Spatial Distribution Characteristics of Phaeozem in Songliao Plain Based on RS
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The Cartographic Steppe: Mapping Environment and Ethnicity in Japan's Imperial Borderlands
The Cartographic Steppe: Mapping Environment and Ethnicity in Japan's Imperial Borderlands The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Christmas, Sakura. 2016. The Cartographic Steppe: Mapping Environment and Ethnicity in Japan's Imperial Borderlands. Doctoral dissertation, Harvard University, Graduate School of Arts & Sciences. Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:33840708 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA The Cartographic Steppe: Mapping Environment and Ethnicity in Japan’s Imperial Borderlands A dissertation presented by Sakura Marcelle Christmas to The Department of History in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the subject of History Harvard University Cambridge, Massachusetts August 2016 © 2016 Sakura Marcelle Christmas All rights reserved. Dissertation Advisor: Ian Jared Miller Sakura Marcelle Christmas The Cartographic Steppe: Mapping Environment and Ethnicity in Japan’s Imperial Borderlands ABSTRACT This dissertation traces one of the origins of the autonomous region system in the People’s Republic of China to the Japanese imperial project by focusing on Inner Mongolia in the 1930s. Here, Japanese technocrats demarcated the borderlands through categories of ethnicity and livelihood. At the center of this endeavor was the perceived problem of nomadic decline: the loss of the region’s deep history of transhumance to Chinese agricultural expansion and capitalist extraction. -
2016 Annual Report.PDF
HAITONG SECURITIES CO., LTD. 海通證券股份有限公司 Annual Report 2016 2016 Annual Report 年度報告 CONTENTS Section I Definition and Important Risk Warnings 3 Section II Company Profile and Key Financial Indicators 7 Section III Summary of the Company’s Business 23 Section IV Report of the Board of Directors 28 Section V Significant Events 62 Section VI Changes in Ordinary Share and Particulars about Shareholders 91 Section VII Preferred Shares 100 Section VIII Particulars about Directors, Supervisors, Senior Management and Employees 101 Section IX Corporate Governance 149 Section X Corporate Bonds 184 Section XI Financial Report 193 Section XII Documents Available for Inspection 194 Section XIII Information Disclosure of Securities Company 195 IMPORTANT NOTICE The Board, the Supervisory Committee, Directors, Supervisors and senior management of the Company represent and warrant that this annual report (this “Report”) is true, accurate and complete and does not contain any false records, misleading statements or material omission and jointly and severally take full legal responsibility as to the contents herein. This Report was reviewed and passed at the twenty-third meeting of the sixth session of the Board. The number of Directors to attend the Board meeting should be 13 and the number of Directors having actually attended the Board meeting was 11. Director Li Guangrong, was unable to attend the Board meeting in person due to business travel, and had appointed Director Zhang Ming to vote on his behalf. Director Feng Lun was unable to attend the Board meeting in person due to business travel and had appointed Director Xiao Suining to vote on his behalf. -
Gully Erosion Control Practices in Northeast China: a Review
Article Gully Erosion Control Practices in Northeast China: A Review Xiaobing Liu 1, Hao Li 1, Shengmin Zhang 2, Richard M. Cruse 3 and Xingyi Zhang 1,* 1 Key Laboratory of Mollisols Agroecology, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Harbin 150081, China 2 Faculty of Engineering Management, University of Chinese Academy of Sciences, Beijing 100049, China 3 Department of Agronomy, Iowa State University, Ames, IA 500011, USA * Correspondence: [email protected] Received: 13 August 2019; Accepted: 10 September 2019; Published: 16 September 2019 Abstract: Gully erosion is the destructive and dramatic form of land degradation