¿con qué deporte escolar sueñan las familias?

[ES]En este artículo se recogen las opiniones de las familias de tres centros escolares (Azkue ikastola de Lekeitio, Betiko ikastola de Leioa y Seber Altube ikastola de Gernika), pertenecientes a la Federación de Ikastolas de Bizkaia (FIB/BIE). Las opiniones recogidas están relacionadas con una manera propia de entender el deporte escolar, que se va a ver materializada en la expresión de sus sueños. Estas opiniones han sido recogidas por los coordinadores de los centros, a través de los debates que se desarrollaban en losgrupos de discusión convocados al efecto con diferentes audiencias (escolares, familias, monitores, profesores y direcciones de los centros). El proceso de investigación seguido en el seminario se centra en procesos de interpelación, interrogación, contrastación y redefinición, por lo que se ajusta a un estudio cualitativo que se centra en la construcción conjunta del conocimiento (Pérez Gómez,1994, Imbernon, 1994).

Patrimonios culturales y museos: más allá de la Historia y del Arte

Cap. 1. La reinvención del museo etnológico. Xavier Roigé i Ventura Cap. 2. La mise en patrimoine du catharisme. Enjeux de territoire, enjeux d’identité. Marie-Carmen Garcia. Cap. 3. Más allá del museo. Las activaciones económicas del patrimonio: de los parques naturales a las fiestas temáticas. Agustí Andreu i Tomàs. Cap. 4. La patrimonialización de un territorio a través de los museos etnográficos: el caso de Extremadura. Aniceto Delgado Méndez. Cap. 5. La situación de los museos, colecciones, centros de interpretación y otros equipamientos patrimoniales del Alto Pirineo catalán. Jordi Abella Pons. Cap. 6. Patrimonio, conocimiento y dinamización. Una experiencia de trabajo en el Priorat (Catalunya). Salvador Palomar. Cap. 7. Experiencias de desarrollo local en el Pirineo aragonés basadas en la valorización del patrimonio. Aurelio García Gállego. Cap. 8. Las dimensiones sociales y culturales del patrimonio edificado: una propuesta para su estudio. Iñaki Arrieta Urtizberea.

Dokumentazioa eta ondare bibliografikoaren komunikazioa

I. Biblioteka Nazionalaren ametsa (El sueño de la Biblioteca Nacional) (Joan Mari Torrealdai). II. La Biblioteca de Catalunya, una biblioteca abierta, fiable y útil a la sociedad (Kataluniako Liburutegia, liburutegi irekia, fidagarria eta gizartearentzat onuragarria) (Dolors Lamarca). III. Armiarma.com: literaturaren sarea (Armiarma.com: portal de Literatura vasca) (Mikel Elorza). IV. GureGipuzkoa.net: atzoko eta gaurko Gipuzkoa iruditan (GureGipuzkoa.net: Gipuzkoa de ayer y hoy en imágenes) (Xabier Eskisabel Sampedro). V. Badok.info: euskal kantagintzaren ataria (Badok.info: portal de la canción y música vasca) (Jon Eskisabel). VI. www.ahotsak.com: Euskal Herriko hizkerak eta ahozko ondarea. Bilketa, katalogazioa eta hedapena (Ahotsak.com: patrimonio oral y dialectológico vasco. Recopilación, catalogación y difusión) (Asier Sarasua Aranberri). VII. La edición digital de La Vanguardia y el uso de la memoria (La Vanguardia-ren edizio digitala eta memoriaren erabilpena) (Ismael Nafría). VIII. El Servicio de Documentación de la Cadena Ser: un valor añadido a la antena (Ser Kateko Dokumentazio zerbitzua, balio erantsia antenarako) (Ana Martínez Concejo). IX. Komunikabideetako informazio dokumentalaren eskaintza (Oferta de información documental en los medios de comunicación) (Alazne Aiestaran, Teresa Agirreazaldegi, Idoia Camacho, Carmen Peñafiel eta Milagros Ronco). X. La Jungla sonora irratiko musika saioaren dokumentazioaren iturriak eta baliabideak (1989-2010) (Fuentes y recursos documentales del programa musical de radio La jungla sonora, 1989-2010) (Joseba Martín). XI. La documentación al servicio de la creación audiovisual: guión y realización del documental El secreto de Urdaneta (Dokumentazioa sormenaren alde: Urdanetaren sekretua dokumentalaren gidoia eta osaketa) (Mikel Urretavizcaya Hidalgo). XII. Semantic tags: folksonomiak hobetzeko proposamena (Semantic tags: propuesta para la mejora de las folksonomías) (Egoitz González Valderrama).

