Year 6 Geography Research Project
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Glossary of Place Names for the Chinese Australian Hometown Heritage Tour, January 2018
Glossary of place names for the Chinese Australian Hometown Heritage Tour, January 2018 Chinese English name or characters Mandarin (pinyin) Cantonese (Yale) ‘Chinese postal romanisation’ (traditional) HONG KONG Hong Kong 香港 Xiānggǎng Hēunggóng Wan Chai 灣仔 Wānzǐ Wāanjái Hong Kong Cemetery 香港墳場 Xiānggǎng féncháng Hēunggóng fàhnchèung Happy Valley 跑馬地 Pǎomǎdì Paaúmàhdeí Hong Kong China Ferry Terminal 中港碼頭 Zhōnggǎng mǎtóu Jūnggóng máhtàuh GUANGDONG Canton [province], Kwangtung 廣東 Guǎngdōng Gwóngdūng Canton [city], Kwangchow (Foo) 廣州(府) Guǎngzhōu(fǔ) Gwóngjāu(fú) Pearl River Delta 珠江三角洲 Zhūjiāng sānjiǎo zhōu Jyūgōng sāamgok jāu Sze Yap, See Yup, Four Counties 四邑 Sìyì Seiyāp Wuyi, Five Counties 五邑 Wǔyì Ńghyāp Sam Yap, Three Counties 三邑 Sānyì Sāamyāp JIANGMEN Kongmoon, Jiangmen 江門 Jiāngmén Gōngmùhn Jiangmen Port 江門港 Jiāngméngǎng Gōngmùhngóng Xi River, West River 西江 Xījiāng Sāigōng Gōngmùhn Ńghyāp Wuyi Museum of Overseas Chinese, 江門五邑華僑華人博 Jiāngmén Wǔyì huàqiáo wahkìuh wahyàhn Jiangmen Museum 物馆 huàrén bówùguǎn bokmahtgún KAIPING Hoiping, Kaiping 開平 Kāipíng Hōipèhng Kaiping diaolou (watchtowers) 開平碉樓 Kāipíng diāolóu Hōipèhng dīulàuh Tangkou 塘口 Tángkǒu Tòhngháu Cangdong [Tse village] 倉東 Cāngdōng Chōngdūng Chōngdūng gāauyuhk Cangdong Heritage Education Centre 倉東教育基地 Cāngdōng jiàoyu jīdì gēideih Li Yuan, Li Garden 立園 Lìyuán Laahpyùhn Chek Ham, Chikan 赤坎 Chìkǎn Chekhām Tan River 潭江 Tán Jiāng Tàahm gōng Zili 自力 Zìlì Jihlihk Dik Hoy, Dihai 荻海 Díhǎi Dihkhói Fengcai Hall 風采堂 Fēngcǎitáng Fūngchóitòhng Majianglong 馬降龍 Mǎjiànglóng Máhgonglùhng Yueshan -
Study on the Stable Isotopes in Surface Waters of the Naqu River Basin, Tibetan Plateau
ESEARCH ARTICLE R ScienceAsia 44 (2018): 403–412 doi: 10.2306/scienceasia1513-1874.2018.44.403 Study on the stable isotopes in surface waters of the Naqu River basin, Tibetan Plateau a,b b b b, b b Guoqiang Dong , Baisha Weng , Tianling Qin , Denghua Yan ∗, Hao Wang , Boya Gong , Wuxia Bib,c, Jianwei Wangb a College of Environmental Science and Engineering, Donghua University, Shanghai 201620 China b State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038 China c College of Hydrology and Water Resources, Hohai University, Nanjing 210098 China ∗Corresponding author, e-mail: [email protected] Received 30 Jan 2018 Accepted 3 Nov 2018 ABSTRACT: To enhance our understanding of the regional hydroclimate in the Central Tibetan Plateau, different types of water samples were collected across the Naqu River basin in the summer (July, August) and winter (January, December) of 2017 for isotopic analysis. With Cuona Lake as the demarcation point, the δ18O values of the river water increased initially and then decreased from upstream to downstream along the river’s mainstream. In the Naqu River system, a general decrease of δ18O values in the trunk stream of the lower reaches (from the head of Cuona Lake) was revealed owing to the gradual dilution of increased isotopically-depleted tributary inflow. Lakes play an important role in regulating runoff and changes in the levels of stable isotopes in rivers or streams. Additionally, the decrease of δ18O is controlled by processes involved in the ‘isotopic altitude effect’. -
Origin and Character of Loesslike Silt in the Southern Qinghai-Xizang (Tibet) Plateau, China
Origin and Character of Loesslike Silt in the Southern Qinghai-Xizang (Tibet) Plateau, China U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1549 Cover. View south-southeast across Lhasa He (Lhasa River) flood plain from roof of Potala Pal ace, Lhasa, Xizang Autonomous Region, China. The Potala (see frontispiece), characteristic sym bol of Tibet, nses 308 m above the valley floor on a bedrock hill and provides an excellent view of Mt. Guokalariju, 5,603 m elevation, and adjacent mountains 15 km to the southeast These mountains of flysch-like Triassic clastic and volcanic rocks and some Mesozoic granite character ize the southernmost part of Northern Xizang Structural Region (Gangdese-Nyainqentanglha Tec tonic Zone), which lies just north of the Yarlung Zangbo east-west tectonic suture 50 km