561 resultados para Roof gutters
Resumo:
A little-known, but ecologically important non-geniculate coralline, Lithothamnion prolifer, is recorded from a number of tropical Indo-Pacific sites, including Fiji, Australia, Kiribati and Indonesia. The species occurs primarily on vertical walls of caves and overhangs in Fiji and Australia, but was also found as rhodoliths in Kiribati. Lithothamnion prolifer is characterized by the combination of characters which follow. The thallus is extremely glossy, smooth, and rosy coloured. Thalli usually produce complanate protuberances, but protuberances become terete when growing on well lit, horizontal substrata, when unattached, or when growing on loose substrata. Conceptacles occur mainly on the tips of protuberances, and tetra/bisporangial conceptacles are large (to 1300 mu m external diameter, with chambers up to 1100 mu m diameter). The tetra/bisporangial conceptacles are flush or only slightly raised, and often extensive and irregularly shaped (resembling small sori). They lack a raised rim, and have flattened pore plates. The rosette cells surrounding the tetra/bisporangial pore appear somewhat sunken below the surrounding roof cells in SEM, and the cells of filaments lining the pore canals of tetra/bisporangial conceptacles do not differ from the cells of filaments making up the rest of the roof. Old conceptacles persist and become buried in the thallus, and are then usually completely filled in by irregularly arranged calcified cells.
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During early mouse neural development, bone morphogenetic protein (BMP) signaling patterns the dorsal neural tube and defines distinct neural progenitor cell domains along the dorsoventral axis. Unlike the ventral signaling molecule Sonic hedgehog, which has long-range activity by establishing a concentration gradient in the ventral neural tube, these dorsally expressed BMPs appear to have a limited domain of action. This raises questions as to how BMP activity is restricted locally and how restricted BMP signaling directs dorsal neural patterning and differentiation. I hypothesize that BMPs are restricted in the dorsal neural tube for correct dorsoventral patterning. ^ Previous studies have shown that the positively charged basic amino acids located at the N-terminus of several BMPs are essential for heparin binding and diffusion. This provides a novel tool to address these questions. Here I adapted a UAS/GAL4 bigenic mouse system to control the ectopic expression of BMP4 and a mutant form of BMP4 that lacks a subset of the N-terminal basic amino acids. The target genes, UAS-Bmp4 and UAS-mBmp4 , were introduced into the Hprt locus by gene targeting in mouse embryonic stem cells. The expression of the GAL4 transactivator was driven by a roof plate specific Wnt1 promoter. ^ The bigenic mouse embryos exhibit phenotype variations, ranging from mid/hindbrain defects, hemorrhage, and eye abnormalities to vasculture formation. Embryonic death starts around E11.5 because of severe hemorrhage. The different expression levels of the activated transgene may account for the phenotype variation. Further marker analysis reveals that mutant BMP4 induces ectopic expression of the dorsal markers MSX1/2 and PAX7 in the ventral neural tube. In addition, the expression of the ventral neural marker NKX2.2 is affected by the expanded BMP4 activity, indicating that ectopic BMP signaling can antagonize ventral signaling. Comparison of the phenotypes of the Wnt1/ Bmp4 and Wnt1/mBmp4 bigenic embryos that express transgenes at the same level, respectively, shows that mutant BMP4 causes the expansion of dorsal neural fates ventrally while wild type BMP4 does not, suggesting that mutant BMP4 acts farther than wild type BMP4. Together, these data suggest that the N-terminus basic amino acid core controls BMP4 long-range activity in neural development, and that BMP signaling patterns the dorsal neural tube through a secondary signaling pathway that involves homeodomain transcription factors MSX1/2 and PAX7. ^
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This paper examines a model of resilience and provides a fictional case example from the classical musical, Fiddler on the Roof along with a discussion of how this model may be helpful in assisting families at various levels of functioning to bounce back and perhaps even experience growth through facing difficult challenges.
