Glacial to paraglacial history and forest recovery in the Oglio glacier system (Italian Alps) between 26 and 15 ka cal BP

The integrated stratigraphic, radiocarbon and palynological record from an end-moraine system of the Oglio valley glacier (Italian Alps), propagating a lobe upstream in a lateral reach, provided evidence for a complete cycle of glacial advance, culmination and withdrawal during the Last Glacial Maximum and early Lateglacial. The glacier culminated in the end moraine shortly after 25.8 +/- 0.8 ka cal BP, and cleared the valley floor 18.3-17.2 +/- 0.3 ka cal BP. A primary paraglacial phase is then recorded by fast progradation of the valley floor.

As early as 16.7 +/- 0.3 ka cal BP, early stabilization of alluvial fans and lake filling promoted expansion of cembran pine. This is an unprecedented evidence of direct tree response to depletion of paraglacial activity during the early Lateglacial, and also documents the cembran pine survival in the mountain belt of the Italian Alps during the last glaciation. Between 16.1 and 14.6 +/- 0.5 ka cal BP, debris cones emplacement points to a moisture increase favouring tree Betula and Pinus sylvestris-mugo. A climate perturbation renewed paraglacial activity. According to cosmogenic ages on glacial deposits and AMS radiocarbon ages from lake records in South-Eastern Alps such phase compares favourably with the Gschnitz stadial and with the oscillations recorded at lakes Ragogna. Langsee and Jeserzersee, most probably forced by the latest freshening phases of the Heinrich Event 1.

A further sharp pine rise marks the subsequent onset of Bolling interstadial. The chronology of the Oglio glacier compares closely with major piedmont glaciers on the Central and Eastern Alpine forelands. On the other hand, the results of the present study imply a chronostratigraphic re-assessment of the recent geological mapping of the Central Italian Alps. (C) 2012 Elsevier Ltd. All rights reserved.

IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0-50,000 Years Cal BP

The IntCal09 and Marine09 radiocarbon calibration curves have been revised utilizing newly available and updated data sets from C measurements on tree rings, plant macrofossils, speleothems, corals, and foraminifera. The calibration curves were derived from the data using the random walk model (RWM) used to generate IntCal09 and Marine09, which has been revised to account for additional uncertainties and error structures. The new curves were ratified at the 21st International Radiocarbon conference in July 2012 and are available as Supplemental Material at www.radiocarbon.org. The database can be accessed at http://intcal.qub.ac.uk/intcal13/.

Late-Glacial and early Holocene marine 14C reservoir ages off North Iceland (16-9 cal kyr BP)

Tephrochronological age models and 48 14C age determinations on molluscs and foraminifera (planktonic and benthic) are applied for the calculation of marine 14C reservoir age variability during a time period covering the Heinrich event H1 to early Holocene (16–9 cal kyr BP). Our data source consists of four high-resolution marine sediment cores (HM107-04, HM107-05, MD99-2271, MD99-2275) from the North Icelandic shelf. The marine reservoir age (ΔR) is found to be extremely variable, ranging from 385 to 1065 14C years. Extreme ΔR values occur at the end of H1, with values around 1000 14C years (~15 cal kyr BP), probably due to reduced northward flow of well-ventilated subtropical surface waters and a southward expansion of polar waters, as well as an expansion of sea ice limiting air-sea gas exchange. With the onset of the Bølling-Allerød interstadial, the ΔR values decrease towards 0 14C years suggesting a more vigorous North Atlantic Current and an active meridional overturning circulation system. During the Younger Dryas stadial, ΔR values are consistently around 700 14C years suggesting e renewed expansion of polar waters and a weakened meridional overtuning circulation. Interestingly, ΔR values remain high (~200 14C years) at the onset of the Holocene suggesting continued high influence of polar waters. Subsequently, ΔR values rapidly decrease to ~¬ 250 14C years around 11 cal kyr BP, indicating increased air-sea CO2 exchange with the coeval atmosphere. The ΔR values average around 0 14C years from around 10.5 to 9.0 cal kyr BP.

Incorporação de resíduos cerâmicos em argamassas de cal aérea sujeitas a condições severas de humidade e salinidade

Trabalho Final de Mestrado para obtenção do grau de Mestre em Engenharia Civil na Área de Especialização de Edificações

A influência das condições de cura nas propriedades das argamassas de cal para revestimentos antigos

Dissertação elaborada no Laboratório Nacional de Engenharia Civil (LNEC) para obtenção do grau de Mestre em Engenharia Civil na Área de Especialização de Edificações no âmbito do protocolo de cooperação entre o ISEL e o LNEC

Incorporação de resíduo da indústria petrolífera em argamassas de cal hidráulica para a reabilitação de edifícios

Trabalho Final de Mestrado para obtenção do grau de Mestre em Engenharia Civil na Área de Especialização de Edificações

