"Paddagogik" i förskolan : En studie om små barns kommunikation, samspel och lärande i mötet med en ipad

Syftet med detta arbete är att studera vad som händer med förskolebarns kommunikation, samspel och lärande i mötet med det digitala verktyget ipad. I denna undersökning har jag även tittat närmare på hur pedagogen förhåller sig och påverkar situationen. Jag har närmat mig undersökningsområdet med en kvalitativ ansats där jag använt mig av observation som metod. Mina observationer har utförts på en förskola där jag studerat barn och pedagoger på två av förskolans avdelningar, en avdelning med barn i åldern 1-3 år och en avdelning med barn i åldern 3-5 år.Resultatet påvisar att barnen blir språkligt aktiv och engagerade i mötet med ipaden. De kommunicerar och samspelar med varandra på många olika sätt. Studien visar även att barn möter ipaden under tystnad med koncentration och förundran. Pedagogen, kamraterna och ipadens olika applikationer har betydelse för kommunikationen och lärandet. Ipaden är ett lustfyllt verktyg som barnen möter med total orädsla och nyfikenhet. Barnen uppvisar en stor vilja att vara aktiva och interagera med det digitala verktyget och ipaden kan anses vara ett stöd för barns lärande. Förskolan har gett barnen möjligheter att möta och bli språkliga med det digitala verktyget ipad men undersökningen visar också att miljön och pedagogerna begränsar barnen på olika sätt. Slutsatsen av studien är att ipaden kan användas som ett verktyg för att stärka barns kommunikation, samspel och lärande om den används på ett genomtänkt och medvetet sätt i förskolans verksamhet.

Naturvetenskap i förskolan : En intervjustudie om pedagogers beskrivning av barns naturvetenskapliga lärande i åldern 1-3 år

Syftet med denna studie är att få kunskap om hur pedagoger i förskolan beskriver att de arbetar med naturvetenskap och barn i åldern 1-3 år samt hur de beskriver sina erfarenheter av hur barn lär sig naturvetenskap. För att söka denna kunskap användes följande frågeställningar: ”Hur beskriver pedagoger sina erfarenheter av hur små barn lär sig naturvetenskap?”, ”Vad beskriver pedagoger att små barn i förskolan behöver lära sig i naturvetenskap?”, ”På vilket sätt uttrycker pedagoger att de skapar förutsättningar för små barns naturvetenskapliga lärande?”, samt ”Hur beskriver pedagoger att de arbetar med naturvetenskap med små barn?”. Studien har genomförts genom intervjuer med fem pedagoger i en kommun i Mellansverige. Respondenterna anser att barns naturvetenskapliga lärande handlar om att barn får undersöka, utforska och uppleva naturvetenskap med sin kropp. Intervjusvaren påvisar att barns spontana naturvetenskapliga verksamhet är en stor del av respondenternas arbete med naturvetenskap i förskolan. Respondenterna ser även sig själva och sitt engagemang och intresse som en viktig förutsättning för barns naturvetenskapliga lärande. Sitt arbete med naturvetenskap i förskolan beskriver respondenterna som att det mest handlar om ämnet biologi. Då respondenterna exemplifierade olika aktiviteter eller händelser som de menar speglar deras naturvetenskapliga verksamhet i förskolan så anger de bland annat arbete med växtprocesser, vattenlek, bygglek, årstider, väder, internet och naturkännedom. Genom dessa exempel påvisar respondenterna även aktiviteter inom kemi, fysik och teknik och inte bara inom biologi.

Anhörigperspektivet utifrån föräldrars erfarenheter då barnet har diabetes typ 1 : En litteraturöversikt

Bakgrund: Den största delen av behandlingen vid diabetes typ 1 är egenvård. När ett barn insjuknar i diabetes är det föräldrarna som huvudsakligen ansvarar för egenvården. Detta kan vara både psykiskt och fysiskt påfrestande. Det behövs mer kunskap om föräldrars upplevelser och deras erfarenheter av att vårda ett barn med diabetes. Syfte: Syftet med denna litteraturstudie är att belysa anhörigperspektivet utifrån föräldrars erfarenheter då barnet har diabetes typ 1 samt hur sjuksköterskan kan ge stöd till anhöriga. Metod: En litteraturöversikt. Resultat: Resultatet visar att egenvården skiljer sig mellan små barn och ungdomar, att föräldrar upplever känslor av oro och stress när deras barn fått diagnosen och att sjuksköterskan kan hjälpa och öka sin förståelse genom att stödja. Slutsats: Författarna kan dra slutsatsen att ökad kunskap och förståelse om egenvård vid diabetes typ 1 hos barn, kan bidra till en hjälp för sjuksköterskor att ge föräldrarna ett bra stöd och bemötande i vården.

