^(18)O/^(16)O and D/H studies on the interactions between heated meteoric ground waters and igneous intrusions: Western San Juan Mountains, Colorado and the Isle of Skye, Scotland

Detailed oxygen, hydrogen and carbon isotope studies have been carried out on igneous and metamorphic rocks of the Stony Mountain complex, Colorado, and the Isle of Skye, Scotland, in order to better understand the problems of hydrothermal meteoric water-rock interaction.

The Tertiary Stony Mountain stock (~1.3 km in diameter), is composed of an outer diorite, a main mass of biotite gabbro, and an inner diorite. The entire complex and most of the surrounding country rocks have experienced various degrees of ¹⁸O depletion (up to 10 per mil) due to interaction with heated meteoric waters. The inner diorite apparently formed from a low-¹⁸O magma with δ¹⁸O ≃ +2.5, but most of the isotopic effects are a result of exchange between H₂O and solidified igneous rocks. The low-¹⁸O inner diorite magma was probably produced by massive assimilation and/or melting of hydrothermally altered country rocks. The δ¹⁸O values of the rocks generally increase with increasing grain size, except that quartz typically has δ¹⁸O = +6 to +8, and is more resistant to hydrothermal exchange than any other mineral studied. Based on atom % oxygen, the outer diorites, gabbros, and volcanic rocks exhibit integrated water/rock ratios of 0.3 ± 0.2, 0.15 ± 0.1, and 0.2 ± 0.1, respectively. Locally, water/rock ratios attain values greater than 1.0. Hydrogen isotopic analyses of sericites, chlorites, biotites, and amphiboles range from -117 to -150. δD in biotites varies inversely with Fe/Fe+Mg, as predicted by Suzuoki and Epstein (1974), and positively with elevation, over a range of 600 m. The calculated δD of the mid-to-late-Tertiary meteoric waters is about -100. Carbonate δ¹³C values average -5.5 (PDB), within the generally accepted range for deep-seated carbon.

Almost all the rocks within 4 km of the central Tertiary intrusive complex of Skye are depleted in ¹⁸O. Whole-rock δ¹⁸O values of basalts (-7. 1 to +8.4), Mesozoic shales (-0.6 to + 12.4), and Precambrian sandstones (-6.2 to + 10.8) systematically decrease inward towards the center of the complex. The Cuillin gabbro may have formed from a ¹⁸O-depleted magma (depleted by about 2 per mil); δ¹⁸O of plagioclase (-7.1 to + 2.5) and pyroxene (-0.5 to + 3.2) decrease outward toward the margins of the pluton. The Red Hills epigranite plutons have δ¹⁸O quartz (-2.7 to + 7.6) and feldspar (-6.7 to + 6.0) that suggest about 3/4 of the exchange took place at subsolidus temperatures; profound disequilibrium quartz-feldspar fractionations (up to 12) are characteristic. The early epigranites were intruded as low-¹⁸O melts (depletions of up to 3 per mil) with δ¹⁸O of the primary, igneous quartz decreasing progressively with time. The Southern Porphyritic Epigranite was apparently intruded as a low-¹⁸O magma with δ¹⁸O ≃ -2.6. A good correlation exists between grain size and δ¹⁸O for the unique, high-¹⁸O Beinn an Dubhaich granite which intrudes limestone having a δ¹⁸O range of +0.5 to +20.8, and δ¹³C of -4.9 to -1.0. The δD values of sericites (-104 to -107), and amphiboles, chlorites, and biotites (-105 to -128) from the igneous rocks , indicate that Eocene surface waters at Skye had δD ≃ -90. The average water/rock ratio for the Skye hydrothermal system is approximately one; at least 2000 km³ of heated meteoric waters were cycled through these rocks.

Thus these detailed isotopic studies of two widely separated areas indicate that (1) ¹⁸O-depleted magmas are commonly produced in volcanic terranes invaded by epizonal intrusions; (2) most of the ¹⁸O-depletion in such areas are a result of subsolidus exchange (particularly of feldspars); however correlation of δ¹⁸O with grain size is generally preserved only for systems that have undergone relatively minor meteoric hydrothermal exchange; (3) feldspar and calcite are the minerals mos t susceptible to oxygen isotopic exchange, whereas quartz is very resistant to oxygen isotope exchange; biotite, magnetite, and pyroxene have intermediate susceptibilities; and (4) basaltic country rocks are much more permeable to the hydrothermal convective system than shale, sandstone, or the crystalline basement complex.