Crònica legislativa del País Basc. Segon semestre de 2014. Dos sentencias y un Auto sobre el uso del euskera en las entidades locales vascas ¿no cabe que las administraciones se relacionen en euskera?

Crónica jurisprudencial y legislativa correspondiente al segundo semestre de 2014 en materia de lengua y derecho.

A Câmara Municipal do Rio de Janeiro, das invasões corsárias ao governo de Luis Vahia Monteiro (1710 a 1732): uma história de conflitos pelo uso do território colonial.

As câmaras municipais constituíram-se em um dos mais notáveis mecanismos de manutenção do vasto império ultramarino português. Originavam-se dos antigos conselhos medievais, aglutinavam os interesses das elites coloniais ao serem compostas pelos homens bons da colônia, detinham considerável poder sobre a sociedade local além de terem a liberdade de representar ao rei de Portugal seus anseios ou dificuldades. Paralelo, ao poder do senado da câmara municipal, encontravam-se as autoridades nomeadas pelo rei de Portugal: governadores coloniais. Este compartilhamento do poder na colônia gerava, muitas vezes, conflitos entre a câmara municipal e os funcionários régios. No Rio de Janeiro, setecentista, vários fatores internos e externos à colônia deterioraram as relações entre os governadores coloniais e os membros do senado.Tal situação agrava-se com as incursões corsárias francesas de 1710 e 1711 que demonstraram a fragilidade do império português que há muito deixara de ter um poder naval significativo, perdendo espaços para potências como a França, Inglaterra e Holanda. Incapaz de conter os inimigos no vasto oceano, desprovido de meios navais capazes de patrulhar os litorais de suas colônias na África, Ásia e América, em especial o do Brasil, o império português dependia cada vez mais dos recursos humanos de suas colônias para a manutenção do seu território ultramarino. A corte portuguesa sofreu duro impacto com a conquista da cidade do Rio de Janeiro por Duguay-Trouin e, ao longo dos próximos anos, procurou fortalecer o sistema defensivo de sua colônia com o envio de tropas e navios além da construção de novas fortalezas e o reaparelhamento do sistema defensivo já existente.Todo este esforço para a guerra era bancado, em sua maior parte, com recursos da própria colônia do Rio de Janeiro. Obviamente este ônus não agradava a incipiente elite mercantil que florescia na colônia resultando no fato de que a política de enclausurar o Rio de Janeiro entre muralhas e fortificações, ás custas da economia colonial, colocou em campos opostos os funcionários do rei e os membros do senado por várias vezes nas primeiras décadas do século XVIII. Surgiram inevitáveis conflitos pelo uso e posse do território urbano do Rio de Janeiro cada vez mais pontilhado por fortalezas, sulcado por extensas valas e trincheiras a impedir-lhe o crescimento urbano. Além do conflito territorial, em função da expansão da atividade mercantil desenvolvida pelos colonos, as disputas comerciais envolveram as elites locais, ávidas por lucros e impulsionadas ao comércio devido à descoberta do ouro na região das Minas, e as autoridades e comerciantes lusos, uns querendo controlar a atividade comercial que crescia em acelerado ritmo, outros querendo lucrar e disputar espaços com as elites coloniais locais. No meio destes embates encontrava-se a Câmara Municipal do Rio de Janeiro, objetivo maior desta pesquisa, a defender os interesses das elites da colônia, pois delas era representante. Era uma disputa em que, muitas vezes, seus membros pagaram com a perda da liberdade e dos seus bens frente a governadores coloniais mais intolerantes

Estado e construção ferroviária: quinze anos decisivos para a economia brasileira, 1852-1867

