Ecological Impact of Large-Scale Water Transfer Project

Total Page:16

File Type:pdf, Size:1020Kb

Ecological Impact of Large-Scale Water Transfer Project Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Hydrol. Earth Syst. Sci. Discuss., 8, 10465–10500, 2011 Hydrology and www.hydrol-earth-syst-sci-discuss.net/8/10465/2011/ Earth System HESSD doi:10.5194/hessd-8-10465-2011 Sciences © Author(s) 2011. CC Attribution 3.0 License. Discussions 8, 10465–10500, 2011 This discussion paper is/has been under review for the journal Hydrology and Earth System Ecological impact of Sciences (HESS). Please refer to the corresponding final paper in HESS if available. large-scale water transfer project Quantitative analysis on the ecological D. H. Yan et al. impact of large-scale water transfer project on water resource area in a Title Page changing environment Abstract Introduction Conclusions References D. H. Yan1,2, H. Wang1,2, H. H. Li1,2, G. Wang1,2, T. L. Qin1,2,3, D. Y. Wang1,2,3, and Tables Figures L. H. Wang1,2,4 1 State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, J I China Institute of Water Resources and Hydropower Research, Beijing, 100038, China 2Water Resources Department, China Institute of Water Resources and Hydropower J I Research, Beijing, 100038, China Back Close 3Environmental Science and Engineering Department, Donghua University, Shanghai, 201620, China Full Screen / Esc 4School of Hydraulic Engineering, Dalian University of Technolgoy, Dalian, 116023, China Received: 19 October 2011 – Accepted: 9 November 2011 – Published: 30 November 2011 Printer-friendly Version Correspondence to: G. Wang ([email protected]) Interactive Discussion Published by Copernicus Publications on behalf of the European Geosciences Union. 10465 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract HESSD The interbasin long-distance water transfer project is a key support for the reasonable allocation of water resources in a large-scale area, which can optimize the spatiotem- 8, 10465–10500, 2011 poral change of water resources to reinforce the guarantee of the access of water re- 5 sources. And large-scale water transfer projects have a deep influence on ecosystems; Ecological impact of besides, global climate change causes the uncertainty and additive effect of the eco- large-scale water logical impact of water transfer projects. Therefore, how to assess the ecological and transfer project environmental impact of large-scale water transfer projects in both construction and operation has triggered a lot of attention. The water-output area of the western route of D. H. Yan et al. 10 China’s South-North Water Transfer Project was taken as the study area of the present article. According to relevant evaluation principles and on the basis of background analysis on the eco-environment of the study area, the influence factors were identi- Title Page fied and evaluation indexes were established. The climate-hydrology-ecology coupled Abstract Introduction simulation model was used to imitate the laws of ecological and environmental change 15 of the water resource area in a changing climate. The emphasis of influence analy- Conclusions References sis and quantitative evaluation was placed on the reservoir construction and operation Tables Figures scheduling, representative river corridors and wetlands, natural reserves and the wa- ter environment of river basins below the dam sites. In the end, an overall influence evaluation of the impact of the project on the water circulation and ecological evolution J I 20 of the water resource area was conducted. The research results were as follows: the J I environmental impacts of the western route project in the water resource area were concentrated on two aspects, i.e. the permanent destruction of vegetation during the Back Close phase of dam construction and river impoundment, and the significant influence on the Full Screen / Esc hydrological situation of natural river corridor after the implementation of water transfer. 25 Its impact on local climate, vegetation ecology, typical wetlands, natural reserves and Printer-friendly Version the water environment of river basins below the dam sites was small. Interactive Discussion 10466 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | 1 Introduction HESSD With the increase of the world’s population, the rapid development of agriculture and industry and the increasing urbanization, the uneven spatiotemporal distribution of wa- 8, 10465–10500, 2011 ter resource and its quality deteriorate. To cope with the serious limitation of water 5 resource to economic development, many countries have undertaken water transfer Ecological impact of projects. From 1940 to 1980, the world witnessed the peak period of the construc- large-scale water tion of large-scale long-distance interbasin water transfer projects (Yang, 2003; Wang, transfer project 2009). After 1980, with the uprising consciousness of environmental protection, people became cautious of the construction of water transfer projects and a series of reports D. H. Yan et al. 10 concerning the negative ecological impacts