Initial Environmental Examination
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Chemical Weathering in the Upper Huang He (Yellow River) Draining the Eastern Qinghai-Tibet Plateau
Geochimica et Cosmochimica Acta, Vol. 69, No. 22, pp. 5279–5294, 2005 Copyright © 2005 Elsevier Ltd Printed in the USA. All rights reserved 0016-7037/05 $30.00 ϩ .00 doi:10.1016/j.gca.2005.07.001 Chemical weathering in the Upper Huang He (Yellow River) draining the eastern Qinghai-Tibet Plateau 1 1,2, 3 3 1 LINGLING WU, YOUNGSOOK HUH, *JIANHUA QIN, GU DU, and SUZAN VAN DER LEE 1Department of Geological Sciences, Northwestern University, 1850 Campus Drive, Evanston, Illinois 60208-2150 USA 2School of Earth and Environmental Sciences, Seoul National University, San 56-1, Sillim-dong, Gwanak-gu, Seoul 151-742, Korea 3Chengdu Institute of Geology and Mineral Resources, Chengdu, Sichuan 610082 P.R.C. (Received December 17, 2004; accepted in revised form July 5, 2005) Abstract—We examined the fluvial geochemistry of the Huang He (Yellow River) in its headwaters to determine natural chemical weathering rates on the northeastern Qinghai-Tibet Plateau, where anthropogenic impact is considered small. Qualitative treatment of the major element composition demonstrates the dominance of carbonate and evaporite dissolution. Most samples are supersaturated with respect to calcite, 87 86 dolomite, and atmospheric CO2 with moderate (0.710–0.715) Sr/ Sr ratios, while six out of 21 total samples have especially high concentrations of Na, Ca, Mg, Cl, and SO4 from weathering of evaporites. We used inversion model calculations to apportion the total dissolved cations to rain-, evaporite-, carbonate-, and silicate-origin. The samples are either carbonate- or evaporite-dominated, but the relative contributions of the ϫ 3 four sources vary widely among samples. -
Report on Domestic Animal Genetic Resources in China
Country Report for the Preparation of the First Report on the State of the World’s Animal Genetic Resources Report on Domestic Animal Genetic Resources in China June 2003 Beijing CONTENTS Executive Summary Biological diversity is the basis for the existence and development of human society and has aroused the increasing great attention of international society. In June 1992, more than 150 countries including China had jointly signed the "Pact of Biological Diversity". Domestic animal genetic resources are an important component of biological diversity, precious resources formed through long-term evolution, and also the closest and most direct part of relation with human beings. Therefore, in order to realize a sustainable, stable and high-efficient animal production, it is of great significance to meet even higher demand for animal and poultry product varieties and quality by human society, strengthen conservation, and effective, rational and sustainable utilization of animal and poultry genetic resources. The "Report on Domestic Animal Genetic Resources in China" (hereinafter referred to as the "Report") was compiled in accordance with the requirements of the "World Status of Animal Genetic Resource " compiled by the FAO. The Ministry of Agriculture" (MOA) has attached great importance to the compilation of the Report, organized nearly 20 experts from administrative, technical extension, research institutes and universities to participate in the compilation team. In 1999, the first meeting of the compilation staff members had been held in the National Animal Husbandry and Veterinary Service, discussed on the compilation outline and division of labor in the Report compilation, and smoothly fulfilled the tasks to each of the compilers. -
China: Xining Flood and Watershed Management Project
E2007 V4 Public Disclosure Authorized China: Xining Flood and Watershed Management Project Public Disclosure Authorized Environmental Assessment Summary Public Disclosure Authorized Environmental Science Research & Design Institute of Gansu Province October 1, 2008 Public Disclosure Authorized Content 1. Introduction .................................................................................................................................. 1 1.1 Project background............................................................................................................ 1 1.2 Basis of the EA.................................................................................................................. 3 1.3 Assessment methods and criteria ...................................................................................... 4 1.4 Contents of the report........................................................................................................ 5 2. Project Description....................................................................................................................... 6 2.1 Task................................................................................................................................... 6 2.2 Component and activities.................................................................................................. 6 2.3 Linked projects................................................................................................................ 14 2.4 Land requisition and resettlement -
