Protection Efficacy of National Wetland Reserves in China
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Environmental Changes in Chaohu Lake (Southeast, China) Since the Mid 20Th Century: the Interactive Impacts of Nutrients, Hydrology and Climate
Limnologica 43 (2013) 10–17 Contents lists available at SciVerse ScienceDirect Limnologica journal homepage: www.elsevier.com/locate/limno Environmental changes in Chaohu Lake (southeast, China) since the mid 20th century: The interactive impacts of nutrients, hydrology and climate Xu Chen a,b, Xiangdong Yang a,∗, Xuhui Dong a, Enfeng Liu a a State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, People’s Republic of China b Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, People’s Republic of China article info abstract Article history: Chaohu Lake, the fifth largest freshwater lake in the Yangtze floodplain, is faced with multiple stresses Received 21 June 2011 from anthropogenic disturbances and climate change. To explore the ecological changes in Chaohu Lake Received in revised form 31 October 2011 since the mid 20th century, we examined diatoms, geochemical indicators and particle size in 210Pb- Accepted 6 March 2012 dated sediment core from the lake. Diatom succession revealed that the lake had switched to a eutrophic Available online 11 June 2012 state since the late 1970s. Redundancy analysis using limnological data, hydrological and meteorological variables showed that sedimentary total phosphorus (TP) and total organic carbon (TOC), annual mean Keywords: temperature, annual mean wind velocity, and water-level amplitude (WLA) were five significant factors Diatoms Nutrient loading influencing diatom succession. Diatom assemblages from 1950 till 1978 were driven by WLA and wind. Hydrological alteration The establishment of Chaohu Dam baffled hydrological connectivity between the lake and the Yangtze Climate warming River in 1962, and reducing water exchange-induced flow. -
Supplement of a Systematic Examination of the Relationships Between CDOM and DOC in Inland Waters in China
Supplement of Hydrol. Earth Syst. Sci., 21, 5127–5141, 2017 https://doi.org/10.5194/hess-21-5127-2017-supplement © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Supplement of A systematic examination of the relationships between CDOM and DOC in inland waters in China Kaishan Song et al. Correspondence to: Kaishan Song ([email protected]) The copyright of individual parts of the supplement might differ from the CC BY 3.0 License. Figure S1. Sampling location at three rivers for tracing the temporal variation of CDOM and DOC. The average widths at sampling stations are about 1020 m, 206m and 152 m for the Songhua River, Hunjiang River and Yalu River, respectively. Table S1 the sampling information for fresh and saline water lakes, the location information shows the central positions of the lakes. Res. is the abbreviation for reservoir; N, numbers of samples collected; Lat., latitude; Long., longitude; A, area; L, maximum length in kilometer; W, maximum width in kilometer. Water body type Sampling date N Lat. Long. A(km2) L (km) W (km) Fresh water lake Shitoukou Res. 2009.08.28 10 43.9319 125.7472 59 17 6 Songhua Lake 2015.04.29 8 43.6146 126.9492 185 55 6 Erlong Lake 2011.06.24 6 43.1785 124.8264 98 29 8 Xinlicheng Res. 2011.06.13 7 43.6300 125.3400 43 22 6 Yueliang Lake 2011.09.01 6 45.7250 123.8667 116 15 15 Nierji Res. 2015.09.16 8 48.6073 124.5693 436 83 26 Shankou Res. -
Family-Sisoridae-Overview-PDF.Pdf
