Ni-Zn-Sm nanopowder ferrites: Morphological aspects and magnetic properties

Ni-Zn ferrites have been widely used in components for high-frequency range applications due to their high electrical resistivity, mechanical strength and chemical stability. Ni-Zn ferrite nanopowders doped with samarium with a nominal composition of Ni0.5Zn0.5Fe2-xSmxO4 (x = 0.0, 0.05, and 0.1 mol) were obtained by combustion synthesis using nitrates and urea as fuel. The morphological aspects of Ni-Zn-Sm ferrite nanopowders were investigated by X-ray diffraction, nitrogen adsorption by BET, sedimentation, scanning electron microscopy and magnetic properties. The results indicated that the Ni-Zn-Sm ferrite nanopowders were composed of soft agglomerates of nanoparticles with a high surface area (55.8-64.8 m(2)/g), smaller particles (18-20 nm) and nanocrystallite size particles. The addition of samarium resulted in a reduction of all the magnetic parameters evaluated, namely saturation magnetization (24-40 emu/g), remanent magnetization (2.2-3.5 emu/g) and coercive force (99.3-83.3 Oe). (c) 2007 Elsevier B. V. All rights reserved.

Luminescence and defect centres in MgSrAl(10)O(17):Sm(3+) phosphor

An efficient reddish orange emission MgSrAl(10)O(17):Sm(3+) phosphor was prepared by the combustion method. The phosphor has been characterized by X-ray diffraction, scanning electron microscopy, thermogravimetric analysis measurements. Photoluminescence spectrum revealed that samarium ions are present in trivalent oxidation states. The phosphor exhibits two thermally stimulated luminescence (TSL) peaks at 210 degrees C and 450 degrees C. Electron spin resonance studies were carried out to identify the defect centres responsible for the TSL process in MgSrAl(10)O(17):Sm(3+) phosphor. Three defect centres have been identified in irradiated phosphor and these centres are tentatively assigned to an O(-) ion and F(+) centres. O(-) ion (hole centre) correlates with the 210 degrees C TSL peak while one of the F+ centres (electron centre) appears to relate to the 450 degrees C TSL peak. (C) 2010 Elsevier B.V. All rights reserved.

Precambrian history of the Zona Transversal of the Borborema Province, NE Brazil: Insights from Sm-Nd and U-Pb geochronology

The Borborema Province has three major subprovinces. The northern subprovince lies north of the Patos shear zone and is comprised of Paleoproterozoic cratonic basement with Archean nuclei, plus overlying Neoproterozoic supracrustal rocks and Brasiliano plutonic rocks. The central subprovince occurs between the Patos and Pernambuco shear zones and is mainly comprised of the Zona Transversal. The southern subprovince occurs between the Pernamabuco shear zone and the Sao Francisco craton and is comprised of a tectonic collage of various blocks, terranes, or domains ranging in age from Archean to Neoproterozoic. This report focuses on the Zona Transversal, especially on Brasiliano rocks for which we have the most new information. Paleoproterozoic gneisses with ages of 2.0-2.2 Ga occur discontinuously throughout the Zona Transversal. The Cariris Velhos suite consists of metavolcanic, metasedimentary, and metaplutonic rocks yielding U-Pb zircon ages of 995-960 Ma. This suite is mainly confined to a 100 km wide belt that extends for more than 700 km within the Alto Pajeu terrane. Sm-Nd model ages in metaigneous rocks cluster about 1.3-1.6 Ga, indicating that older crust was involved in genesis of their magmas. Brasiliano supracrustal rocks dominate the Pianco-Alto Brigida terrane, and they probably also constitute significant parts of the Alto Pajeu and Rio Capibaribe terranes. They are only slightly older than early stages of Brasiliano plutonism, with detrital zircon ages at least as young as 620 Ma; most T(DM) ages range from 1.2 to 1.6 Ga. Brasiliano plutons range from ca. 640 to 540 Ma, and their T(DM) ages range from 1.2 to 2.5 Ga. Previous workers have shown significant correlations among U-Pb ages, Sm-Nd model ages, petrology, and geochemistry, and we are able to reinforce and extend these correlations. Stage I plutons formed 640 -610 Ma and have T(DM) ages less than 1.5 Ga. Stage 11 (610-590 Ma) contains few plutons, but coincides with the peak of compressional deformation, metamorphism, and formation of migmatites. Stage III plutons (590 to ca. 575 Ma) have older T(DM) ages (ca. 1.8-2.0 Ga), as do Stage IV plutons (575 to ca. 550 Ma; T(DM) from 1.9 to 2.4 Ga). Stage III plutons formed during the transition from compressional to transcurrent deformation, while Stage IV plutons are mainly post-tectonic. Stage V plutons (550-530 Ma) are commonly undeformed (except along younger shear zones) and have A-type geochemistry. The five stages have distinct geochemical properties, which suggest that the tectonic settings evolved from early, arc-related magma-genesis (Stage I) to within-plate magma-genesis (Stage V), with perhaps some intermediate phases of extensional environments. (C) 2011 Elsevier Ltd. All rights reserved.

