South-To-North Water Diversion Project, China
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Water Situation in China – Crisis Or Business As Usual?
Water Situation In China – Crisis Or Business As Usual? Elaine Leong Master Thesis LIU-IEI-TEK-A--13/01600—SE Department of Management and Engineering Sub-department 1 Water Situation In China – Crisis Or Business As Usual? Elaine Leong Supervisor at LiU: Niclas Svensson Examiner at LiU: Niclas Svensson Supervisor at Shell Global Solutions: Gert-Jan Kramer Master Thesis LIU-IEI-TEK-A--13/01600—SE Department of Management and Engineering Sub-department 2 This page is left blank with purpose 3 Summary Several studies indicates China is experiencing a water crisis, were several regions are suffering of severe water scarcity and rivers are heavily polluted. On the other hand, water is used inefficiently and wastefully: water use efficiency in the agriculture sector is only 40% and within industry, only 40% of the industrial wastewater is recycled. However, based on statistical data, China’s total water resources is ranked sixth in the world, based on its water resources and yet, Yellow River and Hai River dries up in its estuary every year. In some regions, the water situation is exacerbated by the fact that rivers’ water is heavily polluted with a large amount of untreated wastewater, discharged into the rivers and deteriorating the water quality. Several regions’ groundwater is overexploited due to human activities demand, which is not met by local. Some provinces have over withdrawn groundwater, which has caused ground subsidence and increased soil salinity. So what is the situation in China? Is there a water crisis, and if so, what are the causes? This report is a review of several global water scarcity assessment methods and summarizes the findings of the results of China’s water resources to get a better understanding about the water situation. -
Ganges River Mekong River Himalayan Mountains Huang He (Yellow) River Yangtze River Taklimakan Desert Indus River Gobi Desert B
Southern & Eastern Asia Physical Features and Countries Matching Activity Cut out each card. Match the name to the image and description. Ganges Mekong Himalayan River River Mountains Huang He Yangtze Taklimakan (Yellow) River Desert River Indus Gobi Bay of River Desert Bengal Yellow Indian Sea of Sea Ocean Japan Korean South China India Peninsula Sea China Indonesia Vietnam North South Japan Korea Korea Southern & Eastern Asia Physical Features and Countries Matching Activity Southern & Eastern Asia Physical Features and Countries Matching Activity Southern & Eastern Asia Physical Features and Countries Matching Activity Asia’s largest desert that stretches across southern Mongolia and northern China Largest and longest river in China’s second largest river China; very important that causes devastating because it provides floods. It is named for the hydroelectric power, water for muddy yellow silt it carries. irrigation, and transportation for cargo ships. Flows through China, Starts in the Himalayan Myanmar (Burma), Thailand, Mountains; most important river in Laos, Cambodia, and India because it runs through the Vietnam. One of the region’s most fertile and highly populated most important crops, rice, is areas; considered sacred by the grown in the river basin. Hindu religion. World’s highest mountain range that sits along the Located in northwestern northern edge of India; China between two mountain includes Mount Everest, the ranges highest mountain in the world. Begins high in the Himalayas and slowly runs through India Third largest -
Numerical Simulations of Spread Characteristics of Toxic Cyanide in the Danjiangkou Reservoir in China Under the Effects of Dam Cooperation
Hindawi Publishing Corporation Mathematical Problems in Engineering Volume 2014, Article ID 373510, 10 pages http://dx.doi.org/10.1155/2014/373510 Research Article Numerical Simulations of Spread Characteristics of Toxic Cyanide in the Danjiangkou Reservoir in China under the Effects of Dam Cooperation Libin Chen, Zhifeng Yang, and Haifei Liu State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing 100875, China Correspondence should be addressed to Zhifeng Yang; [email protected] Received 16 June 2014; Revised 1 September 2014; Accepted 1 September 2014; Published 29 September 2014 Academic Editor: Ricardo Aguilar-Lopez´ Copyright © 2014 Libin Chen et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Many accidents of releasing toxic pollutants into surface water happen each year in the world. It is believed that dam cooperation can affect flow field in reservoir