Bibliografías temáticas / KAIST

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Literatura académica sobre el tema "KAIST"

Autor: Grafiati
Publicado: 10 de marzo de 2023

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Artículos de revistas sobre el tema "KAIST"

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Heo, Seongkook, Sunjun Kim, Jaehyun Han, Jiseong Gu, Jaeyeon Lee, Jeongmin Son, Jin Gun Jung, Eunhye Youn, Sunggeun Ahn y Geehyuk Lee. "Human-computer interaction lab @KAIST". Interactions 22, n.º 2 (25 de febrero de 2015): 14–17. http://dx.doi.org/10.1145/2732252.

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Tyler, Neil. "Touch Sound Localisation Technology". New Electronics 52, n.º 1 (8 de enero de 2019): 7. http://dx.doi.org/10.12968/s0047-9624(22)60853-8.

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Ju-Young, Shin. "KAIST, Center for Advanced Functional Polymers". Seikei-Kakou 13, n.º 10 (20 de octubre de 2001): 686–88. http://dx.doi.org/10.4325/seikeikakou.13.686.

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Wohn, D. Y. "Familiar Tune for New KAIST Leader". Science 313, n.º 5795 (29 de septiembre de 2006): 1867d. http://dx.doi.org/10.1126/science.313.5795.1867d.

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Pransky, Joanne. "The Pransky interview: Dr Jun Ho Oh, Professor and Director of Humanoid Robot Research Center, KAIST; Cofounder, Rainbow Robotics Co." Industrial Robot: An International Journal 44, n.º 6 (16 de octubre de 2017): 695–99. http://dx.doi.org/10.1108/ir-08-2017-0141.

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Purpose The following paper is a “Q&A interview” conducted by Joanne Pransky of Industrial Robot Journal as a method to impart the combined technological, business and personal experience of a prominent, robotic industry PhD-turned-entrepreneur regarding the commercialization and challenges of bringing a technological invention to market. This paper aims to discuss these issues. Design/methodology/approach The interviewee is Dr Jun Ho Oh, Professor of Mechanical Engineering at the Korea Advanced Institute of Science and Technology (KAIST) and Director of KAIST’s Hubolab. Determined to build a humanoid robot in the early 2000s to compete with Japan’s humanoids, Dr Oh and KAIST created the KHR1. This research led to seven more advanced versions of a biped humanoid robot and the founding of the Robot for Artificial Intelligence and Boundless Walking (Rainbow) Co., a professional technological mechatronics company. In this interview, Dr Oh shares the history and success of Korea’s humanoid robot research. Findings Dr Oh received his BSc in 1977 and MSc in Mechanical Engineering in 1979 from Yonsei University. Oh worked as a Researcher for the Korea Atomic Energy Research Institute before receiving his PhD from the University of California (UC) Berkeley in mechanical engineering in 1985. After his PhD, Oh remained at UC Berkeley to do Postdoctoral research. Since 1985, Oh has been a Professor of Mechanical Engineering at KAIST. He was a Visiting Professor from 1996 to 1997 at the University of Texas Austin. Oh served as the Vice President of KAIST from 2013-2014. In addition to teaching, Oh applied his expertise in robotics, mechatronics, automatic and real-time control to the commercial development of a series of humanoid robots. Originality/value Highly self-motivated and always determined, Dr Oh’s initial dream of building the first Korean humanoid bipedal robot has led him to become one of the world leaders of humanoid robots. He has contributed widely to the field over the nearly past two decades with the development of five versions of the HUBO robot. Oh led Team KAIST to win the 2015 DARPA Robotics Challenge (DRC) and a grand prize of US$2m with its humanoid robot DRC-HUBO+, beating 23 teams from six countries. Oh serves as a robotics policy consultant for the Korean Ministry of Commerce Industry and Energy. He was awarded the 2016 Changjo Medal for Science and Technology, the 2016 Ho-Am Prize for engineering, and the 2010 KAIST Distinguished Professor award. He is a member of the Korea Academy of Science and Technology.
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Heo, Jung-Woo, In-Ho Lee y Jun-Ho Oh. "Development of Humanoid Robots in HUBO Laboratory, KAIST". Journal of the Robotics Society of Japan 30, n.º 4 (2012): 367–71. http://dx.doi.org/10.7210/jrsj.30.367.

