967 resultados para Regimes de Tempo
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This article seeks to explain how and why groups and networks of undocumented migrants mobilizing in Berlin, Montréal, and Paris since the beginning of the 2000s construct different types of claims. The authors explore the relationship between undocumented migrants and state authorities at the local level through the concept of the citizenship regime and its specific application to undocumented migrants (which they describe as the “borderline citizenship regime”). Despite their common formal exclusion from citizenship, nonstatus migrants experience different degrees and forms of exclusion in their daily lives, in terms of access to certain rights and services, recognition, and belonging within the state (whether through formally or nonformally recognized means). As a result, they have an opportunity to create different, specific forms of leeway in the society in which they live. The concurrence of these different degrees of exclusion and different forms of leeway defines specific conditions of mobilization. The authors demonstrate how the content of their claims is influenced by these conditions of mobilization.
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Soil organic matter (SOM) vitally impacts all soil functions and plays a key role in the global carbon (C) cycle. More than 70% of the terrestric C stocks that participate in the active C cycle are stored in the soil. Therefore, quantitative knowledge of the rates of C incorporation into SOM fractions of different residence time is crucial to understand and predict the sequestration and stabilization of soil organic carbon (SOC). Consequently, there is a need of fractionation procedures that are capable of isolating functionally SOM fractions, i.e. fractions that are defined by their stability. The literature generally refers to three main mechanisms of SOM stabilization: protection of SOM from decomposition by (i) its structural composition, i.e. recalcitrance, (ii) spatial inaccessibility and/or (iii) interaction with soil minerals and metal ions. One of the difficulties in developing fractionation procedures for the isolation of functional SOM fractions is the marked heterogeneity of the soil environment with its various stabilization mechanisms – often several mechanisms operating simultaneously – in soils and soil horizons of different texture and mineralogy. The overall objective of the present thesis was to evaluate present fractionation techniques and to get a better understanding of the factors of SOM sequestration and stabilization. The first part of this study is attended to the structural composition of SOM. Using 13C cross-polarization magic-angle spinning (CPMAS) nuclear magnetic resonance (NMR) spectroscopy, (i) the effect of land use on SOM composition was investigated and (ii) examined whether SOM composition contributes to the different stability of SOM in density and aggregate fractions. The second part of the present work deals with the mineral-associated SOM fraction. The aim was (iii) to evaluate the suitability of chemical fractionation procedures used in the literature for the isolation of stable SOM pools (stepwise hydrolysis, treatments using oxidizing agents like Na2S2O8, H2O2, and NaOCl as well as demineralization of the residue obtained by the NaOCl treatment using HF (NaOCl+HF)) by pool sizes, 13C and 14C data. Further, (iv) the isolated SOM fractions were compared to the inert organic matter (IOM) pool obtained for the investigated soils using the Rothamsted Carbon Model and isotope data in order to see whether the tested chemical fractionation methods produce SOM fractions capable to represent this pool. Besides chemical fractionation, (v) the suitability of thermal oxidation at different temperatures for obtaining stable SOC pools was evaluated. Finally, (vi) the short-term aggregate dynamics and the factors that impact macroaggregate formation and C stabilization were investigated by means of an incubation study using treatments with and without application of 15N labeled maize straw of different degradability (leaves and coarse roots). All treatments were conducted with and without the addition of fungicide. Two study sites with different soil properties and land managements were chosen for these investigations. The first one, located at Rotthalmünster, is a Stagnic Luvisol (silty loam) under different land use regimes. The Ah horizons of a spruce forest and continuous grassland and the Ap and E horizons of two plots with arable crops (continuous maize and wheat cropping) were examined. The soil of the second study site, located at Halle, is a Haplic Phaeozem (loamy sand) where the Ap horizons of two plots with arable crops (continuous maize and rye cropping) were investigated. Both study sites had a C3-/C4-vegetational change on the maize plot for the purpose of tracing the incorporation of the younger, maize-derived C into different SOM fractions and the calculation of apparent C turnover times of these. The Halle site is located near a train station and industrial areas, which caused a contamination with