Resumo:
High tunnels are simple, plastic-covered, passive solar-heated structures in which crops are grown in the ground. They are used by fruit and vegetable growers to extend the growing season and intensify production in cold climates. The covered growing area creates a desert-like environment requiring carefully monitored irrigation practices. In contrast, the exterior expanse of a high tunnel generates a large volume of water with every measurable rainfall. Each 1,000 ft of high tunnel roof will generate approximately 300 gallons from a half inch of rain. Unless the high tunnel site is elevated from the surrounding area or drainage tiles installed, or other drainage accommodations are made around the perimeter, the soil along the inside edge of the high tunnel is nearly continuously saturated. High volumes of water can also create an erosion problem. The objective of this project was to design and construct a system that enables growers using high tunnels in their production operation to reduce drainage problems, erosion, and crop loss due to excess moisture in and around their high tunnel(s) without permanent environmental and soil mediations.
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La inundación repentina en áreas urbanas por sobrecarga de las redes de drenaje es un problema recurrente con impactos negativos de importancia creciente. Las cubiertas vegetadas ("naturadas") retienen parte de la lámina de agua precipitada, reduciendo el escurrimiento superficial y generando hidrogramas de escorrentía directa con caudales pico menores y más retardados. Dichas propiedades hacen que esta tecnología pueda contribuir a reducir la sobrecarga de cauces urbanos. En esta comunicación se presentan los primeros resultados (parciales) de la determinación de la eficiencia de retención hídrica (en forma indirecta a partir de la cantidad de agua percolada), en parcelas de ensayo que simulen "cubiertas naturadas", con dos profundidades de sustrato y con dos situaciones respecto a la cobertura (con y sin vegetación). Los mismos muestran una tendencia positiva de las "cubiertas naturadas" en la contribución a la reducción del escurrimiento, siendo mayor la retención en las parcelas vegetadas y sustrato de mayor espesor.
Resumo:
La inundación en áreas urbanas por sobrecarga de las redes de drenaje es un problema recurrente de importancia creciente. Las cubiertas vegetadas (naturadas) retienen parte de la lámina de agua precipitada, reduciendo el escurrimiento superficial y generando hidrogramas de escorrentía directa con caudales pico menores y más retardados. Estas propiedades hacen que esta tecnología pueda contribuir a reducir la sobrecarga de cauces urbanos. Los resultados obtenidos a lo largo de casi dos años de estudio permitieron estimar una capacidad de retención de las cubiertas ensayadas (en la Ciudad de Buenos Aires), que ha sido variable en función de la precipitación, del grado de cobertura y profundidad del sustrato. Es así que el porcentaje retenido ha sido alto (73% a 100%) con precipitaciones menores o iguales a los 20 mm, alrededor del 60% con lluvias de 35 a 40 mm, y con precipitaciones cercanas a 100 mm los porcentajes de retención se redujeron notablemente, alcanzando valores cercanos al 30%. Estos resultados posicionan las cubiertas vegetadas, para las condiciones y sitio del ensayo, como una alternativa dentro del manejo hídrico integrado en cuencas urbanas.
Análisis morfométrico in vivo de la cámara pulpar de los primeros molares en función de la ubicación
Resumo:
Se realizó un estudio a través de mediciones radiográficas en una población de Mendoza, Argentina, con el objetivo de analizar morfométricamente la cámara pulpar de primeros molares superiores e inferiores en función de la ubicación (superior / inferior). Un total de doscientos cuarenta piezas dentarias fueron seleccionadas teniendo como criterio de inclusión primeros molares superiores e inferiores sanos. Las radiografías bitewing fueron procesadas y analizadas mediante el software lmage Pro Plus 4.5. Los datos estadísticos fueron analizados mediante Test Student. Los resultados obtenidos han mostrado diferencias significativas, lo que se expresa al contrastar de acuerdo a la ubicación que los molares superiores presentaron coronas clínicas más altas, una mayor altura pulpar y una mayo1 distancia desde el surco vestibular al techo de la cámara pulpar, dl piso de la misma y a la furcación.
