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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. -
Lugares De Procedencia De Los Moriscos Granadinos Establecidos En Murcia Después De 1570
MVRGETANA. ISSN: 0213-0939. Número 131, Año LXV, 2014. Pág. 257-272. LUGARES DE PROCEDENCIA DE LOS MORISCOS GRANADINOS ESTABLECIDOS EN MURCIA DESPUÉS DE 1570 ROBERT POCKLINGTON Resumen: Tras el fracaso del levantamiento de 1568-70, los moriscos fueron deportados del Reino de Granada y repartidos por Castilla. Debido a la cercanía de la importante población mo- risca de Valencia, el rey prohibió que los expulsados se instalasen en Murcia. Se examinan los motivos de que, pese a esta prohibición, en los años siguientes la ciudad albergara varios miles de moriscos granadinos, y se compila la relación de los lugares de donde eran naturales, reflejando la manera en que articulaban estos nombres, cuyo caudal constituye una valiosa fuente de información lingüística sobre su pronunciación y la etimología de los topónimos. Palabras claves: moriscos, expulsión, topónimos, pronunciación, etimología. Abstract: After the collapse of the 1568-70 revolt, the Moriscos were deported from the Kingdom of Granada and distributed throughout Castile. The king forbade them from settling in Murcia because of the proximity of the important Morisco population of Valencia. In this paper the reasons for the presence of several thousand Granada Moriscos in Murcia in the ensuing years, despite the prohibition, are examined, and a full list of their places of origin is drawn up, reflecting the differing ways in which they articulated these place-names, and constituting a valuable bank of linguistic data concerning their pronunciation and the etymologies of the toponyms. Keywords: moriscos, deportation, toponyms, pronunciation, etymology 258 ROBERT POCKLINGTON El 1 de noviembre de 1570, finalizada la lucha en casi todos los frentes y aca- bada la rebelión y levantamiento de los moriscos granadinos, éstos fueron reunidos pueblo por pueblo en las iglesias para ser conducidos bajo escolta fuera del Reino de Granada.1 Con ello, el último intento de restituir un reino musulmán en España había fracasado, y les esperaba el exilio y su diseminación por todo el interior peninsular. -
Recorreguts Naturalístics I Geològics Per Terres De
ALGEPS REVISTA DE GEOLOGIA, SÈRIE B nº 558 - Juny del 2011 ISSN 1132 – 7014 D.L.B. 28.178 - 92 10 pàgines RECORRIDO GEOLÓGICO Y MINERO POR LAS COMARCA DE SORBAS: DESDE LA VENTA DEL POBRE Y NÍJAR A LUCAINENA DE LAS TORRES, TURRILLAS Y A TABERNAS Josep M. Mata-Perelló _______________________________________________________________ Aquest recorregut va ésser experimentat amb docents el dia 28 DE DESEMBRE DEL 2009 2 3 RECORRIDO GEOLÓGICO Y MINERO POR LAS COMARCA DE SORBAS: DESDE LA VENTA DEL POBRE Y NÍJAR A LUCAINENA DE LAS TORRES, TURRILLAS Y A TABERNAS Por Josep M. MATA-PERELLÓ NOTAS PRELIMINARES Como en otros recorridos de RECERCA GEOLÒGICA I MINERALÒGICA ..., si se dispone del tiempo suficiente, pueden efectuarse parando en todas las paradas e hijuelas. En caso contrario, recomendamos prescindir de las denominadas PARADAS - CONDICIONALES. Por otra parte y como de costumbre, creemos oportuno recomendar, que antes de iniciar el recorrido del itinerario se busque la información más amplia posible acerca del estado del recorrido de los diferentes tramos a realizar, tanto por pistas forestales, como por carreteras en mal estado de conservación. También y por otra parte, y en todo momento, recomendamos tener el máximo respeto para el Medio Natural que nos circunda. INTRODUCCIÓN El recorrido de este itinerario transcurrirá en su casi totalidad por tres unidades geológicas. Así, en un principio (por los alrededores del Cabo de Gata y entre éste y la Sierra Alhamilla) lo hará entre afloramientos cuaternarios y neógenos de la Depresión de Níjar Mientras que luego (por la Sierra Alhamilla) lo hará entre los materiales paleozoicos y triásicos de los Mantos Inferiores del Complejo Nevado - Filábride, dentro de las Zonas Intermedias de las Cordilleras Béticas. -
Redalyc.Quaternary Pedostratigraphy of the Nevado De Toluca Volcano
