39 resultados para Geosequestration of greenhouse gases
Resumo:
El impacto ambiental directo de la construcción naval, que se refiere a la construcción, mantenimiento y reparación de buques, no es de ninguna manera pequeño. La construcción de buques depende de un gran número de procesos que por sí mismos constituyen un riesgo significativo de daño medio ambiental en el entorno de los astilleros y que conducen a emisiones significativas de gases de efecto invernadero. Además, la construcción naval utiliza algunos materiales que no sólo puede llevar a graves consecuencias para el daño ambiental durante su producción y su uso en el proceso de construcción de la nave, sino también posteriormente durante la reparación de buques, el funcionamiento y las actividades de reciclaje. (OECD 2010) El impacto ambiental directo de la construcción naval constituye de por sí, un desafío importante para la industria. Pero este impacto no queda limitado a su entorno inmediato, aunque la Construcción Naval no es directamente responsable de la repercusión en el medio ambiente de la operación y el reciclaje de buques comerciales, si es una parte integral de estas actividades. (OECD 2010) En esta tesis se sugiere que el sector de la construcción naval puede y debe aceptar sus responsabilidades ambientales no solo en el entorno del astillero; también en la operación de los buques, sus productos; tomando conciencia, a través de un enfoque de ciclo de vida, del desempeño ambiental de la industria en su conjunto. Es necesario intensificar esfuerzos a medida que el impacto ambiental de la industria es cada vez más visible en el dominio público, en pro de un crecimiento verde que permita aumentar la capacidad de actividad o producción económica al tiempo que reduce o elimina, los impactos ambientales. Este será un imperativo para cualquier futura actividad industrial y exigirá naturalmente conocimiento ambiental intrincado perteneciente a todos los procesos asociados. Esta tesis - aprovechando como valiosa fuente de información los desarrollos y resultados del proyecto europeo: “Eco_REFITEC”. FP7-CP-266268, coordinado por el autor de esta Tesis, en nombre de la Fundación Centro Tecnológico SOERMAR - tiene como primer objetivo Investigar la interpretación del concepto de Construcción Naval y Transporte Marítimo sostenible así como las oportunidades y dificultades de aplicación en el sector de la Construcción y reparación Naval. Ello para crear o aumentar el entendimiento de la interpretación del concepto de transporte marítimo sostenible y la experiencia de su aplicación en particular en los astilleros de nuevas construcciones y reparación. Pretende también contribuir a una mejor comprensión de la industria Marítima y su impacto en relación con el cambio climático, y ayudar en la identificación de áreas para la mejora del desempeño ambiental más allá de las operaciones propias de los astilleros; arrojando luz sobre cómo puede contribuir la construcción naval en la mejora de la eficiencia y en la reducción de emisiones de CO2 en el transporte marítimo. Se espera con este enfoque ayudar a que la Industria de Construcción Naval vaya abandonando su perspectiva tradicional de solo mirar a sus propias actividades para adoptar una visión más amplia tomando conciencia en cuanto a cómo sus decisiones pueden afectar posteriormente las actividades aguas abajo, y sus impactos en el medio ambiente, el cambio climático y el crecimiento verde. Si bien cada capítulo de la tesis posee su temática propia y una sistemática específica, a su vez retoma desde una nueva perspectiva cuestiones importantes abordadas en otros capítulos. Esto ocurre especialmente con algunos ejes que atraviesan toda la tesis. Por ejemplo: la íntima relación entre el transporte marítimo y el sector de construcción naval, la responsabilidad de la política internacional y local, la invitación a buscar nuevos modos de construir el futuro del sector a través de la consideración de los impactos ambientales, económicos y sociales a lo largo de ciclo de vida completo de productos y servicios. La necesidad de una responsabilidad social corporativa. Estos temas no se cierran ni terminan, sino que son constantemente replanteados tratando de enriquecerlos. ABSTRACT The direct environmental impact of shipbuilding, which refers to construction, maintenance and repair of vessels, is by no means small. Shipbuilding depends on a large number of processes which by themselves constitute significant risks of damage to the shipyards‘ surrounding environment and which lead to significant emissions of greenhouse gases. In addition, shipbuilding uses some materials which not only may carry serious implications for environmental harm during their production and usage in the ship construction process, but also subsequently during ship repairing, operation, and recycling activities. (OECD 2010) The direct environmental impact of shipbuilding constitutes a major challenge for the industry. But this impact is not limited on their immediate surroundings, but while not being directly responsible for the impact on the environment from the operation and final recycling of commercial ships, shipbuilding is an integral part of these activities. (OECD 2010) With this in mind, this thesis is suggested that the shipbuilding industry can and must take up their environmental responsibilities not only on their immediate surroundings, also on the ships operation, becoming aware through a “life cycle” approach to ships, the environmental performance of the industry as a whole. As the environmental impact of the industry is becoming increasingly visible in the public domain much more effort is required for the sake of “green growth” which implies the ability to increase economic activity or output while lowering, or eliminating, environmental impacts. This will be an imperative for any future industrial activity and will naturally demand intricate environmental knowledge pertaining to all associated processes. This thesis making use as a valuable source of information of the developments and results of an European FP7-collaborative project called "Eco_REFITEC, coordinated by the author of this thesis on behalf of the Foundation Center Technology SOERMAR, has as its primary objective to investigate the interpretation of a sustainable Shipbuilding and Maritime Transport concept and the challenges and opportunities involved in applying for the Shipbuilding and ship repair Sector. It is done to improve the current understanding regarding sustainable shipping and to show the application experience in shipbuilding and ship repair shipyards. Assuming that sustainability is more than just an act but a process, this academic work it also aims to contribute to a much better understanding of the maritime industry and its impact with respect to climate change, and help in identifying areas for better environmental performance beyond the shipyard's own operations; shedding light on how shipbuilding can contribute in improving efficiency and reducing CO2 emissions in shipping. It is my hope that this thesis can help the Shipbuilding Industry to abandon its traditional perspective where each simply looks at its own activities to take a broader view becoming aware as to how their decisions may further affect downstream activities and their impacts on the environment, climate change and green growth. Although each chapter will have its own subject and specific approach, it will also take up and re-examine important questions previously dealt with. This is particularly the case with a number of themes which will reappear as the thesis unfolds. As example I will point to the intimate relationship between the shipping and shipbuilding industry, the responsibility of international and local policy, the call to seek other ways of building the future of the sector through the consideration of the environmental, economic and social impacts over the full life cycle of the products and services, the need for a corporate social responsibility. These questions will not be dealt with once and for all, but reframed and enriched again and again.
