Impact of Land Uses on Heavy Metal Distribution in the Selenga River System in Mongolia
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
List of Rivers of Mongolia
Sl. No River Name Russian Name Draining Into 1 Yenisei River Russia Arctic Ocean 2 Angara River Russia, flowing out of Lake Baikal Arctic Ocean 3 Selenge River Сэлэнгэ мөрөн in Sükhbaatar, flowing into Lake Baikal Arctic Ocean 4 Chikoy River Arctic Ocean 5 Menza River Arctic Ocean 6 Katantsa River Arctic Ocean 7 Dzhida River Russia Arctic Ocean 8 Zelter River Зэлтэрийн гол, Bulgan/Selenge/Russia Arctic Ocean 9 Orkhon River Орхон гол, Arkhangai/Övörkhangai/Bulgan/Selenge Arctic Ocean 10 Tuul River Туул гол, Khentii/Töv/Bulgan/Selenge Arctic Ocean 11 Tamir River Тамир гол, Arkhangai Arctic Ocean 12 Kharaa River Хараа гол, Töv/Selenge/Darkhan-Uul Arctic Ocean 13 Eg River Эгийн гол, Khövsgöl/Bulgan Arctic Ocean 14 Üür River Үүрийн гол, Khövsgöl Arctic Ocean 15 Uilgan River Уйлган гол, Khövsgöl Arctic Ocean 16 Arigiin River Аригийн гол, Khövsgöl Arctic Ocean 17 Tarvagatai River Тарвагтай гол, Bulgan Arctic Ocean 18 Khanui River Хануй гол, Arkhangai/Bulgan Arctic Ocean 19 Ider River Идэр гол, Khövsgöl Arctic Ocean 20 Chuluut River Чулуут гол, Arkhangai/Khövsgöl Arctic Ocean 21 Suman River Суман гол, Arkhangai Arctic Ocean 22 Delgermörön Дэлгэрмөрөн, Khövsgöl Arctic Ocean 23 Beltes River Бэлтэсийн Гол, Khövsgöl Arctic Ocean 24 Bügsiin River Бүгсийн Гол, Khövsgöl Arctic Ocean 25 Lesser Yenisei Russia Arctic Ocean 26 Kyzyl-Khem Кызыл-Хем Arctic Ocean 27 Büsein River Arctic Ocean 28 Shishged River Шишгэд гол, Khövsgöl Arctic Ocean 29 Sharga River Шарга гол, Khövsgöl Arctic Ocean 30 Tengis River Тэнгис гол, Khövsgöl Arctic Ocean 31 Amur River Russia/China -
Part I Master Plan
PART I MASTER PLAN CHAPTER 1 INTRODUCTION I MASTER PLAN PART I MASTER PLAN CHAPTER 1 INTRODUCTION 1.1 Background of the Study In Mongolia some 50% of the total population of about 2.4 million are nomadic families. For the nomadic families Sum centers are key places for supplying their vital goods, and also for receiving public services such as administration, medical care, education, etc. As of November 1997, the electric power at 117 out of 314 Sum centers in total in Mongolia is being supplied from the national power transmission network. At the remaining 197 Sum centers, the electric power is supplied by the diesel engine generators by Sum center independently. Most of these diesels generating facilities were manufactured during the former Soviet Union era and installed long ago from 1963 to 1990. During the Social Republic era of the country, Mongolia depended on the Soviet Union for the supply of spare parts necessary for maintenance of the generating equipment and technical guidance. Due to the corruption of the Soviet Union's economy in 1991 and associated transition to a market economy, the following four factors caused troubles to the operation and maintenance of the Sum's generating facilities, i.e. (1) the lack of business operating senses, (2) the interruption of spare parts supply, (3) the lack of technical capability and (4) shortage of management budget. The operation of much equipment has been obliged to be kept stopped after failure, as operators cannot repair them. The affected generation quantity, and aggravated the conditions of daily lives of people in Sum center and caused serious effects to the socio-economic activities of the Sum centers. -
2 Interaction Between Groundwater of Shallow Aquifers and Surface Water in Russian Territory of the Baikal Basin
