The Report on the Quantity Monitoring, Threatening Factors and Protection Proposals of Breeding Population of Oriental White Stork in Sanjiang Plain
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Characteristics of Nitrate in Major Rivers and Aquifers of the Sanjiang Plain, China
View Online / Journal Homepage Journal of Dynamic Article LinksC< Environmental Monitoring Cite this: DOI: 10.1039/c2em30032j www.rsc.org/jem PAPER Characteristics of nitrate in major rivers and aquifers of the Sanjiang Plain, China Yingjie Cao,ab Changyuan Tang,*b Xianfang Song,a Changming Liua and Yinghua Zhanga Received 16th January 2012, Accepted 6th July 2012 DOI: 10.1039/c2em30032j À The characteristics of nitrate (NO3 ) in major rivers and aquifers of the Sanjiang Plain, China were investigated by hydrogeochemical conditions, nitrogen isotope technique and CFCs trace. An overall À understanding on the sources and fate of NO3 in the surface water and the groundwater was obtained. À The NO3 concentrations in the surface water were low and no samples exceeds the WTO standards. À However, 11.4% of the groundwater samples exceeded the WTO standards, indicating local NO3 pollution in rural areas. Redox condition analysis revealed that most of the surface water had oxic condition, while for the shallow groundwater (mean well depth smaller than 30 m), the redox condition began to change into anoxic zone, and the deep groundwater (mean well depth larger than 50 m) 15 showed strong anoxic condition. The d N-NO3 data indicated soil N and fertilizer contributed the À major sources in the surface water, and NO3 in the groundwater mainly showed a manure origin. In the Songhua–Heilong River, dilution effect was dominating, while for the Wusuli River, it showed that À À mix with water contained excess of NO3 resulted in the NO3 concentration increased along the river. À Additionally, the NO3 transportation in the groundwater was analyzed by groundwater ages derived À from environmental tracer (CFCs) data. -
Saving the Flagship Species of North-East Asia
North-East Asian Subregional Programme for Environmental Cooperation (NEASPEC) SAVING THE FLAGSHIP SPECIES THE FLAGSHIP SAVING SAVING THE FLAGSHIP SPECIES OF NORTH-EAST ASIA OF NORTH-EAST ASIA United Nations ESCAP United Nations Economic and Social Commission for Asia and the Pacific Environment and Sustainable Development Division United Nations Building Rajadamnern Nok Avenue Nature Conservation Strategy of NEASPEC Bangkok 10200 Thailand Tel: (662) 288-1234; Fax: (662) 288-1025 E-mail: [email protected] E-mail: [email protected] Website: <http://www.unescap.org/esd> United Nations ESCAP ECONOMIC AND SOCIAL COMMISSION FOR ASIA AND THE PACIFIC ESCAP is the regional development arm of the United Nations and serves as the main economic and social development centre for the United Nations in Asia and the Pacific. Its mandate is to foster cooperation between its 53 members and 9 associate members. ESCAP provides the strategic link between global and country-level programmes and issues. It supports the Governments of the region in consolidating regional positions and advocates regional approaches to meeting the region’s unique socio-economic challenges in a globalizing world. The ESCAP office is located in Bangkok, Thailand. Please visit our website at www.unescap.org for further information. Saving the Flagship Species The grey shaded area of the map represents the members and associate members of ESCAP of North-East Asia: United Nations publication Nature Conservation Strategy of NEASPEC Copyright© United Nations 2007 ST/ESCAP/2495 -
6. Tourism Guide 2010 English Version Combined.Pdf
