Soils in the Memory of World Nations
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Some Remarks on the Origin of Ideology of Divine Warfare in Early Dynastic Lagaš
ISSN 2518-1521 (Online), ISSN 2226-2830 (Print) ВІСНИК МАРІУПОЛЬСЬКОГО ДЕРЖАВНОГО УНІВЕРСИТЕТУ СЕРІЯ: ІСТОРІЯ. ПОЛІТОЛОГІЯ, 2017, ВИП. 18 The historiographic review of M. Hrushevsky’s sociological researches emphasized the many-sided nature of the prominent historian’s scientific heritage. Especially it concerns the representatives of the emigrant and contemporary Ukrainian historical science. The historians of diaspora (L.Vynar, S. Zabrovarny, O. Pritsak) proved that the sociological-comparative method used by M. Hrushevsky in the historical research as social, economic and cultural synthesis of the nation’s history enhanced the capabilities to study it more systematically. It was stated that the outstanding scientist popularized the social history of Ukraine in the West-European scientific community with the help of his public lectures on historic and sociological topics. The contemporary Ukrainian historians (V. Bilodid, O. Kopylenko, V. Telvak, L. Chugaevska, I. Shostak, O. Yas and others) analysed the historian’s sociological works and stated world outlook evolution of Mykhailo Hrushevsky from the romantic narodnik movement to the critical rethinking of sociology. The analysis of M. Hrushevsky’s sociological heritage defined the interrelation of “public and national” and the state system as well as the main issues of sociology as a science and sociological ideas in Ukrainian national studies. The contemporary historians traced rethinking the historian’s research strategies. Key words: sociological works, emigrant period, historiographic analysis, Ukrainian historians, historians of diaspora, contemporary scientists. УДК 355.48(358) V. Sazonov SOME REMARKS ON THE ORIGIN OF IDEOLOGY OF DIVINE WARFARE IN EARLY DYNASTIC LAGAŠ Current article discusses the problem of origin of ideology of divine warfare and theology of war of Ancient Mesopotamian rulers in the Early Dynastic Lagaš (26-24th centuries BCE). -
Age and Pedogenic Reconstruction of a Paleo–Relict Chernozem Soil from Central Transylvanian Basin
AGE AND PEDOGENIC RECONSTRUCTION OF A PALEO–RELICT CHERNOZEM SOIL FROM CENTRAL TRANSYLVANIAN BASIN F. PENDEA1, Z. SZÁNTÓ2, A. S. BADARAU1 and S. DEZSI1 1Babes–Bolyai University, Faculty of Geography, Cluj–Napoca Clinicilor street no 5–7, 3400 Cluj–Napoca, Romania 2Institute of Nuclear Research, Laboratory of Environmental Studies, H 4001 Debrecen P.O Box 51, Hungary Abstract: The “chernozem” area of Transylvanian Lowland has been of much debate in the last two centuries. The paper presents pedological and geochronological evidence that the chernozem soils of the Central Transylvania have relict Late Glacial–Early Holocene features and at least partially must be clasiffied as paleo–relict in the sense of Reuter (2000). Key words: radiocarbon dating, pedogenic carbonates, paleo–relict features, Central Transylvania During the last century a much debated issue for Romanian pedological and botanical scientific communities was the age and origin of the Central Transylvanian Mollisol cover in conjunction with the associated forest–steppe vegetation. In this study we have found at least partial evidence that the chernozem soil cover in Central Transylvanian was a stable feature long before the ascent of human activities and that, in the Late Holocene, they have suffered a degradation process to the present state of Haplic and Luvic chernozem. The process is somewhat similar with that inferred for Central and Southern Germany, where chernozems formed in the dry steppe or forest–steppe conditions were degraded to brown earths, the resulting polygenetic cover being named Braunerde (Parabraunerde)–Tschernozem (Catt 1989). Because the nature and properties of different soil horizons can hold information with respect to the time pedogenic factor an investigation was undertaken to determine if the typical chernozem features were indeed Late Holocene (Post–Neolithic) as it has been accepted before. -
