543 resultados para Potable


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Introducción: Según la OMS, más del 50% de la población adulta está infectada con el Helicobacter Pylori, con prevalencias de hasta el 90%. La mayoría de contagios se produce antes de los 10 años de edad. Desde el descubrimiento del H. Pylori (1983), se lo ha relacionado con la úlcera péptica, gastritis, reflujo gastroesofágico e incluso, cáncer gástrico. Metodología: Se realizó un estudio transversal analítico. La muestra estuvo conformada por 250 niños escolares de la etnia Shuar del cantón Sucúa. La prueba utilizada para la detección del Helicobacter pylori es la identificación de antígenos en las heces por inmunocromatografía. Para establecer la significancia de asociación de variables se utilizó el OR con su intervalo de confianza al 95%. Resultados: El promedio de edad fue de 8.8 años (DS 2.0), con predominio de las mujeres (54.4%). El 56.4% consume agua potable, el 71.65% vive en hacinamiento, el 42% tiene servicios de letrinización y el 49.2% cuenta con servicios de alcantarillado. Se encontró asociación significativa con el nivel de instrucción OR 1.68, IC95% (1 – 2.84), p=0.049; letrinización OR 1.99, IC95% (1.17 – 3.36), p=0.01; deposiciones al aire libre OR 4.32, IC95% (2.13 – 8.77), p=0.000. Conclusiones: La prevalencia de Helicobacter pylori es alta en la población escolar de la etnia Shuar; está asociada a un nivel bajo de instrucción de los progenitores y una inadecuada infraestructura de servicios básicos.

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Antecedentes. Las enfermedades provocadas por parásitos, constituyen problemas serios de salud en la población, presentan una alta incidencia de infección por parásitos intestinales, Objetivo: Determinar la prevalencia de parasitismo en los niños del Centro de Apoyo Nutricional y Pedagógico Santo Hermano Miguel. Cuenca Septiembre 2015 - Enero 2016. Método y materiales: Se realizó un estudio de tipo descriptivo de corte transversal. Se trabajó con una población infantil de 100 niños que va entre 5 a 11 años. Los resultados obtenidos tuvieron un uso confidencial exclusivamente para fines de investigación y fueron analizados mediante software SPSS 15 y Excel. Resultados: El 25% de la población infantil es del género masculino, y el 75 % femenino, de los cuales el 80% presenta parasitismo, el 65% mono parasitismo y el 35% poli parasitismo. Las especies patógenas observadas son: Entamoeba histolytica 85%, Giardia lamblia 3,8%, Trichomona intestinalis 1,3% y Taenia saginata 2,5%.Según las características socioeconómicas, el 100% de la población consume agua potable. El 83% se lavan las manos antes de comer, el 71% lava las frutas antes de consumirlas, el 100% utiliza el servicio sanitario, a su vez el 42% presentan dolor abdominal, el 12% presentan diarrea, el 14% tiene prurito anal y el 46% tiene falta de apetito. Conclusiones: Los hábitos de higiene personal y de alimentación no se están llevando de la forma correcta por ello existe un porcentaje alto de parasitismo, por más que se cuente con los servicios básicos, esto no garantiza un parasitismo negativo

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41 p.

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Introducción ¿Por qué Centroamérica pone tanto empeño en la prosecución de un acuerdo que implica concesiones sustanciales a EE.UU. y que, además, exige a los países centroamericanos un elevado esfuerzo de adecuación y de reducciones arancelarias? Ante el nuevo TLC de Centroamérica con los EE.UU. se pueden anticipar negociaciones en agricultura, integración de servicios y en el contenido de las leyes salariales y de regulación ambiental, Asimismo, la apertura del mercado de seguros, las telecomunicaciones, aeropuertos, etc. En la agenda de EE.UU. no se excluye nada. Todos los bienes y servicios estarán incluidos, desde productos agrícolas fuertemente subsidiados en EE.UU., hasta el agua potable seguridad social, educación universitaria y ciertos servicios bancarios

