803 resultados para San Juan province
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Incluye Bibliografía
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Editorial .-- Discusión abierta: Nexo Agua, Energía y Alimentación. Conflictos por el agua en la región. Eficiencia energética y regulación. Políticas e institucionalidad en agua potable. Impactos y vulnerabilidad al cambio climático de los ríos de Mendoza y San Juan .-- Reuniones: − Políticas de Agua en el Contexto de la Agenda de Desarrollo Post-2015. Consulta Regional sobre Seguridad Hídrica. Latinosan 2016. -- Noticias de la Red: Bolivia: Ley de la Década del Riego. Chile: Política Nacional de Recursos Hídricos. Costa Rica: Comité Nacional de Hidrología y Meteorología. Honduras: Comisión Presidencial de Coordinación del Sector Agua. Perú: Decreto que Regula el Régimen de Monitoreo y Gestión de Aguas Subterráneas. -- Cursos: Tópicos Técnicos en Materia de Evacuación y Disposición de Aguas Servidas Rurales.
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Pós-graduação em Agronomia (Energia na Agricultura) - FCA
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A pesca de curral é uma das artes de pesca mais tradicionais e produtivas da costa paraense e com uma produção que chega a representar 10% da produção pesqueira do Nordeste paraense (Santos et al., 2005). Sua produtividade depende tanto do modo como o curral é feito quanto do local onde é instalado. Para a realização desse trabalho, 12 currais de pesca foram selecionados em relação ao tipo (coração, enfia e cachimbo), ao local de instalação (“de beira” ou “de fora”) e ao tipo de ambiente em que se encontra (beira de rio, beira de praia e banco de areia), foram georreferenciados e tiveram sua produtividade pesqueira acompanhada durante o período de safra (junho, julho e agosto) de 2012. Na comunidade de São João de Ramos, foram monitorados 3 currais de beira do tipo coração, instalados as margens do rio Paruipema, e 3 currais de fora do tipo enfia, instalados em bancos de areia nas praias do rato e do marinheiro. Na comunidade do Aê, foram monitorados os 6 currais classificados como currais de beira, sendo 3 do tipo coração e 3 do tipo cachimbo, e todos se encontravam instalados na praia Ponta de Itaipu. Foram capturados 4.274 indivíduos, distribuídos em 9 ordens, 20 famílias e 43 espécies de peixes. A ordem Perciformes foi a que apresentou o maior número de famílias (10 famílias ou 50% do total), o maior número de espécies (19 ou 44%) e o maior número de indivíduos (3.190 ou 75% do total). As famílias Sciaenidae e Ariidae são as mais abundantes na região tanto em número de espécies quanto em indivíduos. A família Sciaenidae foi a que apresentou o maior número de indivíduos (2.855 ou 67%), mas apresentou menos espécies (8 ou 19%) que a família Ariidae, com 10 espécies ou 23% do total. Das 43 espécies capturadas, as quatro mais representadas foram: Macrodon ancylodon (51%), Arius couma (9%), Cynoscion virescens (9%) e Mugil incilis (4%). A comparação da captura entre os currais e localidades ao longo dos meses de monitoramento indicou que a produção total dos currais diferiu entre os tipos de currais associados com sua localidade.
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O Batólito Guaporeí é um corpo de aproximadamente 240 km2 alongado segundo a direção NW, localizado na região de Vila Bela da Santíssima Trindade, estado de Mato Grosso. Situa-se nos domínios da Província Rondoniana-San Ignácio, no Terreno Paraguá, na porção meridional do Cráton Amazônico. É formado por monzogranitos e, subordinadamente, granodioritos, quartzo-monzonitos e sienogranitos, caracterizados por granulação grossa e textura, em geral, porfirítica a porfiroclástica. Possui biotita como mineral máfico primário, por vezes, associada a anfibólio, e encontra-se metamorfizado na fácies xisto verde, exibindo estrutura milonítica, em estreitas zonas de cisalhamento. Evidências geoquímicas indicam que essas rochas derivam de um magma cálcio-alcalino de alto potássio a shoshonítico, metaluminoso a levemente peraluminoso evoluído por cristalização fracionada associada à assimilação crustal, possivelmente gerado em ambiente de arco continental. Duas fases de deformação relacionadas à Orogenia San Ignácio, caracterizadas pelo estiramento e alinhamento mineral evidenciadas pelas foliações S1 e S2, foram identificadas nestas rochas. Foi obtida pelo método de evaporação de Pb em zircão uma idade de 1.314 ± 3 Ma, interpretada como idade de cristalização do corpo granítico. Dados Sm-Nd em rocha total indicam idade modelo TDM em torno de 1,7 Ga e valor negativo para εNd (t = 1,3) (-14), corroborando a hipótese de envolvimento crustal na gênese do magma. Os resultados obtidos apontam semelhanças entre essas rochas e aquelas de região adjacente em território boliviano, sugerindo que o Granito Guaporeí representa uma extensão do Complexo Granitoide Pensamiento.