Resumo:
El empleo de biomasa como combustible para la generación de bio-energía va en aumento en la actualidad, debido a su impacto medioambiental nulo en cuanto a las emisiones de CO2. Por lo tanto la generación de cenizas de biomasa, residuo de la producción de esta energía, constituye un problema medioambiental con un claro impacto social y económico. Este tipo de ceniza tiene contenidos en óxidos que la hacen atractiva para su empleo como sustituto parcial del cemento Portland, lo cual proporciona una salida eco-eficiente a este residuo, reduciendo al mismo tiempo la emisión de gases de efecto invernadero asociada a la fabricación del cemento. Esta investigación se centra en el desarrollo de nuevos e innovadores materiales base-cemento eco-eficientes que incorporan ceniza de biomasa para su aplicación integral en construcción. Para ello, se emplea una ceniza de biomasa (CB) procedente de un combustor de lecho fluidizado, cuya biomasa de combustión es principalmente restos de corteza de eucalipto, suministrada por el grupo ENCE-Navia (Asturias). El trabajo desarrollado en la presente tesis doctoral, tiene como primera fase la caracterización de esta ceniza y el análisis de viabilidad de su valorización en materiales base-cemento. Dentro de este análisis, se propone la activación de la ceniza CB mediante tratamiento hidrotermal (TH) en diferentes condiciones de medio activante, temperatura y tiempo de proceso, con el objetivo de favorecer la formación de fases hidratadas que potencien la valorización de la ceniza en el campo de los materiales de construcción. Como fase hidratada de interés se obtiene la fase tobermorita (Ca2.25(Si3O7.5(OH)1.5)(H2O)), precursora del gel C-S-H, responsable del desarrollo de resistencias mecánicas en los materiales base-cemento. El proceso de TH se optimiza para la síntesis más eficiente de esta fase. El estudio posterior de las propiedades mecánicas y micro-estructurales de pastas de cemento eco-eficientes que incorporan la ceniza CB y la ceniza tratada hidrotermalmente, CB-TH, confirma una mayor viabilidad de incorporación de la ceniza CB como sustituto parcial del cemento Portland. Como siguiente paso en el desarrollo de estos innovadores materiales base-cemento eco-eficientes se amplía el estudio multi-escalar de los materiales que incorporan CB mediante diferentes ensayos físico-mecánicos y de durabilidad. Los resultados indican que la presencia de la ceniza de biomasa no tiene efectos negativos sobre las propiedades físicas de los morteros eco-eficientes estudiados. Sin embargo, la adición de CB proporciona una mejor durabilidad del material al producir modificaciones de la microestructura que dificultan el transporte de agentes agresivos. Por otro lado, los morteros con un 10 y 20% de sustitución parcial de cemento por la ceniza de biomasa CB (CB-10 y CB-20) presentan una resistencia a compresión de 53.3 y 50.5 MPa a 28 días de curado, respectivamente. Estos morteros son comparables con un cemento Portland tradicional tipo CEM I de clase de resistencia 42.5 R. Por último, y con el fin de proporcionar la apertura de estos nuevos cementos eco-eficientes al mercado en el campo de los materiales de construcción, se estudian propiedades concretas relacionadas con diferentes tipos de aplicaciones. Concretamente se estudian en detalle las propiedades relativas a la aplicación en baldosas de mortero y los resultados indican unas prestaciones del material eco-eficiente con incorporación de CB similares o mejoradas con respecto al cemento Portland. Se analiza también la viabilidad de aplicación estructural de los cementos eco-eficientes desarrollados mediante el estudio de la adherencia al acero, que resulta similar a la del material de referencia. En cuanto a los resultados de extracción y caracterización de la fase acuosa de los poros, en todas las matrices eco-eficientes se obtiene un pH que garantiza la pasivación de la armadura. Sin embargo, el alto contenido en cloruros de dicha fase acuosa sugiere la conveniencia de realizar un análisis más detallado para la aplicación de los nuevos materiales eco-eficientes en hormigón armado. Se comprueba que todas las matrices que incorporan CB en porcentajes entre un 10 y un 90%, se pueden considerar adecuadas como nuevos materiales de construcción más eco-eficientes en aplicaciones con distintos niveles de exigencias mecánicas y sin problemas ambientales asociados con procesos de lixiviación. Con el presente trabajo de investigación se completan los objetivos iniciales de la tesis, con la obtención de nuevos e innovadores materiales base-cemento eco-eficientes que incorporan cenizas de biomasa (CB) con aplicación integral en el campo de la construcción. ABSTRACT The use of biomass as a fuel for the generation of bio-energy is increasing nowadays, due to its zero environmental impact in terms of CO2 emissions. Therefore the generation of biomass ash, a by-product of this energy, is an environmental problem with a clear social and economic impact. This type of ash contains oxides that make it attractive to be used as a partial replacement of Portland cement, providing an eco-efficient solution to this residue, while reducing the emission of greenhouse gases associated with the production of cement. The present research is focused on the development of new and innovative eco-efficient cement-based materials that incorporate biomass ash for their comprehensive application in construction. For this purpose a biomass ash (CB) is used from a fluidized bed forest combustor mainly fed with the bark of eucalyptus trees, provided by the ENCE-Navia (Asturias) group. The work includes in the first stage the characterization of the raw materials and the analysis of viability of their valorization in cement-based materials. Within this analysis, the activation of the ash is proposed by hydrothermal treatment (HT) in different conditions of activation medium, temperature and process duration, aiming an enhanced formation of hydrated phases to improve the ash valorization in the construction materials field. As an interesting hydrated phase, the tobermorite (Ca2.25(Si3O7.5(OH)1.5)(H2O)) is obtained from the process. This phase is considered as a precursor of the gel C-S-H, responsible for the development of mechanical strength in cement-based materials. HT process is optimized for the most efficient synthesis of tobermorite. The analysis of mechanical and microstructural properties of eco-efficient cement pastes incorporating CB ash and hydrothermally treated ash, CB-TH, confirms an improved viability of incorporation of CB ash as a partial replacement for Portland cement in the case. As a next step in the development of these innovative eco-efficient cement-based materials, a multiscale study of the materials that incorporate CB by different physical-mechanical and durability tests is carried out. The results indicate that the presence of biomass ash does not give rise to negative effects on the physical properties of the eco-efficient mortars analyzed. Nevertheless, the addition of CB produces a better durability performance due to microstructural modifications that hinder the transport of aggressive agents through the material. Moreover, mortars with a 10% and 20% of partial substitution of cement by the CB biomass ash (CB-10 and CB-20) show a compressive resistance of 53.3 and 50.5 MPa at 28 days of curing, respectively. These mortars are comparable to an ordinary Portland cement type CEM I with a resistance class of 42.5R. Finally, and in order to provide the opening of these new eco-efficient cement to the market in the field of construction materials, certain properties specifically related to different types of applications are studied. Among these, the properties concerning the application in mortar tiles are analyzed and the results indicate a similar, or even better performance of the eco-efficient mortar that incorporates CB, with respect to Portland cement. The viability of structural application of the developed eco-efficient cement is also performed considering the study of the adhesion to steel, with results similar to those of the reference material. Regarding the results of extraction and analysis of the aqueous phase of the pores, a pH value guaranteeing reinforcement passivation is obtained for all the eco-efficient matrices. However, high chloride content is obtained suggesting the suitability of a more detailed study to evaluate the application of these new eco-efficient materials in reinforced concrete. It is established that all the matrices incorporating CB in percentages between 10 and 90% may be considered adequate as new more eco-efficient construction materials in applications with different levels of mechanical demand and without environmental problems associated to leaching processes. In this research the initial objectives of the thesis are fulfilled by obtaining new and innovative eco-efficient cement-based materials that incorporate biomass ashes (CB) with comprehensive application in the construction field.