in Northeast China. The region is the grain production and ecological security base of China where the fertile and productive Mollisols are distributed. Though the region was agriculturally developed relatively recently, it went through high intensity cultivation and fast succession processes within short-time scales. Coupled with irrational farming practice choice and land use, hillslope erosion and gully erosion are seriously threatening agricultural production and environmental stability in the region. The awareness of gully erosion by the local governments started in the 1970s, and conservation measures were thus implemented. In this paper, based on our survey, communications with local farmers and stakeholders as well as investigation for gully erosion for the past three years, we summarize the practical and efficient practices to manage gully erosion developed by researchers and farmers in Northeast China during the past 50 years. These practices include various drop structures, soil check dams, masonry check dams, gabion check dams, wicker check dams, continuous live wicker, a shrub plant enclosure, and an arbor plant enclosure. -
World Reference Base for Soil Resources 2014 International Soil Classification System for Naming Soils and Creating Legends for Soil Maps
ISSN 0532-0488 WORLD SOIL RESOURCES REPORTS 106 World reference base for soil resources 2014 International soil classification system for naming soils and creating legends for soil maps Update 2015 Cover photographs (left to right): Ekranic Technosol – Austria (©Erika Michéli) Reductaquic Cryosol – Russia (©Maria Gerasimova) Ferralic Nitisol – Australia (©Ben Harms) Pellic Vertisol – Bulgaria (©Erika Michéli) Albic Podzol – Czech Republic (©Erika Michéli) Hypercalcic Kastanozem – Mexico (©Carlos Cruz Gaistardo) Stagnic Luvisol – South Africa (©Márta Fuchs) Copies of FAO publications can be requested from: SALES AND MARKETING GROUP Information Division Food and Agriculture Organization of the United Nations Viale delle Terme di Caracalla 00100 Rome, Italy E-mail: [email protected] Fax: (+39) 06 57053360 Web site: http://www.fao.org WORLD SOIL World reference base RESOURCES REPORTS for soil resources 2014 106 International soil classification system for naming soils and creating legends for soil maps Update 2015 FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2015 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. -
Report on Domestic Animal Genetic Resources in China
Country Report for the Preparation of the First Report on the State of the World’s Animal Genetic Resources Report on Domestic Animal Genetic Resources in China June 2003 Beijing CONTENTS Executive Summary Biological diversity is the basis for the existence and development of human society and has aroused the increasing great attention of international society. In June 1992, more than 150 countries including China had jointly signed the "Pact of Biological Diversity". Domestic animal genetic resources are an important component of biological diversity, precious resources formed through long-term evolution, and also the closest and most direct part of relation with human beings. Therefore, in order to realize a sustainable, stable and high-efficient animal production, it is of great significance to meet even higher demand for animal and poultry product varieties and quality by human society, strengthen conservation, and effective, rational and sustainable utilization of animal and poultry genetic resources. The "Report on Domestic Animal Genetic Resources in China" (hereinafter referred to as the "Report") was compiled in accordance with the requirements of the "World Status of Animal Genetic Resource " compiled by the FAO. The Ministry of Agriculture" (MOA) has attached great importance to the compilation of the Report, organized nearly 20 experts from administrative, technical extension, research institutes and universities to participate in the compilation team. In 1999, the first meeting of the compilation staff members had been held in the National Animal Husbandry and Veterinary Service, discussed on the compilation outline and division of labor in the Report compilation, and smoothly fulfilled the tasks to each of the compilers. -