to the south (see figs. 2, 3). Mountains are part of the Gangdese Island Arc at south margin of Lhasa continental block. Light-tan areas on flanks of mountains adjacent to almost vegetation-free flood plain are modern and ancient climbing sand dunes that exhibit evidence of strong winds. From flood plain of Lhasa He, and from flood plain of much larger Yarlung Zangbo to the south (see figs. 2, 3, 13), large dust storms and sand storms originate today and are common in capitol city of Lhasa. Blowing silt from larger braided flood plains in Pleistocene time was source of much loesslike silt described in this report. Photograph PK 23,763 by Troy L. P6w6, June 4, 1980. ORIGIN AND CHARACTER OF LOESSLIKE SILT IN THE SOUTHERN QINGHAI-XIZANG (TIBET) PLATEAU, CHINA Frontispiece. -
Imperial China and the West Part I, 1815–1881
China and the Modern World: Imperial China and the West Part I, 1815–1881 The East India Company’s steamship Nemesis and other British ships engaging Chinese junks in the Second Battle of Chuenpi, 7 January 1841, during the first opium war. (British Library) ABOUT THE ARCHIVE China and the Modern World: Imperial China and the West Part I, 1815–1881 is digitised from the FO 17 series of British Foreign Office Files—Foreign Office: Political and Other Departments: General Correspondence before 1906, China— held at the National Archives, UK, providing a vast and significant primary source for researching every aspect of Chinese-British relations during the nineteenth century, ranging from diplomacy to trade, economics, politics, warfare, emigration, translation and law. This first part includes all content from FO 17 volumes 1–872. Source Library Number of Images The National Archives, UK Approximately 532,000 CONTENT From Lord Amherst’s mission at the start of the nineteenth century, through the trading monopoly of the Canton System, and the Opium Wars of 1839–1842 and 1856–1860, Britain and other foreign powers gradually gained commercial, legal, and territorial rights in China. Imperial China and the West provides correspondence from the Factories of Canton (modern Guangzhou) and from the missionaries and diplomats who entered China in the early nineteenth century, as well as from the envoys and missions sent to China from Britain and the later legation and consulates. The documents comprising this collection include communications to and from the British legation, first at Hong Kong and later at Peking, and British consuls at Shanghai, Amoy (Xiamen), Swatow (Shantou), Hankow (Hankou), Newchwang (Yingkou), Chefoo (Yantai), Formosa (Taiwan), and more. -
PRC: Anhui Chao Lake Environmental Rehabilitation Project
Due Diligence Report of Environment Project Number: 44036 September 2015 PRC: Anhui Chao Lake Environmental Rehabilitation Project Prepared by Anhui Provincial Project Management Office (APPMO) For Subproject H1 Hefei City Binhu New District Beilaowei Environment Improvement Subproject L1 Chao Lake Basin Lu’an Eastern New Town District Water Environment Improvement Subproject WW1 Wuwei County Wucheng Water Environment (Wuwei Section of Xi River) Integrated Improvement This due diligence report of environment is a document of the borrower. The views expressed herein do not necessarily represent those of ADB’s Board of Directors, Management, or staff, and may be preliminary in nature. In preparing any country program or strategy, financing any project, or by making any designation of or reference to a particular territory or geographic area in this document, the Asian Development Bank does not intend to make any judgments as to the legal or other status of any territory or area. CURRENCY EQUIVALENT $1 = CNY6.3549 (on 3 September 2015) ABBREVIATIONS ADB - Asian Development Bank A2/0 - Anaerobic-anoxic-oxic AP - Affected Person APG - Anhui Provincial Government As - Arsenic BOD5 - 5-day biochemical oxygen demand Cd - Cadmium CLMA - Chao Lake Management Authority CNY - Chinese Yuan COD - Chemical oxygen demand Cr - Chromium DFR - Draft final report DMF - Design and Monitoring Framework DRC - Development and Reform Commission EA - Executing Agency EFS - Engineering Feasibility Study EHS - Environmental Health and Safety EIA - Environmental -