Comparação estratigráfica e isotópica (Sm-Nd) das regiões do Cerro Morado e La Torre, bacia de Ischigualasto-Villa Unión, noroeste argentino

A bacia de Ischigualasto-Villa Unión (Stipanicic e Bonaparte, 1972), que consiste de uma bacia alongada no sentido NW-SE e preenchida por rochas sedimentares Triássicas, foi gerada durante o Eo-Triássico pela reativação de descontinuidades crustais pré-existentes, associadas ao Gondwanides, na região central andina. Esta limitada a oeste, pelo vale do Rio Bermejo, no qual se encontra a zona de sutura do Vale Fértil, que se caracteriza pela borda ativa da bacia. Aqui, apresentar-se-á uma revisão da estratigrafia da bacia de Ischigualasto-Villa Unión, detalhando-se duas áreas chaves do registro estratigráfico inferior da bacia, na região do Cerro Morado e La Torre. Nestas áreas utilizou-se de técnicas estratigráficas e isotópicas (Sm-Nd em rocha total), com o objetivo de estabelecer uma correlação entre seus registros estratigráficos e suas áreas-fonte, além de caracterizar o comportamento tectônico. Ambos os perfis apresentam na porção inferior o preenchimento por um sistema aluvial-fluvial (Formação Tarjados sensu Romer & Jensen, 1966), subdividido em 4 associações de fácies: leques aluviais, canais fluviais, barras longitudinais e planície de inundação; e, na porção superior, o preenchimento por um sistema lacustre-deltáico (Formação Los Chañares sensu Frenguelli, 1944, no Cerro Morado e, Formação Lomas Blancas sensu Bossi e Herbst, 1968, em La Torre), subdividido em 4 associações de fácies: lacustre, pró delta, frente deltáica e planicie deltáica. Sobre as últimas unidades ocorre um lacólito de diabásio (Formação Los Baldecitos) A formação Tarjados apresenta as maiores idades TDM na região do Cerro Morado, variando entre 1,33 e 1,60 Ga, enquanto que em La Torre os valores oscilam entre 1,03 e 1,30 Ga. Isso é interpretado aqui como uma variação da área fonte entre as duas regiões na época de sua sedimentação, cujas regiões poderiam estar compartimentadas em termos tectônicos a época de sua deposição. A formação Los Chañares possui idades TDM variando entre 0,90 e 1,36 Ga, e a formação Lomas Blancas possui idades TDM entre 0,99 e 1,35 Ga, com dominância de valores próximos a 1 Ga nos dois blocos. Os diabásios da formação Los Baldecitos possuem idades TDM entre 0,51 e 0,33 Ga, cujo dado é interpretado com uma extração mantélica próxima a 130 Ma de um manto modificado pela orogenia do Ciclo Gondwânico, ou até mesmo pelo processo de slab break-off da crosta oceânica consumida pela colisão do micro-continente Cuyania com a proto-margem do Gondwana (Ramos, 1999). Todas as rochas dessa formação obtiveram valores de Epsilon Nd positivos. A integração dos dados estratigráficos e isotópicos nos permite interpretar as duas áreas como meio-grábens distintos na etapa inicial de preenchimento, em função da discrepância entre as idades TDM entre as áreas. A partir da transgressão lacustre as áreas-fonte são uniformizadas e o alto estrutural pré-existente é transgredido.

Structural Aspects of the Distinct Biochemical Properties of Glutaredoxin 1 and Glutaredoxin 2 from Saccharomyces cerevisiae

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Thermal studies on solid 1,4-bis(3-carboxy-3-oxo-prop-1-enyl) benzene of lighter trivalent lanthanides

Solid-state compounds of general formula Ln(2)L(3)center dot nH(2)O, where L represents 1,4-bis(3-carboxy-3-oxo-prop-1-enyl)benzene and Ln = La, Ce, Pr, Nd, Sm, were synthesized. Complexometric titrations with EDTA, thermogravimetry (TG), differential thermal analysis (DTA), differential scanning calorimetry (DSC), X-ray powder diffractometry, elemental analysis and infrared spectroscopy have been employed to characterize and to study the thermal behavior of these compounds in dynamic air atmosphere. The results led to information about the composition, dehydration, crystallinity, and thermal decomposition of the synthesized compounds.