Chernozems Kastanozems Phaeozems
Chernozems Kastanozems Phaeozems Peter Schad Soil Science Department of Ecology Technische Universität München Steppes dry, open grasslands in the mid-latitudes seasons: - humid spring and early summer - dry late summer - cold winter occurrence: - Eurasia - North America: prairies - South America: pampas Steppe soils Chernozems: mostly in steppes Kastanozems: steppes and other types of dry vegetation Phaeozems: steppes and other types of medium-dry vegetation (till 1998: Greyzems, now merged to the Phaeozems) all steppe soils: mollic horizon Definition of the mollic horizon (1) The requirements for a mollic horizon must be met after the first 20 cm are mixed, as in ploughing 1. a soil structure sufficiently strong that the horizon is not both massive and hard or very hard when dry. Very coarse prisms (prisms larger than 30 cm in diameter) are included in the meaning of massive if there is no secondary structure within the prisms; and Definition of the mollic horizon (2) 2. both broken and crushed samples have a Munsell chroma of less than 3.5 when moist, a value darker than 3.5 when moist and 5.5 when dry (shortened); and 3. an organic carbon content of 0.6% (1% organic matter) or more throughout the thickness of the mixed horizon (shortened); and Definition of the mollic horizon (3) 4. a base saturation (by 1 M NH4OAc) of 50% or more on a weighted average throughout the depth of the horizon; and Definition of the mollic horizon (4) 5. the following thickness: a. 10 cm or more if resting directly on hard rock, a petrocalcic, petroduric or petrogypsic horizon, or overlying a cryic horizon; b. -
Supplementary Data Figure S1. High Collision Energy ESI-MS Spectra of Peaks 51(A), 54(B), 59(C), 75(D), 80(E), and 83(F)
Supplementary data Figure S1. High collision energy ESI-MS spectra of peaks 51(A), 54(B), 59(C), 75(D), 80(E), and 83(F). 1 Table S1-1. Chemical structures of the detected compounds in different parts of P. ginseng root (PPD-type). R O OH 2 PPD R1O No Name R1 R2 38/84 malnoylfloralginsenosides Rd6 Glc(2,1)Glc(6)-Mal Glc(6)-Mal β-D-Glucopyranoside, (3β,12β)-20-(β-D- glucopyranosyloxy)-12-hydroxydammar-24-en-3-yl 2-O-[6-O-(2-carboxyacetyl)-β-D-glucopyranosyl]-, 6- 38/84 (hydrogen propanedioate) Glc-[6-Mal]-(2,1)Glc-[6-Mal] Glc 42 Notoginsenoside R4 Glc(2,1)Glc Glc(6,1)Glc(3,1)Xyl 44/52 Yesanchinoside J Glc-[6-Ace]-(2,1)Glc Glc(6,1)Glc(6,1)Xyl malonyl-ginsenoside Ra3/ malonyl- Glc(6,1)Glc(3,1)Xyl/Glc(6,1 45 notoginsenoside R4 Glc(2,1)Glc(6)-Mal )Glc(6,1)Xyl 48 Ginsenoside Ra2 Glc(2,1)Glc Glc(6,1)Ara(f 2,1) Xyl 49 Ginsenoside Ra3 Glc(2,1)Glc Glc(6,1)Glc(3,1)Xyl 50 Rb1 Glc(2,1)Glc Glc(6,1)Glc 51/58/66/70/72/73 Ra5 Glc(2,1)Glc(6)-Ace Glc(6,1)Ara(p 4,1)Xyl 2 (3β,12β)-3-[[2-O-(6-O-Acetyl-β-D-glucopyranosyl)-β- D-glucopyranosyl]oxy]-12-hydroxydammar-24-en- 20-yl O-β-D-xylopyranosyl-(1→2)-O-α-L- 51/58/66/70/72/73 arabinopyranosyl-(1→6)-β-D-glucopyranoside Glc(2,1)Glc(6)-Ace Glc(6,1)Ara(p 2,1)Xyl 56 Rc Glc(2,1)Glc Glc(6,1)Ara(f) 57/62 Ra1 Glc(2,1)Glc Glc(6,1)Ara(p 4,1)Xyl 54/61/64/74 Quinquenoside R1 Glc(2,1)Glc(6)-Ace Glc(6,1)Glc (3β,12β)-20-[[6-O-(6-O-Acetyl-β-D-glucopyranosyl)- β-D-glucopyranosyl]oxy]-12-hydroxydammar-24-en- 54/61/64/74 3-yl 2-O-β-D-glucopyranosyl-β-D-glucopyranoside Glc(2,1)Glc Glc(6,1)Glc(6)-Ace 55 malonyl-ginsenoside Rb1 Glc(2,1)Glc(6)-Mal -
Effects of Cutting Frequency on Alfalfa Yield and Yield Components in Songnen Plain, Northeast China
