Study on the Spatial Differentiation of the Populations on Both Sides of the “Qinling-Huaihe Line” in China
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Review Statement of World Biosphere Reserve [ July 2013 ]
Review Statement of World Biosphere Reserve [ July 2013 ] Prefeace According to the Resolution 28 C/2.4 on Statutory Framework of MAB (Man and Biosphere) Program passed on the 28th session of the UNESCO General Conference, Article 4 has been clearly identified as the criteria which shall be followed by biosphere reserves. In addition, it is stipulated in Article 9 that a Decennium Review shall be conducted on the world biosphere reserve every a decade, this Review shall be based on the report prepared by the relevant authority; the Review result shall be submitted to the relevant national secretariat. The related text of Statutory Framework is attached in Annex 3. This Review Statement will be helpful for each country preparing national reports and update data as stipulated in Article 9, and the secretariat timely accessing to data associated with the biosphere reserve. This Statement shall contribute to the inspection of MAB ICC on the biosphere reserve, and judge whether it can meet all criteria mentioned in Article 9 of the Legal Framework, especially three major functions. It shall be noted that is required to specify how the biosphere reserve achieves the various criteria in the last part of the Statement (Criteria and Progress). The information from Decennium Review will be used by UNESCO for the following purposes: (a) Inspection of the relevant autorities of International Advisory Committee and MAB ICC on the biosphere reserve; and (b) the world's information system, especially the UNESCO's MAB network and publications, so as to promote communication among people concerned the world biosphere reserve and influence each other. -
Seasonal Concentration Distribution of PM1.0 and PM2.5 and a Risk
www.nature.com/scientificreports OPEN Seasonal concentration distribution of PM1.0 and PM2.5 and a risk assessment of bound trace metals in Harbin, China: Efect of the species distribution of heavy metals and heat supply Kun Wang1, Weiye Wang1, Lili Li1, Jianju Li1, Liangliang Wei1 ✉ , Wanqiu Chi1, Lijing Hong1,2, Qingliang Zhao1 & Junqiu Jiang1 To clarify the potential carcinogenic/noncarcinogenic risk posed by particulate matter (PM) in Harbin, a city in China with the typical heat supply, the concentrations of PM1.0 and PM2.5 were analyzed from Nov. 2014 to Nov. 2015, and the compositions of heavy metals and water-soluble ions (WSIs) were determined. The continuous heat supply from October to April led to serious air pollution in Harbin, thus leading to a signifcant increase in particle numbers (especially for PM1.0). Specifcally, coal combustion under heat supply conditions led to signifcant emissions of PM1.0 and PM2.5, especially heavy metals 2− − + and secondary atmospheric pollutants, including SO4 , NO3 , and NH4 . Natural occurrences such as dust storms in April and May, as well as straw combustion in October, also contributed to the increase in WSIs and heavy metals. The exposure risk assessment results demonstrated that Zn was the main contributor to the average daily dose through ingestion and inhalation, ADDIng and ADDinh, respectively, among the 8 heavy metals, accounting for 51.7–52.5% of the ADDIng values and 52.5% of the ADDinh values. The contribution of Zn was followed by those of Pb, Cr, Cu and Mn, while those of Ni, Cd, and Co were quite low (<2.2%). -
North and Central Asia FAO-Unesco Soil Tnap of the World 1 : 5 000 000 Volume VIII North and Central Asia FAO - Unesco Soil Map of the World
FAO-Unesco S oilmap of the 'world 1:5 000 000 Volume VII North and Central Asia FAO-Unesco Soil tnap of the world 1 : 5 000 000 Volume VIII North and Central Asia FAO - Unesco Soil map of the world Volume I Legend Volume II North America Volume III Mexico and Central America Volume IV South America Volume V Europe Volume VI Africa Volume VII South Asia Volume VIIINorth and Central Asia Volume IX Southeast Asia Volume X Australasia FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS UNITED NATIONS EDUCATIONAL, SCIENTIFIC AND CULTURAL ORGANIZATION FAO-Unesco Soilmap of the world 1: 5 000 000 Volume VIII North and Central Asia Prepared by the Food and Agriculture Organization of the United Nations Unesco-Paris 1978 The designations employed and the presentation of material in this publication do not irnply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations or of the United Nations Educa- tional, Scientific and Cultural Organization con- cerning the legal status of any country, territory, city or area or of its authorities, or concerning the delirnitation of its frontiers or boundaries. Printed by Tipolitografia F. Failli, Rome, for the Food and Agriculture Organization of the United Nations and the United Nations Educational, Scientific and Cultural Organization Published in 1978 by the United Nations Educational, Scientific and Cultural Organization Place de Fontenoy, 75700 Paris C) FAO/Unesco 1978 ISBN 92-3-101345-9 Printed in Italy PREFACE The project for a joint FAO/Unesco Soil Map of vested with the responsibility of compiling the techni- the World was undertaken following a recommenda- cal information, correlating the studies and drafting tion of the International Society of Soil Science. -