FAMILY Sisoridae Bleeker, 1858 - sisorid catfishes SUBFAMILY Sisorinae Bleeker, 1858 - sisorid catfishes [=Sisorichthyoidei, Bagarina, Nangrina] GENUS Ayarnangra Roberts, 2001 - sisorid catfishes Species Ayarnangra estuarius Roberts, 2001 - Irrawaddy ayarnangra GENUS Bagarius Bleeker, 1853 - sisorid catfishes Species Bagarius bagarius (Hamilton, 1822) - goonch, dwarf goonch [=buchanani, platespogon] Species Bagarius rutilus Ng & Kottelat, 2000 - Red River goonch Species Bagarius suchus Roberts, 1983 - crocodile catfish Species Bagarius yarrelli (Sykes, 1839) - goonch, giant devil catfish [=carnaticus, lica, nieuwenhuisii] GENUS Caelatoglanis Ng & Kottelat, 2005 - sisorid catfishes Species Caelatoglanis zonatus Ng & Kottelat, 2005 - Chon Son catfish GENUS Conta Hora, 1950 - sisorid catfishes Species Conta conta (Hamilton, 1822) - Mahamanda River catfish [=elongata] Species Conta pectinata Ng, 2005 - Dibrugarh catfish GENUS Erethistes Muller & Troschel, 1849 - sisorid catfishes [=Hara, Laguvia] Species Erethistes filamentosus (Blyth, 1860) - Megathat Chaung catfish [=maesotensis] Species Erethistes hara (McClelland, 1843) - Hooghly River catfish [=asperus, buchanani, saharsai, serratus] Species Erethistes horai (Misra, 1976) - Terai catfish Species Erethistes jerdoni (Day, 1870) - Sylhet catfish Species Erethistes koladynensis (Anganthoibi & Vishwanath, 2009) - Koladyne River catfish Species Erethistes longissimus (Ng & Kottelat, 2007) - Mogaung catfish Species Erethistes mesembrinus (Ng & Kottelat, 2007) - Langkatuek catfish Species Erethistes -
Determination of Geochronology and Sedimentation Rates of Shallow Lakes in the Middle Yangtze Reaches Using 210Pb, 137Cs and Spheroidal Carbonaceous Particles
Determination of geochronology and sedimentation rates of shallow lakes in the middle Yangtze reaches using 210Pb, 137Cs and spheroidal carbonaceous particles Xu Chen1*, Qianglong Qiao1, Suzanne McGowan2, Linghan Zeng1,2, Mark A Stevenson3, Lei Xu1, Chunling Huang1, Jia Liang1, Yanmin Cao4 1State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China 2School of Geography, University of Nottingham, Nottingham NG7 2RD, UK 3School of Natural and Environmental Sciences, Newcastle University, Newcastle- upon-Tyne NE1 7RU, UK 4College of Resources and Environmental Science, South-Central University for Nationalities, Wuhan 430074, China *Corresponding author; e-mail address: [email protected] https://doi.org/10.1016/j.catena.2018.11.041 Catena Abstract: Accurate chronologies for recent sediments of shallow lakes in the Yangtze floodplain are critical to calibrate proxy records for reconstructing environmental changes during the past century. This study presents the results of detailed 210Pb analysis from eight lake sediment cores collected from the middle Yangtze reaches, 210 southeast China. Unsupported Pb activities generally declined exponentially with mass depth in the eight cores. The chronologies and sedimentation rates for the sediment cores were calculated using different 210Pb-based mathematical models. The 137Cs chronomarker (i.e. the 1963 fallout peak) and the spheroidal carbonaceous particle (SCP) chronomarker (i.e. the start of the rapid increase in 1970 AD) were selected to validate the 210Pb dating. Sedimentation rates derived from different models were validated using historical data including lake area, arable land area, sediment discharge and reservoir volume in the Yangtze basin. The SCP-corrected CRS (constant rate of supply) model performs better than other models, based on validation using historical documents in the Yangtze basin. -
Flood Control for the Red River [Vietnam]
Total Disaster Risk Management - Good Practices - Chapter 3 Vietnam Flood Control for the Red River The Red River, the Delta and Floods The history of the development of Vietnamese civilizations is closely linked to the Red River (Hong River) Delta. As the second largest granary of Vietnam, the Delta holds a significant meaning in the life of the Vietnamese people. This is where approximately 15–20 % of Vietnam’s rice is produced. A population of 17 million now inhabits the 16,500-km2 area of the Red River Delta. The catchment area of the Red River is estimated at 169,000 km2, half of which lies in China. The Red River at Hanoi comprises three major tributary systems, the Da, Thao and Lo Rivers. The