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The Upper Jefferson River is one of the most dewatered rivers in Montana. The river exists in an intermontane basin filled with sediment transported from the Highland Mountains to the west, the Tobacco Root Mountains to the east, and the Jefferson River from the south. The Upper Jefferson River Valley is highly dependent on the Jefferson River as the main industry in the valley is agriculture. A majority of the valley is irrigated and used to grow crops, and a good portion is also used for cattle grazing. The residents of the Upper Jefferson River Valley use the aquifer as the main source of potable water. The Jefferson River is also widely used for recreation. This study took place in the Waterloo area of the Upper Jefferson River Valley, approximately 20 miles south of Whitehall, Montana. The Waterloo area provides significant groundwater base flow to the Jefferson River, which is particularly important during the late irrigation season when the river is severely dewatered, and elevated surface-water temperatures occur, creating irrigation water shortages and poor trout habitat. This area contains two springfed streams, Willow Springs and Parson’s Slough, which discharge to the Jefferson River providing cool water in the late season as well as providing the most important trout spawning habitat in the valley. The area is bordered on both the east and west by irrigation ditches, and about 60% of the study area is irrigated. Tile drains were installed in the study area in close proximity to Parsons Slough causing some concern by neighboring residents. This study evaluated relationships between surface water, groundwater, and irrigation practices so that water managers and others can make informed management decisions about the Upper Jefferson River. Data was collected via a network of groundwater wells and surface-water sites. Additionally, water-quality samples were taken and an aquifer test was conducted to determine aquifer properties. The field data were analyzed and a groundwater budget was created in order to evaluate the aquifer. Results of the groundwater budget show that seepage from the irrigation canals and irrigation recharge have the biggest influence on recharge of the aquifer. There is significant groundwater outflow from the aquifer in the spring-fed streams as well as discharge to the Jefferson River. In comparing previous study results to this study’s results, there is no evidence of the water table decreasing due to irrigation practice changes or tile drain installation. However, given the amount of recharge irrigation practices contribute to the aquifer, if significant changes were made, they may affect groundwater elevations. Also lining the irrigation ditches would have a significant impact on the aquifer, as the amount of seepage would be greatly reduced.

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Access to improved potable water sources is recognized as one of the key factors in improving health and alleviating global poverty. In recently years, substantial investments have been made internationally in potable water infrastructure projects, allowing 2.3 billion people to gain access to potable water from 1990-2012. One such project was planned and installed in Solla, Togo, a rural village in the northern part of the country, from 2010-2012. Ethnographic studies revealed that, while the community has access to potable water, an estimated 45% of the village’s 1500 residents still rely on unprotected sources for drinking and cooking. Additionally, inequality in system use based on income level was revealed, with the higher income groups accessing the system more regularly than lower income groups. Cost, as well as the availability of cheaper sources, was identified as the main deterrent from using the new water distribution system. A new water-pricing scheme is investigated here with the intention of making the system accessible to a greater percentage of the population. Since 2012, a village-level water committee has been responsible for operations and maintenance (O&M), fulfilling the community management model that is recommended by many development theorists in order to create sustainable projects. The water committee received post-construction support, mostly in the form of technical support during system breakdowns, from the Togolese Ministry of Water and Sanitation (MWSVH). While this support has been valuable in maintaining a functional water supply system in Solla, the water committee still has managerial challenges, particularly with billing and fee collection. As a result, the water committee has only received 2% - 25% of the fees owed at each private connection and public tap stand, making their finances vulnerable when future repairs and capital replacements are necessary. A new management structure is proposed by the MWSVH that will pay utilities workers a wage and will hire an accountant in order to improve the local management and increase revenue. This proposal is analyzed under the new water pricing schemes that are presented. Initially, the rural water supply system was powered by a diesel-generator, but in 2013, a solar photo-voltaic power supply was installed. The new system proved a fiscal improvement for the village water committee, since it drastically reduced their annual O&M costs. However, the new system pumps a smaller volume of water on a daily basis and did not meet the community’s water needs during the dry season of 2014. A hydraulic network model was developed to investigate the system’s reliability under diesel-generator (DGPS) and solar photovoltaic (PVPS) power supplies. Additionally, a new system layout is proposed for the PVPS that allows pumping directly into the distribution line, circumventing the high head associated with pumping solely to the storage tank. It was determined that this new layout would allow for a greater volume of water to be provided to the demand points over the course of a day, meeting a greater fraction of the demand than with the current layout.

