Dynamical models for the Earth's geoid

The Earth's largest geoid anomalies occur at the lowest spherical harmonic degrees, or longest wavelengths, and are primarily the result of mantle convection. Thermal density contrasts due to convection are partially compensated by boundary deformations due to viscous flow whose effects must be included in order to obtain a dynamically consistent model for the geoid. These deformations occur rapidly with respect to the timescale for convection, and we have analytically calculated geoid response kernels for steady-state, viscous, incompressible, self-gravitating, layered Earth models which include the deformation of boundaries due to internal loads. Both the sign and magnitude of geoid anomalies depend strongly upon the viscosity structure of the mantle as well as the possible presence of chemical layering.

Correlations of various global geophysical data sets with the observed geoid can be used to construct theoretical geoid models which constrain the dynamics of mantle convection. Surface features such as topography and plate velocities are not obviously related to the low-degree geoid, with the exception of subduction zones which are characterized by geoid highs (degrees 4-9). Recent models for seismic heterogeneity in the mantle provide additional constraints, and much of the low-degree (2-3) geoid can be attributed to seismically inferred density anomalies in the lower mantle. The Earth's largest geoid highs are underlain by low density material in the lower mantle, thus requiring compensating deformations of the Earth's surface. A dynamical model for whole mantle convection with a low viscosity upper mantle can explain these observations and successfully predicts more than 80% of the observed geoid variance.

Temperature variations associated with density anomalies in the man tie cause lateral viscosity variations whose effects are not included in the analytical models. However, perturbation theory and numerical tests show that broad-scale lateral viscosity variations are much less important than radial variations; in this respect, geoid models, which depend upon steady-state surface deformations, may provide more reliable constraints on mantle structure than inferences from transient phenomena such as postglacial rebound. Stronger, smaller-scale viscosity variations associated with mantle plumes and subducting slabs may be more important. On the basis of numerical modelling of low viscosity plumes, we conclude that the global association of geoid highs (after slab effects are removed) with hotspots and, perhaps, mantle plumes, is the result of hot, upwelling material in the lower mantle; this conclusion does not depend strongly upon plume rheology. The global distribution of hotspots and the dominant, low-degree geoid highs may correspond to a dominant mode of convection stabilized by the ancient Pangean continental assemblage.

High frequency wave propagation in the earth: theory and observation

The wave-theoretical analysis of acoustic and elastic waves refracted by a spherical boundary across which both velocity and density increase abruptly and thence either increase or decrease continuously with depth is formulated in terms of the general problem of waves generated at a steady point source and scattered by a radially heterogeneous spherical body. A displacement potential representation is used for the elastic problem that results in high frequency decoupling of P-SV motion in a spherically symmetric, radially heterogeneous medium. Through the application of an earth-flattening transformation on the radial solution and the Watson transform on the sum over eigenfunctions, the solution to the spherical problem for high frequencies is expressed as a Weyl integral for the corresponding half-space problem in which the effect of boundary curvature maps into an effective positive velocity gradient. The results of both analytical and numerical evaluation of this integral can be summarized as follows for body waves in the crust and upper mantle:

1) In the special case of a critical velocity gradient (a gradient equal and opposite to the effective curvature gradient), the critically refracted wave reduces to the classical head wave for flat, homogeneous layers.

2) For gradients more negative than critical, the amplitude of the critically refracted wave decays more rapidly with distance than the classical head wave.

3) For positive, null, and gradients less negative than critical, the amplitude of the critically refracted wave decays less rapidly with distance than the classical head wave, and at sufficiently large distances, the refracted wave can be adequately described in terms of ray-theoretical diving waves. At intermediate distances from the critical point, the spectral amplitude of the refracted wave is scalloped due to multiple diving wave interference.