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Vilches, A., K. Fobelets, K. Michelakis, S. Despotopoulos, C. Papavassiliou, T. Hackbarth y U. Konig. "SiGe HMODFET “KAIST” Micropower Model and Amplifier Realization". IEEE Transactions on Circuits and Systems I: Regular Papers 51, n.º 6 (junio de 2004): 1100–1105. http://dx.doi.org/10.1109/tcsi.2004.829242.

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Kim, Youngmin y Jinsu Choi. "A Study on KAIST Undergraduate Students" Perception of Questions in Lectures". Journal of Gifted/Talented Education 32, n.º 3 (30 de septiembre de 2022): 383–406. http://dx.doi.org/10.9722/jgte.2022.32.3.383.

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Hyun Soo Woo, Woo Seok Kim, Woojin Ahn, Doo Yong Lee y Sun Young Yi. "Haptic Interface of the KAIST-Ewha Colonoscopy Simulator II". IEEE Transactions on Information Technology in Biomedicine 12, n.º 6 (noviembre de 2008): 746–53. http://dx.doi.org/10.1109/titb.2008.920617.

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Hyoung, Kim Tae. "DL Talk by Prof. Seonghwan Cho from KAIST [Chapters]". IEEE Solid-State Circuits Magazine 7, n.º 4 (2015): 103. http://dx.doi.org/10.1109/mssc.2015.2474279.

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Tesis sobre el tema "KAIST"

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Hakim, Bahzad. "Recherches hydrologiques et hydrochimiques sur quelques karsts méditerranéens Liban, Syrie et Maroc /". Beyrouth : Publications de l'Université libanaise : Distribution, Librairie orientale, 1985. http://catalog.hathitrust.org/api/volumes/oclc/23644045.html.

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Kunz, Manuel. "Karst Springs of Lake Ohrid". Zürich : ETH, Eidgenössische Technische Hochschule Zürich, 2006. http://e-collection.ethbib.ethz.ch/show?type=dipl&nr=222.

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Dogwiler, Toby J. "Fluvial disturbances in karst streams /". free to MU campus, to others for purchase, 2002. http://wwwlib.umi.com/cr/mo/fullcit?p3060093.

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Caetano, Bicalho Cristina. "Hydrochemical characterization of transfers in karst aquifers by natural and anthropogenic tracers. Example of a Mediterranean karst system, the Lez karst aquifer (Southern France)". AgroParisTech, 2010. http://pastel.archives-ouvertes.fr/docs/00/56/95/44/PDF/these_CCBICALHO_2010.pdf.