GEF - UNDP - UNOPS Project Integrated Natural Resources Management in the Baikal Basin Transboundary Ecosystem Groundwater Resources in Shallow Transboundary Aquifers in the Baikal Basin: Current Knowledge, Protection and Management A Contribution to the Transboundary Diagnostic Analysis of the Lake Baikal Basin Photo by V.Urbazaev September 2013 UNESCO-IHP This report has been prepared by Dr Jaroslav Vrba, UNESCO-IHP Senior Consultant and Scientific-Technical Coordinator of the Project, in collaboration with the following national experts from Mongolia and the Russian Federation: Dr Borchuluun Urtnasan, Freelance Consultant, Ulaanbataar, Mongolia Dr Buyankhishig Nemer, Associate Professor, Mongolian University of Science and Technology, Ulaanbataar, Mongolia Dr Alexey Maksimovich Plyusnin, Deputy Director for Science of Geological Institute of Siberian Branch of Russian Academy of Science, Chief of Laboratory of Hydrogeology and Geoecology. Ulan-Ude, Russian Federation Dr Marina Aleksandrovna Tugarina, Associate Professor, Irkutsk State Technical University, Department of Applied Geology. Irkutsk, Russian Federation. Acknowledgements The project team wishes to express their gratitude to the following individuals who have actively supported in the activities carried out in the framework of the UNESCO-led groundwater resources activities and contributed to the preparation of this report: Dr Sergey V. Kudelya, Project Manager, Integrated Natural Resources Management in the Baikal Basin Transboundary Ecosystem Mr Boris V. Baduyev, Lake Baikal Project Coordination Unit in Ulan-Ude Dr Munkhbat Tserendorj and Dr Tumurchudur Sodnom, National Project Technical Director for Mongolia Dr Alexander A. Shekhovtsov, National Technical Project Director for the Russian Federation Prof. Alexander I. Smirnov, UNESCO Chair on Water Resources and Rector of Irkutsk State University, Russian Federation Dr Lunten Janchivdorj, UNESCO Chair on Sustainable Groundwater Management, Institute of Geoecology, Mongolian Academy of Sciences, Ulaanbaatar, Mongolia Dr Larisa D. -
Relict Topography Within the Hangay Mountains in Central Mongolia: 2 Quantifying Long-Term Exhumation and Relief Change in an Old Landscape 3 4 Kalin T
1 Relict topography within the Hangay Mountains in central Mongolia: 2 Quantifying long-term exhumation and relief change in an old landscape 3 4 Kalin T. McDannella,b*, Peter K. Zeitlera, and Bruce D. Idlemana 5 6 aDepartment of Earth & Environmental Sciences, Lehigh University, 1 W Packer Ave., Bethlehem, PA 18015, USA 7 8 bNatural Resources Canada, Geological Survey of Canada, 3303 33 St NW, Calgary, AB T2L 2A7 9 10 Corresponding author: [email protected] 11 12 Key Points 13 ° New bedrock and detrital apatite (U-Th)/He cooling ages were determined for the Hangay 14 Mountains and central Mongolia 15 ° Thermo-kinematic modeling suggests relief change in the Mesozoic with slow exhumation 16 rates on the order of <20 m/My since the Cretaceous 17 ° Coupled Pecube-Neighborhood Algorithm modeling is successfully applied in a slowly 18 eroding setting 19 20 Abstract 21 The Hangay Mountains are a high-elevation, low-relief landscape within the greater Mongolian 22 Plateau of central Asia. New bedrock apatite (U-Th)/He single-grain ages from the Hangay span 23 ~70 to 200 Ma, with a mean of 122.7 ± 24.0 Ma (2σ). Detrital apatite samples from the Selenga 24 and Orkhon Rivers, north of the mountains, yield dominant (U-Th)/He age populations of ~115 25 to 130 Ma, as well as an older population not seen in the Hangay granitic bedrock data. These 26 low-temperature data record regional exhumation of central Mongolia in the Mesozoic followed 27 by limited erosion of <1-2 km since the Cretaceous, ruling out rapid exhumation of this 28 magnitude associated with any late Cenozoic uplift. -
Irrigation Feasibility Study Report
