2016 年臺灣地球科學聯合學術研討會大會開幕式2016 Taiwan
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(Basidiomycetes) in Taiwan
The Corticiaceae (Basidiomycetes) in Taiwan Dissertation zur Erlangung des Grades eines Doktors der Naturwissenschaften (Dr. rer. nat.) im Fachbereich 18 Naturwissenschaften am Institut für Biologie der Universität Kassel vorgelegt von I-Shu Lee aus Taiwan 2010 Tag der Mündlichen Prüfung: Kassel, am 26. Mai 2010 1. Berichterstatter: Prof. Dr. Ewald Langer 2. Berichterstatter: PD Dr. Roland Kirschner 3. Berichterstatter: Prof. Dr. Kurt Weising 4. Berichterstatter: Prof. Dr. Friedrich Schmidt Acknowledgement i Acknowledgement It was Prof. Dr. Chee-Jen Chen who introduced me to fungal field, and sent me to Germany for learning further knowledge. I am greatly indebted to Prof. Dr. Ewald Langer, the leader of Ecology department in Biology institute, Kassel University. He taught me the principles and fundamentals of mycology, and has concentrated my attention towards the Corticiaceae in Taiwan. I own them both much thankfulness for their support and teaching during all these years. I also want to express my sincere thanks to Dr. Clovis Douanla-Meli, who has willing to guide me on fungi determination. Moreover, thanks to Torsten Bernauer, who with Dr. C. Douanla-Meli together helped me correct this thesis. We have discussed several collections and text descriptions. My special thanks go to all members of Ecology department. Carola Weißkopf, Inge Aufenanger, and Ulrike Frieling taught me the skills of fungal cultures and related molecular technology. I am also grateful to be the partner with them in this department. Collections came available for study thanks to the kind help of Prof. Dr. C. J. Chen, Prof. Dr. E. Langer, and Dr. Gitta Langer. I render my thanks to Dr. -
Chi-Chi, Taiwan Earthquake Event Report
TM Event Report Chi-Chi, Taiwan Earthquake .8E 7km depth N 120 23.8 6 M7. m. a. 47 1: 99 19 , 1 2 r e b m e t p e S Chi-Chi Reconnaissance Team Weimin Dong, Ph.D. Laurie Johnson, AICP RMS Team Leader, Earthquake Engineer RMS Event Response Coordinator, Urban Planner Guy Morrow, S.E. Craig Van Anne, M.S. RMS, Structural Engineer OYO RMS, Fire Protection Engineer Akio Tanaka Shukyo Segawa OYO RMS, Geophysicist OYO Corporation, Geophysicist Hideo Kagawa Chin-Hsun Yeh, Ph.D. Engineering & Risk Services, National Center for Research in Earthquake Structural Engineer Engineering, Associate Research Fellow Lun-Chang Chou, Ph.D. Kuo-Liang Wen, Ph.D. National Science and Technology Program for National Science and Technology Program for Hazards Mitigation, National Taiwan University Hazards Mitigation, National Taiwan University Yi-Ben Tsai, Ph.D. Wei-ling Chiang, Ph.D. National Central University, Professor National Central University, Professor Wenko Hsu Institute for Information Industry, Engineer, Special Systems Division The reconnaissance team members arrived in Taiwan on Wednesday, September 23, two days after the earthquake, and initially spent 20 man-days in the field. OYO RMS, OYO, and ERS reconnaissance team members jointly presented preliminary findings at a seminar in Tokyo on October 11. RMS joined Pacific Gas & Electric (PG&E) and members of the Technical Council on Lifeline Earthquake Engineering (TCLEE) on October 10 in a week-long mission to further investigate power disruption and associated business interruption impacts, and collect additional loss data. Many of the team members, particularly our Taiwanese colleagues, have continued investigations of this earthquake. -
Luce Chapel.Pdf
1 Luce Chapel is a renowned architecture in Taiwan. With its outstanding achievements, it certainly stands outin the modern architectural movement of Preface post-war Taiwan. In October 2014, Luce Chapel was chosen to be one of the ten global classic modern architectures, and the first project within Asian architecture,which received the first “Keeping It Modern” (hereafter abbreviated as KIM) Grant from the Getty Foundation. The Grant acknowledgesthese 20th century modern architectures as milestones of human civilization. With high experimental mentalities, groups of architects and engineersof the previous centuryboldlytried out exploratory materials and cutting edge construction techniques, and built innovative architectures thathave stimulated changes in their surrounding