Revised Draft Experiences with Inter Basin Water
REVISED DRAFT EXPERIENCES WITH INTER BASIN WATER TRANSFERS FOR IRRIGATION, DRAINAGE AND FLOOD MANAGEMENT ICID TASK FORCE ON INTER BASIN WATER TRANSFERS Edited by Jancy Vijayan and Bart Schultz August 2007 International Commission on Irrigation and Drainage (ICID) 48 Nyaya Marg, Chanakyapuri New Delhi 110 021 INDIA Tel: (91-11) 26116837; 26115679; 24679532; Fax: (91-11) 26115962 E-mail: [email protected] Website: http://www.icid.org 1 Foreword FOREWORD Inter Basin Water Transfers (IBWT) are in operation at a quite substantial scale, especially in several developed and emerging countries. In these countries and to a certain extent in some least developed countries there is a substantial interest to develop new IBWTs. IBWTs are being applied or developed not only for irrigated agriculture and hydropower, but also for municipal and industrial water supply, flood management, flow augmentation (increasing flow within a certain river reach or canal for a certain purpose), and in a few cases for navigation, mining, recreation, drainage, wildlife, pollution control, log transport, or estuary improvement. Debates on the pros and cons of such transfers are on going at National and International level. New ideas and concepts on the viabilities and constraints of IBWTs are being presented and deliberated in various fora. In light of this the Central Office of the International Commission on Irrigation and Drainage (ICID) has attempted a compilation covering the existing and proposed IBWT schemes all over the world, to the extent of data availability. The first version of the compilation was presented on the occasion of the 54th International Executive Council Meeting of ICID in Montpellier, France, 14 - 19 September 2003. -
Satellite-Derived Particulate Organic Carbon Flux in the Changjiang River Through Different Stages of the Three Gorges
Remote Sensing of Environment 223 (2019) 154–165 Contents lists available at ScienceDirect Remote Sensing of Environment journal homepage: www.elsevier.com/locate/rse Satellite-derived particulate organic carbon flux in the Changjiang River through different stages of the Three Gorges Dam T ⁎ Dong Liua,b, Yan Baib,e, , Xianqiang Heb,e, Delu Panb, Chen-Tung Arthur Chenc, Teng Lib,YiXud, Chaohai Gongd, Lin Zhangb a Key Laboratory of Watershed Geographic Sciences, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China b State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China c Department of Oceanography, National Sun Yat-sen University, Kaohsiung 80424, Taiwan d Lower Changjiang River Bureau of Hydrological and Water Resources Survey, Nanjing 210011, China e Institute of Oceanography, Shanghai Jiao Tong University, Shanghai 200240, China ARTICLE INFO ABSTRACT Keywords: As the largest Asian river and fourth world's largest river by water flow, the Changjiang River transports a Particulate organic carbon considerable amount of terrigenous particulate organic carbon (POC) into ocean, which has experienced sig- Changjiang River nificant pressure from human activities. We conducted monthly sampling (from May 2015 to May 2016) at Three Gorges Dam Datong, the most downstream non-tidal hydrological station along the Changjiang River. To monitor long-term Landsat data POC variations, we developed a two-step POC algorithm for Landsat satellite data and calculated monthly POC Bio-optical model flux during 2000–2016. Monthly POC flux ranged from a minimum of 1.4 × 104 t C in February 2016 to a maximum of 52.04 × 104 t C in May 2002, with a mean of 13.04 × 104 t C/month. -
Quaternary Glaciation of the Bailang River Valley, Qilian Shan
http://www.paper.edu.cn Quaternary International 97–98 (2002) 103–110 Quaternary glaciation of the Bailang River Valley, Qilian Shan Shangzhe Zhou*, Jijun Li, Shiqiang Zhang Department of Geography, Lanzhou University, Lanzhou 730000, People’s Republic of China Abstract The Qilian Shan, on the Northeast margin of the Qinghai–Tibetan Plateau, is weakly influenced by the Asian monsoon. Until recently, the Quaternary glacial geology of this region has been poorly understood. This paper describes a sequence of Quaternary glacial deposits in the upper reaches of the Bailang River. Using electron spin resonance (ESR), thermoluminescence (TL) and radiocarbon dating, tills, loess, buried soils and landforms were dated. The oldest till was dated B463 ka BP by ESR. A younger till and its outwash terrace were dated to B135 and 130 ka BP. The loess on this outwash terrace was dated to 141.7711.4 ka BP at its base and 43.773.5 ka BP in its central part by TL dating. A buried soil on a younger till was dated at 6920778 ka BP using 14C. The glacial landforms and these dating results show that glacial advances occurred during the Little Ice Age, the Neoglacial, MIS2–4, MIS6, and MIS12. Glaciation during MIS12 implies that the Qilian Mountains were rising coevally with the Qinghai–Tibetan Plateau, and were probably at a sufficient elevation for glaciation since at least 463 ka BP. r 2002 Elsevier Science Ltd and INQUA. All rights reserved. 