Técnica para a observação do comportamento do Triatoma infestans (Klug, 1834) em uma miniatura de casa de pau-a-pique e sapê

Com o objetivo de observar e registrar o comportamento do Triatoma infestans quanto a movimentos, posturas e estados fisiológicos, como preconizam os etólogos, foi construída uma réplica de uma casa de paua-pique e sapê com uma proteção externa de acrílico transparente. Para o registro das atividades empregou-se a cinematografia com lapso de tempo, através de uma filmadora super-8 sincronizada a um flash eletrônico e programada para disparos simultâneos de 1 fotograma a cada 30 segundos. A análise dos dados foi feita com um projetor super-8 e um editor, que permitiu observar cada fotograma. Com um período de registros durante 6 dias ininterruptos, os resultados permitiram concluir que: a) na ausência de estímulo alimentar, não ocorre atividade locomotora no T. infestans, independente de ser dia ou noite, mesmo com o inseto privado de alimentos; b) em presençaa do estímulo alimentar a atividade locomotora ocorre durante as 24 horas do dia, embora em proporção significantemente maior no período de obscuridade.

The role of a transcrustal shear zone in orogenic gold mineralization at the Aijanahalli Mine, Dharwar Craton, South India

The Ajjanahalli gold mine is spatially associated with a Late Archean craton-scale shear zone in the eastern Chitradurga greenstone belt of the Dharwar craton, India. Gold mineralization is hosted by an similar to100-m-wide antiform in a banded iron formation. Original magnetite and siderite are replaced by a peak metamorphic alteration assemblage of chlorite, stilpnomelane, minnesotaite, sericite, ankerite, arsenopyrite, pyrite, pyrrhotite, and gold at ca. 300degrees to 350degreesC. Elements enriched in the banded iron formation include Ca, Mg, C, S, An, As, Bi. Cu, Sb, Zn, Pb, Se, Ag, and Te, whereas in the wall rocks As, Cu, Zn, Bi, Ag, and An are only slightly enriched. Strontium correlates with CaO, MgO, CO2, and As, which indicates cogenetic formation of arsenopyrite and Mg-Ca carbonates. The greater extent of alteration in the Fe-rich banded iron formation layers than in the wall rock reflects the greater reactivity of the banded iron formation layers. The ore fluids, as interpreted from their isotopic composition (delta(18)O = 6.5-8.5parts per thousand; initial Sr-87/Sr-86 = 0.7068-0.7078), formed by metamorphic devolatilization of deeper levels of the Chitradurga greenstone belt. Arsenopyrite, chalcopyrite, and pyrrhotite have delta(34)S values within a narrow range between 2.1 and 2.7 per mil, consistent with a sulfur source in Chitradurga greenstone belt lithologies. Based on spatial and temporal relationships between mineralization, local structure development, and sinistral strike-slip deformation in the shear zone at the eastern contact of the Chitradurga greenstone belt, we suggest that the Ajjanahalli gold mineralization formed by fluid infiltration into a low strain area within the first-order structure. The ore fluids were transported along this shear zone into relatively shallow crustal levels during lateral terrane accretion and a change from thrust to transcurrent tectonics. Based on this model of fluid flow, exploration should focus on similar low strain areas or potentially connected higher order splays of the first-order shear zone.

Stable hydrogen and oxygen isotope composition of waters from mine tailings in different climatic environments

The stable isotope composition of waters (delta H-2, delta O-18) can be used as a natural tracer of hydrologic processes in systems affected by acid mine drainage. We investigated the delta H-2 and delta O-18 values of pore waters from four oxidizing sulfidic mine tailings impoundments in different climatic regions of Chile (Piuquenes at La Andina with Alpine climate, Cauquenes and Caren at El Teniente with Mediterranean climate, and Talabre at the Chuquicamata deposit with hyperarid climate). No clear relationship was found between altitude and isotopic composition. The observed displacement of the tailings pore waters from the local meteoric water line toward higher delta O-18 values (by similar to +2% delta O-18 relative to delta H-2) is partly due to water-rock interaction processes, including hydration and O-isotope exchange with sulfates and Fe(III) oxyhydroxides produced by pyrite oxidation. In most tailings, from the saturated zone toward the surface, isotopically different zones can be distinguished. Zone I is characterized by an upward depletion of H-2 and O-18 in the pore waters from the saturated zone and the lowermost vadose zone, due to ascending diffused isotopically light water triggered by the constant loss of water vapor by evaporation at the surface. In zone II, the capillary flow of a mix of vapor and liquid water causes an evaporative isotopic enrichment in H-2 and O-18. At the top of the tailings in dry climate a zone III between the capillary zone and the surface contains isotopically light diffused and atmospheric water vapor. In temperate climates, the upper part of the profile is affected by recent rainfall and zone III may not differ isotopically from zone II.