and then can be applied to avoiding and reducing spread speed of toxic pollutants to drinking water intake mouth. However, few studies investigated the effects of dam cooperation on the spread characteristics of toxic pollutants in reservoir, especially the source reservoir for water diversion with more than one dam. The Danjiangkou Reservoir is the source reservoir of the China’ South-to-North Water Diversion Middle Route Project. The human activities are active within this reservoir basin and cyanide-releasing accident once happened in upstream inflow. In order to simulate the spread characteristics of cyanide in the reservoir in the condition of dam cooperation, a three-dimensional water quality model based on the Environmental Fluid Dynamics Code (EFDC) has been built and put into practice. -
How Geography "Mapped" East Asia, Part One: China by Craig Benjamin, Big History Project, Adapted by Newsela Staff on 01.26.17 Word Count 1,354 Level 1020L
How Geography "Mapped" East Asia, Part One: China By Craig Benjamin, Big History Project, adapted by Newsela staff on 01.26.17 Word Count 1,354 Level 1020L TOP: The Stalagmite Gang peaks at the East Sea area of Huangshan mountain in China. Photo by: Education Images/UIG via Getty Images MIDDLE: Crescent Moon Lake and oasis in the middle of the desert. Photo by: Tom Thai, Flickr. BOTTOM: Hukou Waterfall in the Yellow River. Photo by: Wikimedia The first in a two-part series In what ways did geography allow for the establishment of villages and towns — some of which grew into cities — in various regions of East Asia? What role did climate play in enabling powerful states and civilizations to appear in some areas while other locations remained better suited for a nomadic lifestyle? Let's begin to answer these questions with a story about floods in China. China's two great rivers — the Yangtze and the Yellow — have flooded regularly for as long as we can measure in the historical and geological record. Catastrophic floodwaters This article is available at 5 reading levels at https://newsela.com. Nothing can compare, though, to the catastrophic floods of August 19, 1931. The Yangtze river rose an astonishing 53 feet above its normal level in just one day. It unleashed some of the most destructive floodwaters ever seen. The floods were caused by a "perfect storm" of conditions. Monsoon rains, heavy snowmelt, and unexpected rains pounded huge areas of southern China. All this water poured into the Yangtze. The river rose and burst its banks for hundreds of miles. -
Effects of Water Level Increase on Phytoplankton Assemblages in a Drinking Water Reservoir
Portland State University PDXScholar Environmental Science and Management Faculty Publications and Presentations Environmental Science and Management 2018 Effects of Water Level Increase on Phytoplankton Assemblages in a Drinking Water Reservoir Yangdong Pan Portland State University, [email protected] Shijun Guo Nanyang Normal University, Nanyang, Henan, China Yuying Li Nanyang Normal University, Nanyang,Henan, China Wei Yin Nanyang Normal University, Henan, China Pengcheng Qi Nanyang Normal University, Henan, China See next page for additional authors Follow this and additional works at: https://pdxscholar.library.pdx.edu/esm_fac Part of the Hydrology Commons, and the Natural Resources Management and Policy Commons Let us know how access to this document benefits ou.y Citation Details Pan, Y., Guo, S., Li, Y., Yin, W., Qi, P., Shi, J., ... & Zhu, J. (2018). Effects of Water Level Increase on Phytoplankton Assemblages in a Drinking Water Reservoir. Water, 10(3), 256. This Article is brought to you for free and open access. It has been accepted for inclusion in Environmental Science and Management Faculty Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Authors Yangdong Pan, Shijun Guo, Yuying Li, Wei Yin, Pengcheng Qi, Jainwei Shi, Lanqun Hu, Bing Li, Shengge Bi, and Jingya Zhu This article is available at PDXScholar: https://pdxscholar.library.pdx.edu/esm_fac/240 water Article Effects of Water Level Increase on Phytoplankton Assemblages -
Polycyclic Aromatic Hydrocarbons in the Estuaries of Two Rivers of the Sea of Japan
