Anomaly-free constraints in neutrino seesaw models

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

NOLEN-SCHIFFER ANOMALY AND RHO(0)-OMEGA MIXING

The Nolen-Schiffer anomaly is the long standing discrepancy between theory and experiment of binding energy differences of mirror nuclei. It appears that the anomaly is largely explained by the charge symmetry breaking force generated by the rho(0)-omega mixing. In this paper I discuss the effect of the rho(0)-omega mixing to the binding energy differences in relativistic models of the nucleus. I also discuss the issue of momentum dependence of rho(0)-omega mixing amplitude and present an alternative explanation of the anomaly based on the partial restoration of chiral symmetry in the nucleus.

A model for the Schottky anomaly in metallic Nd2-yCeyCuO4

We present a simple model for the doped compound Nd2-yCevCuO4, in order to explain some recent experimental results on the latter. Within a Hartree-Fock context, we start from an impurity Anderson-like model and consider the magnetic splitting of the Nd-4f ground state Kramers doublet due to exchange interactions with the ordered Cu moments. Our results are in very good agreement with the experimental data, yielding a Schottky anomaly peak for the specific heat that reduces its amplitude, broadens and shifts to lower temperatures, upon Ce doping. For overdoped compounds at low temperatures, the specific heat behaves linearly and the magnetic susceptibility is constant. A smooth transition from this Fermi liquid-like behavior occurs as temperature is increased and, at high temperatures, the susceptibility exhibits a Curie-like behavior. Finally, we discuss some improvements our model is amenable to incorporate, (C) 1998 Elsevier B.V. B.V. All rights reserved.

Unusual early morning development of the equatorial anomaly in the Brazilian sector during the Halloween magnetic storm

The solar events that occurred at the end of October 2003 gave rise to very strong geomagnetic disturbances that peaked twice with Dst values reaching -345 nT around 0000 UT on 30 October and -400 nT around 2300 UT, on the same day. Disturbances in several ionospheric parameters were observed over Brazil. This work will focus on the ionospheric response to the initial westward prompt penetration electric field and on the strong intensification of the equatorial ionization anomaly that occurred because of the electric field polarity reversal that followed in the early morning hours of 29 October. The F layer peak height over the equator first decreased under the strong prompt penetration westward electric field, which was followed by significant height increase under eastward electric field. We have used Sheffield University Plasmasphere Ionosphere Model (SUPIM) with an intensified westward disturbed electric field in the presunrise hours, presumably due to prompt penetration from the magnetosphere, in order to study the effect of such a field in the ionosphere. The simulation results showed that prompt penetration of magnetospheric electric fields of westward polarity to the nightside equatorial region seems to be the most probable cause of the initial F layer height decreases. The intensification of the equatorial ionization anomaly and the unusual enhancement on F layer peak density, which was not modeled by the SUPIM, are explained as caused by the strong eastward electric field that followed the initial phase in combination with a highly variable disturbed meridional/transequatorial wind system as inferred from the F2 layer peak height variations. The highly dynamic wind pattern, with a short-term response (2-4 hours), is compatible with the predictions of some previous theoretical model calculations reported in the literature.

The SU(2) Skyrme model and anomaly

The SU(2) Shyrme model, expanding in the collective coordinates variables, gives rise to second-class constraints. Recently this system was embedded in a more general Abelian gauge theory using the BFFT Hamiltonian method. in this work we quantize this gauge theory computing the Noether current anomaly using for this two different methods: an operatorial Dirac first class formalism and the non-local BV quantization coupled with the Fujikawa regularization procedure. (C) 2000 Elsevier B.V. B.V. All rights reserved.

Neutrinos in anomaly mediated supersymmetry breaking with R-parity violation

We show that a supersymmetric standard model exhibiting anomaly mediated supersymmetry breaking can generate naturally the observed neutrino mass spectrum as well mixings when we include bilinear R-parity violation interactions. In this model, one of the neutrinos gets its mass due to the tree-level mixing with the neutralinos induced by the R-parity violating interactions while the other two neutrinos acquire their masses due to radiative corrections. One interesting feature of this scenario is that the lightest supersymmetric particle is unstable and its decay can be observed at high energy colliders, providing a falsifiable test of the model.