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The International Space Station (ISS) requires a substantial amount of potable water for use by the crew. The economic and logistic limitations of transporting the vast amount of water required onboard the ISS necessitate onboard recovery and reuse of the aqueous waste streams. Various treatment technologies are employed within the ISS water processor to render the waste water potable, including filtration, ion exchange, adsorption, and catalytic wet oxidation. The ion exchange resins and adsorption media are combined in multifiltration beds for removal of ionic and organic compounds. A mathematical model (MFBMODEL™) designed to predict the performance of a multifiltration (MF) bed was developed. MFBMODEL consists of ion exchange models for describing the behavior of the different resin types in a MF bed (e.g., mixed bed, strong acid cation, strong base anion, and weak base anion exchange resins) and an adsorption model capable of predicting the performance of the adsorbents in a MF bed. Multicomponent ion exchange ii equilibrium models that incorporate the water formation reaction, electroneutrality condition, and degree of ionization of weak acids and bases for mixed bed, strong acid cation, strong base anion, and weak base anion exchange resins were developed and verified. The equilibrium models developed use a tanks-inseries approach that allows for consideration of variable influent concentrations. The adsorption modeling approach was developed in related studies and application within the MFBMODEL framework was demonstrated in the Appendix to this study. MFBMODEL consists of a graphical user interface programmed in Visual Basic and Fortran computational routines. This dissertation shows MF bed modeling results in which the model is verified for a surrogate of the ISS waste shower and handwash stream. In addition, a multicomponent ion exchange model that incorporates mass transfer effects was developed, which is capable of describing the performance of strong acid cation (SAC) and strong base anion (SBA) exchange resins, but not including reaction effects. This dissertation presents results showing the mass transfer model's capability to predict the performance of binary and multicomponent column data for SAC and SBA exchange resins. The ion exchange equilibrium and mass transfer models developed in this study are also applicable to terrestrial water treatment systems. They could be applied for removal of cations and anions from groundwater (e.g., hardness, nitrate, perchlorate) and from industrial process waters (e.g. boiler water, ultrapure water in the semiconductor industry).

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This case study sought to determine how the potable water network of Cerro Prieto, Peru could be improved. The network as it exists now is branched and operated intermittently, exposing residents to water contamination risks and inconvenience. Using EPANET, it was found that the as-built network can support continuous water service, all points could stay over 10 psi, and the current water consumption rate could be maintained. To keep all points over 20 psi, the height of elevated water tank must be increased 6 feet, and the pump switched on whenever the tank drains. It was also found that almost the entire community would benefit from several possible closed loops in the network, but the high cost gives downstream loops higher priority. Due to the scarcity of water in the region, the first action must be assessing the well capacity, and a water conservation plan that may include water meters.

