Geochemistry and Environmental Assessment of Major and Trace Elements in the Surface Sediments of the Wei River, China
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Effects of Human Activities in the Wei River Basin on the Lower Yellow River, China
Pol. J. Environ. Stud. Vol. 26, No. 6 (2017), 2555-2565 DOI: 10.15244/pjoes/70629 ONLINE PUBLICATION DATE: 2017-08-31 Original Research Effects of Human Activities in the Wei River Basin on the Lower Yellow River, China Li He Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, 100101 Beijing Received: 15 March 2017 Accepted: 22 April 2017 Abstract Water and soil conservation practices in the Wei River Basin (WRB) may in��uence the Lower Wei River (LWR) itself and the Lower Yellow River (LYR), of which the Wei is a tributary. Based on data of measured and natural runoff and suspended sediment load (SSL) in the WRB, the connections between runoff and SSL from the WRB and deposition in the LWR, the elevation of Tonggguan Hydrology Station, and deposition in the LYR are analyzed. For the compound effects of human activity and climate change in the WRB, the amount of deposition reduction in the LWR during 2000-2009 is about three times what it decreased dur- ing 1970-1979. For per square kilometers of soil conservation, the effect of human activities in the WRB on deposition in the LWR during period of 2000-09 is about four times that of the period of 1970-1979. As decreased runoff and SSL from the WRB, deposition in the LYR decreased during the periods of 1970-1979 and 1990-1999, while deposition in the LYR increased during the periods of 1980-1989 and 2000-2009. For the planned reservoir in the Jing River Basin, the decreased deposition in the LYR may be smaller than that of the LWR. -
Xiao Gang (503-551): His Life and Literature
Xiao Gang (503-551): His Life and Literature by Qingzhen Deng B.A., Guangzhou Foreign Language Institute, China, 1990 M.A., Kobe City University of Foreign Languages, Japan, 1996 Ph.D., Nara Women's University, Japan, 2001 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF Doctor of Philosophy in The Faculty of Graduate Studies (Asian Studies) THE UNIVERSITY OF BRITISH COLUMBIA (Vancouver) February 2013 © Qingzhen Deng, 2013 ii Abstract This dissertation focuses on an emperor-poet, Xiao Gang (503-551, r. 550-551), who lived during a period called the Six Dynasties in China. He was born a prince during the Liang Dynasty, became Crown Prince upon his older brother's death, and eventually succeeded to the crown after the Liang court had come under the control of a rebel named Hou Jing (d. 552). He was murdered by Hou before long and was posthumously given the title of "Emperor of Jianwen (Jianwen Di)" by his younger brother Xiao Yi (508-554). Xiao's writing of amorous poetry was blamed for the fall of the Liang Dynasty by Confucian scholars, and adverse criticism of his so-called "decadent" Palace Style Poetry has continued for centuries. By analyzing Xiao Gang within his own historical context, I am able to develop a more refined analysis of Xiao, who was a poet, a filial son, a caring brother, a sympathetic governor, and a literatus with broad and profound learning in history, religion and various literary genres. Fewer than half of Xiao's extant poems, not to mention his voluminous other writings and many of those that have been lost, can be characterized as "erotic" or "flowery". -
To Increase the Benefits of Water Investment for Regional and National Development ---A Case Study of Shaanxi Province
Global Water Partnership(China) WACDEP Work Package Three Outcome Report To increase the Benefits of Water Investment For Regional and National Development ---A case study of Shaanxi Province Research Office of Shaanxi Provincial People’s Congress Shaanxi Provincial Water Resources Department Xi’an Jiaotong University Copyright @ 2016 by GWP China Abstract Water is not only the indispensable and irreplaceable natural resources for human survival and development, but also very important strategic resources. Water is the infrastructure and the basic industry of the national economic and social development. With the economic growth, the pressure on scarce resources