202 Copyright © 2020 by Academic Publishing House Researcher S.R.O
European Journal of Contemporary Education, 2020, 9(1) Copyright © 2020 by Academic Publishing House Researcher s.r.o. All rights reserved. Published in the Slovak Republic European Journal of Contemporary Education E-ISSN 2305-6746 2020, 9(1): 202-211 DOI: 10.13187/ejced.2020.1.202 www.ejournal1.com WARNING! Article copyright. Copying, reproduction, distribution, republication (in whole or in part), or otherwise commercial use of the violation of the author(s) rights will be pursued on the basis of international legislation. Using the hyperlinks to the article is not considered a violation of copyright. The History of Education The Public Education System in Voronezh Governorate in the Period 1703–1917. Part 1 Aleksandr А. Cherkasov a , b , с , *, Sergei N. Bratanovskii d , e, Larisa A. Koroleva f a International Network Center for Fundamental and Applied Research, Washington, USA b Volgograd State University, Volgograd, Russian Federation с American Historical Association, Washington, USA d Plekhanov Russian University of Economics, Moscow, Russian Federation e Institute of State and Law of RAS, Moscow, Russian Federation f Penza State University of Architecture and Construction, Penza, Russian Federation Abstract This paper examines the public education system in Voronezh Governorate in the period 1703–1917. This part of the collection represents an attempt to reproduce a picture of how the region’s public education system developed between 1703 and 1861. In putting this work together, the authors drew upon a pool of statistical data published in Memorandum Books for Voronezh Governorate, reports by the Minister of Public Education, and Memorandum Books for certain educational institutions (e.g., the Voronezh Male Gymnasium). -
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. -
What Is Digital Signal Processing?
Chapter 1 What Is Digital Signal Processing? A signal, technically yet generally speaking, is a a formal description of a phenomenon evolving over time or space; by signal processing we denote any manual or “mechanical” operation which modifies, analyzes or other- wise manipulates the information contained in a signal. Consider the sim- ple example of ambient temperature: once we have agreed upon a formal model for this physical variable – Celsius degrees, for instance – we can record the evolution of temperature over time in a variety of ways and the resulting data set represents a temperature “signal”. Simple processing op- erations can then be carried out even just by hand: for example, we can plot thesignalongraphpaperasinFigure1.1,orwecancomputederivedpa- rameters such as the average temperature in a month. Conceptually, it is important to note that signal processing operates on an abstract representation of a physical quantity and not on the quantity it- self. At the same time, the type of abstract representation we choose for the physical phenomenon of interest determines the nature of a signal process- ing unit. A temperature regulation device, for instance, is not a signal pro- cessing system as a whole. The device does however contain a signal pro- cessing core in the feedback control unit which converts the instantaneous measure of the temperature into an ON/OFF trigger for the heating element. The physical nature of this unit depends on the temperature model: a sim- ple design is that of a mechanical device based on the dilation of a metal sensor; more likely, the temperature signal is a voltage generated by a ther- mocouple and in this case the matched signal processing unit is an opera- tional amplifier. -
Peasantry As the Main Military Force During Ukrainian Revolution Period 1917–19211
