Giving Full Play to Geothermal in Renewable Energy Development in Tibet, China
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Microgeneration Potential in New Zealand
Prepared for Parliamentary Commissioner for the Environment Microgeneration Potential in New Zealand A Study of Small-scale Energy Generation Potential by East Harbour Management Services ISBN: 1-877274-33-X May 2006 Microgeneration Potential in New Zealand East Harbour Executive summary The study of the New Zealand’s potential for micro electricity generation technologies (defined as local generation for local use) in the period up to 2035 shows that a total of approximately 580GWh per annum is possible within current Government policies. If electricity demand modifiers (solar water heating, passive solar design, and energy efficiency) are included, there is approximately an additional 15,800GWh per annum available. In total, around 16,400GWh of electricity can be either generated on-site, or avoided by adopting microgeneration of energy services. The study has considered every technology that the authors are aware of. However, sifting the technologies reduced the list to those most likely to be adopted to a measurable scale during the period of the study. The definition of micro electricity generation technologies includes • those that generate electricity to meet local on-site energy services, and • those that convert energy resources directly into local energy services, such as the supply of hot water or space heating, without the intermediate need for electricity. The study has considered the potential uptake of each technology within each of the periods to 2010, 2020, and 2035. It also covers residential energy services and those services for small- to medium-sized enterprises (SMEs) that can be obtained by on-site generation of electricity or substitution of electricity. -
Sendtnera 7: 163-201
© Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.biologiezentrum.at 163 Contributions to the knowledge of the genus Astragalus L. (Leguminosae) VII-X' D. PODLECH Abstract: PODLECH, D.: Contributions to the knowledge of the genus Astragalus L. (Legumi- nosae) VII-X. - Sendtnera 7: 163-201. 2001. ISSN 0944-0178. VII. A survey of Astragalus L. sect. Leucocercis. The section, endemic in Iran with six species, is revised. Synonymy, descriptions, the investigated specimens and a key for the species are given. VIII. New typifications and changes of typification in Astragalus-s^QcxQS. 12 wrongly typified species are re-typified. 19 taxa are typified here. IX. Some new species in genus Astragalus: 27 new species, one subspecies and one section are described here. They belong to the following sections: Sect. Caprini: A. behbehanensis, A. bozakmanii, A. spitzenbergeri. Sect. Cenantrum: A. tecti-mundi subsp. orientalis. Sect. Chlorostachys: A. poluninii, A. rhododendrophila. Sect. Cystium: A. owirensis. Sect. Dissitiflori: A. argentocalyx, A. bingoellensis, A. doabensis, A. fruticulosus, A. lanzhouensis, A. montis-karkasii, A. pravitzii, A. recurvatus, A. saadatabadensis, A. sata-kandaoensis , A. wakha- nicus. Sect. Hemiphaca: A. sherriffii, A. tsangpoensis. Sect. Incani: A. olurensis, A. zaraensis. Sect. Komaroviella: A. damxungensis. Sect. Onobrychoidei: A. ras- montii. Sect. Polycladus: A. austrotibetanus, A. cobresiiphila, A. conaensis. Sect. Pseudotapinodes, sect, nov.: A. dickorei. X. New names and combinations are given. Four illegitimate names are changed, two taxa have been raised in rank. Zusammenfassung: VII. A survey of Astragalus L. sect. Leucocercis. Eine Revision von Astragalus L. sect. Leucocercis wird vorgestellt. Die Sektion ist endemisch im Iran und umfasst sechs Arten. -
Origin and Character of Loesslike Silt in the Southern Qinghai-Xizang (Tibet) Plateau, China