environments, histories, local culture, and forever transformed the philosophical approaches of architecture. However, the Getty Foundation also regards these architectures to be under various degrees of risks. Being fifty to sixty or even older, many of these innovative materials and techniques boldly used at the time oftheirsconstruction were not, and still have not been scientifically tested and analyzed to this very day. Furthermore, the productions of many of these materials have been discontinued due to low adoptions in the market, making conservations even more difficult. Therefore, the Getty Foundation KIM grants promote the sustainable conservation of modern architecture. This focus has also been the core value of the Luce Chapel conservation project. Built in 1963, Luce Chapel has stood on the campus of Tunghai University for over 50 years. This building was designed and built to function as a church building, and has maintained its religious purpose over the years.However, as the number of faculty and students continues to grow,the space demand for community engagements and ceremonial activities of colleges and departments on campus have also increased extensively. -
Journal of Environmental Radioactivity 155-156 (2016) 71E83
Journal of Environmental Radioactivity 155-156 (2016) 71e83 Contents lists available at ScienceDirect Journal of Environmental Radioactivity journal homepage: www.elsevier.com/locate/jenvrad Dose estimation for nuclear power plant 4 accident in Taiwan at Fukushima nuclear meltdown emission level * Mei-Ling Tang, Ben-Jei Tsuang , Pei-Hsuan Kuo Dept. of Environmental Engineering, National Chung-Hsing University, Taichung, Taiwan article info abstract Article history: An advanced Gaussian trajectory dispersion model is used to evaluate the evacuation zone due to a nuclear Received 20 July 2015 meltdown at the Nuclear Power Plant 4 (NPP4) in Taiwan, with the same emission level as that occurred at Received in revised form Fukushima nuclear meltdown (FNM) in 2011. Our study demonstrates that a FNM emission level would 30 January 2016 pollute 9% of the island's land area with annual effective dose 50 mSv using the meteorological data on 11 Accepted 31 January 2016 March 2011 in Taiwan. This high dose area is also called permanent evacuation zone (denoted as PEZ). The Available online 23 February 2016 PEZ as well as the emergency-planning zone (EPZ) are found to be sensitive to meteorological conditions on the event. In a sunny day under the dominated NE wind conditions, the EPZ can be as far as 100 km with the Keywords: fi fi Radionuclides rst 7-day dose 20 mSv. Three hundred sixty- ve daily events using the meteorological data from 11 Dispersion model March 2011to 9 March 2012 are evaluated. It is found that the mean land area of Taiwan in becoming the PEZ Nuclear power plant is 11%. -
The Tablelands in the Puli Basin (Central Taiwan)—A
The tablelands in the Puli Basin (central Taiwan)— a geochronological and geomorphological approach to Late Quaternary fluvial sedimentary and erosional processes Die Hauptterrassen im Puli-Becken (Zentral Taiwan)— Studien zur Geochronologie und Geomorphologie spätquartärer fluvialer Erosions- und Akkumulationsprozesse Dissertation Zur Erlangung des akademischen Grades Doktor der Naturwissenschaften (Dr. rer. nat.) am Fachbereich Geowissenschaften der Freien Universität Berlin vorgelegt von Chia-Han Tseng Berlin, 2014 Erstgutachterin: Prof. Dr. Margot Böse Zweitgutachter: Prof. Dr. Bernd Wünnemann Tag der Disputation: 04.Juni.2014 Acknowledgements First of all, I would like to thank Prof. Dr. Margot Böse for giving me the chance to do the doctorate in Germany, a country which I find interesting and want to understand more, and for her encouragement and supports for the entire work. Many thanks will also be given to the German Academic Exchange Service (DAAD, Deutscher Akademischer Austausch Dienst) for providing the scholarship to let me complete my work in the past four years without worrying about the living. I would also like to thank Dirk Wenske, Christopher Lüthgens, Robert Hebenstreit, Tony Reimann, Jacob Hardt, and Marc Bauersachs not only for their valuable opinions and discussions about my research, but also for their great help and suggestions on my stay in Berlin, which really made me have a feeling of “just like home” here in Germany. I also want to thank Mrs. Martine Friedmann for her kind help with some budget affairs and for her delicious home-made cakes. I also appreciate deeply Dr. Phillip Hoelzmann for his valuable comments and discussions on the results of grain size analyses. -