Intressenters agerande – vid ett undantag från revisionsplikt för små aktiebolag

Ever since Sweden joined EU on the 1st of January 1995 the auditing is regulated not only by our Swedish laws but also by EG:s directives. In the fourth directive the member states are given a possibility to dispense small companies from the duty to audit the accounts. It is up to every member state to decide whether they want to dispense the small companies or not and today Sweden is one of few member states who does not.The purpose of this essay was to describe how lenders and Skatteverket will act in case of a dispensation for small companies from the duty to audit the accounts. The study has been carried out by interviewing four lenders and Skatteverket.The study shows that the lenders and Skatteverkets acting in case of a dispensation for small companies from the duty to audit the accounts will part from each others. While the lenders stand before a big change Skatteverkets work will be next to unaltered.Half the lenders think that they will continue to demand that the companies’ accounts be audited. The other half thinks that they will adjust their demands that the accounts be audited to each specific company. Skatteverket trusts in the increasing number of samples to guarantee the quality with the companies’ financial reports.

"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.

Små citroner gula : En studie i hur estetiska lärprocesser iscensätts, värderasoch realiseras, samt hur en lärmiljö med – ”The Wow Factor”påverkar inlärning på gymnasienivå

Uppsatsens syfte är att studera hur estetiska lärprocesser används för att stimulera lärandet och utveckla eleverna på gymnasial nivå i ämnet religionskunskap. För att få svar har under-sökningen fokuserat på hur estetiska lärprocesser iscensätts i praktiken, kopplat till teori om hur dessa lärprocesser kan påverka och stimulera elevens utveckling och lärande. Studien grundar sig på kvalitativa intervjuer gjorda på två olika skolor, en privat skola och en kom-munal med gymnasielärare i ämnet religion. Intervjutexterna har tolkats hermeneutiskt för att inte bara synliggöra samtalet mellan informanter och forskare, utan även belysa den tolkade texten som på så sätt även den kan ses som ett samtal mellan tolkare, läsare och text. Studien har använt ett teoretiskt ramverk där tre teoretiska perspektiv belyst estetiska lärprocesser samt kringliggande problematik i ämnet. Studien är av komparativ art och analysverktygen har selekterats utifrån tanken att med olika teoretikers perspektiv bemöta och besvara studiens frågeställningar.Resultatet påvisar att det råder en tveksamhet om vad som kan betraktas som estetiska lärpro-cesser och vad som ska inkluderas i begreppet bland informanterna. Dock råder en samstäm-mighet i att det rör sig om praktiskt, kreativt engagemang i grupp som kännetecknar estetiken i verksamheten. Värderingsfrågan visade sig ha två dimensioner. Den ena aspekten var att in-formanterna värderade de estetiska lärprocesserna högt som ur motivations-, engagemangs- och personlighetsutvecklande perspektiv. Däremot värderades de estetiska lärprocesserna lågt ur ett betygsgrundande perspektiv.De estetiska lärprocesserna iscensätts främst genom film, möten och miljöbyten. Film an-vänds främst som visuell och känslomässig förstärkning av undervisningens valda innehåll. Möten med personer aktiva inom det aktuella undervisningstemat används i lika stor utsträck-ning för att öka elevernas minnesförnimmelse och engagemang samt verklighetsrelatering, det vill säga koppling till extern kunskap. Möten kunde även i mer abstrakt betydelse innefatta möten med andra, redan befintliga kulturer i dess omgivning som synliggjorts genom den estetiska lärprocessen.Fördelarna med att använda sig av de estetiska lärprocesserna i undervisningen visade sig i huvudsak vara att de skapade utrymme för känslor och att de bidrar till en större studiemoti-vation samt ett ökat engagemang bland eleverna. Respekt för andra människor ur ett sociokul-turellt perspektiv var vad informanterna anser att de estetiska lärprocesserna genererar i ett vidgat lärande perspektiv, det vill säga ett externt lärande. Nackdelarna kan sammanfattas med de bristande resurser som stod till pedagogernas förfogande i form av tid och utbildning i ämnet, vilket i hög grad kom att belysa bedömningsproblematiken.