Atmospheric cosmic rays in the South Atlantic anomaly region

To study the production and propagation of fast secondaries particles in the atmosphere, data collected during eleven quiet-time balloon flights are analysed. Comparisons of these data with those obtained in different geomagnetic rigidity regions permit to estimate the contributions of the proton and electron components in the measured intensities. Derivations of this last component in the «upward» and «downward» moving electrons fluxes indicate that in the anomaly region a fraction of these particles, produced by the primary protons, are leaving the atmosphere and will not return to the Earth. © 1991 Società Italiana di Fisica.

Gravity Data and Crustal Structure of North-Central Brazil

The Bouguer gravity anomaly of the northwest Ceará state in north-central Brazil was separated into its regional and residual components which were interpreted separately. By assuming that the sources of the regional anomalies are the depth variations of the crust-mantle interface, the mapping of these variations permited identifying crustal thickening zones which may be related to regional structures. The gravity residual sources coincide with occurrences of high-grade rocks (granulites) associated to medium-grade gneisses. Besides, the major strike-slip zones present significant signatures in the gravity data. This geophysical interpretation is compatible with the interpretation that the tectonic framework of the area is related to two crustal blocks conjoined by an A-type suture. The blocks are displaced along an oblique ramp with dextral movement, which played an important role in uplifting high-grade rocks from the lower crust to upper crustal levels. The suture zone corresponds to an imbricated compressive system dipping to the east and complicated by late dextral strike-slip shear zones.

Axial anomaly through analytic regularization

In this work we consider the two-point Green's functions in (1 + 1)-dimensional quantum electrodynamics and show that the correct implementation of analytic regularization gives a gauge invariant result for the vacuum polarization amplitude and the correct coefficient for the axial anomaly.

Aplicação dos métodos gravimétrico e magnetométrico para a definição do comportamento estrutural da faixa de dobramentos Araguaia

O presente trabalho consiste na interpretação de informações gravimétricas e aeromagnetométricas (Projeto Geofísico Brasil-Canadá - PGBC) da região setentrional da Faixa de Dobramentos Araguaia, envolvendo uma área de aproximadamente 129.000km², compreendida entre os meridianos 47°50’W e 50°30’W e paralelos 4°50'S e 9°00'S. Abrange porções sudeste do Estado do Pará, noroeste de Goiás e oeste do Maranhão. Os trabalhos de campo constaram de levantamentos gravimétrico e altimétrico, ao longo de rodovias que constituem a rede viária regional, e os resultados obtidos, após correções e reduções, foram então organizados de forma a constituírem um mapa de anomalias Bouguer, apresentado em escala 1:500.000. O padrão gravimétrico da faixa de dobramentos Araguaia se caracteriza por mostrar feições predominantemente longitudinais, com curvas isoanômalas de direções submeridianas, concordante com o comportamento litológico-estrutural conhecido para a área. Na porção centro-meridional desse mapa aparece uma zona de anomalia negativa, alongada e intensa (menos de -100mgal), a qual sofre duas importantes inflexões para NW, sendo uma correlacionável ao Lineamento Carajás, e a outra na altura do paralelo 5°30'S. Apresenta zonas de altos gravimétricos, notadamente na porção noroeste (domínio cratônico), relacionada à influência das metavulcânicas do Grupo Grão Pará, e na porção nordeste, devida a massas densas introduzidas na crosta. Destaca-se também o relativo alto gravimétrico acompanhando o flanco oriental do eixo de ocorrência das braquidobras, podendo ser devido a massas excedentes colocadas sob essa região, através de esforços tectônicos, produzindo elevações do nível de base da crosta e consequentemente do embasamento. De forma genérica o flanco oriental da faixa mostra um gradiente mais intenso que o ocidental, devido principalmente à configuração geométrica das estruturas nesse setor. Da mesma forma merece destaque o gradiente regional ascendente de sul para norte. A análise das cartas de intensidade magnética do PGBC fornecem condições à individualização de diversos domínios magnéticos, perfeitamente correlacionáveis litológico e estruturalmente com as unidades geotectônicas que compõem o arcabouço regional, assim como suas subunidades. A execução de modelamento simples, quer para as informações gravimétricas como magnetométricas, objetivaram fornecer subsídios semi-quantitativos à interpretação, de forma a auxiliar no estabelecimento do padrão geométrico do embasamento da faixa de dobramentos Araguaia, assim como das estruturas a ela impostas. Assim, por meio do processamento das informações gravimétricas, verificou-se um padrão geométrico na forma de fatias imbricadas, estabelecidas sobre o substrato. A grande anomalia negativa da porção centro-meridional da faixa pode estar relacionada a uma deficiência de massa profunda (depressão na base da crosta) ou ainda a uma associação entre contraste de densidade e espessamento do pacote de supracrustais, nessa porção. O baixo gravimétrico da porção sudeste da área, entre Guarai e Tupirama, é devido a uma depressão do embasamento, da mesma forma como a anomalia negativa associada ao Lineamento Carajás está relacionada a uma estrutura sinformal conhecida.

