Paulding's Works.

Spine title.

Tre novelle inedite;

The three tales do not have individual titles.

Registrum Matthei Parker diocesis cantuariensis.

Pt. 3- has imprint: Oxford, Oxford University Press.

On My Mind

Thesis (Master's)--University of Washington, 2016-06

Seismic Response Analysis of a Full-Scale Base-Isolated Structure via Measurements and Modeling

The full-scale base-isolated structure studied in this dissertation is the only base-isolated building in South Island of New Zealand. It sustained hundreds of earthquake ground motions from September 2010 and well into 2012. Several large earthquake responses were recorded in December 2011 by NEES@UCLA and by GeoNet recording station nearby Christchurch Women's Hospital. The primary focus of this dissertation is to advance the state-of-the art of the methods to evaluate performance of seismic-isolated structures and the effects of soil-structure interaction by developing new data processing methodologies to overcome current limitations and by implementing advanced numerical modeling in OpenSees for direct analysis of soil-structure interaction.

This dissertation presents a novel method for recovering force-displacement relations within the isolators of building structures with unknown nonlinearities from sparse seismic-response measurements of floor accelerations. The method requires only direct matrix calculations (factorizations and multiplications); no iterative trial-and-error methods are required. The method requires a mass matrix, or at least an estimate of the floor masses. A stiffness matrix may be used, but is not necessary. Essentially, the method operates on a matrix of incomplete measurements of floor accelerations. In the special case of complete floor measurements of systems with linear dynamics, real modes, and equal floor masses, the principal components of this matrix are the modal responses. In the more general case of partial measurements and nonlinear dynamics, the method extracts a number of linearly-dependent components from Hankel matrices of measured horizontal response accelerations, assembles these components row-wise and extracts principal components from the singular value decomposition of this large matrix of linearly-dependent components. These principal components are then interpolated between floors in a way that minimizes the curvature energy of the interpolation. This interpolation step can make use of a reduced-order stiffness matrix, a backward difference matrix or a central difference matrix. The measured and interpolated floor acceleration components at all floors are then assembled and multiplied by a mass matrix. The recovered in-service force-displacement relations are then incorporated into the OpenSees soil structure interaction model.

Numerical simulations of soil-structure interaction involving non-uniform soil behavior are conducted following the development of the complete soil-structure interaction model of Christchurch Women's Hospital in OpenSees. In these 2D OpenSees models, the superstructure is modeled as two-dimensional frames in short span and long span respectively. The lead rubber bearings are modeled as elastomeric bearing (Bouc Wen) elements. The soil underlying the concrete raft foundation is modeled with linear elastic plane strain quadrilateral element. The non-uniformity of the soil profile is incorporated by extraction and interpolation of shear wave velocity profile from the Canterbury Geotechnical Database. The validity of the complete two-dimensional soil-structure interaction OpenSees model for the hospital is checked by comparing the results of peak floor responses and force-displacement relations within the isolation system achieved from OpenSees simulations to the recorded measurements. General explanations and implications, supported by displacement drifts, floor acceleration and displacement responses, force-displacement relations are described to address the effects of soil-structure interaction.

Sweat Lodges in Iron Age Iberian Peninsula: New Data, Typologies and Interpretations

Three questions on the study of NO Iberian Peninsula sweat lodges are posed. First, the new sauna of Monte Ornedo (Cantabria), the review of the one of Armea (Ourense), and the Cantabrian pedra formosa type are discussed. Second, the known types of sweat lodges are reconsidered underlining the differences between the Cantabrian and the Douro - Minho groups as these differences contribute to a better assessment of the saunas located out of those territories, such as those of Monte Ornedo or Ulaca. Third, a richer record demands a more specific terminology, a larger use of archaeometric analysis and the application of landscape archaeology or art history methodologies. In this way the range of interpretation of the sweat lodges is opened, as an example an essay is proposed that digs on some already known proposals and suggests that the saunas are material metaphors of wombs whose rationale derives from ideologies and ritual practices of Indo-European tradition.

A educação pré-escolar e a promoção da interculturalidade : o papel dos contos tradicionais

Relatório de Estágio apresentado à Escola Superior de Educação do Instituto Politécnico de Castelo Branco para cumprimento dos requisitos necessários à obtenção do grau de Mestre em Educação Pré-Escolar e Ensino do 1º Ciclo do Ensino Básico.