river is the source of various positive aspects for human life, such as water resources and rich alluvium (it is called the Red River as the large amount of alluvium it carries colors it red all year round). However, these go hand in hand with a much less expected occurrence: floods. Increased flash floods as a result of deforestation in the upstream parts of the Red River basin, and raised bed levels of the rivers due to the deposition of sediment, are causing higher flood levels, endangering the ever increasing socio-economic value of the capital. The land in low-lying areas of the river delta is protected against flooding by river dyke systems. According to official historical records, in 1108, King Ly Nhan Tong ordered the construction of the first dyke with solid foundations on a large scale aimed at protecting the capital of Thang Long (now Hanoi). -
Diatom Community Succession and Nutrient Evolution Recorded from a Sediment Core of the Longgan Lake, a Large Shallow Lake in East China
第 30 卷 第 6 期 水 生 生 物 学 报 Vol . 30 ,No . 6 2 0 0 6 年 1 1 月 ACTA HYDROBIOLOGICA SINICA Nov. , 2 0 0 6 DIATOM COMMUNITY SUCCESSION AND NUTRIENT EVOLUTION RECORDED FROM A SEDIMENT CORE OF THE LONGGAN LAKE, A LARGE SHALLOW LAKE IN EAST CHINA DONG Xu2Hui and YANG Xiang2Dong ( Nanjing Institute of Geography &Limnology , the Chinese Academy of Sciences , Nanjing 210008 , China) Abstract :The Longgan Lake is a shallow mesotrophic macrophyted2ominated lake. According to the high2resolution diatom research from its sediment core , the diatom community succession was built , and the total phosphorus (TP) and chlorophyll2a (Chl2a) con2 centration were quantitatively reconstructed for the past 2000 years , based on the diatom2TP and diatom2Chla transfer functions. The shifts of diatom assemblages also mirrored the developments of aquatic plant , reflecting the characters of aquatic ecosystem evolution. The inferred epilimnetic TP concentration fluctuated within a small range of 36 to 62μg/ L , indicating the lake remained a relative stable mesotrophic status in the long historical period. The periodical variations of the diatom assemblage and trophic sta2 tus suggest a mitigating function of shallow macrophyte2dominated lakes to nutrient input. The changes of lakesptrophic status donpt linearly respond to the human disturbance in the catchment. The dynamics mechanism of phosphorus in macrophyte2dominated lakes , as inferred from diatoms , will provide a scientific foundation for the prediction of trophic status change in a shallow lake , as well as the lake ecological restoration and management decisions. Key words :Diatom assemblage ; Nutrient ; Quantitative reconstruction ; Aquatic macrophyte ; Longgan Lake CLC number :X172 Document code :A Article ID :100023207(2006) 0620702209 The importance of aquatic vegetation to the ecologi2 on the environment reconstruction based on the sediment cal restoration has been recognized commonly by limnolo2 biomarker such as diatom have made rapid gists and lake managements[1 —4 ] . -
APPENDIX 6D Profile of the Inland Waterway Master Plan Projects
APPENDIX 6D Profile of the Inland Waterway Master Plan Projects ANNEX 6D Profile of the Inland Waterway Master Plan Projects A. Ongoing/Committed Project Profile Project Name: Sector: Upgrading of Northern Trans Mekong corridor (to Class III) (253km) CW01 Project Background & Objective: None of the corridors provide good transport continuity at present , and improvements will help improve region – wide accessibility re- lieve congestion on the main corridors, reduce transportation costs and supports economic development in the provinces. Project Description: (i) To improve the standard (up to Class III/300DWT vessels) and connectivity of the canal network in Northern Trans Mekong corri- dor(253km):Dredging, bank protection, ship lock, bridge improvements, navigation aids for 24-hour navigation, as one of the