Scheme Comparisons of Nanpan River Grand Bridge on Railway from Yunnan to Guangxi
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Controls on Modern Erosion and the Development of the Pearl River Drainage in the Late Paleogene
Marine Geology xxx (xxxx) xxx–xxx Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margo Invited research article Controls on modern erosion and the development of the Pearl River drainage in the late Paleogene ⁎ Chang Liua, Peter D. Clifta,b, , Andrew Carterc, Philipp Böningd, Zhaochu Hue, Zhen Sunf, Katharina Pahnked a Department of Geology and Geophysics, Louisiana State University, Baton Rouge 70803, USA b School of Geography Science, Nanjing Normal University, Nanjing 210023, China c Department of Earth and Planetary Sciences, Birkbeck College, University of London, London WC1E 7HX, UK d Max Planck Research Group for Marine Isotope Geochemistry, Institute of Chemistry and Biology of the Marine Environment (ICBM), University of Oldenburg, 26129, Germany e State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China f Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, 164 Xingangxi Road, Guangzhou 510301, China ARTICLE INFO ABSTRACT Keywords: The Pearl River and its tributaries drains large areas of southern China and has been the primary source of Zircon sediment to the northern continental margin of the South China Sea since its opening. In this study we use a Nd isotope combination of bulk sediment geochemistry, Nd and Sr isotope geochemistry, and single grain zircon U-Pb Erosion dating to understand the source of sediment in the modern drainage. We also performed zircon U-Pb dating on Provenance Eocene sedimentary rocks sampled by International Ocean Discovery Program (IODP) Expedition 349 in order to Pearl River constrain the source of sediment to the rift before the Oligocene. -
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Advances in Social Science, Education and Humanities Research, volume 85 4th International Conference on Management Science, Education Technology, Arts, Social Science and Economics (MSETASSE 2016) Discussions on Development of Cultural Tourism Industry in Region at the Source of the Pearl River Jingfeng Wang School of economics and management, Qujing Normal University, Qujing Yunnan, 655011, China Key words: Source of the Pearl River, Cultural tourism, Development. Abstract. The Pearl River is one of the three large inland rivers of China. The region at the source of the Pearl River is rich in natural landscape resources and human landscapes, has a profound historical and cultural foundation, and is distinctively featured by minority folk-custom, all of which are advantageous conditions for the development of cultural tourism industry. Yet the development situation of cultural tourism industry at the source of the Pearl River is still less than satisfactory. Only by transformation and upgrading of scenic region at the source of the Pearl River, and development of minority folk-custom-themed the Three Kingdoms History-themed cultural tourism, and cultural heritage tourism products, the cultural tourism industry at the source of the Pearl River can have more development opportunities. Overview of the Pearl River and of Its Source The Pearl River is one of the three inland rivers of China. By streamflow, the Pearl River is the second largest inland river in China, second only to the Yangtze River; by length, the Pearl River is the third largest inland river in China, following the Yangtze River and the Yellow River. The main stream of the Pearl River is 2320km long in total, the basin area is 446,768km2 [1], its river basin stretches over Yunnan, Guizhou, Guangxi, Hunan, Jiangxi, Guangdong, Hong Kong and Macao, and it flows into the South China Sea from the 8th estuary in the Pearl River Delta. -
Tradable Discharge Permits System for Water Pollution of the Upper Nanpan River, China