The Variations of Land Surface Phenology in Northeast China and Its Responses to Climate Change from 1982 to 2013
remote sensing Article The Variations of Land Surface Phenology in Northeast China and Its Responses to Climate Change from 1982 to 2013 Jianjun Zhao 1,†, Yanying Wang 1,†, Zhengxiang Zhang 1,*, Hongyan Zhang 1,*, Xiaoyi Guo 1,†, Shan Yu 1,2,†, Wala Du 3,† and Fang Huang 1,† 1 School of Geographical Sciences, Northeast Normal University, Changchun 130024, China; [email protected] (J.Z.); [email protected] (Y.W.); [email protected] (X.G.); [email protected] (S.Y.); [email protected] (F.H.) 2 Inner Mongolia Key Laboratory of Remote Sensing and Geographic Information System, Huhhot 010022, China 3 Ecological and Agricultural Meteorology Center of Inner Mongolia Autonomous Region, Huhhot 010022, China; [email protected] * Correspondence: [email protected] (Z.Z.); [email protected] (H.Z.); Tel./Fax: +86-431-8509-9550 (Z.Z.); +86-431-8509-9213 (H.Z.) † These authors contributed equally to this work. Academic Editors: Petri Pellikka, Lars Eklundh, Alfredo R. Huete and Prasad S. Thenkabail Received: 4 February 2016; Accepted: 4 May 2016; Published: 12 May 2016 Abstract: Northeast China is located at high northern latitudes and is a typical region of relatively high sensitivity to global climate change. Studies of the land surface phenology in Northeast China and its response to climate change are important for understanding global climate change. In this study, the land surface phenology parameters were calculated using the third generation dataset from the Global Inventory Modeling and Mapping Studies (GIMMS 3g) that was collected from 1982 to 2013 were estimated to analyze the variations of the land surface phenology in Northeast China at different scales and to discuss the internal relationships between phenology and climate change. -
Tetrao Urogalloides) in Northeast China from 1950 to 2010 Based on Local Historical Documents
Pakistan J. Zool., vol. 48(6), pp. 1825-1830, 2016. Decline and Range Contraction of Black-Billed Capercaillie (Tetrao urogalloides) in Northeast China from 1950 to 2010 Based on Local Historical Documents Yueheng Ren, Li Yang, Rui Zhang, Jiang Lv, Mujiao Huang and Xiaofeng Luan* School of Nature Conservation, Beijing Forestry University, NO.35 Tsinghua East Road Haidian District, Beijing, P. R. China, Beijing, 100083, P. R. China, Yueheng Ren, Li Yang, Rui Zhang contributed equally. A B S T R A C T Article Information Received 21 August 2015 The black-billed capercaillie (Tetrao urogalloides) is a large capercaillie which is considered an Revised 14 March 2016 endangered species that has undergone a dramatic decline throughout the late 20th century. This Accepted 19 May 2016 species is now rare or absent in Northeast China and needs immediate protection. Effective Available online 25 September 2016 conservation and management could be hampered by insufficient understanding of the population decline and range contraction; however, any historical information, whilst being crucial, is rare. In Authors’ Contribution this paper, we present local historical documents as one problem-solving resource for large-scale YR, LY and XL conceived and designed the study. LY, YR, JL and analysis of this endangered species in order to reveal the historical population trend in Northeast MH were involved in data collection. China from 1950 to 2010. Our results show that the population was widely distributed with a large YR, LY and RZ were involved in population in Northeast China before the 1980s. Because of increasing habitat destruction in data processing. -
Exploring Wintertime Regional Haze in Northeast China: Role of Coal and Biomass Burning
Atmos. Chem. Phys., 20, 5355–5372, 2020 https://doi.org/10.5194/acp-20-5355-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Exploring wintertime regional haze in northeast China: role of coal and biomass burning Jian Zhang1, Lei Liu1, Liang Xu1, Qiuhan Lin1, Hujia Zhao2, Zhibin Wang3, Song Guo4, Min Hu4, Dantong Liu1, Zongbo Shi5, Dao Huang1, and Weijun Li1 1Department of Atmospheric Sciences, School of Earth Sciences, Zhejiang University, Hangzhou, 310027, China 2Institute of Atmospheric Environment, China Meteorological Administration, Shenyang, 110016, China 3Research Center for Air Pollution and Health, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou, 310058, China 4State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China 5School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham, B15 2TT, UK Correspondence: Weijun Li ([email protected]) Received: 6 November 2019 – Discussion started: 8 January 2020 Revised: 18 March 2020 – Accepted: 1 April 2020 – Published: 7 May 2020 Abstract. As one of the intense anthropogenic emission 223 µg m−3) with predominantly OM (98–133 µg m−3) and regions across the relatively high-latitude ( > 40◦ N) areas unexpectedly high KC (3.8 µg m−3). TEM also showed that on Earth, northeast China faces the serious problem of re- K-rich particles internally mixed with OM (named K-OM) gional haze during the heating period of the year. Aerosols increased from 4 %–5 % by number to 50 %–52 %. The re- in polluted haze in northeast China are poorly understood sults indicate that there were different sources of aerosol compared with the haze in other regions of China such as particles causing the Haze-I and Haze-II formation: Haze-I the North China Plain. -
