How Important Are the Wetlands in the Middle-Lower Yangtze River Region: an Ecosystem Service Valuation Approach
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Space Structure of Smart Land Use in Maanshan Based on Buffer Extention
International Conference on Electrical, Mechanical and Industrial Engineering (ICEMIE 2016) Space Structure of Smart Land Use in Maanshan Based on Buffer Extention Shenmin Wang*, Qifang Ma, Wenqi Liu and Xinyue Zhang School of Geography and Remote Sensing, Nanjing University of Information Science & Technology, Nanjing 210044, China *Corresponding author Abstract—The research of land suitability evaluation based on proposed in Maanshan City Smart land use spatial structure GIS using buffer diffusion methods, to optimize the Ma ' Anshan optimization scheme. city’s intensive land-use spatial structure in order to achieve The highest land use efficiency, meet requirements of the smart use of land. Research results indicate that Ma ' Anshan Industrial land II. RESEARCH METHODS AND IDEAS should be radiate from the urban to the surrounding, some Industrial land in the urban area may converted into A. Research Methods corresponding commercial land and residential land, industrial 1) Suitability evaluation method in mining area should accumulated development to formed industrial zone , conurbation in southern area of the city should Land suitability evaluation is a specific type of spatial appropriately increased commercial land. location area problem. The main idea of GIS land suitability evaluation is for specific units of land, the reasonable division Keywords- land use; suitability evaluation;GIS; maanshan for a certain number of evaluation unit, the integration of multiple quantitative data of different impact factor for the I. INTRODUCTION evaluation unit of land use suitability of the influence degree. Finally, through the overlay will be different aspects of the Smart growth is a concept of urban planning, which economic, social and ecological factors was performed to gradually became popular in the United States in the late 1990s, quantify the effects of comprehensive, finally get the and was later cited and studied by scholars from various evaluation unit for a suitable quantitative evaluation of specific countries around the world [1-2]. -
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. -
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. -
Conservation Status Assessment and a New Method for Establishing Conservation Priorities for Freshwater Mussels
Received: 8 March 2018 Revised: 9 November 2019 Accepted: 17 December 2019 DOI: 10.1002/aqc.3298 RESEARCH ARTICLE Conservation status assessment and a new method for establishing conservation priorities for freshwater mussels (Bivalvia: Unionida) in the middle and lower reaches of the Yangtze River drainage Xiongjun Liu1,2 | Xue Yang3 | David T. Zanatta4 | Manuel Lopes-Lima5 | Arthur E. Bogan6 | Alexandra Zieritz7,8 | Shan Ouyang3 | Xiaoping Wu1,2,3 1Key Laboratory of Poyang Lake Environment and Resource Utilization, School of Resources Abstract Environmental and Chemical Engineering, 1. The freshwater mussel (Unionida) fauna of the Yangtze River is among the most Nanchang University, Nanchang, People's Republic of China diverse on Earth. In recent decades, human activities have caused habitat degra- 2School of Resources Environmental & dation in the river, and previous studies estimated that up to 80% of the mussel Chemical Engineering, Nanchang University, species in the Yangtze River are Threatened or Near Threatened with extinction. Nanchang, People's Republic of China 3School of Life Sciences, Nanchang University, However, a comprehensive and systematic evaluation of the conservation status Nanchang, People's Republic of China of this fauna has yet to be completed. 4 Central Michigan University, Institute for 2. This study evaluated the conservation status of the 69 recognized freshwater Great Lakes Research, Mount Pleasant, MI mussel species in the middle and lower reaches of the Yangtze River, using the 5CIBIO/InBIO – Research Center -
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 ] . -
Two Distinct Flyways with Different Population Trends Of
13 Two distinct flyways with different population trends of Bewick’s Swan Cygnus columbianus bewickii in East Asia LEI FANG1, JUNJIAN ZHANG2,3, QINGSHAN ZHAO2, DIANA SOLOVYEVA4, DIDIER VANGELUWE5, SONIA B. ROZENFELD6, THOMAS LAMERIS7, ZHENGGANG XU8, INGA BYSYKATOVA-HARMEY9, NYAMBAYAR BATBAYAR10, KAN KONISHI11, OUN-KYONG MOON12 , BU HE13, KAZUO KOYAMA14, SACHIKO MORIGUCHI15,16, TETSUO SHIMADA17, JINYOUNG PARK18, HWAJUNG KIM18, GUANHUA LIU19, BINHUA HU20, DALI GAO21, LUZHANG RUAN22, TSEVEENMYADAG NATSAGDORJ10, BATMUNKH DAVAASUREN10, ALEXEY ANTONOV23, ANASTASIA MYLNIKOVA4, ALEXANDER STEPANOV4,9, GEORGE KIRTAEV6, DMYTRY ZAMYATIN6, SAVAS KAZANTZIDIS24, TSUNEO SEKIJIMA15, IDERBAT DAMBA2,3, HANSOO LEE25, BEIXI ZHANG2,3, YANBO XIE26, EILEEN C. REES27, LEI CAO2,3,* & ANTHONY D. FOX28 1Life Sciences, University of Science and Technology of China, Hefei, China. 2State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, China. 3School of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China. 4Laboratory of Ornithology, Institute of Biological Problems of the North, Magadan, Russia. 5Royal Belgian Institute of Natural Sciences, Brussels, Belgium. 6Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences, Moscow, Russia. 7Department of Animal Ecology, Netherlands Institute of Ecology (NIOO-KNAW), Wageningen, Netherlands. 8Key Laboratory of Forestry Remote Sensing Based on Big Data & Ecological Security of Hunan Province, Central South University of Forestry and Technology, Changsha 410004, China. 9Institute of Biological Problems of Cryolitozone, Siberian Branch of the Russian Academy of Sciences, Yakutsk, Russia. 10Wildlife Sciences and Conservation Center of Mongolia, Union Building, B-701, UNESCO Str., Ulaanbaatar 14210, Mongolia. 11Hamatonbetsu Lake Kutcharo Waterfowl Observatory, Kutcharo-kohan, Hamatonbetsu-cho, Esashi-gun, Hokkaido 098-5739, Japan. -