of both construction and operation of these projects (Davies et al., 1992; Meador, 1992; Nardini, 1997) came out. Since then, countries all over the world began to conduct ecological influence evaluation on water Title Page transfer projects, and carry out thorough researches on environmental problems and Abstract Introduction ecological influence caused by those projects (Graf, 2006; Morais, 2008; Braatne et 15 al., 2008; Kittinger et al., 2009; Baran and Myschowoda, 2009; Growns et al., 2009; Conclusions References Wu et al., 2010; Olden and Naiman, 2010). At the same time, laws and regulations Tables Figures specialized in the construction and the operation of water transfer projects were pub- lished so as to mitigate and even prevent the ecological and environmental problems (Yang, 2003; Wang, 2009). Besides, studies on evaluation of ecological and environ- J I 20 mental influence of water transfer projects have gradually developed into an important J I field (Doledec, 1996; Bombino et al., 2006; Shah and Kumar, 2008). Meanwhile, ac- companied by the aggravation of the global climate change, the evaluation concerning Back Close the ecological influence of the water transfer project in a changing environment has Full Screen / Esc become increasingly valued, and a few studies in this field were carried out (Zeilhofer 25 and Moura, 2009; Olden and Naiman, 2010; Doll and Zhang, 2010; Moiwo et al., 2010; Printer-friendly Version Pittock and Finlayson, 2011). Oversize water transfer projects, especially those which cross rivers and are of long Interactive Discussion distance, are all huge systematic projects. They have a large span of space and time 10467 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | and therefore impose a broad array of impacts on the ecosystems of a river basin (Petts, 1984; Casado et al., 1989; Poff et al., 1997; Rosenberg et al., 1997; Friedl HESSD and Wuest,¨ 2002; Brismar, 2004; Burke et al., 2009). What’s more, the environmental 8, 10465–10500, 2011 and ecological influence of project under the background of global climate change is 5 extremely complex, thus there is considerable uncertainty. Present relevant studies are short of global, comprehensive and systematic research as they are focused on a Ecological impact of certain aspect of the ecological influence, such as the hydrological situation, pollutant large-scale water transport patterns and biodiversity (Morais, 2008; Hu et al., 2008; Koutsos et al., 2010; transfer project Ouyang et al., 2011), or they are targeted at a certain area, such as the water-output D. H. Yan et al. 10 area, water-intake area and the river delta (Xu et al., 2011; Ligon et al., 2011; Restrepo and Cantera, 2011). And the climate change aspect has been inadequately treated in the environmental impact assessment of large water transfer projects. Judging from the Title Page experiences of existing water transfer projects, the estimation of their impact on ecology and environment is insufficient, and the negative influence of projects in the phase of Abstract Introduction 15 operation is becoming increasingly significant. The western route of China’s South- North Water Transfer Project (SNWTP) locates its water-output area in the Qinghai- Conclusions References Tibet Plateau, which is the sensitive area of global climate change. Therefore, studies Tables Figures of the ecological influence evaluation of this area are of great importance and have triggered a lot of concerns (Yang et al., 2002; Berkoff, 2003; Ghassemi and White, J I 20 2006). In the present article, some explorations of the evaluation of the ecological influence J I of the western route project on its water-output area in a changing climate are con- Back Close ducted. This study aims to contributing to show how, and to what extent, the western route project of SNWTP will impact on ecology and environment in water resource area Full Screen / Esc 25 and regions related to water transfer. The specific objectives of this paper are to (1) evaluate the influence of the reservoir construction on the local climate of the water Printer-friendly Version resource area; (2) evaluate the influence of water transfer on the hydrological situation of typical water-reduction river reaches; (3) evaluate the influence of water transfer on Interactive Discussion typical wetlands and natural reserves; and (4) evaluate the influence of water transfer 10468 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | on water environment below the dam sites. The quantitative assessment of the four aspects above are based upon a simulation and forecast platform which will be intro- HESSD duced in Sect. 2.5. However, for saving space, the assessment results other than the 8, 10465–10500, 2011 model itself are focused on in this article. Ecological impact of 5 2 Materials and methods large-scale water transfer project 2.1 Study area D. H. Yan et al. The first-stage of western route project of SNWTP is located at the southeast edge of the Qinghai-Tibet Plateau, with the geographic coordinates of Latitude 99◦200– ◦ 0 ◦ 0 ◦ 0 102 10 E and Longitude 31 30 –33 20 N.
