Proyectos

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]The world's transition to using cleaner energy sources to address climate change has led to a sharp rise in the demand for base and precious metals. Consequently, discovering new ore deposits to meet this growing demand and prevent supply shortages has emerged as one of the greatest challenges of the 21st century. Discovery of new magmatic-hydrothermal ore deposits can be improved based on a fundamental understanding of the geological processes that control the flux and focusing of ore-constituting elements in the Earth’s crust, and by identifying the differences between the bulk-rock and mineral chemistry of ore-forming and ordinary—barren—granitoids. Large metal anomalies in the Earth’s upper crust, such as porphyry copper-(molybdenum) deposits (PCDs), occur in intimate association with oxidized and water-rich arc magmatism in subduction zones. However, these deposits occur in restricted crustal domains and form in response to specific tectono-magmatic events, indicating that not all arc magmas have the same ore-forming potential. Understanding why only some magmas produced large PCDs while most other arc magmas remain barren is a fundamental scientific question and key to developing efficient exploration strategies. The volatile element composition of arc magmas, including water, sulfur, and halogens such as chlorine and fluorine, as well as their oxygen fugacity, exert a critical control on their ore-forming potential (i.e., ore fertility). These components are not only key to the complexation and transport of ore metals during hydrothermal activity, but also influence the amount of ore metals transported by magmas and the efficiency to which they are transferred from magmas to exsolved fluids. Magmatic differentiation in lower crustal hot zones beneath thick crustal regions is expected to enhance the volatile element budget and oxygen fugacity of evolving magmas that are discharged to the upper crust. This occurs due to the accumulation of incompatible volatile elements during successive cycles of recharge by mafic magmas and crystallization, facilitated by the deeper and hotter conditions beneath thicker arc crusts. As such, an increasingly recognized hypothesis holds that ore-forming magmas display a particularly increased budget of volatile elements and higher oxygen fugacities when compared to barren arc magmas, and that this is largely influenced by the arc crust thickness. The proposed work will test this hypothesis by focusing on the Miocene to Mio-Pliocene magmatism and associated world-class PCD mineralization in the Andes of central Chile. From the Early Miocene to the Mio-Pliocene, the arc segment located between latitudes ~33–34.5° S in the Andes of central Chile has seen a continued increase in crustal thickness and has evolved from being barren in the Early Miocene to producing some of the largest PCDs of the world in the Mio-Pliocene, such as El Teniente and Rio Blanco-Los Bronces. This geological scenario and the spatial and age distribution of the associated outcropping intrusive rocks offer a unique opportunity to investigate the temporal evolution of the volatile composition of magmas and its consequences for ore fertility. The goal of this proposal is to examine, adopting a regional scale perspective, the evolution in the volatile composition and oxygen fugacity of magmas produced in this arc segment and its relationship to magmatic ore fertility, as well as how this may have been influenced by changes in crustal thickness. To achieve this, I will sample an extensive suite of granitoids that represent a continuum from Early Miocene to Mio-Pliocene magmas, including porphyry-forming intrusions. By combining zircon petrochronology, apatite, biotite, and amphibole mineral chemistry, in conjunction with the bulk-rock composition of intermediate to felsic intrusive rocks, I will be able to constrain relative changes in the hydration state, sulfur contents, halogen and oxygen fugacities, as well as in their associated crustal thickness during the evolution of the selected arc segment. This will be done by implementing a combination of cutting-edge analytical techniques, including synchrotron-based sulfur X-ray absorption near edge structure spectroscopy, electron probe microanalysis, (laser ablation) inductively coupled plasma mass spectrometry, and X-ray fluorescence spectrometry. I aim at (1) testing the differences in the volatile composition of barren and ore-forming intrusive rocks; (2) determining whether there is a gradual change in the volatile systematics of magmas during the evolution of the studied arc segment; and (3) analyzing the relationship between variations in crustal thickness and the volatile composition of associated magmas. The results of this proposal will lead to a better understanding of the magmatic controls underpinning the formation of giant PCDs and will provide valuable insights into identifying the differences between the bulk-rock and mineral chemistry of ore-forming and barren granitoids as tools for vectoring mineralized regions.