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Stable Hydrogen and Oxygen Isotope Characteristics of Bottled Water in China: a Consideration of Water Source
Stable Hydrogen and Oxygen Isotope Characteristics of Bottled Water in China: A Consideration of Water Source Supplementary Materials: Table 1. Inventory of sampling stations. Ave.(‰) σ(‰) Brand Source site Origin Lon./° Lat./° Alt/m Date δ2H δ18O δ2H δ18O Daqishanquan Tonglu spring 119.72 29.77 158.41 −31.3 −5.53 − − 2015.5.22 Bamaboquan Bama spring 107.25 24.14 244.08 −46.3 −6.99 − − 2015.6.6 1626.9 Baishite Lanzhou spring 103.81 36.02 −63.06 −9.61 − − 2015.4.22 5 Wudangshanqu Danjiangkou spring 111.48 32.55 147.41 −18.75 −3.86 − − 2015.3.11 an Xiaoyushanquan Guantao spring 115.30 36.53 43.33 −65.01 −9.24 − − 2015.7.05 2015.4.24 2015.5.31 Lao Shan (4) Qingdao spring 120.68 36.20 4.06 −50.87 −7.65 0.36 0.09 2015.7.16 2015.5.20 Shenshuiyu Sishui spring 117.30 35.55 340.20 −63.66 −8.88 - - 2015.6.27 2015.5.20 HOSANMI (2) Haikou spring 110.01 19.7 63.46 −45.80 −6.99 0.05 0.00 2015.6.09 2015.1.07 1062.5 −107.0 AER (3) Arxan spring 119.94 47.19 −14.58 1.96 0.71 2015.3.29 8 8 2015.5.07 2695.2 2015.6.04 Angsiduo (2) Haidong spring 102.13 36.20 −57.37 −8.73 0.08 0.08 3 2015.6.01 Nongfu Spring Changbai 2015.8.09 spring 127.84 42.52 738.31 −94.15 −13.6 0.33 0.04 (2) Shan 2015.8.10 2014.11.04 Evergrande ice Changbai 2720.5 2015.3.06 spring 127.88 41.99 −86.00 −12.22 0.34 0.11 spring (4) Shan 2 2015.4.11 2015.8.17 2015.4.02 2015.7.09 ALKAQUA (4) Antu spring 128.17 42.48 655.72 −98.68 −13.88 0.02 0.02 2015.7.10 2015.9.06 Master Kong Yanbian spring 129.52 42.90 183.16 −85.54 −12.06 - - 2015.6.04 Yaquan Hotan spring 79.92 37.12 1379 −43.23 −7.12 - -
Research on the Present Situation, Problems and Countermeasures Of
Advances in Social Science, Education and Humanities Research, volume 427 5th International Conference on Social Sciences and Economic Development (ICSSED 2020) Research on the Present Situation, Problems and Countermeasures of Precision Poverty Alleviation in Badong County Yahong Gong1 Weiliang Tu2,* 1Economics and Management of Yangtze University School, Jingzhou, 434023, Hubei Email: [email protected] 2Economics and Management of Yangtze University School, Jingzhou, 434023, Hubei * Corresponding author: Weiliang Tu ABSTRACT Targeted poverty alleviation means accurate identification, assistance and management of the poor. Through the analysis of the current situation of poverty and precision poverty alleviation practice in the rural areas of Badong county, we can find out the difficult problems in the precise poverty alleviation work and overcome the problem of poverty alleviation in the deep poverty-stricken areas. We should improve the strategy of targeted poverty alleviation through multiple channels, establish a long-term mechanism of poverty alleviation through industry, education, entrepreneurship, and improve the skills of poverty alleviation teams, in an effort to reduce the poor population in Badong county. Keywords: targeted poverty alleviation, problem, long-term mechanism zone, 12 townships and 491 villages (neighborhood committees). In 2016, the resident population of Badong 1. INTRODUCTION county was 570,000, among which more than 520,000 were rural residents, accounting for 91.23% of the total In the past, China mainly focused on the extensive poverty population of the county. alleviation model. Later, the targeted poverty alleviation model was put forward in light of the extensive poverty alleviation model. The targeted poverty alleviation model 2.2. Poverty situation. was a scientific and effective program that accurately identified, assisted and managed the targets of poverty Badong county is one of the poorest counties and cities in alleviation[4]. -
Landscape Analysis of Geographical Names in Hubei Province, China