Recommended publications
  • Triplophysa Pseudostenura, a New Nemacheiline Loach (Cypriniformes: Balitoridae) from the Yalong River of China
    Zootaxa 3586: 272–280 (2012) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ ZOOTAXA Copyright © 2012 · Magnolia Press Article ISSN 1175-5334 (online edition) urn:lsid:zoobank.org:pub:06C92974-A6A3-4D2F-97CC-2D3CA362B41F Triplophysa pseudostenura, a new nemacheiline loach (Cypriniformes: Balitoridae) from the Yalong River of China CHUNLIN HE1,2, E ZHANG2 & ZHAOBIN SONG1,3,4 1Sichuan Key Laboratory of Conservation Biology on Endangered Wildlife, College of Life Sciences, Sichuan University, Chengdu 610065 P. R. China 2Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan 430072 P. R. China 3Key Laboratory of Bio-Resources and Eco-Environment of Ministry of Education, College of Life Sciences, Sichuan University, Chengdu 610065 P. R. China 4Corresponding author. E-mail: [email protected] Abstract A new species of nemacheiline loach, Triplophysa pseudostenura, is described from the Yalong River, a tributary of the upper Yangtze River drainage in China. Previous collectors misidentified the species as T. stenura. Triplophysa pseudostenura can be separated from T. stenura and other valid species of Triplophysa by the following combination of characters: body smooth and without scales; head tapering; lips thin and smooth; trunk and caudal peduncle slender, laterally compressed; depth of caudal peduncle tapering posteroventrally approaching caudal fin; posterior chamber of gas bladder reduced or absent; intestine short, forming a zigzag loop posterior to bottom of ‘U’-shaped stomach; insertion of pelvic fins anterior to dorsal-fin origin; caudal fin deeply concave. Key words: Teleost, new species, Upper Yangtze River, fish Introduction The genus Triplophysa is a species-rich group in the subfamily Nemacheilinae, and is currently hypothesized to have 126 species, 108 of which are thus far known from China (He 2008; He et al.
    [Show full text]
  • Download Article
    Advances in Social Science, Education and Humanities Research, volume 40 3rd International Conference on Education, Language, Art and Inter-cultural Communication (ICELAIC 2016) Huoer of Tibetan Culture and Its Application in Landscape Architecture Miao Tan Qing Wu Sichuan Agricultural University Sichuan Agricultural University Chengdu, China Chengdu, China Ai Cheng Xiao-Min Chen Sichuan Agricultural University Sichuan Agricultural University Chengdu, China Chengdu, China Yi-Mei Feng Xiao-Fang Yu* Sichuan Agricultural University Sichuan Agricultural University Chengdu, China Chengdu, China Abstract—Huoer culture, which is located in “Huoer Zhang the process of planning and design, the author gives an insight valley” of Western Sichuan Plateau that is the ancient Tibetan into the local Huoer cultural and integrates it into landscape and Yi corridor, has a history of thousands of years. But it has design. He hopes to be able to explore new train of the disappeared in the vast history since ancient time nearest to the traditional regional culture element thought on the exploration, present, no one to ask. The author had the opportunity to development and protection. participate in the planning and design of "Huoer Zhang valley wetland park”, thus to understand the ancient mysterious and of long standing culture. The paper, combined with the experience II. THE SOURCE OF “HUOER” AND “HUOER CULTURE” of the author, by looking up a large number of ancient books and records, knowing the local scholars oral and going on some field A. The Brief Introduction of Huoer research, attempts to make generalizations of the Huoer culture. The Ganzi, Luhuo and Daofu country area, which belong to the north of Kang said by traditional Tibetan, is located in the Keywords—Huoer culture; Huoer Zhang valley; landscape core area of Ganzi Tibetan autonomous prefecture in Sichuan architecture province.