and ecological environment protection is highlighted. The need for government at all levels to speed up the water investment and improve people's welfare is pressing. Therefore, a comprehensive assessment of water investment in Shaanxi Province is of great practical significance. Relatively speaking, Shaanxi Province is short of water resources with less total amount and per capita share. In addition, the spatial distribution of water resources is also extremely unreasonable: the southern part of Shaanxi Province which is part of the Yangtze River basin takes up over 70% while the northern part which is highly populated with fast industrial development only shares 30% of it. The conflict between the demand for water resources and the distribution, to some extent, restrict the social and economic development. The Shaanxi Provincial Government has put the water sector in an important place. It is even so from 2010 to now with a dramatic increase on investment, reaching a total investment amount of 22.408 billion RMB in 2013. -
Emergence, Concept, and Understanding of Pan-River-Basin
HOSTED BY Available online at www.sciencedirect.com International Soil and Water Conservation Research 3 (2015) 253–260 www.elsevier.com/locate/iswcr Emergence, concept, and understanding of Pan-River-Basin (PRB) Ning Liu The Ministry of Water Resources, Beijing 10083, China Received 10 December 2014; received in revised form 20 September 2015; accepted 11 October 2015 Available online 4 November 2015 Abstract In this study, the concept of Pan-River-Basin (PRB) for water resource management is proposed with a discussion on the emergence, concept, and application of PRB. The formation and application of PRB is also discussed, including perspectives on the river contribution rates, harmonious levels of watershed systems, and water resource availability in PRB system. Understanding PRB is helpful for reconsidering river development and categorizing river studies by the influences from human projects. The sustainable development of water resources and the harmonization between humans and rivers also requires PRB. & 2015 International Research and Training Center on Erosion and Sedimentation and China Water and Power Press. Production and Hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/). Keywords: Aquatic Base System; Harmonization of humans and rivers; Pan-River-Basin; River contribution rate; Water transfer 1. Emergence of Pan-River-Basin A river basin (or watershed) is the area of land where surface water, including rain, melting snow, or ice, converges to a single point at a lower elevation, usually the exit of the basin. From the exit, the water joins another water body, such as a river, lake, reservoir, estuary, wetland, or the ocean. -
Earth-Science Reviews 197 (2019) 102900
Earth-Science Reviews 197 (2019) 102900 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev From the headwater to the delta: A synthesis of the basin-scale sediment load regime in the Changjiang River T ⁎ Leicheng Guoa,NiSub, , Ian Townenda,c, Zheng Bing Wanga,d,e, Chunyan Zhua,d, Xianye Wanga, Yuning Zhanga, Qing Hea a State Key Lab of Estuarine and Coastal Research, East China Normal University, Dongchuang Road 500, Shanghai 200241, China b State Key Lab of Marine Geology, Tongji University, Siping Road 1239, Shanghai 200090, China c School of Ocean and Earth Sciences, University of Southampton, Southampton, UK d Department of Hydraulic Engineering, Faculty of Civil Engineering and Geosciences, Delft University of Technology, Delft 2600GA, the Netherlands e Marine and Coastal Systems Department, Deltares, Delft 2629HV, the Netherlands ARTICLE INFO ABSTRACT Keywords: Many large rivers in the world delivers decreasing sediment loads to coastal oceans owing to reductions in Sediment load sediment yield and disrupted sediment deliver. Understanding the sediment load regime is a prerequisite of Source-to-sink sediment management and fluvial and deltaic ecosystem restoration. This work examines sediment load changes Sediment starvation across the Changjiang River basin based on a long time series (1950–2017) of sediment load data stretching from Changjiang the headwater to the delta. We find that the sediment loads have decreased progressively throughout the basin at multiple time scales. The sediment loads have decreased by ~96% and ~74% at the outlets of the upper basin and entire basin, respectively, in 2006–2017 compared to 1950–1985. -