Volcanoes in North Taiwan
Volcanoes in north Taiwan Sheng-Rong Song Department of Geosciences, National Taiwan University Volcanic Provenance of Taiwan 120o 121o 122o E WBP N.P. N Tatun 1、Western Provenance t Kungkuan Keelung ai r Tsa olingsh an o 2、Eastern Provenance St 25 N n a Kuanhsi- w Chutung 3、Northern Provenance ai T W.P. e n a 4 、Kueishantou r r x o e e T l SRT 24 p n e i t a la m Penghu S o Eurasian Plate Pl Philippine Sea Plate l hills C t E.P. Islands a t o s o ao a F n o a n C r n a te s T e Coastal o W Range 23 Lutao L.V Intraplate Basalts Arc-related Lanhsu 22o Volcanics Chung et al.,, 1994 Western Provenance 福建 福建 福建 臺灣 澎湖 臺灣 西部 中部 東部 海峽 群島 西部 西北 西邊 東南 0 大 陸 地 殼 50 大陸岩石圈地函 TH AB 100 AB AB, BA km NE,BA 軟流圈對流上拱 0 50 100km Chung, 1990 Coastal Range of east Eastern Provenance Taiwan Eurasian Plate Okinawa Trough TaiwanLutaoRyukyu Arc North LanhsuLuzon Arc 80 mm/yr Hsuilanhsu South China Philippine Sea Sea Plate Hsiulanhsu ~1000-1300 BP Northern Provenance 0.29~2.1 Ma N Penghiahsu Chinshan KUANYINSHAN (Hsinchuang) VOLCANO Fault 0 5 10 0.5~2.6Mienhuahsu Ma (km) Huapinghsu TATUN VOLCANO CHILUNG Nankan t Chilungtao GROUP aul VOLCANO Fault0.36~0.63 Ma F ~1.0 Ma GROUP ao nchi Ka LINKOU WESTERN 0.8~1.2 Ma TABLELAND FOOTHILLS TA IP EI BASIN ult Fa TAOYUAN TERRACE h HSUEHSHAN hi uc TERRANE Ch Evolution of volcanism in northern Taiwan Westward Advance of Western Edge of Subducting Philippine Plate (WEP) 3 Ma 5 Ma 2 Ma 4 Ma 1 Ma 2 Ma 1 Ma 0 100 km 0 Ma 0 Ma Opening of Okinawa Trough S M R 2 Ma 1 Ma 0 Ma Southward Migration of 0 Ma N55oW Ryukyu Trench 1 Ma 2 Ma Northwestward 7 cm/yr Advance of 3 Ma Manlia Trench 4 Ma 5 Ma Wang et al., 2004 Tatun Volcano Group – Active? Or Extinct? Two definitions of active volcano Empirical Definition 1. -
Tectonic Controls on the Stratigraphic Development of the Rifted Taipei T Basin: a Late Quaternary Marine-Influenced Inland Half Graben
Quaternary International 482 (2018) 27–45 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Tectonic controls on the stratigraphic development of the rifted Taipei T Basin: A late quaternary marine-influenced inland half graben ∗ Pin-Ju Sua,b, Andrew Tien-Shun Linc, , Jyr-Ching Hua, Louis Shu-Yu Tenga a Institute of Geosciences, National Taiwan University, No. 1, Sec. 4, Roosevelt Rd., Taipei, 10617, Taiwan, Republic of China b Central Geological Survey, No. 2, Ln. 109, Huaxin St., Zhonghe Dist., New Taipei, 235, Taiwan, Republic of China c Department of Earth Sciences, National Central University, No. 300, Zhongda Rd., Zhongli Dist., Taoyuan, 32001, Taiwan, Republic of China ARTICLE INFO ABSTRACT Keywords: We establish the three-dimensional stratigraphic architecture of the Taipei Basin and its spatiotemporal pa- Basin subsidence laeoenvironmental development during the past 50 kyr by analysing 36 borehole cores and 177 age dates. We Rift basin calculate the rates of basin subsidence from the borehole data at depths where radiocarbon age dates are Stratigraphic development available. Our results indicate that, during the eustatic sea level falling period (35–20 ka), low rates of sediment Eustatic fluctuation supply and/or rapid basin subsidence controlled sedimentation, leading to a change in the depositional en- Sediment supply vironment from gravelly braided rivers, through sandy braided rivers, to meandering rivers with falling eustatic Taipei Basin sea level. During the early stage of eustatic sea level rise (∼20–10.2 ka), balanced rates of sediment supply, eustasy and basin subsidence maintained the meandering river environment. Rapid sea level rise led to the initial appearance of estuarine facies at ∼10.2 ka and widened the distribution of the estuarine environment after 8.5 ka; however, the coeval phases of rapid basin subsidence ∼10.6–10.2 ka and 9–8.5 ka promoted the first ap- pearance and widening of the estuary, respectively. -
Maritime Trade and Deerskin in Iron Age Central Taiwan