Vegetable Production and Irrigated Agriculture Project (RRP MON 51423-002) Irrigation Feasibility Study Report Project Number: 51423-002 February 2020 Proposed Loans and Administration of Grant Mongolia: Vegetable Production and Irrigated Agriculture Project i Table of Contents I. PROJECT CONTEXT AND RATIONALE 1 A. Need for investment 1 B. Objective 2 C. Subproject Selection 2 II. IRRIGATION SUBPROJECT DESIGN 6 A. General Design Principles 6 B. Subproject 1 – Tsakhir Irrigation and Drainage System Design 36 C. Subproject 2 – Yolton Irrigation and Drainage System Design 58 D. Subproject 3 - Erdeneburen Irrigation and Drainage System Design 84 E. Subproject 4 – Boomiin Am Irrigation and Drainage System Design 111 F. Subproject 5 – Khoid Gol Design of Irrigation and Drainage System 128 G. Subproject 6 – Tsul-Ulaan Irrigation and Drainage System Design 157 H. Subproject 7 – Ulaandel Irrigation and Drainage System Design 181 I. Subproject 9 – Khuren Tal Irrigation and Drainage System Design 203 J. Subproject 10 – Nogoon Khashaa Irrigation and Drainage System Design 224 K. Subproject 12 – Iven Gol Irrigation and Drainage System Design 245 L. Subproject 13 – Okhindiin Tal Irrigation and Drainage System Design 268 M. Subproject 14 – Sugnugur Irrigation and Drainage System Design 284 N. Subproject 16 – Dulaanii Tal Irrigation and Drainage System Design 307 III. TOTAL INVESTMENT AND FINANCIAL PLAN 327 IV. IMPLEMENTATION AND OPERATING ARRANGEMENTS 328 A. Implementation Schedule 328 B. Operation and Maintenance of Irrigation Systems 328 C. Capacity Building 331 V. PROJECT OUTCOME AND IMPACTS 332 A. Project Monitoring 332 B. Social Impact Assessment 332 C. Environmental Impact Assessment 332 VI. CRITICAL RISKS 333 A. Extreme Climate 333 B. -
ABSTRACT BAYASGALAN, GANTULGA. Late Cenozoic Landscape Evolution in the Khangay Mountains, Mongolia
ABSTRACT BAYASGALAN, GANTULGA. Late Cenozoic Landscape Evolution in the Khangay Mountains, Mongolia. (Under the direction of Dr. Karl W. Wegmann). Timing, rates, and systems responsible for uplift of intracontinental mountain ranges provide insight into the creation of high-elevation regions on Earth that are distant from active plate tectonic margins. The Khangay Mountains in central Mongolia is an intriguing research site that is suitable for investigating the timing of geologic processes responsible for topographic uplift and the development of continental scale drainage patterns, as well as the climatic-geomorphic responses to such. This dissertation focuses on defining shallow crustal and surficial processes contributing to the development of the Khangay Mountains at both short and long topographic wavelengths, as well as the topographic evolution of the range. The first chapter of this dissertation focuses on cross-strike drainage development via the formation and capture of small tectonic basins (lakes) in front of an active thrust known as the Bayankhongor fault along the southern flank of the Khangay Mountains. The field research site contains ample geomorphological features that I will use to reconstruct the interplay between surface uplift by faulting, temporary formation of lakes in footwall basins and fluvial incision. Although ultimately these landforms (e.g. water gaps) reflect the defeat of rivers during sustained rock uplift, the role of climate oscillations in their formation is an underexplored topic. I used a coupled tectonics–landscape evolution-climate change model to test the hypothesis that a ~130 km2 late Quaternary lake in the Galuut Valley along the southern flank of the Khangay Mountains drained, perhaps catastrophically. -
Journal Biology 2004 1