Contents Introduction section Page 1 Introduction to the Greater Tumen Region Page 2 Highlights Page 4 Practical Information Guide section Page 5 China Page 9 Heilongjiang Page 12 Jilin Page 15 Liaoning Page 17 Inner Mongolia Page 19 Mongolia Page 23 Khentii Page 25 Sükhbaatar Page 27 Dornod Page 30 Ulaan Baatar Page 31 ROK Page 35 Gangwon The GTI Page 38 Gyeongbuk The Greater Tumen Initiative (GTI) is an intergovernmental cooperation Page 41 Ulsan mechanism in Northeast Asia, supported Page 43 Busan by the United Nations Development Programme (UNDP), with a four- country membership: the People’s Page 45 Russia Republic of China, Mongolia, the Republic of Korea and the Russian Federation. Created in 1995, the GTI Page 49 Primorsky Krai has remained a unique platform for Page 53 The Russian Far East promoting economic cooperation and fostering peace, stability and sustainable development in the region. The GTI Page 55 GTI bordering area: DPRK serves as a catalyst for expanding policy dialogue among member states and for strengthening the fundamentals for Page 57 Rajin-Sonbong economic growth. Regional cooperation fostered by the GTI has proven to be an effective way to improve basic infrastructure, ensure energy security, boost tourism development, facilitate trade and investment, and promote environmental sustainability in the region. Introduction to the Greater Tumen Region The Tumen River starts its life over 2,000m above sea level in majestic Tian Chi, a volcanic crater lake surrounded by jagged, snow-dappled peaks. It then proceeds northeast on a gentle, 500km-long journey, one that sees its fish-filled waters pass through three time zones, and brushing against three national borders before emptying into the sea. -
대외경제정책연구원-2014 KIEP Visiting Fellows Program.Hwp
2014 2014 KIEP KIEP Visiting Fellows Program KIEP Fellows Visiting Visiting Fellows Program Edited by JEONG Hyung-Gon Edited by JEONG Hyung-Gon 370 Sicheong-daero, Sejong-Si 339-705, Korea Tel: (8244) 414-1042 / Fax: (8244) 414-1043 URL: http://www.kiep.go.kr 2014 KIEP Visiting Fellows Program Edited by JEONG Hyung-Gon The Contents of the KIEP Visiting Fellow Program do not reflect or represent the official opinion of KIEP. The KIEP Visiting Fellows Program is published with the aim of promoting discussions among researchers, and to remember the outstanding achievements by the visiting fellows who came to KIEP. KOREA INSTITUTE FOR INTERNATIONAL ECONOMIC POLICY (KIEP) 370 Sicheong-daero, Sejong-Si 339-705, Korea Tel: (8244) 414-1042 Fax: (8244) 414-1043 URL: http://www.kiep.go.kr LEE Il Houng, President Published 2015 in Korea by KIEP ⓒ 2015 KIEP Acknowledgements In 2009, Korea Institute for International Economic Policy (KIEP) launched "Visiting Fellows Program (VFP)" with the view of advancing cross-border exchanges of knowledge, information, insights and expertise. Since its inception, the VFP has demonstrated that sharing thoughts and ideas through face-to-face contacts and dialogue works as a catalyst for enhancing mutual understanding among scholars and professionals with diverse background. By successfully implementing the VFP for the past 7 years, KIEP has been motivated to assume the role as a hub for international economic research in the region. As a host of the program, KIEP has many mandates. One of those tasks is to let more people know what has been accomplished through the program and how valuable it is. -
Family-Sisoridae-Overview-PDF.Pdf
FAMILY Sisoridae Bleeker, 1858 - sisorid catfishes SUBFAMILY Sisorinae Bleeker, 1858 - sisorid catfishes [=Sisorichthyoidei, Bagarina, Nangrina] GENUS Ayarnangra Roberts, 2001 - sisorid catfishes Species Ayarnangra estuarius Roberts, 2001 - Irrawaddy ayarnangra GENUS Bagarius Bleeker, 1853 - sisorid catfishes Species Bagarius bagarius (Hamilton, 1822) - goonch, dwarf goonch [=buchanani, platespogon] Species Bagarius rutilus Ng & Kottelat, 2000 - Red River goonch Species Bagarius suchus Roberts, 1983 - crocodile catfish Species Bagarius yarrelli (Sykes, 1839) - goonch, giant devil catfish [=carnaticus, lica, nieuwenhuisii] GENUS Caelatoglanis Ng & Kottelat, 2005 - sisorid catfishes Species Caelatoglanis zonatus Ng & Kottelat, 2005 - Chon Son catfish GENUS Conta Hora, 1950 - sisorid catfishes Species Conta conta (Hamilton, 1822) - Mahamanda River catfish [=elongata] Species Conta pectinata Ng, 2005 - Dibrugarh catfish GENUS Erethistes Muller & Troschel, 1849 - sisorid catfishes [=Hara, Laguvia] Species Erethistes filamentosus (Blyth, 1860) - Megathat Chaung catfish [=maesotensis] Species Erethistes hara (McClelland, 1843) - Hooghly River catfish [=asperus, buchanani, saharsai, serratus] Species Erethistes horai (Misra, 1976) - Terai catfish Species Erethistes jerdoni (Day, 1870) - Sylhet catfish Species Erethistes koladynensis (Anganthoibi & Vishwanath, 2009) - Koladyne River catfish Species Erethistes longissimus (Ng & Kottelat, 2007) - Mogaung catfish Species Erethistes mesembrinus (Ng & Kottelat, 2007) - Langkatuek catfish Species Erethistes -