International Journal of Environmental Research and Public Health Article Polycyclic Aromatic Hydrocarbons in the Estuaries of Two Rivers of the Sea of Japan Tatiana Chizhova 1,*, Yuliya Koudryashova 1, Natalia Prokuda 2, Pavel Tishchenko 1 and Kazuichi Hayakawa 3 1 V.I.Il’ichev Pacific Oceanological Institute FEB RAS, 43 Baltiyskaya Str., Vladivostok 690041, Russia; [email protected] (Y.K.); [email protected] (P.T.) 2 Institute of Chemistry FEB RAS, 159 Prospect 100-let Vladivostoku, Vladivostok 690022, Russia; [email protected] 3 Institute of Nature and Environmental Technology, Kanazawa University, Kakuma, Kanazawa 920-1192, Japan; [email protected] * Correspondence: [email protected]; Tel.: +7-914-332-40-50 Received: 11 June 2020; Accepted: 16 August 2020; Published: 19 August 2020 Abstract: The seasonal polycyclic aromatic hydrocarbon (PAH) variability was studied in the estuaries of the Partizanskaya River and the Tumen River, the largest transboundary river of the Sea of Japan. The PAH levels were generally low over the year; however, the PAH concentrations increased according to one of two seasonal trends, which were either an increase in PAHs during the cold period, influenced by heating, or a PAH enrichment during the wet period due to higher run-off inputs. The major PAH source was the combustion of fossil fuels and biomass, but a minor input of petrogenic PAHs in some seasons was observed. Higher PAH concentrations were observed in fresh and brackish water compared to the saline waters in the Tumen River estuary, while the PAH concentrations in both types of water were similar in the Partizanskaya River estuary, suggesting different pathways of PAH input into the estuaries. -
Transboundary River Basin Overview – Salween
0 [Type here] Irrigation in Africa in figures - AQUASTAT Survey - 2016 Transboundary River Basin Overview – Salween Version 2011 Recommended citation: FAO. 2011. AQUASTAT Transboundary River Basins – Salween River Basin. Food and Agriculture Organization of the United Nations (FAO). Rome, Italy The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO. FAO encourages the use, reproduction and dissemination of material in this information product. Except where otherwise indicated, material may be copied, downloaded and printed for private study, research and teaching purposes, or for use in non-commercial products or services, provided that appropriate acknowledgement of FAO as the source and copyright holder is given and that FAO’s endorsement of users’ views, products or services is not implied in any way. All requests for translation and adaptation rights, and for resale and other commercial use rights should be made via www.fao.org/contact-us/licencerequest or addressed to [email protected]. -
In Koguryo Dynasty the State-Formation History Starts from B
International Journal of Korean History(Vol.6, Dec.2004) 1 History of Koguryŏ and China’s Northeast Asian Project 1Park Kyeong-chul * Introduction The Koguryŏ Dynasty, established during the 3rd century B.C. around the Maek tribe is believed to have begun its function as a centralized entity in the Northeast Asia region. During the period between 1st century B.C. and 1st century A.D. aggressive regional expansion policy from the Koguryŏ made it possible to overcome its territorial limitations and weak economic basis. By the end of the 4th century A.D., Koguryŏ emerged as an empire that had acquired its own independent lebensraum in Northeast Asia. This research paper will delve into identifying actual founders of the Koguryŏ Dynasty and shed light on their lives prior to the actual establishment of the Dynasty. Then on, I will analyze the establishment process of Koguryŏ Dynasty. Thereafter, I will analyze the history of Koguryŏ Dynasty at three different stages: the despotic military state period, the period in which Koguryŏ emerged as an independent empire in Northeast Asia, and the era of war against the Sui and Tang dynasty. Upon completion of the above task, I will illustrate the importance of Koguryŏ history for Koreans. Finally, I attempt to unearth the real objectives why the Chinese academics are actively promoting the Northeast Asian Project. * Professor, Dept. of Liberal Arts, Kangnam University 2 History of Koguryŏ and China’s Northeast Asian Project The Yemaek tribe and their culture1 The main centers of East Asian culture in approximately 2000 B.C. were China - by this point it had already become an agrarian society - and the Mongol-Siberian region where nomadic cultures reign. -
Shanghai, China Overview Introduction