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Solleiro Rebolledo, Elizabeth; Macías, José Luis; Gama Castro, Jorge Enrique; Sedov, Sergey; Sulerzhitsky, Leopold D. Quaternary pedostratigraphy of the Nevado de Toluca volcano Revista Mexicana de Ciencias Geológicas, vol. 21, núm. 1, 2004, pp. 101-109 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57221112 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de Ciencias Geológicas,Quaternary v. 21 pedostratigraphy núm. 1, 2004, p. of101-109 the Nevado de Toluca volcano 101 Quaternary pedostratigraphy of the Nevado de Toluca volcano Elizabeth Solleiro-Rebolledo1,*, José Luis Macías2, Jorge Gama-Castro1, Sergey Sedov1, and Leopold D. Sulerzhitsky3 1 Instituto de Geología, 2 Insituto de Geofísica, Universidad Nacional Autónoma de México, Cd. Universitaria, 04510 México, D.F., Mexico 3 Geological Institute, Russian Academy of Sciences,Pyzhevsky 7, 119017 Moscow, Russia * [email protected] ABSTRACT Paleosol sequences of the Nevado de Toluca volcano (NTV) preserve a detailed record of late Quaternary environmental change. In fact, some studies have been used the NTV paleosols to interpret paleoenvironmental conditions, however some uncertainties still remain concerning their stratigraphic position and correlation. In this paper, we present the results of the NTV pedostratigraphy by using different paleosol units and based on present day tephrostratigraphy. We recognized eight Pleistocene paleosols, labeled PT0–PT7 which cover the 100,000–10,000 yr BP interval. -
Red De Alta 01
A R D E A N G A I R G Ó E N D T.M. ORIA A D I E C T.M. TABERNO N I V M O U R P R C T.M. PURCHENA I A T.M. PULPÍ T.M. PARTALOA T.M. LÚCAR T.M. URRÁCAL T.M. ALBOX T.M. HUÉRCAL-OVERA T.M. SOMONTÍN T.M. ARMUÑA T.M. OLULA T.M. FINES DEL RIO T.M. TÍJOLA T.M. PURCHENA T.M. ARBOLEAS O T.M. ALCONTAR T.M. SERÓN T.M. CANTORIA T.M. SUFLÍ T.M. ZURGENA T.M. MACAEL T.M. BAYARQUE E T.M. SIERRO T.M. LÍJAR T.M. LAROYA Cantoria T.M. CUEVAS N DEL ALMANZORA T.M. ALBANCHEZ T.M. CHERCOS T.M. ANTAS NUEVO Á T.M. CÓBDAR T.M. BACARES T.M. VERA T.M. BENITAGLA R T.M. ALCUDIA T.M. TAHAL DE MONTEAGUD T.M. LUBRÍN T.M. SENES BENIZALON R T.M. GARRUCHA T.M. CASTRO T.M. VELEFIQUE DE FILABRES T.M. OLULA T.M. ULEILA T.M. BÉDAR E DE CASTRO DEL T.M. LOS GALLARDOS DEL CAMPO T PLANO GUÍA T.M. MOJÁCAR T.M. MARÍA T.M. TURRE T.M. VELEZ-BLANCO I T.M. VELEZ-RUBIO T.M. CHIRIVEL T.M. GERGAL A R D E A N G A I R G Ó E N D T.M. ORIA A D I E C T.M. TABERNO N I V M O U R P R C T.M. PURCHENA I A T.M. -
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. -
Tigray Esia Soil Characteristics
TIGRAY ESIA SOIL CHARACTERISTICS INTRODUCTION The purpose of this Chapter is to describe the receiving environment in terms of soils within the Project site and surrounding area, to establish the extent to which agricultural soils will be removed from the site as a result of the proposed Tigray IAIP and RTC site developments and to identify potential risks to the identified soils and recommend associated mitigation measures. This was established by undertaking a fertility analysis of the soils sampled at the sites and calculating the potential risks that the proposed development will pose to the soils, with and without mitigation measures being put in place. The description provided in this chapter is based on primary data obtained from site investigations. AIMS AND OBJECTIVES The main aims of the soils investigation within this overarching study are threefold: 1. To establish the agricultural value of the soils to be removed in order for the proposed Tigray IAIP and its associated RTC to be built; 2. To establish the main soil-associated risks identified as a result of the proposed project, and 3. To identify potential mitigation measures associated with these risks. METHODOLOGY DESKTOP ASSESSMENT A detailed desktop assessment was undertaken for the Tigray IAIP and RTC sites. This included assessing the ISRIC World Soils Database, based on the World Reference Base Classification System (WRB, 2006) in order to establish the soil types according to an international standard system. Information associated with the outcomes of the ISRIC world soils database outcomes was reviewed, as was general information associated with Ethiopian soils, and, specifically, those found in the Tigray region. -