1. Introduction were unable to date each advance. Recently, we have applied modern dating techniques to define the timing of The Qilian Shan (Shan=Mountains), lying between glaciations in a succession of well-preserved sediments Gansu and Qinghai Provinces of China, is an impressive and landforms along the Bailang River. -
Feasibility of Coal Hydrogasification Technology in China
0? ^ ^ ~~ null tit WU2^3B lt±) M-r s ®f£5fe (tt) ## fNfc VfiK 12^3 M 221 1 #*, wmicm&i-a c & t < @* lx, e@mao^mic#i& i"5 «T##&#'i-5?K7k*Wn#%'(kK#<D#a:&##g%t lx, rro SfflIt& W«1" 5 ±X&5 & tfc£@3-tt ic MX 5 P$9F% & 5 * ^s|+iE t L XfTtcXV'6. ¥/$ ll ¥Sic*5V'Xi4. =piaic*5 it531^/v^-E^fl.iiLt^nfSM A, #&#)##&#& Ltc0 Lxfs%K###%mi% • Kit *##-#*, ^©fiScS^Sf? StfcfctOXfeSo The Feasibility of Coal Hydrogasification Technology in China Final Report Beijing Research Institute of Coal Chemistry China Coal Research Institute December 1999 Content I Outline of Natural Gas in China 1. Present Status and Development of Natural Gas Resources in China 1.1 Natural Gas Resources and Their Distribution in China........................................... 1 1.2 Present Pipeline and Conveyance of Natural Gas...............................* ..................... 8 1.3 Construction and Development Plan for Natural Gas........................* ..................... 9 1.4 Importation of Natural Gas and LNG and Future Plans........................................ 12 1.5 General Conditions Status of Coalbed Methane............................................... ° *' * 18 2. Present Status of Town Gas for Major Chinese Cities 2.1 General Status of Supply and Demand of Town Gas in Chinese Cities.................. 20 2.2 General Status of Supply and Demand of Fuel Gas in Major Chinese Cities......... 22 2.3 Reorganization, Present Status and Plan for Construction ...................................... 24 of Fuel Gas Facilities in Major Chinese Cities 2.4 Present Status and Related Developing Plan using Natural Gas as Fuel Gas * " * * 33 2.5 Production, Present Status of Supply and Outlook * .................................................36 for Liquid Petroleum Gas (LPG) 3. -
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. -
Policy Note on Integrated Flood Risk Management Key Lesson Learned and Recommendations for China
Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized Strategy Resources Partnership China CountryWater WATER PARTNERSHIP PROGRAM PARTNERSHIP WATER THE WORLDBANK (2013-2020) China Country Water Resources Partnership Strategy © 2013 The World Bank 1818 H Street NW Washington DC 20433 Telephone: 202-473-1000 Internet: www.worldbank.org This work is a product of the staff of The World Bank with external contributions. The findings, interpretations, and conclusions expressed in this work do not necessarily reflect the views of The World Bank, its Board of Executive Directors or the governments they represent. The World Bank does not guarantee the accuracy of the data included in this work. The boundaries, colors, denominations, and other information shown on any map in this work do not imply any judgment on the part of The World Bank concerning the legal status of any territory or the endorsement or acceptance of such boundaries. Rights and Permissions The material in this work is subject to copyright. Because The World Bank encourages dissemination of its knowledge, this work may be reproduced, in whole or in part, for noncommercial purposes as long as full attribution to this work is given. Any queries on rights and licenses, including subsidiary rights, should be addressed to the Office of the Publisher, The World Bank, 1818 H Street NW, Washington, DC 20433, USA; fax: 202-522-2422; e-mail: [email protected]. Table of Contents ACKNOWLEDGMENTS ..................................................................................................................VII -
Gansu Cultural and Natural Heritage Protection and Development Project Management Office July 20Th, 2007 Public Disclosure Authorized Annex A: Maps of Each Site