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La source karstique du Lez, localisée dans le bassin Méditerranéen (sud-est de la France), fournit de l’eau potable pour la ville de Montpellier et son agglomération depuis le XIXe siècle. Depuis 1981, un pompage intensif est effectué directement dans le conduit principal au moyen d’une station souterraine de pompage, avec un débit maximal autorisé de 1,700 l/s. Afin de mieux caractériser la dynamique et l’origine des eaux souterraines, mais également d'évaluer l’impact de trois décennies d’un pompage intensif de l’aquifère, des prélèvements ont été réalisés dans différentes conditions hydrologiques depuis mars 2006. La source du Lez ainsi que d’autres sources et forages appartenant à ce système et aux systèmes karstiques voisins ont été régulièrement échantillonnées pour le suivi en continu des paramètres physico-chimiques, des éléments majeurs et en trace, du Carbone Organique Total (COT), des coliformes fécaux et totaux ainsi que des 18O, 2H, 13CTDIC et 87Sr/86Sr. Au moment des crues de reprise qui surviennent après l’étiage, des eaux fortement minéralisées sont identifiées à la source du Lez. Ce comportement singulier a été étudié à un pas de temps fin. L’utilisation d’analyses statistiques multivariées a permis de caractériser les différents types d'eau s’écoulant à la source du Lez. Une approche couplée intégrant les données hydrochimiques et isotopiques a permis de définir les différents types d’eau et les lithologies associées, ainsi que les principales réactions qui contrôlent la chimie des eaux souterraines. Parmi les cinq types d’eau identifiés, deux correspondant à des pôles géochimiques très contrastés, et sont à mentionner : le premier pôle correspond à des eaux géochimiquement plus évoluées, caractérisées par une forte minéralisation, un enrichissement marqué en Cl, Na, Mg, Li, B et Br, des rapports Sr/Ca, Mg/Ca et Cl/Br élevés ainsi que des valeurs en 13CTDIC et 87Sr/86Sr enrichies. Ces eaux, qui correspondent à une signature évaporitique, sont vraisemblablement issues d’un réservoir profond, et associées à un temps moyen de résidence important. Parmi toutes les sources et forages étudiés, cette signature chimique a été uniquement observée pour les eaux de la source du Lez. Le second pôle correspond à des eaux faiblement minéralisées, contenant de fortes concentrations en NO3, bactéries et COT, représentant le flux d’infiltration rapide. Elles soulignent la vulnérabilité du système à l’infiltration rapide et à la contamination anthropique via des systèmes de pertes et de réseaux de fractures bien développé. Des déconvolutions d’hydrogramme à l'aide de multiples traceurs ont été réalisées pour estimer les proportions de participation des deux ou trois pôles d’eau précédemment définis dans les multiples événements de crue survenus entre 2008 et 2010. En considérant les chlorures comme traceur, la participation moyenne des différents types d’eau à l’écoulement à la source est la suivante : 12% pour les eaux profondes, 5% pour les eaux nouvellement infiltrées et 83% pour les eaux de l'aquifère principal. La comparaison entre les données obtenues dans cette étude et les données obtenues avant l’installation de la station souterraine de pompage (données de 1973-1974) montre des changements notables dans la composition chimique des eaux de la source du Lez, en indiquant une diminution de la proportion de participation du réservoir profond aux écoulements à cette source. Cette modification de la composition chimique des eaux peut être attribuée au pompage intensif du système karstique et, en l’absence de changement climatique perceptible, traduit les conséquences directes de ce forçage anthropique sur le fonctionnement général de l’aquifère. L’approche multi-traceurs combinée à l'hydrodynamique apparaît comme un outil très efficace pour caractériser les écoulements souterrains et leurs origines, et semble être potentiellement applicable à d'autres systèmes karstiques complexes similaires comprenant des compartiments profonds qui contribuent à l’écoulement de la source, notamment sur le pourtour méditerranéen où la crise messinienne à permis la mise en place d’une karstification profonde
The Lez karst spring, located in the Mediterranean basin (southern France), supplies with water the metropolitan area of Montpellier (France) since the 19th century. Since 1981, an intense pumping is being performed directly in the main conduit with a maximum exploitation flow rate of about 1,700 l/s. To improve the understanding of groundwater origins and circulation dynamics in this karst system, as well as the impact of three decades of intense water exploitation, groundwater samples have been collected during various hydrologic conditions since March 2006. The springs and wells of the Lez karst system as well as surrounding springs and wells have been monitored for: physicochemical parameters, major and trace elements, Total Organic Carbon (TOC), faecal and total coliforms, 18O, 2H, 13CTDIC and 87Sr/86Sr. During the first recharge events of autumn, high-mineralized waters have been observed at the Lez spring. This singular behaviour was monitored in a fine time-lag. A multivariate statistical analysis revealed the existence of different water-types discharging at the Lez spring. A coupled approach integrating geochemistry and isotopes were applied and provided insight into the different end-members, associated lithologies and the main reactions that control groundwater chemistry. Between the five distinguished water-types, the two more contrasting ones are emphasized: the first one correspond to more geochemically evolved, long residence-time waters, issued from deep layers where evaporite fingerprinting was identified. They are characterized by high mineralization and high concentrations in Cl, Na, Mg, Li, B and Br elements, high Sr/Ca, Mg/Ca and Cl/Br ratios and enriched 13CTDIC and 87Sr/86Sr. Between all the studied springs and wells, this chemical fingerprinting has been uniquely observed for the Lez spring groundwaters. The second water-type corresponds to low mineralized waters with high concentrations in NO3, bacteria and TOC, and represents the flux of rapid infiltration waters. They underline the vulnerability of the system to surface infiltration and anthropogenic contamination through the infiltration of waters by sinkholes and well-developed fracture networks. Hydrograph deconvolutions using multiple tracers were used to estimate the participation of two or three end-members in the various flood-events that occurred between 2008 and 2010. If we use chloride as tracer, the mean estimated participation of the different water types are, as follows: 12% for deep waters; 5% for recent waters and 83% for main aquifer waters. The comparison between present and former studies carried out before the installation of the pumping plant (1973-1974 dataset), indicates historical changes in water hydrogeochemistry, evidencing a decrease of the deep compartment participation to the outflow of the Lez spring. This change in water hydrogeochemistry may be attributed to the intense pumping of the karst system and, in the absence of noticeable climatic changes, traduces the direct consequences of anthropogenic forcing on the overall functioning of the aquifer. The multi-tracers approach combined to hydrodynamics appears as a very efficient tool for characterizing groundwater flows and their origins and seems to be potentially applicable to other similar complex Mediterranean karst systems that were subjected to deep karstification during the Messinian crisis. The features of this crisis seem to play a relevant role on the hydrogeological behaviour of the aquifer and chemical characteristics of waters by the participation of a deep compartment to the outflow of the karst system
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Semler, Keith R. "Development of a Karst Tourism Management Index to Assess Tourism-Driven Degradation of Protected Karst Sites". TopSCHOLAR®, 2019. https://digitalcommons.wku.edu/theses/3143.