Genetic Structure and Eco-Geographical Differentiation of Lancea Tibetica in the Qinghai-Tibetan Plateau
G C A T T A C G G C A T genes Article Genetic Structure and Eco-Geographical Differentiation of Lancea tibetica in the Qinghai-Tibetan Plateau Xiaofeng Chi 1,2 , Faqi Zhang 1,2,* , Qingbo Gao 1,2, Rui Xing 1,2 and Shilong Chen 1,2,* 1 Key Laboratory of Adaptation and Evolution of Plateau Biota, Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Xining 810001, China; [email protected] (X.C.); [email protected] (Q.G.); [email protected] (R.X.) 2 Qinghai Provincial Key Laboratory of Crop Molecular Breeding, Xining 810001, China * Correspondence: [email protected] (F.Z.); [email protected] (S.C.) Received: 14 December 2018; Accepted: 24 January 2019; Published: 29 January 2019 Abstract: The uplift of the Qinghai-Tibetan Plateau (QTP) had a profound impact on the plant speciation rate and genetic diversity. High genetic diversity ensures that species can survive and adapt in the face of geographical and environmental changes. The Tanggula Mountains, located in the central of the QTP, have unique geographical significance. The aim of this study was to investigate the effect of the Tanggula Mountains as a geographical barrier on plant genetic diversity and structure by using Lancea tibetica. A total of 456 individuals from 31 populations were analyzed using eight pairs of microsatellite makers. The total number of alleles was 55 and the number per locus ranged from 3 to 11 with an average of 6.875. The polymorphism information content (PIC) values ranged from 0.2693 to 0.7761 with an average of 0.4378 indicating that the eight microsatellite makers were efficient for distinguishing genotypes. -
Mercury Accumulation in Vegetable Houttuynia Cordata Thunb. from Two
www.nature.com/scientificreports OPEN Mercury accumulation in vegetable Houttuynia cordata Thunb. from two diferent geological areas in southwest China and implications for human consumption Qingfeng Wang1,2*, Zhonggen Li1,2, Xinbin Feng2, Ao Wang4, Xinyu Li2,3, Dan Wang1 & Leilei Fan1 Houttuynia cordata Thunb. (HCT) is a common vegetable native to southwest China, and grown for consumption. The results suggested that THg contents in all parts and MeHg in underground parts of HCT in Hg mining areas were much higher than those in non-Hg mining areas. The highest THg and MeHg content of HCT were found in the roots, followed by the other tissues in the sequence: roots > leaves > rhizomes > aboveground stems (THg), and roots > rhizomes > aboveground stems > leaves (MeHg). The average THg bioaccumulation factor (BCF) of HCT root in the Hg mining area and in non-Hg mining areas could reach 1.02 ± 0.71 and 0.99 ± 0.71 respectively, indicating that HCT is a Hg accumulator. And the THg and MeHg contents in all tissues of HCT, including the leaves, were signifcantly correlated with THg and MeHg content in the soil. Additionally, preferred dietary habits of HCT consumption could directly afect the Hg exposure risk. Consuming the aboveground parts (CAP) of HCT potentially poses a high THg exposure risk and consuming the underground parts (CUP) may lead to a relatively high MeHg exposure risk. Only consuming the rhizomes (OCR) of the underground parts could signifcantly reduce the exposure risk of THg and to some extent of MeHg. In summary, HCT should not be cultivated near the Hg contaminated sites, such as Hg tailings, as it is associated with a greater risk of Hg exposure and high root Hg levels, and the roots should be removed before consumption to reduce the Hg risk. -
Numerical Experiment on Impact of Anomalous Sst Warming in Kuroshio Extension in Previous Winter on East Asian Summer Monsoon