    [Show full text]
  • GIS Based Analysis of Traffic Routes and Geological Division of Qinghai-Tibetan In
    2018 International Conference on Advanced Chemical Engineering and Environmental Sustainability (ICACEES 2018) ISBN: 978-1-60595-571-1 GIS Based Analysis of Traffic Routes and Geological Division of Qinghai-Tibetan in Prehistoric Period Changjun Xu, Yan Zhu and Ying Wang ABSTRACT The environment of Qinghai-Tibet Plateau is Harsh, but it is not a restricted area for life. The obviously evidence suggests that humans have expanded to the plateau area at the time of the last deglacial. Through long-term practice, the more stable pattern of traffic is formed. Through the construction of natural factor simulation - site distribution correction method, using GIS to obtain the traffic simulation results of Qinghai-Tibet Plateau in the prehistoric period, combined with archaeological evidence to confirm the simulation routes. Plateau is divided into four districts based on the simulation results, namely: northeast area, southeast area, southwest area and northwest area without man. The routes site density of the northeast area is high. And the number of sites falling into the routes accounted for 88.56% of the total number of sites in this area. The earliest routes were formed during the paleolithic period. The direction of the routes is east-west direction. The routes closely link to the internal of northeast area and link to out of the Loess Plateau and the northern 1area of China. The formation and development of the routes laid the foundation for the spread of pottery, wheat, millet and the formation of the Silk Road. The direction of routes is north-south direction in the southeast area. The northern part of the route connects the upper of the Yellow River area.
    [Show full text]
  • Quantitative Analysis on the Environmental Impact of Large-Scale Water Transfer Project on Water Resource Area in a Changing Environment
    Hydrol. Earth Syst. Sci., 16, 2685–2702, 2012 www.hydrol-earth-syst-sci.net/16/2685/2012/ Hydrology and doi:10.5194/hess-16-2685-2012 Earth System © Author(s) 2012. CC Attribution 3.0 License. Sciences Quantitative analysis on the environmental impact of large-scale water transfer project on water resource area in a changing environment D. H. Yan1,2, H. Wang1,2, H. H. Li1,2, G. Wang1,2, T. L. Qin1,2,3, D. Y. Wang1,2,3, and L. H. Wang1,2,4 1State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing, 100038, China 2Water Resources Department, China Institute of Water Resources and Hydropower Research, Beijing, 100038, China 3Environmental Science and Engineering Department, Donghua University, Shanghai, 201620, China 4School of Hydraulic Engineering, Dalian University of Technology, Dalian, 116023, China Correspondence to: G. Wang ([email protected]) Received: 19 October 2011 – Published in Hydrol. Earth Syst. Sci. Discuss.: 30 November 2011 Revised: 6 July 2012 – Accepted: 10 July 2012 – Published: 13 August 2012 Abstract. The interbasin long-distance water transfer project the phase of dam construction and river impoundment, and is key support for the reasonable allocation of water re- the significant influence on the hydrological situation of nat- sources in a large-scale area, which can optimize the spatio- ural river corridor after the implementation of water extrac- temporal change of water resources to secure the amount tion. The impact on local climate, vegetation ecology, typical of water available. Large-scale water transfer projects have wetlands, natural reserves and the water environment of river a deep influence on ecosystems; besides, global climate basins below the dam sites was small.
    [Show full text]
  • Important Notice
    IMPORTANT NOTICE THIS OFFERING IS AVAILABLE ONLY TO INVESTORS WHO ARE OUTSIDE THE UNITED STATES IN AN OFFSHORE TRANSACTION IN RELIANCE ON REGULATION S UNDER THE US SECURITIES ACT OF 1933, AS AMENDED (THE “SECURITIES ACT”). IMPORTANT: You must read the following disclaimer before continuing. The following disclaimer applies to the Prospectus following this page. You are advised to read this disclaimer carefully before accessing, reading or making any other use of the attached Prospectus. In accessing the Prospectus, you agree to be bound by the following terms and conditions, including any modifications to them from time to time, each time you receive any information from us as a result of such access. IF YOU DO NOT AGREE TO THE TERMS DESCRIBED IN THIS NOTICE, YOU MAY NOT READ, ACCESS OR OTHERWISE USE THE ATTACHED PROSPECTUS. THE OFFER GDRS HAVE NOT BEEN, AND WILL NOT BE, REGISTERED UNDER THE SECURITIES ACT OR THE SECURITIES LAWS OF ANY STATE OF THE UNITED STATES OR ANY OTHER JURISDICTION AND MAY NOT BE OFFERED OR SOLD WITHIN THE UNITED STATES, EXCEPT PURSUANT TO AN EXEMPTION FROM, OR IN A TRANSACTION NOT SUBJECT TO, THE REGISTRATION REQUIREMENTS OF THE SECURITIES ACT AND ANY APPLICABLE STATE OR LOCAL SECURITIES LAWS. YOU ARE NOT AUTHORISED TO AND MAY NOT FORWARD OR DELIVER THE ATTACHED PROSPECTUS, ELECTRONICALLY OR OTHERWISE, TO ANY OTHER PERSON OR REPRODUCE SUCH PROSPECTUS IN ANY MANNER WHATSOEVER. FAILURE TO COMPLY WITH THIS DIRECTIVE MAY RESULT IN A VIOLATION OF THE SECURITIES ACT OR THE APPLICABLE LAWS OF OTHER JURISDICTIONS. CONFIRMATION OF YOUR REPRESENTATION: You have been sent the attached Prospectus on the basis that you have confirmed that: (1) you are outside the United States, and, to the extent you purchase the securities described in the attached Prospectus, you will be doing so in an offshore transaction in reliance on Regulation S under the Securities Act; and (2) you consent to delivery of the attached Prospectus and any amendments or supplements thereto by electronic transmission.