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""][/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]The recently awarded Fondecyt Iniciación no. 11241126 (PI Jorge Romero) aims to determine the distribution and geometry of slope instability and its controlling factors (i.e., textural and compositional characteristics of rocks, their mass structure and discontinuities, and their mechanical rock properties) at the San José and Nevados de Chillán Volcanic Complexes. Specific objectives involve encompassing the production of thematic maps to represent the factors contributing to instability (e.g., magmatic intrusions, hydrothermal alteration areas, observed landslides, etc.) and defining and characterizing lithotechnical units based on field observations. In addition, it should determine the mechanical rock properties of natural samples based on laboratory tests that represent different scenarios. Lastly, these results should be incorporated into numerical models to represent unstable areas, failure planes, and conditions for failure.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]Tenacibaculosis is an emerging pathogen recently classified as high-risk disease. Since 2020 it is the second pathogen after Piscirickettsia salmonis producing higher mortalities in Atlantic salmon. Diverses species of Tenacibaculosis has been described in Chile, but Tenacibaculum dicentrarchi present the higher prevalence in culture centers. Before 2018, underreporting of Tenacibaculosis was possible due to the external signology is similar with Piscirickettsiosis. P. salmonis is the main pathogen in Chilean salmon farming, causing the principals mortalities because of diseases. In recent years, concerns related to Tenacibaculosis and Piscirickettsiosis coinfection have increased due to detrimental effects on the health status of fish in comparison to the single infection. Our proposal aim to characterize the immune response elicit by T. dicentrarchi in Atlantic salmon and describe how it is related to a coinfection by P. salmonis. First, we propose the description of the single infection of T. dicentrarchi due to the lack of information about the immune response it induces in Atlantic salmon. Then, we propose the characterization of the coinfection between T. dicentrarchi and P. salmonis and the possible weaker of the health status of the fish due to T. dicentrarchi may favors the development of the secondary infection. Therefore, we hypothesize that “Tenacibaculum dicentrarchi chronic infection triggers a type 2 immunity (Th2/M2) IL-4/13/ IL-10+ phenotype in head kidney and spleen of Atlantic salmon, increasing the secretion of anti-inflammatory cytokine IL-10, which favor and increase the severity of Piscirickettsia salmonis coinfection”. The general objective of the proposal is to demonstrate that a chronic infection of Tenacibaculum dicentrarchi causes in Atlantic salmon a status of head kidney and spleen immunosuppression presented an IL 4/13/ IL-10+ phenotype and increasing the mortality provoked by Piscirickettsia salmonis coinfection. To demonstrate the hypothesis, three specific objectives are proposed. First specific objective is “Characterize the immunological response of the single infection of T. dicentrarchi and coinfection with T. dicentrarchi and P. salmonis in Atlantic salmon under field conditions during outbreak seasons”. For this specific objective, we designed the Trial 1: Field sampling in open-sea cages during a single infection of T. dicentrarchi in winter and a coinfection with T. dicentrarchi and P. salmonis in spring. The analysis of the immune response will be through gene expression by RT-PCR and proteins by ELISA and western blotting. Then, the second objective propose is “Verify the type 2 immunity (Th2/M2) IL-4/13/ IL-10+ phenotype elicit by a T. dicentrarchi infection in Atlantic salmon under controlled conditions of laboratory”. To accomplish this goal we designed the Trial 2: A single infection challenge with T. dicentrarchi in Atlantic salmon in laboratory conditions in order to better characterize the immune response at a cellular level by flow cytometry and a molecular level by RNA-seq, RT-PCR and protein level. The final specific objective is “Characterize at the immunological level the development and severity of P. salmonis infection in Atlantic salmon infected by T. dicentrarchi under controlled conditions of laboratory”. To achieve this objective we designed the Trial 3: A coinfection with T. dicentrarchi and P. salmonis in Atlantic salmon in laboratory conditions with the respective single infection controls of each pathogen and posterior analysis by molecular and protein level. The expected results are: 1) The characterization of the immune response at functional level of the single infection of T. dicentrarchi and the coinfection of T. dicentrarchi and P. salmonis in Atlantic salmon in open-sea cages; 2) Verification that T. dicentrarchi triggers a type 2 immunity (Th2/M2) with an increase in the secretion of cytokine IL-10 demonstrated through transcript, protein, and cellular analysis in laboratory conditions that will let us a better resolution of the immune response characterization in comparison with the field conditions; 3) Characterization of the development of a more harmful P. salmonis infection due to the weaker health status on Atlantic salmon produced by of T. dicentrarchi, which means a higher bacterial load of P. salmonis and mortality rate in coinfected fish with T. dicentrarchi and P. salmonis. The results obtained in this research will provide animal health information to improve the productive management of salmonids and contribute to the knowledge of the health status of Atlantic salmon in the context of the two main pathogens affecting Chilean aquaculture nowadays.