These theoretical results applied to published amplitude data for P-waves refracted by the major crustal and upper mantle horizons (the Pg, P*, and Pn travel-time branches) suggest that the 'granitic' upper crust, the 'basaltic' lower crust, and the mantle lid all have negative or near-critical velocity gradients in the tectonically active western United States. On the other hand, the corresponding horizons in the stable eastern United States appear to have null or slightly positive velocity gradients. The distribution of negative and positive velocity gradients correlates closely with high heat flow in tectonic regions and normal heat flow in stable regions. The velocity gradients inferred from the amplitude data are generally consistent with those inferred from ultrasonic measurements of the effects of temperature and pressure on crustal and mantle rocks and probable geothermal gradients. A notable exception is the strong positive velocity gradient in the mantle lid beneath the eastern United States (2 x 10^-3 sec^-1), which appears to require a compositional gradient to counter the effect of even a small geothermal gradient.

New seismic-refraction data were recorded along a 800 km profile extending due south from the Canadian border across the Columbia Plateau into eastern Oregon. The source for the seismic waves was a series of 20 high-energy chemical explosions detonated by the Canadian government in Greenbush Lake, British Columbia. The first arrivals recorded along this profile are on the Pn travel-time branch. In northern Washington and central Oregon their travel time is described by T = Δ/8.0 + 7.7 sec, but in the Columbia Plateau the Pn arrivals are as much as 0.9 sec early with respect to this line. An interpretation of these Pn arrivals together with later crustal arrivals suggest that the crust under the Columbia Plateau is thinner by about 10 km and has a higher average P-wave velocity than the 35-km-thick, 62-km/sec crust under the granitic-metamorphic terrain of northern Washington. A tentative interpretation of later arrivals recorded beyond 500 km from the shots suggests that a thin 8.4-km/sec horizon may be present in the upper mantle beneath the Columbia Plateau and that this horizon may form the lid to a pronounced low-velocity zone extending to a depth of about 140 km.

The structure of liquid argon as determined by x-ray diffraction

X-ray diffraction measurements and subsequent data analyses have been carried out on liquid argon at five states in the density range of 0.91 to 1.135 gm/cc and temperature range of 127 to 143°K. Duplicate measurements were made on all states. These data yielded radial distribution and direct correlation functions which were then used to compute the pair potential using the Percus-Yevick equation. The potential minima are in the range of -105 to -120°K and appear to substantiate current theoretical estimates of the effective pair potential in the presence of a weak three-body force.

The data analysis procedure used was new and does not distinguish between the coherent and incoherent absorption factors for the cell scattering which were essentially equal. With this simplification, the argon scattering estimate was compared to the gas scattering estimate on the laboratory frame of reference and the two estimates coincided, indicating the data normalized. The argon scattering on the laboratory frame of reference was examined for the existence of the peaks in the structure factor and the existence of an observable third peak was considered doubtful.

Numerical studies of the effect of truncation, normalization, the subsidiary peak phenomenon in the radial distribution function, uncertainties in the low angle data relative to errors in the direct correlation function and the distortion phenomenon are presented.

The distortion phenomenon for this experiment explains why the Mikolaj-Pings argon data yielded pair potential well depths from the Percus-Yevick equation that were too shallow and an apparent slope with respect to density that was too steep compared to theoretical estimates.

The data presented for each measurement are: empty cell and cell plus argon intensity, absorption factors, argon intensity, smoothed argon intensity, smoothed argon intensity corrected for distortion, structure factor, radial distribution function, direct correlation function and the pair potential from the Percus-Yevick equation.

Solar flare particle propagation--comparison of a new analytic solution with spacecraft measurements