Flood Control for the Red River [Vietnam]
Total Disaster Risk Management - Good Practices - Chapter 3 Vietnam Flood Control for the Red River The Red River, the Delta and Floods The history of the development of Vietnamese civilizations is closely linked to the Red River (Hong River) Delta. As the second largest granary of Vietnam, the Delta holds a significant meaning in the life of the Vietnamese people. This is where approximately 15–20 % of Vietnam’s rice is produced. A population of 17 million now inhabits the 16,500-km2 area of the Red River Delta. The catchment area of the Red River is estimated at 169,000 km2, half of which lies in China. The Red River at Hanoi comprises three major tributary systems, the Da, Thao and Lo Rivers. The river is the source of various positive aspects for human life, such as water resources and rich alluvium (it is called the Red River as the large amount of alluvium it carries colors it red all year round). However, these go hand in hand with a much less expected occurrence: floods. Increased flash floods as a result of deforestation in the upstream parts of the Red River basin, and raised bed levels of the rivers due to the deposition of sediment, are causing higher flood levels, endangering the ever increasing socio-economic value of the capital. The land in low-lying areas of the river delta is protected against flooding by river dyke systems. According to official historical records, in 1108, King Ly Nhan Tong ordered the construction of the first dyke with solid foundations on a large scale aimed at protecting the capital of Thang Long (now Hanoi). -
Habitat Specialisation in the Reed Parrotbill Paradoxornis Heudei Evidence from Its Distribution and Habitat
FORKTAIL 29 (2013): 64–70 Habitat specialisation in the Reed Parrotbill Paradoxornis heudei—evidence from its distribution and habitat use LI-HU XIONG & JIAN-JIAN LU The Reed Parrotbill Paradoxornis heudei is found in habitats dominated by Common Reed Phragmites australis in East Asia. This project was designed to test whether the Reed Parrotbill is a specialist of reed-dominated habitats, using data collected through literature review and field observations. About 87% of academic publications describing Reed Parrotbill habitat report an association with reeds, and the species was recorded in reeds at 92% of sites where it occurred. On Chongming Island, birds were only recorded in transects covered with reeds or transects with scattered reeds close to large reedbeds. At the Chongxi Wetland Research Centre, monthly monitoring over three years also showed that the species was not recorded in habitats without reeds. The density of Reed Parrotbills was higher in reedbeds than mixed vegetation (reeds with planted trees) and small patches of reeds. The species rarely appeared in mixed habitat after reeds disappeared. These results confirm that the species is a reed specialist and highlights that conservation of reed-dominated habitat is a precondition to conserve the Reed Parrotbill. INTRODUCTION METHODS Habitat specialisation results in some species having a close Three sets of information on Reed Parrotbill distribution and relationship with only a few habitat types (Futuyma & Moreno habitat use were used: (1) distribution and habitat use data in the 1988), and habitat specialists have some specific life-history Chinese part of its range, collated from academic publications, web characteristics, for example, they often have weak dispersal abilities news, communication with birdwatchers and personal (Krauss et al. -
Table of Codes for Each Court of Each Level