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Gabbroic xenoliths and diverse megacrysts (e.g., clinopyroxenes, amphiboles and plagioclases), which correspond to the lithology ranging from gabbro-norite to gabbro, occur in the Pleisto-Holocene alkali basalts from Jeju Island, South Korea. The gabbroic xenoliths consist primarily of moderate-K2O plagioclase, Ti-Al-rich clinopyroxene and CaO-rich orthopyroxene; additionally, TiO2-rich amphibole (kaersutite) and Ti-Fe oxides might or might not be present. The plagioclase is the most dominant phase (approx. 60-70 vol.%). The xenoliths and megacrysts provide evidence for the modal metasomatism of the lower continental crust by the mafic magmas during the Pleistocene. The coarse grain size (up to 5 mm), moderate Mg# [=100xMg/(Mg+Fe(total)) atomic ratio] of pyroxenes (70-77) and textural features (e.g., poikilitic) indicate that the gabbroic xenoliths are consistent with a cumulus origin. The clinopyroxenes from these xenoliths are enriched in REE with smooth convex-upward MREE patterns, which are expected for cumulus minerals formed from a melt enriched in incompatible trace elements. The strikingly similar major and trace element variations and the patterns of constituent minerals clearly indicate a genetic link between the gabbroic xenoliths (plus megacrysts) and the host basalt, indicating that the xenoliths belong to the Jeju Pleisto-Holocene magma system. On the basis of the textural features, the mineral equilibria and the major and trace element variations, the xenoliths appear to have crystallized from basaltic melts at the reservoir-roof environment within the lower crust (4-7 kbars) above the present Moho estimates beneath Jeju Island, where the xenoliths represent wall rocks. Following the consolidation of the xenolith lithologies, volatile- and incompatible element-enriched melt/fluid, as metasomatic agents, infiltrated through the grain boundaries and/or cracks and reacted with the preexisting anhydrous phases, which produced the metasomatic amphiboles. This volatile-enriched melt/fluid could have evolved from the initially anhydrous compositions to the volatile-saturated compositions by the active fractional crystallization in the Jeju Pleisto-Holocene magma system. This process was significant in that it was a relatively young event and played an important role in the formation of the hydrous minerals and the metasomatization of the lower continental crust, which is a plume-impacted area along the Asian continental margin. The major and trace element analyses of the mineral phases from the xenoliths were performed to define the principal geochemical characteristics of the crustal lithosphere segment represented by the studied xenoliths.
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Stalagmites are important palaeo-climatic archives since their chemical and isotopic signatures have the potential to record high-resolution changes in temperature and precipitation over thousands of years. We present three U/Th-dated records of stalagmites (MA1-MA3) in the superhumid southern Andes, Chile (53°S). They grew simultaneously during the last five thousand years (ka BP) in a cave that developed in schist and granodiorite. Major and trace elements as well as the C and O isotope compositions of the stalagmites were analysed at high spatial and temporal resolution as proxies for palaeo-temperature and palaeo-precipitation. Calibrations are based on data from five years of monitoring the climate and hydrology inside and outside the cave and on data from 100 years of regional weather station records. Water-insoluble elements such as Y and HREE in the stalagmites indicate the amount of incorporated siliciclastic detritus. Monitoring shows that the quantity of detritus is controlled by the drip water rate once a threshold level has been exceeded. In general, drip rate variations of the stalagmites depend on the amount of rainfall. However, different drip-water pathways above each drip location gave rise to individual drip rate levels. Only one of the three stalagmites (MA1) had sufficiently high drip rates to record detrital proxies over its complete length. Carbonate-compatible element contents (e.g. U, Sr, Mg), which were measured up to sub-annual resolution, document changes in meteoric precipitation and related drip-water dilution. In addition, these soluble elements are controlled by leaching during weathering of the host rock and soils depending on the pH of acidic pore waters in the peaty soils of the cave's catchment area. In general, higher rainfall resulted in a lower concentration of these elements and vice versa. The Mg/Ca record of stalagmite MA1 was calibrated against meteoric precipitation records for the last 100 years from two regional weather stations. Carbonate-compatible soluble elements show similar patterns in the three stalagmites with generally high values when drip rates and detrital tracers were low and vice versa. d13C and d18O values are highly correlated in each stalagmite suggesting a predominantly drip rate dependent kinetic control by evaporation and/or outgassing. Only C and O isotopes from stalagmite MA1 that received the highest drip rates show a good correlation between detrital proxy elements and carbonate-compatible elements. A temperature-related change in rainwater isotope values modified the MA1 record during the Little Ice Age (~0.7-0.1 ka BP) that was ~1.5 °C colder than today. The isotopic composition of the stalagmites MA2 and MA3 that formed at lower drip rates shows a poor correlation with stalagmite MA1 and all other chemical proxies of MA1. 'Hendy tests' indicate that the degassing-controlled isotope fractionation of MA2 and MA3 had already started at the cave roof, especially when drip rates were low. Changing pathways and residence times of the seepage water caused a non-climatically controlled isotope fractionation, which may be generally important in ventilated caves during phases of low drip rates. Our proxies indicate that the Neoglacial cold phases from ~3.5 to 2.5 and from ~0.7 to 0.1 ka BP were characterised by 30% lower precipitation compared with the Medieval Warm Period from 1.2 to 0.8 ka BP, which was extremely humid in this region.