Resumo:
Debido a la complejidad de los procesos que controlan el intercambio de gases de carbono (C) y nitrógeno (N) entre el suelo y la atmósfera, en los sistemas forestales y agroforestales, son comprensibles las incógnitas existentes respecto a la estimación de los flujos de los gases de efecto invernadero (GEI) y la capacidad como reservorios de carbono de los suelos, bajo diferentes formas de uso y regímenes de alteración a escala regional y global. Esta escasez de información justifica la necesidad de caracterizar la dinámica de intercambio de GEI en los ecosistemas Mediterráneos, en especial en el contexto actual de cambio climático, y el incremento asociado de temperatura y periodos de sequía, alteración de los patrones de precipitación, y el riesgo de incendios forestales; cuyas consecuencias afectarán tanto a los compartimentos de C y de N del suelo como a la capacidad de secuestro de C de estos ecosistemas. Dentro de este contexto se enmarca la presente tesis doctoral cuyo objetivo ha sido cuantificar y caracterizar los flujos de dióxido de carbono (CO2), de oxido nitroso (N2O) y de metano (CH4), junto con los stocks de C y N, en suelos forestales de Quercus ilex, Quercus pyrenaica y Pinus sylvestris afectados por incendios forestales; así como el estudiar el efecto de la gestión y la cubierta arbórea en la respiración del suelo y los stocks de C y N en una dehesa situada en el centro de la Península Ibérica. De manera que los flujos de CO2, N2O y CH4; y los parámetros físico-químicos y biológicos del suelo fueron estudiados en los diferentes tratamientos y ecosistemas a lo largo del trabajo que se presenta. Los resultados obtenidos muestran la existencia de variaciones temporales y espaciales de la respiración del suelo dentro de una escala geográfica pequeña, controladas principalmente por la temperatura y la humedad del suelo; y por los contenidos de C y N del suelo en un bosque de Pinus sylvestris en la vertiente norte de la Sierra de Guadarrama , en España. El análisis de los efectos de los incendios forestales a largo plazo (6-8 años) revela que las pérdidas anuales de C a través de la respiración del suelo en las zonas quemadas de Quercus ilex, Quercus pyrenaica y Pinus sylvestris fueron 450 gCm-2yr-1, 790 gCm-2yr-1 y 1220 gCm-2yr-1, respectivamente; lo que representa una reducción del 43%, 22% y 11% en comparación con las zonas no quemadas de dichas especies, debido a la destrucción de la masa arbórea. El efecto del fuego también alteró los flujos N2O y CH4 del suelo, de una forma diferente en los distintos ecosistemas y estacionalidades estudiadas. De tal modo, que los suelos quemados mostraron una mayor oxidación del CH4 en las masas de Q. ilex, y una menor oxidación en las de P. sylvestris; además de una disminución de los flujos de N2O en Q. pyrenaica. Los incendios también afectaron los parámetros microclimáticos de los suelos forestales, observándose un incremento de la temperatura del suelo y una disminución de la humedad en los emplazamientos quemados que en los no quemados. Los cationes intercambiables, el pH, el cociente C/N, el contenido en raicillas y la biomasa microbiana también disminuyeron en las zonas quemadas. Aunque el C orgánico del suelo no se alteró de manera significativa, si lo hizo la calidad de la materia orgánica, disminuyendo el carbono lábil y aumentando las formas recalcitrantes lo que se tradujo en menor sensibilidad de la respiración del suelo a la temperatura (valores de Q10) en las zonas quemadas. Los resultados del estudio realizado en la Dehesa muestran que las actividades silvopastorales estudiadas afectaron levemente y de forma no constante a la respiración del suelo y las condiciones microclimáticas del suelo. Se observó una reducción 12% de la respiración del suelo por efecto del pastoreo no intensivo. Sin embargo, se observaron incrementos de 3Mg/ha en los stocks de C y de 0.3 Mg/ha en los stocks de N en los suelos pastoreados en comparación con los no pastoreados. Aunque, no se observó un claro efecto de la labranza sobre la respiración del suelo en nuestro experimento, sin embargo si se observó una disminución de 3.5 Mg/ha en las reservas de C y de 0.3 Mg/ ha en las de N en los suelos labrados comparados con los no labrados. La copa del arbolado influyó de forma positiva tanto en la respiración del suelo, como en los stocks de C y N de los suelos. La humedad del suelo jugó un papel relevante en la sensibilidad de la respiración a la temperatura del suelo. Nuestros resultados ponen de manifiesto la sensibilidad de la respiración del suelo a cambios en la humedad y los parámetros edáficos, y sugieren que la aplicación de modelos estándar para estimar la respiración del suelo en áreas geográficas pequeñas puede no ser adecuada a menos que otros factores sean considerados en combinación con la temperatura del suelo. Además, las diferentes respuestas de los flujos de gases de efecto invernadero a los cambios, años después de la ocurrencia de incendios forestales, destaca la necesidad de incluir estos cambios en las futuras investigaciones de la dinámica del carbono en los ecosistemas mediterráneos. Por otra parte, las respuestas divergentes en los valores de respiración del suelo y en los contenidos de C y N del suelo observados en la dehesa, además de la contribución de la copa de los árboles en los nutrientes del suelo ilustran la importancia de mantener la gestión tradicional aplicada en beneficio de la capacidad de almacenar C en la dehesa estudiada. La información obtenida en este trabajo pretende contribuir a la mejora del conocimiento de la dinámica y el balance de C en los sistemas mediterráneos, además de ayudar a predecir el impacto del cambio climático en el intercambio de C entre los ecosistemas forestales y agroforestales y la atmósfera. ABSTRACT Due to the complexity of the processes that control the exchange of carbon (C) and nitrogen (N) gasses between soils and the atmosphere in forest and agroforestry ecosystems, understandable uncertainties exist as regards the estimation of greenhouse gas (GHG) fluxes and the soil sink capacity at regional