Chemical Properties of the Forest Litter in Istria and the Croatian Littoral
Ekológia (Bratislava) Vol. 33, No. 3, p. 242–251, 2014 doi:10.2478/eko-2014-0023 CHEMICAL PROPERTIES OF THE FOREST LITTER IN ISTRIA AND THE CROATIAN LITTORAL ANDRIJA ŠPOLJAR1, DAMIR BARČIĆ2*, TOMISLAVA PEREMIN VOLF1, STJEPAN HUSNJAK3, IVICA MARTINOVIĆ1 1 College of Agriculture at Križevci, Milislava Demerca 1, 48260 Križevci, Croatia 2 University of Zagreb Faculty of Forestry, Svetošimunska 25, 10 000 Zagreb, Croatia; e-mail: [email protected] 3 University of Zagreb Faculty of Agriculture, Svetošimunska 25, 10 000 Zagreb, Croatia * Author for correspondence Abstract Špoljar A., Barčić D., Peremin Volf T., Husnjak S., Martinović I.: Chemical properties of the forest litter in Istria and the Croatian Littoral. Ekológia (Bratislava), Vol. 33, No. 3, p. 242–251, 2014. The experiment was set up in the forest ecosystem with diverse vegetation zones in the area of Istria and the Croatian Littoral. Research included the following systematic soil units: lithic lepto- sols, rendzic leptosols, rendzic leptosols – eroded, mollic leptosols, chromic cambisol and chromic luvisols. The average quantity of the forest litter in the studied systematic soil units reaches 13.36 t/ha (Tables 1−3). The “wealth” of organic matter in the studied soil units can be presented with the following series: chromic cambisols (CMx) > mollic leptosols (LPm), organogenic, rendzic leptosols (LPk) > lithic leptosols (LPq) > chromic cambisols (CMx) – Terra rossa, chromic luvi- sols (LVx) > rendzic leptosols (LPk) – eroded. As expected, the lowest value of total nitrogen was found in the lithic leptosols in relation to almost all the other soils, except when compared with chromic cambisol and rendzic leptosols (p < 0.05). -
El Cerro Del Nacimiento (Macael), Un Asentamiento Argarico En El Valle Medio Del Rio Almanzora
CUAD. PREH. GR. 12-13, 1987-88, pp. 81-100 EL CERRO DEL NACIMIENTO (MACAEL), UN ASENTAMIENTO ARGARICO EN EL VALLE MEDIO DEL RIO ALMANZORA GABRIEL MARTINEZ FERNANDEZ RESUMEN A través del estudio del asentamiento argárico del Cerro del Nacimiento se pretende esbozar algu nos de los rasgos que caracterizan a la organización del espacio de habitación y la explotación del territorio durante la Edad del Bronce. En cuanto al urbanismo la nota más característica es la ade cuación de las estructuras a la topografía del emplazamiento elegido. Por otro lado. el patrón de asentamiento. y la evolución del mismo, se insinuarían a partir de la propuesta de integración de di ferentes recursos y potencialidades naturales, haciendo especial incidencia en las posibilidades hí dricas y territoriales para el regadío. Palabras clave: Edad del Bronce. Urbanismo. Irrigación. ABSTRACT Through the study of the Argaric settlement of the Cerro del Nacimiento. we hope to trace sorne of the features which characterize the organization of dwelling space and the exploitation of territory in the Bronze Age. As for (town) planning. the most characteristic feature is the way in which the structures are adapted to the topography of the chosen place. Furthermore. the pattern of the settle ment and its evolution can be detected from the evidence of attempts to integrate the different natu ral resources and potential of the site, with special reference to the factors of water and terrain for irrigation. Key words: Bronze Age, Urbanism, Irrigation. l. LOCALIZACION Está localizado el Cerro del Nacimiento en las estribaciones septentrionales de la Sierra de los Filabres, dentro del término municipal de Macael, a 1,5 km. -
Annex: Soil Groups, Characteristics, Distribution and Ecosystem Services
Status of the World’s Main Report Soil Resources Annex Soil groups, characteristics, distribution and ecosystem services © FAO | Giuseppe Bizzarri © FAO INTERGOVERNMENTAL TECHNICAL PANEL ON SOILS Disclaimer and copyright Recommended citation: FAO and ITPS. 2015. Status of the World’s Soil Resources (SWSR) – Main Report. Food and Agriculture Organization of the United Nations and Intergovernmental Technical Panel on Soils, Rome, Italy 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. ISBN 978-92-5-109004-6 © FAO, 2015 FAO encourages the use, reproduction and dissemination of material in this information product. Except where otherwise indicated, material may be copied, downloaded and printed for private study, research and teaching purposes, or for use in non-commercial products or services, provided that appropriate acknowledgement of FAO as the source and copyright holder is given and that FAO’s endorsement of users’ views, products or services is not implied in any way. -