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Manganese-iron oxide concretions are presently forming on Patrick Sill in upper Jervis Inlet. The marine geology of Patrick Sill and the adjoining basins (Queen's Reach and Princess Royal Reach) was studied to define the environment in which the concretions form. The river at the inlet head is the principal source of sediment to the upper basin. The average grain size of surficial bottom sediments within this basin decreases uniformly with distance from the source. Patrick Sill separates the upper from the lower basin. The sediment distribution pattern within the lower basin differs markedly from the upper basin as there is no dominant source of material but rather many localized sources. Abundant shallow marine faunal remains recovered in deep water sediment samples indicate that sediments deposited as deltas off river and stream mouths periodically slump to the basin floors. Geologic and optical turbidity information for the upper basin can best be explained by slumping from the delta at the inlet head with the initiation of turbidity or density currents. Patrick Sill appears to create a downstream barrier to this flow. The mineralogy of the bottom sediments indicates derivation from a granitic terrain. If this is so, the sediments presently being deposited in both basins are reworked glacial materials initially derived by glacial action outside the present watershed. Upper Jervis Inlet is mapped as lying within a roof pendant of pre-batholithic rocks, principally slates. Patrick Sill is thought to be a bedrock feature mantled with Pleistocene glacial material. The accumulation rate of recent sediments on the sill is low especially in the V-notch or medial depression. The manganese-iron oxide concretions are forming within the depression and apparently nowhere else in the study area. Also forming within the depression are crusts of iron oxide and what are tentatively identified as glauconite-montmorillonoid pellets. The concretions are thought to form by precipitation of manganese-iron oxides on pebbles and cobbles lying at the sediment water interface. The oxide materials are mobile in the reducing environment of the underlying clayey-sand sediment but precipitate on contact with the oxygenating environment of the surficial sediments. The iron crusts are thought to be forming on extensive rocky surfaces above the sediment water interface. The overall appearance and evidence of rapid formation of the crusts suggests they formed from a gel in sea water. Reserves of manganese-iron concretions on Patrick Sill were estimated to be 117 metric tons. Other deposits of concretions have recently been found in other inlets and in the Strait of Georgia but, to date, the extent of these has not been determined.
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To investigate the geochemistry of trace elements in coals from the Dingji Mine of the Huainan Coalfield, Anhui province, China, 416 borehole samples of coal, one parting, two floor and two roof mudstones were collected from 9 minable coal seams in 24 boreholes drilled during exploration. The abundances of 47 elements in each sample were determined by various instruments. The boron concentration in the coals suggests that marine influence decreased from coal seam 1 to 13-1. The geometric means of the elements Sn, Bi, Sb, and B are higher than the average for the corresponding elements in the coals from China, the U.S., and world. The enrichment of certain elements in the Shanxi or Upper Shihezi Formations is related to their depositional environment. The roof, floor and parting samples have higher contents of some elements than coal seams. The mineral matters in the coals from the Dingji Mine were found to consist mainly of granular quartz, clay minerals, and carbonate minerals. The elements are classified into two groups based on their stratigraphic distribution from coal seam 1 to 13-1, and the characteristics of each group are discussed. Based on the correlation coefficients of elemental concentrations with ash yield, four groups of elements with different affinities were identified.
Resumo:
A historical study and a construction pathology survey were conducted prior to proposing a solution for restoring the upper windows on the south side of Old San Carlos College at Saragossa (16th-17th centuries), wich had been forteited to add a third storey to the cloister. Althought initially designed to a simple large hall format, the church is a harmonius blend of Aragonese Gothic architecture and typical Jesuit scheme, consisting in a central nave flanket by chapel-confessional and raised galleries for the community. A subsequent enlargement of the roof, wich rests on the original framing over the central nave, reduced the mechanical strength of the principal rafters on the opposite side, prompting a concomitant imbalance of forces that has affected the entire structure. In view of the foregoing, in addition to restituting the upper window, the proposal solution envisages restoring the roof over the central nave to its original design, and with the interior lighting in the church.