Estudo geoquímico e geocronológico Rb-Sr e Sm-Nd em zonas de cisalhamento mineralizadas em ouro e suas relações com as rochas encaixantes e geocronológico Sm-Nd em mineralizações de scheelita na faixa Seridó

Great part of the gold mineralizations are associated with shearing zones through which circulate a great volume of fluids, that interact with the host rocks, originating leaching or precipitation of chemical elements, including gold. The studied mineralizations are inserted in the Seridó Belt. The tungsten mineralization in Brejuí Mine is hosted in calcsilicate rocks from Jucurutu Formation. The São Francisco auriferous mineralization has as host rocks mica-schists from Seridó Formation, while the Ponta da Serra and Fazenda Simpático mineralizations are hosted in orthogneisses of this fold belt basement. The research conducted on these mineralizations had the purpose of integrate the data of chemical elements behavior during the shearing/mineralizing event, and its influence on the isotopic systems Rb-Sr and Sm-Nd. The studies of chemical mobility in the auriferous mineralizations showed that elements that during the shearing displayed in general an immobile behavior were Al, Ti and Zr. Among the elements that were mobilized during the event, K and Rb showed mass gain in ali belts of transformed rocks, while the elements Ca, Na and Sr normally lost mass. Petrographic studies showed that the minerais biotite and plagioclase, in all investigated mineralizations, played an important role in the chemical reactions occurred in the transformed rocks to the generation of muscovite, cordierite and sillimanite, justifying the input of K to the formation of muscovite, and the release of Na and Ca from plagioclase to the fluid phase. In the São Francisco auriferous mineralization, the results of the Rb-Sr isotopic analysis yielded ages of 645 ± 19 Ma and 596 ± 17 Ma, with both samples, from original and transformed rocks. Two ages, 569 ± 20 Ma. and 554 ± 19 Ma., were obtained with samples frem the transformed rocks domain. These ages suggest that there were two metamorphic pulses during the emplacement of the mineralized shearing zone. The Sm-Nd data yielded TDM ages of 1,31 Ga and 1,26 Ga with 3Nd (0,6 Ga) of -0,26 e -0,40 for the original and final transformed rocks, respectively. In case of the orthogneisses of Caicó Complex, e.g. the Ponta da Serra and Fazenda Simpático mineralizations, the Rb-Sr data did not yield ages with geological significance. In the Ponta da Serra mineralization, the Sm-Nd isotopic data yielded T DM ages of 2,56 Ga and 2,63 Ga to the original rocks and of 2,71 Ga to the mineralized sheared rock, and values of 3Nd (2,0 Ga) between -3,70 e -5,42 to the original and sheared rock, respectively. In the Fazenda Simpático, Sm-Nd data yielded TDM between 2,65 and 2,69 Ga with values of 3Nd (2,0 Ga) between -5,25 e -5,52. Considering the Sm-Nd data, the TDM ages may be admitted as the age of the parental magma extraction, producer of the protoliths of the orthogneisses from Ponta da Serra and Fazenda Simpático mineralizations. The chemical mobility studies showed that in the basement hosted mineralizations, Rb achieved mass while Sr lost mass, as Sm as well as Nd were strongly mobilized. The Sm/Nd ratio remained constant, however, confirming the isochemical character of those elements. In the basement mineralizations, Rb-Sr ages are destituted of geological significance, because of the partial opening of the isotopic system during the tectono-metamorphic transformations. In the tungsten mineralization, the diagram Sm-Nd constructed with the whole-rock data of calcsilicatic and the high-temperature paragenesis (garnet, diopside and iron-pargasitic hornblende) indicated an 631 ± 24 Ma age, while with the whole-rock data and low-temperature paragenesis (vesuvianite, epidote and calcite), a 537 ± 107 Ma age was obtained. These ages, associated with the petrographic observations, suggest that there was a time gap among the hydrothernal events responsible by the formation of the high and low temperature paragenesis in the calcsilicatic rocks mineralized in scheelite

Protonectin (1-6): A novel chemotactic peptide from the venom of the social wasp Agelaia pallipes pallipes

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Search for neutral supersymmetric Higgs bosons in multijet events at root s=1.96 TeV

We have performed a search for neutral Higgs bosons produced in association with bottom quarks in p (p) over bar collisions, using 260 pb(-1) of data collected with the D0 detector in Run II of the Fermilab Tevatron Collider. The cross sections for these processes are enhanced in many extensions of the standard model (SM), such as in its minimal supersymmetric extension at large tan beta. The results of our analysis agree with expectations from the SM, and we use our measurements to set upper limits on the production of neutral Higgs bosons in the mass range of 90 to 150 GeV.