African Journal of Biotechnology Vol. 11(21), pp. 4782-4790, 13 March, 2012 Available online at http://www.academicjournals.org/AJB DOI: 10.5897/AJB12.092 ISSN 1684–5315 © 2012 Academic Journals Full Length Research Paper Effects of cutting frequency on alfalfa yield and yield components in Songnen Plain, Northeast China Ji-shan Chen, Fen-lan Tang, Rui-fen Zhu ,Chao Gao, Gui-li Di and Yue-xue Zhang* Institute of Pratacultural Science, Heilongjiang Academy of Agricultural Sciences, Harbin, Heilongjiang 150086, China. Accepted 27 February, 2012 The productivity and quality of alfalfa ( Medicago sativa L.) is strongly influenced by cutting frequency (F). To clarify that the yield and quality of alfalfa if affected by F, an experiment was conducted on Songnen Plain in Northeast China to investigate the responses of yield components and quality to 3 cutting frequencies (F30, F40 and F60) among 3 cultivars (C) (Longmu, Aohan, Zhaodong). Result from two consecutive years showed that cutting frequency had a greater effect on reducing forage yield and yield components at F40. Cultivars had no effect on 2-year total forage yield and alfalfa quality. Alfalfa at the F40 always had higher crude protein (CP), and neutral detergent fibre (NDF) than F30 and F60 treatments. The interaction (C×F) on forage yield and components (CP and NDF) was not significant. This study provides evidence that: i) 40-day intervals can be advocated for cultivars growing in North- east China; and ii) at F40 utilization, Longmu is a well-adapted alfalfa variety in the Songnen Plain because of higher yield and quality under three cuttings. -
Table of Codes for Each Court of Each Level
Table of Codes for Each Court of Each Level Corresponding Type Chinese Court Region Court Name Administrative Name Code Code Area Supreme People’s Court 最高人民法院 最高法 Higher People's Court of 北京市高级人民 Beijing 京 110000 1 Beijing Municipality 法院 Municipality No. 1 Intermediate People's 北京市第一中级 京 01 2 Court of Beijing Municipality 人民法院 Shijingshan Shijingshan District People’s 北京市石景山区 京 0107 110107 District of Beijing 1 Court of Beijing Municipality 人民法院 Municipality Haidian District of Haidian District People’s 北京市海淀区人 京 0108 110108 Beijing 1 Court of Beijing Municipality 民法院 Municipality Mentougou Mentougou District People’s 北京市门头沟区 京 0109 110109 District of Beijing 1 Court of Beijing Municipality 人民法院 Municipality Changping Changping District People’s 北京市昌平区人 京 0114 110114 District of Beijing 1 Court of Beijing Municipality 民法院 Municipality Yanqing County People’s 延庆县人民法院 京 0229 110229 Yanqing County 1 Court No. 2 Intermediate People's 北京市第二中级 京 02 2 Court of Beijing Municipality 人民法院 Dongcheng Dongcheng District People’s 北京市东城区人 京 0101 110101 District of Beijing 1 Court of Beijing Municipality 民法院 Municipality Xicheng District Xicheng District People’s 北京市西城区人 京 0102 110102 of Beijing 1 Court of Beijing Municipality 民法院 Municipality Fengtai District of Fengtai District People’s 北京市丰台区人 京 0106 110106 Beijing 1 Court of Beijing Municipality 民法院 Municipality 1 Fangshan District Fangshan District People’s 北京市房山区人 京 0111 110111 of Beijing 1 Court of Beijing Municipality 民法院 Municipality Daxing District of Daxing District People’s 北京市大兴区人 京 0115 -
Impact of Plant Roots and Soil Organisms on Soil Micromorphology and Hydraulic Properties
CMYK Biologia, Bratislava, 61/Suppl. 19: S339—S343, 2006 S339 Impact of plant roots and soil organisms on soil micromorphology and hydraulic properties Radka Kodešová1,VítKodeš2, Anna Žigová3 &JiříŠimůnek4 1Czech University of Agriculture in Prague, Department of Soil Science and Geology, Kamýcka 129,CZ–16521 Prague, Czech Republic; e-mail: [email protected] 2Czech Hydrometeorological Institute, Department of Water Quality, Na Šabatce 17,CZ–14306 Prague, Czech Republic 3Academy of Sciences of the Czech Republic, Institute of Geology, Rozvojová 269,CZ–16502 Prague, Czech Republic 4University of California Riverside, Department of Environmental Sciences, Riverside, CA 92521,USA Abstract: A soil micromorphological study was performed to demonstrate the impact of soil organisms on soil pore structure. Two examples are shown here. First, the influence of earthworms, enchytraeids and moles on the pore structure of a Greyic Phaeozem is demonstrated by comparing two soil samples taken from the same depth of the soil profile that either were affected or not affected by these organisms. The detected image porosity of the organism-affected soil sample was 5 times larger then the porosity of the not-affected sample. The second example shows macropores created by roots and soil microorganisms in a Haplic Luvisol and subsequently affected by clay coatings. Their presence was reflected in the soil water retention curve, which displayed multiple S-shaped features as obtained from the water balance carried out for the multi-step outflow experiment. The dual permeability models implemented in HYDRUS-1D was applied to obtain parameters characterizing multimodal soil hydraulic properties using the numerical inversion of the multi-step outflow experiment. -