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The intent of this research was to create and evaluate a karst tourism management index (KTMI). This index is intended to be a new management tool designed to quantify environmental disturbances caused specifically by tourism activities in karst regions, particularly show caves and springs. In an effort to assess the effectiveness of the index as a management tool in karst terrains, after development, the index was applied to six case study sites. A review of the management policies at each study site was conducted with the use of standard policy critique methods and semistructured interviews with managers at the study sites. After interviews were completed, the newly created index was applied to the study areas with the aid of park land managers. Including land managers in the application process allowed for active land managers to provide more meaningful feedback on potential improvements to the KTMI to ensure the most universally applicable and thoroughly field-tested index tool was created. Upon application and continual refinement of the index to the six study sites, a new data-driven management tool to measure disturbances to karst terrains by tourism was developed. The KTMI consist of an Overall Score category that is broken down into the two main categories of Management and Tourism. The KTMI contains 168 indicators that all need to be scored individually to obtain results, with Management containing 100 of the indicators and Tourism containing the other 68 indicators.
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Florea, Lee John. "The karst of west-central Florida". [Tampa, Fla] : University of South Florida, 2006. http://purl.fcla.edu/usf/dc/et/SFE0001783.

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Wright, Winfield G. "Modeling karst aquifer response to rainfall". Thesis, Virginia Polytechnic Institute and State University, 1986. http://hdl.handle.net/10919/76043.

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A finite-element model (HYDMATCH) uses spring hydrograph discharge data to generate a linear regression relation between fracture conductivity and potential gradient in a karst aquifer system. Rainfall excess in the form of potential energy from sinkhole sub-basins is input to element nodes and routed through a one-dimensional finite-element mesh to the karst spring represented by the last node in the finite element mesh. A fracture-flow equation derived from the Navier-Stokes equation uses fracture conductivities from the regression equation and potential gradient in the last element of the mesh to determine discharge at the spring. Discharge hydrograph data from Nininger spring, located in Roanoke, Virginia, was used to test the performance of the model. Excess from a one-half inch rain was introduced into sinkhole nodes and the regression equation generated by matching discharges from the known hydrograph for the one-half inch rainfall. New rainfall excess data from a one-inch rainfall was input to the sinkhole nodes and routed through the finite-element mesh. The spring hydrograph for the one-inch rainfall was calculated using the regression equation which was determined previously. Comparison of the generated hydrograph for the one-inch rainfall to a known hydrograph for a one-inch rainfall shows similar shapes and discharge values. Areas in need of improvement in order to accurately model ground-water flow in karst aquifers are a reliable estimate of rainfall excess, a better estimation of baseflow and antecedent aquifer conditions, and the knowledge of the karst aquifer catchment boundaries. Models of this type may then be useful to predict flood discharges and contaminant travel times in karst aquifers.
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Pierskalla, William P. Jr. "RETHINKING KARST HAZARD ASSESSMENT IN KENTUCKY". UKnowledge, 2019. https://uknowledge.uky.edu/ees_etds/67.