and global scale under different forms of land use and disturbance regimes. These uncertainties justify the need to characterize the exchange dynamics of GHG between the atmosphere and soils in Mediterranean terrestrial ecosystems, particularly in the current context of climate change and the associated increase in temperature, drought periods, heavy rainfall events, and increased risk of wildfires, which affect not only the C and N pools but also the soil C sink capacity of these ecosystems. Within this context, the aims of the present thesis were, firstly, to quantify and characterize the fluxes of carbon dioxide (CO2), nitrous oxide (N2O) and methane (CH4) as well as the C and N stocks in Quercus ilex, Quercus pyrenaica and Pinus sylvestris stands affected by wildfires, and secondly, to study the effects of Quercus ilex canopy and management on both soil respiration and C and N pools in dehesa systems in the center of Iberian Peninsula. Soil CO2, N2O and CH4 fluxes, and soil physical-chemical and biological parameters were studied under the different treatments and ecosystems considered in this study. The results showed seasonal and spatial variations in soil respiration within small geographic areas, mainly controlled by soil temperature and moisture in addition to soil carbon and nitrogen stocks in mixed pine–oak forest ecosystems on the north facing slopes of the Sierra de Guadarrama in Spain. The analysis of long term effects of wildfires (6–8 years) revealed that annual carbon losses through soil respiration from burned sites in Quercus ilex, Quercus pyrenaica and Pinus sylvestris stands were 450 gCm-2yr-1, 790 gCm-2yr-1 and 1220 gCm-2yr-1, respectively; with burned sites emitting 43%, 22% and 11% less in burned as opposed to non-burned sites due the loss of trees. Fire may alter both N2O and CH4 fluxes although the magnitude of such variation depends on the site, soil characteristics and seasonal climatic conditions. The burned sites showed higher CH4 oxidation in Q.ilex stands, and lower oxidation rates in P. sylvestris stands. A reduction in N2O fluxes in Q. pyrenaica stands was detected at burned sites along with changes in soil microclimate; higher soil temperature and lower soil moisture content. Exchangeable cations, the C/N ratio, pH, fine root and microbial biomass were also found to decrease at burned sites. Although the soil organic carbon was not significantly altered, the quality of the organic matter changed, displaying a decrease in labile carbon and a relative increase in refractory forms, leading to lower sensitivity of soil respiration to temperature (Q10 values) at burned sites. The results from the dehesa study show that light grazing and superficial tilling practices used in the studied dehesa system in Spain had a slight but non-consistent impact on soil respiration and soil microclimate over the study period. The reduction in soil respiration in the dehesa system due to the effects of grazing was around 12 %. However, increments of 3Mg/ha in C stocks and 0.3 Mg/ha in N stocks in grazed soils were observed. Although no clear effect of tilling on soil respiration was found, a decrease of 3.5 Mg/ha in C stocks and 0.3 Mg/ha in N stocks was detected for tilled soils. The presence of a tree canopy induced increases in soil respiration, soil C and N stocks, while soil moisture was found to play an important role in soil respiration temperature response. Our results suggest that the use of standard models to estimate soil respiration in small geographical areas may not be adequate unless other factors are considered in addition to soil temperature. Furthermore, the different responses of GHG flux to climatic shifts, many years after the occurrence of wildfire, highlight the need to include these shifts in C dynamics in future research undertaken in Mediterranean ecosystems. Furthermore, divergent responses in soil respiration and soil C and N stocks to grazing or tilling practices in Dehesa systems, and the influence of tree canopy on soil respiration and soil nutrient content, illustrate the importance of maintaining beneficial management practices. Moreover, the carbon sequestration capacity of the Dehesa system studied may be enhanced through improvements in the management applied. It is hoped that the information obtained through this research will contribute towards improving our understanding of the dynamics and balance of C in Mediterranean systems, and help predict the impact of climate change on the exchange of C between forest and agroforestry ecosystems and the atmosphere.
Resumo:
BACKGROUND: The immediate lethality caused by spinosad has been widely studied on Spodoptera exigua (H ¿ ubner). However, long-term effects can also provide valuable information on insecticide toxic action. Here, the persistence of spinosad on Capsicum annuum L. foliage and the lethal and sublethal effects of greenhouse-aged foliar residues of this insecticide on third instars of S. exigua are reported. RESULTS: Foliage was collected at 0, 3, 5, 10, 20, 30, 40 and 50 days after application, and spinosad residues were measured. Residues decreased over time according to first-order kinetics. The average rate constant and half-life of disappearance were 4.44×10?3 and156 daysand5.80×10?3 and120 days for60and120 mg L?1 respectively. Larval mortalitygradually decreased, corresponding to the residues, but was still appreciable (35 and 65% for 60 and 120 mg L?1 respectively) when the larvae were fed with foliage collected 50 days after treatment. Subsequently, pupal development was reduced and varied between 20 and 60% and between 21 and 41% for 60 and 120 mg L?1, respectively, in all ages of leaf residues that were bioassayed. At all time points, the consumption rate by the larvae was reduced between 62 and 84% for both concentrations that were bioassayed. CONCLUSION: It is concluded that, under the present greenhouse conditions, the degradation of spinosad was slower than that reported by other authors in the field, and, because of that, its residues could cause lethal and sublethal effects to S. exigua larvae.