high amounts of fossil C. The investigation of aggregate and density fractions by 13C CPMAS NMR spectroscopy revealed that density fractionation isolated SOM fractions of different composition. The consumption of a considerable part (10–20%) of the easily available O-alkyl-C and the selective preservation of the more recalcitrant alkyl-C when passing from litter to the different particulate organic matter (POM) fractions suggest that density fractionation was able to isolate SOM fractions with different degrees of decomposition. The spectra of the aggregate fractions resembled those of the mineral-associated SOM fraction obtained by density fractionation and no considerable differences were observed between aggregate size classes. Comparison of plant litter, density and aggregate size fractions from soil under different land use showed that the type of land use markedly influenced the composition of SOM. While SOM of the acid forest soil was characterized by a large content (> 50%) of POM, which contained high amounts of spruce-litter derived alkyl-C, the organic matter in the biologically more active grassland and arable soils was dominated by mineral-associated SOM (> 95%). This SOM fraction comprised greater proportions of aryl- and carbonyl-C and is considered to contain a higher amount of microbially-derived organic substances. Land use can alter both, structure and stability of SOM fractions. All applied chemical treatments induced considerable SOC losses (> 70–95% of mineral-associated SOM) in the investigated soils. The proportion of residual C after chemical fractionation was largest in the arable Ap and E horizons and increased with decreasing C content in the initial SOC after stepwise hydrolysis as well as after the oxidative treatments with H2O2 and Na2S2O8. This can be expected for a functional stable pool of SOM, because it is assumed that the more easily available part of SOC is consumed first if C inputs decrease. All chemical treatments led to a preferential loss of the younger, maize-derived SOC, but this was most pronounced after the treatments with Na2S2O8 and H2O2. After all chemical fractionations, the mean 14C ages of SOC were higher than in the mineral-associated SOM fraction for both study sites and increased in the order: NaOCl < NaOCl+HF ≤ stepwise hydrolysis << H2O2 ≈ Na2S2O8. The results suggest that all treatments were capable of isolating a more stable SOM fraction, but the treatments with H2O2 and Na2S2O8 were the most efficient ones. However, none of the chemical fractionation methods was able to fit the IOM pool calculated using the Rothamsted Carbon Model and isotope data. In the evaluation of thermal oxidation for obtaining stable C fractions, SOC losses increased with temperature from 24–48% (200°C) to 100% (500°C). In the Halle maize Ap horizon, losses of the young, maize-derived C were considerably higher than losses of the older C3-derived C, leading to an increase in the apparent C turnover time from 220 years in mineral-associated SOC to 1158 years after thermal oxidation at 300°C. Most likely, the preferential loss of maize-derived C in the Halle soil was caused by the presence of the high amounts of fossil C mentioned above, which make up a relatively large thermally stable C3-C pool in this soil. This agrees with lower overall SOC losses for the Halle Ap horizon compared to the Rotthalmünster Ap horizon. In the Rotthalmünster soil only slightly more maize-derived than C3-derived SOC was removed by thermal oxidation. Apparent C turnover times increased slightly from 58 years in mineral-associated SOC to 77 years after thermal oxidation at 300°C in the Rotthalmünster Ap and from 151 to 247 years in the Rotthalmünster E horizon. This led to the conclusion that thermal oxidation of SOM was not capable of isolating SOM fractions of considerably higher stability. The incubation experiment showed that macroaggregates develop rapidly after the addition of easily available plant residues. Within the first four weeks of incubation, the maximum aggregation was reached in all treatments without addition of fungicide. The formation of water-stable macroaggregates was related to the size of the microbial biomass pool and its activity. Furthermore, fungi were found to be crucial for the development of soil macroaggregates as the formation of water-stable macroaggregates was significantly delayed in the fungicide treated soils. The C concentration in the obtained aggregate fractions decreased with decreasing aggregate size class, which is in line with the aggregate hierarchy postulated by several authors for soils with SOM as the major binding agent. Macroaggregation involved incorporation of large amounts maize-derived organic matter, but macroaggregates did not play the most important role in the stabilization of maize-derived SOM, because of their relatively low amount (less than 10% of the soil mass). Furthermore, the maize-derived organic matter was quickly incorporated into all aggregate size classes. The microaggregate fraction stored the largest quantities of maize-derived C and N – up to 70% of the residual maize-C and -N were stored in this fraction.
