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Topic: Soil Classification
Programme: M.Sc.(Environmental Science) Course: Soil Science Semester: IV Code: MSESC4007E04 Topic: Soil Classification Prof. Umesh Kumar Singh Department of Environmental Science School of Earth, Environmental and Biological Sciences Central University of South Bihar, Gaya Note: These materials are only for classroom teaching purpose at Central University of South Bihar. All the data/figures/materials are taken from several research articles/e-books/text books including Wikipedia and other online resources. 1 • Pedology: The origin of the soil , its classification, and its description are examined in pedology (pedon-soil or earth in greek). Pedology is the study of the soil as a natural body and does not focus primarily on the soil’s immediate practical use. A pedologist studies, examines, and classifies soils as they occur in their natural environment. • Edaphology (concerned with the influence of soils on living things, particularly plants ) is the study of soil from the stand point of higher plants. Edaphologist considers the various properties of soil in relation to plant production. • Soil Profile: specific series of layers of soil called soil horizons from soil surface down to the unaltered parent material. 2 • By area Soil – can be small or few hectares. • Smallest representative unit – k.a. Pedon • Polypedon • Bordered by its side by the vertical section of soil …the soil profile. • Soil profile – characterize the pedon. So it defines the soil. • Horizon tell- soil properties- colour, texture, structure, permeability, drainage, bio-activity etc. • 6 groups of horizons k.a. master horizons. O,A,E,B,C &R. 3 Soil Sampling and Mapping Units 4 Typical soil profile 5 O • OM deposits (decomposed, partially decomposed) • Lie above mineral horizon • Histic epipedon (Histos Gr. -
Eletrochemical Changes in Gleysol of the Amazon Estuary
http://dx.doi.org/10.4322/rca.1796 ORIGINAL ARTICLE George Rodrigues da Silva1* Paulo Augusto Lobato da Silva2 Sérgio Brazão e Silva1 Mário Lopes da Silva Junior1 Eletrochemical changes in Gleysol of the Marcos André Piedade Gama1 Antonio Rodrigues Fernandes1 Amazon estuary Alterações eletroquímicas em Gleissolo do estuário 1 Universidade Federal Rural da Amazônia – UFRA, Instituto de Ciências Agrárias, Av. Presidente Tancredo Neves, 2501, 66077-830, Belém, PA, amazônico Brasil 2 Empresa de Assistência Técnica e Extensão Rural do Estado do Pará – EMATER/PA, Rodovia BR- 316, km 12, s/n, 67105-970, Ananindeua, PA, ABSTRACT: Electrochemical reactions are intensified by soil flooding, which changes Brasil the dynamics of nutrients and negatively affects plant growth. In this work, we aimed to Corresponding Author: evaluate the changes in the redox potential (Eh), pH and nutrient availability in a Haplic E-mail: [email protected] Gleysol soil from a floodplain of the Guamá River, Belém, Pará State. During the period of floods (61 days), samples soils were collected on alternate days and analyzed in dry and wet conditions. Flooding resulted in higher pH values and decreased Eh, which stabilized after 32 days of flooding and did not affect the values of total nitrogen. An increase in the KEYWORDS Oxidation-reduction concentrations of phosphorus, sulfur, iron, manganese, copper and zinc were observed, and Availability of nutrients they were subsequently reduced with time of submergence. The reduction of sulfur occurred Waterlogged soils at low Eh and pH values near neutrality. The results show that nitrogen and sulfur do not limit agricultural production in the lowland soils of the Guamá River. -
The Impact of White Pine (Pinus Strobus) on a Mollisol After Seven Decades of Soil Development