Table of Codes for Each Court of Each Level Corresponding Type Chinese Court Region Court Name Administrative Name Code Code Area Supreme People’s Court 最高人民法院 最高法 Higher People's Court of 北京市高级人民 Beijing 京 110000 1 Beijing Municipality 法院 Municipality No. 1 Intermediate People's 北京市第一中级 京 01 2 Court of Beijing Municipality 人民法院 Shijingshan Shijingshan District People’s 北京市石景山区 京 0107 110107 District of Beijing 1 Court of Beijing Municipality 人民法院 Municipality Haidian District of Haidian District People’s 北京市海淀区人 京 0108 110108 Beijing 1 Court of Beijing Municipality 民法院 Municipality Mentougou Mentougou District People’s 北京市门头沟区 京 0109 110109 District of Beijing 1 Court of Beijing Municipality 人民法院 Municipality Changping Changping District People’s 北京市昌平区人 京 0114 110114 District of Beijing 1 Court of Beijing Municipality 民法院 Municipality Yanqing County People’s 延庆县人民法院 京 0229 110229 Yanqing County 1 Court No. 2 Intermediate People's 北京市第二中级 京 02 2 Court of Beijing Municipality 人民法院 Dongcheng Dongcheng District People’s 北京市东城区人 京 0101 110101 District of Beijing 1 Court of Beijing Municipality 民法院 Municipality Xicheng District Xicheng District People’s 北京市西城区人 京 0102 110102 of Beijing 1 Court of Beijing Municipality 民法院 Municipality Fengtai District of Fengtai District People’s 北京市丰台区人 京 0106 110106 Beijing 1 Court of Beijing Municipality 民法院 Municipality 1 Fangshan District Fangshan District People’s 北京市房山区人 京 0111 110111 of Beijing 1 Court of Beijing Municipality 民法院 Municipality Daxing District of Daxing District People’s 北京市大兴区人 京 0115 -
Hydrochemical Formation Mechanism of Mineral Springs in Changbai Mountain, China
Hydrochemical Formation Mechanism of Mineral Springs in Changbai Mountain, China Jialin Li Jilin University min jian Bian ( [email protected] ) Jilin university Yihan Li Jilin University Yuxi Ma Jilin University Yanmei Li University of Guanajuato: Universidad de Guanajuato Research Article Keywords: Hydrochemical formation mechanism, Cluster analysis, PCA , Metasilicic-acid mineral springs, Changbai Mountain Posted Date: February 18th, 2021 DOI: https://doi.org/10.21203/rs.3.rs-208397/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License 1 Hydrochemical formation mechanism of mineral springs in 2 Changbai Mountain, China 3 Jialin Li1,2, Jianmin Bian1,2*, Yihan Li1,2, Yuxi Ma1,2, Yanmei Li3 4 1Key Laboratory of Groundwater Resources and Environment, Ministry of Education, 5 Jilin University, Changchun 130021, China 6 2College of New Energy and Environment, Jilin University, Changchun 130021, 7 China 8 3Department of Mine, Metallurgy and Geology Engineering, Engineering Division, 9 University of Guanajuato, Guanajuato C.P. 36020, Mexico 10 *Corresponding author. Tel:+86-1800-431-9968; E-mail:[email protected] 11 (Jianmin Bian) 12 Declarations 13 •Funding 14 This research was funded by the National Key R&D Program of China, grant number 15 2019YFC0409103, and the Key R&D Program of Science and Technology 16 Department of Jilin Province, grant number 20190303076SF. 17 The funding body has funded sample collection tests and data analysis. 18 •Competing interests 19 Not applicable 20 •Availability of data and material 21 Not applicable 22 •Code availability 23 Not applicable 24 • Author contributions 25 Jialin Li: Data curation, Formal analysis, Methodology, Software, Roles/Writing - 26 original draft. -
DRAINAGE BASINS of the SEA of OKHOTSK and SEA of JAPAN Chapter 2
60 DRAINAGE BASINS OF THE SEA OF OKHOTSK AND SEA OF JAPAN Chapter 2 SEA OF OKHOTSK AND SEA OF JAPAN 61 62 AMUR RIVER BASIN 66 LAKE XINGKAI/KHANKA 66 TUMEN RIVER BASIN Chapter 2 62 SEA OF OKHOTSK AND SEA OF JAPAN This chapter deals with major transboundary rivers discharging into the Sea of Okhotsk and the Sea of Japan and their major transboundary tributaries. It also includes lakes located within the basins of these seas. TRANSBOUNDARY WATERS IN THE BASINS OF THE SEA OF OKHOTSK AND THE SEA OF JAPAN1 Basin/sub-basin(s) Total area (km2) Recipient Riparian countries Lakes in the basin Amur 1,855,000 Sea of Okhotsk CN, MN, RU … - Argun 164,000 Amur CN, RU … - Ussuri 193,000 Amur CN, RU Lake Khanka Sujfun 18,300 Sea of Japan CN, RU … Tumen 33,800 Sea of Japan CN, KP, RU … 1 The assessment of water bodies in italics was not included in the present publication. 1 AMUR RIVER BASIN o 55 110o 120o 130o 140o SEA OF Zeya OKHOTSK R U S S I A N Reservoir F E mur D un A E mg Z A e R Ulan Ude Chita y ilka a A a Sh r od T u Ing m n A u I Onon g ya r re A Bu O n e N N Khabarovsk Ulaanbaatar Qiqihar i MONGOLIA a r u u gh s n s o U CHIN A S Lake Khanka N Harbin 45o Sapporo A Suj fu Jilin n Changchun SEA O F P n e JA PA N m Vladivostok A Tu Kilometres Shenyang 0 200 400 600 The boundaries and names shown and the designations used on this map Ch’ongjin J do not imply official endorsement or acceptance by the United Nations. -