    [Show full text]
  • Ecological and Social Vulnerability Issues in the Western Route of South to North Water Transfer Project
    2017 International Conference on Energy Development and Environmental Protection (EDEP 2017) ISBN: 978-1-60595-482-0 Ecological and Social Vulnerability Issues in the Western Route of South to North Water Transfer Project a b,* Yi LIN and Wen BAO Business School, Chengdu University of Information and Technology, Chengdu, P.R. China [email protected], [email protected] *Corresponding author Keywords: Western Route, North Water Transfer Project, Ecological vulnerability, Social vulnerability, Sustainable development. Abstract. Western Route of South to North Water Transfer Project (Western Route Project for short) is a major infrastructure project to solve the uneven spatial and temporal distribution of water resources in West China. The ambitious water transfer project will divert water from China's longest river, the Yangtze River, to Northwest China, where water shortage has become a bottleneck restricting sustainable development. After completion, the project will relieve water shortages in over six provinces in north and Northwest China, affecting about tens of million people. At the same time, it will bring many serious ecological and social problems in the project affected areas. 1. Introduction The Western Route Project goes from the upper reaches of Yangtze River (the Tongtian, Yalong and Dadu Rivers) near the Bayankala Mountain to into the upper reaches of the Yellow River. It aims to ultimately divert 17 billion m3 of fresh water annually from the Yangtze River to the arid Northwest and Central China provinces like Qinghai, Gansu, Shannxi, Shanxi Provinces, and the Ningxia Hui Autonomous Region and the Inner Mongolia Autonomous Region. At the same time, the Western Route Project is also expected to supply areas on both sides of the Yellow River with water and replenish the Black River and the Shiyang River with water to restore their ecological function.
    [Show full text]
  • A Preliminary Study on the Place-Name Relics of Kangba Luhuo Named by Ergong
    2020 3rd International Conference on Economy Development and Social Sciences Research (EDSSR 2020) A Preliminary Study on the Place-Name Relics of Kangba Luhuo Named by Ergong Xiangqiu Zhuoma, Luorong Qu Pi Sichuan Minzu College, China, Kangding, Sichuan, China Keywords: Luhuo place name, Ergong name, Ruins Abstract. Kangba Luhuo is the earliest and the only paleohuman activity area with primary strata, and it is the cultural center for the communication between south, agriculture and North and animal husbandry. Taking kangba Luhuo place-names as the research object, this paper traces the historical relics of Ergong language, in order to discuss that Kangba Luhuo is the central area of Ergong language. 1. Introduction Luhuo is located in Ganzi Tibetan Autonomous Prefecture, ganzi Prefecture in the north and central part of Sichuan Province. It is adjacent to Daofu County in the east, Ganzi County in the northwest, Xinlong County in the southwest, Seda County in the north, and Rangtang and Jinchuan counties in Aba Prefecture in the northeast. Line 317 of Sichuan and Tibet runs through the whole country from southeast to northwest. The Liaohuo county calendar is an important thoroughness to Tibet and the important town of tea and horse ancient road. Luhuo is the center of North Kang, traffic, is a semi - agricultural semi - pastoral area. Stove huo is on the river of fresh water. Xianshui River, a tributary of yalong River on the left bank, was named Xianshui river and Zhoujiang River in ancient times. It originated at the south foot of Bayankala Mountain in Dali County, Qinghai Province, and was named Niqu or Nike River in the north.