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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 -
Potential Indicator Value of Subfossil Gastropods in Assessing the Ecological Health of the Middle and Lower Reaches of the Yangtze River Floodplain System (China)
geosciences Article Potential Indicator Value of Subfossil Gastropods in Assessing the Ecological Health of the Middle and Lower Reaches of the Yangtze River Floodplain System (China) Giri Kattel 1,2,3,*, Yongjiu Cai 1, Xiangdong Yang 1, Ke Zhang 1, Xu Hao 4, Rong Wang 1 and Xuhui Dong 5 1 State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology Chinese Academy of Sciences, Nanjing 210008, China; [email protected] (Y.C.); [email protected] (X.Y.); [email protected] (K.Z.); [email protected] (R.W.) 2 Environmental Hydrology and Water Resources Group, Department of Infrastructure Engineering, University of Melbourne, Melbourne, Parkville, VIC 3010, Australia 3 Department of Hydraulic Engineering, Tsinghua University, Beijing 100084, China 4 Hoan Environmental Monitoring Corporation, Nanjing 210008, China; [email protected] 5 School of Geographical Sciences, Gunagzhou University, Guangzhou 510006, China; [email protected] * Correspondence: [email protected]; Tel.: +61-428-171-180 Received: 20 April 2018; Accepted: 15 June 2018; Published: 17 June 2018 Abstract: The lakes across China’s middle and lower reaches of the Yangtze River system have a long history of sustaining human pressures. These aquatic resources have been exploited for fisheries and irrigation over millennia at a magnitude of scales, with the result that many lakes have lost their ecological integrity. The consequences of these changes in the ecosystem health of lakes are not fully understood; therefore, a long-term investigation is urgently needed. Gastropods (aquatic snails) are powerful bio-indicators that link primary producers, herbivores, and detritivores associated with macrophytes and grazers of periphyton and higher-level consumers. -
Bulletin on the Ecological and Environmental Monitoring Results of the Three Gorges Project 2004
Bulletin On the Ecological and Environmental Monitoring Results of the Three Gorges Project 2004 State Environmental Protection Administration May 2004 Content Summary..........................................................................................................................................1 Chapter 1 Progress of the Three Gorges Project..........................................................................2 Chapter 2 Economic and Social Development..............................................................................3 2.1 Population, Society and Economy ..........................................................................................3 2.2 Migration Settlement...............................................................................................................4 Chapter 3 State of the Natural Ecological Environment .............................................................6 3.1 Climate....................................................................................................................................6 3.2 Terrestrial Plants......................................................................................................................9 3.3 Terrestrial Animals..................................................................................................................9 3.4 Fishery Resources and Environment.....................................................................................10 3.5 Peculiar Fishes and Rare Aquatic Animals ...........................................................................13 -
Decline in Transparency of Lake Hongze from Long-Term MODIS Observations: Possible Causes and Potential Significance
remote sensing Article Decline in Transparency of Lake Hongze from Long-Term MODIS Observations: Possible Causes and Potential Significance Na Li 1,2,3, Kun Shi 2,3,4,*, Yunlin Zhang 2,3 , Zhijun Gong 2,3, Kai Peng 2,3, Yibo Zhang 2,3 and Yong Zha 1 1 Key Laboratory of Virtual Geographic Environment of Education Ministry, Nanjing Normal University, Nanjing 210023, China; [email protected] (N.L.); [email protected] (Y.Z.) 2 Taihu Lake Laboratory Ecosystem Station, State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China; [email protected] (Y.Z.); [email protected] (Z.G.); [email protected] (K.P.); [email protected] (Y.Z.) 3 University of Chinese Academy of Sciences, Beijing 100049, China 4 CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China * Correspondence: [email protected]; Tel.: (+86)-25-86882174 Received: 12 December 2018; Accepted: 12 January 2019; Published: 18 January 2019 Abstract: Transparency is an important indicator of water quality and the underwater light environment and is widely measured in water quality monitoring. Decreasing transparency occurs throughout the world and has become the primary water quality issue for many freshwater and coastal marine ecosystems due to eutrophication and other human activities. Lake Hongze is the fourth largest freshwater lake in China, providing water for surrounding cities and farms but experiencing significant water quality changes. However, there are very few studies about Lake Hongze’s transparency due to the lack of long-term monitoring data for the lake.