Impact of Climate Change and Anthropogenic Activities on Stream Flow and Sediment Discharge in the Wei River Basin, China
EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Natural Hazards Natural Hazards and Earth System and Earth System Sciences Sciences Discussions Open Access Open Access Atmospheric Atmospheric Chemistry Chemistry and Physics and Physics Discussions Open Access Open Access Atmospheric Atmospheric Measurement Measurement Techniques Techniques Discussions Open Access Open Access Biogeosciences Biogeosciences Discussions Open Access Open Access Climate Climate of the Past of the Past Discussions Open Access Open Access Earth System Earth System Dynamics Dynamics Discussions Open Access Geoscientific Geoscientific Open Access Instrumentation Instrumentation Methods and Methods and Data Systems Data Systems Discussions Open Access Open Access Geoscientific Geoscientific Model Development Model Development Discussions Open Access Open Access Hydrol. Earth Syst. Sci., 17, 961–972, 2013 Hydrology and Hydrology and www.hydrol-earth-syst-sci.net/17/961/2013/ doi:10.5194/hess-17-961-2013 Earth System Earth System © Author(s) 2013. CC Attribution 3.0 License. Sciences Sciences Discussions Open Access Open Access Ocean Science Ocean Science Discussions Impact of climate change and anthropogenic activities on stream Open Access Open Access flow and sediment discharge in the Wei River basin, China Solid Earth Solid Earth Discussions P. Gao1,4,5, V. Geissen2,4, C. J. Ritsema3,4, X.-M. Mu1,5, and F. Wang1,5 1State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation of Northwest A & F University, 712100 Yangling, Shaanxi, China Open Access Open Access 2Land Dynamic Group, University of Wageningen, P.O. -
World Bank Document
SFG2574 REV WB-Funded Project Public Disclosure Authorized Han River Inland Waterway Improvement Project in Hubei (Yakou Navigation Complex Project) Cumulative Effects Assessment Report Public Disclosure Authorized (Project Supplemental Environmental Impact Assessment Report) Public Disclosure Authorized July 2017 Public Disclosure Authorized Acronyms and Abbreviations CEA/CIA Cumulative Effects/Impacts Assessment CEQ Council for Environmental Quality EA Environmental Assessment EIA Environmental Impact Assessment ESIA Environmental and Social Impact Assessment IFC International Finance Group HRB Han River Basin MLHR Middle and Lower Reaches of Han River MEP Ministry of Environmental Protection NEPA National Environmental Policy Act (United States) NGO Non-governmental Organizations RCIA Rapid Cumulative Impact Assessment RFFAs Reasonably Foresseable Future Activities VECs Valued Environmental Components RFFA Reasonably Foreseeable Future Actions SEPA State Environmental Protection Agency WB World Bank WBG World Bank Group mu 1 hactare = 15 mu - I - Contents 1 Introduction ........................................................................................................... 1 1.1 Yakou Complex ................................................................................................................ 1 1.2 Han River Basin and Cascade Development .................................................................... 3 1.3 CEA Purpose, Scope and Methodology ........................................................................ -
Assessment of Sediment Impact on the Risk of River Diversion During Dam Construction: a Simulation-Based Project Study on the Jing River, China