DOI https://doi.org/10.36059/978-966-397-138-4/88-103 PEASANTRY AS THE MAIN MILITARY FORCE DURING UKRAINIAN REVOLUTION PERIOD 1917–19211 Masnenko V. V. INTRODUCTION The modern period was the time of social transformations of the humanity. The main tendency was the demolition of traditional society in all aspects of being. Another feature was the mass character of political life (alongside with the development of parliamentary system and mass political parties). The social roles and behaviors of different social layers changed as well. The emancipation of peasantry, in its broader meaning, was one of the leading tendencies of the general process of modernization. The determining factor that accelerated this process was the emerging of mass army with the mechanism of conscription. In agrarian societies the peasantry was the main component of military service. Ukrainian peasantry in Russian empire was a latecomer to this modernization process. However, it only slowed down its emancipation and it accelerated only during the World War I and the following revolutionary events. The aim is to investigate the peculiarities of Ukrainian peasantry militarization that determined its leading role in the events of Ukrainian revolution 1917–1921, including the participation in regular armies, rebellion movement and peasantry war. 1. During the World War I The World War I was the turning point of the modernization. Millions of peasants were torn apart from their traditional agrarian lifestyle and peasant world; they lost the connection with their usual way of keeping the household. Such a drastic catastrophic event could not but substantially transform the peasant’s outlook. -
Culman-2009-AGEE-Inpress.Pdf
G Model AGEE-3535; No of Pages 12 Agriculture, Ecosystems and Environment xxx (2009) xxx–xxx Contents lists available at ScienceDirect Agriculture, Ecosystems and Environment journal homepage: www.elsevier.com/locate/agee Long-term impacts of high-input annual cropping and unfertilized perennial grass production on soil properties and belowground food webs in Kansas, USA S.W. Culman a,*, S.T. DuPont b,1, J.D. Glover c, D.H. Buckley a, G.W. Fick a, H. Ferris b, T.E. Crews d a Department of Crop and Soil Sciences, Cornell University, Ithaca, NY 14853, United States b Department of Nematology, University of California, Davis, CA 95616, United States c The Land Institute, 2440 E. Water Well Road, Salina, KS 67401, United States d Environmental Studies, Prescott College, Prescott, AZ 86301, United States ARTICLE INFO ABSTRACT Article history: Soil ecosystem properties and processes which simultaneously maintain native fertility and sustain Received 10 May 2009 plant yields are of principal interest in sustainable agriculture. Native prairies in Kansas are relevant in Received in revised form 2 November 2009 this context, as some have been annually harvested for hay for over 75 years with no fertilization or Accepted 5 November 2009 detectable decline in yield or soil fertility. In contrast, annual crop production has resulted in significant Available online xxx reductions in soil fertility and now requires intensive inputs to maintain yields. Soil food webs were compared between hayed native grasslands and adjacent annual croplands in order to determine the Keywords: long-term effects of these two production systems on soil ecosystem properties. -
Guidebook for Field Excursions Xllth International Symposium and Field Seminar on Paleopedology
'1 ■ I VJ 1 ■ ’ »■ " ' . ... !■ 1|Щ 11 ■ Institute of Geography, Russian Academy of Sciences Moscow State University, Soil Science Institute V.V. Dokuchaev Soil Science Institute Institute of History and Material Culture, Russian Academy of Sciences Kursk State University Upetsk State University W. Alekhin Centrul-Chemozemic State Biospheric Reserve Natural Architectural-Archaeological Museum-Resort "Dhmogorid' Guidebook for Field Excursions Xllth International Symposium and Field Seminar on Paleopedology ‘Paleosols, pedosediments and landscape morphology as archives of environmental evolution” 10 -15 August, 2013, Kursk, Russia Moscow 2013 ■ ....... ... - Guidebook for Field Excursions Xllth International Symposium and Field Seminar on Paleopedology CONTENTS Introduction (S.A. Sycheva) 5 1. General