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There is strong evidence to indicate that carbon dioxide and other greenhouse gases are accumulating at unprecedented concentrations in out atmosphere contributing to global climate change. Evidence is equally strong that human activities, mainly the burning of fossil fuels, are driving force in this process (IPCC 2007). While different industries contribute varying amounts to total anthropogenic greenhouse gases, it is incumbent upon each to understand its contribution and search for sensible ways to reduce overall greenhouse gas production. The aim of this paper is the development of a methodology to determine the amount of CO2 emissions of a highway, allowing providing solutions that can improve the energy footprint and reduce its emissions
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In this paper the very first geochemical and isotopic data related to surface and spring waters and dissolved gases in the area of Hontomín–Huermeces (Burgos, Spain) are presented and discussed. Hontomín–Huermeces has been selected as a pilot site for the injection of pure (>99%) CO2. Injection and monitoring wells are planned to be drilled close to 6 oil wells completed in the 1980s for which detailed stratigraphical logs are available, indicating the presence of a confined saline aquifer at the depth of about 1500 m into which less than 100,000 tons of iquid CO2 will be injected, possibly starting in 2013. The chemical and features of the spring waters suggest that they are related to a shallow hydrogeological system as the concentration of the Total Dissolved Solids approaches 800 mg/L with a Ca2+(Mg2+)-HCO3− composition, similar to that of the surface waters. This is also supported by the oxygen and hydrogen isotopic ratios that have values lying between those of the Global and the Mediterranean Meteoric Water Lines. Some spring waters close to the oil wells are haracterized by relatively high concentrations of NO3− (up to 123 mg/L), unequivocally suggesting an anthropogenic source that adds to the main water–rock interaction processes. The latter can be referred to Ca-Mg-carbonate and, at a minor extent, Al-silicate dissolution, being the outcropping sedimentary rocks characterized by Palaeozoic to Quaternary rocks. Anomalous concentrations of Cl−, SO42−, As, B and Ba were measured in two springs discharging a few hundred meters from the oil wells and in the Rio Ubierna. These contents are significantly higher than those of the whole set of the studied waters and are possibly indicative of mixing processes, although at very low extent, between deep and shallow aquifers. No evidence of deep-seated gases interacting with the Hontomín–Huermeces waters was recognized in the chemistry of the disolved gases. This is likely due to the fact that they are mainly characterized by an atmospheric source as highlighted by the high contents of N2, O2 and Ar and by N2/Ar ratios that approach that of ASW (Air Saturated Water) and possibly masking any contribution related to a deep source. Nevertheless, significant concentrations (up to 63% by vol.) of isotopically negative CO2 (<−17.7‰ V-PDB) were found in some water samples, likely related to a biogenic source. The geochemical and isotopic data of this work are of particular importance when a monitoring program will be established to verify whether CO2 leakages, induced by the injection of this greenhouse gas, may be affecting the quality of the waters in the shallow hydrological circuits at Hontomín–Huermeces. In this respect, carbonate chemistry, the isotopic carbon of dissolved CO2 and TDIC (Total Dissolved Inorganic Carbon) and selected trace elements can be considered as useful parameters to trace the migration of the injected CO2 into near-surface environments.
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Governments are working in new policies to slow down total energy consumption and greenhouse gases (GHG) emissions, promoting the deployment of electric vehicles (EVs) in all countries. In order to facilitate this deployment and help to reduce the final costs of their batteries, additional utilization of EVs when those are parked has been proposed. EVs can be used to minimize the total electricity cost of buildings (named vehicle to building applications, V2B). In this paper an economic evaluation of EVs in the Building Energy Management System is shown. The optimal storage capacity and its equivalent number of EVs are determined. This value is then used for determining the optimal charging schedule to be applied to the batteries. From this schedule, the total expected profit is derived for the case of a real hotel in Spain.
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Natural analogs offer a valuable opportunity to investigate the long-term impacts associated with thepotential leakage in geological storage of CO2.Degassing of CO2and radon isotopes (222Rn?220Rn) from soil, gas vents and thermal water dischargeswas investigated in the natural analog of Campo de Calatrava Volcanic Field (CCVF; Central Spain) todetermine the CO2?Rn relationships and to assess the role of CO2as carrier gas for radon. Furthermore,radon measurements to discriminate between shallow and deep gas sources were evaluated under theperspective of their applicability in monitoring programs of carbon storage projects.CO2flux as high as 5000 g m?2d?1and222Rn activities up to 430 kBq m?3were measured;220Rn activi-ties were one order of magnitude lower than those of222Rn. The222Rn/220Rn ratios were used to constrainthe source of the Campo de Calatrava soil gases since a positive correlation between radon isotopic ratiosand CO2fluxes was observed. Thus, in agreement with previous studies, our results indicate a deepmantle-related origin of CO2for both free and soil gases, suggesting that carbon dioxide is an efficientcarrier for Rn. Furthermore, it was ascertained that the increase of222Rn in the soil gases was likely pro-duced by two main processes: (i) direct transport by a carrier gas, i.e., CO2and (ii) generation at shallowlevel due to the presence of relatively high concentrations of dissolved U and Ra in the thermal aquiferof Campo de Calatrava.The diffuse CO2soil flux and radon isotopic surveys carried out in the Campo de Calatrava VolcanicFields can also be applicable to geochemical monitoring programs in CCS (Carbon Capture and Storage)areas as these parameters are useful to: (i) constrain CO2leakages once detected and (ii) monitor both theevolution of the leakages and the effectiveness of subsequent remediation activities. These measurementscan also conveniently be used to detect diffuse leakages.