MARITIME TRADE AND DEERSKIN IN IRON AGE CENTRAL TAIWAN: A ZOOARCHAEOLOGICAL PERSPECTIVE A DISSERTATION SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAI‘I AT MĀNOA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN ANTHROPOLOGY DECEMBER 2017 By Ling-Da Yen Dissertation Committee: Barry Rolett, Chairperson Richard Gould Seth Quintus Tianlong Jiao Shana Brown © 2017, Ling-Da Yen ii ACKNOWLEDGMENTS My dissertation would not have been completed without the support of my mentors, colleagues, and family members. Here, I would like to express my sincere appreciation to the people who have helped me academically and emotionally. First, I would like to thank my committee members. As my advisor and committee chair, Dr. Barry Rolett’s continual support and encouragement helped me overcome many obstacles. His support and advice were especially invaluable to me during the frustrating periods of formulating my project and writing my dissertation. Dr. Richard Gould helped to move my dissertation toward new directions and guided me through the whole process of dissertation writing. I especially thank him for giving me academic advice, and sharing his remarkable knowledge regarding maritime archaeology. Dr. Seth Quintus provided me with valuable comments and advice on my work. I also benefited from discussions with him about anthropological concepts and statistical methods that improved my dissertation. I am grateful to Dr. Tianlong Jiao for his guidance in Chinese archaeology, as well as the opportunities he offered me to work at the Bishop Museum, Honolulu. Dr. Shana Brown acted as an exemplary university representative and offered me professional help in history. -
The Relationship Between Tropospheric Ozone and Atmospheric Circulation in Taiwan
THE RELATIONSHIP BETWEEN TROPOSPHERIC OZONE AND ATMOSPHERIC CIRCULATION IN TAIWAN I-CHIEN LAI A dissertation submitted for the degree of Doctor of Philosophy Climatic Research Unit School of Environmental Sciences University of East Anglia June 2010 © This copy of the thesis has been supplied on condition that anyone who consults it is understood to recognise that its copyright rests with the author and that no quotation from the dissertation, nor any information derived therefrom, may be published without the author’s prior, written consent. Abstract The aim of the study is to investigate the relationship between variability in tropospheric ozone in Taiwan and the regional atmospheric circulation, paying particular attention to the influence of long-range transport on ozone pollution levels. The study period is 1994 to 2004. The data used in this study include air pollution data from the Taiwan Air Quality Monitoring Network and NCEP/NCAR reanalysis data. The spatial and temporal variations in weather types have been characterised using an objective circulation classification scheme and relationships with episodes of high ozone levels over Taiwan have been determined. The signature of the large-scale atmospheric circulation associated with high ozone pollution and the connection with long-range transport of ozone precursors and ozone have been identified using spatial composites and back-trajectory analysis. Trajectories were calculated using the Hybrid Single-Particle Integrated Trajectory model. The air pollution data analysis shows that Taiwan experiences a seasonal cycle in ozone levels, with maxima in spring and autumn and a minimum in summer. The spatial composite and back trajectory analyses indicate that long-range transport does play a role in increasing high ozone episodes in Taiwan. -
Hazard Assessment of Volcanic Ballistic Impacts at Mt Chihshin, Tatun Volcano Group, Northern Taiwan
Author's personal copy Nat Hazards https://doi.org/10.1007/s11069-018-3192-4 ORIGINAL PAPER Hazard assessment of volcanic ballistic impacts at Mt Chihshin, Tatun Volcano Group, northern Taiwan A. Nurmawati1 · K. I. Konstantinou1 Received: 2 July 2017 / Accepted: 26 January 2018 © Springer Science+Business Media B.V., part of Springer Nature 2018 Abstract This study investigates the hazard posed by Volcanic Ballistic Projectiles (VBPs) in the area surrounding Mt Chihshin, Tatun Volcano Group, northern Taiwan. Based on the volcano’s current evolutionary stage, we consider two types of volcanic activ- ity during which VBPs can be generated, namely hydrothermal and vulcanian eruptions. Hydrothermal eruptions may occur after a sudden decompression of water in the hydro- thermal system of the volcano, typically due to