Shanghai, China Overview Introduction The name Shanghai still conjures images of romance, mystery and adventure, but for decades it was an austere backwater. After the success of Mao Zedong's communist revolution in 1949, the authorities clamped down hard on Shanghai, castigating China's second city for its prewar status as a playground of gangsters and colonial adventurers. And so it was. In its heyday, the 1920s and '30s, cosmopolitan Shanghai was a dynamic melting pot for people, ideas and money from all over the planet. Business boomed, fortunes were made, and everything seemed possible. It was a time of breakneck industrial progress, swaggering confidence and smoky jazz venues. Thanks to economic reforms implemented in the 1980s by Deng Xiaoping, Shanghai's commercial potential has reemerged and is flourishing again. Stand today on the historic Bund and look across the Huangpu River. The soaring 1,614-ft/492-m Shanghai World Financial Center tower looms over the ambitious skyline of the Pudong financial district. Alongside it are other key landmarks: the glittering, 88- story Jinmao Building; the rocket-shaped Oriental Pearl TV Tower; and the Shanghai Stock Exchange. The 128-story Shanghai Tower is the tallest building in China (and, after the Burj Khalifa in Dubai, the second-tallest in the world). Glass-and-steel skyscrapers reach for the clouds, Mercedes sedans cruise the neon-lit streets, luxury- brand boutiques stock all the stylish trappings available in New York, and the restaurant, bar and clubbing scene pulsates with an energy all its own. Perhaps more than any other city in Asia, Shanghai has the confidence and sheer determination to forge a glittering future as one of the world's most important commercial centers. -
Korean War Timeline America's Forgotten War by Kallie Szczepanski, About.Com Guide
Korean War Timeline America's Forgotten War By Kallie Szczepanski, About.com Guide At the close of World War II, the victorious Allied Powers did not know what to do with the Korean Peninsula. Korea had been a Japanese colony since the late nineteenth century, so westerners thought the country incapable of self-rule. The Korean people, however, were eager to re-establish an independent nation of Korea. Background to the Korean War: July 1945 - June 1950 Library of Congress Potsdam Conference, Russians invade Manchuria and Korea, US accepts Japanese surrender, North Korean People's Army activated, U.S. withdraws from Korea, Republic of Korea founded, North Korea claims entire peninsula, Secretary of State Acheson puts Korea outside U.S. security cordon, North Korea fires on South, North Korea declares war July 24, 1945- President Truman asks for Russian aid against Japan, Potsdam Aug. 8, 1945- 120,000 Russian troops invade Manchuria and Korea Sept. 9, 1945- U.S. accept surrender of Japanese south of 38th Parallel Feb. 8, 1948- North Korean People's Army (NKA) activated April 8, 1948- U.S. troops withdraw from Korea Aug. 15, 1948- Republic of Korea founded. Syngman Rhee elected president. Sept. 9, 1948- Democratic People's Republic (N. Korea) claims entire peninsula Jan. 12, 1950- Sec. of State Acheson says Korea is outside US security cordon June 25, 1950- 4 am, North Korea opens fire on South Korea over 38th Parallel June 25, 1950- 11 am, North Korea declares war on South Korea North Korea's Ground Assault Begins: June - July 1950 Department of Defense / National Archives UN Security Council calls for ceasefire, South Korean President flees Seoul, UN Security Council pledges military help for South Korea, U.S. -
Holocene Environmental Archaeology of the Yangtze River Valley in China: a Review
land Review Holocene Environmental Archaeology of the Yangtze River Valley in China: A Review Li Wu 1,2,*, Shuguang Lu 1, Cheng Zhu 3, Chunmei Ma 3, Xiaoling Sun 1, Xiaoxue Li 1, Chenchen Li 1 and Qingchun Guo 4 1 Provincial Key Laboratory of Earth Surface Processes and Regional Response in the Yangtze-Huaihe River Basin, School of Geography and Tourism, Anhui Normal University, Wuhu 241002, China; [email protected] (S.L.); [email protected] (X.S.); [email protected] (X.L.); [email protected] (C.L.) 2 State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China 3 School of Geograpy and Ocean Science, Nanjing University, Nanjing 210023, China; [email protected] (C.Z.); [email protected] (C.M.) 4 School of Environment and Planning, Liaocheng University, Liaocheng 252000, China; [email protected] * Correspondence: [email protected] Abstract: The Yangtze River Valley is an important economic region and one of the cradles of human civilization. It is also the site of frequent floods, droughts, and other natural disasters. Conducting Holocene environmental archaeology research in this region is of great importance when studying the evolution of the relationship between humans and the environment and the interactive effects humans had on the environment from 10.0 to 3.0 ka BP, for which no written records exist. This Citation: Wu, L.; Lu, S.; Zhu, C.; review provides a comprehensive summary of materials that have been published over the past Ma, C.; Sun, X.; Li, X.; Li, C.; Guo, Q.