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Current karst hazard maps in Kentucky reflect the general lithology of the state and ignore or significantly reduce the impact of the actual sinkholes present within these areas. These maps rely on equal weighting, by area, of the Karst Potential Index (KPI) map and the sinkhole inventory map. The KPI is based on a 1:500,000 geologic map and less than 500 data points of carbonate rocks. The sinkhole inventory is derived from topographic maps updated in the 1970s with approximately 10-foot resolution. This method gives a preferential weighting of the KPI over the sinkhole data. Consequently, the current method is broad in scope and ineffective in hazard assessment. There is a need for a reliable karst hazard map for land use planners, government emergency planning agencies, and other stakeholders. In this study, more detailed geology information and LiDAR (Light Detection and Ranging) data are applied to three counties (Bullitt, Logan, and Woodford) to generate a more accurate assessment of karst hazard. An assessment method based on sinkhole density is also tested. By refining the hazard score to more precise areas of concern, future stakeholders will find this data useful in emergency planning and land assessment.
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Birk, Steffen. "Characterisation of karst systems by simulating aquifer genesis and spring responses model development and application to gypsum karst /". Tübingen : Universität Tübingen, 2002. http://www.bsz-bw.de/cgi-bin/xvms.cgi?SWB10236361.

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Furey, Neil M. "Bat assemblages in Vietnamese karst diversity, reproduction, echolocation and ecomorphology /". Thesis, Available from the University of Aberdeen Library and Historic Collections Digital Resources, 2009. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?application=DIGITOOL-3&owner=resourcediscovery&custom_att_2=simple_viewer&pid=33557.

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Thesis (Ph.D.)--Aberdeen University, 2009.
With: Description of a new species od Murina from Vietnam (Chiroptera: Vespertilionidae : Murininae) Gábor Csobra ... et al. Museum of Texas Tech University Occasional papers: 2007, 268. With: A new species of Kerivoula (Chiroptera: Vespertilionidae) from Southeast Asia /Paul J. Bates ... et al. Acta Chiropterologica. 2007: 9(2) 323-337. Includes bibliographical references.
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Libros sobre el tema "KAIST"

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Vecgrāvis, Kristaps. Kaist k̦ekarā vīnogas. Rīgā: JD, 2005.

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Cho, Ho-jin. Sŏuldae sidae chŏngsin kwa KAIST p'ŭrop'esyŏnŏllijŭm: SNU zeitgeist & KAIST professionalism. Kyŏnggi-do Koyang-si: Choŭn Ttang, 2016.

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O-chʻan, Kwŏn, ed. KAIST MBA bijŭnisŭ pʻiltoksŏ 20. Sŏul-si: Haebaragi, 2005.

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Kukhoe ro kan KAIST: K'aisŭt'ŭ kyosudŭl i mal hanŭn kukka mirae chŏllyak! Sŏul-si: Simbooks, 2015.

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Ki-hyŏng, Ko, Arganbright Deane y Conference Board of the Mathematical Sciences., eds. Enhancing university mathematics: Proceedings of the First KAIST International Symposium on Teaching. Providence, RI: American Mathematical Society, 2007.

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K'aisŭt'ŭ. KAIST 100-yŏn ŭi kkum: Kwahak kisul ŭi mirae rŭl sangsang hada. Sŏul: Chisik Konggam, 2022.

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Hye-sil, Chʻoe, ed. Dijitʻŏl sidae ŭi munhwa yesul: Tʻonghap ŭi kanŭngsŏng ŭl kkum kkunŭn KAIST saramdŭl. Sŏul: Munhak kwa Chisŏngsa, 1999.

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Sŏ Nam-p'yo ch'ŏnil ŭi kirok: MIT rŭl pakkugo KAIST rŭl tijain han ch'ongjang. Sŏul-si: Tonga Ilbosa, 2009.

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Mujhase kaisā neha: Kahānī-saṅgraha = Mujhse kaisa neh. Nayī Dillī: Kitābaghara Prakāśana, 2012.

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G, Hahn S., Myung Hyo Chul 1937- y Zelmanov Efim 1955-, eds. Recent progress in algebra: An International Conference on Recent Progress in Algebra, August 11-15, 1997, KAIST, Taejon, South Korea. Providence, R.I: American Mathematical Society, 1999.

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Capítulos de libros sobre el tema "KAIST"

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Lim, Jaeheung, Jun Yeon Yun, Jinhong Ahn y Young June Park. "A CNT Network Platform Integrated on the CMOS Circuit". En KAIST Research Series, 3–18. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9981-2_1.

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Sohn, Hoon, Hyung Jin Lim y Suyoung Yang. "A Fatigue Crack Detection Methodology". En KAIST Research Series, 233–53. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9981-2_10.