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El cultivo de café es de gran importancia a nivel mundial (ICO, 2011), y en el Ecuador ha sido uno de los cultivos más importantes en la generación de divisas (COFENAC, 2011). Sin embargo en los sistemas productivos de este país se puede apreciar el uso inapropiado de fertilizantes, lo que conlleva a una pérdida de nutrientes, por lo que es importante estudiar las dosis adecuadas para la fertilización tanto mineral como orgánica. El objetivo del trabajo fue evaluar el efecto de la fertilización mineral y orgánica en diferentes dosis en un monocultivo de café en la provincia de Loja, sobre las propiedades del suelo, la emisión de los principales gases que provocan el efecto invernadero y la fenología y productividad del cultivo. En la provincia de Loja (Ecuador) se seleccionó un área de 2.520 m2 en la que se establecieron 21 parcelas de café arábigo (Coffea arabica L.) var. caturra y se aplicó tres tratamientos con tres repeticiones de fertilización mineral y tres orgánicos con dosis: bajas minerales (MIN 1= 157 Kg NPK ha-1 año-1 para el primer año y 425 Kg NPK ha-1 año-1 para el segundo año), medias minerales (MIN 2= 325 Kg NPK ha-1 año-1 para el primer año y 650 Kg NPK ha-1 año-1 en el segundo año) y altas minerales (MIN 3= 487 y 875 Kg NPK ha-1 año-1 para el primer y segundo año respectivamente), bajas orgánicas (ORG 1= 147 Kg NPK ha-1 año-1 en el primer año y 388 Kg NPK ha-1 año-1 en el año dos), medias orgánicas (ORG 2= 265 Kg NPK ha-1 año-1 para el primer año y 541 Kg NPK ha-1 año-1 en el segundo año), altas orgánicas (ORG 3= 368 Kg NPK ha-1 año-1 para el primer año y 727 Kg NPK ha-1 año-1 en el segundo año) y fertilización cero (TES = sin fertilización). Se usó urea, roca fosfórica y muriato de potasio en la fertilización mineral y humus (Bioabor) en la orgánica, más un tratamiento testigo, cada tratamiento tuvo tres repeticiones. El tiempo de evaluación de los fertilizantes aplicados fue de dos años consecutivos, la fertilización se la realizó dos veces por año y en base a análisis del suelo y demandas nutricionales del cultivo. para determinar las características del suelo se realizó muestreos de suelos en cada parcela a una profundidad de 20 cm de estas muestras los parámetro iniciales determinados fueron: color (Munsell), textura (método del hidrómetro), pH (relación 1:2,5 suelo-agua), Materia orgánica (Walkey y Black), Nitrógeno (Micro Kjendahl), Fósforo (Bray y Kurtz), Potasio (Olsen), estos procesos se repitieron cada seis meses para poder evaluar los cambios de que se producen debido a la fertilización mineral y orgánica en el cultivo. Las emisiones de gases efecto invernadero desde el suelo al ambiente se determinaron por el método de cámara cerrada (Rondón, 2000) y la concentración por cromatografía de gases. Las mediciones fisiológicas (altura de planta, ancho de copa, grosor de tallo y producción) se las evaluó cada dos meses, a excepción de la producción que fue anual al término de cada cosecha. Además se realizó el análisis económico de la productividad del cultivo. El análisis estadístico de datos se lo realizó con el programa SPSS v. 17.0. Las medias fueron comprobadas mediante ANOVAS de un factor con test de Tukey (P < 0,05). El beneficio económico se estimó en términos de ingresos y gastos totales que se presentaron en el ensayo. Los resultados obtenidos al término del ensayo indican que los tratamientos MIN 2 y MIN 3 produjeron cambios más significativos en comparación con los otros tratamientos establecidos en la mejora de fertilidad del suelo, el pH ha sido menos afectado en la acidificación en comparación con los tratamientos orgánicos que se han acidificado mayormente; la materia orgánica (MO) tuvo incrementos considerablemente bueno en estos dos tratamientos, sin embargo fueron superados por los tratamientos de fertilización orgánica; el nitrógeno total (Nt )y el potasio (K) también presentaron mejores valores al termino del ensayo y el fósforo (P) mostro incrementos buenos aunque un poco menores que los de los tratamientos ORG 2 y ORG 3. En lo que respecta a las emisiones de gases efecto invernadero, los flujos acumulados de óxido nitroso (N2O) en los dos años han aumentado en todos los tratamientos en comparación con el tratamiento Testigo, pero de manera considerable y con mayores flujos en el tratamiento MIN 3 y MIN 2 que se podrían considerarse los de mayor contaminación por N2O al ambiente lo que se le atribuye a las dosis de fertilización mineral aplicadas en el periodo de investigación, los tratamiento MIN 1 y todos los tratamientos orgánicos muestran menores emisiones al ambiente. Las emisiones de metano (CH4) no muestran mayores diferencias de emisiones entre tratamientos, siendo los mayores emisores los tratamientos ORG 3 y ORG 2 posiblemente debido al abono orgánico y añadido al suelo; para las emisiones de dióxido de carbono (CO2) de manera similar al CH4 el tratamiento ORG 3 fue el que presento mayores emisiones, los flujos de CO2 al ambiente de los otros tratamientos fueron menores y no presentaron diferencias significativas entre ellos. La variables fisiológicas en todos los casos apoyaron al desarrollo de las plantas de café, esto al ser comparadas con el tratamiento Testigo, sin embargo las que alcanzaron las mayores altitudes, anchos de copas y diámetro de tallo fueron las plantas del tratamiento MIN 3, seguido del MIN 3, no mostrando significancia entre ellos, y para los tratamientos orgánicos el que presento muy buenos resultados en estas variables ha sido el ORG 3, el cual no presento diferencias significativas con el MIN 2, lo cual comprueba que la fertilización mineral es más efectiva en este caso frente a la orgánica. Para el primer año de producción el tratamiento mineral con fertilización MIN 3 es el que obtuvo mayor producción no presentando diferencia estadística con el tratamiento con el MIN 2, no obstante fueron significativamente mayores que los otros tratamientos. Vale indicar que también el tratamiento MIN 1 y el tratamiento ORG 3 han presentado una producción considerable de café no mostrando diferencias estadísticas entre ellos. Para el segundo año la producción el cultivo mostró mayores rendimientos que el primer año de evaluación en todos los tratamientos, esto debido a la fisiología propia del cultivo y por otra parte se atribuye a la adición de fertilizantes que se ha realizado durante todo el ensayo; de manera similar al anterior los tratamientos MIN 3 y MIN 2 obtuvieron mejores rendimientos, no enseñando diferencias estadísticas significativas entre ellos, no obstante el tratamiento mineral dosis MEDIA no presentó significancia estadística con el ORG 3. El benéfico económico ha resultado mayor en el tratamiento MIN 3 y MIN 2, aunque el tratamiento MIN 2, es el que obtiene la mejor relación costo-beneficio; los tratamientos ORG 2 y ORG 3 y Testigo has producido beneficios negativos para el productor. En cuanto a la parte ambiental se considera que los mejores tratamientos en cuanto ha cuidado ambiental serían los tratamientos MIN 1 y ORG 1, sin embargo a nivel de producción y rentabilidad para el productor baja. ABSTRACT Coffee growing has great importance worldwide (ICO, 2011), and in Ecuador, it has been one of the most important crops to generate income (COFENAC, 2011). However, in the productive systems of this country, the inappropriate use of fertilizers has been observed which produces loss of nutrients, thus it is important to study suitable doses for mineral and organic fertilizing. The purpose of the study was to evaluate the effect of mineral and organic fertilizing at different doses in a coffee monoculture in the province of Loja on soil characteristics, emission of the main gasses that produce the greenhouse effect and the phenology and productivity of crops. In the province of Loja (Ecuador) an area