ECONOMY AND ENVIRONMENT PROGRAM FOR SOUTHEAST ASIA Tradable Discharge Permits System for Water Pollution of the Upper Nanpan River, China Wendong Tao, Weimin Yang & Bo Zhou EEPSEA RESEARCH REPORT SERIES EEPSEA is supported by a consortium of donors and administered by IDRC. Mailing Address: Tanglin PO Box 101, Singapore 912404 Visiting Address: 7th Storey RELC Building, 30 Orange Grove Road Telephone: 65 235 1344 Fax: 65 235 1849 Internet: [email protected] or [email protected] Website: http://www.idrc.org.sg/eepsea Comments should be sent to the authors at Yunnan Institute of Environmental Sciences or at Yunnan Environmental Protection Bureau, 23 Wang Jia Ba Kunming 650034, CHINA. E-mail: [email protected] or [email protected] The Economy and Environment Program for South East Asia (EEPSEA) was established in May, 1993 to support research and training in environmental and resource economics. Its objective is to enhance local capacity to undertake the economic analysis of environmental problems and policies. It uses a local networking approach, involving courses, meetings, technical support, access to literature and opportunities for comparative research. Member countries are Thailand, Malaysia, Indonesia, the Philippines, Vietnam, Cambodia, Laos, China, PNG and Sri Lanka. EEPSEA's funding is provided by a consortium of donors. As of June 1998, these sponsors consisted of IDRC (Canada), Sida (Sweden), Danida (Denmark), the Ministries ofForeign Affairs of Norway and the Netherlands and the MacArthur Foundation (USA). EEPSEA Research Reports are the outputs of research projects supported by EEPSEA. They have been peer reviewed and edited. In some cases, longer versions are available from the authors. -
Market-Based Approaches for Environmental Management in Asia July 2021
GREENING MARKETS MARKET-BASED APPROACHES FOR ENVIRONMENTAL MANAGEMENT IN ASIA JULY 2021 ASIAN DEVELOPMENT BANK GREENING MARKETS MARKET-BASED APPROACHES FOR ENVIRONMENTAL MANAGEMENT IN ASIA JULY 2021 ASIAN DEVELOPMENT BANK Creative Commons Attribution 3.0 IGO license (CC BY 3.0 IGO) © 2021 Asian Development Bank 6 ADB Avenue, Mandaluyong City, 1550 Metro Manila, Philippines Tel +63 2 8632 4444; Fax +63 2 8636 2444 www.adb.org Some rights reserved. Published in 2021. ISBN 978-92-9262-934-2 (print); 978-92-9262-935-9 (electronic); 978-92-9262-936-6 (ebook) Publication Stock No. TCS210239-2 DOI: http://dx.doi.org/10.22617/TCS210239-2 The views expressed in this publication are those of the authors and do not necessarily reflect the views and policies of the Asian Development Bank (ADB) or its Board of Governors or the governments they represent. ADB does not guarantee the accuracy of the data included in this publication and accepts no responsibility for any consequence of their use. The mention of specific companies or products of manufacturers does not imply that they are endorsed or recommended by ADB in preference to others of a similar nature that are not mentioned. By making any designation of or reference to a particular territory or geographic area, or by using the term “country” in this document, ADB does not intend to make any judgments as to the legal or other status of any territory or area. This work is available under the Creative Commons Attribution 3.0 IGO license (CC BY 3.0 IGO) https://creativecommons.org/licenses/by/3.0/igo/. -
Kunming Qingshuihai Water Supply Project
Resettlement Plan Project Number: 40052 November 2007 PRC: Kunming Qingshuihai Water Supply Project Prepared by Kunming Municipal Government This report has been submitted to ADB by the Kunming Project Management Office and is made publicly available in accordance with ADB’s Public Communications Policy (2011). It does not necessarily reflect the views of ADB. Your attention is directed to the “Terms of Use” section of this website. Resettlement Planning Document Resettlement Plan Document Stage: Final Project Number: 40052 November 2007 PRC: Kunming Qingshuihai Water Supply Project Prepared by the Kunming Municipal Government. The resettlement plan is a document of the borrower. The views expressed herein do not necessarily represent those of ADB’s Board of Directors, Management, or staff, and may be preliminary in nature. ADB-Financed Kunming Qingshuihai Water Supply Project (KQWSP) RESETTLEMENT PLAN KQWSP Project Management Office (KPMO) Kunming Water Supply Group Co., Ltd. (KWSG) Yunnan Water Resources and Hydropower Survey, Design and Research Institute (YDRI) 12 July 2007 Table of Contents Executive Summary i A. Background i B. Impact of Land Acquisition and House Demolition i C. Policy and Legal Framework ii D. Compensation Standard, Income and Livelihood Restoration Scheme ii E. Institutional Resettlement iii F. Negotiation, Complaint, Grievance and Information Disclosure iv G. Monitoring and Evaluation iv H. Budget iv I. PROFILE OF THE PROJECT 1 A. Background 1 B. Brief Introduction 1 II. PROJECT IMPACT AND SOCIAL AND ECONOMIC PROFILE 8 A. Measures to Avoid or Minimize Land Acquisition and House Demolition 8 B. Range of Survey for Land Acquisition and House Demolition Impacts 11 C. -
