Chemical Water Quality in Selenge River Basin in Mongolia: Spatial-Temporal Patterns and Land Use Influence

Total Page:16

File Type:pdf, Size:1020Kb

Chemical Water Quality in Selenge River Basin in Mongolia: Spatial-Temporal Patterns and Land Use Influence Chemical water quality in Selenge River Basin in Mongolia: spatial-temporal patterns and land use influence DISSERTATION for the award of the degree “Doctor rerum naturalium” (Dr.rer.nat.) of the Georg-August-Universität Göttingen within the doctoral program HIGRADE of the “Helmholtz- Centre for Environmental Research-UFZ” Submitted by Gunsmaa Batbayar (MSc) From Mongolia Göttingen, June 2018 Thesis Committee Prof. Dr. Martin Kappas Department of Cartography, GIS and Remote Sensing, institute of Geography, University of Göttingen Prof. Dr. Daniel Karthe Environmental Engineering Section, German-Mongolian Institute for Resources and Technology (GMIT) Members of the Examination Board Reviewer: Prof. Dr. Martin Kappas, Department of Cartography, GIS and Remote Sensing, Institute of Geography, University of Göttingen Second Reviewer: Prof. Dr. Daniel Karthe Environmental Engineering Section, German-Mongolian Institute for Resources and Technology (GMIT) Further members of the Examination Board PD Dr. Dr. h.c. Martin Pfeiffer, Bayreuth Center of Ecology and Environmental Research BayCEER, University of Bayreuth Prof. Dr. Daniela Sauer, Abteilung Physische Geographie, Georg-August Universität Göttingen Prof. Dr. Hans Ruppert, Georg-August-Universität, Geowissenschaftliches Zentrum, Dept. Sedimentologie/Umweltgeologie Dr. Michael Schlund, Department of Cartography, GIS and Remote Sensing, Institute of Geography, University of Göttingen Date of the oral examination: 09.07.2018 Acknowledgments First of all, I would like to express my sincere thanks to my supervisors PD Dr. Dr. h.c. Martin Pfeiffer, Prof. Dr. Daniel Karthe, Prof. Dr. Martin Kappas, and Prof. Dr. Dietrich Borchardt for offering me this wonderful opportunity to join the UFZ community in Magdeburg and Georg-August University Göttingen in Germany. Thank you for your continuous supervision, support and advice which helped me to successfully complete this research and I would like to say that without your help it was not possible to finalize. I would like to express my special appreciation to my scientific advisor PD Dr. Dr. h.c. Martin Pfeiffer, as my teacher and mentor; you have been tremendous “Bagsh” for me. Your advice on both research as well as on my career have been precious. This research was financially supported by the German Academic Exchange Service (DAAD) Integrated Water Resources scholarship No.A/12/97034, Integrated Water Resource Management (IWRM) in Central Asia: Model Region Mongolia (MoMo) Project in its third phase (2013-2018) which was provided by the German Federal Ministry of Education and Research (BMBF; grant no. 033L003A as well as the Helmholtz Interdisciplinary Graduate School for Environmental Research (HIGRADE).) I would be always appreciate to DAAD particularly Ms.Carolin Wax, for her full support and advice. I would like to express special gratitude to staff members of Department of the Aquatic Ecosystem Analysis and Management (UFZ) and ARSOlux team (UFZ) for their complete support and special thanks goes to the Water Analysis and Chemometrics team of the River Ecology Department (UFZ) for sample analysis. My special gratitude goes to Dr.Wolf von Tümpling for his valuable advice and guidance. The field work in Mongolia was not possible to finalize without help as following Dr.Konrad Siegfried, Prof. Dr. Galbadrakh.R, Dr. Saulyegul.A, Dr. Enkhdol.T, Batchuluun.Ts, Irmuunzaya.Kh, Bolortuya.Kh, Khishigdelger B and Dr.Davaa for their valuable help and support. Thank you from the bottom of my heart to Irmgard Pfeiffer, Saame (Natsagsuren) and Katja Westphal for their endless help support and love which made me feels motivated and inspired. As well as I would like to send my big thanks to my friends and colleagues Oyudari Vova, Eva Hasikova, Valerie Wentzky, Jingshui Huang, Siqing Tao, Shauchien, Pei Ying, Erik Sartory, Munkhdavaa Munkhjargal I really appreciated and enjoyed our dinner nights, hiking days, coffee break and all precious time we shared together. Finally, I would like to express my deepest personal gratitude to my family, especially my parents, Batbayar Dashmagvan and Tuya Otgon and my sister, Densmaa Batbayar for their enduring love, help and support. Each of them has played a big role to stay motivated during my research until completion. 