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=""]Monogenetic volcanoes are the most common expression of magmatism on the Earth’s surface, and they are found in every tectonic setting, yet key aspects of the behavior and evolution of monogenetic volcanic systems remain poorly understood. Understanding the processes that govern the evolution of monogenetic volcanoes, and the timescales over which these processes operate, is critical for hazard assessment in active distributed volcanic fields. The Southern Volcanic Zone (SVZ), one of the three volcanic regions of The Andes, displays a diverse landscape characterized by historically and potentially active volcanic structures, including ~60 large stratovolcanoes, three giant silicic caldera systems, and hundreds of small eruptive centers. Even these monogenetic volcanoes are considerably smaller in size and volume, they tend to be grouped in space and time, forming distributed volcanic fields, and provide information from source to surface processes that are usually obscured by the commonly dominant more evolved compositions in the Andean arc. Among the Holocene clustered small eruptive centers within the SVZ, this project focuses on the youngest distributed volcanic field in Chile, Carrán-Los Venados, which includes not only the most recent monogenetic eruption in Chile, which occurred in 1979, but it also hosts two other historical eruptions in 1907 and 1955. The Carrán-Los Venados distributed volcanic field (CLV) has received limited attention, despite its placement at position No. 9 in the specific risk ranking of active volcanoes in Chile compiled by SERNAGEOMIN in 2020. Past research on the CLV has mostly focused on chronicling and observing the impacts of the historic eruptions. While some studies have touched upon the geochemical and tectonic aspects of the region, there remains a distinct absence of a comprehensive and cohesive examination of the entire volcanic field. Therefore, building upon previous research conducted in CLV, this project aims to tackle this knowledge gap, and we propose to carry out a detailed multi-disciplinary study (physical volcanology, petrology/geochemistry, and volcanic hazards). Primary research questions include: When did the volcanism start in CLV? What processes contribute to the formation of this volcanism, and what are the magmatic factors that influence its evolution? Where does the volcanic activity take place, and how does it manifest on the surface? What should we expect in the next eruption? To answer these questions, we propose a methodology based on deposit characterization and mapping, geochronology, morphometry, rheology, petrography, mineral chemistry, geothermobarometry and hygrometry, and geochemical characterization and modelling. The integration of these diverse datasets will provide key constraints on the sources, processes, and timescales of magma ascent and storage leading to eruption of the CLV clustered small eruptive centers and small stratovolcanoes, providing an important framework for better understanding the behavior of distributed volcanic fields globally. Furthermore, this project aims to provide valuable support to undergraduate and graduate students, who will have the unique opportunity to engage in all aspects of this research project, making it a significant component of their dissertation studies. Additionally, the study will foster ongoing international collaboration, creating avenues for future student and faculty exchanges. Moreover, it will facilitate outreach educational initiatives for the local community, including specialized seminars, thereby promoting knowledge dissemination and interactive learning experiences.[/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 proyecto tiene como objetivo desarrollar e implementar modelos de aprendizaje automático (Machine Learning, ML) para analizar datos ómicos generados a partir de plantas agronómicas, con el fin de identificar patrones moleculares clave asociados a su productividad, resistencia a estreses abióticos (como sequía y salinidad) y bióticos (como plagas y enfermedades), y su adaptación a condiciones climáticas cambiantes.[/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 main objective of this proposal is to study the miRNA:mRNA post-transcriptional regulatory networks in non-model plant species associated with the process of climate change stress resilience.The proposal integrates the development of computational algorithms, the use of massive data of public non-coding RNA sequences, and the use of a biological model to study post-transcriptional regulatory networks (at the genome-scale) in biological processes associated with climate resilience and adaptation of endemic plant species.