Mongolian Journal of Biological Sciences 2003 Vol. 1(2): 59-72 Summer birds in Arkhangai province, Mongolia, July-August 2002. Anthony S. Cheke 139 Hurst Street, Oxford OX4 1HE, UK; [email protected] Abstract A list of breeding birds for Tsetserleg and its surroundings is given for the first time, and additions are noted for the Khorgo-Terkhiin Tsagaan Nuur National Park The presence of Eurasian Griffons and Lammergeiers in the Khangai mountains is confirmed, and Black-headed Gulls suspected of breeding near Tsagaan Nuur, a new locality. An apparent marked increase in breeding/summering numbers of Tufted Duck and Velvet Scoter and a possible range expansion of Daurian Redstarts was noted. Mass mortality was observed in House Sparrows from eating moths. Key words: breeding checklist, Gypsy Moth, sparrow, Tsetserleg, Khorgo, Terkhiin-Tsagaan-Nuur Introduction (=Karakorum), Sansar (=Rashaant), Erdenesant and Lün; the more direct northern route via Ogii Mainly through the effort of East German Nuur, an interesting lake, is no longer in regular expeditions in the 1970s and 1980s, and the activity use. Names are spelt here in the current of Mongolian ornithologists in the last decade, the transliteration system recognised for Mongolian overall composition of the Mongolian avifauna is Cyrillic script (Mayhew 2001); the German well-known - but not many sites are well literature uses different spellings - e.g. Zezerleg/ documented. The country is large (1,566,500km²) Cecerleg for Tsetserleg. and sparsely populated (2.65m; 1.69/km²), but has Tsetserleg was visited by German expeditions large numbers of domestic animals (c70m, only en route to other places, and their visits to the exceeding the carrying capacity, Avaadorj & lake Terkhiin Tsagaan Nuur (Mey 1994, Stephan Badrakh 2001); the principal way of life outside 1988) were brief and confined to the eastern end the capital is nomadic herding. -
Study on the Distribution and Habitat Characteristicsof Brandt’S Vole
88 Enkhbold N, Dazhao Shi, Mongolian Journal of Agricultural Sciences №13 (02), 2014:88-95 STUDY ON THE DISTRIBUTION AND HABITAT CHARACTERISTICSOF BRANDT’S VOLE Enkhbold.N1, DazhaoShi2 ,Batsaikhan. N1 , Deng Wang2 ,Tseveendorj.D1, Erdenetuya.B1 1-Plant Protection Research Institute 2-College of Agronomy and Biotechnology, China Agricultural University E-mail: [email protected] ABSTRACT Many species have suffered changed habitable area due to recent climate change or/and human activities. Brandt’s vole (Lasiopodomysbrandtii) is same as it.The species is undergoing a continuous habitat change as a consequence of the human’s production, climate change and retrogressive succession of grassland ecosystems. The distribution of the Brandt’s vole was update in China and Mongolia.Based on the historical distribution map, which was made by overlaying the historical data with vegetation type’s map of the grassland resources in China and Mongolia. And the distribution map was modified according to the on-site investigate data in recent years. The current species’ distribution was range Hulunbei’er, northern Xilinguole, which comprise a landscape through the east of DornodAimag, Mongolia, and southern Hunshandake Sandy Land in China which just includes the areas around the Zhengxiangbai Qi. There were no the species in the east of Daxinganling Mountains, Liaoning, Shanxi province and Xinjiang Uyghur Autonomous Region of China. The species’ distribution is discontinuous in Mongolia, including western, middle and eastern Mongolia. The western distribution along Hangay Mountains and extends for the west, the northern boundary extended to between Ider river and Chulouk river. Southward reaches of the Malhin along the plain between Hangay Mountain and Altay Mountain. -
The Harmonized Water Quality Monitoring Program in the Selenga River Basin