Era uma vez... Branca de Neve e a representação feminina no conto clássico e no filme espelho, espelho meu

Esta dissertação tem por objetivo analisar as mudanças ocorridas na representação feminina, ao longo do tempo, em contos de fadas e suas adaptações, através de um viés comparativo. Para esta pesquisa, selecionamos como corpus as duas versões do conto “Branca de Neve”, dos Irmãos Grimm – uma publicada entre os anos de 1812 e 1815 e a outra publicada em 1822 –, e o filme Espelho, espelho meu (2012), dirigido por Tarsem Singh com história de Melissa Wallack e roteiro de Jason Keller e Marc Klein. Nossa análise pauta-se nas informações obtidas em História da vida privada, organizada por Georges Duby e Philiphe Ariès (1991) e Minha história das mulheres, de Michelle Perrot (2008). Como principal fundamentação teórica, utilizamos as concepções de Linda Hutcheon, em especial aquelas constantes em seu livro Uma teoria da adaptação (2013). Além disso, durante a escrita desta dissertação, também fizemos uso dos estudos de Bruno Bettelheim (2007), Tomás Enrique Creus (2006) e Carl Gustav Jung (2000). Ao longo deste estudo, procuramos ainda compreender as mudanças na representação feminina nos contos de fadas clássicos, comparando-se as adaptações referidas, relacionando-as com as alterações sociais acontecidas ao longo do tempo.

Sagans betydelse för barns språkliga och emotionella utveckling i förskolan : En intervjustudie om hur pedagoger i förskolan arbetar med sagor

Syftet med denna studie är att undersöka hur pedagoger i förskolan arbetar med sagor som ett hjälpmedel till barns språkliga och emotionella utveckling. För att göra detta har jag använt kvalitativa intervjuer med fem pedagoger på tre olika förskolor. Jag har utgått från det sociokulturella perspektivet i mina intervjuer för att undersöka hur samarbetet mellan pedagoger och barn ser ut i sagoarbetet. Mitt resultat visar att pedagogerna är överens om att litteraturen är mycket viktig för barnens utveckling och att det finns många olika metoder som man kan använda sig av i arbetet med sagorna. Pedagogerna var överens om att man måste variera arbetssättet för att göra sagorna mer levande och därmed väcka barnens intresse för litteratur. 

Geoffrey Chaucer's The prologue to the book of the tales of Canterbury : The Knights tale : The nun's priest's tale /

Mode of access: Internet.

High-resolution seismic images of potentially seismogenic structures beneath the northwest Canterbury Plains, New Zealand

The transpressional boundary between the Australian and Pacific plates in the central South Island of New Zealand comprises the Alpine Fault and a broad region of distributed strain concentrated in the Southern Alps but encompassing regions further to the east, including the northwest Canterbury Plains. Low to moderate levels of seismicity (e. g., 2 > M 5 events since 1974 and 2 > M 4.0 in 2009) and Holocene sediments offset or disrupted along rare exposed active fault segments are evidence for ongoing tectonism in the northwest plains, the surface topography of which is remarkably flat and even. Because the geology underlying the late Quaternary alluvial fan deposits that carpet most of the plains is not established, the detailed tectonic evolution of this region and the potential for larger earthquakes is only poorly understood. To address these issues, we have processed and interpreted high-resolution (2.5 m subsurface sampling interval) seismic data acquired along lines strategically located relative to extensive rock exposures to the north, west, and southwest and rare exposures to the east. Geological information provided by these rock exposures offer important constraints on the interpretation of the seismic data. The processed seismic reflection sections image a variably thick layer of generally undisturbed younger (i.e., < 24 ka) Quaternary alluvial sediments unconformably overlying an older (> 59 ka) Quaternary sedimentary sequence that shows evidence of moderate faulting and folding during and subsequent to deposition. These Quaternary units are in unconformable contact with Late Cretaceous-Tertiary interbedded sedimentary and volcanic rocks that are highly faulted, folded, and tilted. The lowest imaged unit is largely reflection-free Permian Triassic basement rocks. Quaternary-age deformation has affected all the rocks underlying the younger alluvial sediments, and there is evidence for ongoing deformation. Eight primary and numerous secondary faults as well as a major anticlinal fold are revealed on the seismic sections. Folded sedimentary and volcanic units are observed in the hanging walls and footwalls of most faults. Five of the primary faults represent plausible extensions of mapped faults, three of which are active. The major anticlinal fold is the probable continuation of known active structure. A magnitude 7.1 earthquake occurred on 4 September 2010 near the southeastern edge of our study area. This predominantly right-lateral strike-slip event and numerous aftershocks (ten with magnitudes >= 5 within one week of the main event) highlight the primary message of our paper: that the generally flat and topographically featureless Canterbury Plains is underlain by a network of active faults that have the potential to generate significant earthquakes.