Geologic Factors Affecting Seismic Monitoring in China
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Geologic Factors Affecting Seismic Monitoring in China John R. Matzkoi Open-File Report 95-562 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey. JReston, Virgina 1995 Geologic Factors Affecting Seismic Monitoring in China Table of Contents Introduction ...................................................... 4 Rock Environments ................................................. 4 Igneous Rocks ............................................... 4 Metamorphic and Sedimentary Rocks ................................ 5 Ground Water Occurrences and Conditions ............................ 6 Principal Tectonic Regions ............................................. 7 Active Tectonics ..................................................... 8 Quaternary Volcanism ................................................ 10 Crustal Thickness and Characteristics ..................................... 11 Seismicity ........................................................ 13 Heat Flow ........................................................ 13 Salt Deposits ...................................................... 14 Oil and Natural Gas Development ........................................ 15 Mining Regions .................................................... 16 Karst ........................................................... 17 Loess -
Transboundary Cooperation Between Neighbouring Protected Areas for Amur Leopard and Tiger Conservation • Proposal 2
Annex V. New Proposals on Three Target Feline Species of the NEASPEC Nature Conservation Strategy The following proposals have been submitted by the Russian Government in consultation with partner agencies and experts in China and Mongolia, respectively. • Proposal 1. Ensure Transboundary Cooperation Between Neighbouring Protected Areas for Amur Leopard and Tiger Conservation • Proposal 2. Transboundary Cooperation Between Neighbouring Protected Areas in China and Russia for Tiger Conservation in Lesser Khingan Mountains • Proposal 3. Evaluation of the Current Status of two Snow Leopard Subpopulations in Transboundary Area Between Russia and Mongolia [Proposal 1]: Transboundary Cooperation Between Neighbouring Protected Areas for Amur Leopard and Tiger Conservation The lower Tumen River area, bordered by China, DPR Korea and Russia, is the last habitat on Earth for Amur Leopard, currently estimated to number less than 100 individuals in the world, and the isolated Eastern-Manchurian population of Amur Tiger, which is now successfully recovering in North East China. Tigers and leopards come and go between China and Russia passing over the fence and sometimes reach the Korean Peninsula across the frozen river. The border is a political creation by humans, not of nature. In 2004, NEASPEC had elaborated the proposal for creation of transboundary protected area, based on existing nature reserves in Russia, China and DPRK. During last decade, the situation was really improved when the large national park “Land of leopard” (LLNP) was established in Russia in 2012, and the pilot Tiger and Leopard national park (TLNP) was launched in China. Total area of these bordering protected areas is about 1.8 million ha, which are now serves as the home for about 40 tigers and 90 leopards. -
Distribution of Igneous Rocks in China Revealed by Aeromagnetic Data
Accepted Manuscript Distribution of igneous rocks in China revealed by aeromagnetic data Shengqing Xiong, Hai Yang, Yanyun Ding, Zhankui Li, Wei Li PII: S1367-9120(16)30269-3 DOI: http://dx.doi.org/10.1016/j.jseaes.2016.08.016 Reference: JAES 2793 To appear in: Journal of Asian Earth Sciences Received Date: 25 March 2016 Revised Date: 13 August 2016 Accepted Date: 22 August 2016 Please cite this article as: Xiong, S., Yang, H., Ding, Y., Li, Z., Li, W., Distribution of igneous rocks in China revealed by aeromagnetic data, Journal of Asian Earth Sciences (2016), doi: http://dx.doi.org/10.1016/j.jseaes. 2016.08.016 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. Distribution of igneous rocks in China revealed by aeromagnetic data Shengqing Xiong1, 2, Hai Yang1, Yanyun Ding1, Zhankui Li1, Wei Li1 1 China Aero Geophysical Survey and Remote Sensing Center for Land and Resources, Beijing 100083, China 2 Key Laboratory of Airborne Geophysics and Remote Sensing Geology, Ministry of Land and Resources, Beijing 100083, China Corresponding author: Shengqing Xiong China Aero Geophysical Survey and Remote Sensing Center for Land and Resources No.31 Xueyuan Road, Haidian District, Beijing 10083, P. -