Journal of the Iowa Academy of Science: JIAS Volume 111 Number 3-4 Article 4 2004 The Impact of White Pine (Pinus strobus) on a Mollisol After Seven Decades of Soil Development Irina Kovda Institute of Geography, Moscow Eric C. Brevik Iowa State University Thomas E. Fenton Moscow State University Maria Gerasimova Valdosta State University Let us know how access to this document benefits ouy Copyright © Copyright 2005 by the Iowa Academy of Science, Inc. Follow this and additional works at: https://scholarworks.uni.edu/jias Part of the Anthropology Commons, Life Sciences Commons, Physical Sciences and Mathematics Commons, and the Science and Mathematics Education Commons Recommended Citation Kovda, Irina; Brevik, Eric C.; Fenton, Thomas E.; and Gerasimova, Maria (2004) "The Impact of White Pine (Pinus strobus) on a Mollisol After Seven Decades of Soil Development," Journal of the Iowa Academy of Science: JIAS, 111(3-4), 58-66. Available at: https://scholarworks.uni.edu/jias/vol111/iss3/4 This Research is brought to you for free and open access by the Iowa Academy of Science at UNI ScholarWorks. It has been accepted for inclusion in Journal of the Iowa Academy of Science: JIAS by an authorized editor of UNI ScholarWorks. For more information, please contact [email protected]. Jour. Iowa Acad. Sci. 111(3,4):58-66, 2004 The Impact of White Pine (Pinus strobus) on a Mollisol After Seven Decades of Soil Development IRINA KOVDA1, ERIC C. BREVIK2A, THOMAS E. FENTON2, and MARIA GERASIMOVA3 1 Institute of Geography, Staromonetny 29, Moscow, 109017, -
Prairie Wetland Soils: Gleysolic and Organic Angela Bedard-Haughn Department of Soil Science, University of Saskatchewan
PS&C Prairie Soils & Crops Journal Agricultural Soils of the Prairies Prairie Wetland Soils: Gleysolic and Organic Angela Bedard-Haughn Department of Soil Science, University of Saskatchewan Summary Gleysolic and Organic soils are collectively referred to as “wetland soils”. They are found in wet low-lying or level landscape positions. Gleysolic soils are found throughout the agricultural Prairies, in association with Chernozemic and Luvisolic soils. In semi-arid regions, they are frequently tilled in dry years and can be very productive due to their relatively high levels of soil moisture and nutrients. In the Prairie Provinces, Organic soils tend to be mostly associated with the Boreal transition zones at the northern and eastern perimeter of the Prairies. With proper management, these can also provide productive agricultural land, particularly for forages. Introduction Soils of the Gleysolic and Organic orders are collectively referred to as “wetland soils”. Soil maps of the agricultural region of the Canadian Prairies seldom have areas mapped as dominantly Gleysolic8 or Organic9; however, these soils are found throughout the region wherever climate and/or topography have led to persistent water-saturated conditions. Gleysols are mineral soils with colors that reflect intermittent or prolonged anaerobic (i.e., saturated, low oxygen) conditions (Fig. 1A). Organic soils reflect permanent anaerobic conditions, which lead to soils that are made up of variably decomposed plant residues, mostly from water-tolerant (i.e., hydrophytic) vegetation (Fig. 1B). Figure 1: A) Humic Luvic Gleysol, Saskatchewan and B) Typic Fibrisol (Organic), Manitoba7. Of the some 100,000,000 ha covered by the Canada Land Inventory (CLI) in the Prairie Provinces12, Gleysolic soils occupy less than 15% of the Prairie ecoregions and up to 40% in the Mid-Boreal (boreal = “northern”) Upland (Alberta) and Interlake Plain (Manitoba) ecoregions12. -