Gansu Cultural and Natural E1659 Heritage v 3 Protection and Development Project Public Disclosure Authorized Consolidated Environmental Assessment & Environmental Public Disclosure Authorized Management Plan Volume III Public Disclosure Authorized World Bank Financed Gansu Cultural and Natural Heritage Protection and Development Project Management Office July 20th, 2007 Public Disclosure Authorized Annex A: Maps of Each Site Figure.1 Map for Yardang National Geological Park Suodong Highway Figure.2 Figure.2 TownMap of Suoyang Ancient Figure.3 Map for Jiuquan Museum Figure.4 Map for Wei Jin Folk Culture Park Figure.5 Map for Jiayuguan Great Wall Figure.6 Map for Majishan Scenic Area Figure.7 Map for Lutusi Ancient Government Centre Figure.8 Map for Shi Chuan Ancient Pear Orchard Figure.9 Map for Qingcheng Ancient Town Figure.10 Map for Yellow River Stone Forest National Park Figure.11 Map for Mati Temple Scenic Park Annex B Further Information on Baseline Conditions at the Eleven Priority Sites Yardang National Geological Park Topography and Physiography Yardang National Geological Park located at 180 kilometres northwest to Dunhuang City, Gansu province. Yardang National Geological Park situated in the west extension of Anxi-Duanhuang basin, and connected with Luobupo which located at west of Yardang National Geological Park. Yardang National Geological Park belongs to plain area with high to the east and low to the west. Yardang National Geological Park has an area of about 398.4 square kilometres with a length about 15-25 km of from east to west and the width about 15-20 km from north to south. The elevation of Gansu is decrease from 1050 metres in east to 860 metres in west. -
Winter-To-Summer Seasonal Migration of Microlithic Human Activities On
www.nature.com/scientificreports OPEN Winter‑to‑summer seasonal migration of microlithic human activities on the Qinghai‑Tibet Plateau Guangliang Hou1,2*, Jingyi Gao2, Youcheng Chen3, Changjun Xu4, Zhuoma Lancuo1, Yongming Xiao5, Linhai Cai5 & Yuanhong He6 The Qinghai‑Tibet Plateau (QTP) has become a valuable site for investigation of adaptive regimes of prehistoric humans to extreme environments. At present most studies have focused solely on a single site. Using a more integrated approach that covers the complete scope of the plateau is needed to better understand the expansion logic of prehistoric humans moving towards the plateau. Here, we conducted accelerator mass spectrometry 14C dating of two microlithic sites. Canxiongashuo (CXGS) and Shalongka (SLK), which are located at the inner and marginal areas of the QTP, respectively. By using geographic information system, literature, and natural environmental factors, we constructed a model for the relationship between traveling distance and time, and we also used these factors to construct a plateau environmental index. The results indicated that the ages of the CXGS and SLK sites are 8.4–7.5 cal. ka BP and 8.4–6.2 cal. ka BP, respectively. Combining the archaeological evidence and literature, hunter‑gatherers may have seasonal migration activities at low altitude in winter and high altitude in summer in order to make full use of natural resources. Our model of relationship between traveling distance and time shows that hunter‑gatherers in CXGS site was active on the plateau all year‑round at approximately 8.3 cal. ka BP. According to EI and archaeological remains, we propose that SLK site was a winter camp of prehistoric hunter‑gatherers. -
UNIVERSITY of CALIFORNIA, SAN DIEGO Qinghai Across Frontiers
UNIVERSITY OF CALIFORNIA, SAN DIEGO Qinghai Across Frontiers: State- and Nation-Building under the Ma Family, 1911-1949 A dissertation submitted in partial satisfaction of the requirements of the degree Doctor of Philosophy in History by William Brent Haas Committee in Charge: Professor Joseph W. Esherick, Co-Chair Professor Paul G. Pickowicz, Co-Chair Professor Weijing Lu Professor Richard Madsen Professor David Ringrose 2013 Copyright William Brent Haas, 2013 All rights reserved The Dissertation of William Brent Haas is approved, and it is acceptable in quality and form for publication on microfilm and electronically: Co-Chair Co-Chair University of California, San Diego 2013 iii Table of Contents Signature Page………………………………………………………………………….. iii Table of Contents……………………………………………………………………….. iv List of Tables…….……………………………………………………………………… v List of Illustrations……………………………………………………………………… vi Acknowledgements……………………………………………………………………....vii Vita……………………………………………………………………………………...xiii Abstract of the Dissertation….……………………………………………………...……ix Introduction………………………………………………………………………………. 1 Chapter One Frontier Militarists in a Transfrontier Province …………………………..13 Chapter Two Fighting for the Frontier: The 1932-1933 Yushu Borderland War……......47 Chapter Three Repelling Reclamation in the “Wastelands” of Qinghai, 1933-1934……93 Chapter Four Schooling at the Frontier: Structuring Education and Practicing Citizenship in Qinghai, 1911-1949………………………………………………………….155 Chapter Five Schooling Mongols and Tibetans: Adaptation and Centralization in