    [Show full text]
  • Oligocene-Early Miocene Topographic Relief Generation Of
    Oligocene-Early Miocene Topographic Relief Generation of Southeastern Tibet Triggered by Thrusting Cao Kai, Guocan Wang, Philippe Leloup, Gweltaz Mahéo, Yadong Xu, Pieter van der Beek, Anne Replumaz, Kexin Zhang To cite this version: Cao Kai, Guocan Wang, Philippe Leloup, Gweltaz Mahéo, Yadong Xu, et al.. Oligocene-Early Miocene Topographic Relief Generation of Southeastern Tibet Triggered by Thrusting. Tectonics, American Geophysical Union (AGU), 2019, 38 (1), pp.374 - 391. 10.1029/2017tc004832. hal-03080776 HAL Id: hal-03080776 https://hal.archives-ouvertes.fr/hal-03080776 Submitted on 19 Dec 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Oligocene-Early Miocene topographic relief generation of 2 southeastern Tibet triggered by thrusting 3 Kai Cao 1, 2*, Wang G. C. 1, 2, Leloup P.H. 3, Mahéo G. 3, 4 Xu Y. D. 4, 5, van der Beek P.A. 6, Replumaz A. 6, Zhang K. X. 4 5 1 School of Earth Sciences, Center for Global Tectonics, China University of 6 Geosciences, Wuhan 430074, China 7 2 State Key Laboratory of Geological Processes and Mineral Resources,
    [Show full text]
  • Quantitative Analysis on the Ecological Impact of Large-Scale Water Transfer Project on Water Resource Areachanging in Environment a D
    Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Hydrol. Earth Syst. Sci. Discuss., 8, 10465–10500, 2011 Hydrology and www.hydrol-earth-syst-sci-discuss.net/8/10465/2011/ Earth System doi:10.5194/hessd-8-10465-2011 Sciences © Author(s) 2011. CC Attribution 3.0 License. Discussions This discussion paper is/has been under review for the journal Hydrology and Earth System Sciences (HESS). Please refer to the corresponding final paper in HESS if available. Quantitative analysis on the ecological impact of large-scale water transfer project on water resource area in a changing environment D. H. Yan1,2, H. Wang1,2, H. H. Li1,2, G. Wang1,2, T. L. Qin1,2,3, D. Y. Wang1,2,3, and L. H. Wang1,2,4 1State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing, 100038, China 2Water Resources Department, China Institute of Water Resources and Hydropower Research, Beijing, 100038, China 3Environmental Science and Engineering Department, Donghua University, Shanghai, 201620, China 4School of Hydraulic Engineering, Dalian University of Technolgoy, Dalian, 116023, China Received: 19 October 2011 – Accepted: 9 November 2011 – Published: 30 November 2011 Correspondence to: G. Wang ([email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. 10465 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract The interbasin long-distance water transfer project is a key support for the reasonable allocation of water resources in a large-scale area, which can optimize the spatiotem- poral change of water resources to reinforce the guarantee of the access of water re- 5 sources.
    [Show full text]
  • Distribution Characteristics of Typical Geological Relics in the Western Sichuan Plateau
    Open Geosciences 2020; 12: 307–323 Research Article Qizhong Wang, Zhongquan Li*, Yuan Yin, Shuang Yang, Wei Long, Fang Lai, and Jinmiao Hu Distribution characteristics of typical geological relics in the Western Sichuan Plateau https://doi.org/10.1515/geo-2020-0104 protection and development of regional geological relics received November 11, 2019; accepted March 18, 2020 were put forward. Abstract: The Western Sichuan Plateau (WSP), located in Keywords: Western Sichuan Plateau, geological relics, the eastern margin of the Qinghai–Tibet Plateau, is the most genetic mechanism, distribution characteristics strongly deformed region of the continental crust in China. Frequent tectonic movements shape the unique topography and landform of the WSP and have also produced abundant geological heritage resources. Based on the existing geolo- 1 Introduction and regional gical heritage survey data in Sichuan Province, the nearest geologic setting index analysis method of employing a regional spatial point model was used to reveal the distribution rules and the The Western Sichuan Plateau (WSP) is located in the genetic mechanism of typical geological relics in the WSP for eastern section of the Hengduan Mountains, between the the first time. Results indicate that the formation and Qinghai–Tibet Plateau and the Sichuan Basin, and is a distribution of geological relics in the WSP are generally transitional zone between the first step and the second step. controlled by tectonic movement and supplemented by the It is adjacent to the Laji Mountains, Buerhanbuda comprehensive action of external forces such as flowing Mountains, Qilian Mountains, and the Qaidam Basin to water. Their distribution shows a condensed spatial distribu- the north; and is adjacent to the Yunnan–Guizhou Plateau tion pattern and extends along the strike of a fault zone and in the south, the northern Tibetan Plateau in the west, and river strike strip.