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In the course of the ‘Livestock Revolution’, extension and intensification of, among others, ruminant livestock production systems are current phenomena, with all their positive and negative side effects. Manure, one of the inevitable secondary products of livestock rearing, is a valuable source of plant nutrients and its skillful recycling to the soil-plant interface is essential for soil fertility, nutrient - and especially phosphorus - uses efficiency and the preservation or re-establishment of environmentally sustainable farming systems, for which organic farming systems are exemplarily. Against this background, the PhD research project presented here, which was embedded in the DFG-funded Research Training Group 1397 ‘Regulation of soil organic matter and nutrient turnover in organic agriculture ’ investigated possibilities to manipulate the diets of water buffalo (Bubalus bubalis L.) so as to produce manure of desired quality for organic vegetable production, without affecting the productivity of the animals used. Consisting of two major parts, the first study (chapter 2) tested the effects of diets differing in their ratios of carbon (C) to nitrogen (N) and of structural to non-structural carbohydrates on the quality of buffalo manure under subtropical conditions in Sohar, Sultanate of Oman. To this end, two trials were conducted with twelve water buffalo heifers each, using a full Latin Square design. One control and four tests diets were examined during three subsequent 7 day experimental periods preceded each by 21 days adaptation. Diets consisted of varying proportions of Rhodes grass hay, soybean meal, wheat bran, maize, dates, and a commercial concentrate to achieve a (1) high C/N and high NDF (neutral detergent fibre)/SC (soluble carbohydrate) ratio (HH), (2) low C/N and low NDF/SC ratio (LL); (3) high C/N and low NDF/SC ratio (HL) and (4) low C/N and high NDF/SC (LH) ratio. Effects of these diets, which were offered at 1.45 times maintenance requirements of metabolizable energy, and of individual diet characteristics, respectively, on the amount and quality of faeces excreted were determined and statistically analysed. The faeces produced from diets HH and LL were further tested in a companion PhD study (Mr. K. Siegfried) concerning their nutrient release in field experiments with radish and cabbage. The second study (chapter 3) focused on the effects of the above-described experimental diets on the rate of passage of feed particles through the gastrointestinal tract of four randomly chosen animals per treatment. To this end, an oral pulse dose of 683 mg fibre particles per kg live weight marked with Ytterbium (Yb; 14.5 mg Yb g-1 organic matter) was dosed at the start of the 7 day experimental period which followed 21 days of adaptation. During the first two days a sample for Yb determination was kept from each faecal excretion, during days 3 – 7 faecal samples were kept from the first morning and the first evening defecation only. Particle passage was modelled using a one-compartment age-dependent Gamma-2 model. In both studies individual feed intake and faecal excretion were quantified throughout the experimental periods and representative samples of feeds and faeces were subjected to proximate analysis following standard protocols. In the first study the organic matter (OM) intake and excretion of LL and LH buffaloes were significantly lower than of HH and HL animals, respectively. Digestibility of N was highest in LH (88%) and lowest in HH (74%). While NDF digestibility was also highest in LH (85%) it was lowest in LL (78%). Faecal N concentration was positively correlated (P≤0.001) with N intake, and was significantly higher in faeces excreted by LL than by HH animals. Concentrations of fibre and starch in faecal OM were positively affected by the respective dietary concentrations, with NDF being highest in HH (77%) and lowest in LL (63%). The faecal C/N ratio was positively related (P≤0.001) to NDF intake; C/N ratios were 12 and 7 for HH and LL (P≤0.001), while values for HL and LH were 11.5 and 10.6 (P>0.05). The results from the second study showed that dietary N concentration was positively affecting faecal N concentration (P≤0.001), while there was a negative correlation with the faecal concentration of NDF (P≤0.05) and the faecal ratios of NDF/N and C/N (P≤0.001). Particle passage through the mixing compartment was lower (P≤0.05) for HL (0.033 h-1) than for LL (0.043 h-1) animals, while values of 0.034 h-1 and 0.038 h-1 were obtained for groups LH and HH. At 55.4 h, total tract mean retention time was significantly (P≤0.05) lower in group LL that in all other groups where these values varied between 71 h (HH) and 79 h (HL); this was probably due to the high dietary N concentration of diet LL which was negatively correlated with time of first marker appearance in faeces (r= 0.84, P≤0.001), while the dietary C concentration was negatively correlated with particle passage through the mixing compartment (r= 0.57, P≤0.05). The results suggest that manure quality of river buffalo heifers can be considerably influenced by diet composition. Despite the reportedly high fibre digestion capacity of buffalo, digestive processes did not suppress the expression of diet characteristics in the faeces. This is important when aiming at producing a specific manure quality for fertilization purposes in (organic) crop cultivation. Although there was a strong correlation between the ingestion and the faecal excretion of nitrogen, the correlation between diet and faecal C/N ratio was weak. To impact on manure mineralization, the dietary NDF and N concentrations seem to be the key control points, but modulating effects are achieved by the inclusion of starch into the diet. Within the boundaries defined by the animals’ metabolic and (re)productive requirements for energy and nutrients, diet formulation may thus take into account the abiotically and biotically determined manure turnover processes in the soil and the nutrient requirements of the crops to which the manure is applied, so as to increase nutrient use efficiency along the continuum of the feed, the animal, the soil and the crop in (organic) farming systems.