Vol.17 No.1 JOURNAL OF TROPICAL METEOROLOGY March 2011 Article ID: 1006-8775(2011) 01-0018-09 NUMERICAL EXPERIMENT ON IMPACT OF ANOMALOUS SST WARMING IN KUROSHIO EXTENSION IN PREVIOUS WINTER ON EAST ASIAN SUMMER MONSOON 1, 2 1 1 3 WANG Xiao-dan (王晓丹) , ZHONG Zhong (钟 中) , TAN Yan-ke (谭言科) , DU Nan (杜 楠) (1. Institute of Meteorology, PLA University of Science and Technology, Nanjing 211101 China; 2. Institute of Aeronautical Meteorology, Air force Academy of Equipment, Beijing 100085 China; 3. Meteorological Center in Chengdu Air Command, Chengdu 610041 China) Abstract: The impact of anomalous sea surface temperature (SST) warming in the Kuroshio Extension in the previous winter on the East Asian summer monsoon (EASM) was investigated by performing simulation tests using NCAR CAM3. The results show that anomalous SST warming in the Kuroshio Extension in winter causes the enhancement and northward movement of the EASM. The monsoon indexes for East Asian summer monsoon and land-sea thermal difference, which characterize the intensity of the EASM, show an obvious increase during the onset period of the EASM. Moreover, the land-sea thermal difference is more sensitive to warmer SST. Low-level southwesterly monsoon is clearly strengthened meanwhile westerly flows north (south) of the subtropical westerly jet axis are strengthened (weakened) in northern China, South China Sea, and the Western Pacific Ocean to the east of the Philippines. While there is an obvious decrease in precipitation over the Japanese archipelago and adjacent oceans and over the area from the south of the Yangtze River in eastern China to the Qinling Mountains in southern China, precipitation increases notably in northern China, the South China Sea, the East China Sea, the Yellow Sea, and the Western Pacific to the east of the Philippines. -
Interaction and Social Complexity in Lingnan During the First Millennium B.C
Interaction and Social Complexity in Lingnan during the First Millennium B.C. FRANCIS ALLARD SEPARATED FROM AREAS north of it by mountain ranges and drained by a single river system, the region of Lingnan in southeastern China is a distinct physio graphic province (Fig. 1). The home of historically recorded tribes, it was not until the late first millennium B.C. that Lingnan was incorporated into the ex panding Chinese polities of central and northern China. The Qin, Han, and probably the Chu before them not only knew of those they called barbarians in southeastern China but also pursued an expansionary policy that would help es tablish the boundaries of the modem Chinese state in later times. The first millennium B.C. in Lingnan witnessed the development of a bronze metallurgy and its subsequent widespread use by the seventh or sixth centuries B.C. Archaeological work over the last decades has led to the discovery of a num ber ofBronze Age burials scattered over much of northern Lingnan and dating to approximately 600 to 200 B.C., a period covering the middle-late Spring and Autumn period and all of the Warring States period (Fig. 2). These important discoveries have helped establish the region as the theater for the emergence of social complexity before the arrival of the Qin and Han dynasties in Lingnan. Nevertheless, and in keeping with traditional models of interpretation, Chinese archaeologists have tried to understand this material in the context of contact with those expanding states located to the north of Lingnan. The elaborate ma terial culture and complex political structures associated with these states has usually meant that change in those so-called peripheral areas (including Lingnan) could only be the result of cultural diffusion from the center. -
Transport Corridors and Regional Balance in China: the Case of Coal Trade and Logistics Chengjin Wang, César Ducruet
Transport corridors and regional balance in China: the case of coal trade and logistics Chengjin Wang, César Ducruet To cite this version: Chengjin Wang, César Ducruet. Transport corridors and regional balance in China: the case of coal trade and logistics. Journal of Transport Geography, Elsevier, 2014, 40, pp.3-16. halshs-01069149 HAL Id: halshs-01069149 https://halshs.archives-ouvertes.fr/halshs-01069149 Submitted on 28 Sep 2014 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. Transport corridors and regional balance in China: the case of coal trade and logistics Dr. Chengjin WANG Key Laboratory of Regional Sustainable Development Modeling Institute of Geographical Sciences and Natural Resources Research Chinese Academy of Sciences, Beijing 100101, China Email: [email protected] Dr. César DUCRUET1 National Centre for Scientific Research (CNRS) UMR 8504 Géographie-cités F-75006 Paris, France Email: [email protected] Pre-final version of the paper published in Journal of Transport Geography, special issue on “The Changing Landscapes of Transport and Logistics in China”, Vol. 40, pp. 3-16. Abstract Coal plays a vital role in the socio-economic development of China. Yet, the spatial mismatch between production centers (inland Northwest) and consumption centers (coastal region) within China fostered the emergence of dedicated coal transport corridors with limited alternatives. -