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Jung, Jinhwan, Deawoo Kim, Hankyeol Lee y Yung Yi. "Data Networking for Autonomous Fatigue Crack Detection". En KAIST Research Series, 257–79. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9981-2_11.

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Kim, Deawoo, Jinhwan Jung, Hankyeol Lee y Yung Yi. "Energy-Efficient Sensing Data Delivery for Low Power Environmental Sensors". En KAIST Research Series, 281–306. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9981-2_12.

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Chung, Sae-Young y Si-Hyeon Lee. "Coding for Wireless Sensor Networks". En KAIST Research Series, 307–23. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9981-2_13.

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Kim, Il-Doo, Seon-Jin Choi, Sang-Joon Kim y Ji-Su Jang. "Exhaled Breath Sensors". En KAIST Research Series, 19–49. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9981-2_2.

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Jang, Jungwoo, Jihun Lee, Mingyu Kang y Yoon-Kyu Song. "Implantable Neural Sensors for Brain Machine Interface". En KAIST Research Series, 51–73. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9981-2_3.

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Jun, Sang Beom. "Implantable Brain Interface: High-Density Microelectrode Array for Neural Recording". En KAIST Research Series, 75–105. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9981-2_4.

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Oh, Wang-Yuhl. "Optical Coherence Tomography for Clinical Applications". En KAIST Research Series, 107–37. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9981-2_5.

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Park, Inkyu, Daejong Yang y Kyungnam Kang. "Microfabricated and Nanoengineered Chemical Sensors for Air Quality Monitoring System". En KAIST Research Series, 141–70. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9981-2_6.

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Actas de conferencias sobre el tema "KAIST"

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Han, Dongsoo, Sangjae Lee y Sunghoon Kim. "KAILOS: KAIST indoor locating system". En 2014 International Conference on Indoor Positioning and Indoor Navigation (IPIN). IEEE, 2014. http://dx.doi.org/10.1109/ipin.2014.7275535.

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Baik, Seungjoon, Seong Gu Kim, Seong Jun Bae, Yoonhan Ahn, Jekyoung Lee y Jeong Ik Lee. "Preliminary Experimental Study of Precooler in Supercritical CO2 Brayton Cycle". En ASME Turbo Expo 2015: Turbine Technical Conference and Exposition. American Society of Mechanical Engineers, 2015. http://dx.doi.org/10.1115/gt2015-42915.

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The supercritical carbon dioxide (S-CO2) Brayton power conversion cycle has been receiving worldwide attention because of high thermal efficiency due to relatively low compression work near the critical point (30.98°C, 7.38MPa) of CO2. The S-CO2 Brayton cycle can achieve high efficiency with simple cycle configuration at moderate turbine inlet temperature (450∼650°C) and relatively high density of S-CO2 makes possible to design compact power conversion cycle. In order to achieve compact cycle layout, a highly compact heat exchanger such as printed circuit heat exchanger (PCHE) is widely used. Since, the cycle thermal efficiency is a strong function of the compressor inlet temperature in the S-CO2 power cycle, the research team at KAIST is focusing on the thermal hydraulic performance of the PCHE as a precooler. The investigation was performed by first developing a PCHE in-house design code named KAIST-HXD. This was followed by constructing the designed PCHE and testing it in the KAIST experimental facility, S-CO2PE. The test results of the PCHE were compared to the test results of a shell and tube type heat exchanger as well.
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Choi, Hyunseok, Yumi Lee, Jinseok Park y Songcheol Hong. "Digital polar CMOS power amplifier researches in KAIST". En 2015 Asia-Pacific Microwave Conference (APMC). IEEE, 2015. http://dx.doi.org/10.1109/apmc.2015.7413433.

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Kang, Sungwon, In-Young Ko, Jongmoon Baik, Hojin Choi y Danhyung Lee. "KAIST-CMU MSE Program - The Past and the Future". En 2010 23rd IEEE Conference on Software Engineering Education and Training. IEEE, 2010. http://dx.doi.org/10.1109/cseet.2010.24.

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Yi, Sun, Hyun Woo, Woojin Ahn, Woo Kim y Doo Lee. "Clinical Evaluation of the KAIST-Ewha Colonoscopy Simulator II". En 2006 SICE-ICASE International Joint Conference. IEEE, 2006. http://dx.doi.org/10.1109/sice.2006.315458.