mass removal processes, while vulcanian eruptions are caused by solidified magma that plugs the eruptive vent and gets blasted when this caprock is no longer able to withstand the pressure in the volcanic conduit. Ini- tial velocities of ejected VBPs were estimated for each type of activity based on physi- cal models and inserted as initial conditions to the equations that describe their motion. A hydrothermal eruption is assumed to occur at the NW flank of Mt Chihshin near the Hsiaoyiokeng fumarole, which is a place prone to flank instability, while a vulcanian erup- tion is assumed to originate from a central vent at the peak of Mt Chihshin. Modeling results suggest that the radii of the areas impacted by VBPs vary between 0.1 and 1.1 km for a hydrothermal eruption, while they become 1.4–5.1 km for a vulcanian eruption. -
Temporal Variations of Gas Compositions of Fumaroles in the Tatun Volcano Group, Northern Taiwan
Journal of Volcanology and Geothermal Research 178 (2008) 624–635 Contents lists available at ScienceDirect Journal of Volcanology and Geothermal Research journal homepage: www.elsevier.com/locate/jvolgeores Temporal variations of gas compositions of fumaroles in the Tatun Volcano Group, northern Taiwan Hsiao-Fen Lee a, Tsanyao Frank Yang a,⁎, Tefang Faith Lan a, Cheng-Hong Chen a, Sheng-Rong Song a, Shuhjong Tsao b a Department of Geosciences, National Taiwan University, No. 1, Sec. 4, Roosevelt Road, Taipei 106, Taiwan b Central Geological Survey, MOEA, P.O. Box 968, Taipei 235, Taiwan ARTICLE INFO ABSTRACT Article history: Hydrothermal activity is common in the Tatun Volcano Group of northern Taiwan. Helium isotopic Received 15 October 2007 compositions of fumarolic samples show that mantle component occupies more than 60% in the previous Accepted 10 June 2008 study. Along with recent seismic results, a magma reservoir is inferred to have existed beneath the area of Available online 18 June 2008 Da-you-keng, where fumarolic venting is the most active in Tatun Volcano Group. Progressive increases of HCl concentrations and SO /H S ratio in fumaroles from Da-you-keng have been observed since August 2004. Keywords: 2 2 The HCl concentration changed from almost the detection limit to thousands of ppm, even up to 30,000 ppm. Tatun Volcano Group Taiwan SO2/H2S ratios varied from almost 0 to 3; hence SO2 became the dominated S species in this area. These volcanic gases variations were accompanied by rising temperature of fumaroles in the Tatun Volcano Group, especially in 3He/4He the area of Da-you-keng (from boiling point to 131 °C). -
Three-Dimensional Density Structures of Taiwan and Tectonic Implications
Journal of Asian Earth Sciences 124 (2016) 247–259 Contents lists available at ScienceDirect Journal of Asian Earth Sciences journal homepage: www.elsevier.com/locate/jseaes Full length article Three-dimensional density structures of Taiwan and tectonic implications based on the analysis of gravity data ⇑ Hsien-Hsiang Hsieh a,b, Horng-Yuan Yen a, a Department of Earth Sciences, National Central University, Jhongli, Taiwan, ROC b Institute of Oceanography, National Taiwan University, Taipei, Taiwan, ROC article info abstract Article history: Taiwan is located in a collision and subduction area and has a complex tectonic history. To better under- Received 19 October 2015 stand the complicated structure beneath Taiwan, gravity studies, in addition to seismic and geological Received in revised form 17 April 2016 studies, provide useful geophysical information for studying shallow depths. Previous gravity studies Accepted 4 May 2016 of Taiwan in the last 30 years focused on local regionalized explanations and 2-D profile modeling. Available online 6 May 2016 This study is the first to complete a 3-D gravity inversion of Taiwan, and it provides a more comprehen- sive and large-scale tectonic analysis. Keywords: Following 3-D gravity inversion using the least squares method, we sliced horizontal and vertical pro- 3-D gravity inversion files from the 3-D density model to visualize tectonic changes. The low Bouguer anomaly was caused by Density structure Taiwan thick sediment and crust layers. The high-density layers are located in special tectonic areas such as the TAIGER Peikang and Kuanying basement highs. The deepest Moho depth beneath the middle of the Central Range is 45–50 km.