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The objective of this work was to evaluate the energy and economic efficiency indexes per unit of cotton agro-ecosystem area in family production systems of Paraguay and Brazil; and, to establish a relationship between the energy and economic. Typologies presented by the Program to Support Small Cotton Holdings (Paraguay), and by the National Program for Strengthening Family Agriculture (Brazil). Family systems of the two countries were identified; these are located from Paraguay (San Juan–CA) and from Brazil (Leme–SP). To construct the energy expenditure structure of the cotton agro-ecosystem, as well as to assess the economic efficiency, the mean values obtained were considered, when they presented similarities in production systems and they were within the typology proposed in this study. From the technical itinerary observed the Paraguayan agro-ecosystem depended (fossil fuel 56.76%) and industrial source (35.99%). Thus, the energy balance of the agricultural stage was established, which attained a value of 17,740.69 MJ ha-1; an energy efficiency of 5.28, and a cultural efficiency of 3.04. The Brazilian agro-ecosystem depended on energy from industrial source (insecticides 39.82%) and from fossil fuel (33.59%); it reached an energy balance of 19,547.88 MJ ha-1; an energy efficiency of 2.12, and a cultural efficiency index of 0.71. In the economic and energy indicator ratio, with regard to the months referring to the harvest time, that is to say, March, April, and May, the maximum economic efficiency indicator of paraguay was attained in the month of May (1,00), and from Brazil in the month of May (1,71). Both production systems analyzed were presented efficient, however, dependent of external circumstances and non-renewable energy sources.
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The objective of this work was to evaluate the energy and economic efficiency indexes per unit of cotton agro-ecosystem area in family production systems of Paraguay and Brazil; and, to establish a relationship between the energy and economic. Typologies presented by the Program to Support Small Cotton Holdings (Paraguay), and by the National Program for Strengthening Family Agriculture (Brazil). Family systems of the two countries were identified; these are located from Paraguay (San Juan–CA) and from Brazil (Leme–SP). To construct the energy expenditure structure of the cotton agro-ecosystem, as well as to assess the economic efficiency, the mean values obtained were considered, when they presented similarities in production systems and they were within the typology proposed in this study. From the technical itinerary observed the Paraguayan agro-ecosystem depended (fossil fuel 56.76%) and industrial source (35.99%). Thus, the energy balance of the agricultural stage was established, which attained a value of 17,740.69 MJ ha-1; an energy efficiency of 5.28, and a cultural efficiency of 3.04. The Brazilian agro-ecosystem depended on energy from industrial source (insecticides 39.82%) and from fossil fuel (33.59%); it reached an energy balance of 19,547.88 MJ ha-1; an energy efficiency of 2.12, and a cultural efficiency index of 0.71. In the economic and energy indicator ratio, with regard to the months referring to the harvest time, that is to say, March, April, and May, the maximum economic efficiency indicator of paraguay was attained in the month of May (1,00), and from Brazil in the month of May (1,71). Both production systems analyzed were presented efficient, however, dependent of external circumstances and non-renewable energy sources.
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Homalometron elongatum is reexamined using heat-killed material that was not subjected to pressure during fixation from Gerres cinereus collected from San Juan Harbor, Puerto Rico, U.S.A. The new material is compared with some paratype specimens and differs by having a much less variable forebody length, and a median rather than submedian genital pore. Tegumental spines reportedly cover the anterior end of the body but we observed tegumental spines covering the entire body surface in both the paratype and new material. Homalometron lesliorum n. sp. is described from Eucinostomus currani from the Pacific coasts of Costa Rica and Nicaragua. The new species has three pairs of oral papillae surrounding the mouth and thus resembles three other congeners: H. elongatum, Homalometron carapevae, and Homalometron papilliferum. Homalometron lesliorum n. sp. is distinguished from the three species by having the anterior extent of the vitelline follicles at or above the base of the ventral sucker, compared with posterior to the ventral sucker at the level of the seminal vesicle (H. elongatum) or further posterior at the posterior margin of the ovary (H. carapevae and H. papilliferum). The four species are further differentiated from one another by sucker width ratio, tegumental spine size and distribution, egg size, host preference, and biogeography. Comparison of nuclear ribosomal DNA (3' end of 18S, internal transcribed spacer [ITS]1, ITS2, and 5' end of 28S) between H. elongatum and H. lesliorum n. sp. revealed one variable base (n = 162) at the 3' end of 18S, 12 variable bases (n = 476) at ITS1, 10 variable bases (n = 310) at ITS2, and 11 variable bases (n = 1,325) at the 5' end fragment of 28S. Nuclear ribosomal DNA from Homalometron pallidum and Homalometron armatum are included for further comparison with H. elongatum and H. lesliorum n. sp.