A combined search for the standard model Higgs boson at root S=1.96 TeV

We present new results of the search for WH --> lvb (b) over bar production in p (p) over bar collisions at a center-of-mass energy of root S = 1.96 TeV, based on a dataset with integrated luminosity of 0.44 fb(-1). We combine these new results with previously published searches by the do collaboration, for WH and ZH production analyzed in the E(T)b (b) over bar final state, for ZH (--> l(+)l(-)b (b) over bar) production, for WH (-->. WWW) production, and for H (--> W W) direct production. No signal-like excess is observed either in the W H analysis or in the combination of all D0 Higgs boson analyses. We set 95% C.L. (expected) upper limits on sigma(p (p) over bar --> WH) x B(H --> b (b) over bar) ranging from 1.6 (2.2) ph to 1.9 (3.3) pb for Higgs boson masses between 105 and 145 GeV, to be compared to the theoretical prediction of 0.13 pb for a Standard Model (SM) Higgs boson with mass in m(H) = 115 GeV. After combination with the other do Higgs boson searches, we obtain for in H = 115 GeV an observed (expected) limit 8.5 (12.1) times higher than the SM predicted Higgs boson production cross section. For m(H) = 160 GeV, the corresponding observed (expected) ratio is 10.2 (9.0). (C) 2008 Elsevier B.V. All rights reserved.

High-pressure granulites from Carire, Borborema Province, NE Brazil: Tectonic setting, metamorphic conditions and U-Pb, Lu-Hf and Sm-Nd geochronology

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Photoluminescence in disordered sm-doped PbTiO3: Experimental and theoretical approach

Sm-doped PbTiO3 powder was synthesized by the polymeric precursor method, and was heat treated at different temperatures. The x-ray diffraction, photoluminescence, and UV-visible were used as a probe for the structural order degree short-, intermediate-, and long-range orders. Sm-3+ ions were used as markers of these order-disorder transformations in the PbTiO3 system. From the Rietveld refinement of the Sm-doped PbTiO3 x-ray diffraction data, structural models were obtained and analyzed by periodic ab initio quantum mechanical calculations using the CRYSTAL 98 package within the framework of density functional theory at the B3LYP level. This program can yield important information regarding the structural and electronic properties of crystalline and disordered structures. The experimental and theoretical results indicate the presence of the localized states in the band gap, due to the symmetry break, which is responsible for visible photoluminescence at room temperature in the disordered structure. (c) 2006 American Institute of Physics.

Geological evolution of the basement rocks in the east-central part of the Rondonia Tin Province, SW Amazonian craton, Brazil: U-Pb and Sm-Nd isotopic constraints

On the basis of geologic, petrologic, and U-Pb geochronologic data the basement rocks in the east-central part of the Rondonia Tin Province (RTP, southwestern Amazonian craton) are grouped into five lithologic associations: (1) tonalitic gneiss (1.75 Ga); (2) enderbitic granulite (1.73 Ga); (3) paragneiss; (4) granitic and charnockitic augen gneisses (1.57-1.53 Ga); and (5) fine-grained granitic gneiss and charnockitic granulite (1.43-1.42 Ga). The first three are related to development of the Paleoproterozoic Rio Negro-Juruena Province and represent the oldest crust in the region. The tonalitic gneisses and enderbitic granulites show calc-alkaline affinities and Nd isotopic compositions (initial epsilon(Nd) = +0-1 to -1.5; T-DM of 2.2-2.1 Ga) that suggest a continental arc margin setting for the original magmas. The paragneisses yield T-DM values of 2.2-2.1 Ga suggesting that source material was primarily derived from the Ventuari-Tapajos and Rio Negro-Juruena crusts, but detrital zircon ages and an intrusive granitoid bracket deposition between 1.67 and 1.57 Ga. The granitic and charnockitic augen gneisses show predominantly A-type and within-plate granite affinities, but also some volcanic arc granite characteristics. The initial epsilon(Nd) values (+0.6 to +2.0) indicate mixing of magmas derived from depleted mantle and older crustal sources. These rocks are correlated to the 1.60-1.53 Ga Serra da Providencia intrusive suite that reflects inboard magmatism coeval with the Cachoeirinha orogen located to the southeast. The fine-grained granitic gneiss and charnockitic granulites represent the first record of widespread magmatism at 1.43-1.42 Ga in northern Rondonia. Their geochemical signatures and the slightly positive initial epsilon(Nd) values (+0.7 to +1.2) are very similar to those of the most evolved granites of the calc-alkaline Santa Helena batholith farther southeast. U-Pb monazite and Sm-Nd whole-rock-garnet ages demonstrate that a high-grade tectonometa-morphic episode occurred in this region at 1.33-1.30 Ga. This episode attained upper-amphibolite conditions and is interpreted as the peak of the Rondonian-San Ignacio orogeny. The U-Pb and Sm-Nd data presented here and data published on rapakivi granites elsewhere indicate that the east-central part of the RTP is a poly-orogenic region characterized by successive episodes of magmatism, metamorphism, and deformation between 1.75 and 0.97 Ga. (C) 2002 Elsevier B.V. B.V. All rights reserved.

