Antiguo Poblado de Algarrobito ubicado en el Valle del Elqui Chile, y su Patrón Urbano Bioclimático

La importancia de conocer bien el entorno para un proyecto arquitectónico es que podemos adaptarlo a nuestras necesidades fisiológicas de Confort Térmico. Podemos decir entonces que el edificio juega un papel fundamental como técnica de control de nuestro entorno. El edificio nos debería entregar un entorno controlado para que nos sintamos bien térmicamente, considerando además, que la arquitectura por sí misma puede lograr dicho confort la mayor parte de las veces. De no ser así, los usuarios tienden a colocar elementos mecánicos, para generar frío o calor artificialmente. Es fundamental entonces que nuestros edificios, tengan una correcta interacción con los recursos naturales del lugar para lograr dicho confort térmico. Pero lograr el Confort Térmico en todos los edificios de una ciudad como unidad, no logrará que la ciudad entera sea confortable térmicamente, ya que las complejas interacciones hacen que la problemática se deba enfrentar como algo sistémico. Esto quiere decir, que para que una ciudad o un conjunto logren la Confortabilidad Térmica deseada por sus habitantes debiera haber sido planificada conforme a variables urbanas que interactúen con el medio natural en forma eficiente. Con la observación de ciertos conjuntos habitacionales antiguos en el interior del Valle del Elqui, Chile y de sus relaciones entre variables urbanas y naturales, queda de manifiesto ciertas características que conllevan a pensar que existió una planificación ambiental en éstos que llevaron a lograr un conjunto con características bioclimáticas. Las evidencias de la existencia en primer lugar de un patrón urbanístico en dichos conjuntos habitacionales antiguos, hacen pensar que dicho patrón se trataría de un patrón bioclimático rural planificado, lo que hace que exista un gran interés por el estudio de estos conjuntos. Hasta ahora, en Chile, los pocos estudios de Confort Térmico que existen, están orientados a edificaciones aisladas, al Confort térmico interior de la edificación en el ámbito urbano, y en nada a Patrones Bioclimáticos de Conjuntos Habitacionales en una situación de ruralidad como a la referida en esta investigación. Además, los estudios referidos al clima urbano, difieren a los del clima rural, por lo que se necesitan mayores estudios aún para comprender mejor la problemática. Es por esto, que la mayoría de los casos mencionados en este estudio son contextualizados al ámbito urbano por carecer de otros estudios rurales. Es en este sentido que esta investigación cobra real importancia y pretende establecer la relación existente entre las variables morfológicas rurales y los recursos naturales del lugar y que generan un confort térmico ideal para sus habitantes, al mismo tiempo, se analiza la existencia de un Patrón Bioclimático en un poblado denominado Algarrobito ubicado en la cuenca del Valle del Elqui, Chile. Es en este sentido que el propósito principal de este trabajo es determinar la real existencia de un Patrón Bioclimático que relacione la morfología rural y edificada de los antiguos poblados pertenecientes a la cuenca del Valle de Elqui Chile con el microclima del lugar. La metodología empleada se basa en realizar primeramente el estudio del microclima del lugar a través de las Cartas Bioclimáticas. Para ello se obtuvo información de datos climatológicos de las estaciones meteorológicas ubicadas en la cuenca del Valle de Elqui, principalmente las más cercanas al lugar de estudio. Mediante una revisión exhaustiva de la información arquitectónica, así como de una labor de reconocimiento en terreno realizada en el poblado seleccionado y de la aplicación del Climograma local, se identificaron las diferentes zonas bioclimáticas del poblado antiguo y potenciales áreas de estudio en el conjunto. Esta actividad incluyó un estudio preliminar de la energía solar local, vientos, humedad, temperaturas y su interacción con el conjunto, permitiendo una primera aproximación a la problemática del espacio exterior y las viviendas. Esto permitió en base a las condicionantes del lugar, la arquitectura vernácula y los materiales descubrir un Patrón en el antiguo conjunto que permitía entregar confortabilidad térmica a sus habitantes y darse cuenta también, que el nuevo conjunto emplazado en el sector no seguía ese patrón con las disfuncionalidades que ello llevaba. Con esto quedó demostrado en primer lugar la existencia de un Patrón Bioclimático rural, los beneficios del patrón, la importancia de éste como causante de Confortabilidad Térmica del conjunto, y por ende de mejor eficiencia energética, así como también, que el nuevo conjunto no sigue para nada este Patrón, pero que existe también la posibilidad de rectificación y por supuesto, que los nuevos desarrollos residenciales del Valle del Elqui, puedan planificarse en base al patrón bioclimático descubierto. ABSTRACT Knowing the environment of an architectonic proyect is really important for adjusting it to our physiological needs of Thermal Comfort. So we can say that the building plays a key role as a technique of control of our environment. The building should give us a controlled environment to make us feel good thermally, and it usually can reach pleasurable temperatures by itself. If it isn't like that, people cooled or heated the ambience with mechanical elements. So a correct interaction between the buildings and natural resources is important to reach a thermal comfort. But achieving Thermal Comfort in all the buildings of a city as a unit will not achieve the whole city is thermally comfortable, because the complex interactions cause the problem needs to be solved as something systemic. This means that for a city or a set reach the Thermal Comfortability desired by its inhabitants, it should have been planned according to the urban variables that interact with the natural environment efficiently. Observing some old housing complexes in Elqui Valley, Chile, and the relationships between their natural and urban variables, some features lead to think that the environmental planning in these led to achieve a set with bioclimatic features. First, the evidences about the existence of an urban pattern in those old housing complexes, make thinking that the pattern would be a planned urban pattern, which generates interest in its study. In Chile, there have been few studies about Thermal Comfort, oriented to isolated buildings and indoor thermal comfort, but Bioclimatic Urban Patterns haven't been studied at all. In this sense, this investigation acquires a real importance and pretends to establish the relationship between urban variables and natural resources of the place that generates a good thermal comfort for its habitants. At the same time, the existence of a Bioclimatic Urban Pattern in Algarrobito, located in Elqui Valley basin, Chile, is analized. It is in this sense that the main purpose of this work is to determine the real existence of a Bioclimatic Urban Pattern, that links the urban and constructive form of the old villages of it with its microclimate. The methodology used is based on performing first the study of the microclimate of the place through the Bioclimatic Cards. To do this, weather stations, located in Elqui valley, near the place that was studied, were used to obtain information of climatological data. The different bioclimatic zones to the old town and potential areas of study in the set were identified, through an exhaustive review of the architectural information, a field reconnaissance work performed on the selected town and the application of the Local Climograph. This activity included a preliminary study of the local solar energy, the winds, the moisture, the temperatures, and their interaction with the set, allowing a first aproximation to troubles of outer space and housing. This allowed, based on the conditions of the place, vernacular architecture and materials, discovering an urban pattern in the old set, which allowed to give thermal comfort to its inhabitants and realize that the new set of the place did not follow this pattern, with the dysfunctions that it carried. These points demonstrated, in first place, the existence of a Bioclimatic Urban Pattern, the benefits of it, the importance of it as a cause of Thermal Comfortability, and therefore a better efficiency of energy, also that the new set doesn’t follow this Pattern at all, but that the posibility of rectification exists and, of course, that the new residencial development in Elqui Valley can be planned based on bioclimatic pattern discovered.