1 Dissertation content This doctoral thesis consists of a general introduction and four papers. The papers will be referred to by their Roman numbers (Papers I-IV). The published papers are reprinted by permission from the respective copyright holders. I. Pfeiffer, M., Batbayar, G., Hofmann, J., Siegfried, K., Karthe, D., Hahn-Tomer, S. (2015). Investigating arsenic (As) occurrence and sources in ground, surface, waste and drinking water in northern Mongolia Environ. Earth Sci. 73 (2), 649 – 662. II. Batbayar, G., Pfeiffer, M., von Tümpling, W., Kappas, M., Karthe, D. (2017). Chemical water quality gradients in the Mongolian sub-catchments of the Selenga River basin Environ. Monit. Assess. 189 (8), art. 420. III. Karthe, D., Chalov, S., Moreido, V., Pashkina, M., Romanchenko, A., Batbayar, G., Kalugin, A., Westphal, K., Malsy, M., Flörke, M. (2017). Assessment of runoff, water and sediment quality in the Selenga River basin aided by a web-based geoservice Water Resour. 44 (3), 399 – 416. IV. Batbayar, G., Pfeiffer, M., Kappas, M., Karthe, D. (2018). GIS based impact assessment of land use impacts on water quality in case of Kharaa River Basin. Submitted to Ambio. List of relevant book chapter, not included as part of this thesis Batbayar, G., Karthe, D., Pfeiffer, M., von Tümpling, W., Kappas, M. (2015). Influence of urban settlement and mining activities on surface water quality in northern Mongolia, In: Karthe, D., Chalov, S.R., Kasimov, N.S., Kappas, M., (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 23 Ibidem-Verlag, Stuttgart, p. 73 - 86 2 Author contributions The contributions from listed authors are divided as follows for each article: I. MP and GB led the writing with the help of all co-authors. GB, MP, JH, DK, KS acquired spatial and temporal data. All co-authors contributed to the data analysis and the design of the study. The writing was assisted by all co-authors. The study and related methods were designed by KS with help of MP and JH. The field data were collected by GB, MP, KS, and JH. II. GB, MP and DK led the writing with the help of all co-authors. GB acquired the spatial and temporal data. Data analysis was done by GB and MP. The writing was assisted by all co-authors. The study methods were designed by GB, MP, WT and DK. III. DK led the writing and all co-authors compiled the datasets and all co-authors did the data analysis. The water quality data analysis and chapter writing was done by GB and KW. The study and related methods were designed by all co-authors. All co- authors contributed to the field data collection. IV. GB and MP collected the field data and statistical analysis was done by GB and MP. Sub watershed delineation was done by GB and land use data was obtained by MOMO project. The study and related methods were designed by all co-authors. Writing was led by GB. 3 Contents Acknowledgments ......................................................................................................................................... 1 Dissertation content ...................................................................................................................................... 2 Contents ........................................................................................................................................................ 4 Figures .......................................................................................................................................................... 7 Tables ............................................................................................................................................................ 7 Chapter1. General introduction ................................................................................................................... 10 1.1 Study region ................................................................................................................................ 10 1.2 Context and summaries of the papers ......................................................................................... 11 Chapter2. Investigating arsenic (As) occurrence and sources in ground surface, waste and drinking water in northern Mongolia …………………………………………………………………………………………………………………..15 2.1 Abstract ................................................................................................................................................. 16 2.2 Introduction ........................................................................................................................................... 16 2.3 Material and Methods ........................................................................................................................... 18 2.3.1 Study Region ...................................................................................................................................... 18 2.3.2 Sampling Procedure ........................................................................................................................... 19 2.3.3 Chemical Analyses ............................................................................................................................