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]Los problemas en la teoría de parada óptima se aplican a muchas situaciones en la vida. Por ejemplo, cuando decidimos mudarnos, tenemos que determinar cuándo dejar de buscar una casa; al estacionar el auto, debemos decidir cuándo tomar un lugar disponible en lugar de seguir buscando uno mejor; cuando ocurre un terremoto, el gobierno debe decidir cuándo dejar de observar y comenzar a evacuar a la población, etc. Aunque algunas de estas decisiones deben tomarse con más frecuencia que otras y el riesgo involucrado no es el mismo en todas las situaciones, la idea detrás de todos estos problemas es similar: un tomador de decisiones observa un proceso que evoluciona en el tiempo e implica cierta aleatoriedad. Basándose solo en lo que se conoce, se debe tomar una decisión que maximice la recompensa o minimice el costo. Entonces, la pregunta principal aquí es: ¿cuándo deberíamos detenernos? Responder a esta pregunta es importante para tomar buenas decisiones. Sin embargo, no siempre es fácil debido a la información incompleta sobre el futuro. Esto llevó al surgimiento de un subcampo de la teoría de probabilidad, la teoría de parada óptima, que tiene como objetivo mejorar las probabilidades de tomar una buena decisión. El objetivo de este proyecto es estudiar diferentes problemas en este campo, modelándolos y obteniendo resultados teóricos así como también estudiar el impacto de los resultados en la práctica.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

Proyecto de investigación que apunta al estudio de practicas sostenibles para el manejo de sistemas silvopastoril en el secano costero. El proyecto involucra el estudio de la materia orgánica del suelo, además de una serie de variables que pueden impactar el manejo de los agroecosistemas

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]Proyecto de investigación que apunta al estudio de practicas sostenibles para el manejo de sistemas silvopastoril en el secano costero. El proyecto involucra el estudio de la materia orgánica del suelo, además de una serie de variables que pueden impactar el manejo de los agroecosistemas[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]Proyecto de investigación que apunta al estudio de practicas sostenibles para el manejo de sistemas silvopastoril en el secano costero. El proyecto involucra el estudio de la materia orgánica del suelo, además de una serie de variables que pueden impactar el manejo de los agroecosistemas[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]SaviaLab es la combinación de dos términos: Savia (la energía, elemento vivificador) y Laboratorio (lugar con los medios para realizar investigaciones, experimentos y trabajos científicos y técnicos). SaviaLab es una iniciativa impulsada por la Fundación para la Innovación Agraria (FIA), que busca ser un agente activo en el desarrollo de las comunidades educativas locales, impulsando la innovación temprana con un enfoque silvoagropecuario, para la construcción de una sociedad más analítica y propositiva. Promoviendo formas de vivir que reconozcan y releven las heterogeneidades culturales, ambientales y sociales, favoreciendo prácticas colaborativas en el respeto de la sabiduría y valores tradicionales en un entorno en constante transformación. Buscamos contribuir con las comunidades educativas locales, en el desarrollo y fortalecimiento de habilidades y competencias, que favorezcan y promuevan el bienestar y el desarrollo integral de sus miembros y sus entornos, a través de procesos de innovación temprana con un enfoque silvoagropecuario. SaviaLab se trabajará en grupos de estudiantes quienes desarrollarán un proyecto de innovación a lo largo de toda la experiencia formativa. El avance del proyecto se llevará a cabo a través de la realización de actividades individuales y grupales, así como en clases o salidas a terreno, todas apoyadas con material didáctico en formato hojas de trabajo. Además, cada docente podrá adoptar la metodología a diversas asignaturas o talleres, según su especialidad, y así propiciar el trabajo colaborativo entre docentes. El modelo de innovación propuesto por SaviaLab, comprende un proceso de 2 fases: La fase Formativa seguida de la fase Concurso, espacio en donde los equipos de docentes y estudiantes presentan los resultados de lo desarrollado en la fase Formativa. La fase formativa, considera 6 etapas conducentes al desarrollo de una idea innovadora, las cuales se distribuyen en dos unidades. Cada una de estas etapas plantea desafíos diferentes que adquieren sentido al ser considerados como parte de un proceso mayor: la innovación temprana. En su versión 2024, se ejecutará en un formato híbrido, que considera actividades presenciales y actividades remotas tanto para la Fase Formativa como para la Fase Concurso.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]El propósito del proyecto consiste en conocer si el cine de índole intercultural funciona como un mecanismo educativo capaz de contrarrestar actitudes de racismo o discriminación en escuelas públicas de las regiones de O'Higgins y del Maule, específicamente, en escuelas públicas que ofrecen enseñanza básica y que tienen alta matrícula con niños y niñas migrantes[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]