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. -
Kaolinite Dating from Acrisol and Ferralsol
Kaolinite dating from Acrisol and Ferralsol: A new key to understanding the landscape evolution in NW Amazonia (Brazil) Maximilien Mathian, Guilherme Taitson Bueno, Etienne Balan, Emmanuel Fritsch, Nádia Regina Do Nascimento, Madeleine Selo, Thierry Allard To cite this version: Maximilien Mathian, Guilherme Taitson Bueno, Etienne Balan, Emmanuel Fritsch, Nádia Regina Do Nascimento, et al.. Kaolinite dating from Acrisol and Ferralsol: A new key to understand- ing the landscape evolution in NW Amazonia (Brazil). Geoderma, Elsevier, 2020, 370, pp.114354. 10.1016/j.geoderma.2020.114354. hal-03047287 HAL Id: hal-03047287 https://hal.archives-ouvertes.fr/hal-03047287 Submitted on 14 Dec 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Kaolinite dating from Acrisol and Ferralsol: a new key to 2 understanding the landscape evolution in NW Amazonia (Brazil) 3 4 Maximilien Mathian1, Guilherme Taitson Bueno2, Etienne Balan1, Emmanuel Fritsch1, Nádia 5 Regina do Nascimento3, Madeleine Selo1, Thierry Allard1 6 7 1Sorbonne Université, Institut de minéralogie, de physique des matériaux et de cosmochimie, UMR 8 CNRS 7590, IRD, MNHN, Université Pierre et Marie Curie, 4 Place Jussieu, 75005, France 9 2Federal University of Goiás - UFG, Instituto de Estudos Socioambientais, Av. -
Soils Diversity Iberian Peninsula
SOILS DIVERSITY IN THE SOUTHWEST OF IBERIAN PENINSULA Beatriz Ramírez1; Luís Fernández-Pozo1; José Cabezas1; Rui Alexandre Castanho1*; Luís Loures2 1 Environmental Resources Analysis Research Group (ARAM). University of Extremadura. Badajoz. Spain. 2 ESAE – Portalegre Polytechnic School, Portugal and Research Centre for Spatial and Organizational Dynamics (CIEO), University of Algarve, Portugal. * Presenter | 28.04.2017 |Room 2.20 authors contacts: [email protected] | [email protected]| joca fer @unex.es | [email protected] | [email protected] INTRODUCTION An increase in the development of Digital Soil Cartography methods has been noticed in recent decades. The proposal put forward by the World Reference Base for Soil Resource (WRB) (FAO, 1998) establishes that, for the World Map Soils, a first level with 30 soils typologies and for the second 531. In Europe, the development of this mapping has been coordinated by European Soil Bureau Network (ESBN), the European Environment Agency (EEA) and also by Food and Agriculture Organization of the United Nations (FAO), identifying 26 first level soils typologies and 134 from the second level. INTRODUCTION Taking as reference the mentioned soil map, the research group have been studied the pedodiversity in the Southwest of Iberian Peninsula (Euro region Alentejo-Centro- Extremadura, EUROACE) through the use of Geographical Information Systems and diversity algorithms. The pedodiversity concept, takes its origin in ecological measures and defines, according to Ibañez et al., (1998): “the soil variability in a specific area or region, determined by its constitution, types, attributes and the conditions in which the different types of soils were formed ". The edafodiversity analysis, using diversity indexes, has allowed to approach in a quantitative and rigorous way the soils geography, and also enable to classify to the edafo-rate according to their spatial distribution typologies. -
The Muencheberg Soil Quality Rating (SQR)