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
    [Show full text]
  • Journal Biology 2004 3
    Mongolian Journal of Biological Sciences 2004 Vol. 2(1): 39-42 Hydrochemical Characteristics of Selenge River and its Tributaries on the Territory of Mongolia Bazarova J.G. 1, Dorzhieva S.G.1, Bazarov B.G. 1, Barkhutova D.D.2, Dagurova O.P.2, Namsaraev B.B. 2 and Zhargalova S.O.2 1Baikal Institute of Nature Management of SB RAS, Ulan-Ude, 2Institute of General and Experimental Biology of SB RAS, Ulan-Ude, E-mail: [email protected] Abstract Hydrochemical research of the Selenge and its main tributary the Orkhon river on the territory of Mongolia has been conducted. Concentrations of the main water ions were measured. Distribution of - + heavy metals was determined. Dynamics of biogenic elements (NO3 , NH4 , phosphates) and degree of phenol pollution was determined. Key words: Baikal, biogenic, heavy metals, ions, phenol, Selenge River Introduction river is polluted along its entire length. To assess the current ecological condition in the Mongolian During the last 30-40 years Lake Baikal has part of the Selenge river basin, it is necessary to been influenced by various anthropogenic factors. implement hydrobiological and hydrochemical Industrial and household waste water have changed monitoring. It requires information not only of the chemical composition of Baikal with a chemical composition, but of biogenic components deterioration in water quality in the basin territory. in the processes of accumulation and According to sustainable development policy, transformation in water, bottom sediments and river protection of Baikal region is considered
    [Show full text]
  • The Influence of Climatic Change and Human Activity on Erosion Processes in Sub-Arid Watersheds in Southern East Siberia
    HYDROLOGICAL PROCESSES Hydrol. Process. 17, 3181–3193 (2003) Published online in Wiley InterScience (www.interscience.wiley.com). DOI: 10.1002/hyp.1382 The influence of climatic change and human activity on erosion processes in sub-arid watersheds in southern East Siberia Leonid M. Korytny,* Olga I. Bazhenova, Galina N. Martianova and Elena A. Ilyicheva Institute of Geography, Siberian Branch of the Russian Academy of Sciences, 1 Ulanbatorskaya St., Irkutsk, 664033, Russia Abstract: A LUCIFS model variant is presented that represents the influence of climate and land use change on fluvial systems. The study considers trends of climatic characteristics (air temperature, annual precipitation totals, rainfall erosion index, aridity and continentality coefficients) for the steppe and partially wooded steppe watersheds of the south of East Siberia (the Yenisey River macro-watershed). It also describes the influence of these characteristics on erosion processes, one indicator of which is the suspended sediment yield. Changes in the river network structure (the order of rivers, lengths, etc.) as a result of agricultural activity during the 20th century are investigated by means of analysis of maps of different dates for one of the watersheds, that of the Selenga River, the biggest tributary of Lake Baikal. The study reveals an increase of erosion process intensity in the first two-thirds of the century in the Selenga River watershed and a reduction of this intensity in the last third of the century, both in the Selenga River watershed and in most of the other watersheds of the study area. Copyright 2003 John Wiley & Sons, Ltd. KEY WORDS LUCIFS; Yenisey watershed; fluvial system; climate change; land use change; river network structure; erosion processes.