water Article Assessment of Sediment Impact on the Risk of River Diversion during Dam Construction: A Simulation-Based Project Study on the Jing River, China Zida Song 1, Quan Liu 1,* ID , Zhigen Hu 1, Huian Li 2 and Jianqing Xiong 2 1 State Key Laboratory of Water Resources & Hydropower Engineering Science, Wuhan University, Wuhan 430072, China; [email protected] (Z.S.); [email protected] (Z.H.) 2 Yellow River Engineering Consulting Co., Ltd., Zhengzhou 450003, China; [email protected] (H.L.); [email protected] (J.X.) * Correspondence: [email protected]; Tel.: +86-130-7127-9891 Received: 28 January 2018; Accepted: 14 February 2018; Published: 17 February 2018 Abstract: Dams are vital for water resource utilization, and river diversion is key for dam construction safety. As sandy river basins are important exploitation areas that have special diversion features, the impact of sediment on the risk of river diversion during dam construction should be assessed. Diversion uncertainty is the origin of diversion risk, and sediment uncertainty changes the storage and discharge patterns of the diversion system. Two Gumbel–Hougaard (GH) copula functions are adopted to couple the random variables of flood and sediment, so that the sediment impacts on diversion storage and discharge can be obtained by the sampling of flood peaks. Based on variable coupling and sediment amendment, a method of Monte Carlo simulation (MCS) with a water balance calculation can quantitatively assess the risk of sandy river diversion, by evaluating the probability of upstream cofferdam overtopping. By introducing one diversion project on the Jing River in China with a clear water contrast, the risk values of dam construction diversion with or without sediment impacts can be obtained. -
A Regional Archaeology of the Guan River Valley, Henan, China
A REGIONAL ARCHAEOLOGY OF THE GUAN RIVER VALLEY, HENAN, CHINA by Yanxi Wang (Under the Direction of Stephen A. Kowalewski) ABSTRACT This study examines the history of settlement patterns, land use practices, sociopolitical structure, and the inter-regional integration in the Guan Valley, Henan, China from 4000 B.C. to the modern period (A.D.1911). The Guan Valley is an environmentally diverse region and culturally peripheral to three cultural core areas: the Central Plain, the Yangtze River region, and the Guanzhong Basin. This regional full-coverage survey located 96 sites in 135 km2 in the middle Guan Valley. The earliest occupation dated to the Middle Yangshao period (4000-3500 B.C.). In the Late Yangshao (3500-2900 B.C.), occupations increased rapidly and expanded to the upper reach and tributaries of the Guan River. After an occupational rock bottom during the early states period (1900-771 B.C.), occupations recovered rapidly and reached a new level of organization complexity in the Eastern Zhou (770-221 B.C.). This pattern continued into the Qinhan period (220 B.C.-A.D. 220), when hamlets increased in number and expanded into hilly areas. After Qinhan, settlements decreased in number and hierarchy simplified. A Land use analysis explores several environmental conditions associated with settlement locations. Compared to historic occupations (after 1900 B.C.), prehistoric settlements were more affected by some environmental variables, for example, flood risks. In the historic period, there was a growing trend towards the exploitation of hilly areas. Regional primacy characterized settlement systems of most periods. The formation and maintenance of the primate center went through several changes-ceremonial center during Late Yangshao, gateway community during Longshan (2900-1900 B.C.), and administrative center since the Eastern Zhou. -
Bibliography
BIBLIOGRAPHY Chen Zhengxiang. Cultural Geography of China. Beijing: Joint Publishing Co., 1983. Collected by the Garden Bureau of Beijing Dongcheng District. General Investigations of Beijing Fair Documents. Beijing: Beijing Yanshan Publishing House, 2002. E. Saarineen. City: Its Development, Declining and Future, translated by Gu Qiyuan. Beijing: China Building Industry Press, 1986. Feng Tianyu, etc. Cultural History of China. Shanghai: People’s Publishing House, 1991. Feng Youlan. A Newly Compiled History of Chinese Philosophy. Shanghai: People’s Publishing House, 1986. Franz Boas. Primitive Art. Shanghai: Shanghai Literature and Art Publishing House, 1989. Fu Chonglan. Cities Along the Great Wall. Hong Kong: Oriental Press, 1990. Fu Chonglan. Qufu City and Chinese Confucianism. Beijing: China Social Sciences Publishing House, 2003. Fu Chonglan. The History of Lhasa. Beijing: China Social Sciences Publishing House, 1994. Fu Chonglan. Urban Individual