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The basement rock of the Pampean flat-slab (Sierras Pampeanas) in the Central Andes was uplifted and rotated in the Cenozoic era. The Western Sierras Pampeanas are characterised by meta-igneous rocks of Grenvillian Mesoproterozoic age and metasedimentary units metamorphosed in the Ordovician period. These rocks, known as the northern Cuyania composite terrane, were derived from Laurentia and accreted toward Western Gondwana during the Early Paleozoic. The Sierra de Umango is the westernmost range of the Western Sierras Pampeanas.This range is bounded by the Devonian sedimentary rocks of the Precordillera on the western side and Tertiary rocks from the Sierra de Maz and Sierra del Espinal on the eastern side and contains igneous and sedimentary rocks outcroppings from the Famatina System on the far eastern side. The Sierra de Umango evolved during a period of polyphase tectonic activity, including an Ordovician collisional event, a Devonian compressional deformation, Late Paleozoic and Mesozoic extensional faulting and sedimentation (Paganzo and Ischigualasto basins) and compressional deformation of the Andean foreland during the Cenozoic. A Nappe System and an important shear zone, La Puntilla-La Falda Shear Zone (PFSZ), characterise the Ordovician collisional event, which was related to the accretion of Cuyania Terrane to the proto-Andean margin of Gondwana. Three continuous deformational phases are recognised for this event: the D1 phase is distinguished by relics of 51 preserved as internal foliation within interkinematic staurolite por-phyroblasts and likely represents the progressive metamorphic stage; the D2 phase exhibits P-T conditions close to the metamorphic peak that were recorded in an 52 transposition or a mylonitic foliation and determine the main structure of Umango; and the D3 phase is described as a set of tight to recumbent folds with S3 axial plane foliation, often related to thrust faults, indicating the retrogressive metamorphic stage. The Nappe System shows a top-to-the S/SW sense direction of movement, and the PFSZ served as a right lateral ramp in the exhumation process. This structural pattern is indicative of an oblique collision, with the Cuyania Terrane subducting under the proto-Andean margin of Gondwana in the NE direction. This continental subduction and exhumation lasted at least 30 million years, nearly the entire Ordovician period, and produced metamorphic conditions of upper amphibolite-to-granulite facies in medium- to high-pressure regimes. At least two later events deformed the earlier structures: D4 and D5 deformational phases. The D4 deformational phase corresponds to upright folding, with wavelengths of approximately 10 km and a general N-S orientation. These folds modified the S2 surface in an approximately cylindrical manner and are associated with exposed, discrete shear zones in the Silurian Guandacolinos Granite. The cylindrical pattern and subhorizontal axis of the D4 folds indicates that the S2 surface was originally flat-lying. The D4 folds are responsible for preserving the basement unit Juchi Orthogneiss synformal klippen. This deformation corresponds to the Chanica Tectonic during the interval between the Devonian and Carboniferous periods. The D5 deformational phase comprehends cuspate-lobate shaped open plunging folds with E W high-angle axes (D5 folds) and sub-vertical spaced cleavage. The D5 folds and related spaced cleavage deformed the previous structures and could be associated with uplifting during the Andean Cycle. (C) 2012 Elsevier Ltd. All rights reserved.