Entropy 2014, 16, 6313-6337; doi:10.3390/e16126313 OPEN ACCESS entropy ISSN 1099-4300 www.mdpi.com/journal/entropy Article Landscape Analysis of Geographical Names in Hubei Province, China Xixi Chen 1, Tao Hu 1, Fu Ren 1,2,*, Deng Chen 1, Lan Li 1 and Nan Gao 1 1 School of Resource and Environment Science, Wuhan University, Luoyu Road 129, Wuhan 430079, China; E-Mails: [email protected] (X.C.); [email protected] (T.H.); [email protected] (D.C.); [email protected] (L.L.); [email protected] (N.G.) 2 Key Laboratory of Geographical Information System, Ministry of Education, Wuhan University, Luoyu Road 129, Wuhan 430079, China * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel: +86-27-87664557; Fax: +86-27-68778893. External Editor: Hwa-Lung Yu Received: 20 July 2014; in revised form: 31 October 2014 / Accepted: 26 November 2014 / Published: 1 December 2014 Abstract: Hubei Province is the hub of communications in central China, which directly determines its strategic position in the country’s development. Additionally, Hubei Province is well-known for its diverse landforms, including mountains, hills, mounds and plains. This area is called “The Province of Thousand Lakes” due to the abundance of water resources. Geographical names are exclusive names given to physical or anthropogenic geographic entities at specific spatial locations and are important signs by which humans understand natural and human activities. In this study, geographic information systems (GIS) technology is adopted to establish a geodatabase of geographical names with particular characteristics in Hubei Province and extract certain geomorphologic and environmental factors. -
Journal of Hydrology 569 (2019) 218–229
Journal of Hydrology 569 (2019) 218–229 Contents lists available at ScienceDirect Journal of Hydrology journal homepage: www.elsevier.com/locate/jhydrol Water quality variability in the middle and down streams of Han River under the influence of the Middle Route of South-North Water diversion T project, China ⁎ Yi-Ming Kuoa,1, , Wen-wen Liua,1, Enmin Zhaoa, Ran Lia, Rafael Muñoz-Carpenab a School of Environmental Studies, China University of Geosciences, Wuhan 430074, China b Department of Agricultural and Biological Engineering-IFAS, University of Florida, Gainesville, FL, USA ARTICLE INFO ABSTRACT This manuscript was handled by Huaming Guo, The middle and down streams of Han River are complex river systems influenced by hydrologic variations, Editor-in-Chief, with the assistance of Chong- population distributions, and the engineering projects. The Middle Route of China’s South-to-North Water Yu Xu, Associate Editor Transfer (MSNW) project planned to transfer 95 billion m3 annually from Han River to north China. The op- Keywords: eration of the MSNW project may alter the flow rate and further influence the water quality of Han River. This Min/max autocorrelation factor analysis study used min/max autocorrelation factor analysis (MAFA) and dynamic factor analysis (DFA) to analyze Dynamic factor analysis spatio-temporal variations of the water quality variables in three typical tributary-mainstream intersection zones Han River in Han River from June 2014 to April 2017. MAFA results showed that chlorophyll-a (Chl-a), chemical oxygen Flow rate − demand (COD), suspend solid (SS) and phosphate (PO 3 ) (represented as trophic dynamics) are main con- Water transfer 4 cerned water quality variables in densely populated zones (Zones 1 and 3), and total nitrogen (TN), nitrate Water quality variation − 3− nitrogen (NO3 ), COD, and PO4 (regarded as nutrient formations dynamics) represent the underlying water quality variations in agricultural cultivation zone (Zone 2). -
Archaeological Observation on the Exploration of Chu Capitals
Archaeological Observation on the Exploration of Chu Capitals Wang Hongxing Key words: Chu Capitals Danyang Ying Chenying Shouying According to accurate historical documents, the capi- In view of the recent research on the civilization pro- tals of Chu State include Danyang 丹阳 of the early stage, cess of the middle reach of Yangtze River, we may infer Ying 郢 of the middle stage and Chenying 陈郢 and that Danyang ought to be a central settlement among a Shouying 寿郢 of the late stage. Archaeologically group of settlements not far away from Jingshan 荆山 speaking, Chenying and Shouying are traceable while with rice as the main crop. No matter whether there are the locations of Danyang and Yingdu 郢都 are still any remains of fosses around the central settlement, its oblivious and scholars differ on this issue. Since Chu area must be larger than ordinary sites and be of higher capitals are the political, economical