Origin and Character of Loesslike Silt in the Southern Qinghai-Xizang (Tibet) Plateau, China U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1549 Cover. View south-southeast across Lhasa He (Lhasa River) flood plain from roof of Potala Pal ace, Lhasa, Xizang Autonomous Region, China. The Potala (see frontispiece), characteristic sym bol of Tibet, nses 308 m above the valley floor on a bedrock hill and provides an excellent view of Mt. Guokalariju, 5,603 m elevation, and adjacent mountains 15 km to the southeast These mountains of flysch-like Triassic clastic and volcanic rocks and some Mesozoic granite character ize the southernmost part of Northern Xizang Structural Region (Gangdese-Nyainqentanglha Tec tonic Zone), which lies just north of the Yarlung Zangbo east-west tectonic suture 50 km to the south (see figs. 2, 3). Mountains are part of the Gangdese Island Arc at south margin of Lhasa continental block. Light-tan areas on flanks of mountains adjacent to almost vegetation-free flood plain are modern and ancient climbing sand dunes that exhibit evidence of strong winds. From flood plain of Lhasa He, and from flood plain of much larger Yarlung Zangbo to the south (see figs. 2, 3, 13), large dust storms and sand storms originate today and are common in capitol city of Lhasa. Blowing silt from larger braided flood plains in Pleistocene time was source of much loesslike silt described in this report. Photograph PK 23,763 by Troy L. P6w6, June 4, 1980. ORIGIN AND CHARACTER OF LOESSLIKE SILT IN THE SOUTHERN QINGHAI-XIZANG (TIBET) PLATEAU, CHINA Frontispiece. -
The Lhasa Jokhang – Is the World's Oldest Timber Frame Building in Tibet? André Alexander*
The Lhasa Jokhang – is the world's oldest timber frame building in Tibet? * André Alexander Abstract In questo articolo sono presentati i risultati di un’indagine condotta sul più antico tempio buddista del Tibet, il Lhasa Jokhang, fondato nel 639 (circa). L’edificio, nonostante l’iscrizione nella World Heritage List dell’UNESCO, ha subito diversi abusi a causa dei rifacimenti urbanistici degli ultimi anni. The Buddhist temple known to the Tibetans today as Lhasa Tsuklakhang, to the Chinese as Dajiao-si and to the English-speaking world as the Lhasa Jokhang, represents a key element in Tibetan history. Its foundation falls in the dynamic period of the first half of the seventh century AD that saw the consolidation of the Tibetan empire and the earliest documented formation of Tibetan culture and society, as expressed through the introduction of Buddhism, the creation of written script based on Indian scripts and the establishment of a law code. In the Tibetan cultural and religious tradition, the Jokhang temple's importance has been continuously celebrated soon after its foundation. The temple also gave name and raison d'etre to the city of Lhasa (“place of the Gods") The paper attempts to show that the seventh century core of the Lhasa Jokhang has survived virtually unaltered for 13 centuries. Furthermore, this core building assumes highly significant importance for the fact that it represents authentic pan-Indian temple construction technologies that have survived in Indian cultural regions only as archaeological remains or rock-carved copies. 1. Introduction – context of the archaeological research The research presented in this paper has been made possible under a cooperation between the Lhasa City Cultural Relics Bureau and the German NGO, Tibet Heritage Fund (THF). -
Geothermal Energy
Geothermal energy Adele Manzella CNR - Institute of Geosciences and Earth Resources Via Moruzzi 1 – 56124 PISA, Italy [email protected] Geothermal Energy Pros Cons Research What is How is used frontiers Status and perspectives What is the source of geothermal energy? What part is used? What is Geothermal Energy IGG – Institute of Geosciences and Earth Resources National Research Council of Italy WHAT is Geothermal energy Geothermal Energy The basis of geothermal energy is the From Greek gêo (earth) e immense heat content of the earth’s thermòs (heat) interior: the Earth is slowly cooling down. Since billions of years the heat in the Earth Crust is constantly supplied by Heat inside the Earth the decay of natural radioactive isotopes or the cooling of hot, shallow magmatic ~ 30 °C/km bodies. > 1000 °C > 3000 °C The resource is vast and ubiquitous and > 5000 °C has a corresponding large potential for utilization. WHAT is Geothermal energy Temperature in the ground has a daily (few cm) and seasonal (few meters) fluctuations, becoming essentially constant and equal to the average air temperature at about 18-20 m depth. Below this depth, it essentially increases with depth (geothermal gradient). Shallow geothermal: exploits the underground constant T= average air T The resource is vast and ubiquitous and has a corresponding large potential for Deep geothermal: exploits the utilization. underground heat at T>> air T WHAT is Geothermal energy The temperature increase with depth, as well as volcanoes, geysers, hot springs etc., are in a sense the visible or tangible expression of the heat in the interior of the Earth, but this heat also engenders other phenomena that are less discernable by man, but of such magnitude that the Earth has been compared to an immense "thermal engine”. -