APPENDIX 6D Profile of the Inland Waterway Master Plan Projects
APPENDIX 6D Profile of the Inland Waterway Master Plan Projects ANNEX 6D Profile of the Inland Waterway Master Plan Projects A. Ongoing/Committed Project Profile Project Name: Sector: Upgrading of Northern Trans Mekong corridor (to Class III) (253km) CW01 Project Background & Objective: None of the corridors provide good transport continuity at present , and improvements will help improve region – wide accessibility re- lieve congestion on the main corridors, reduce transportation costs and supports economic development in the provinces. Project Description: (i) To improve the standard (up to Class III/300DWT vessels) and connectivity of the canal network in Northern Trans Mekong corri- dor(253km):Dredging, bank protection, ship lock, bridge improvements, navigation aids for 24-hour navigation, as one of the com- ponents of Development of transport infrastructure of Mekong River Delta. (ii) Main Project Components is Dredging, Bank protection, Improving and building bridges, Enhancing alarming system, Building Rach Chanh Dock and Building Tan Chau Port: Estimated Cost (2009): Original Schedule: US 99.3 million (including CW02) 2009–2015 Financial Source: Implementation Agency World Bank , Vietnam VIWA 6D-1 Project Name: Sector: Updating of Southern coastal corridor (to Class III) (153km) CW02 Project Background & Objective: This improvements will help improve region –wide accessibility, relieve congestion on the main corridors, reduce transportation costs and support economic development in the province. Project Description: (i) To improve the standard (up to Class III/300DWT vessels) and connectivity of the canal network in the southern coastal corri- dor(153km) (ii) Location is Gia Rai–Bac Liec–Dai Ngai (103km) and Cho Gao Canal (50km) (iii) Main components are as follows: Dredging, bank protections, ship lock, bridge improvements, navigation aids for 24-hour naviga- tion .These are one of the components of Development of transport infrastructure of Mekong River Delta. -
Sources of Metasilicate in Mineral Water of Jingyu County, Northeastern China
E3S Web of Conferences 98, 01052 (2019) https://doi.org/10.1051/e3sconf/20199801052 WRI-16 Sources of metasilicate in mineral water of Jingyu County, northeastern China Changlai Xiao1, Yajie Yuan1, Xiujuan Liang1,*,Weifei Yang1, and Ying Sun1 1Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, No 2519, Jiefang Road, Changchun130021, PR China Abstract. The source of metasilicate in mineral water of Jingyu County. located in Changbai Mountains of northeastern China, was analysed through two groups of water-rock interaction experiments. One is a hydrolysis immersion experiment using basalt and the other is an immersion experiment utilizing a mixture of soil, scoria, and clastic basalt under the same conditions. Results indicate that the metasilicate in mineral water is mainly derived from the hydrolysis of silicates and silica in the basalt, scoria, and soil. In the first immersion experiment, the release of metasilicate is linear, with dissolved metasilicate increasing continuously through time at a stable release rate of about 0.01 mg/(kgday). The second experiment indicates that the contribution of soil and scoria to metasilicate in mineral water is higher than that of clastic basalt under the same conditions. 1 Introduction Many studies on hydrogeochemical characteristics of groundwater and on water-rock interactions have been conducted by different scholars [1-4]. Natural mineral water has attracted much attention due to its special components that are beneficial to our health [2-4]. Changbai Mountains is one of the three largest natural mineral water sources in the world, comparable to the Alps and the North Caucasus mountains. It is also a source of mineral water, with a large area of 16,300 km2 covered with basalt.