com- ponents of Development of transport infrastructure of Mekong River Delta. (ii) Main Project Components is Dredging, Bank protection, Improving and building bridges, Enhancing alarming system, Building Rach Chanh Dock and Building Tan Chau Port: Estimated Cost (2009): Original Schedule: US 99.3 million (including CW02) 2009–2015 Financial Source: Implementation Agency World Bank , Vietnam VIWA 6D-1 Project Name: Sector: Updating of Southern coastal corridor (to Class III) (153km) CW02 Project Background & Objective: This improvements will help improve region –wide accessibility, relieve congestion on the main corridors, reduce transportation costs and support economic development in the province. Project Description: (i) To improve the standard (up to Class III/300DWT vessels) and connectivity of the canal network in the southern coastal corri- dor(153km) (ii) Location is Gia Rai–Bac Liec–Dai Ngai (103km) and Cho Gao Canal (50km) (iii) Main components are as follows: Dredging, bank protections, ship lock, bridge improvements, navigation aids for 24-hour naviga- tion .These are one of the components of Development of transport infrastructure of Mekong River Delta. -
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Report on the State of the Environment in China 2016
2016 The 2016 Report on the State of the Environment in China is hereby announced in accordance with the Environmental Protection Law of the People ’s Republic of China. Minister of Ministry of Environmental Protection, the People’s Republic of China May 31, 2017 2016 Summary.................................................................................................1 Atmospheric Environment....................................................................7 Freshwater Environment....................................................................17 Marine Environment...........................................................................31 Land Environment...............................................................................35 Natural and Ecological Environment.................................................36 Acoustic Environment.........................................................................41 Radiation Environment.......................................................................43 Transport and Energy.........................................................................46 Climate and Natural Disasters............................................................48 Data Sources and Explanations for Assessment ...............................52 2016 On January 18, 2016, the seminar for the studying of the spirit of the Sixth Plenary Session of the Eighteenth CPC Central Committee was opened in Party School of the CPC Central Committee, and it was oriented for leaders and cadres at provincial and ministerial -
Back Matter (PDF)
Index Page numbers in italics refer to Figures. Page numbers in bold refer to Tables. acoustic Doppler current profiler (ADCP) 156, 182 Bulimina spp. 202, 202, 205, 206 agriculture, impact on weathering 48 butterfly delta 2, 90 anthropogenic impact 5–6, 15 Diaokou lobe 191–192, 192 13C isotope analysis 198 Lingdingyang Bay 182 14C age measurement Pearl River delta sediments 48 Beibu Gulf 92, 92, 95, 96 apatite fission track (AFT), provenance evidence southern mud depocentre 90 18–20, 23 Diaokou lobe sediments 188 40Ar/39Ar dating, role in provenance studies 20–21 Gulf of Tonkin 75 offshore cores 212, 215 Baiyun Sag 32, 33 offshore Hainan Island Bashi Straits 9, 10 method 102 10Be date 199 results 104, 104 Beibu Gulf 100, 101 Cangzhou rise 186 geological setting 88–90 carbonate location 87 offshore Hainan Island sediment study map 88 methods 104 sea-level change post glacial 101–102 results 110 sediment movement 2 South China Sea sediment 200 southern mud depocentre 89 Cassidulina carinata 202, 205, 206 sediment study Cathaysia Block 123, 124 methods 90 Cathaysia (South China) terrane 11, 12,19 results Central Yellow Sea Mud 88 14C dating 92, 92, 95, 96 Changjiang (Yangtze) River 88, 224, 225, 225, 226 geochemistry 93–95, 94 catchment climate 140 lithology 93 catchment geology 139–140 seismic profiles 90, 91,92–93 delta sedimentary system 233, 234, 236, 237, 248, 249 results discussed 96–97 discharge pattern 156, 230, 231 Beijiang River 32, 33 gravity flow 231 Beipanjiang River 32, 33 history of inputs to East China Sea 140 Bohai Basin 186 -