of 2.520 m2 was chosen, where 21 plots of Arabica coffee (Coffea arabica L.), the caturra variety were cultivated and three treatments with three repetitions each one for mineral and organic fertilization were used with doses that ranged from: mineral low (MIN 1= 157 Kg NPK ha-1 año-1 for the first year y 425 Kg NPK ha-1 año-1 for the second year), mineral medium (MIN 2= 325 Kg NPK ha-1 año-1 for the first year y 650 Kg NPK ha-1 año-1 I the second year) y mineral high (MIN 3= 487 y 875 Kg NPK ha-1 año-1 for the first and second year respectively), organic low (ORG 1= 147 Kg NPK ha-1 año-1 in the first year y 388 Kg NPK ha-1 año-1 in the second year), organics medium (ORG 2= 265 Kg NPK ha-1 año-1 for the first year y 541 Kg NPK ha-1 año-1 in the second year), organics high (ORG 3= 368 Kg NPK ha-1 año-1 for the first year and 727 Kg NPK ha-1 año-1 in the second year) y fertilization zero (TES = no fertilization).; urea, phosphoric rock and muriate of potash were used in the mineral fertilization and humus (Bioabor) in the organic, plus a blank treatment. Time to evaluate the applied fertilizers was for two consecutive years, fertilization was done twice per year based on soil analysis and nutritional requirements of the crops. In order to determine the characteristics of the soil, samples of soil in each plot with a depth of 20 cm were done; from these samples, the determined initial parameters were: color (Munsell), texture (hydrometer method), pH (soil-water 1:2,5 relation), organic matter (Walkey y Black), nitrogen (Micro Kjendahl), phosphorus (Bray y Kurtz), potassium (Olsen); these processes were repeated each six months in order to evaluate the changes that are produced due to mineral and organic fertilization in the crops. The emissions of greenhouse gasses from the soil to the atmosphere were determined by using enclosure method (Rondón, 2000) and the concentration, by using gas chromatography during the whole testing. The physiological measures (plant height, width of the top of the tree, thickness of the stem and production) were evaluated each two months, except for production which was annual at the end of each harvest. Moreover, the economic analysis of the productivity of the crops was done. The statistical analysis of the data was done using SPSS v. 17.0. The means were proved by ANOVAS with a factor of a Tukey test (P < 0,05). The economic benefit was estimated in terms of incomes and total expenses which were presented in the essay. The results obtained at the end of the essay show that the MIN 2 and MIN 3 treatments produced more meaningful changes in comparison with the other treatments used to improve soil fertility; pH was less affected in the acidification compared with the organic treatments which were greatly acidified; organic matter (MO) had increased considerably in these two treatments; however, they were surpassed by the organic treatments of fertilization; total nitrogen (Nt) and potassium (K) also presented better results at the end of the essay and phosphorus (P) showed good increasing figures although a little lower compared with ORG 2 and ORG 3 treatments. Regarding the emission of the greenhouse gasses, the fluxes accumulated from nitrous oxide (N2O) in two years increased in all the treatments in comparison with the blank treatment, but in a greater form and with higher fluxes in the MIN 3 and MIN 2 treatments which can be considered as the ones with greater contamination of N2O in the atmosphere, this can be due to the applied mineral doses to fertilize during the process; MIN 1 treatments and all the organic ones showed lower emission to the atmosphere. Methane emissions (CH4) did not show major differences in emissions in the treatments, being the greater emissions the ORG 3 and ORG 2 treatments; this is possibly due to the organic compost added to the soil; regarding carbon dioxide (CO2) emissions, in a similar way to CH4, the ORG 3 treatment was the one that presented greater emissions, the CO2 emissions to the atmosphere in the other treatments were lower and did not present meaningful differences among them. The physiological variables in all the cases helped coffee crops grow, this was observed when compared with the blank treatment; however, plants that reached the greatest height, width of top and diameter of stem were the plants of the MIN 3 treatment, followed by MIN 3, which did not show much significance among them, and for the organic treatments, the one that presented great results in these variables was ORG 3, which did not show meaningful differences compared with MIN 2, which proves that mineral fertilization is more effective in this case compared with the organic. In the first year of production, the mineral treatment with MIN 3 fertilization obtained greater production and thus did not show statistical difference with MIN 2 treatment, although the other treatments were greater. It is worth mentioning that MIN 1 treatment and ORG 3 treatment presented a meaningful production of coffee, not showing statistical differences among them. For the second year, the production of the crops showed greater profits than in the first year of evaluation in all the treatments, this was due to the physiological properties of the crops and on the other hand, it might be due to the addition of fertilizers during the whole essay; in a similar way, MIN 3 and MIN 2 performed better, not showing greater statistical differences among them, although the mineral treatment MEDIUM doses did not show statistical difference compared with ORG 3. The economic benefit was greater in the MIN 3 and MIN 2 treatments, although MIN 2 treatment is the one that shows the best cost-benefit ratios; ORG 2 and ORG 3 treatments and the blank produced negative benefits for the producer. Regarding the environment, the best treatments to care for the atmosphere are considered to be MIN 1 and ORG 1 treatments; however, regarding production volume and profitability they were low for the producer.
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The influence of atmospheric gases and tropospheric phenomena becomes more relevant at frequencies within the THz band (100 GHz to 10 THz), severely affecting the propagation conditions. The use of radiosoundings in propagation studies is a well established measurement technique in order to collect information about the vertical structure of the atmosphere, from which gaseous and cloud attenuation can be estimated with the use of propagation models. However, some of these prediction models are not suitable to be used under rainy conditions. In the present study, a method to identify the presence of rainy conditions during radiosoundings is introduced, with the aim of filtering out these events from yearly statistics of predicted atmospheric attenuation. The detection procedure is based on the analysis of a set of parameters, some of them extracted from synoptical observations of weather (SYNOP reports) and other derived from radiosonde observations (RAOBs). The performance of the method has been evaluated under different climatic conditions, corresponding to three locations in Spain, where colocated rain gauge data were available. Rain events detected by the method have been compared with those precipitations identified by the rain gauge. The pertinence Received 26 June 2012, Accepted 31 July 2012, Scheduled 15 August 2012 * Corresponding author: Gustavo Adolfo Siles Soria (gsiles@grc.ssr.upm.es). 258 Siles et al. of the method is discussed on the basis of an analysis of cumulative distributions of total attenuation at 100 and 300 GHz. This study demonstrates that the proposed method can be useful to identify events probably associated to rainy conditions. Hence, it can be considered as a suitable algorithm in order to filter out this kind of events from annual attenuation statistics.