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Canonical test cases for sloshing wave impact problems are pre-sented and discussed. In these cases the experimental setup has been simpli?ed seeking the highest feasible repeatability; a rectangular tank subjected to harmonic roll motion has been the tested con?guration. Both lateral and roof impacts have been studied, since both cases are relevant in sloshing assessment and show speci?c dynamics. An analysis of the impact pressure of the ?rst four impact events is provided in all cases. It has been found that not in all cases a Gaussian ?tting of each individual peak is feasible. The tests have been conducted with both water and oil in order to obtain high and moderate Reynolds number data; the latter may be useful as simpler test cases to assess the capabilities of CFD codes in simulating sloshing impacts. The re-peatability of impact pressure values increases dramatically when using oil. In addition, a study of the two-dimensionality of the problem using a tank con?guration that can be adjusted to 4 di?erent thicknesses has been carried out. Though the kinemat-ics of the free surface does not change signi cantly in some of the cases, the impact pressure values of the ?rst impact events changes substantially from the small to the large aspect ratios thus meaning that attention has to be paid to this issue when reference data is used for validation of 2D and 3D CFD codes.
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Proof carrying code (PCC) is a general is originally a roof in ñrst-order logic of certain vermethodology for certifying that the execution of an un- ification onditions and the checking process involves trusted mobile code is safe. The baste idea is that the ensuring that the certifícate is indeed a valid ñrst-order code supplier attaches a certifícate to the mobile code proof. which the consumer checks in order to ensure that the The main practical difñculty of PCC techniques is in code is indeed safe. The potential benefit is that the generating safety certiñeates which at the same time: i) consumer's task is reduced from the level of proving to allow expressing interesting safety properties, ii) can be the level of checking. Recently, the abstract interpre- generated automatically and, iii) are easy and efficient tation techniques developed, in logic programming have to check. In [1], the abstract interpretation techniques been proposed as a basis for PCC. This extended ab- [5] developed in logic programming1 are proposed as stract reports on experiments which illustrate several is- a basis for PCC. They offer a number of advantages sues involved in abstract interpretation-based certifica- for dealing with the aforementioned issues. In particution. First, we describe the implementation of our sys- lar, the xpressiveness of existing abstract domains will tem in the context of CiaoPP: the preprocessor of the be implicitly available in abstract interpretation-based Ciao multi-paradigm programming system. Then, by code certification to deñne a wide range of safety propermeans of some experiments, we show how code certifi- ties. Furthermore, the approach inherits the automation catión is aided in the implementation of the framework. and inference power of the abstract interpretation en- Finally, we discuss the application of our method within gines used in (Constraint) Logic Programming, (C)LP. the área, of pervasive systems
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Esta tesis analiza las acciones de los pobladores en la creación, consolidación y transformación de su hábitat y en su relación con la política pública de vivienda y barrio en Chile. A partir de la observación directa en terreno y de la revisión de material proveniente de diversas fuentes afirmamos que, aunque los pobladores han hecho un trabajo de producción del hábitat de gran magnitud y generalizado, las políticas públicas no han reconocido suficientemente su papel en la construcción de la ciudad, no han incorporado a cabalidad las potencialidades e innovaciones surgidas de sus prácticas y estrategias, y nunca les han abierto un espacio claro en la toma de decisiones y en la puesta en obra de los programas habitacionales. En el contexto latinoamericano, la política habitacional chilena de los últimos 20 años se ha considerado un éxito y un ejemplo a seguir, puesto que ha demostrado ser eficaz en la disminución del déficit habitacional. Sin embargo, ha tenido efectos urbanos y sociales nefastos, como la construcción de extensos bolsones periféricos de pobreza que se degradan aceleradamente, y la desintegración social que genera la expulsión de los sin casa a la periferia, donde pierden sus redes familiares y sociales. Desde una trinchera opuesta, los allegados, los sin casa que viven al alero de otras familias y representan la mayoría de la demanda por vivienda, exigen quedarse en barrios ya consolidados y evitan las periferias, en parte por mantener una red familiar y social que se sustenta en la proximidad física, en parte por los equipamientos y servicios con que cuentan estos barrios y la cercanía a las fuentes de empleo. Al mismo tiempo, los responsables de diseñar la política habitacional no han buscado establecer una forma de colaboración con los pobladores —principales receptores de la política— con el fin ajustar