The Muencheberg Soil Quality Rating (SQR) FIELD MANUAL FOR DETECTING AND ASSESSING PROPERTIES AND LIMITATIONS OF SOILS FOR CROPPING AND GRAZING Lothar Mueller, Uwe Schindler, Axel Behrendt, Frank Eulenstein & Ralf Dannowski Leibniz-Zentrum fuer Agrarlandschaftsforschung (ZALF), Muencheberg, Germany with contributions of Sandro L. Schlindwein, University of St. Catarina, Florianopolis, Brasil T. Graham Shepherd, Nutri-Link, Palmerston North, New Zealand Elena Smolentseva, Russian Academy of Sciences, Institute of Soil Science and Agrochemistry (ISSA), Novosibirsk, Russia Jutta Rogasik, Federal Agricultural Research Centre (FAL), Institute of Plant Nutrition and Soil Science, Braunschweig, Germany 1 Draft, Nov. 2007 The Muencheberg Soil Quality Rating (SQR) FIELD MANUAL FOR DETECTING AND ASSESSING PROPERTIES AND LIMITATIONS OF SOILS FOR CROPPING AND GRAZING Lothar Mueller, Uwe Schindler, Axel Behrendt, Frank Eulenstein & Ralf Dannowski Leibniz-Centre for Agricultural Landscape Research (ZALF) e. V., Muencheberg, Germany with contributions of Sandro L. Schlindwein, University of St. Catarina, Florianopolis, Brasil T. Graham Shepherd, Nutri-Link, Palmerston North, New Zealand Elena Smolentseva, Russian Academy of Sciences, Institute of Soil Science and Agrochemistry (ISSA), Novosibirsk, Russia Jutta Rogasik, Federal Agricultural Research Centre (FAL), Institute of Plant Nutrition and Soil Science, Braunschweig, Germany 2 TABLE OF CONTENTS PAGE 1. Objectives 4 2. Concept 5 3. Procedure and scoring tables 7 3.1. Field procedure 7 3.2. Scoring of basic indicators 10 3.2.0. What are basic indicators? 10 3.2.1. Soil substrate 12 3.2.2. Depth of A horizon or depth of humic soil 14 3.2.3. Topsoil structure 15 3.2.4. Subsoil compaction 17 3.2.5. Rooting depth and depth of biological activity 19 3.2.6. -
Diagnostic Horizons
Exam III Wednesday, November 7th Study Guide Posted Tomorrow Review Session in Class on Monday the 4th Soil Taxonomy and Classification Diagnostic Horizons Epipedons Subsurface Mollic Albic Umbric Kandic Ochric Histic Argillic Melanic Spodic Plaggen Anthropic Oxic 1 Surface Horizons: Mollic- thick, dark colored, high %B.S., structure Umbric – same, but lower B.S. Ochric – pale, low O.M., thin Histic – High O.M., thick, wet, dark Sub-Surface Horizons: Argillic – illuvial accum. of clay (high activity) Kandic – accum. of clay (low activity) Spodic – Illuvial O.M. accumulation (Al and/or Fe) Oxic – highly weathered, kaolinite, Fe and Al oxides Albic – light colored, elluvial, low reactivity Elluviation and Illuviation Elluviation (E horizon) Organic matter Clays A A E E Bh horizon Bt horizon Bh Bt Spodic horizon Argillic horizon 2 Soil Taxonomy Diagnostic Epipedons Diagnostic Subsurface horizons Moisture Regimes Temperature Regimes Age Texture Depth Soil Taxonomy Soil forming processes, presence or Order Absence of major diagnostic horizons 12 Similar genesis Suborder 63 Grasslands – thick, dark Great group 250 epipedons High %B.S. Sub group 1400 Family 8000 Series 19,000 Soil Orders Entisols Histosols Inceptisols Andisols Gelisols Alfisols Mollisols Ultisols Spodosols Aridisols Vertisols Oxisols 3 Soil Orders Entisol Ent- Recent Histosol Hist- Histic (organic) Inceptisol Incept- Inception Alfisol Alf- Nonsense Ultisol Ult- Ultimate Spodosol Spod- Spodos (wood ash) Mollisol Moll- Mollis (soft) Oxisol Ox- oxide Andisol And- Ando (black) Gelisol -
Assessment of Variability in the Quality of an Acrisol Under Different Land Use Systems in Ghana