    [Show full text]
  • Archaeological Investigations of Xiongnu Sites in the Tamir River
    Archaeological Investigations of Xiongnu Sites in the Tamir River Valley Results of the 2005 Joint American-Mongolian Expedition to Tamiryn Ulaan Khoshuu, Ogii nuur, Arkhangai aimag, Mongolia David E. Purcell and Kimberly C. Spurr Flagstaff, Arizona (USA) During the summer of 2005 an archaeological investigations, and What is known points to this area archaeological expedition jointly their results, are the focus of this as one of the most important mounted by the Silkroad Foun- article, which is a preliminary and cultural regions in the world, a fact dation of Saratoga, California, incomplete record of the project recently recognized by the U.S.A. and the Mongolian National findings. Not all of the project data UNESCO through designation of University, Ulaanbataar, investi- — including osteological analysis of the Orkhon Valley as a World gated two sites near the the burials, descriptions or maps Heritage Site in 2004 (UNESCO confluence of the Tamir River with of the graves, or analyses of the 2006). Archaeological remains the Orkhon River in the Arkhangai artifacts — is available as of this indicate the region has been aimag of central Mongolia (Fig. 1). writing. Consequently, the greater occupied since the Paleolithic (circa The expedition was permitted emphasis falls on one of the two 750,000 years before present), (Registration Number 8, issued sites. It is hoped that through the with Neolithic sites found in great June 23, 2005) by the Ministry of Silkroad Foundation, the many numbers. As early as the Neolithic Education, Culture and Science of different collections from this period a pattern developed in Mongolia. The project had multiple project can be reunited in a which groups moved southward goals: archaeological investiga- scholarly publication.
    [Show full text]
  • Trans-Baykal (Rusya) Bölgesi'nin Coğrafyasi
    International Journal of Geography and Geography Education (IGGE) To Cite This Article: Can, R. R. (2021). Geography of the Trans-Baykal (Russia) region. International Journal of Geography and Geography Education (IGGE), 43, 365-385. Submitted: October 07, 2020 Revised: November 01, 2020 Accepted: November 16, 2020 GEOGRAPHY OF THE TRANS-BAYKAL (RUSSIA) REGION Trans-Baykal (Rusya) Bölgesi’nin Coğrafyası Reyhan Rafet CAN1 Öz Zabaykalskiy Kray (Bölge) olarak isimlendirilen saha adını Rus kâşiflerin ilk kez 1640’ta karşılaştıkları Daur halkından alır. Rusçada Zabaykalye, Balkal Gölü’nün doğusu anlamına gelir. Trans-Baykal Bölgesi, Sibirya'nın en güneydoğusunda, doğu Trans-Baykal'ın neredeyse tüm bölgesini işgal eder. Bölge şiddetli iklim koşulları; birçok mineral ve hammadde kaynağı; ormanların ve tarım arazilerinin varlığı ile karakterize edilir. Rusya Federasyonu'nun Uzakdoğu Federal Bölgesi’nin bir parçası olan on bir kurucu kuruluşu arasında bölge, alan açısından altıncı, nüfus açısından dördüncü, bölgesel ürün üretimi açısından (GRP) altıncı sıradadır. Bölge topraklarından geçen Trans-Sibirya Demiryolu yalnızca Uzak Doğu ile Rusya'nın batı bölgeleri arasında bir ulaşım bağlantısı değil, aynı zamanda Avrasya geçişini sağlayan küresel altyapının da bir parçasıdır. Bölgenin üretim yapısında sanayi, tarım ve ulaşım yüksek bir paya sahiptir. Bu çalışmada Trans-Baykal Bölgesi’nin fiziki, beşeri ve ekonomik coğrafya özellikleri ele alınmıştır. Trans-Baykal Bölgesinin coğrafi özelliklerinin yanı sıra, ekonomik ve kültürel yapısını incelenmiştir. Bu kapsamda konu ile ilgili kurumsal raporlardan ve alan araştırmalarından yararlanılmıştır. Bu çalışma sonucunda 350 yıldan beri Rus gelenek, kültür ve yaşam tarzının devam ettiği, farklı etnik grupların toplumsal birliği sağladığı, yer altı kaynaklarının bölge ekonomisi için yüzyıllardır olduğu gibi günümüzde de önem arz ettiği, coğrafyasının halkın yaşam şeklini belirdiği sonucuna varılmıştır.