Late Quaternary extinction of a tree species in eastern North America

Widespread species- and genus-level extinctions of mammals in North America and Europe occurred during the last deglaciation [16,000–9,000 yr B.P. (by 14C)], a period of rapid and often abrupt climatic and vegetational change. These extinctions are variously ascribed to environmental change and overkill by human hunters. By contrast, plant extinctions since the Middle Pleistocene are undocumented, suggesting that plant species have been able to respond to environmental changes of the past several glacial/interglacial cycles by migration. We provide evidence from morphological studies of fossil cones and anatomical studies of fossil needles that a now-extinct species of spruce (Picea critchfieldii sp. nov.) was widespread in eastern North America during the Last Glacial Maximum. P. critchfieldii was dominant in vegetation of the Lower Mississippi Valley, and extended at least as far east as western Georgia. P. critchfieldii disappeared during the last deglaciation, and its extinction is not directly attributable to human activities. Similarly widespread plant species may be at risk of extinction in the face of future climate change.

Camp, court and siege; a narrative of personal adventure and observation during two wars: 1861-1865; 1870-1871.

The writer served successively on the staffs of Generals T. Williams, T.W. Sherman, and W.B. Franklin, 1862-1864 and E.R.S. Canby, 1865 in Louisiana and the lower Mississippi Valley; and was assistant secretary and secretary of the U.S. legation at Paris, 1866-1871.

Transportation lines on the Mississippi River system and the Gulf intercoastal waterway.

"Compiled 1968- under the supervision of the Division Engineer, United States. Army Engineer Division Lower Mississippi Valley."

Pa Mong Project, Laos-Thailand : stage 1--interim report.

"Prepared for the Committee for Co-ordination of Investigations of the Lower Mekong Basin (Cambodia, Laos, Thailand, Republic of Vietnam) under agreement with the Agency for International Development, United States Department of State by Bureau of Reclamation, United States Department of the Interior"--Cover.

Methodism and early days in Stephens City, Virginia. 1732-1905.

"Dedicatory [note]" signed: Inez Virginia Steele.

Characterization of Organophosphate Pesticides in Urine and Home Environment Dust in an Agricultural Community

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

Mesozoic to recent evolution of the Andean forearc of northern Chile (22-24 s)

The Andean forearc of northern Chile comprises four morphotectonic units, which include from east to west: 1) The Cordillera de la Costa: composed of Jurassic granites and andesites, thought to represent a volcanic arc, the Mejillones terrane, an accreted allochthonous terrane, and the Lower Cretaceous Coloso basin, which formed through forearc extension along the suture between the Mejillones terrane and the Jurassic arc. Palaeomagnetic studies of the above units have identified approximately 29+/-11 degrees of clockwise rotation. Rotation is due to extension (caused by subduction roll back and slab pull), at an angle to the direction of absolute motion of the South American Plate. 2) The Central Depression: a large arid basin containing isolated fault-bounded blocks of pre-Mesozoic metamorphosed igneous rocks, Triassic sediments and volcanics, and Jurassic carbonates, deposited in a. back-arc basin setting. The isolated blocks formed through extension along previous thrust faults, these originated through compression of the back-arc basin due to accretion of the Jurassic volcanic arc. 3) The Precordillera.: composed of Permian-Triassic rift-related sediments and volcanics, Jurassic continental sediments synchronous with back-arc basin sedimentation, and Cretaceous and Oligo-Miocene continental sediments deposited in foreland basins. Palaeomagnetism has identified clockwise rotation in rocks ranging in age from Jurassic-Miocene. Rotation in the Precordillera. affected larger structural blocks than in the Cordillera de la Costa. 4) The Salar Depression: a. series of arid continental basins developed on continental crust. These basins nay have originated in the Triassic, when rifting of the South American craton is thought to have taken place. In conclusion, palaeomagnetic and geological evidence is consistent with the view that the north Chilean forearc was largely under an extensional stress regime. However, the presence of extensive compressional structures in Palaeocene and older rocks in the forearc together with the currently active foreland thrust belt of Argentina. indicate that throughout the evolution of the Andean Orogen, a delicate balance between compressional and extensional tectonic regimes has existed.