Inversão gravimétrica rápida do relevo do embasamento aplicando o funcional da variação total

Apresentamos um novo método de inversão linear bidimensional de dados gravimétricos produzidos por bacias sedimentares com relevo do embasamento descontínuo. O método desenvolvido utiliza um modelo interpretativo formado por um conjunto de fitas horizontais bidimensionais justapostas cujas espessuras são os parâmetros a serem estimados. O contraste de densidade entre o embasamento e os sedimentos é presumido constante e conhecido. As estimativas das espessuras foram estabilizadas com o funcional da Variação Total (VT) que permite soluções apresentando descontinuidades locais no relevo do embasamento. As estimativas do relevo são obtidas através da resolução de um sistema de equações lineares, resolvido na norma L₁. Como métodos lineares subestimam as estimativas de profundidade do embasamento de bacias maiores que cerca de 500 m, amplificamos as estimativas de profundidade através da modificação da matriz associada ao modelo interpretativo de fitas. As estimativas obtidas através deste procedimento são em geral ligeiramente superestimadas. Desse modo, elas são corrigidas através de uma correção definida pela expressão da placa Bouguer. Testes em dados sintéticos e reais produziram resultados comparáveis aos produzidos pelo método não linear, mas exigiram menor tempo computacional. A razão R entre os tempos exigidos pelo método não linear e o método proposto cresce com o número de observações e parâmetros. Por exemplo, para 60 observações e 60 parâmetros, R é igual a 4, enquanto para 2500 observações e 2500 parâmetros R cresce para 16,8. O método proposto e o método de inversão não linear foram aplicados também em dados reais do Steptoe Valley, Nevada, Estados Unidos, e da ponte do POEMA, no Campus do Guamá em Belém, produzindo soluções similares às obtidas com o método não linear exigindo menor tempo computacional.

Fractional fermion charges induced by axial-vector and vector gauge potentials and parity anomaly in planar graphenelike structures

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Effect of essential oil from Citrus aurantium in maternal reproductive outcome and fetal anomaly frequency in rats

Citrus aurantium L., commonly known as bitter orange, is widely used in folk medicine, but there is little data in the literature about the s on pregnancy. The aim of the present study was to evaluate the influence of essential oil obtained from fruits of Citrus aurantium on the maternal reproductive outcome and fetal anomaly incidence in rats. Pregnant Wistar rats were randomized into four groups (n minimum = 12 animals/group): G1 = control, G2 to G4 = treated with essential oil from C. aurantium at dose 125, 250 and 500 mg/kg, respectively. Rats were orally treated, by gavage, with plant essential oil or vehicle during pre-implantation and organogenic period (gestational day 0-14). On gestational day 20 the rats were anaesthetized and the gravid uterus was weighed with its contents and the fetuses were analyzed. Results showed that the treated group with 500 mg/kg presented decreased placental weights and placental index, although the treatment with bitter orange essential oil did not show any alteration in maternal reproductive performance, toxicological , changes in ossification sites, and malformation index. In conclusion, the treatment of Citrus aurantium essential oil was not teratogenic and did not alter the maternal reproductive outcome.