los programas públicos a las necesidades de las familias de bajos ingresos y a las realidades socioculturales de sus barrios. Por el contrario, han privilegiado una alianza con el sector privado, que conoce muy limitadamente las demandas de las familias. Así, en lugar de construir ciudades más justas, la política habitacional ha alimentado un mercado inmobiliario sustentado en la especulación del suelo y fomentado la industria de la construcción. La pregunta que guía esta investigación es cómo incorporar el conocimiento acumulado y los procedimientos probados por los pobladores al diseño y la implementación de programas habitacionales y urbanos que promuevan procesos de regeneración de las poblaciones y mejoren la distribución de la vivienda social en la ciudad. Sostenemos que los pobladores, a lo largo de una trayectoria de más de medio siglo, han adquirido y consolidado todas las competencias para construir vivienda, mejorar sus barrios e incorporarse a la discusión sobre ordenamiento territorial. Así, hoy están capacitados para asumir un papel protagónico en la definición de políticas públicas que apunte a la construcción de ciudades más sostenibles y equitativas. La producción social del hábitat vinculada al derecho a la ciudad y a la participación de los pobladores «desde abajo» está bastante documentada en la literatura latinoamericana. En Chile se han escrito numerosos trabajos y evaluaciones sobre la política habitacional, pero los estudios sobre el movimiento de pobladores, enfocados desde las ciencias sociales o multidisciplinares, tienen un auge primero, durante los años 60 y principios de los 70 y luego, en la segunda mitad de los 80, pero posteriormente dejan de publicarse, a excepción de algunas investigaciones de historia urbana o social. En cuanto a los estudios que abordan las acciones de los pobladores desde una mirada puesta en los resultados de la producción y la gestión habitacional y urbana, estos han sido especialmente escasos y ninguno abarca un período largo. La tesis aborda entonces las acciones específicas que emprenden los pobladores a distintas escalas territoriales —el conjunto, el barrio, la población, la ciudad y el país—, su relación con la política habitacional y su articulación con los demás actores que intervienen en la producción material del hábitat. Lo realizado por los pobladores se estudia a la luz del largo plazo, desde la promulgación de la primera ley de vivienda en 1906 hasta nuestros días, con el énfasis puesto entre los años 1990 y 2010, período de producción masiva y sostenida de vivienda social, financiada por el Estado y construida por el sector privado en la periferia urbana, y más detalladamente entre 2006 y 2010, cuando los pobladores irrumpen con la «gestión vecinal» y la «autogestión» como medios para implementar los programas habitacionales del gobierno. Para ello se recorre toda la trayectoria y se complementa con procesos particulares, a la manera de un lente de acercamiento con el cual se focalizan y amplifican trece casos de estudios, para ilustrar modos de producción y gestión concretos y mostrar cómo estos se inscriben en modos de hacer genéricos de los pobladores. Finalmente, con el lente centrado en el último ciclo de este proceso escribimos el capítulo inédito de los últimos veinte años de esta historia. Primero se realiza la reconstrucción de tres casos de estudio «en profundidad», que incluyen la génesis, la consolidación y las transformaciones del conjunto o barrio. Estos casos de estudio «en profundidad» se ponen en perspectiva reconstruyendo la trayectoria histórica de la producción y gestión realizada por los pobladores. Esta reconstrucción de largo período se profundiza con tres casos de estudio «específicos», de dimensión histórica, que tratan el conflicto del acceso a suelo. Finalmente se analizan las interrogantes que plantean estos procesos hoy en día para la producción y gestión de vivienda y barrio a futuro, a partir de entrevistas a actores claves y de la reconstrucción de siete casos de estudio «específicos» de acceso a suelo ilustrativos del período actual. La tesis sustenta que los pobladores, con las acciones de gestión y autogestión que realizan desde 2006, e interviniendo en la discusión sobre los instrumentos de planificación territorial a partir del mismo año, se sitúan actualmente en una nueva plataforma de acción y negociación desde la cual pueden incorporarse, con todas las competencias necesarias, a la definición de las políticas públicas y así dotarlas de pertinencia y coherencia para contribuir a superar la pobreza con respuestas más acorde a sus realidades. ABSTRACT This thesis analyzes the actions of pobladores in the creation, consolidation and transformation of their habitat and their relationship with Chilean public housing and neighbourhood policy. Through direct observation in the field and the review of material from various sources we can affirm that although the pobladores have undertaken widespread work in the production of their environment, public policies have not sufficiently recognized their role in the construction of the city. Public policy has failed to fully incorporate the potential and innovation arising from practices and strategies employed by social housing recipients and has never opened a clear space for them in decision-making or the commissioning