[/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=""]Producción Escalable de Inmunoestimulantes Nanoestructurados para el Control de Piscirickettsiosis en Salmón del Atlántico[/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=""]PROPOSAL ABSTRACT: Traditional archaeology proposes that the first settlers of South America moved preferentially along the Andes or the Pacific coast. Given that the Andean Puna (>3,000 masl) was an outstanding ecological megapatch that concentrated similar resources throughout the Andes, it was an attractive migratory route. This paved the way for the establishment of a unique Altiplano socio-ecological system, which later became the cradle of more complex cultural developments. Stable resources, temperate climate and relatively easy movements along the coastline has made the Pacific coast an even stronger candidate to explain early human dispersal and the construction of long-term cultural niche. In contrast, the Intermediate Depression in the hyperarid core of the Atacama Desert, between the Pacific coast and the Andes has not been perceived as a sufficiently productive enough ecosystem to support early human settling and dispersion. Theoretically, it has been assumed that it was used as an area of complementary resources for both coastal and Andean hunter-gatherer societies. In this proposal, we expect to show that this traditional view is incorrect and propose that the Intermediate Depression was not just an area of complementary resources and a barrier for human dispersal. On the contrary, we aim to provide new data showing how this region facilitated local settling and the expansion of H. sapiens into different ecosystems of South America, as it acted as an interglacial ecological refuge. Moreover, we propose that, despite an almost complete lack of rainfall, the Pampa del Tamarugal (PdT) was a much more productive and complex ecosystem during the Pleistocene-Holocene transition than today. Well-dated early residential areas, along with certain geomorphological and hydroclimatic features such as high watertable, mild temperatures and relatively warm winters generated extensive and diverse wetlands, creating some enclaves of the PdT very attractive compared to other regions. One of our main goals is to find these places, and ecologically and culturally characterize them. Conversely, we will investigate the potential of this basin as a glacial refuge a self-contained ecosystem that harbored many species of plants and animals that today occur at higher elevations, and uniquely suited to sustain small populations of hunter-gatherers that moved into the region, who then adopted and transformed this environment into their home. In this context, this proposal aims to research and understand how human societies developed long-term residential systems in a former ecological refuge withing this hyperarid desert. By describing and analyzing the dynamically productive environmental conditions of the PdT, we will address three major research problems: (a) the development of long-term residential systems, which gave rise to a conspicuous Intermediate Depression or pampa socio-ecological system, (b) the emergence of the PdT as a glacial refuge during the last glacial-interglacial transition; and (c) the coevolution and interdependence of the natural and cultural systems that ended with the disappearance of the pampa socio-ecological system and concomitant sequential extinction and extirpation of its biodiversity. The corollary of this process was that at the beginning of the Holocene, when the availability of water became insufficient, an exodus took place that must have had profound consequences for these groups, who had to abandon this landscape that they co-created for almost 2,000 years. Consequently, unlike the Andes or the Pacific coast, this early socio-ecological system did not continue into the Holocene. The lack of high quality and publicly available archaeological, paleoecological and paleontological datasets has weakened the general theoretical debate on early human migrations, settlement and the development of local socio-ecological systems. Here, we conceive human societies as part of the natural ecosystems on which they depend for their subsistence using a socio-ecological approach to analyze and understand the relationship and mutual influence between humans and what we consider nature today. This does not mean that early hunter-gatherers did not exploit or overexploit natural resources, but that they viewed them as social beings and heavily sanction overexploitation when it occurs or try to avoid it, for example through the implementation of taboos. Our project proposes