Effects of Atmospheric CO2 Consumption on Rock Weathering in the Pearl River Basin, China
E3S Web of Conferences 98, 06011 (2019) https://doi.org/10.1051/e3sconf/20199806011 WRI-16 Effects of atmospheric CO2 consumption on rock weathering in the Pearl River basin, China Xiaoqun Qin1,*, Zhongcheng Jiang1, Liankai Zhang1, Qibo Huang1, and Pengyu Liu1 1Institute of Karst Geology, ChineseAcademy of Geological Sciences, Guilin 541004, China Abstract: Atmospheric CO2 is absorbed and dissolved in water via karst processes not only in carbonate rock areas, but in all rock areas of the earth. The chemical and isotopic analysis results, particularly of strontium, for water samples collected from eleven stations along the Pearl River, four times over the course of one year, showed that due to weathering by - 2+ 2+ carbonate or silicate rocks, HCO3 , Ca , and Mg have become the main ions in the river water. Through river ion stoichiometric and flux calculations, the carbonate rock weathering rate and atmospheric CO2 consumption were found to be 27.6 mm/ka and 540 x 103 mol/km2.a, which are 10.8 and 6.7 times the corresponding values for silicate rock. With the beneficial climatic conditions for rock erosion and large areas of carbonate rock in the Pearl River Basin, the atmospheric CO2 consumption value is about 2.6 times the average value for the 60 major rivers in the world. 1 Introduction Rock weathering is a universal, and one of the most influential, geological processes that occurs on the earth’s surface. Atmospheric CO2 is an important driving force for the karst geological processes [1]. Atmospheric CO2 can be removed by chemical weathering of rocks and produce huge carbon sinks, thereby reducing atmospheric CO2. -
Inland Fisheries Resource Enhancement and Conservation in Asia Xi RAP PUBLICATION 2010/22
RAP PUBLICATION 2010/22 Inland fisheries resource enhancement and conservation in Asia xi RAP PUBLICATION 2010/22 INLAND FISHERIES RESOURCE ENHANCEMENT AND CONSERVATION IN ASIA Edited by Miao Weimin Sena De Silva Brian Davy FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS REGIONAL OFFICE FOR ASIA AND THE PACIFIC Bangkok, 2010 i The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. ISBN 978-92-5-106751-2 All rights reserved. Reproduction and dissemination of material in this information product for educational or other non-commercial purposes are authorized without any prior written permission from the copyright holders provided the source is fully acknowledged. Reproduction of material in this information product for resale or other commercial purposes is prohibited without written permission of the copyright holders. Applications for such permission should be addressed to: Chief Electronic Publishing Policy and Support Branch Communication Division FAO Viale delle Terme di Caracalla, 00153 Rome, Italy or by e-mail to: [email protected] © FAO 2010 For copies please write to: Aquaculture Officer FAO Regional Office for Asia and the Pacific Maliwan Mansion, 39 Phra Athit Road Bangkok 10200 THAILAND Tel: (+66) 2 697 4119 Fax: (+66) 2 697 4445 E-mail: [email protected] For bibliographic purposes, please reference this publication as: Miao W., Silva S.D., Davy B. -
Coal, Water, and Grasslands in the Three Norths