and cultural cen- scale and have public amenities such as large buildings ters of Chu State, the research on Chu capitals directly or altars. The site ought to have definite functional sec- affects further study of Chu culture. tions and the cemetery ought to be divided into that of Based on previous research, I intend to summarize the aristocracy and the plebeians. The relevant docu- the exploration of Danyang, Yingdu and Shouying in ments and the unearthed inscriptions on tortoise shells recent years, review the insufficiency of the former re- from Zhouyuan 周原 saying “the viscount of Chu search and current methods and advance some personal (actually the ruler of Chu) came to inform” indicate that opinion on the locations of Chu capitals and later explo- Zhou had frequent contact and exchange with Chu. -
Lithofacies Palaeogeography of the Late Permian Wujiaping Age in the Middle and Upper Yangtze Region, China
Journal of Palaeogeography 2014, 3(4): 384-409 DOI: 10.3724/SP.J.1261.2014.00063 Lithofacies palaeogeography and sedimentology Lithofacies palaeogeography of the Late Permian Wujiaping Age in the Middle and Upper Yangtze Region, China Jin-Xiong Luo*, You-Bin He, Rui Wang School of Geosciences, Yangtze University, Wuhan 430100, China Abstract The lithofacies palaeogeography of the Late Permian Wujiaping Age in Middle and Upper Yangtze Region was studied based on petrography and the “single factor analysis and multifactor comprehensive mapping” method. The Upper Permian Wujiaping Stage in the Middle and Upper Yangtze Region is mainly composed of carbonate rocks and clastic rocks, with lesser amounts of siliceous rocks, pyroclastic rocks, volcanic rocks and coal. The rocks can be divided into three types, including clastic rock, clastic rock-limestone and lime- stone-siliceous rock, and four fundamental ecological types and four fossil assemblages are recognized in the Wujiaping Stage. Based on a petrological and palaeoecological study, six single factors were selected, namely, thickness (m), content (%) of marine rocks, content (%) of shallow water carbonate rocks, content (%) of biograins with limemud, content (%) of thin- bedded siliceous rocks and content (%) of deep water sedimentary rocks. Six single factors maps of the Wujiaping Stage and one lithofacies palaeogeography map of the Wujiaping Age were composed. Palaeogeographic units from west to east include an eroded area, an alluvial plain, a clastic rock platform, a carbonate rock platform where biocrowds developed, a slope and a basin. In addition, a clastic rock platform exists in the southeast of the study area. Hydro- carbon source rock and reservoir conditions were preliminarily analyzed based on lithofacies palaeogeography. -
5 Mitigation Measures of Environment Influence
E4803 V2 Certificate No.: GHPZJZ No. 2608 Public Disclosure Authorized Traffic Integration Demonstration Project of Wuhan Public Disclosure Authorized City Circle Supported by World Bank Loan- Urban Transport Infrastructure Subproject in Anlu, Xiaogan Public Disclosure Authorized Environmental Management Plan Public Disclosure Authorized Prepared by: Hubei Gimbol Environment Technology Co., Ltd Anlu Yunan Asset Management Co., Ltd. March, 2015 1 Contents 1 Preface ……………………………………………………………………………..1 1.1 EMP objective………………………………………………..……….….… 1 1.2 EMP design ……………………………………………………………………….……………………..2 2 Environmental Policies and Regulations Documents …………………………..4 2.1 Related laws and regulations …………………………………………………………….………4 2.2 Technical specifications and standards ………………………………………….………….6 2.3Safety guarantee policies of the World Bank ………………………….………………….7 2.4 Related technical documents ………………………………………………………….…………8 2.5 Applicable standards ……………………………………………………………………..………….8 3 Project Overview ………………………………………………………………...14 3.1Project overview ………………………………………………………………………..……….……14 3.2 Construction organization ……………………………………………………………..………..17 4. Environmental Impact of the Project …………………………………….……19 4.1 Goal of environmental protection ……………………………………………………..…….19 4.2 Identification of environmental impact of engineering construction ……..…54 4.3 Influence on ecological environment …………………………………………..………….57 4.4 Influence on water environment ………………………………………………………………61 4.5 Impact on acoustic environment ………………………………………………………………65 4.6 Ambient -