Character. Beijing: Social Sciences Academic Press, 2003. Fu Chonglan. Urban Planning Construction at the Turn of the Centuries. Beijing: Science Press, 1991. Fu Chonglan, Chen Guangting & Dong Liming. Problem Report of Chinese Urban Development. Beijing: China Social Sciences Publishing House, 2003. Gu Yanwu (Qing dynasty). Notes on the Residence of the Capital Throughout the Past Dynasties. Beijing: Zhonghua Book Company, 1984. © Social Sciences Academic Press 2019 361 C. Fu and W. Cao, Introduction to the Urban History of China, China Connections, https://doi.org/10.1007/978-981-13-8207-9 362 BIBLIOGRAPHY Gu Zhun. The Greek System of City State. Beijing: China Social Sciences Press, 1979. H. Blij. Geography: Realms, Regions and Concepts, 7th edition. New York: Wiley, 1994. He Yeju. Chinese History of Ancient Urban Planning. -
Simulation of Blue and Green Water Resources in the Wei River Basin, China
486 Evolving Water Resources Systems: Understanding, Predicting and Managing Water–Society Interactions Proceedings of ICWRS2014, Bologna, Italy, June 2014 (IAHS Publ. 364, 2014). Simulation of blue and green water resources in the Wei River basin, China ZONGXUE XU & DEPENG ZUO Key Laboratory of Water and Sediment Sciences, Ministry of Education, College of Water Sciences, Beijing Normal University, Beijing 100875, China [email protected] Abstract The Wei River is the largest tributary of the Yellow River in China and it is suffering from water scarcity and water pollution. In order to quantify the amount of water resources in the study area, a hydrological modelling approach was applied by using SWAT (Soil and Water Assessment Tool), calibrated and validated with SUFI-2 (Sequential Uncertainty Fitting program) based on river discharge in the Wei River basin (WRB). Sensitivity and uncertainty analyses were also performed to improve the model performance. Water resources components of blue water flow, green water flow and green water storage were estimated at the HRU (Hydrological Response Unit) scales. Water resources in HRUs were also aggregated to sub-basins, river catchments, and then city/region scales for further analysis. The results showed that most parts of the WRB experienced a decrease in blue water resources between the 1960s and 2000s, with a minimum value in the 1990s. The decrease is particularly significant in the most southern part of the WRB (Guanzhong Plain), one of the most important grain production basements in China. Variations of green water flow and green water storage were relatively small on the spatial and temporal dimensions. -
Temporal Trends of NDVI in the Jing River Basin of China
Emerging hot Spot Analysis and the Spatial- temporal Trends of NDVI in the Jing River Basin of China Bin Xu ( [email protected] ) Changan University: Chang'an University https://orcid.org/0000-0002-6367-5377 Bin Qi Chang'an University Kai Ji Chang'an University Zhao Liu Chang'an University Lin Deng Chang'an University Ling Jiang Chang'an University Research Article Keywords: Emerging hot spot analysis, Jing River Basin, NDVI, Trends Posted Date: May 28th, 2021 DOI: https://doi.org/10.21203/rs.3.rs-482991/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License 1 Emerging hot spot analysis and the spatial-temporal trends of NDVI in the Jing 2 River Basin of China a,b,c,d,* a a a a a 3 Bin Xu , Bin Qi , Kai Ji , Zhao Liu , Lin Deng , Ling Jiang 4 aSchool of Water and Environment, Chang’an University, No. 126 Yanta Road, Xi’an, 710054, Shaanxi, China; 5 bKey Laboratory of Degraded and Unused Land Consolidation Engineering, Ministry of Natural Resources, No. 7 6 Guangtai Road, Xi’an, 710075, Shaanxi, China; 7 cKey Laboratory of Subsurface Hydrology and Ecological Effects in Arid Region, Ministry of Education, Chang’an 8 University, No. 126 Yanta Road, Xi’an, 710054, Shaanxi, China 9 dShaanxi Key Laboratory of Land Consolidation, No. 126 Yanta Road, Xi’an, 710054, Shaanxi, China; 10 *Corresponding author. 11 E-mail addresses: [email protected] (Bin Xu) 12 Abstract: As an important indicator of vegetation coverage, the Normalized Difference Vegetation Index 13 (NDVI) reflects the changing pattern and evolving trend of the environment.