ECO: argamassas de cal hidráulica para reabilitação de edifícios

Dissertação de Natureza Científica para obtenção do grau de Mestre em Engenharia Civil na Área de Especialização de Edificações

Caracterización y determinación del proceso para la producción de cal comercial a partir de la piedra caliza

La cal es un material producido a partir de la calcinación de la roca caliza y tiene diversas utilidades en el mundo de la industria como la siderúrgica, papelera, alimentaria, en la construcción, entre otras. Es fundamental conocer todas las características de la caliza para poder determinar su grado de calcinación. Con el presente trabajo se pretende estudiar las propriedades de la caliza para su posterior calcinación y el dimensionamento de una planta de producción de cal desde que el mineral llega de la explotación hasta que sale al mercado.Para determinar los equipos se calularon sus dimensiones para una producción de 600 t/h de cal, sabiendo que la planta principal de machaquero solo trabajará 5 días de la semana en jornadas de 8 horas, mientras que a partir del horno de calcinación estará en funcionamento los 7 dias de la semana, 24 horas al día. A partir de esas consideraciones se obtienen las dimensiones de todos los equipos y se realiza un estudio para la elección de un horno, o un horno de eje vertical y un horno rotativo, así como el combustible empleado, ya que es una parte fundamental para determinar los costes para la producción de cal.Tmbién fue objeto de este trabajo, el estudio ambiental de la instalación de la planta, en función de la mezcla de combustible empleada y del impacto en el entorno de la lisma, así como un estudio de viabilidad de la planta, estimando unos costes de la misma y un precio de mercado "ex Works".

Letter - Cal Cavendish to Sean O'Sullivan, 25 May 1975

A letter from Cal Cavendish of Cavenidish Country in Calgary, Alberta. Cavendish has written a song about former prime minister R. Honourable John Diefenbaker. He has included the lyrics to his song. A few of the lyrics: "...Well it took a little while, but he reached his destiny, He was right, he was wrong, but he ran this big country. He didn't waste much time when he had a job to do, He worked the House of Commons like a prairie thrashing crew. Good old John, we heard you John, when a man got paid for the job when the job got done."

Estudio del ejercicio de liderazgo en una empresa petroquímica por Rigoberto Américo Garza López

Tesis (Maestría en Ciencias de la Administración con Especialidad en Relaciones Industriales) U.A.N.L.

La morada vital y los historiable en la obra de Américo Castro

UANL

Les impacts urbains des évènements sportifs internationaux : les cas du parc municipal Américo Renné Giannetti à Belo Horizonte (Brésil) et la Coupe du monde de 2014

Cette étude a eu l’objectif d’analyser et d’identifier les différentes visions de la revitalisation du Parc Municipal Américo Renné Giannetti, à Belo Horizonte (Brésil), dans le contexte de transformations spatiales de la ville pour la Coupe du monde arrivée en 2014. Pour le développement de cette recherche, on a utilisé des démarches distinctes. La première a consisté à faire un abordage sur les projets de restructurations urbaines pour les évènements internationaux qui en transformant certains espaces (comme les parcs urbains et certaines aires historiques) tentent à dynamiser l’entrepreneuriat urbain en transformant ces espaces, les villes et les pays hôtes en « produits » consommés par un public très spécifique. Les autres étapes ont consisté à démontrer le rôle social du Parc Municipal ainsi qu’à présenter les observations de terrain et les entrevues avec les différents acteurs engagés dans la revitalisation du parc central de Belo Horizonte. L’analyse des différentes visions du projet nous a conduits à conclure que la revitalisation du parc pour la Coupe du monde a eu des enjeux politiques, touristiques, en répondant aussi les intérêts du secteur privé. Dans ce contexte les répercutions sociales sont inévitables vu qu’en répondant le besoin de certains citoyens, la transformation de l’espace entraine des exclusions et réaffirme la ségrégation dans le milieu.

L'Entrevista: Joan Ferrer. "Cal estudiar la Bíblia perquè és el fonament de la nostra cultura"

Joan Ferrer (Calella, 1960) va ser deixeble i col·laborador del filòleg Joan Coromines. És professor titular de Llengua i cultura hebrea i aramea a la Universitat de Girona. Fa unes setmanes ha presentat la primera història i gramàtica del jiddisch en castellà i prepara, juntament amb Eduard Feliu i Pere Casanellas -és a punt de sortir- el Diccionari Girona hebreu-català, català-hebreu, que també serà el primer d'aquestes característiques. Per Ferrer, l'interès per la cultura jueva no és sinó un acte de justícia, el reconeixement vers una comunitat, una llengua i una cultura que eren una part indestriable de Catalunya des de temps immemorials i que forma part d'una manera compartida d'entendre el món