China and Tibet—Two Lands of Stunning Beauty and Centuries-Old Civilizations Steeped in Legend and Tradition
DYNASTIES OF CHINA AND T IBET TTHEHE HHIMALAYASIMALAYAS ANDAND TTHEHE YYANGTZEANGTZE May 26 to June 9, 2018 Dear Members and Friends: I invite you to join The Field Museum on a journey through China and Tibet—two lands of stunning beauty and centuries-old civilizations steeped in legend and tradition. Travel with the Museum’s preeminent experts—Gary M. Feinman, MacArthur Curator of Mesoamerican, Central American, and East Asian Anthropology, and Linda Nicholas, Adjunct Curator of Anthropology—who bring in-depth knowledge and understanding of these ancient cultures. This exceptional journey encompasses the breadth of China—from the Himalayan “Rooftop of the World,” with three nights in Tibet’s seldom-visited city of Lhasa, through the dramatic gorges of the Yangtze River to the historic neighborhoods of Old Shanghai. You will experience the imperial formality of Mandarin Beijing, the dynastic treasures of historic Xi’an and the Tibetan Buddhist “Sun City” of Lhasa with its architectural masterpiece, the Potala Palace—a symbol of peace and the historic home of the Dalai Lama. Our three-night cruise travels the fabled Yangtze River from Chongqing to Yichang through captivating landscapes, historic port cities and resplendent gorges aboard the deluxe VICTORIA JENNA, relaunched in 2016 after an extensive refurbishment. Cruise the magnifi cent Three Gorges, visit the extraordinary engineering marvel of the Three Gorges Dam, and enjoy a private boat tour on the spectacular Goddess Stream in the Wu Gorge. Your land accommodations include fi ve-star hotels such as Shanghai’s legendary FAIRMONT PEACE and the renowned PENINSULA BEIJING. Visit eight UNESCO World Heritage sites during specially arranged, included excursions accompanied by experienced, English-speaking guides. -
17-Point Agreement of 1951 by Song Liming
FACTS ABOUT THE 17-POINT “Agreement’’ Between Tibet and China Dharamsala, 22 May 22 DIIR PUBLICATIONS The signed articles in this publication do not necessarily reflect the views of the Central Tibetan Administration. This report is compiled and published by the Department of Information and International Relations, Central Tibetan Administration, Gangchen Kyishong, Dharamsala 176 215, H. P., INDIA Email: [email protected] Website: www.tibet.net and ww.tibet.com CONTENTS Part One—Historical Facts 17-point “Agreement”: The full story as revealed by the Tibetans and Chinese who were involved Part Two—Scholars’ Viewpoint Reflections on the 17-point Agreement of 1951 by Song Liming The “17-point Agreement”: Context and Consequences by Claude Arpi The Relevance of the 17-point Agreement Today by Michael van Walt van Praag Tibetan Tragedy Began with a Farce by Cao Changqing Appendix The Text of the 17-point Agreement along with the reproduction of the original Tibetan document as released by the Chinese government His Holiness the Dalai Lama’s Press Statements on the “Agreement” FORWARD 23 May 2001 marks the 50th anniversary of the signing of the 17-point Agreement between Tibet and China. This controversial document, forced upon an unwilling but helpless Tibetan government, compelled Tibet to co-exist with a resurgent communist China. The People’s Republic of China will once again flaunt this dubious legal instrument, the only one China signed with a “minority” people, to continue to legitimise its claim on the vast, resource-rich Tibetan tableland. China will use the anniversary to showcase its achievements in Tibet to justify its continued occupation of the Tibetan Plateau. -
An Annotated List of Birds Wintering in the Lhasa River Watershed and Yamzho Yumco, Tibet Autonomous Region, China