De la paraula a la imatge: "Casa tomada" i Corcs

Treball de recerca realitzat per alumnes d’ensenyament secundari i guardonat amb un Premi CIRIT per fomentar l'esperit científic del Jovent l’any 2008. Adaptació del relat breu “Casa tomada” de Julio Cortázar al llenguatge cinematogràfic.

O proxecto de creto agrícola e a proposta de redención foral (1886). A resposta liberal de Montero Ríos e Díaz de Rábago á crise finisecular

Este estudo plantexa as interaccións habidas entre pensamento económico e a toma de decisións políticas a traveso dun caso concreto. Analizámo-las propostas referidas á política agraria plantexadas polo Ministro de Fomento Eugenio Montero Ríos (1885-1886) e a influencia que nelas exerciu o economista Joaquín Díaz de Rábago. Ámbolos dous foron galegos destacados da segunda metade do XIX . A investigación centrouse nas concomitancias entre as propostas lexislativas e as obras publicadas. Ainda que tamén pescudamos aspectos biográficos máis correspondencia persoal co gallo de evidencia-la amizade e a cooperación existentes entre eles.

Mujeres en la casa, la escuela y la fábrica. El singular discurso de la domesticidad de la escuela economista española (1861-1909)

Los textos de la Escuela Economista Española (segunda mitad del XIX) contienen una valoración del papel de las mujeres en la economía y la sociedad transgresor frente al discurso dominante, que defendía un único y exclusivo rol para todas las mujeres: el hogar y la maternidad. La mayoría de los miembros de esta corriente económica defienden el trabajo femenino en las fábricas, basándose en argumentos salariales; e incluso demandan una formación profesional para aquellas que en muchos casos ni tan siquiera eran alfabetizadas por ser mujeres. Los textos de estos economistas transmiten nuevas ideas sobre el papel económico y social de las mujeres en una España dominada por un discurso que negaba la necesidad del trabajo femenino para las familias trabajadoras.

Geochemistry of highly acidic mine water following disposal into a natural lake with carbonate bedrock

Acid mine drainage (AMD) from the Zn-Pb(-Ag-Bi-Cu) deposit of Cerro de Pasco (Central Peru) and waste water from a Cu-extraction plant has been discharged since 1981 into Lake Yanamate, a natural lake with carbonate bedrock. The lake has developed a highly acidic pH of similar to 1. Mean lake water chemistry was characterized by 16,775 mg/L acidity as CaCO(3), 4330 mg/L Fe and 29,250 mg/L SO(4). Mean trace element concentrations were 86.8 mg/L Cu, 493 mg/L Zn, 2.9 mg/L Pb and 48 mg/L As, which did not differ greatly from the discharged AMD. Most elements showed increasing concentrations from the surface to the lake bottom at a maximal depth of 41 m (e.g. from 3581 to 5433 mg/L Fe and 25,609 to 35,959 mg/L SO(4)). The variations in the H and 0 isotope compositions and the element concentrations within the upper 10 m of the water column suggest mixing with recently discharged AMD, shallow groundwater and precipitation waters. Below 15 m a stagnant zone had developed. Gypsum (saturation index, SI similar to 0.25) and anglesite (SI similar to 0.1) were in equilibrium with lake water. Jarosite was oversaturated (SI similar to 1.7) in the upper part of the water column, resulting in downward settling and re-dissolution in the lower part of the water column (SI similar to -0.7). Accordingly, jarosite was only found in sediments from less than 7 m water depth. At the lake bottom, a layer of gel-like material (similar to 90 wt.% water) of pH similar to 1 with a total organic C content of up to 4.40 wet wt.% originated from the kerosene discharge of the Cu-extraction plant and had contaminant element concentrations similar to the lake water. Below the organic layer followed a layer of gypsum with pH 1.5, which overlaid the dissolving carbonate sediments of pH 5.3-7. In these two layers the contaminant elements were enriched compared to lake water in the sequence As < Pb approximate to Cu < Cd < Zn = Mn with increasing depth. This sequence of enrichment was explained by the following processes: (i) adsorption of As on Fe-hydroxides coating plant roots at low pH (up to 3326 mg/kg As), (ii) adsorption at increasing pH near the gypsum/calcite boundary (up to 1812 mg/kg Pb, 2531 mg/kg Cu. and 36 mg/kg Cd), and (iii) precipitation of carbonates (up to 5177 mg/kg Zn and 810 mg/kg Mn: all data corrected to a wet base). The infiltration rate was approximately equal to the discharge rate, thus gypsum and hydroxide precipitation had not resulted in complete clogging of the lake bedrocks. (C) 2010 Elsevier Ltd. All rights reserved.