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The anisotropy of the Biscayne Aquifer which serves as the source of potable water for Miami-Dade County was investigated by applying geophysical methods. Electrical resistivity imaging, self potential and ground penetration radar techniques were employed in both regional and site specific studies. In the regional study, electrical anisotropy and resistivity variation with depth were investigated with azimuthal square array measurements at 13 sites. The observed coefficient of electrical anisotropy ranged from 1.01 to 1.36. The general direction of measured anisotropy is uniform for most sites and trends W-E or SE-NW irrespective of depth. Measured electrical properties were used to estimate anisotropic component of the secondary porosity and hydraulic anisotropy which ranged from 1 to 11% and 1.18 to 2.83 respectively. 1-D sounding analysis was used to models the variation of formation resistivity with depth. Resistivities decreased from NW (close to the margins of the everglades) to SE on the shores of Biscayne Bay. Porosity calculated from Archie's law, ranged from 18 to 61% with higher values found along the ridge. Higher anisotropy, porosities and hydraulic conductivities were on the Atlantic Coastal Ridge and lower values at low lying areas west of the ridge. The cause of higher anisotropy and porosity is attributed to higher dissolution rates of the oolitic facies of the Miami Formation composing the ridge. The direction of minimum resistivity from this study is similar to the predevelopment groundwater flow direction indicated in published modeling studies. Detailed investigations were carried out to evaluate higher anisotropy at West Perrine Park located on the ridge and Snapper Creek Municipal well field where the anisotropy trend changes with depth. The higher anisotropy is attributed to the presence of solution cavities oriented in the E-SE direction on the ridge. Similarly, the change in hydraulic anisotropy at the well field might be related to solution cavities, the surface canal and groundwater extraction wells.

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El presente estudio de corte descriptivo hace una revisión teórica de 68 artículos de 11 países de Latinoamérica con el fin de dar a conocer el panorama organizacional con relación a la cultura organizacional y el liderazgo en la región y cómo este ha ido evolucionando en el tiempo. La metodología utilizada se enfocó en un conteo de frecuencias usando el modelo de liderazgo y cultura organizacional de Bass y Avolio (Bass, 1999) permitiendo ordenar en tres estilos de liderazgo la información encontrada en la revisión teórica, y a su vez cada uno de los liderazgos con sus creencias, éstas tomadas como variables de la cultura organizacional. Finalmente se encontraron diferentes tipos de tendencias a nivel de los tipos de liderazgo implementados en las organizaciones y la cultura organizacional que se adopta. Se plantea la necesidad de profundizar más y de forma empírica en la temática planteada para que se conozcan las transformaciones que se han dado en el contexto organizacional y el impacto sea mayor en un futuro cercano.

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La política del comparendo ambiental como herramienta pedagógica para el adecuado manejo de los residuos sólidos, pretende responsabilizar a la ciudadanía sobre el aseo del espacio público, en tanto la gestión por sí sola del Estado o las empresas privadas no ha logrado alcanzar este objetivo. El presente trabajo busca analizar, en el marco del servicio público domiciliario de aseo, la gestión del comparendo ambiental en el espacio público de la UPZ 97 Chicó Lago del 2014 al 2016, haciendo énfasis en las relaciones de los actores desde una perspectiva de gobernanza. De esa manera nos aproximamos a la noción de la ciudadanía frente al comparendo ambiental, para determinar cómo la política incluye su participación en la gestión del aseo en el espacio público.

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El mayor consumo de agua en Costa Rica ocurre en el Valle Central, pues ahíestá asentada cerca del 60% de la población del país. Sin embargo, la disponibilidad de agua está disminuyendo debido al crecimiento demográfico y al decreciente volumen de los ríos y aguas subterráneas.El Valle Central posee cerca de 57 ríos que podrían utilizarse como fuente de agua potable. pero sólo 10 de ellos tienen sus nacientes ubicadas en bosques primarios y son adecuadas para este fin. Las nacientes de la mayoría de los otros ríos se encuentran en tierras económicamente improductivas, tales como pastizales y áreas de bosques muy alterados, que pierden su volumen de agua durante la estación seca.Las proyecciones de crecimiento demográfico hasta el año 2100 permiten visualizar un marcado incremento en la demanda de agua, el cual se mantendrá durante los próximos 50 años. Consecuentemente, para proporcionar un adecuado suministro de agua para esta creciente población. es fundamental detener la contaminación de las aguas subterráneas y recobrar el volumen de agua de los ríos.En este trabajo se propone un plan sencillo para aumentar el volumen de agua de los ríos del Valle Central y para proteger nuestros acuíferos. Se mencionan también otros beneficios económicos y sociales que tendría la aplicación de esta propuesta.Abstract: About 60% of the popuiation of Costa Rica lives in the Central Valley where consequcntly occurs the highest water consumption. As a contrast water shortness is increasing in this country due to population growth and diminishing volume of river and subterranean water.There are about 57 rivers in the Central Valley that could be used as a source of water but only 10 of them have their headwaters inside primary forest and are appropriate for this purpose. The headwaters of mosi of the nvers lay in underproductive lands such as grass fields and very disturbed forest and bose their water volume during dry season.Population growth estimates until year 2100 allow foreseeing a high rate of increase in water demand for the next 50 years. In order to have an adequate supply of water for ihis expanding population it is mandatory to stop subterranean water pollution and to recovcr nver water volume.In this paper 1 propose a simple plan to augment the water volume of the headwaters of the rivers of the Central Valley and to protect our subterranean water sources. Other social and economic benefits that stem from this plan are also analyzed.