A new analytic solution has been obtained to the complete Fokker-Planck equation for solar flare particle propagation including the effects of convection, energy-change, corotation, and diffusion with ĸ_r = constant and ĸ_Ɵ ∝ r². It is assumed that the particles are injected impulsively at a single point in space, and that a boundary exists beyond which the particles are free to escape. Several solar flare particle events have been observed with the Caltech Solar and Galactic Cosmic Ray Experiment aboard OGO-6. Detailed comparisons of the predictions of the new solution with these observations of 1-70 MeV protons show that the model adequately describes both the rise and decay times, indicating that ĸ_r = constant is a better description of conditions inside 1 AU than is ĸ_r ∝ r. With an outer boundary at 2.7 AU, a solar wind velocity of 400 km/sec, and a radial diffusion coefficient ĸ_r ≈ 2-8 x 10²⁰ cm²/sec, the model gives reasonable fits to the time-profile of 1-10 MeV protons from "classical" flare-associated events. It is not necessary to invoke a scatter-free region near the sun in order to reproduce the fast rise times observed for directly-connected events. The new solution also yields a time-evolution for the vector anisotropy which agrees well with previously reported observations.

In addition, the new solution predicts that, during the decay phase, a typical convex spectral feature initially at energy T_o will move to lower energies at an exponential rate given by T_KINK = T_oexp(-t/Ƭ_KINK). Assuming adiabatic deceleration and a boundary at 2.7 AU, the solution yields Ƭ_KINK ≈ 100h, which is faster than the measured ~200h time constant and slower than the adiabatic rate of ~78h at 1 AU. Two possible explanations are that the boundary is at ~5 AU or that some other energy-change process is operative.

Phase-shifting apodizers for increasing focal depth

We propose the use of a phase-shifting apodizers to increase focal depth, and we study the axial and radial behavior of this kind of apodizer under the condition that the axial intensity distribution is optimized for high focal depth. (C) 2002 Optical Society of America.

Superresolution by three-zone pure phase plate with 0, pi, 0 phase variation

Superresolution is very important in imaging and optical storage systems, and has attracted much attention. In this article, concentric three-zone phase plate with 0, pi, 0 phase variation has been investigated numerically to show that this kind of phase plate can be used to obtain three-dimensional superresolution. In addition, the number of intensity maximum, focal depth, focal shift, full-width half-maximum, and relative intensity of side lobe are listed for different radii of the phase zones, which paves the way for design of the phase plate. Therefore, one can choose values of radii for desired intensity distribution in focal region, such as for the purpose of radial superresolution with high focal depth in optical storage. (c) 2006 Elsevier Ltd. All rights reserved.

Detecção e classificação de VTCDs em sistemas de distribuição de energia elétrica usando redes neurais artificiais.

O objetivo deste trabalho é conhecer e compreender melhor os imprevistos no fornecimento de energia elétrica, quando ocorrem as variações de tensão de curta duração (VTCD). O banco de dados necessário para os diagnósticos das faltas foi obtido através de simulações de um modelo de alimentador radial através do software PSCAD/EMTDC. Este trabalho utiliza um Phase-Locked Loop (PLL) com o intuito de detectar VTCDs e realizar a estimativa automática da frequência, do ângulo de fase e da amplitude das tensões e correntes da rede elétrica. Nesta pesquisa, desenvolveram-se duas redes neurais artificiais: uma para identificar e outra para localizar as VTCDs ocorridas no sistema de distribuição de energia elétrica. A técnica aqui proposta aplica-se a alimentadores trifásicos com cargas desequilibradas, que podem possuir ramais laterais trifásicos, bifásicos e monofásicos. No desenvolvimento da mesma, considera-se que há disponibilidade de medições de tensões e correntes no nó inicial do alimentador e também em alguns pontos esparsos ao longo do alimentador de distribuição. Os desempenhos das arquiteturas das redes neurais foram satisfatórios e demonstram a viabilidade das RNAs na obtenção das generalizações que habilitam o sistema para realizar a classificação de curtos-circuitos.