Simulating the Route of the Tang-Tibet Ancient Road for One Branch of the Silk Road Across the Qinghai-Tibet Plateau
RESEARCH ARTICLE Simulating the route of the Tang-Tibet Ancient Road for one branch of the Silk Road across the Qinghai-Tibet Plateau 1 1 2 3 1 Zhuoma Lancuo , Guangliang HouID *, Changjun Xu , Yuying Liu , Yan Zhu , Wen Wang4, Yongkun Zhang4 1 Key Laboratory of Physical Geography and Environmental Process, College of Geography, Qinghai Normal University, Xining, Qinghai Province, China, 2 Key Laboratory of Geomantic Technology and Application of Qinghai Province, Provincial geomantic Center of Qinghai, Xining, Qinghai Province, China, 3 Department of a1111111111 computer technology and application, Qinghai University, Xining, Qinghai Province, China, 4 State Key a1111111111 Laboratories of Plateau Ecology and Agriculture, Qinghai University, Xining, Qinghai Province, China a1111111111 a1111111111 * [email protected] a1111111111 Abstract As the only route formed in the inner Qinghai-Tibet plateau, the Tang-Tibet Ancient Road OPEN ACCESS promoted the extension of the Overland Silk Roads to the inner Qinghai-Tibet plateau. Con- Citation: Lancuo Z, Hou G, Xu C, Liu Y, Zhu Y, sidering the Complex geographical and environmental factors of inner Qinghai-Tibet Pla- Wang W, et al. (2019) Simulating the route of the teau, we constructed a weighted trade route network based on geographical integration Tang-Tibet Ancient Road for one branch of the Silk Road across the Qinghai-Tibet Plateau. PLoS ONE factors, and then adopted the principle of minimum cost and the shortest path on the net- 14(12): e0226970. https://doi.org/10.1371/journal. work to simulate the ancient Tang-Tibet Ancient Road. We then compared the locations of pone.0226970 known key points documented in the literature, and found a significant correspondence in Editor: Wenwu Tang, University of North Carolina the Qinghai section. -
79397-89388 Payment for Watershed Services.Pdf
United Nations Development Programme Country: China PROJECT DOCUMENT Payment for Watershed Services in the Chishui River Basin for the Project Title: Conservation of Globally Significant Biodiversity UNDAF Outcome 1: Government and other stakeholders ensure environmental sustainability, Outcome(s): address climate change, and promote a green, low carbon economy Expected CP Outcome(s): Outcome 4: Low carbon and other environmentally sustainable strategies and technologies are adapted widely to meet China’s commitments and compliance with Multilateral Environmental Agreements; and Outcome 5. The vulnerability of poor communities and ecosystems to climate change is reduced Expected CPAP Output (s): Output 4.1 Policy and capacity barriers for the sustained and widespread adoption of low carbon and other environmentally sustainable strategies and technologies removed, and Output 5.1 A strengthened policy, legal, institutional framework for the sustainable use of land, water, the conservation of biodiversity, and other natural resources in fragile ecosystems is enforced. Executing Entity/Implementing Partner: Ministry of Environmental Protection Implementing Ent ity/Responsible Partners: Environmental Protection Department of Guizhou Brief Description The Chishui River is one of the most important tributaries of the upper Yangtze River, because of its diverse landscapes, richness in biodiversity and abundance in water resources. It is the only major tributary of the Upper Yangtze that remains free-flowing without a mainstream dam. The Chishui River Basin (CRB) is an important storehouse of biodiversity, lying within the Upper Yangtze Freshwater Ecoregion and the Guizhou Plateau Broadleaf and Mixed Forests Terrestrial Ecoregion. The basin also lies on the eastern margin of the Mountains of Southwest China biodiversity hotspot, and contains part of the China Danxia World Heritage Site.