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Transport climate change impacts have become a worldwide concern. The use of Intelligent Transport Systems (ITS) could contribute to a more effective use of resources in toll road networks. Management of toll plazas is central to the reduction of greenhouse gas (GHG) emissions, as it is there that bottlenecks and congestion occur. This study focuses on management strategies aimed at reducing climate change impacts of toll plazas by managing toll collection systems. These strategies are based on the use of different collection system technologies – Electronic Toll Collection (ETC) and Open Road Tolling (ORT) – and on queue management. The carbon footprint of various toll plazas is determined by a proposed integrated methodology which estimates the carbon dioxide (CO2) emissions of the different operational stages at toll plazas (deceleration, service time, acceleration, and queuing) for the different toll collection systems. To validate the methodology, two main-line toll plazas of a Spanish toll highway were evaluated. The findings reveal that the application of new technologies to toll collection systems is an effective management strategy from an environmental point of view. The case studies revealed that ORT systems lead to savings of up to 70% of CO2 emissions at toll plazas, while ETC systems save 20% comparing to the manual ones. Furthermore, queue management can offer a 16% emissions savings when queue time is reduced by 116 seconds. The integrated methodology provides an efficient environmental management tool for toll plazas. The use of new technologies is the future of the decarbonization of toll plazas.
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CO2 capture and storage (CCS) projects are presently developed to reduce the emission of anthropogenic CO2 into the atmosphere. CCS technologies are expected to account for the 20% of the CO2 reduction by 2050. Geophysical, ground deformation and geochemical monitoring have been carried out to detect potential leakage, and, in the event that this occurs, identify and quantify it. This monitoring needs to be developed prior, during and after the injection stage. For a correct interpretation and quantification of the leakage, it is essential to establish a pre-injection characterization (baseline) of the area affected by the CO2 storage at reservoir level as well as at shallow depth, surface and atmosphere, via soil gas measurements. Therefore, the methodological approach is important because it can affect the spatial and temporal variability of this flux and even jeopardize the total value of CO2 in a given area. In this sense, measurements of CO2 flux were done using portable infrared analyzers (i.e., accumulation chambers) adapted to monitoring the geological storage of CO2, and other measurements of trace gases, e.g. radon isotopes and remote sensing imagery were tested in the natural analogue of Campo de Calatrava (Ciudad Real, Spain) with the aim to apply in CO2 leakage detection; thus, observing a high correlation between CO2 and radon (r=0,858) and detecting some vegetation indices that may be successfully applied for the leakage detection.
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Due to a growing concern over global warming, the bituminous mixture industry is making a constant effort to diminish its emissions by reducing manufacturing and installation temperatures without compromising the mechanical properties of the bituminous mixtures. The use of mixtures with tyre rubber has demonstrated that these mixtures can be economical and ecological and that they improve the behaviour of the pavements. However, bituminous mixtures with a high rubber content present one major drawback: they require higher mixing and installation temperatures due to the elevated viscosity caused by the high rubber content and thus they produce larger amounts of greenhouse gas emissions than conventional bituminous mixtures. This article presents a study of the effect of four viscosity-reducing additives (Sasobit®, Asphaltan A®, Asphaltan B® and Licomont BS 100®) on a bitumen modified with 15% rubber. The results of this study indicate that these additives successfully reduce viscosity, increase the softening temperature and reduce penetration. However, they do not have a clear effect on the test for elastic recovery and ductility at 25 °C.
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Fundación Ciudad de la Energía (CIUDEN) is carrying out a project of geological storage of CO2, where CO2 injection tests are planned in saline aquifers at a depth of 1500 m for scientific objectives and project demonstration. Before any CO2 is stored, it is necessary to determine the baseline flux of CO2 in order to detect potential leakage during injection and post-injection monitoring. In November 2009 diffuse flux measurements of CO2 using an accumulation chamber were made in the area selected by CIUDEN for geological storage, located in Hontomin province of Burgos (Spain). This paper presents the tests carried out in order to establish the optimum sampling methodology and the geostatistical analyses performed to determine the range, with which future field campaigns will be planned.
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El presente Proyecto tiene como propósito el estudio de la viabilidad de la implantación de energía geotérmica de muy baja entalpia para la climatización de un edificio empresarial en Madrid. Para ello se emplearon cálculos teóricos y simulaciones realizadas mediante programas informaticos especializados con el fin de estimar los parámetros técnicos necesarios para su viabilidad. Se estimo el suministro de la potencia necesaria a través de tres bombas de calor tipo agua-agua que sustituyen a las bombas de calor aire-agua individuales anteriormente instaladas. El intercambio de calor se realiza a través de sondas geotérmicas U-Simple. Se dimensionaron los colectores, bombas de circulación, deposito de inercia y vaso de expansión necesarios para funcionamiento del sistema. El estudio económico determino la necesidad de una alta inversión inicial, con una rentabilidad a medio plazo. Además de los beneficios económicos se realizo un estudio de las emisiones de gases de efecto invernadero demostrando la reducción de los mismos, lo que refleja que además de ser una tecnología económicamente viable es una energía limpia. ABSTRACT The objective of the present project is to evaluate the viability of the imposition of a low-enthalpy geothermal energy system for air conditioning in a business building in Madrid. In this study, both theoretical calculations and numerical simulations in specialized programs were used in order to estimate the technical parameters needed for its viability. We estimated the necessary power supply, which is delivered by three heat water-water pumps that substitute the individual heat air-water pumps previously installed. The heat exchange is achieved through geothermal vertical simple-U probes. Also in this work we have measured the collectors, flow pumps, inertia deposit and the water expansion vessel needed for the proper operation of the system. The economic study determined the need of a high initial investment with mid-term profit. In addition to the economic benefits, the greenhouse gases emissions were evaluated, finding that the geothermal energy system implies a reduction of these emissions. This reflects the fact that, in addition to being economically viable, the geothermal energy is considered a clean energy.