characterization of the environment and soils of the Central Russian Upland (S.A. Sycheva, I. V. Kovda, A. V.Kashkin) 9 1.1. Geology and relief 9 1.2. Climate 10 1.3. Hydrology 11 1.4. Vegetation 11 1.5. Soils 12 1.6. Human history and agricultural development of landscapes 12 KURSK SITE 14 2. Aleksandrov Quarry (S.A. Sycheva, E. D. Sheremetskaya, T.M. Grigorieva, M.A. Bronnikova, S.N. Sedov, V.S. Gunova, A.N. Siniakova, P.R.Pushkina) 14 2.1. General characteristics, geochronology and stratigraphy 14 2.2. Description of the composite generalized stratigraphic section 15 2.2.1. Morphology 15 2.2.2. Analytical data 20 2.3. Ryshkov (Mikulino) paleosols and paleocatena (MIS 5e) 23 2.3.1. Ryshkov paleosol on the paleoslope (section 15): interpretation of properties 23 2.3.2. Ryshkov pedolithocomplex in the bottom 27 2.4. Early Valdai Kukuev and Streletsk paleosols (MIS 5 & MIS 5a) 28 2.4.1. -
Structural State of Chernozem After Long-Term Post-Agrogenic Transformation Demydenko O
UDC 631.434 © 2019 Structural state of chernozem after long-term post-agrogenic transformation Demydenko O. Cherkasy State Agricultural Research Station of the National Institute of Agriculture of NAAS, 13 Dokuchaieva Str., Holodnianske village, Smilianskyi district, Cherkasy oblast, Ukraine, 20731; e-mail: [email protected] The purpose. To determine the main laws of transformation and regulatory parameters of the structural state change of chernozems of the forest-steppe zone in conditions of long-term post-agrogenic transformation according to the results of dry sieving of soil samples and statistical analysis of the data using the method of principal components, factor and non-parametric analysis. Methods. Laboratory analytical, experimental field, statistical. Results. The performed statistical processing of results of the analysis of dry sieving of the structure of chernozems in the long-term post-agrogenic state demonstrates the promise of using factor, cluster and non-parametric analysis methods. An important role in the restoration of the structure of chernozems is played by a combination of structural units 3.0—0.5 mm in size, with which the additional density in the humus horizon is inversely proportional, and with the humus content, it is directly proportional. The carried out clustering indicates that the content of the presented chernozems in the state of virgin soil and long-term deposits is the separated and not similar state of soil objects. But there is a general pattern of formation of a set of structural units of 3.0-0.5 mm similar to chernozems in the state of virgin soil, which content exceeds 40-50% of the content of parts in the agronomically valuable interval. -
History of East European Chernozem Soil Degradation; Protection and Restoration by Tree Windbreaks in the Russian Steppe
Sustainability 2015, 7, 705-724; doi:10.3390/su7010705 OPEN ACCESS sustainability ISSN 2071-1050 www.mdpi.com/journal/sustainability Article History of East European Chernozem Soil Degradation; Protection and Restoration by Tree Windbreaks in the Russian Steppe Yury G. Chendev 1, Thomas J. Sauer 2,*, Guillermo Hernandez Ramirez 3 and Charles Lee Burras 4 1 Department of Natural Resources Management and Land Cadastre, Belgorod State University, Belgorod 308015, Russia; E-Mail: [email protected] 2 USDA-ARS, National Laboratory for Agriculture and the Environment, Ames, IA 50011, USA 3 Department of Renewable Resources, University of Alberta, Edmonton, AB T6G 2R3, Canada; E-Mail: [email protected] 4 Department of Agronomy, Iowa State University, Ames, IA 50011, USA; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-515-294-3416; Fax: +1-515-294-8125. Academic Editor: Marc A. Rosen Received: 30 October 2014 / Accepted: 29 December 2014 / Published: 8 January 2015 Abstract: The physiographic region of the Central Russian Upland, situated in the Central part of Eastern Europe, is characterized by very fertile grassland soils—Chernozems (Mollisols in the USDA taxonomy). However, over the last several centuries this region has experienced intense land-use conversion. The most widespread and significant land-use change is the extensive cultivation of these soils. As a result, Chernozems of the region that were some of the most naturally fertile soils in the world with thick A horizons had become, by the second half of the 19th century, weakly productive, with decreased stocks of organic matter. -