Esta pesquisa procura ampliar e aprofundar o entendimento sobre a participação do Estado na construção ferroviária no século XIX. Com este objetivo, partimos da análise do processo histórico de formação do Estado brasileiro, de 1822 aos anos 1850, a fim de identificar configurações e traços culturais do sistema político no qual se inserem, como prioridade de governo, as políticas públicas e, em especial, o projeto ferroviário. Consideramos que as linhas básicas da política ferroviária, no Império, foram traçadas no período 1852-1867, durante a construção de seis ferrovias pioneiras. Detectamos, ainda, razoável correlação entre o traçado dos caminhos de ferro e os já conhecidos caminhos das minas, que conduziam a zonas onde se localizavam jazigos de pedras e metais preciosos, ferro, carvão, petróleo e outros recursos minerais. Observamos que a participação do Estado na construção ferroviária, no período, desenvolveu-se em duas frentes: como empresário responsável pela construção e gestão de malhas ferroviárias e como agente de regulação de empresas privadas, nacionais e estrangeiras, privilegiadas com longa lista de subvenções e incentivos, entre os quais se destaca a garantia de juro mínimo para os capitais investidos na construção de estradas de ferro.

Charles Henry Gilbert (1859-1928), Naturalist-in-Charge: the 1906 North Pacific Expedition of the Steamer Albatross

Fishery science pioneers often faced challenges in their field work that are mostly unknown to modern biologists. Some of the travails faced by ichthyologist and, later, fishery biologist Charles Henry Gilbert (1859-1928) during his service as Naturalist-in-Charge of the North Pacific cruise ofthe U.S. Bureau of Fisheries Steamer Albatross in 1906, are described here, as are accomplishments of the cruise. The vessel left San Francisco, Calif., on 3 May 1906, just after the great San Francisco earthquake, for scientific exploration of waters of the Aleutian islands, Bering Sea, Kamchatka, Sakhalin, and Japan, returning to San Francisco in December. Because the expedition occurred just after the war between Japan and Russia of 1904-05 floating derelict mines in Japanese waters were often a menace. Major storms caused havoc in the region, and the captain of the Albatross, Lieutenant Commander LeRoy Mason Garrett (1857-1906), U.S.N., was lost at sea, apparently thrown from the vessel during a sudden storm on the return leg of the cruise. Despite such obstacles, Gilbert and the Albatross successfully completed their assigned chores. They occupied 339 dredging and 48 hydrographic stations, and discovered over 180 new species of fishes and many new species of invertebrates. The expedition's extensive biological collections spawned over 30 descriptive publications, some of which remain today as standards of knowledge.

Os limites da flexibilização e informalidade na produção e trabalho contemporâneos: imigração laboral boliviana e a indústria de vestuário de São Paulo

A migração laboral de bolivianos para São Paulo é um processo intrinsecamente relacionado aos planos de ajuste estrutural ocorridos na Bolívia e no Brasil na segunda metade dos anos 1980 e no início da década de 1990, respectivamente. Para a Bolívia, o Decreto 21.060 implicou a privatização de mineradoras e conseqüentes demissões em massa, além de uma abertura econômica que favoreceu migrações internas para as regiões cocaleiras e para as periferias das grandes cidades. Posteriormente, esses migrantes e seus familiares se destinaram a países limítrofes como Argentina e Brasil. Destaca-se nesse contexto a localidade de El Alto, origem de grande parte dos imigrantes que se destinaram a São Paulo. Do lado brasileiro, houve também uma abertura econômica que foi prejudicial a amplos setores da indústria, como a cadeia têxtil-vestuário. Para reduzir os custos de produção e aumentar sua competitividade em relação às mercadorias asiáticas, a indústria de vestuário se reestruturou defensivamente e subcontratou grande parte de sua produção material às oficinas informais que empregam imigrantes bolivianos geralmente jovens, indocumentados e com baixa qualificação profissional. Nessa pesquisa, relacionamos esse fluxo populacional às transformações estruturais ocorridas nos dois países, destacando as mudanças nas relações de trabalho decorrentes do processo de reestruturação produtiva. Também abordamos as redes de solidariedade desses imigrantes e os meios pelos quais estes vêm revertendo uma inserção na sociedade de destino em que predominam condições precárias de trabalho e habitação, além de uma instabilidade permanente decorrente da irregularidade documental que atinge grande parte desses trabalhadores.