    [Show full text]
  • Colonization of Northern Eurasia by Modern Humans: Radiocarbon Chronology and Environment
    Journal of Archaeological Science (2002) 29, 593–606 doi:10.1006/jasc.2001.0753, available online at http://www.idealibrary.com on Colonization of Northern Eurasia by Modern Humans: Radiocarbon Chronology and Environment P. M. Dolukhanov* Department of Archaeology, University of Newcastle upon Tyne, NE1 7RU, U.K. A. M. Shukurov School of Mathematics and Statistics, University of Newcastle upon Tyne, NE1 7RU, U.K. P. E. Tarasov Department of Geography, Moscow State University, Vorobyevy Gory, Moscow 119899, Russia G. I. Zaitseva Radiocarbon Laboratory, Institute for History of Material Culture, Russian Academy of Sciences, St Petersburg, Dvortsovaya nab. 18, 191186 Russia (Received 30 January 2001, revised manuscript accepted 25 July 2001) The distribution of frequencies of radiocarbon-dated Palaeolithic sites in northern Eurasia shows three peaks of 40–30, 24–18 and 17–1 ka . We argue that these peaks reflect the waves in the colonization of that area by Anatomically Modern Humans stemming from Central and Eastern Europe and caused by environmental stress. 2002 Elsevier Science Ltd. All rights reserved. Keywords: NORTHERN EURASIA, ANATOMICALLY MODERN HUMANS, RADIOCARBON, UPPER PALAEOLITHIC, LAST ICE AGE, PALAEOCLIMATE. Introduction glacial’’), and OIS 3 consisting of the Late Glacial Maximum (LGM) and the Late Glacial Recession. he present article is aimed at the discussion of the initial dispersal of anatomically modern T humans (AMH) in northern Eurasia, as Data and Methods inferred mainly from radiocarbon chronology and Radiocarbon age palaeoenvironmental evidence. In this respect this article may be viewed as a direct development of the The main resource of the present study consists of the previous publication, focused on East European Plain database of radiocarbon measurements of Siberia’s (Dolukhanov, Shukurov & Sokoloff, 2001).
    [Show full text]
  • DRAINAGE BASINS of the WHITE SEA, BARENTS SEA and KARA SEA Chapter 1
    38 DRAINAGE BASINS OF THE WHITE SEA, BARENTS SEA AND KARA SEA Chapter 1 WHITE SEA, BARENTS SEA AND KARA SEA 39 41 OULANKA RIVER BASIN 42 TULOMA RIVER BASIN 44 JAKOBSELV RIVER BASIN 44 PAATSJOKI RIVER BASIN 45 LAKE INARI 47 NÄATAMÖ RIVER BASIN 47 TENO RIVER BASIN 49 YENISEY RIVER BASIN 51 OB RIVER BASIN Chapter 1 40 WHITE SEA, BARENT SEA AND KARA SEA This chapter deals with major transboundary rivers discharging into the White Sea, the Barents Sea and the Kara Sea and their major transboundary tributaries. It also includes lakes located within the basins of these seas. TRANSBOUNDARY WATERS IN THE BASINS OF THE BARENTS SEA, THE WHITE SEA AND THE KARA SEA Basin/sub-basin(s) Total area (km2) Recipient Riparian countries Lakes in the basin Oulanka …1 White Sea FI, RU … Kola Fjord > Tuloma 21,140 FI, RU … Barents Sea Jacobselv 400 Barents Sea NO, RU … Paatsjoki 18,403 Barents Sea FI, NO, RU Lake Inari Näätämö 2,962 Barents Sea FI, NO, RU … Teno 16,386 Barents Sea FI, NO … Yenisey 2,580,000 Kara Sea MN, RU … Lake Baikal > - Selenga 447,000 Angara > Yenisey > MN, RU Kara Sea Ob 2,972,493 Kara Sea CN, KZ, MN, RU - Irtysh 1,643,000 Ob CN, KZ, MN, RU - Tobol 426,000 Irtysh KZ, RU - Ishim 176,000 Irtysh KZ, RU 1 5,566 km2 to Lake Paanajärvi and 18,800 km2 to the White Sea. Chapter 1 WHITE SEA, BARENTS SEA AND KARA SEA 41 OULANKA RIVER BASIN1 Finland (upstream country) and the Russian Federation (downstream country) share the basin of the Oulanka River.