Aplicação de métodos radiométricos (Rb-Sr e Sm-Nd) na análise de bacias sedimentares o exemplo da Bacia do Paraná

Os métodos radiométricos (Rb-Sr e Sm-Nd) têm sido aplicados, com sucesso, em rochas sedimentares visando a obtenção de idades deposicionais e informações sobre proveniência. Em muitos casos, apesar dos resultados geologicamente significativos, ainda persistem dúvidas em relação a extensão e interpretação dos dados obtidos. Isto ocorre porque as rochas sedimentares resultam da mistura de fragmentos detríticos de diversas proveniências com diferentes sistemas isotópicos, conseqüentemente, já contendo um registro isotópico da rocha fonte. No caso do método Rb-Sr, aplicado em rochas sedimentares de granulometria fina, pode-se obter idades absolutas para o evento deposicional. Isto é viável desde que este registro isotópico proveniente das rochas fonte seja apagado no momento da deposição, ou seja, deve ocorrer a homogeneização isotópica do Sr no ambiente sedimentar. Para tanto, devem ser observados alguns pré-requisitos em relação a amostragem, granulometria, ambiente deposicional e composição mineralógica das amostras, entre outros. No entanto, ainda existem questionamentos em relação a esta metodologia especialmente quanto à ocorrência e à extensão do processo de homogeneização isotópica do Sr em ambiente sedimentar.(Continua0 O método Sm-Nd, apesar de ser uma técnica relativamente nova quando aplicada a rochas sedimentares, tem se tornado uma ferramenta fundamental para auxílio na determinação de proveniência de rochas sedimentares. As maiores dificuldades estão na correta interpretação dos valores obtidos e sua associação com um ambiente sedimentar, ou seja, de baixa temperatura. Neste trabalho, foram aplicados os métodos radiométricos Rb-Sr e Sm-Nd em amostras de rochas sedimentares coletadas em diferentes contextos geológicos da Bacia do Paraná. Foram tentativamente testados os diferentes parâmetros que atuam no sentido da homogeneização isotópica do Sr e do comportamento do Nd. Os resultados obtidos permitiram aprimorar a metodologia radiométrica Rb-Sr e Sm-Nd quando aplicada em rochas sedimentares, bem como obter resultados sobre a idade deposicional de diferentes unidades sedimentares e, por vezes, sua proveniência.

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.

Projected length annealing of etched Sm-152 ion tracks in apatite

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Antibodies to yeast Sm motif 1 cross-react with human Sm core polypeptides

Two regions common to all UsnRNP core polypeptides have been described: Sm motif 1 and Sm motif 2. Rabbits were immunized with a 22 amino-acid peptide containing one segment of Sm motif 1 (YRGTLVSTDNYFNLQL-NEAEEF, corresponding to residues 11-32) from yeast F protein. After immunization, the rabbit sera contained antibodies that not only reacted specifically with the peptide from yeast F protein but also cross-reacted with Sm polypeptides from mammals; that is, with purified human U1snRNPs. The results suggest that the peptide used and human Sm polypeptides contain a common feature recognized by the polyclonal antibodies. A large collection of human systemic lupus erythematosus sera was assayed using the yeast peptide as an antigen source. Seventy per cent of systemic lupus erythematosus sera contain an antibody specificity that cross-reacts with the yeast peptide.

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

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)