS, 2007). The WMO Polar Space Task Group (PSTG, http://www.wmo.int/pages/prog/sat/pstg_en.php) identified the need to review the requirements for permafrost monitoring and to update these requirements in 2013. Relevant surveys with focus on satellite data are already available from the ESA DUE Permafrost User requirements survey (2009), the United States National Research Council (2014) and the ESA - CliC - IPA - GTN -P workshop in February 2014. These reports have been reviewed and specific needs discussed within the community and a white paper submitted to the WMO PSTG. Acquisition requirements for monitoring of especially terrain changes (incl. rock glaciers and coastal erosion) and lakes (extent, ice properties etc.) with respect to current satellite missions have been specified. About 50 locations ('cold spots') where permafrost (Arctic and Antarctic) in situ monitoring has been taking place for many years or where field stations are currently established have been identified. These sites have been proposed to the WMO Polar Space Task Group as focus areas for future monitoring by high resolution satellite data. The specifications of these sites including meta-data on site instrumentation have been published as supplement to the white paper (Bartsch et al. 2014, doi:10.1594/PANGAEA.847003). The representativity of the 'cold spots' around the arctic has been in the following assessed based on a landscape units product which has been developed as part of the FP7 project PAGE21. The ESA DUE Permafrost service has been utilized to produce a pan-arctic database (25km, 2000-2014) comprising Mean Annual Surface Temperature, Annual and summer Amplitude of Surface Temperature, Mean Summer (July-August) Surface Temperature. Surface status (frozen/unfrozen) related products have been also derived from the ESA DUE Permafrost service. This includes the length of unfrozen period, first unfrozen day and first frozen day. In addition, SAR (ENVISAT ASAR GM) statistics as well as topographic parameters have been considered. The circumpolar datasets have been assessed for their redundancy in information content. 12 distinct units could be derived. The landscape units reveal similarities between North Slope Alaska and the region from the Yamal Peninsula to the Yenisei estuary. Northern Canada is characterized by the same landscape units like western Siberia. North-eastern Canada shows similarities to the Laptev coast region. This paper presents the result of this assessment and formulates recommendations for extensions of the in situ monitoring networks and categorizes the sites by satellite data requirements (specifically Sentinels) with respect to the landscape type and related processes.

Abundância das formas imaturas de Psaroniocompsa incrustata ( Lutz, 1910) (Diptera: Simuliidae) em um criadouro natural no rio Pium/RN, e sua fauna associada

The species psaroniocompsa incrustata (Lutz, 1910) was studied in relation to its abundance in different and seasonal periods, the physico-chemical of the breending ground and the fauna predation added to the immature of the species. The study was developed during eight months, from April to July, 2005 (rainy season) and from October, 2005 to January, 2006 (drought season), in one natural breending ground situated in the Pium river, that is part of the hydrographical basin of the Pirangi river in Rio Grande do Norte. The immature of Simuliidae were collected manually in vegetal substrate. At the same place, it was made one sampling of the associated fauna using Suber collectors and the measurement of the environment variants. It was also made one analysis of the stomach content of possible enemies of the simulídeos, to observe the predation of the associated fauna. It was collected 7.713 samples, all from de species P. Incrustata, it was observed a bigger abundance in the drought season, and the entomologic fauna associated totalizing 20.1314 species, distributed in the kinds: Diptera, Ephemeroptera, Odonata, Trichoptera, e Hemiptera, with a bigger representativity of Dipteros. The analysis of the stomach content of the species from the families Libellulidae and Hydropsychidae showed the presence of the simulídeos in only 4% of the material analysed, therefore it was not confirmed the presence of one efficient biological control of the simulídeos in this breending ground

Meios de comunicação e mudanças na política : esses homens poderosos e suas máquinas de comunicar

Tese (doutorado)—Universidade de Brasília, Faculdade de Comunicação, Programa de Pós-Graduação em Comunicação, 2016.

Abundância das formas imaturas de Psaroniocompsa incrustata ( Lutz, 1910) (Diptera: Simuliidae) em um criadouro natural no rio Pium/RN, e sua fauna associada

The species psaroniocompsa incrustata (Lutz, 1910) was studied in relation to its abundance in different and seasonal periods, the physico-chemical of the breending ground and the fauna predation added to the immature of the species. The study was developed during eight months, from April to July, 2005 (rainy season) and from October, 2005 to January, 2006 (drought season), in one natural breending ground situated in the Pium river, that is part of the hydrographical basin of the Pirangi river in Rio Grande do Norte. The immature of Simuliidae were collected manually in vegetal substrate. At the same place, it was made one sampling of the associated fauna using Suber collectors and the measurement of the environment variants. It was also made one analysis of the stomach content of possible enemies of the simulídeos, to observe the predation of the associated fauna. It was collected 7.713 samples, all from de species P. Incrustata, it was observed a bigger abundance in the drought season, and the entomologic fauna associated totalizing 20.1314 species, distributed in the kinds: Diptera, Ephemeroptera, Odonata, Trichoptera, e Hemiptera, with a bigger representativity of Dipteros. The analysis of the stomach content of the species from the families Libellulidae and Hydropsychidae showed the presence of the simulídeos in only 4% of the material analysed, therefore it was not confirmed the presence of one efficient biological control of the simulídeos in this breending ground