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La monografía presenta la auto-organización sociopolítica como la mejor manera de lograr patrones organizados en los sistemas sociales humanos, dada su naturaleza compleja y la imposibilidad de las tareas computacionales de los regímenes políticos clásico, debido a que operan con control jerárquico, el cual ha demostrado no ser óptimo en la producción de orden en los sistemas sociales humanos. En la monografía se extrapola la teoría de la auto-organización en los sistemas biológicos a las dinámicas sociopolíticas humanas, buscando maneras óptimas de organizarlas, y se afirma que redes complejas anárquicas son la estructura emergente de la auto-organización sociopolítica.
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We examine the long-run relationship between the parallel and the official exchange rate in Colombia over two regimes; a crawling peg period and a more flexible crawling band one. The short-run adjustment process of the parallel rate is examined both in a linear and a nonlinear context. We find that the change from the crawling peg to the crawling band regime did not affect the long-run relationship between the official and parallel exchange rates, but altered the short-run dynamics. Non-linear adjustment seems appropriate for the first period, mainly due to strict foreign controls that cause distortions in the transition back to equilibrium once disequilibrium occurs
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En la Universidad de Santiago se han realizado dos estudios con el objetivo de clarificar los aspectos más importantes relacionados con el ocio infantil y para conocer las prácticas de ocio y empleo del tiempo libre en niños adolescentes de la Comunidad Autónoma de Galicia. Se realizó el estudio sobre 1066 sujetos, de los cuales de entre 6 y 14 años pertenecientes a centros estatales y de iniciativa social. Los instrumentos utilizados para le recogida de datos fueron dos cuestionarios. Uno para niños con edades comprendidas entre 6 y 9 años, y otro para niños de 10 a 14 años. Para el tratamiento de la información se aplicaron diversas técnicas estadísticas y se utilizó el programa 'BMDP'. Los resultados obtenidos fueron que para el 66 por ciento de los niños entre 6 y 9 años, su tiempo libre se lo dedican a estar con los amigos, mientras que para los niños de 10 y 14 años es solo el 25 por ciento. Ellos, prefieren deporte y cine, y entre ellos, los niños disponen de más tiempo libre que las chicas. Sin embargo, los niños entre 10 y 14 años están más satisfechos, y dentro de este grupo más los chicos que las chicas, que los de 6 a 9 años. Este estudio se ha complementado con el realizado por García Señorán en 1900. En definitiva, se hace necesaria una planificación del tiempo libre desde la infancia, utilizando sus intereses por la actividades y potenciando las actividades motoras y creativas que ayuden a su desarrollo personal. Por tanto, la escuela debe de abrir todas las posibles vías para su desarrollo integral, a través de actividades y actuaciones acordes con sus propias motivaciones y experiencias.