用于高重复频率热容主振荡功率放大器激光系统的波前检测技术

高重复频率热容主振荡功率放大器(MOPA)激光系统的工作过程一般只持续几秒至几十秒,在此过程中系统输出光束的波前畸变是动态变化的。采用环路径向剪切干涉(CRWSI)技术对高重复频率热容MOPA系统波前畸变的变化过程进行检测,并对系统的总体结构进行了设计。搭建了一个简化的实验系统,采用平凹透镜来代替光放大器产生波前畸变,并由此对环路径向剪切干涉仪的测量精度进行了验证。结果表明,实验测量结果与理论计算值之间的峰值误差为7.8%(0.02λ)。

Dinâmica de crescimento de Centrolobium robustum (Vell.) Mart. ex Benth. (Leguminosae-Papilionoideae) na Floresta Atlântica, Rio de Janeiro, Brasil

O conhecimento sobre o ritmo de crescimento radial e a idade das árvores é um aspecto básico para compreender a dinâmica das populações, bem como o desenvolvimento e a sobrevivência das espécies. Nos trópicos, entretanto, estudos populacionais com este enfoque ainda são escassos, a despeito da urgente necessidade de preservação e manejo de suas florestas. Este trabalho tem por objetivo: i) Descrever a atividade cambial e o comportamento fenológico de Centrolobium robustum (Vell.) Mart. ex Benth., correlacionando estes parâmetros entre si; ii) Avaliar a influência da sazonalidade climática e do fotoperíodo sobre a atividade cambial e o comportamento fenológico e iii) Caracterizar o padrão estrutural dos anéis de crescimento e determinar, a partir destes, a idade e as taxas de crescimento radial da espécie na Reserva Biológica do Tinguá, RJ. Para a análise da atividade cambial, amostras de câmbio foram coletadas trimestralmente, processadas segundo técnicas usuais de anatomia vegetal e observadas sob microscopia ótica de campo claro, de fluorescência, de polarização e microscopia eletrônica de transmissão. O acompanhamento fenológico foi realizado mensalmente e os índices de atividade e de intensidade foram utilizados para analisar as fenofases reprodutivas e vegetativas, respectivamente. Para a investigação dendrocronológica, foram coletadas amostras com auxílio de sonda de Pressler, as quais foram polidas e observadas sob microscópio estereoscópico. Os resultados evidenciaram um ciclo anual de atividade e dormência cambial, caracterizados, respectivamente, pela presença de células em processo de divisão e diferenciação junto ao câmbio e de células completamente diferenciadas e deposição de calose em elementos de tubo crivado adjacentes à zona cambial. A dormência cambial coincidiu com a senescência e queda foliar, enquanto a atividade foi mais evidente na presença de folhas adultas na copa. A sazonalidade da atividade cambial apresentou correlação significativa com os dados de temperatura, precipitação e fotoperíodo do mês de realização das coletas. Foi constatado o regime sazonal da atividade cambial em associação ao clima e ao comportamento fenológico da espécie, conferindo caráter anual aos anéis de crescimento. Os resultados permitiram estabelecer o padrão dendroecológico de C. robustum e as idades e taxas de crescimento da população estudada.

Os esquemas de FORÇA e a metáfora da GUERRA: uma análise sociocognitiva dos usos do mas em mediação

Neste estudo qualitativo, objetiva-se descrever os usos do conector mas em um corpus de mediação endoprocessual, à luz da Linguística Cognitiva, baseando-se, sobretudo, na Teoria da Metáfora Conceptual e nos conceitos de categorização, esquemas imagéticos e modelos cognitivos idealizados (MCIs). Investigam-se as bases cognitivas que fundamentam os sentidos do mas e a função argumentativa desse conector na mediação, a partir de duas hipóteses gerais, a saber: (i) defende-se que o conector mas funciona como um gatilho para a ativação do MCI de guerra, em termos do qual é conceptualizado o conceito de discussão, como afirmam Lakoff e Johnson (2002[1980]); e (ii) acredita-se que tal conector possa ser caracterizado como uma categoria radial, formada a partir dos diferentes esquemas imagéticos que fundamentam as ocorrências desse elemento na interação. Tendo em vista essas hipóteses, objetiva-se: (i) apontar as funções argumentativas do mas na mediação, sinalizadas pelos mapeamentos metafóricos ativados durante a discussão e (ii) descrever os sentidos evidenciados pelos usos do mas no gênero analisado, os quais são evocados pelos diferentes esquemas imagéticos em que se baseiam. Os resultados indicam que esse conector pode ser compreendido como uma categoria radial, formada a partir de esquemas de força distintos. Além disso, verifica-se que os três usos mais próximos ao centro da categoria relacionam-se fortemente a um confronto ou a uma disputa de posição entre os participantes da interação, enquanto os três mais periféricos são estreitamente ligados a uma estratégia de manutenção da posição argumentativa do falante. Considera-se que esta pesquisa possa colaborar para o estudo do conector mas, devido à observação do comportamento semântico-discursivo desse item em um gênero pouco contemplado, a mediação; e, devido à escolha do paradigma adotado, que permite analisar o conector em todas as suas ocorrências, não havendo necessidade de separar os usos chamados de interfrásticos daqueles denominados inícios acessórios ou pré-começos