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Lee, Eu Hwak, Hee Cheon No, Dong Won Lee y Chul Hwa Lee. "Downcomer Boiling During LBLOCA with Direct Vessel Injection of APR1400". En 14th International Conference on Nuclear Engineering. ASMEDC, 2006. http://dx.doi.org/10.1115/icone14-89553.

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An experimental study has been performed to investigate thermal-hydraulic phenomena in the downcomer during LBLOCA with Direct Vessel Injection (DVI), which is a new Safety Injection System (SIS) of the Advanced Power Reactor 1400 MW (APR1400). In order to understand the downcomer boiling phenomena experimentally, the KAIST Downcomer Boiling experiment has been performed with the same as the thickness of the reactor vessel of APR1400 (21 cm) and a height of 150 cm to observe downcomer boiling phenomena and to measure local parameters such as local phase velocities, local void fraction, collapsed water level and heat flux from the heated wall. From the KAIST Downcomer Boiling experiment, we visually observed strong liquid recirculation and vapor jetting near the heated wall due to the axial migration of voids only in the thin layer (about 4 cm) of the heated wall but little bubble migration out of the bubble region. Local phase velocities and local void fraction were measured to estimate the drift-flux parameters in the downcomer channel. Heat flux from the heated side was back-calculated to find the CHF and to estimate nucleate boiling heat transfer coefficients.
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Ahn, Yoonhan, Jekyoung Lee, Seong Gu Kim, Jeong Ik Lee y Jae Eun Cha. "The Design Study of Supercritical Carbon Dioxide Integral Experiment Loop". En ASME Turbo Expo 2013: Turbine Technical Conference and Exposition. American Society of Mechanical Engineers, 2013. http://dx.doi.org/10.1115/gt2013-94122.

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The Supercritical Carbon Dioxide cycle (S-CO2 cycle) can achieve relatively high efficiency in the moderate temperature (450–750°C) region because the cycle takes advantage of non-ideal properties variation near the critical point. The S-CO2 cycle was originally considered as an attractive candidate for power conversion cycle of the next generation reactors. However due to many benefits of the S-CO2 cycle, it is not only limited to the nuclear application but also considered in other conventional and renewable energy system applications including fossil fuel power plant systems, ship propulsion applications, concentrated solar power systems, fuel cell bottoming power cycles and so on. The major studies settle on the S-CO2 recompressing cycle (also known as Feher cycle) which reduces the waste heat and increases the recuperated heat by recompressing some portion of the flow without heat rejection to increase the thermodynamic efficiency of the cycle. To develop and verify the characteristics of the S-CO2 recompressing cycle, Korean Atomic Energy Research Institute (KAERI) and KAIST research team designed a Supercritical Carbon Dioxide Integral Experiment Loop (SCIEL). 550°C turbine inlet temperature and 20 MPa compressor outlet pressure condition are expected for SCIEL operation and the layout is recompressing cycle but other layouts will be studied as well. The experimental loop facility is designed for studying unique phenomena in components under various conditions and developing the strategy to improve the component performance and overall cycle efficiency. The operating condition and thermodynamic efficiency for SCIEL are evaluated from an in-house code developed by KAIST research team. The effect of the split flow, component sensitivity, and optimum cycle pressure ratio will also be analyzed for the preliminary design of SCIEL. Furthermore, turbomachinery sizes and heat exchanger sizes are estimated from other in-house codes developed by KAIST research team. The overall component specification and performance of SCIEL will be compared to other S-CO2 test loop facilities in other research institutes.
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Cho, Dong-Ho, Nam Pyo Suh, Uooyeol Yoon y Guho Jung. "Shaped Magnetic Field in Resonance Technology and its Application to Transportation System". En ASME 2015 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2015. http://dx.doi.org/10.1115/imece2015-53190.