FORKTAIL 23 (2007): 1–11 An annotated list of birds wintering in the Lhasa river watershed and Yamzho Yumco, Tibet Autonomous Region, China AARON LANG, MARY ANNE BISHOP and ALEC LE SUEUR The occurrence and distribution of birds in the Lhasa river watershed of Tibet Autonomous Region, People’s Republic of China, is not well documented. Here we report on recent observations of birds made during the winter season (November–March). Combining these observations with earlier records shows that at least 115 species occur in the Lhasa river watershed and adjacent Yamzho Yumco lake during the winter. Of these, at least 88 species appear to occur regularly and 29 species are represented by only a few observations. We recorded 18 species not previously noted during winter. Three species noted from Lhasa in the 1940s, Northern Shoveler Anas clypeata, Solitary Snipe Gallinago solitaria and Red-rumped Swallow Hirundo daurica, were not observed during our study. Black-necked Crane Grus nigricollis (Vulnerable) and Bar-headed Goose Anser indicus are among the more visible species in the agricultural habitats which dominate the valley floors. There is still a great deal to be learned about the winter birds of the region, as evidenced by the number of apparently new records from the last 15 years. INTRODUCTION limited from the late 1940s to the early 1980s. By the late 1980s the first joint ventures with foreign companies were The Lhasa river watershed in Tibet Autonomous Region, initiated and some of the first foreign non-governmental People’s Republic of China, is an important wintering organisations were allowed into Tibet, enabling our own area for a number of migratory and resident bird species. -
Comments to the Author This Paper Quantifies Streamflow and Groundwater Changes Due to Climate Change in an Alpine Region with a Large Glacier
Response to D. Van Hoy (SC1) Comments to the Author This paper quantifies streamflow and groundwater changes due to climate change in an alpine region with a large glacier. This type of work is very important and is likely applicable to other mountainous areas (e.g. the Rocky Mountains in North America and the Andes in South America). Overall the methods of this paper are relatively easy to understand. There is a good use of appropriate references throughout the paper including relevant papers at nearby study sites on the Tibetan Plateau. I think the paper is worthy of being published, however there are some issues with grammar and sections where the paper could stand to be reworded to increase readability and be more concise. The paper is also lacking in regards to the site description, explanation of methods, and analysis. For more details, see the comments and questions below. Response: Many thanks for the positive reviews that we received with respect to our paper hess-2018-541 entitled “Quantifying streamflow and active groundwater storage in response to climate warming in an alpine catchment on the Tibetan Plateau”. Those comments are all valuable and very helpful for revising and improving our paper. We have addressed the reviewers’ concerns and suggestions carefully. The major revisions include the clarification of the purpose of the paper, the validity of recession flow analysis, the improvement of the writing, and the thoroughly revision of the Figures. The concept of the active groundwater storage were defined. We descripted the vegetation (Figure S2) and the rock/soil types throughout the catchment (Figure S5). -
Escape to Lhasa Strategic Partner
4 Nights Incentive Programme Escape to Lhasa Strategic Partner Country Name Lhasa, the heart and soul of Tibet, is a city of wonders. The visits to different sites in Lhasa would be an overwhelming experience. Potala Palace has been the focus of the travelers for centuries. It is the cardinal landmark and a structure of massive proportion. Similarly, Norbulingka is the summer palace of His Holiness Dalai Lama. Drepung Monastery is one of the world’s largest and most intact monasteries, Jokhang temple the heart of Tibet and Barkhor Market is the place to get the necessary resources for locals as well as souvenirs for tourists. At the end of this trip we visit the Samye Monastery, a place without which no journey to Tibet is complete. StrategicCountryPartner Name Day 1 Arrive in Lhasa Country Name Day 1 o Morning After a warm welcome at Gonggar Airport (3570m) in Lhasa, transfer to the hotel. Distance (Airport to Lhasa): 62kms/ 32 miles Drive Time: 1 hour approx. Altitude: 3,490 m/ 11,450 ft. o Leisure for acclimatization Lhasa is a city of wonders that contains many culturally significant Tibetan Buddhist religious sites and lies in a valley next to the Lhasa River. StrategicCountryPartner Name Day 2 In Lhasa Country Name Day 2 o Morning: Set out to visit Sera and Drepung Monasteries Founded in 1419, Sera Monastery is one of the “great three” Gelukpa university monasteries in Tibet. 