    [Show full text]
  • U-Th)/He Dating
    Journal of Earth Science, Vol. 31, No. 4, p. 735–742, August 2020 ISSN 1674-487X Printed in China https://doi.org/10.1007/s12583-020-1328-4 Cenozoic Uplift of the Central Yunnan Fragment, Southwestern China, Revealed by Apatite (U-Th)/He Dating Ke Wu , Youpu Dong *, Jiaxin Duan, Xin Ru, Dongyue Zhang, Dan Wang Faculty of Land Resource Engineering, Kunming University of Science and Technology, Kunming 650093, China Ke Wu: https://orcid.org/0000-0003-4915-242X; Youpu Dong: https://orcid.org/0000-0002-2829-7585 ABSTRACT: The age of central Yunnan fragment uplift has long been debated, with estimates ranging from the Late Eocene to about 1 Ma. To determine the central Yunnan fragment uplift time in the Ce- nozoic, apatite (U-Th)/He (AHe) was used to analyze the low-temperature thermochronology of samples from the Jiaozi Mountain area of the eastern central Yunnan fragment. The sampling area is located in the Dongchuan District of Kunming, Yunnan Province, near the Xiaojiang fault zone. The results show that AHe ages from the eastern part of central Yunnan fragment were mainly concentrated around 25.7–37.9 Ma, and intensive uplift had happened before 36.5 Ma. Together with previous low- temperature thermochronology research on the western and eastern central Yunnan fragment, we con- cluded that the Yunnan Plateau uplifted prior to 36.5 Ma, in a west to east sequence. The uplift caused a change in paleo-geographical terrain, which may have altered the ancient river systems of the south- east Tibetan Plateau. KEY WORDS: central Yunnan fragment, (U-Th)/He dating, uplift, Cenozoic.
    [Show full text]
  • Triplophysa Pseudostenura, a New Nemacheiline Loach (Cypriniformes: Balitoridae) from the Yalong River of China
    Zootaxa 3586: 272–280 (2012) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ ZOOTAXA Copyright © 2012 · Magnolia Press Article ISSN 1175-5334 (online edition) urn:lsid:zoobank.org:pub:06C92974-A6A3-4D2F-97CC-2D3CA362B41F Triplophysa pseudostenura, a new nemacheiline loach (Cypriniformes: Balitoridae) from the Yalong River of China CHUNLIN HE1,2, E ZHANG2 & ZHAOBIN SONG1,3,4 1Sichuan Key Laboratory of Conservation Biology on Endangered Wildlife, College of Life Sciences, Sichuan University, Chengdu 610065 P. R. China 2Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan 430072 P. R. China 3Key Laboratory of Bio-Resources and Eco-Environment of Ministry of Education, College of Life Sciences, Sichuan University, Chengdu 610065 P. R. China 4Corresponding author. E-mail: [email protected] Abstract A new species of nemacheiline loach, Triplophysa pseudostenura, is described from the Yalong River, a tributary of the upper Yangtze River drainage in China. Previous collectors misidentified the species as T. stenura. Triplophysa pseudostenura can be separated from T. stenura and other valid species of Triplophysa by the following combination of characters: body smooth and without scales; head tapering; lips thin and smooth; trunk and caudal peduncle slender, laterally compressed; depth of caudal peduncle tapering posteroventrally approaching caudal fin; posterior chamber of gas bladder reduced or absent; intestine short, forming a zigzag loop posterior to bottom of ‘U’-shaped stomach; insertion of pelvic fins anterior to dorsal-fin origin; caudal fin deeply concave. Key words: Teleost, new species, Upper Yangtze River, fish Introduction The genus Triplophysa is a species-rich group in the subfamily Nemacheilinae, and is currently hypothesized to have 126 species, 108 of which are thus far known from China (He 2008; He et al.
    [Show full text]