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KAIST has developed the Shaped Magnetic Field in Resonance (SMFIR) technology that transfers a large amount of energy to electric vehicles when they are running or stationary. The wireless charging SMFIR technology provides a solution to the commercialization barriers of electric vehicles such as the problems of batteries and charging infrastructure. Using 20-kHz wireless power transfer system based on the SMFIR technology, our eco-friendly On Line Electric Vehicle (OLEV) bus was wirelessly powered by 100 kW through a power grid embedded under the road. On the other hand, using high-capacity, high-efficiency and low-cost 60kHz power supply and pickup systems based on the SMFIR technology, tram and high speed train were wirelessly powered by 180 kW and 1 MW through a power grid built in rail roads, respectively. The commercial OLEV tram has been operated commercially from July 2011 in Seoul National Grand Park. Also, the OLEV shuttle bus has been operated for convenience of students and faculty members at KAIST campus since Oct. 2012. In addition, the world’s first intra-city OLEV bus with 100 KW pickup capacity has been operated commercially at Gumi city from March 2014. Then, airgap is about 20 cm and maximum power transfer efficiency is 85 %.
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Kong, Hong Jin. "Sinmyung laser system in KAIST and development of lasers using SBS cell". En 17th Congress of the International Commission for Optics: Optics for Science and New Technology. SPIE, 1996. http://dx.doi.org/10.1117/12.2315973.

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Yi, Sun Young, Kum Hei Ryu, Hyun Soo Woo, Woojin Ahn, Woo Seok Kim y Doo Yong Lee. "Quantitative Analysis of Colonoscopy Skills Using the KAIST-Ewha Colonoscopy Simulator II". En 2007 Frontiers in the Convergence of Bioscience and Information Technologies. IEEE, 2007. http://dx.doi.org/10.1109/fbit.2007.58.

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Informes sobre el tema "KAIST"

1

Yakura, S. J. Visit of the Korea Advanced Institute Science and Technology (KAIST). Fort Belvoir, VA: Defense Technical Information Center, septiembre de 1994. http://dx.doi.org/10.21236/ada292395.

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Pardo Igúzquiza, Eulogio. Karst y fractales. Ilustre Colegio Oficial de Geólogos, diciembre de 2022. http://dx.doi.org/10.21028/eog.2022.12.05.

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¿Qué tienen en común la distribución de galaxias en el universo, la red del metro de Madrid y la estrategia de caza de la tribu de los Hadza en el norte de Tanzania? La respuesta es que las tres están conectadas con el karst, tal y como se describe en este trabajo, a través del carácter fractal del mismo. En efecto, el karst presenta un comportamiento fractal tanto en superficie como en el subsuelo. En superficie, tanto la topografía kárstica como las depresiones cerradas (dolinas) que caracterizan el paisaje kárstico son fractales. En el karst subterráneo, la red de conductos kársticos (cuevas) presenta asimismo un comportamiento fractal.
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Lugo, Ariel E., Leopoldo Miranda Castro, Abel Vale, Tania del Mar López, Enrique Hernández Prieto, Andrés García Martinó, Alberto R. Puente Rolón et al. Puerto Rican Karst-A Vital Resource. Washington, DC: U.S. Department of Agriculture, Forest Service, Washington Office, 2001. http://dx.doi.org/10.2737/wo-gtr-65.

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Brunton, F. R. Karst and hazards lands Mitigation: some guidelines for geological and geotechnical investigations in Ontario karst terrains. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/299760.

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Baichtal, James F. y Douglas N. Swanston. Karst landscapes and associated resources: a resource assessment. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station, 1996. http://dx.doi.org/10.2737/pnw-gtr-383.

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Drumm, E. C., W. F. Kane, J. Ben-Hassine, J. A. Scarborough y R. H. Ketelle. Subsidence of residual soils in a karst terrain. Office of Scientific and Technical Information (OSTI), junio de 1990. http://dx.doi.org/10.2172/6512544.

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NMR Publikations. Kast mindre mat - Guide til miljøvennlig og lønnsom kjøkkendrift. Nordisk Ministerråd, septiembre de 2012. http://dx.doi.org/10.6027/anp2012-742.

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Novichkova, Tatiana. Map of karst caves in the territory of the Russian Federation. Editado por Larisa Loginova. Publishing house "Roskartografiya", octubre de 2007. http://dx.doi.org/10.15356/dm2016-10-17-1.

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White, William B. y Jonathan B. Martin. Frontiers of Karst Research: Proceedings and recommendations of the workshop held in San Antonio, Texas on 3-5 May 2007. Karst Waters Institute Special Publication 13. Fort Belvoir, VA: Defense Technical Information Center, enero de 2009. http://dx.doi.org/10.21236/ada500922.

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BIRK, Steffen y Thomas WAGNER. New directions in the application of hydrograph recession models to karst aquifers. Cogeo@oeaw-giscience, septiembre de 2011. http://dx.doi.org/10.5242/iamg.2011.0261.

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