Spatial-Temporal Features of Wuhan Urban Agglomeration Regional Development Pattern—Based on DMSP/OLS Night Light Data
Journal of Building Construction and Planning Research, 2017, 5, 14-29 http://www.scirp.org/journal/jbcpr ISSN Online: 2328-4897 ISSN Print: 2328-4889 Spatial-Temporal Features of Wuhan Urban Agglomeration Regional Development Pattern—Based on DMSP/OLS Night Light Data Mengjie Zhang1*, Wenwei Miao1, Yingpin Yang2, Chong Peng1, Yaping Huang1 1School of Architecture and Urban Planning, Huazhong University of Science and Technology, Wuhan, China 2Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing, China How to cite this paper: Zhang, M.J., Miao, Abstract W.W., Yang, Y.P., Peng, C. and Huang, Y.P. (2017) Spatial-Temporal Features of Wu- Based on the night light data, urban area data, and economic data of Wuhan han Urban Agglomeration Regional De- Urban Agglomeration from 2009 to 2015, we use spatial correlation dimen- velopment Pattern—Based on DMSP/OLS sion, spatial self-correlation analysis and weighted standard deviation ellipse Night Light Data. Journal of Building Con- struction and Planning Research, 5, 14-29. to identify the general characteristics and dynamic evolution characteristics of https://doi.org/10.4236/jbcpr.2017.51002 urban spatial pattern and economic disparity pattern. The research results prove that: between 2009 and 2013, Wuhan Urban Agglomeration expanded Received: February 3, 2017 Accepted: March 5, 2017 gradually from northwest to southeast and presented the dynamic evolution Published: March 8, 2017 features of “along the river and the road”. The spatial structure is obvious, forming the pattern of “core-periphery”. The development of Wuhan Urban Copyright © 2017 by authors and Agglomeration has obvious imbalance in economic geography space, pre- Scientific Research Publishing Inc. -
Present Status, Driving Forces and Pattern Optimization of Territory in Hubei Province, China Tingke Wu, Man Yuan
World Academy of Science, Engineering and Technology International Journal of Environmental and Ecological Engineering Vol:13, No:5, 2019 Present Status, Driving Forces and Pattern Optimization of Territory in Hubei Province, China Tingke Wu, Man Yuan market failure [4]. In fact, spatial planning system of China is Abstract—“National Territorial Planning (2016-2030)” was not perfect. It is a crucial problem that land resources have been issued by the State Council of China in 2017. As an important unordered and decentralized developed and overexploited so initiative of putting it into effect, territorial planning at provincial level that ecological space and agricultural space are seriously makes overall arrangement of territorial development, resources and squeezed. In this regard, territorial planning makes crucial environment protection, comprehensive renovation and security system construction. Hubei province, as the pivot of the “Rise of attempt to realize the "Multi-Plan Integration" mode and Central China” national strategy, is now confronted with great contributes to spatial planning system reform. It is also opportunities and challenges in territorial development, protection, conducive to improving land use regulation and enhancing and renovation. Territorial spatial pattern experiences long time territorial spatial governance ability. evolution, influenced by multiple internal and external driving forces. Territorial spatial pattern is the result of land use conversion It is not clear what are the main causes of its formation and what are for a long period. Land use change, as the significant effective ways of optimizing it. By analyzing land use data in 2016, this paper reveals present status of territory in Hubei. Combined with manifestation of human activities’ impact on natural economic and social data and construction information, driving forces ecosystems, has always been a specific field of global climate of territorial spatial pattern are then analyzed. -
Research on Slope Deformation Regularity of the Badong Formation in the Three-Gorges Reservoir Area