Crocodile farming: a multi-million dollar industry

Crocodiles have a long breeding life, which ranges from 25-30 years. There are 27 species and subspecies of crocodiles throughout the world, 18 of which are in danger of extinction, the rest being threatened with declining population due to overhunting and habitat destruction. Two known crocodile species exist in the Philippines: Crocodylus mindorensis (freshwater crocodile) and C. porosus (saltwater crocodile). Killing adult crocodiles, as is being done now, drastically reduces the potential population. Moreover, toxic wastes from mines, destruction of marshes and riverine habitats, and the conversion of their natural habitats for fishponds additionally threaten their populations. Estimates indicate that there are only about 100 Philippine crocodiles in the wild now. The Crocodile Farming Institute (CFI) was established in Palawan, in 1987, in order to save the crocodiles from extinction in the Philippines. It is now one of the components of the Palawan Wildlife and Conservation Center, and aims to conserve the 2 endangered species in the Philippines and also to develop and introduce a suitable crocodile farming technology that will help uplift the socio-economic well-being of the Filipino people. CFI believes in the potential of commercial utilization of crocodiles as a dollar-generating industry for the Philippines. It is a very profitable business and could be a multi-million dollar industry. A brief outline is given of the economic and marketing potentials of farming crocodiles in the Philippines.

金川镍矿岩体移动与开采稳定性研究

The two major issues in mining industry are work safety and protection of ground environment when carrying on underground mining activities. Cut-and-fill mining method is increasingly applied in China owing to its advantages of controlling ground pressure and protecting the ground environment effectively. However, some cut-and-fill mines such as Jinchuan nickel mine which has big ore body, broken rock mass and high geostress have unique characteristics on the law of ground pressure and rock mass movement that distinguish from other mining methods. There are still many problems unknown and it is necessary for the further analysis. In this dissertation, vast field survey, geology trenching and relative data analysis are carried out. The distribution of ground fissures and the correlation of the fissures with the location of underground ore body is presented. Using of monitoring data by three-dimension fissure meter and GPS in Jinchuan Deposit Ⅱ, the rule of the surface deformation and the reason of ground fissures generation are analyzed. It is shown that the stress redistribution in surrounding rocks resulting from mining, the existence of the void space underground and the influence of on-going mining activities are three main reasons for the occurrence of ground fissures. Based on actual section planes of No.1 ore body, a large-scale 3D model is established. By this model, the complete process of excavation and filling is simulated and the law of rock mass movement and stability caused by Cut-and-fill Mining is studied. According to simulation results, it is concluded that the deformation of ground surface is still going on developing; the region of subsidence on the ground surface is similar with a circle; the area on the hanging wall side is larger than one on the lower wall side; the contour plots show the centre of subsidence lay on the hanging wall side and the position is near the ore body boundary of 1150m and 1250m where ore body is the thickest. Along strike-line of Jinchuan Deposit Ⅱ, the deformation at the middle of filling body is larger than that in the two sides. Because of the irregular ore body, stress concentrates at the boundary of ore body. With the process of excavation and filling, the high stress release and the stress focus disappear on the hanging wall side. The cut-and-fill mechanism is studied based on monitoring data and numerical simulation. The functions of filling body are discussed. In this dissertation, it is concluded that the stress of filling body is just 2MPa, but the stress of surrounding rock mass is 20MPa. We study the surface movement influenced by the elastic modulus of backfill. The minimal value of the elastic modulus of backfill which can guarantee the safety production of cut-and-fill mine is obtained. Finally, based on the real survey results of the horizontal ore layer and numerical simulation, it is indicated that the horizontal ore layer has destroyed. Key words: cut-and-filling mining, 3D numerical simulation, field monitoring, rock mass movement, cut-and-filling mechanism, the elastic modulus of backfill, the horizontal ore layer