Hydro-Geochemical Characteristics and Health Risk Evaluation of Nitrate in Groundwater
Pol. J. Environ. Stud. Vol. 25, No. 2 (2016), 521-527 DOI: 10.15244/pjoes/61113 Original Research Hydro-Geochemical Characteristics and Health Risk Evaluation of Nitrate in Groundwater Jianmin Bian1*, Caihong Liu1, Zhenzhen Zhang1, Rui Wang2, Yue Gao1 1Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, Changchun 130021, China 2Shijiazhuang University of Economics, Shijiazhuang 050031, China Received: 17 April 2015 Accepted: 21 December 2015 Abstract Groundwater is considered a major source of drinking water and its quality a basis for good population health. In order to identify groundwater hydro-chemical characteristics and pollution conditions in Songnen Plain, groundwater hydro-chemical characteristics and nitrate-nitrogen (NO3-N) spatial distribution characteristics and the health risks were analyzed. Results showed that groundwater hydro-chemical type was mainly HCO3-Ca, which was associated with the action of calcite and silicate mineral weathering dissolution. The over standards rate of NO3-N accounted for 50.8%, the coeffi cient of variation was 183.57% which was high spatial variability, the high-risk area accounted for 88.78% of the total study area, and the high-risk area covered the area with water quality of classes IV, V, and part of class III. The high-risk area is mainly distributed in the eastern high plains and in the central low plains, while the low-risk zone accounts for only 11.22% of the total area and is mainly distributed in the western alluvial plain with scattered distribution in other areas. Keywords: health risk evaluation, hydrochemical type, Piper trilinear charts, spatial variability, nitrate nitrogen Introduction nitrogen, and urban living sewage [2-4]. -
Atrocities in China
ATROCITIES IN CHINA: LIST OF VICTIMS IN THE PERSECUTION OF FALUN GONG IN CHINA Jointly Compiled By World Organization to Investigate the Persecution of Falun Gong PO Box 365506 Hyde Park, MA 02136 Contact: John Jaw - President Tel: 781-710-4515 Fax: 781-862-0833 Web Site: http://www.upholdjustice.org Email: [email protected] Fa Wang Hui Hui – Database system dedicated to collecting information on the persecution of Falun Gong Web Site: http://www.fawanghuihui.org Email: [email protected] April 2004 Preface We have compiled this list of victims who were persecuted for their belief to appeal to the people of the world. We particularly appeal to the international communities and request investigation of this systematic, ongoing, egregious violation of human rights committed by the Government of the People’s Republic of China against Falun Gong. Falun Gong, also called Falun Dafa, is a traditional Chinese spiritual practice that includes exercise and meditation. Its principles are based on the values of truthfulness, compassion, and tolerance. The practice began in China in 1992 and quickly spread throughout China and then beyond. By the end of 1998, by the Chinese government's own estimate, there were 70 - 100 million people in China who had taken up the practice, outnumbering Communist Party member. Despite the fact that it was good for the people and for the stability of the country, former President JIANG Zemin launched in July 1999 an unprecedented persecution of Faun Gong out of fears of losing control. Today the persecution of Falun Gong still continues in China. As of the end of March 2004, 918 Falun Gong practitioners have been confirmed to die from persecution.