Applied Mechanics and Materials Vols 117-119 (2012) pp 1638-1645 Online: 2011-10-24 © (2012) Trans Tech Publications, Switzerland doi:10.4028/www.scientific.net/AMM.117-119.1638 Research on Slope Deformation Regularity of the Badong Formation in the Three-Gorges Reservoir Area Huiming Tang 1, a , Xinli Hu 1, b and Chengren Xiong 1,c 1 Engineering Faculty, China University of Geosciences, Wuhan 430074, China a [email protected], b [email protected], c [email protected] Keywords: The Three-Gorge Reservoir, Badong Formation, landslide, Huangtupo landslide, landslide evolution pattern Abstract. The Three-Gorges Reservoir area is characterized by widely distributed strata of Badong Formation, in which large size landslide and deep-reaching loose geological body are likely to form. Therefore, it is significant to reveal the mechanism and patterns of the large size landslide in Badong Formation for better understanding of the development of the nature of deformation and process of formation of the deep-reaching loose stratum slope. In this paper, the geological characteristics of the rock mass of the Badong Formation are concluded on the basis of systematic explanation of the space variation of the lithology combinations and space variation of structural deformation of the Badong Formation in the Three-Gorges Reservoir area. To demonstrate the basic law of long-term deformation of the Badong Formation slopes and the patterns of later stage reform and landslide evolution, the authors exemplify the Huangtupo landslide that is typical in the Badong Formation. Introduction The Three-Gorge Reservoir area is characterized by widely distributed strata of Badong Formation, in which large size landslide and deep-reaching loose geological body are likely to form. -
People's Republic of China: Hubei Enshi Qing River Upstream
Project Administration Manual Project Number: 47048-002 March 2020 People’s Republic of China: Hubei Enshi Qing River Upstream Environment Rehabilitation Contents ABBREVIATIONS iv I. PROJECT DESCRIPTION 1 II. IMPLEMENTATION PLANS 8 A. Project Readiness Activities 8 B. Overall Project Implementation Plan 9 III. PROJECT MANAGEMENT ARRANGEMENTS 12 A. Project Implementation Organizations – Roles and Responsibilities 12 B. Key Persons Involved in Implementation 15 C. Project Organization Structure 16 IV. COSTS AND FINANCING 17 A. Detailed Cost Estimates by Expenditure Category 19 B. Allocation and Withdrawal of Loan Proceeds 20 C. Detailed Cost Estimates by Financier 21 D. Detailed Cost Estimates by Outputs 22 E. Detailed Cost Estimates by Year 23 F. Contract and Disbursement S-curve 24 G. Fund Flow Diagram 25 V. FINANCIAL MANAGEMENT 26 A. Financial Management Assessment 26 B. Disbursement 26 C. Accounting 28 D. Auditing and Public Disclosure 28 VI. PROCUREMENT AND CONSULTING SERVICES 30 A. Advance Contracting and Retroactive Financing 30 B. Procurement of Goods, Works and Consulting Services 30 C. Procurement Plan 31 D. Consultant's Terms of Reference 40 VII. SAFEGUARDS 43 A. Environment 43 B. Resettlement 45 C. Ethnic Minorities 52 VIII. GENDER AND SOCIAL DIMENSIONS 53 A. Summary Poverty Reduction and Social Strategy 53 B. Gender Development and Gender Action Plan 53 C. Social Action Plan 54 IX. PERFORMANCE MONITORING, EVALUATION, REPORTING AND COMMUNICATION 61 A. Project Design and Monitoring Framework 61 B. Monitoring 68 C. Evaluation -
Geographical Overview of the Three Gorges Dam and Reservoir, China—Geologic Hazards and Environmental Impacts
Geographical Overview of the Three Gorges Dam and Reservoir, China—Geologic Hazards and Environmental Impacts Open-File Report 2008–1241 U.S. Department of the Interior U.S. Geological Survey Geographical Overview of the Three Gorges Dam and Reservoir, China— Geologic Hazards and Environmental Impacts By Lynn M. Highland Open-File Report 2008–1241 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2008 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Highland, L.M., 2008, Geographical overview of the Three Gorges dam and reservoir, China—Geologic hazards and environmental impacts: U.S. Geological Survey Open-File Report 2008–1241, 79 p. http://pubs.usgs.gov/of/2008/1241/ iii Contents Slide 1...............................................................................................................................................................1