内陆湖沼相和近海沼泽相沉积环境煤中微量元素和矿物的对比研究—以辽宁北票、江西建新和桥头煤研究为例

Using knowledge of geology, geochemistry, coal petrology, mineralogy, by means of a variety of advanced measuring methods such as inductively coupled plasma mass spectrometry (ICP-MS), inductively coupled atomic emission spectrometry (ICP-AES), X-ray powder diffraction (XRD), scanning electron microscopy with energy-dispersive spectrometer(SEM-EDS), sequential chemical extract and density fractions, the characteristics of trace elements and minerals in Jurassic Beipiao coal mine under inland limnetic sedimentary environment and in late Permian Jianxin and Qiaotou coal mines under paralic swamp sedimentary environment were studied. Compared with the average concentration in the world bituminous coals, the Beipiao coal was characterized by relatively high contents of Sc, Ti, Cr, Co, Ni, Zn, Se, Sr, Zr, Y, Ba, REE and Th, and lower contents of V, Rb, Cd, Sn, Pb, Bi and U; while the Jianxin coal was relatively enriched in Li, Sc, Ga, Sr, Y, Nb, Sb, Th and U, with low concentration of Be, Co, Ni, Cu, Ge, Zr, Mo, Cd, Cs, Ba, Pb and Bi; and the Qiaotou coal was enriched in Li, Sc, Sr, Nb, Ta, Zr, REE, Hf, Th and U, with low concentration of Be, V, Co, Ni, Cu, Ge, Mo, Cd, Cs, Ba, Tl, Pb and Bi. The concentrations of Ca, Mg and K in Beipiao coal are higher than those in Jianxin coal and Qiaotou coal, while Fe, S and Ti in Beipiao coal are lower than those in Jianxin coal and Qiaotou coal. The proximate analysis of coal samples was carried out, which indicated that Beipiao coal was medium- to high- ash (5.92-60.68%) with low sulphur coal, and Jianxin coal and Qiaotou coal was medium to high ash (8.85-46.33%) with high sulphur. The reflectivity was measured, which explained that Beipiao coal belonged to high volatile bituminous coal, Jianxin coal was low volatile bituminous coal and Qiaotou coal was low volatile anthracite. Quantitative maceral analyses were studied. The characteristics of rare earth elements (REE) were investigated, which showed that the total contents of REE were higher than that of the world's average content. With the increase of coal's metamorphic grade, the total contents of REE decreased from 98.5 X 10"6 of Beipiao coal to 94.2 X 10"6 of Jianxin coal, and to 75.9 X 10"6 of Qiaotou coal, and 5Eu reduced which indicated that the element Eu depleted. The characteristics of REE was controlled by the metamorphic grade of coal. And REE were mainly absorbed in clay minerals in Beipiao coal samples, while in Jianxin and Qiaotou coal mines, REE were primarily related to clay mineral and pyrite. The variation of trace elements in vertical direction of coal seams was studied, and the results showed that different trace elements differed greatly. The correlation between trace elements and ash were determined. Four major trace elements (aluminium-silicates, sulphide, carbonate and phosphate) accounted for the occurrence and distribution of most elements studied were determined. Coal samples were separated by density fraction, which showed that Cr, Cu, Mo and Pb were closely related to inorganic matters mainly distributed in P >2.6 and dropped remarkably in the density fractions P <2.3 . The occurrences of Co, Cr, Ni, As, Se, Mo, U were studied directly and quantitatively using sequential chemical extract with six steps, which showed that Co. Ni, Mo and U were mainly in the form of mineral, and As, Se chiefly in the form of organic state, while Cr mostly in the form of organic state and mineral. Major mineral phases presented in the Beipiao coal were Kaolinite, illite, quartz, calcite, and small amount of siderite, barite. While major mineral phases in Jianxin and Qiaotou coal were pyrite, kaolinite, and small amount of marcasite, rutile, sphalerite. This is the first time that the chromite in the coal was discovered in China, which indicates that Cr occurrence appeared in the form of chromite. The ratio of Sr/Ba, Sr/Ca and V/Ni in Beipiao coal mine under inland limnetic is smaller than that of in Jianxin and Qiaotou coal mines under paralic swamp. The ratio of K/Na and Th/U of Beipiao coal mine is higher than that of Jianxin and Qiaotou coal mine, which proved that Beipiao coal was not affected by sea water and Jianxin and Qiaotou coal were affected by sea water. Trace elements such as Cr, Ni, Mo in minerals were analyzed by SEM-EDS. The factors controlling the enrichment of trace elements can be divided into syngenetic stage factors and epigenetic stage factors.