The Serido Group of NE Brazil, a late Neoproterozoic pre- to syn-collisional basin in West Gondwana: insights from SHRIMP U-Pb detrital zircon ages and Sm-Nd crustal residence (T-DM) ages

The Serido Group is a deformed and metamorphosed metasedimentary sequence that overlies early Paleoproterozoic to Archean basement of the Rio Grande do Norte domain in the Borborema Province of NE Brazil. The age of the Serido Group has been disputed over the past two decades, with preferred sedimentation ages being either Paleoproterozoic or Neoproterozoic. Most samples of the Serido Formation, the upper part of the Serido Group, have Sm-Nd T-DM ages between 1200 and 1600 Ma. Most samples of the Jucurutu Formation, the lower part of the Serido Group, have T-DM ages ranging from 1500 to 1600 Ma; some basal units have T-DM ages as old as 2600 Ma, reflecting proximal basement. Thus, based on Sm-Nd data, most, if not all, of the Serido Group was deposited after 1600 Ma and upper parts must be younger than 1200 Ma.Cathodoluminescence photos of detrital zircons show very small to no overgrowths produced during ca. 600 Ma Brasiliano deformation and metamorphism, so that SHRIMP and isotope dilution U-Pb ages must represent crystallization ages of the detrital zircons. Zircons from meta-arkose near the base of the Jucurutu Formation yield two groups of ages: ca. 2200 Ma and ca. 1800 Ma. In contrast, zircons from a metasedimentary gneiss higher in the Jucurutu Formation yield much younger ages, with clusters at ca. 1000 Ma and ca. 650 Ma. Zircons from metasedimentary and metatuffaceous units in the Serido Formation also yield ages primarily between 1000 and 650 Ma, with clusters at 950-1000, 800, 750, and 650 Ma. Thus, most, if not all, of the Serido Group must be younger than 650 Ma. Because these units were deformed and metamorphosed in the ca. 600 Ma Brasiliano fold belt during assembly of West Gondwana, deposition probably occurred ca. 610-650 Ma, soon after crystallization of the youngest population of zircons and before or during the onset of Brasiliano deformation.The Serido Group was deposited upon Paleoproterozoic basement in a basin receiving detritus from a variety of sources. The Jucurutu Formation includes some basal volcanic rocks and initially received detritus from proximal 2.2-2.0 Ga (Transamazonian) to late Paleoproterozoic (1.8-1.7 Ga) basement. Provenance for the upper Jucurutu Formation and all of the Serido Formation was dominated by more distal and younger sources ranging in age from 1000 to 650 Ma. We suggest that the Serido basin may have developed as the result of late Neoproterozoic extension of a pre-existing continental basement, with formation of small marine basins that were largely floored by cratonic basement (subjacent oceanic crust has not yet been found). Immature sediment was initially derived from surrounding land; as the basin evolved much of the detritus probably came from highlands to the south (present coordinates). Alternatively, if the Patos shear zone is a major terrane boundary, the basin may have formed as an early collisional foredeep associated with south-dipping subduction. In any case, within 30 million years the region was compressed, deformed, and metamorphosed during final assembly of West Gondwana and formation of the Brasiliano-Pan African fold belts. (C) 2003 Elsevier B.V. All rights reserved.