Ge/Si Ratios Indicating Hydrothermal and Sulfide Weathering Input To
Chemical Geology 410 (2015) 40–52 Contents lists available at ScienceDirect Chemical Geology journal homepage: www.elsevier.com/locate/chemgeo Ge/Si ratios indicating hydrothermal and sulfide weathering input to rivers of the Eastern Tibetan Plateau and Mt. Baekdu Yeongcheol Han a,1, Youngsook Huh a,⁎, Louis Derry b a School of Earth and Environmental Sciences, Seoul National University, Seoul 151-747, Korea. b Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, NY 14853, USA article info abstract Article history: Concentrations of dissolved silicon in river waters reflect a complex interplay among chemical weathering of pri- Received 6 February 2015 mary silicate minerals, formation and weathering of secondary clay minerals, hydrothermal input and biological Received in revised form 29 May 2015 cycling (formation and dissolution of opal phytoliths and growth of diatoms). We applied the Ge/Si ratio to assess Accepted 1 June 2015 the different sources of dissolved Si in rivers hailing from the eastern Tibetan Plateau — the Salween, Mekong, Available online 3 June 2015 Chang Jiang (Yangtze), Hong (Red) and Huang He (Yellow) and from Mt. Baekdu — the Duman. Elevated riverine Keywords: Ge/Si ratios were observed in arid regions with high geothermal activity in the Salween, Chang Jiang and Mt. fl Germanium Baekdu streams. In the Huang He and Hong River basins geothermal in uence was not as pronounced, but Silicon weathering of sulfide- and coal-bearing minerals may be responsible for the high Ge/Si ratios. In rivers where in- Chang Jiang puts from hydrothermal and sulfide weathering are minimal, our data mostly fall in the weathering-limited re- Mekong gime of high riverine Si concentrations and low Ge/Si ratios. -
• -Depth More Than 1.5M Figure 5C.15 Sai Gon–Moc Hoa Route (Ii) Sai
• -Depth more than 1.5m Figure 5C.15 Sai Gon–Moc Hoa Route Grade Width Depth No Route Length Obstacle Project Present Target Present Plan Present Plan Sai Gon–Moc Hoa mainly III & improvement: widening, S3-1 96 III 30–150 50–70 1.9–8.0 1.5 bridge (Vam Co River) partially I removal of obstacles (ii) Sai Gon–Ben Suc Route Location • Route from Sai Gon Port along Sai Gon River to Ho Dau Tieng Dam in Tay Ninh Province. • This route lies on Sai Gon River with length of 89km. Main Role • Connection between Binh Duong and Ho Chi Minh City. • Port areas of Sai Gon, Ben Nghe and Tan Cang Ports and channel to Ha Tien ce- ment factory (section from Te channel confluence to Thanh Da) • Transportation of sand, gravel and wood from upstream to ports at Ho Chi Minh and Binh Duong provinces Target • Grade III • Width 50–70m • Depth more than 1.5m 5C-15 Figure 5C.16 Sai Gon–Ben Suc Route Grade Width Depth No Route Length Obstacle Project Present Target Present Plan Present Plan Sai Gon–Ben Suc I and III, improvement: re- S3-2 89 III 70–200 50–70 2.5–13.2 1.5 bridge (SaiGon River) partially II moval of obstacles (iii) Sai Gon–Ben Keo Route Location • Route between the northern area of Dong Thap Muoi with Ho Chi Minh City via rivers of Sai Gon, Nha Be, Soai Rap, Can Giuoc and Vam Co as well as Nuoc Man canal to Ben Keo on Vam Co Dong River with 165.7km in length Main Role • Connection of Tay Ninh and Long An, and Ho Chi Minh City and Mekong through Tay Ninh Province • Transportation of wood and construction materials to Ho Chi Minh City • Transportation