Captivity and Empire: Russian Captivity Narratives in Fact and Fiction
i CAPTIVITY AND EMPIRE: RUSSIAN CAPTIVITY NARRATIVES IN FACT AND FICTION ТҰТҚЫНДЫҚ ЖӘНЕ ИМПЕРИЯ: ШЫН ДЕРЕКТЕРДЕГІ ЖӘНЕ КӨРКЕМ ӘДЕБИЕТТЕГІ ОРЫС ТҰТҚЫНДЫҚ ХИКАЯЛАРЫ ПЛЕН И ИМПЕРИЯ: РУССКИЕ НАРРАТИВЫ О ПЛЕНУ В ФАКТАХ И В ХУДОЖЕСТВЕННОЙ ЛИТЕРАТУРЕ by YUAN GAO A Thesis Submitted to the School of Humanities and Social Sciences of Nazarbayev University in Partial Fulfillment of the Requirements for the Degree MASTER OF ARTS IN EURASIAN STUDIES ASTANA, KAZAKHSTAN 2016 ii © 2016 YUAN GAO All Rights Reserved iii CAPTIVITY AND EMPIRE: RUSSIAN CAPTIVITY NARRATIVES IN FACT AND FICTION ТҰТҚЫНДЫҚ ЖӘНЕ ИМПЕРИЯ: ШЫН ДЕРЕКТЕРДЕГІ ЖӘНЕ КӨРКЕМ ӘДЕБИЕТТЕГІ ОРЫС ТҰТҚЫНДЫҚ ХИКАЯЛАРЫ ПЛЕН И ИМПЕРИЯ: РУССКИЕ НАРРАТИВЫ О ПЛЕНУ В ФАКТАХ И В ХУДОЖЕСТВЕННОЙ ЛИТЕРАТУРЕ by YUAN GAO Principal adviser: Prof. Alexander Morrison Second reader: Dr. Victoria Thorstensson External reviewer: Dr. Katya Hokanson Electronic Version Approved: Prof. Alexander Morrison Director of the MA Program in Eurasian Studies School of Humanities and Social Sciences Nazarbayev University June 2016 iv Abstract This thesis studies Russian captivity narratives about Central Asia produced during the nineteenth century. Focusing on the captivity theme, this thesis explores diverse individual captivity stories written within the grand context of Russia’s expansion into Central Asia. It aims to show that captivity narratives not only tell of the vulnerability and uncertainty of the empire during its expansion, but also reveal the rapid shift of power in Central Asia in the nineteenth century. They witness Russian captives’ growing awareness of Central Asia as a site of Russia’s future colonization, and the captives’ self-awareness of their Russian and imperial identity. This thesis is organized according to various themes that appear repeatedly in the narratives examined. -
Chernozems (Ch)
CHERNOZEMS (CH) The Reference Soil Group of the Chernozems accommodates soils with a thick black surface layer that is rich in organic matter. Russian soil scientist Dokuchaev coined the name “Chernozems” in 1883 to denote the typical “zonal” soil of the tall grass steppes in continental Russia. Some international syno- nyms: ‘Calcareous Black Soils’, ‘Eluviated Black Soils’ (Canada), and (several suborders of) ‘Mol- lisols’ (USDA Soil Taxonomy). Definition of Chernozems Soils having 1 a mollic horizon with a moist chroma of 2 or less if the texture is finer than sandy loam, or less than 3.5 if the texture is sandy loam or coarser, both to a depth of at least 20 cm, or a mollic horizon which has these chromas directly below a plough layer; and 2 concentrations of secondary carbonates starting within 200 cm from the soil surface; and 3 no petrocalcic horizon between 25 and 100 cm from the soil surface; and 4 no secondary gypsum; and 5 no uncoated silt and sand grains on structural ped surfaces. Common soil units: Chernic, Vertic, Gleyic, Calcic, Luvic, Glossic, Siltic, Vermic, Haplic. Summary description of Chernozems Connotation: black soils rich in organic matter; from R. chern, black, and zemlja, earth or land. Parent material: mostly eolian and re-washed eolian sediments (loess). Environment: regions with a continental climate with cold winters and hot summers; in flat to undulat- ing plains with tall-grass vegetation (forest in the northern transitional zone). Profile development: AhBC-profiles with a dark brown to black mollic surface horizon over a cambic or argic subsurface horizon; commonly with redistribution of calcium carbonate to a calcic horizon or pockets of secondary carbonates in the subsurface soil.