新疆萨吾尔金矿带构造-流体地球化学及成矿作用

The Sawuer gold belt is located in the transition belt between Siberian plate and Kazakhstan-Junggar plate. Based on the geological and geochemical studies on the Kuoerzhenkuola and Buerkesidai gold deposits, in Sawuer gold mineralization belt, the time-space structure of mineralization and mineralizing factor are studied, the metallogenic regularity is concluded in thistheses. The ore bodies have the regularity that orebody are of the extensive and compressive in the sallow and depth of volcanic apparatue, respectively, and the vertical extension of orebody is more intensive than the horizontal extension. The gold deposits were controlled by the fractures of volcanic apparatus and regional faults, and featured by the hydrothermal alteration and metasomatism type disseminated mineralization and filling type vein mineralization. By virtue of the geological and geochemical studies on the two deposits that the formation of the two deposits are significantly related to the volcanic activity, we propose new ideas about their origin: (1) the two deposits are located in the same strata, and share the same genesis. (2) both of two deposits are volcanogenic late-stage hydrothermal gold deposits. Based on mapping of volcanic lithofacies and structure for the first time, it is discovered that a volcanic apparatus existed in the study area. Volcanic-intrusive activity can be divided into three cycles and nine lithofacies. where the two deposits are hosted in the same volcanic cycle, in this case, the wall-rock should belong to the same strata. The 40Ar-39Ar age method is employed in this work to analyze the fluid inclusions of quartz in the ore bodies from Kuoerzhenkuola and Buerkesidai gold deposits. The results show that the main mineralization occurred in 332.05 + 2.02-332.59 + 0.5IMa and 335.53 + 0.32Ma~336.78 + 0.50Ma for Kuoerzhenkuola and Buerkesidai gold deposits respectively, indicating that the two deposits are formed almost at the same time, and the metallogenic epoch of the tow deposits are close to those of the hosting rocks formed by volcanic activity of Sawuer gold belt. This geochronological study supplies new evidence for determining the timing of gold mineralization, the geneses of gold deposits? and identifies that in Hercynian period, the Altai developed tectonic-magmatic-hydrothermal mineralization of Early Carboniferous period, except known two metallogenic mineralization periods including tectonic-magmatic-hydrothermal mineralization of Devonian period and Late Carboniferous-Permian period respectively. The study of fluid inclusions indicates that the ore-forming fluid is a type of NaCl-HbO fluid with medium-low temperature and low salinity, Au is transported by the type of auric-sulfur complex (Au (HS)2-), the ore is formed in reduction condition. Hydrogen and oxygen isotopes of fluid inclusions in the major mineralizating stage show that the solutions mainly originated from magmatic water and meteoric water. The fluid mixing and water-rock reaction cause the deposition of Au. The helium and argon isotope compositions of fluid inclusions hosted in pyrite have been measured from Kuoerzhenkuola and Buerkesidai gold deposits in Sawuer gold belt. The results show that the ore-forming fluids of two deposits possessed the same source and is a mixture of mantle- and partial meteoric water-derived fluid, and the reliability of He and Ar isotopic compositions in Hercynian period is discussed. Isotopic studies including H, O, He, C, S, Pb and Sr reveal the same result that the ore-forming fluids of two deposits possessed the same source: the water derived mainly from magmatic water, partially from meteoric water; the mineralizers and ore materials derived mainly from mantle beneath the island arc, and partially from crust. The ore-forming fluids of two deposits are a mixture of mantle-derived fluids being incorporated by crust-derived fluid, and shallow partial meteoric water. Based on these results, it is proposed that the geneses of the two gold deposits are the same, being volcanogenic late-stage hydrothermal gold deposits that the ore-forming fluids filled in fractures of volcanic apparatus and metasomatized the host rocks in the volcanic apparatus. It is the first time we carried out the geophysical exploration, that is, the EH-4 continuous electrical conductivity image system measurement, the results show that relative large-size mineralizing anomalies in underground have been discovered.lt can confirm the law and genesis of the deposits mentioned above, and change the two abandoned mines to current large-size potenial exploration target.

Analyses of patterns of copper and lead mineralisation in human skeletons excavated from an ancient mining and smelting centre in the Jordanian desert

Grattan, J.P., Al-Saad, Z., Gilbertson, D.D., Karaki, L.O., Pyatt, F.B 2005 Analyses of patterns of copper and lead mineralisation in human skeletons excavated from an ancient mining and smelting centre in the Jordanian desert Mineralogical Magazine. 69(5) 653-666.