    [Show full text]
  • The Linkage of the Precipitation in the Selenga River Basin to Midsummer Atmospheric Blocking
    atmosphere Article The Linkage of the Precipitation in the Selenga River Basin to Midsummer Atmospheric Blocking Olga Yu. Antokhina 1,*, Pavel N. Antokhin 1 , Yuliya V. Martynova 2,3 and Vladimir I. Mordvinov 4 1 Zuev Institute of Atmospheric Optics SB RAS, 634021 Tomsk, Russia; [email protected] 2 Institute of Monitoring of Climatic and Ecological Systems SB RAS, 634055 Tomsk, Russia; [email protected] 3 Siberian Regional Hydrometeorological Research Institute, 630099 Novosibirsk, Russia 4 Institute of Solar-Terrestrial Physics, SB RAS, 664033 Irkutsk, Russia; [email protected] * Correspondence: [email protected]; Tel.: +7-952-154-4669 Received: 3 June 2019; Accepted: 21 June 2019; Published: 24 June 2019 Abstract: The linkage between atmospheric blocking (blocking frequency, BF) and total monthly July precipitation in the Selenga River Basin, the main tributary of Lake Baikal, for the period 1979–2016 was investigated. Based on empirical orthogonal functions (EOF) analysis, two dominant modes of precipitation over the Selenga River Basin were extracted. The first EOF mode (EOF 1) is related to precipitation fluctuations mainly in the Mongolian part of Selenga; the second EOF mode (EOF 2)—in the Russian part of Selenga. Based on two different modes obtained, the total amount of precipitation individually for the Russian and Mongolian part of Selenga was calculated. Correlation analysis has demonstrated that precipitation over the Mongolian part of the Selenga Basin is positively correlated to blocking over Eastern Siberia/Mongolia (80–120◦ E, ESM-BF). Precipitation over the Russian part of the Selenga Basin is positively correlated to blocking over the Urals-Western Siberia (50–80◦ E, UWS-BF) and European blocking (0–50◦ E, E-BF).
    [Show full text]
  • Metadata Describing the Kharaa Yeröö River Basin Water Quality Database
    Metadata describing the Kharaa Yeröö River Basin Water Quality Database Jürgen Hofmann , Ralf Ibisch, Daniel Karthe , Buren Scharaw, Michael Schäffer, Melanie Hartwig, Philipp Theuring , Michael Rode, Saulyegul Avlyush , Vanessa Watson, Vanessa Bremerich , Gerel Osor, Andrew Kaus , Katja Westphal, Martin Pfeiffer , Jörg Priess , Christian Schweitzer, Daniel Krätz, Jonas Gröning , Jens Hürdler, Gunsmaa Batbayar , Sonja Heldt, Olaf Büttner & Dietrich Borchardt Freshwater Metadata Journal DOI 10.15504/fmj.2018.36 Published by University of Natural Resources and ISSN 2312-6604 Life Sciences, Institute of Hydrobiology and Published online: 2018-09-28 Aquatic Ecosystem Management, BOKU - Vienna Freshwater Metadata Journal 36: 1-10 DOI 10.15504/fmj.2018.36 http://freshwaterjournal.eu ISSN 2312-6604 Metadata describing the Kharaa Yeröö River Basin Water Quality Database Jürgen Hofmann 1 , Ralf Ibisch 4, Daniel Karthe 7 , Buren Scharaw 5, Michael Schäffer 4, Melanie Hartwig 4, Philipp Theuring 4 , Michael Rode 3, Saulyegul Avlyush 9 , Vanessa Watson 6, Vanessa Bremerich 1 , Gerel Osor 8, Andrew Kaus 4 , Katja Westphal 3, Martin Pfeiffer 3 , Jörg Priess 3 , Christian Schweitzer 4, Daniel Krätz 4, Jonas Gröning 1 , Jens Hürdler 2, Gunsmaa Batbayar 7 , Sonja Heldt 10, Olaf Büttner 3 & Dietrich Borchardt 3 1 Leibniz-Institute of Freshwater Ecology and Inland Fisheries (IGB), Berlin, Germany; corresponding author: [email protected] 2 formerly: Leibniz-Institute of Freshwater Ecology and Inland Fisheries (IGB), Berlin, Germany 3 Helmholtz-Centre
    [Show full text]