Una casa, una història: patrimoni arquitectònic i humà d'una casa de la Selva del Camp

Treball de recerca realitzat per una alumna d'ensenyament secundari i guardonat amb un Premi CIRIT per fomentar l'esperit científic del Jovent l'any 2009. El treball té com a objecte de recerca un habitatge del municipi de la Selva del Camp. Aquest, es centra tant en els aspectes artístics i decoratius, com en l’anàlisi de l’evolució patrimonial i l’ús social de l’edifici entre els segles XVIII-XX. En la recerca s’ha analitzat, per una banda, el procés de transformació de l’edifici des de l’any 1749 i els elements artístics que encara s’hi conserven com pintures neoclàssiques, treballs de ferro forjat, etc., els quals fan que sigui una de les cases més emblemàtiques del Carrer Major de la Selva. D’altra banda, s’ha indagat en les diferents generacions que, des de mitjan segle XVIII, n’han tingut la propietat i el paper que aquestes famílies han jugat dins la societat selvatana. La casa, en aquests anys, ha pertanyut a dues famílies i al Sindicat Agrícola. La primera, els Fortuny, terratinents i amb càrrecs al govern municipal; l'altra, els Carnicer, comerciants d'avellanes dels quals jo en sóc descendent. De 1910 a 1920 la casa fou al seu del Sindicat Agrícola i a partir de textos de Puig i Ferreter s’ha pogut descriure l’ambient que s'hi vivia i les activitats que s’hi duien a terme. Alhora, el fet d’analitzar les diferents funcions que l’edifici ha tingut al llarg d’aquests anys (residència familiar, corredoria de comerç, premsa d’oli, seu del Centre Republicà o del Sindicat Agrícola) ha permès explicar la història de la vila de la Selva a partir de la d’aquest edifici.

Rosickyite (monoclinic gamma-sulphur) from La Presta Asphalt Mine, Neuchatel, Switzerland: new X-ray powder diffraction data

Rosickyite, the natural monoclinic gamma -form of sulphur, exists in only a few localities around the globe. In the old asphalt mine at La Presta, Neuchatel. Switzerland, rosickyite occurs locally as small, but very well formed crystals suitable for crystallographic studies. It grows as an alteration product of pyrite-rich asphalt. Rosickyite from La Presta mine is pure molecular sulphur, as revealed by gas chromatography-mass spectrometry. The X-ray powder diffraction data of La Presta rosickyite does not match the one previously published for this species. Therefore, a single crystal study was undertaken and a new indexed X-ray powder diffraction diagram for natural rosickyite is proposed.

Casa Museu Lluís Domènech i Montaner : Recurs electrònic

Treball de recerca que té com a principal objectiu elaborar una guia electrònica (pàgina web) de la Casa Museu Lluís Domènech i Montaner. Aquest treball està inscrit dins un aprenentatge museístic i informàtic. Serà un aprenentatge museístic per tot el que comporta la lectura de les sales i els materials que s'hi exposen, i informàtic perquè es tracta de dissenyar i elaborar un recurs electrònic que ha de permetre una presentació agradable, fàcil de progrés, harmoniosa i, alhora, concreta.

Aplicació especialitza en la cerca de feines que es puguin realitzar des de casa

El projecte consisteix en la creació d'una aplicació WEB construïda sota arquitectura J2EE, aquesta aplicació consistirà en mostrar ofertes laborals definides per empresa, categories, hores de treball i condicions contractuals amb un objectiu molt clar, el que totes les ofertes presentades és puguin realitzar des de casa.

Aplicació mòbil per al control d'una casa domòtica

Desenvolupament en .NET d'una aplicació de control d'una casa domòtica mitjançant un dispositiu mòbil amb Windows Mobile 6 o superior.