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Aims. We study galaxy pair samples selected from the Sloan Digital Sky Survey (SDSS-DR7) and we perform an analysis of minor and major mergers with the aim of investigating the dependence of galaxy properties on interactions. Methods. We build a galaxy pair catalog requiring r(p) < 25 kpc h(-1) and Delta V < 350 km s(-1) within redshift z < 0.1. By visual inspection of SDSS images we remove false identifications and we classify the interactions into three categories: pairs undergoing merging, M; pairs with evident tidal features, T; and non disturbed, N. We also divide the pair sample into minor and major interactions according to the luminosity ratio of the galaxy members. We study star formation activity through colors, the 4000 angstrom break, and star formation rates. Results. We find that similar to 10% of the pairs are classified as M. These systems show an excess of young stellar populations as inferred from the D-n(4000) spectral index, colors, and star formation rates of the member galaxies, an effect which we argue is directly related to the ongoing merging process. We find similar to 30% of the pairs exhibiting tidal features (T pairs) with member galaxies showing evidence of old stellar populations. This can be associated either to the disruptive effect of some tidal interactions, or to the longer time-scale of morphological disturbance with respect to the bursts of the tidal induced star formation. Regardless of the color distribution, we find a prominent blue peak in the strongest mergers, while pairs with tidal signs under a minor merger show a strong red peak. Therefore, our results show that galaxy interactions are important in driving the evolution of galaxy bimodality. By adding stellar masses and star formation rates of the two members of the pairs, we explore the global efficiency of star formation of the pairs as a whole. We find that, at a given total stellar mass, major mergers are significantly more efficient (a factor approximate to 2) in forming new stars, with respect to both minor mergers or a control sample of non-interacting galaxies. We conclude that the characteristics of the interactions and the ratio of luminosity galaxy pair members involved in a merger are important parameters in setting galaxy properties.
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Background: Kinins, with bradykinin and des-Arg(9)-bradykinin being the most important ones, are pro-inflammatory peptides released after tissue injury including stroke. Although the actions of bradykinin are in general well characterized; it remains controversial whether the effects of bradykinin are beneficial or not. Kinin-B2 receptor activation participates in various physiological processes including hypotension, neurotransmission and neuronal differentiation. The bradykinin metabolite des-Arg(9)-bradykinin as well as Lys-des-Arg(9)-bradykinin activates the kinin-B1 receptor known to be expressed under inflammatory conditions. We have investigated the effects of kinin-B1 and B2 receptor activation on N-methyl-Daspartate (NMDA)-induced excitotoxicity measured as decreased capacity to produce synaptically evoked population spikes in the CA1 area of rat hippocampal slices. Principal Findings: Bradykinin at 10 nM and 1 mu M concentrations triggered a neuroprotective cascade via kinin-B2 receptor activation which conferred protection against NMDA-induced excitotoxicity. Recovery of population spikes induced by 10 nM bradykinin was completely abolished when the peptide was co-applied with the selective kinin-B2 receptor antagonist HOE-140. Kinin-B2 receptor activation promoted survival of hippocampal neurons via phosphatidylinositol 3-kinase, while MEK/MAPK signaling was not involved in protection against NMDA-evoked excitotoxic effects. However, 100 nM Lys-des-Arg(9)-bradykinin, a potent kinin-B1 receptor agonist, reversed bradykinin-induced population spike recovery. The inhibition of population spikes recovery was reversed by PD98059,showing that MEK/MAPK was involved in the induction of apoptosis mediated by the B1 receptor. Conclusions: Bradykinin exerted protection against NMDA-induced excitotoxicity which is reversed in the presence of a kinin-B1 receptor agonist. As bradykinin is converted to the kinin-B1 receptor metabolite des-Arg(9)-bradykinin by carboxypeptidases, present in different areas including in brain, our results provide a mechanism for the neuroprotective effect in vitro despite of the deleterious effect observed in vivo.
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[ES]El paraje de Piédrola se localiza a seis kilómetros de distancia al noroeste de la localidad de Alcázar de San Juan (Ciudad Real), en dirección al vecino municipio toledano de Quero. En este lugar se localiza uno de los yacimientos arqueológicos más importantes de la comarca, al menos en extensión y cronología. Éste toma su nombre del topónimo de la zona: Piédrola. Los trabajos arqueológicos acometidos desde 2013 en el lugar nos permiten trazar una primera aproximación a la historia de este singular paraje.
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The objective of this study is to gain a quantitative understanding of land use and land cover change (LULCC) that have occurred in a rural Nicaraguan municipality by analyzing Landsat 5 Thematic Mapper (TM) images. By comparing the potential extent of tropical dry forest (TDF) with Landsat 5 TM images, this study analyzes the loss of this forest type on a local level for the municipality of San Juan de Cinco Pinos (63.5 km2) in the Department of Chinandega. Change detection analysis shows where and how land use has changed from 1985 to the present. From 1985 to 2011, nearly 15% of the TDF in San Juan de Cinco Pinos was converted to other land uses. Of the 1434.2 ha of TDF that was present in 1985, 1223.64 ha remained in 2011. The deforestation is primarily a result of agricultural expansion and fuelwood extraction. If current rates of TDF deforestation continue, the municipality faces the prospect of losing its forest cover within the next few decades.
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This is a report on an Engineers Without Borders project located in San Juan El Espino, El Salvador. For this project, EWB Montana Tech is working to mitigate an erosion problem that is making it difficult for children to travel to school.