the novel hypothesis that the Intermediate Depression offered sufficient conditions and resources for the development of a residential system and a unique pampa cultural tradition. Our view contrasts with the idea that the settlement pattern of the terminal Pleistocene hunter-gatherers would have been highly mobile and short-lived. The second novelty of this research is the composite methodology, that integrates different disciplinary methods such as: stable isotope analyses including Sr (to search for regional human mobility); paleogenomics to improve the resolution of morphological bone and plant taxa determination; geochronological dating, involving OSL and U/Th techniques to expand our chronologies; and technomorphological characterization of lithic, bone, wooden and textile artifacts, through complete chaîne opératoire methodology, pedological studies for soil horizon description. In sum, our major goal is to understand a different migration route and settlement system for the early peopling of the western slope of the Andes, by defining and explaining the characteristics of the residential systems developed in the PdT during the Pleistocene-Holocene transition, and the local ecologies associated to them. Our data will contribute towards resolving an old problem: the colonization of South America through the study of what is likely one of the best preserved and mostly unaltered sets of early American sites in all South America.[/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=""]Tactile sensing capabilities are crucial for manual dexterity, yet remain beyond the reach of today’s robots. While recently developed robotic skins can measure contact forces accurately, they cannot bend or stretch, and therefore they cannot cover complex robot parts, such as finger joints or deformable links. Lorenzo and team will develop an innovative skin based on magnetic technology that can measure 3D contact forces on multiple contact points, as well as bend and stretch. This will unlock full-cover articulated and soft robots, which will ultimately lead to vastly advanced robot dexterity in manufacturing, logistics, agriculture, healthcare, and beyond.[/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=""]La ocurrencia de desastres asociados a amenazas naturales representa un desafío muy importante para Chile. Los frecuentes incendios en territorios forestales, los costos asociados a aluviones e inundaciones como las ocurridas en los inviernos de 2021 y de 2023 en la región de O’Higgins, e incluso la permanente amenaza de terremotos y volcanes, representan enormes costos para los territorios. Recientemente, la institucionalidad pública ha avanzado en el desarrollo de políticas de prevención de desastres con la aprobación de la Ley 21.364 (2021), creando el Sistema Nacional de Prevención y Respuesta ante Desastres (SINAPRED), sustituyendo la Oficina Nacional de Emergencia (ONEMI) por el Servicio Nacional de Prevención y Respuesta ante Desastres (SENAPRED). La ciencia tiene mucho que aportar a esta nueva institucionalidad pública. La Universidad de O’Higgins (UOH), por ejemplo, colabora con SENAPRED O’Higgins a través de la Mesa de Peligros Geológicos, instaurada el año 2021. No obstante, el desafío de la prevención de desastres y el fomento de la resiliencia necesita otras perspectivas que consideren las características de los espacios geográficos donde se producen los riesgos. Se necesita un trabajo colaborativo con la institucionalidad pública y la comunidad local, pero sobre todo, una perspectiva interdisciplinaria que aúne los conocimientos de la ciencia social y natural. La propuesta presentada busca generar una red que vincule a investigadores/as nacionales (UOH y Universidad de Chile) con investigadores de universidades de Países Bajos (Universidad Libre de Amsterdam) y Dinamarca (Universidad de Copenhague), para realizar actividades de intercambio de experiencias e investigación aplicada. Estos investigadores han logrado incidir en políticas públicas y estrategias a nivel local y regional en diversos países de Europa. Siguiendo una mirada multi-sectorial y nutridos de varias disciplinas, estos expertos han desarrollado perspectivas, herramientas y conocimientos de los cuales, sin duda, podemos aprender dada la coyuntura chilena con su nueva institucionalidad. El proyecto contempla tres etapas para crear y potenciar esta red. Primero, el equipo nacional visitar Ámsterdam y Copenhague para vincularse con equipos interdisciplinarios, intercambiando experiencias de trabajo aplicado. Destaca el trabajo que realiza el equipo de Chile con SENAPRED O’Higgins, y el trabajo aplicado en Europa con el Proyecto LINKS (https://links-project.eu/). Segundo, un