Ground-state energy shifts of H-like Ti under dense and hot plasma conditions

In this study, by adopting the ion sphere model, the self-consistent. field method is used with the Poisson-Boltzmann equation and the Dirac equation to calculate the ground-state energies of H-like Ti at a plasma electron density from 10(22) cm(-3) to 10(24) cm(-3) and the electron temperature from 100 eV to 3600 eV. The ground-state energy shifts of H-like Ti show different trends with the electron density and the electron temperature. It is shown that the energy shifts increase with the increase in the electron density and decrease with the increase in the electron temperature. The energy shifts are sensitive to the electron density, but only sensitive to the low electron temperature. In addition, an accurately fitting formula is obtained to fast estimate the ground-state energies of H-like Ti. Such fitted formula can also be used to estimate the critical electron density of pressure ionization for the ground state of H-like Ti.

Reproduction in Gammarus (Crustacea, Amphipoda): basic processes

Research on the basic reproduction processes of Gammarus is summarized and reviewed, reproductive strategies in males and females being left to two later papers. The author describes the reproductive systems, the development of eggs (oocytes) in the ovaries, courtship and precopulatory amplexus, mating and the production of sperms, egg laying, mortality and diapause.

利用本征脸方法减少冷原子云吸收成像照片中的干涉条纹

本征脸方法是广泛应用于人脸识别的一种图像处理方法，本文将其引入到原子芯片上囚禁的冷原子云吸收成像照片的图像处理中，以减少其中的干涉条纹，增加信噪比。本文首先介绍了吸收成像照片的标准处理方法以及干涉条纹的产生原因，由于参考照片和吸收成像照片中的干涉条纹会发生随机的相对变化，处理后干涉条纹难以消除。和标准的处理方法相比，本征脸方法不是使用1张而是50张参考照片，利用这些照片重构出一张新的参考照片，这张照片比那50张中的任何一张都更近似于吸收成像照片，因此和只使用1张参考照片相比，处理之后的干涉条纹对比度明显降

Reprodutibilidade de um índice para diagnóstico e avaliação da atividade de lesões de cárie dentária na dentição decídua

O objetivo do presente estudo clínico é verificar a reprodutibilidade intra e interexaminadores de um critério de diagnóstico de cárie dentária (Nyvad et al. 1999) aplicado na dentição decídua, e avaliar o tempo médio necessário para a realização do exame clínico utilizando o referido critério. O mesmo é baseado na combinação de métodos visuais e táteis e propõe a diferenciação entre lesões ativas e inativas, tanto para lesões cavitadas quanto para não cavitadas. A amostra total consistiu de 80 crianças de três a sete anos de idade, de ambos os sexos, estudantes do Centro Educacional Terra Santa (Petrópolis/ RJ). Os responsáveis assinaram um termo de consentimento livre e esclarecido e o trabalho foi aprovado pelo Comitê de Ética em Pesquisa do HUPE-UERJ. Os exames foram realizados após escovação supervisionada, em consultório odontológico sob iluminação artificial, após 3-5s de secagem com ar comprimido, por dois examinadores treinados pelas autoras do índice e calibrados. As concordâncias intra e interexaminadores foram avaliadas pelo percentual de concordância (%) e pelo teste kappa (k), considerando a superfície dentária como unidade de análise e os seguintes pontos de corte: 1) hígida versus cariada; 2) ativa versus inativa; 3) descontinuidade versus hígida; e 4) cavitada versus hígida. O % e o valor de k para confiabilidade interexaminadores para cada ponto de corte foram: 1) % = 0,97 e k = 0,82 (IC: 0,80 - 0,85); 2) % = 0,98 e k = 0,80 (IC: 0,76 - 0,83); 3) % = 0,99 e k = 0,90 (IC: 0,88 - 0,93); 4) % = 99,0 e k = 0,95 (IC: 0,92 - 0,97). O % e o valor de k para confiabilidade intraexaminador para cada ponto de corte foram: 1) % = 0,98 e k = 0,86 (IC: 0,84 - 0,86); 2) % = 0,99 e k = 0,86 (IC: 0,83 - 0,89); 3) % = 0,99 e k = 0,94 (IC: 0,92 - 0,96); 4) % = 0,99 e k = 0,98 (IC: 0,96 - 0,99). O maior % de discordância (65,3% - 158/242) concentrou-se na diferenciação entre supefícies hígidas e lesões não cavitadas: 33,5% (81/242) entre superfície hígida e lesão não cavitada inativa; 26,0% (63/242), entre superfície hígida e lesão não cavitada ativa; e 5,8% (14/242), entre lesão não cavitada ativa e lesão não cavitada inativa. O tempo necessário para realização do exame clínico foi em média 226,5s (128,53). Conclui-se que o índice apresentou reprodutibilidade variando de substancial à quase perfeita e um tempo de exame viável, mostrando-se consistente e reproduzível para a realização de estudos clínicos de cárie dentária na dentição decídua.