Preparers: Federal State Budgetary Institution “Hydrochemical Institute” (FSBI “HI”) and Federal State Budgetary Institution “Buryat Center of Hydrometeorology and Monitoring of Environment” THE HARMONIZED WATER QUALITY MONITORING PROGRAM IN THE SELENGA RIVER BASIN Preparers: Mongolian Institute of Meteorology and Hydrology; Central Laboratory of Environment of Mongolia GEF: “The GEF unites 182 countries in partnership with international institutions, non-governmental organizations (NGOs), and the private sector to address global environmental issues while supporting national sustainable development initiatives. Today the GEF is the largest public funder of projects to improve the global environment. An independently operating financial organization, the GEF provides grants for projects related to biodiversity, climate change, international waters, land degradation, the ozone layer, and persistent organic pollutants. Since 1991, GEF has achieved a strong track record with developing countries and countries with economies in transition, providing $9.2 billion in grants and leveraging $40 billion in co-financing for over 2,700 projects in over 168 countries. www.thegef.org” UNDP: “UNDP partners with people at all levels of society to help build nations that can withstand crisis, and drive and sustain the kind of growth that improves the quality of life for everyone. On the ground in 177 countries and territories, we offer global perspective and local insight to help empower lives and build resilient nations. www.undp.org” UNOPS: is an operational arm of the United Nations, helping a range of partners implement $1 billion worth of aid and development projects every year. UNOPS mission is to expand the capacity of the UN system and its partners to implement peacebuilding, humanitarian and development operations that matter for people in need. -
Water and Environment in the Selenga- Baikal Basin
Daniel Karthe, Sergey Chalov , Nikolay Kasimov, Martin Kappas (eds.) Water and Environment in the Selenga- Baikal Basin: International Research Cooperation for an Ecoregion of Global Relevance ERDSICHT - EINBLICKE IN GEOGRAPHISCHE UND GEOINFORMATIONSTECHNISCHE ARBEITSWEISEN Schriftenreihe des Geographischen Instituts der Universität Göttingen, Abteilung Kartographie, GIS und Fernerkundung Herausgegeben von Prof. Dr. Martin Kappas ISSN 1614-4716 16 Pavel Propastin Remote sensing based study on vegetation dynamics in dry lands of Kazakhstan ISBN 978-3-89821-823-8 17 Matthias Stähle Trinkwasser in Delhi Versorgungsproblematik einer indischen Megastadt ISBN 978-3-89821-827-6 18 Roland Bauböck Bioenergie im Landkreis Göttingen GIS-gestützte Biomassepotentialabschätzung anhand ausgewählter Kulturen, Triticale und Mais ISBN 978-3-89821-959-4 19 Wahib Sahwan Geomorphologische Untersuchungen mittels GIS- und Fernerkundungsverfahren unter Berücksichtigung hydrogeologischer Fragestellungen Fallbeispiele aus Nordwest Syrien ISBN 978-3-8382-0094-1 20 Julia Krimkowski Das Vordringen der Malaria nach Mitteleuropa im Zuge der Klimaerwärmung Fallbeispiel Deutschland ISBN 978-3-8382-0312-6 21 Julia Kubanek Comparison of GIS-based and High Resolution Satellite Imagery Population Modeling A Case Study for Istanbul ISBN 978-3-8382-0306-5 22 Christine von Buttlar, Marianne Karpenstein-Machan, Roland Bauböck Anbaukonzepte für Energiepflanzen in Zeiten des Klimawandels Beitrag zum Klimafolgenmanagement in der Metropolregion Hannover-Braunschweig-Göttingen-Wolfsburg ISBN 978-3-8382-0525-0 Daniel Karthe, Sergey Chalov , Nikolay Kasimov, Martin Kappas (eds.) WATER AND ENVIRONMENT IN THE SELENGA-BAIKAL BASIN: INTERNATIONAL RESEARCH COOPERATION FOR AN ECOREGION OF GLOBAL RELEVANCE ibidem-Verlag Stuttgart Bibliografische Information der Deutschen Nationalbibliothek Die Deutsche Nationalbibliothek verzeichnet diese Publikation in der Deutschen Nationalbibliografie; detaillierte bibliografische Daten sind im Internet über http://dnb.d-nb.de abrufbar. -