Characteristics of large-sized ruby crystal grown by temperature gradient technique

Large ruby with the size of circle divide75 x 45 mm was grown by temperature gradient technique for the first time. Absorption spectrum was carried out in the range of 190-800 nm by spectrophotometer, and the concentration spatial distribution of Cr3+ in ruby was calculated from the absorption coefficient that based on the Beer-Lambert's Law. Cr3+ ions gradually increase alone both the growth axis and the radial direction. The shape and ingredient of the inclusions were measured by means of Leitz ride field microscopy and scanning electron microscopy. Lane photos and X-ray omega scan show the good quality of as grown ruby. The optimized growth conditions were pointed out based on the observation. (C) 2004 Elsevier B.V. All rights reserved.

Yb：Ca5（PO4）3F激光晶体的生长缺陷

采用提拉法生长了质量优异的Yb：Ca5（PO4）2F（Yb：FAP）晶体。运用化学腐蚀，光学显微镜、扫描电子显微镜以及能量散射光谱仪观察了该晶体中的生长条纹和包裹物等宏观缺陷，以及晶体的位错腐蚀形貌、位错密度及其分布情况，同时观察了晶体中亚晶界的形态。由晶体中位错的径向变化以及生长条纹可知：晶体在生长过程中为微凸界面生长。高温下CaF2的挥发造成了在晶体生长后期熔体中组分偏离化学计量比，出现组分过冷，形成包裹物。且位错密度显著增加。Yb：FAP晶体的各向异性使得晶体在（10 10）面的位错蚀坑形状、大小以

Efeitos da programação por nicotina durante a lactação nos níveis de comportamentos associados à ansiedade, busca por novos estímulos e aprendizagem/memória em ratos Wistar adolescentes e adultos