5km north of Lhasa, the Sera Monastery’s setting is one of the prettiest in Lhasa. The Drepung Monastery houses many cultural relics, making it more beautiful and giving it more historical significance. -
Geothermal Gradient Calculation Method: a Case Study of Hoffell Low- Temperature Field, Se-Iceland
International Research Journal of Geology and Mining (IRJGM) (2276-6618) Vol. 4(6) pp. 163-175, September, 2014 DOI: http:/dx.doi.org/10.14303/irjgm.2014.026 Available online http://www.interesjournals.org/irjgm Copyright©2014 International Research Journals Full Length Research Paper Geothermal Gradient Calculation Method: A Case Study of Hoffell Low- Temperature Field, Se-Iceland Mohammed Masum Geological Survey of Bangladesh, 153, Pioneer Road, Segunbagicha, Dhaka-1000, BANGLADESH E-mail: [email protected] ABSTRACT The study area is a part of the Geitafell central volcano in southeast Iceland. This area has been studied extensively for the exploration of geothermal resources, in particular low-temperature, as well as for research purposes. During the geothermal exploration, geological maps should emphasize on young corresponding rocks that could be act as heat sources at depth. The distribution and nature of fractures, faults as well as the distribution and nature of hydrothermal alteration also have to known. This report describes the results of a gradient calculation method which applied to low-temperature geothermal field in SE Iceland. The aim of the study was to familiarize the author with geothermal gradient mapping, low-temperature geothermal manifestations, as well as studying the site selection for production/exploration well drilling. Another goal of this study was to make geothermal maps of a volcanic field and to analyse if some relationship could be established between the tectonic settings and the geothermal alteration of the study area. The geothermal model of the drilled area is consistent with the existence of a structurally controlled low-temperature geothermal reservoir at various depths ranging from 50 to 600 m. -
2008 UPRISING in TIBET: CHRONOLOGY and ANALYSIS © 2008, Department of Information and International Relations, CTA First Edition, 1000 Copies ISBN: 978-93-80091-15-0
2008 UPRISING IN TIBET CHRONOLOGY AND ANALYSIS CONTENTS (Full contents here) Foreword List of Abbreviations 2008 Tibet Uprising: A Chronology 2008 Tibet Uprising: An Analysis Introduction Facts and Figures State Response to the Protests Reaction of the International Community Reaction of the Chinese People Causes Behind 2008 Tibet Uprising: Flawed Tibet Policies? Political and Cultural Protests in Tibet: 1950-1996 Conclusion Appendices Maps Glossary of Counties in Tibet 2008 UPRISING IN TIBET CHRONOLOGY AND ANALYSIS UN, EU & Human Rights Desk Department of Information and International Relations Central Tibetan Administration Dharamsala - 176215, HP, INDIA 2010 2008 UPRISING IN TIBET: CHRONOLOGY AND ANALYSIS © 2008, Department of Information and International Relations, CTA First Edition, 1000 copies ISBN: 978-93-80091-15-0 Acknowledgements: Norzin Dolma Editorial Consultants Jane Perkins (Chronology section) JoAnn Dionne (Analysis section) Other Contributions (Chronology section) Gabrielle Lafitte, Rebecca Nowark, Kunsang Dorje, Tsomo, Dhela, Pela, Freeman, Josh, Jean Cover photo courtesy Agence France-Presse (AFP) Published by: UN, EU & Human Rights Desk Department of Information and International Relations (DIIR) Central Tibetan Administration (CTA) Gangchen Kyishong Dharamsala - 176215, HP, INDIA Phone: +91-1892-222457,222510 Fax: +91-1892-224957 Email: [email protected] Website: www.tibet.net; www.tibet.com Printed at: Narthang Press DIIR, CTA Gangchen Kyishong Dharamsala - 176215, HP, INDIA ... for those who lost their lives, for