Download the Mongolian Final Report
UNDP-GEF project "Integrated Natural Resource Management in the Baikal Basin Transboundary Ecosystem" Final report Tender: RFQ_EMO_2012-029 “Baikal Information Center (BIC) Conception for Mongolia” Executor: Mongolian Institute of Water Research and Development The intellectual property rights belong to UNOPS and UNDP, the information should not be used by a third party before consulting with the project. UNDP-GEF project "Integrated Natural Resource Management in the Baikal Basin Transboundary Ecosystem" The intellectual property rights belong to UNOPS and UNDP, the information should not be used by a third party before consulting with the project. UNDP-GEF project "Integrated Natural Resource Management in the Baikal Basin Transboundary Ecosystem" Contents INTRODUCTION 4 1. Selenge River Basin 4 1.1. Geography 4 1.2. River network 6 1.3. Land cover 7 1.4. Ecological condition 8 Ecological monitoring 10 1.5. Surface water quality 11 Monitoring network 11 Trends in surface water quality 11 1.6. Groundwater quality 12 Monitoring network 12 Trends in groundwater quality 12 1.7. Climate change 13 1.8. Human activities linked to the ecosystems 13 Domestic uses 13 Agriculture and irrigated areas 14 Pasture 15 Mining 15 Forest management 17 Tourism 19 Fishing 19 Dams and flow regulation 20 1.9. River basin organisations 20 1.10. Legislation 21 1.11. Conduct needs BIC assessment study for Mongolia 22 2. Data structure of BIC for Mongolia 24 2.1. General description 24 2.2. Monitoring Network 25 2.3. Water Quality Data and Their Sources 25 2.4. Ecological Data and Their Sources 26 2.5. -
Pmas Article Ar
Vol. 60 No 01 (233) 2020 PMAS DOI: https://doi.org/10.5564/pmas.v60i1.1333 Proceedings of the Mongolian Academy of Sciences ARTICLE AR Morphology of Khorgo Volcano Crater in the Khangai Mountains in Central Mongolia Altanbold Enkhbold1*, Ulambadrakh Khukhuudei2 Sanchir Dorjgochoo3 and Byambabayar Ganbold1 1 Department of Geography, School of Art & Sciences, National University of Mongolia Ulaanbaatar, Mongolia 2 Department of Geology and Geophysics, School of Arts and Sciences, National University of Mongolia Ulaanbaatar, Mongolia 3Department of Magmatism and Metallogeny, Institute of Geology, Mongolian Academy of Sciences Ulaanbaatar, Mongolia __________________________________________________________________________________________________________ ARTICLE INFO: Received: 31 Jan, 2020; Accepted: 18 May, 2020 __________________________________________________________________________________________________________ Abstract: Cenozoic basalt, which is widespread in Mongolia, has been attracting the attention of Central Asian researchers since the beginning of the last century. This study identified the geomorphological shape of the Khorgo volcano. The main purpose of the study is to determine the origin and morphological form of Khorgo volcano, a key representative of Cenozoic volcanism. In general, there are several types of morphological forms associated with lava overflow, and it is important to determine which types are the most common and also to establish a link between them. Geomorphological studies in this area have not been conducted in Mongolia. Spatial improvement and morphometric methods satellite imagery had identified Khorgo volcanic faults. Khangai magmatism had thinned its crust to 45 km during the Tariat-Chuluut volcanic activity. It can be concluded that this was due to the thinning of the continental crust in the Khangai Mountains because of mantle plume. During this time, tectonic faults formed were formed, which had broken through the earth's crust.