Coal, Water, and Grasslands in the Three Norths August 2019 The Deutsche Gesellschaft für Internationale Zusammenarbeit (GIZ) GmbH a non-profit, federally owned enterprise, implementing international cooperation projects and measures in the field of sustainable development on behalf of the German Government, as well as other national and international clients. The German Energy Transition Expertise for China Project, which is funded and commissioned by the German Federal Ministry for Economic Affairs and Energy (BMWi), supports the sustainable development of the Chinese energy sector by transferring knowledge and experiences of German energy transition (Energiewende) experts to its partner organisation in China: the China National Renewable Energy Centre (CNREC), a Chinese think tank for advising the National Energy Administration (NEA) on renewable energy policies and the general process of energy transition. CNREC is a part of Energy Research Institute (ERI) of National Development and Reform Commission (NDRC). Contact: Anders Hove Deutsche Gesellschaft für Internationale Zusammenarbeit (GIZ) GmbH China Tayuan Diplomatic Office Building 1-15-1 No. 14, Liangmahe Nanlu, Chaoyang District Beijing 100600 PRC [email protected] www.giz.de/china Table of Contents Executive summary 1 1. The Three Norths region features high water-stress, high coal use, and abundant grasslands 3 1.1 The Three Norths is China’s main base for coal production, coal power and coal chemicals 3 1.2 The Three Norths faces high water stress 6 1.3 Water consumption of the coal industry and irrigation of grassland relatively low 7 1.4 Grassland area and productivity showed several trends during 1980-2015 9 2. -
Teleconnection Analysis of Runoff and Soil Moisture Over the Pearl River Basin in Southern China
Open Access Hydrol. Earth Syst. Sci., 18, 1475–1492, 2014 Hydrology and www.hydrol-earth-syst-sci.net/18/1475/2014/ doi:10.5194/hess-18-1475-2014 Earth System © Author(s) 2014. CC Attribution 3.0 License. Sciences Teleconnection analysis of runoff and soil moisture over the Pearl River basin in southern China J. Niu1, J. Chen1, and B. Sivakumar2,3 1Department of Civil Engineering, The University of Hong Kong, Pokfulam, Hong Kong, China 2School of Civil and Environmental Engineering, The University of New South Wales, Sydney, NSW 2052, Australia 3Department of Land, Air and Water Resources, University of California, Davis, CA 95616, USA Correspondence to: J. Chen ([email protected]) Received: 26 July 2013 – Published in Hydrol. Earth Syst. Sci. Discuss.: 30 September 2013 Revised: 6 February 2014 – Accepted: 7 March 2014 – Published: 23 April 2014 Abstract. This study explores the teleconnection of two cli- precipitation. Therefore, an important step in the assessment matic patterns, namely the El Niño–Southern Oscillation and prediction of floods or droughts is to understand the re- (ENSO) and the Indian Ocean Dipole (IOD), with hydrolog- lationships between the key hydrological variables (e.g., pre- ical processes over the Pearl River basin in southern China, cipitation, runoff, soil moisture) and climate patterns. particularly on a sub-basin-scale basis. The Variable Infil- Generally speaking, observations of hydrological vari- tration Capacity (VIC) model is used to simulate the daily ables over large-scale basins are scarce, except for precip- hydrological processes over the basin for the study period itation. For instance, even though streamflow gauging sta- 1952–2000, and then, using the simulation results, the time tions currently exist along most large rivers around the world, series of the monthly runoff and soil moisture anomalies for long-term flow observations are still not available, especially its ten sub-basins are aggregated. -
Family Cyprinidae Subfamily Labeoninae
SUBFAMILY Labeoninae Bleeker, 1859 - labeonins, labeos, algae-eaters, carps etc. [=?Paeonomiae, ?Apalopterinae, Platycarinae, Temnochilae, Labeonini, ?Plalacrognathini, Garrae, Gymnostomi, Rohteichthyina, Discognathina, Parapsilorhynchidae, Banganina, Osteochilina, Semilabeoina] Notes: Name in prevailing recent practice ?Paeonomiae McClelland, 1838:943 [ref. 2924] (subfamily) ? Cirrhinus [corrected to Paeonominae by McClelland 1839:225, 261, 264 [ref. 2923]; no stem of the type genus, not available, Article 11.7.1.1] ?Apalopterinae McClelland, 1839:226, 261, 299 [ref. 2923] (subfamily) ? Platycara [no stem of the type genus, not available, Article 11.7.1.1] Platycarinae Macleay, 1841:271 [ref. 32498] (family) Platycara [also Macleay 1842:204 [ref. 32499]] Temnochilae Heckel, 1847:280, 281 [ref. 2068] (Abtheilung) ? Labeo [no stem of the type genus, not available, Article 11.7.1.1] Labeonini Bleeker, 1859d:XXVIII [ref. 371] (stirps) Labeo [family-group name used as valid by: Rainboth 1991 [ref. 32596], Nelson 1994 [ref. 26204], Yue et al. 2000 [ref. 25272], Zhang & Chen 2004 [ref. 27930], Li, Ran & Chen 2006 [ref. 29057], Nelson 2006 [ref. 32486], Zhang & Kottelat 2006 [ref. 28711], Zhang, Qiang & Lan 2008 [ref. 29452], Yang & Mayden 2010, Zheng, Yang, Chen & Wang 2010 [ref. 30961], Zhu, Zhang, Zhang & Han 2011 [ref. 31305], Yang et al. 2012a, Yang et al. 2012b [ref. 32362]] ?Phalacrognathini Bleeker, 1860a:422 [ref. 370] (cohors) ? Labeo [no stem of the type genus, not available, Article 11.7.1.1] Garrae Bleeker, 1863–64:24 [ref. 4859] (phalanx) Garra [also Bleeker 1863b:191 [ref. 397]; stem Garr- confirmed by Smith 1945:259 [ref. 4056], by Cavender & Coburn in Mayden 1992:322 [ref. 23260], by Mirza 2000:356 [ref. -