El Reto de la Gestión de la Calidad y sus Costes en las Entidades No Lucrativas. Modelo y Aplicación al País Vasco

442 p.

Histochemical data on the skin mucous cells during the development of the trout [Translation from: Bollettino della Societa Italiana di Biologia Sperimentale 45, 1273-1276, 1969]

In the skin of Salmo irideus the production of mucus is due to one type of cell specialized as a mucus cell. The histochemical research presented in this paper describes the mucous cells of Salmo irideus and demonstrates observable variation in such cells during the fish's development.

Diseño de un detector para una red de vigilancia radiológica ambiental

[ES]El objetivo de este trabajo es analizar el montaje de un contador proporcional de radiación para su uso en una red de vigilancia radiológica ambiental desde su diseño básico hasta su puesta en marcha. Se realizará un análisis de las razones que nos han llevado a elegir este tipo de contadores de ionización gaseosa (frente a otros tipos), para llegar a la conclusión de que son los más adecuados para la vigilancia radiológica ambiental. Este análisis describirá la solución a la que se ha llegado para construir un contador con los medios al alcance y el porqué de su diseño concreto, así como la metodología de trabajo que se ha seguido para la obtención del mismo. Basándonos en suposiciones teóricas derivadas del análisis geométrico de la instrumentación para la obtención de resultados previsibles, se realizará una verificación mediante ensayos técnicos en el laboratorio. Se presupuestará el material utilizado y las horas requeridas, para llevar una cuenta de lo que le ha costado al departamento y lo que le habría costado en caso de no poseer la instrumentación utilizada. Después de realizar diversos test relacionados con la instrumentación electrónica, se procederá a obtener unas conclusiones derivadas de los ensayos en el laboratorio para su posterior comparación con las estimaciones teóricas. En el anexo I se encuentran los planos de diseño que se han realizado y en el anexo II los resultados finales obtenidos de los ensayos.

A hybrid-parallel framework for the nonlinear seismic analysis of very tall buildings

FRAME3D, a program for the nonlinear seismic analysis of steel structures, has previously been used to study the collapse mechanisms of steel buildings up to 20 stories tall. The present thesis is inspired by the need to conduct similar analysis for much taller structures. It improves FRAME3D in two primary ways.

First, FRAME3D is revised to address specific nonlinear situations involving large displacement/rotation increments, the backup-subdivide algorithm, element failure, and extremely narrow joint hysteresis. The revisions result in superior convergence capabilities when modeling earthquake-induced collapse. The material model of a steel fiber is also modified to allow for post-rupture compressive strength.

Second, a parallel FRAME3D (PFRAME3D) is developed. The serial code is optimized and then parallelized. A distributed-memory divide-and-conquer approach is used for both the global direct solver and element-state updates. The result is an implicit finite-element hybrid-parallel program that takes advantage of the narrow-band nature of very tall buildings and uses nearest-neighbor-only communication patterns.

Using three structures of varied sized, PFRAME3D is shown to compute reproducible results that agree with that of the optimized 1-core version (displacement time-history response root-mean-squared errors are ~〖10〗^(-5) m) with much less wall time (e.g., a dynamic time-history collapse simulation of a 60-story building is computed in 5.69 hrs with 128 cores—a speedup of 14.7 vs. the optimized 1-core version). The maximum speedups attained are shown to increase with building height (as the total number of cores used also increases), and the parallel framework can be expected to be suitable for buildings taller than the ones presented here.

PFRAME3D is used to analyze a hypothetical 60-story steel moment-frame tube building (fundamental period of 6.16 sec) designed according to the 1994 Uniform Building Code. Dynamic pushover and time-history analyses are conducted. Multi-story shear-band collapse mechanisms are observed around mid-height of the building. The use of closely-spaced columns and deep beams is found to contribute to the building's “somewhat brittle” behavior (ductility ratio ~2.0). Overall building strength is observed to be sensitive to whether a model is fracture-capable.