A exposição materna à nicotina durante a lactação em ratos programa para hiperleptinemia e hipotireoidismo na prole adulta. Alterações nos níveis desses hormônios alteram o comportamento. Por isso, resolvemos investigar os efeitos comportamentais a curto e a longo prazo da programação neonatal pela nicotina em ratos Wistar. Foram implantadas minibombas em ratas lactantes contendo nicotina (NIC = 6mg/Kg/Dia) ou uma solução com uma concentração equivalente de solução salina (CON) do 2o dia ao 19o dia de vida pós natal. Sessenta e dois ratos NIC e 48 CON foram testados de acordo com o seguinte protocolo: 1) Em PN30 ou PN75 foram avaliados os níveis de ansiedade no labirinto em cruz elevado (LCE). Entradas em cada área do labirinto (braços abertos e fechados e centro) foram gravadas por um período de 10 minutos; 2) Uma hora após, os animais foram testados no campo vazado (CV) para analisarmos o comportamento de busca por novos estímulos. Os animais tinham 10 minutos para explorar o aparelho. O número de orifícios explorados foi anotado. 3) Em PN31-35 ou PN76-80 o animal foi submetido ao labirinto aquático radial de oito braços (LAROB) para avaliarmos a memória e o aprendizado. Cada animal foi testado 4 vezes por dia durante 5 dias consecutivos sendo a plataforma mantida no mesmo braço durante os 4 primeiros dias e trocada no quinto dia. Eles tinham 2 minutos para encontrar a plataforma de escape. A latência para encontrar a plataforma foi anotada. O percentual de tempo gasto no braço aberto no LCE para os animais NIC em PN30 (6,41,1 %) foi significativamente (ANOVA: P=0,024) menor que o grupo controle PN30 (9,91,4 %). O percentual de entradas no braço aberto foi significativamente menor (ANOVA: P=0,04) para os animais do grupo NIC em PN30 (32,42,9 %) quando comparados com o grupo controle PN30 (38,51,8 %). Não foi observada diferença (ANOVA: P>0,1) entre os grupos no número de entradas no braço fechado para as duas idades. Para o CV não houve diferença entre os grupos para as duas idades (ANOVA: P>0,1). No LAROB, os animais PN75 NIC (27424 s) tiveram uma diminuição significativa (ANOVA: P<0,006) na latência para encontrar a plataforma quando comparado ao grupo controle PN75 nos 4 primeiros dias (41045 s), não havendo diferença no 5o dia. Não houve diferença em PN30 (ANOVA:P>0,1). A programação neonatal pela nicotina resultou em um efeito a curto prazo no aumento dos níveis de ansiedade na adolescência. Não foi observada diferença no comportamento de busca por novos estímulos. Entretanto a programação neonatal por nicotina resultou em um efeito a longo prazo no comportamento-cognitivo observado pelo melhor desempenho na memória/aprendizado quando adulto.

伦纳德琼斯薄膜材料导热系数的分子动力学研究

提出从微观的角度,借助计算机工具,将薄膜破坏发展的细节展现出来的分子动力学研究的思想。使得实验上难以观察的现象变得形象而便于理解。应用分子动力学理论,使用伦纳德琼斯势函数,采用预校正积分法和虚拟外力约束标定方法,模拟薄膜体系的传热系数受体系的密度、温度的影响,同时结合体系粒子的径向分布函数和长程分布函数分析了相应的系统结构特性。另外,采用不同的模拟尺寸获得了低维材料所特有的“高温尺寸效应”。结果显示,导热系数随密度的增加变大,随温度的上升而变大。这些数据现有测量手段是难以得到的,这类模拟可以为研究提供一些

Structural Integrity of the Contralesional Hemisphere Predicts Cognitive Impairment in Ischemic Stroke at Three Months

After stroke, white matter integrity can be affected both locally and distally to the primary lesion location. It has been shown that tract disruption in mirror's regions of the contralateral hemisphere is associated with degree of functional impairment. Fourteen patients suffering right hemispheric focal stroke (S) and eighteen healthy controls (HC) underwent Diffusion Weighted Imaging (DWI) and neuropsychological assessment. The stroke patient group was divided into poor (SP; n = 8) and good (SG; n = 6) cognitive recovery groups according to their cognitive improvement from the acute phase (72 hours after stroke) to the subacute phase (3 months post-stroke). Whole-brain DWI data analysis was performed by computing Diffusion Tensor Imaging (DTI) followed by Tract Based Spatial Statistics (TBSS). Assessment of effects was obtained computing the correlation of the projections on TBSS skeleton of Fractional Anisotropy (FA) and Radial Diffusivity (RD) with cognitive test results. Significant decrease of FA was found only in right brain anatomical areas for the S group when compared to the HC group. Analyzed separately, stroke patients with poor cognitive recovery showed additional significant FA decrease in several left hemisphere regions; whereas SG patients showed significant decrease only in the left genu of corpus callosum when compared to the HC. For the SG group, whole brain analysis revealed significant correlation between the performance in the Semantic Fluency test and the FA in the right hemisphere as well as between the performance in the Grooved Pegboard Test (GPT) and theTrail Making Test-part A and the FA in the left hemisphere. For the SP group, correlation analysis revealed significant correlation between the performance in the GPT and the FA in the right hemisphere.