Total 1 / 2 3 / 4 5 / 6 96 100 ANDERSON JUNIOR COLLEGE JC2 H2 Geography Preliminary Examinations (2017)
ANDERSON JUNIOR COLLEGE JC2 H2 Geography Preliminary Examinations (2017) H2 GEOGRAPHY 9751/01 Paper 1 Structured Essay Questions 15 September 2017 3 hours Additional Materials: Writing Paper World outline map READ THESE INSTRUCTIONS FIRST Write your name and class in the spaces provided below, and on the work you hand in. Write in dark blue or black pen on both sides of the paper. You may use an HB pencil for any diagrams or graphs. Do not use staples, paper clips, highlighters, glue or correction fluid. Answer three questions. One from each section. You should make reference to appropriate examples studied in the field or the classroom, even where such examples are not specifically requested by the question. Diagrams and sketch maps should be drawn whenever they serve to illustrate an answer. The world outline map may be annotated and handed in with relevant answers. You are reminded of the need for good English and clear presentation in your answers. At the end of the examination, fasten all your work securely together. The number of marks is given in brackets [ ] at the end of each question or part question. Name: PDG: Section A Section B Section C Please circle the no. of the attempted question. Total 1 / 2 3 / 4 5 / 6 32 32 32 96 Percentage 100 This question paper consists of 3 printed pages. [Turn Over] 2 Section A - Tropical Environments Answer one question from this section. 1 (a) Explain the differences in the characteristics of the five main tropical climatic zones in the Köppen-Geiger climate classification system. -
Molecular Phylogeny and Biogeography of Percocypris (Cyprinidae, Teleostei)
Molecular Phylogeny and Biogeography of Percocypris (Cyprinidae, Teleostei) Mo Wang1,2, Jun-Xing Yang1*, Xiao-Yong Chen1* 1 State Key Laboratory of Genetic Resources and Evolution, Kunming Institute of Zoology, Chinese Academy of Sciences, Kunming, Yunnan, China, 2 University of Chinese Academy of Sciences, Beijing, China Abstract Fierce predatory freshwater fishes, the species of Percocypris (Cyprinidae, Teleostei) inhabit large rivers or lakes, and have a specific distribution pattern. Only a single species or subspecies occurs in each large-scale drainage basin of the Southeastern Tibetan Plateau. In this study, the molecular phylogenetic relationships for all but one of the described subspecies/species of Percocypris were investigated based on three mitochondrial genes (16S; COI; Cyt b) and one nuclear marker (Rag2). The results of Maximum Likelihood and Bayesian Inference analyses show that Percocypris is a strongly supported monophyletic group and that it is the sister group of Schizothorax. Combined with analyses of morphological characters, our results suggest that Percocypris needs to be reclassified, and we propose that six species be recognized, with corresponding distributions in five main drainages (including one lake). In addition, based on the results of the estimation of divergence times and ancestral drainages, we hypothesize that Percocypris likely originated in the early Miocene from a paleo-connected drainage system containing the contemporary main drainages of the Southeastern Tibetan Plateau. This study suggests that vicariance (due to the uplift of the Tibetan Plateau modifying the large-scale morphologies of drainage basins in the Southeastern Tibetan Plateau) has played an important role in the speciation of the genus. Furthermore, external morphological characters (such as the length of the fins) and an internal trait (the position of pterygiophore) appear to be correlated with different habitats in rivers and the lake.