experto de Europa visitará la UOH. En esta visita, el invitado participará en reuniones y talleres, y colaborará con investigación aplicada en la región. Y tercero, el proyecto realizará una serie de eventos presenciales, como un seminario nacional con el experto internacional, además de talleres aplicados con diferentes partes interesadas. A estos eventos se invitará a representantes de organismos públicos, académicos/as de otras instituciones y a la comunidad interesada en general. Como resultado, esta red permitirá: (1) intercambiar experiencias y difundir conocimiento aplicado sobre la gestión del riesgo a través de perspectivas interdisciplinarias; (3) potenciar el capital humano de estudiantes de la UOH y promover la investigación interdisciplinaria en la gestión del riesgo; y (3) crear y consolidar una entidad que visibilice el trabajo que realiza la UOH en torno a la gestión del riesgo, contribuyendo así a la reducción del riesgo de desastres a nivel regional y de la macrozona.[/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=""]A[/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=""]PINNs[/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=""]La ocurrencia de desastres asociados a amenazas naturales representa un desafío muy importante para Chile. Los frecuentes incendios en territorios forestales, los costos asociados a aluviones e inundaciones como las ocurridas en los inviernos de 2021 y de 2023 en la región de O’Higgins, e incluso la permanente amenaza de terremotos y volcanes, representan enormes costos para los territorios. Recientemente, la institucionalidad pública ha avanzado en el desarrollo de políticas de prevención de desastres con la aprobación de la Ley 21.364 (2021), creando el Sistema Nacional de Prevención y Respuesta ante Desastres (SINAPRED), sustituyendo la Oficina Nacional de Emergencia (ONEMI) por el Servicio Nacional de Prevención y Respuesta ante Desastres (SENAPRED). La ciencia tiene mucho que aportar a esta nueva institucionalidad pública. La Universidad de O’Higgins (UOH), por ejemplo, colabora con SENAPRED O’Higgins a través de la Mesa de Peligros Geológicos, instaurada el año 2021. No obstante, el desafío de la prevención de desastres y el fomento de la resiliencia necesita otras perspectivas que consideren las características de los espacios geográficos donde se producen los riesgos. Se necesita un trabajo colaborativo con la institucionalidad pública y la comunidad local, pero sobre todo, una perspectiva interdisciplinaria que aúne los conocimientos de la ciencia social y natural. La propuesta presentada busca generar una red que vincule a investigadores/as nacionales (UOH y Universidad de Chile) con investigadores de universidades de Países Bajos (Universidad Libre de Amsterdam) y Dinamarca (Universidad de Copenhague), para realizar actividades de intercambio de experiencias e investigación aplicada. Estos investigadores han logrado incidir en políticas públicas y estrategias a nivel local y regional en diversos países de Europa. Siguiendo una mirada multi-sectorial y nutridos de varias disciplinas, estos expertos han desarrollado perspectivas, herramientas y conocimientos de los cuales, sin duda, podemos aprender dada la coyuntura chilena con su nueva institucionalidad. El proyecto contempla tres etapas para crear y potenciar esta red. Primero, el equipo nacional visitar Ámsterdam y Copenhague para vincularse con equipos interdisciplinarios, intercambiando experiencias de trabajo aplicado. Destaca el trabajo que realiza el equipo de Chile con SENAPRED O’Higgins, y el trabajo aplicado en Europa con el Proyecto LINKS (https://links-project.eu/). Segundo, un experto de Europa visitará la UOH. En esta visita, el invitado participará en reuniones y talleres, y colaborará con investigación aplicada en la región. Y tercero, el proyecto realizará una serie de eventos presenciales, como un seminario nacional con el experto internacional, además de talleres aplicados con diferentes partes interesadas. A estos eventos se invitará a representantes de organismos públicos, académicos/as de otras instituciones y a la comunidad interesada en general. Como resultado, esta red permitirá: (1) intercambiar experiencias y difundir conocimiento aplicado sobre la gestión del riesgo a través de perspectivas interdisciplinarias; (3) potenciar el capital humano de estudiantes de la UOH y promover la investigación interdisciplinaria en la gestión del riesgo; y (3) crear y consolidar una entidad que visibilice el trabajo que realiza la UOH en torno a la gestión del riesgo, contribuyendo así a la reducción del riesgo de desastres a nivel regional y de la macrozona.[/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]