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El departamento Capital, provincia de Catamarca, cuenta con una población de 170.000 habitantes, el recurso hídrico es escaso dado que integra la Diagonal Árida Sudamericana. La acelerada urbanización en las dos últimas décadas, la promoción industrial, el cambio del uso del suelo y las prácticas inadecuadas en el tratamiento de los residuos sólidos urbanos, ponen en riesgo las escasas fuentes de agua disponibles. El objetivo fue determinar los riesgos de contaminación de los recursos hídricos superficiales y subterráneos, originados por las actividades humanas. La vulnerabilidad de las aguas subterráneas se determinó con la metodología DIOS propuesta por Foster e Hirata (1991), adaptada también para las aguas superficiales. Los análisis físicos –químicos de las aguas, fueron realizados utilizando técnicas normalizadas según el Standard Methods for the Examination of Water and Wastewater. En sectores de alta demanda de agua subterránea, algunas perforaciones para agua potable fueron contaminadas con nitratos, superando los límites tolerables de 45 mg/l que le asigna el CAA a la potabilidad del agua. Aportes principales: el análisis geográfico integrado a una visión holística multidisciplinaria de conservación y gestión integral del recurso agua, esencial para la vida humana; la localización precisa de zonas de alto riesgo de contaminación y el auspicio de un correcto ordenamiento territorial.

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En la región Caribe algunas cuencas se vieron afectadas en su comportamiento hidrológico, como consecuencia del terremoto de abril de 1991.Un ejemplo evidente de lo anterior es la cuenca del rio Banano, que es la fuente principal del agua potable para la provincia de Limón, y que se presenta un comportamiento de rio aluvial acelerado como consecuencia de cerca de 40 millones de m3 de material deslizado. Los deslizamientos  característicos en la cuenca son deslizamientos de roca (rockslide), aunque puede observarse uno de tipo rotacional (rotational slump); además existen flujos de detritos ( debris flow). Este comportamiento acelerado origina inundaciones en poblados como Aguas Zarcas, Quitaría, Beverly; Polonia, Bomba y María Luisa. Con el fin de minimizar las consecuencias de estas inundaciones se establece una zonificación de áreas inundables para la parte baja de la cuenca en tres clases. Además, en la cuenca se registra un aporte significativo de material en suspensión, lo cual podrá alterar la posibilidad del agua. ABSTRACTThe April 1991 earthquake in Costa Rica caused changes in the hydrological characteristics of several watersheds in the Caribbean region of country.Evidence of these changes was observer in the rio Banano, the principal source of potable water for the province de Limon. The behavior of the alluvial river accelerated as a consequence of nearly 40 million cubic meters of material that moved within the watershed as a result of the earthquake. The characteristical landslides were rockslides, althoung rotational slump and debris flow slides were also observed. The accelerated hydrological changes in the river have caused flooding in populated areas such as Aguas Zarcas, Quitará, Beverly, Polonia, Bomba and Maria Luisa. In order to minimize the consequences of the flooding, the lower part of the watershed was classified in three categories according to flooding susceptibility.The river has also shown an increase in suspended material, which could affect the potability of the water.