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Este artículo se encuentra en el monográfico: La educación en el siglo XX
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O maior rendimento num efectivo de bovinos de carne são os vitelos. O cruzamento de Bos indicus com Bos taurus tem vindo a ser praticado em vários Países como os EUA e o Brasil. A descendência daqui resultante mostra vantagens em relação às raças puras, desde a sua criação, que exige poucos custos, até ao maior lucro proveniente da sua venda. Assim, torna-se interessante explorar esta prática em Portugal onde o custo de produção é significativamente mais alto. A fim de evitar perdas de tempo na detecção de cio e permitir a aplicação de Inseminação Artificial a Tempo Fixo, hoje em dia são frequentemente utilizados protocolos de sincronização de cio e ovulação. Este trabalho teve como objectivo avaliar a influência da gonadotrofina coriónica equina, associada a uma progesterona e prostaglandina na sincronização do estro e da ovulação, sobre a taxa de sincronização e fertilização em vacas de carne Mertolengas (Bos taurus) IATF com sémen de touro de Brahman (Bos indicus). Foram seleccionadas 20 vacas Mertolengas cíclicas e com uma condição corporal entre 2 e 3,5 (escala de 1 a 5, Houghton et al., 1990). No dia 0 foi implantado a todos os animais um implante intravaginal de progesterona (CIDR®; 1,9g; Pfizer). No dia 8 administrou-se prostanglandina F2α (Dinolytic®; 5ml; IM; Pfizer). No dia 9 foi aplicada Gonadotrofina Coriónica (Intergonan® 6000UI; IM; Intervet) e o CIDR® (Pfizer) foi retirado. No dia 11 de tratamento, em horário pré-estabelecido, 48horas após a injecção de eCG foi realizada inseminaçao artificial de todos os animais com sémen de touro Brahman. A sincronização de cio neste estudo teve uma taxa de sucesso de 90% (18/20) e uma taxa de concepção de 40% (8/20). Com o cruzamento destas duas raças é esperado criar uma descendência capaz de produzir vitelos de boa qualidade e com o menor custo possível.
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Nosso objetivo neste trabalho foi expor e defender a relevância da história da educação do tempo presente para a pesquisa histórico-educacional. Partimos dos alicerces da história do tempo presente, destacando alguns conceitos construtores desse campo oriundos de autores como Rémond, François e Chartier (1996). A seguir, trabalhamos os avanços e os desafios enfrentados pelos pesquisadores desse campo. As fontes disponíveis para as pesquisa da história da educação do tempo presente foram destacadas, argumentando que a abundância delas e a proximidades do pesquisador em relação ao tempo da sua ação não facilitam a pesquisa e não diminuem sua necessária rigorosidade. Os alicerces da história do tempo presente, os desafios, os avanços, suas fontes abundantes e sua aplicação rigorosa constroem uma nova epistemologia para a história da educação, marcada pelas incertezas que referenciam a centralidade da problematização na pesquisa histórica. Toda essa argumentação é reforçada pela idéia originária de que a educação, como uma prática social, exige de seus pesquisadores a consecução dos depoimentos orais, das informações e de todos os tipos de documentação oriundas dos sujeitos que a fizeram/fazem.
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H. pylori é um microrganismo responsável por gastrites e implicado, em associação com outros factores, na úlcera gastroduodenal e no cancro gástrico. O diagnóstico da infecção por microrganismo pode realizar-se recorrendo a métodos invasivos através da obtenção de uma biópsia gástrica obtida por endoscopia digestiva alta e a métodos não invasivos. Nenhum dos métodos, desenvolvido até hoje, constitui o método ideal. Todos eles possuem as suas vantagens e desvantagens consoante a situação em que são aplicados. A reacção de polimerização em cadeia (PCR) conduziu a uma modificação fundamental no campo da biologia molecular, abrindo novos horizontes nas ciências médicas e biológicas. Apesar da cultura de H. pylori a partir de biópsia gástrica continuar a ser o método de referência para o diagnóstico da infecção por esta bactéria, ela apresenta inconvenientes que podem ser ultrapassados pela utilização da PCR, como sejam o longo período para a obtenção de resultados e o respeito de condições estritas de transporte da biópsia gástrica. Recentemente foi desenvolvido um protocolo baseado no principio da PCR em tempo real, utilizando o aparelho LightCycler Roche Diagnostics. Este protocolo permite a obtenção de um resultado de detecção da presença de H. pylori na biópsia gástrica assim como do seu perfil de susceptibilidade aos macrólidos. A PCR em tempo real é dotada de uma grande sensibilidade e especificidade, rapidez de obtenção de resultados o que aliado à sua capacidade de detecção de mutações responsáveis pela resistência dos microrganismos aos antibióticos faz com que esta técnica seja a metodologia do futuro no diagnóstico das doenças infecciosas.