Figure S4. Boxplots of the Variation of the Relative Abundances of the Four
A Region bacterivore omnivore plant parasite eukaryvore ● ● ● 20 40 ● ● ● 60 ● ● ● ● ● 40 15 ● 30 ● ● ● ● 40 ● ● ● 10 ● ● 20 ● ● ● 20 Relative abundance (%) 5 20 0 b a b 10 c b a a a a a a a Alb Hainich Schorfheide Alb Hainich Schorfheide Alb Hainich Schorfheide Alb Hainich Schorfheide B soil type bacterivore omnivore plant parasite eukaryvore ● ● ● ● ● 20 40 ● ● ● ● ● ● 60 ● ● ● ● 40 ● 15 ● ● ● ● 30 ● ● ● ● ● ● ● ● ● ● ● ● ● ● 40 ● ● ● ● ● ● ● 20 10 ● ● ● ● ● ● ● ● ● 20 ● ● Relative abundance (%) ● ● 20 5 0 10 b ac ab a bc bc ab ab b b ab ab a a ab ab a a a a a a a a a a a a a a a a Luvisol Luvisol Luvisol Luvisol Vertisol Vertisol Vertisol Vertisol Gleysol Gleysol Gleysol Gleysol Histosol Histosol Histosol Histosol Leptosol Leptosol Leptosol Leptosol Cambisol Cambisol Cambisol Cambisol Stagnosol Stagnosol Stagnosol Stagnosol Albeluvisol Albeluvisol Albeluvisol Albeluvisol C land usage bacterivore omnivore plant parasite eukaryvore ● ● ● ● ● 40 20 ● ● 60 ● ● ● ● ● 40 ● ● 15 ● 30 ● ● 40 ● ● ● ● ● 20 ● ● 10 ● ● 20 ● Relative abundance (%) 20 5 10 0 a a a a a a b a a a a a pasture mowed meadow pasture mowed meadow pasture mowed meadow pasture mowed meadow meadow meadow meadow meadow D LUI bacterivore omnivore plant parasite eukaryvore ● ● ● ● ● 40 ● ● ● ● ● 20 60 ● ● ● ● 40 ● ● ● ● 30 ● 15 ● ● ● ● 40 ● ● ● ● 20 ● ● ● 20 ● 10 Relative abundance (%) ● 20 ● ● 10 0 ● b a b b a a a c b 5 b a a ● low moderate high low moderate high low moderate high low moderate high E C/N ratio bacterivore omnivore plant parasite eukaryvore ● ● ● 20 ● 40 ● ● ● ● 60 ● ● 40 15 ● ● ● ● ● ● 30 ● ● ● ● 40 ● 10 ● ● ● ● 20 ● ● ● 20 Relative abundance (%) 5 20 a a a 10 b a a 0 a b b b a a - >10 - 15 ~10 7 - <10 >10 - 15 ~10 7 - <10 >10 - 15 ~10 7 - <10 >10 - 15 ~10 7 - <10 Figure S4. -
Classification of Soil Systems on the Basis of Transfer Factors of Radionuclides from Soil to Reference Plants
IAEA-TECDOC-1497 Classification of soil systems on the basis of transfer factors of radionuclides from soil to reference plants Proceedings of a final research coordination meeting organized by the Joint FAO/IAEA Programme of Nuclear Techniques in Food and Agriculture and held in Chania, Crete, 22–26 September 2003 June 2006 IAEA-TECDOC-1497 Classification of soil systems on the basis of transfer factors of radionuclides from soil to reference plants Report of the final research coordination meeting organized by the Joint FAO/IAEA Programme of Nuclear Techniques in Food and Agriculture held in Chania, Crete, 22–26 September 2003 June 2006 The originating Section of this publication in the IAEA was: Food and Environmental Protection Section International Atomic Energy Agency Wagramer Strasse 5 P.O. Box 100 A-1400 Vienna, Austria CLASSIFICATION OF SOIL SYSTEMS ON THE BASIS OF TRANSFER FACTORS OF RADIONUCLIDES FROM SOIL TO REFERENCE PLANTS IAEA, VIENNA, 2006 IAEA-TECDOC-1497 ISBN 92–0–105906–X ISSN 1011–4289 © IAEA, 2006 Printed by the IAEA in Austria June 2006 FOREWORD The IAEA Basic Safety Standards for Radiation Protection include the general requirement to keep all doses as low as reasonably achievable, taking account of economic and social considerations, within the overall constraint of individual dose limits. National and Regional authorities have to set release limits for radioactive effluent and also to establish contingency plans to deal with an uncontrolled release following an accident or terrorist activity. It is normal practice to assess radiation doses to man by means of radiological assessment models. In this context the IAEA published (1994), in cooperation with the International Union of Radioecologists (IUR), a Handbook of Parameter Values for the Prediction of Radionuclide Transfer in Temperate Environments to facilitate such calculations.