29. the Amur Subgeosyncline and the Sungari Basin by Teiichi
106 Proc. Japan Acad., 60, Ser. B (1984) [Vol. 60(B), 29. The Amur Subgeosyncline and the Sungari Basin By Teiichi KOBAYASHI, M. J. A. (Communicated, May 12, 1984) Since Schonemann expressed the opinion in 1929 that the Mongol-Amur folded belt had been a geosyncline disturbed by the late Mesozoic orogeny, it was a moot discussion among Stille, Obrutschew and others. In 1942 I have pointed out in this journal, that the Mongolian geosyncline became a folded zone by the Permo-Triassic orogeny, but the Amur subgeosyncline was left behind the Mongoliden and later became a folded zone in the late Mesozoic period. Here I wish to elucidate the history in a further detail with reference to additional data gathered since then. In Northeast Mongolia the Triassic formation containing Ole- nekian ceratites and bivalves and early Keuper plants were found between the marine Upper Permian and the Lower Jurassic con- tinental formation in the Jargalatuin graben in the upper Onon tributary in Mongolia. The plant-bearing Lower Triassic overlies older granite near Chita. In the Lesser Khingan range the Triassic formation disconformably overlies the Upper Permian and yields marine shells from Induan to Ladinian. In Khetin and Vandan areas in the middle Amur valley there is no break from the f ossilif erous Middle and Lower Triassic formation to the Upper Permian for- mation. The Carnic to None formation containing Pseudomonotis over- lies Silurian and Devonian in the upper Amur and Permian and older rocks in east Tr,ansbaikalia with strong discordance. Its thickness attains 5,000 m. This is the molasse of the Ladinian orogeny corre- sponding to the Akiyoshi orogeny in Japan. -
Annex II (Sub-Report) Supplementary Information in the Field of Carbon
Annex II (Sub-Report) Supplementary Information in the field of Carbon Stock For 2018 UNCCD Reporting, China 1. A brief introduction of special carbon program In 2011, the Chinese Academy of Sciences (CAS) initiated the program on carbon revenue and expenditure certification and relevant problems in response to climate change, a CAS Strategic Priority Research Program, also one of the A programs launched by CAS. This special carbon program analyses the key technological problems related to carbon revenue and expenditure, conducts surveillance, research and scientific estimate of the overall carbon revenue and expenditure of the land eco-system through systematic research. The results of the program will be used in major international negotiations on climate change and green and low-carbon development strategies. The special program set up three project groups to address eco-system carbon sequestration. The project groups made investigation into and observation of the carbon stock volume and carbon sequestration abilities of different eco-systems like forests, grassland, bushwood and farmland. The program also made research into the carbon revenue and expenditure characteristics of China's terrestrial ecosystem, the law of space-time distribution, and the carbon sequestration effect of national ecological engineering and related policies whose results provide the relevant scientific basis for national policy making and international negotiation. 1.1 unified, standard and systematic investigation, research and technical methods In order -
Report on the State of the Ecology and Environment in China 2018
Report on the State of the Ecology and Environment in China 2018 The 2018 Report on the State of the Ecology and Environment in China is hereby announced in accordance with the Environmental Protection Law of the People’s Republic of China. Minister of Ministry of Ecology and Environment, the People’s Republic of China May 22, 2019 2018 Report on the State of the Ecology and Environment in China Summary.................................................................................................1 Atmospheric Environment....................................................................9 Freshwater Environment....................................................................20 Marine Environment...........................................................................38 Land Environment...............................................................................43 Natural and Ecological Environment.................................................44 Acoustic Environment.........................................................................46 Radiation Environment.......................................................................49 Climate Change and Natural Disasters............................................52 Infrastructure and Energy.................................................................56 Data Sources and Explanations for Assessment ...............................58 1 Report on the State of the Ecology and Environment in China 2018 Summary The year 2018 was a milestone in the history of China’s ecological environmental