work of the housing programs. Within the Latin America context, the Chilean housing policy of the past 20 years has been considered a success and an example to follow given that it has proven effective in reducing the housing deficit. However it has had disastrous urban and social effects, such as construction of large peripheral pockets of poverty that degrade rapidly, and generates social disintegration through the expulsion of the homeless to the periphery, where they lose their family and social networks. On another front those homeless who live under the roof of relatives and who represent the majority of demand for social housing, request to stay in consolidated neighbourhoods avoiding the periphery, partly to maintain family and social networks based on physical proximity and partly because of the facilities and services available in these neighbourhoods and their adjacency to sources of employment. At the same time, those responsible for designing housing policy have not sought to establish a form of collaboration with the pobladores in order to adjust the public programs to the needs of low-income families and the socio-cultural realities of their neighbourhoods. On the contrary an alliance with the private sector has been favored, a sector which has very limited knowledge of the demands of the recipients. Therefore instead of building more equal cities, housing policy has fueled a housing market which supports land speculation and promotes the construction industry. The question leading this research is how to incorporate the accumulated knowledge and proven procedures of the pobladores in the design and implementation of programs that promote housing and urban regeneration processes and which could improve the distribution of social housing in the city. We maintain that social housing recipients over the course of half a century have acquired and consolidated all the skills to build housing, improve neighborhoods and join the discussion on city planning. These residents are now capable of assuming a leading role in defining public policies that aim to build more sustainable and equitable cities. The social production of the environment linked to the right to the city and resident participation from the «bottom-up» is well documented in Latin American literature. In Chile there are extensive written works and assessments on housing policy with multidisciplinary or social science studies on the movement of the pobladores peaking during the 60’s and early 70’s and then again in the second half of the 80’s but afterwards this stops, with the exception of some research on social or urban history. As for studies that address the actions of the pobladores looking at the results of production and housing and urban management these have been particularly scarce and none of which cover a long period of time. The thesis then addresses the specific actions undertaken by the pobladores at different territorial levels; the housing development, the neighbourhood, the community, the city and State, and their relation to housing policy and its coordination with other actors involved in the production process of the built environment. The accomplishments of the pobladores is studied over the long term, since the enactment of the first housing law in 1906 to the present, with an emphasis between 1990 and 2010, a period of mass production and sustained social housing which was State-funded and built by the private sector in the urban periphery, and in particular between 2006 and 2010, when the pobladores break with the «neighborhood management» and «self-management» as a means to implement the housing programs of the government. To this end the entire process is outlined and is complemented by specific processes which are placed under a lens in order to focus and amplify thirteen case studies illustrating actual ways of production and management and to show how these ways of doing things are generic to the pobladores. Finally, with the lens focused on the last cycle of this process we write the new chapter of the last twenty years of this history. First there is a reconstruction of three case studies «in depth», including their origins, consolidation and the transformation of the sector or neighborhood. These «in depth» case studies are put into perspective reconstructing the historical trajectory of the production and management by the pobladores. This reconstruction over a long period is given great depth by three «specific» case studies, of historical importance, dealing with the conflict of access to land. Finally we analyze the questions raised by these processes for the production and management of housing and neighborhood in the future, based on interviews with key players and the reconstruction of seven case studies specifically regarding access to land and which are illustrative of current practice. The thesis maintains that since 2006 the pobladores through actions of management and selfmanagement and their intervention in the debate on territorial planning has placed them on a new platform for action and negotiation from which they can incorporate themselves, with all the necessary capacities, in the definition of public policy and therefore provide it with a pertinence and coherence to help towards overcoming poverty with answers more according to their realities.