  • Subject of the Russian Federation)
    How to use the Atlas The Atlas has two map sections The Main Section shows the location of Russia’s intact forest landscapes. The Thematic Section shows their tree species composition in two different ways. The legend is placed at the beginning of each set of maps. If you are looking for an area near a town or village Go to the Index on page 153 and find the alphabetical list of settlements by English name. The Cyrillic name is also given along with the map page number and coordinates (latitude and longitude) where it can be found. Capitals of regions and districts (raiony) are listed along with many other settlements, but only in the vicinity of intact forest landscapes. The reader should not expect to see a city like Moscow listed. Villages that are insufficiently known or very small are not listed and appear on the map only as nameless dots. If you are looking for an administrative region Go to the Index on page 185 and find the list of administrative regions. The numbers refer to the map on the inside back cover. Having found the region on this map, the reader will know which index map to use to search further. If you are looking for the big picture Go to the overview map on page 35. This map shows all of Russia’s Intact Forest Landscapes, along with the borders and Roman numerals of the five index maps. If you are looking for a certain part of Russia Find the appropriate index map. These show the borders of the detailed maps for different parts of the country.
    [Show full text]
  • Observed Trends of Climate and River Discharge in Mongolia's Selenga
    water Article Observed Trends of Climate and River Discharge in Mongolia’s Selenga Sub-Basin of the Lake Baikal Basin Batsuren Dorjsuren 1,2 , Denghua Yan 1,3,4,*, Hao Wang 1,3,4, Sonomdagva Chonokhuu 2 , Altanbold Enkhbold 5, Xu Yiran 6, Abel Girma 1,7 , Mohammed Gedefaw 1,7 and Asaminew Abiyu 1 1 College of Environmental Science and Engineering, Donghua University, Shanghai 201620, China; [email protected] (B.D.); [email protected] (H.W.); [email protected] (A.G.); [email protected] (M.G.); [email protected] (A.A.) 2 Department of Environment and Forest Engineering, School of Engineering and Applied Sciences, National University of Mongolia, Ulaanbaatar 210646, Mongolia; [email protected] 3 State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research (IWHR), Beijing 100038, China 4 Water Resources Department, China Institute of Water Resources and Hydropower Research (IWHR), Beijing 100038, China 5 Department of Geography, School of Art & Sciences, National University of Mongolia, Ulaanbaatar 210646, Mongolia; [email protected] 6 School of Resources and Earth Science, China University of Mining and Technology, Xuzhou 221116, China; [email protected] 7 Department of Natural Resource Management, University of Gondar, Gondar 196, Ethiopia * Correspondence: [email protected]; Tel.: +86-10-68781976 Received: 11 September 2018; Accepted: 9 October 2018; Published: 12 October 2018 Abstract: Mongolia’s Selenga sub-basin of the Lake Baikal basin is spatially extensive, with pronounced environmental gradients driven primarily by precipitation and air temperature on broad scales. Therefore, it is an ideal region to examine the dynamics of the climate and the hydrological system.
    [Show full text]
  • Baikal Project 2012-2014 Results and Events Booklet.Pdf
    Photo by Elena Chumak 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. Photo by Elena Chumak Contents Project Achievements
    [Show full text]