Open Journal of Soil Science, 2012, 2, 33-43 33 http://dx.doi.org/10.4236/ojss.2012.21006 Published Online March 2012 (http://www.SciRP.org/journal/ojss) Assessment of Variability in the Quality of an Acrisol under Different Land Use Systems in Ghana Emmanuel Osadu Ghartey, Gabriel N. N. Dowuona*, Eric K. Nartey, Thomas A. Adjadeh, Innocent Y. D. Lawson Department of Soil Science, School of Agriculture, University of Ghana, Legon, Ghana. Email: *[email protected] Received November 10th, 2011; revised December 20th, 2011; accepted December 30th, 2011 ABSTRACT Three land use types (natural fallow, Leucaena leucocephala woodlot and cultivated plots) on a Ferric Acrisol in a semi-arid tropical zone of Ghana were compared to assess their effects on variability in selected soil properties and plant biomass accumulation. Organic carbon accumulation in the representative natural fallow profile was 22.7 g/kg, followed by 16.5 g/kg for the Leucaena woodlot and lastly 11.8 g/kg for the cultivated site. The mean bulk density of the natural fallow, Leucaena woodlot and cultivated sites were from 1.36 Mg/m3, 0.92 Mg/m3 and 1.33 Mg/m3 with corresponding range in mean weight diameter of 0.5 mm - 1.2 mm, 0.6 mm - 1.2 mm and 1.0 mm - 1.2 mm, respec- tively. The lower bulk density observed for the woodlot corresponds to increased total porosity, aeration, and root pro- liferation due to the stronger and extensive rooting system. Significant differences (P < 0.05) in bulk density, mean weight diameter (MWD), clay content, organic carbon and total nitrogen existed among the land use types. -
Impact of Tillage on Physical Characteristics in a Mollisol of Northeast China
Plant Soil Environ. Vol. 60, 2014, No. 7: 309–313 Impact of tillage on physical characteristics in a Mollisol of Northeast China X.W. Chen, A.Z. Liang, S.X. Jia, X.P. Zhang, S.C. Wei Key Laboratory of Mollisols Agroecology, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, P.R. China ABSTRACT Soil management is aimed at the maintenance of optimal soil physical quality for crop production. In order to ex- plore the effects of tillage practices on soil physical properties, a study was conducted to compare the effects of no tillage (NT), moldboard plow (MP) and ridge tillage (RT) on soil bulk density (BD), soil penetration resistance (SPR), soil water content (SWC), soil macroporosity (MAC) and soil air-filled porosity (AFP) in Northeast China. Results showed that both NT and RT led to significant BD increment than MP at 0–20 cm (P < 0.05). Compared with MP, NT and RT increased SPR at the depths of 2.5–17.5 cm (P < 0.05). SWC of 0–10 cm layer was significantly higher in NT and RT than MP soils (P < 0.05). NT showed a significantly lower MAC than MP and RT at 0–20 cm soil depths (P < 0.05). All AFP values were above the limit of 0.10 cm3/cm3 under all tillage treatments. RT im- proved the soil physical quality as evidenced by decreased BD and SPR, and increased SWC, MAC and AFP relative to NT. Keywords: soil bulk density; soil penetration resistance; soil water content; soil macroporosity; soil air-filled porosity Soil physical properties can influence the avail- factor is soil air-filled porosity (AFP), an important ability and uptake of water, oxygen and nutrients criterion for soil aeration which is commonly used for plant growth (Filho et al. -
Soil Organic Matter As Sole Indicator of Soil Degradation
Environ Monit Assess (2017) 189:176 DOI 10.1007/s10661-017-5881-y Soil organic matter as sole indicator of soil degradation S.E. Obalum & G.U. Chibuike & S. Peth & Y. Ouyang Received: 27 July 2016 /Accepted: 7 March 2017 # Springer International Publishing Switzerland 2017 Abstract Soil organic matter (SOM) is known to play properties as well. Thus, functions of SOM almost al- vital roles in the maintenance and improvement of many ways affect various soil properties and processes and soil properties and processes. These roles, which largely engage in multiple reactions. In view of its role in soil influence soil functions, are a pool of specific contribu- aggregation and erosion control, in availability of plant tions of different components of SOM. The soil func- nutrients and in ameliorating other forms of soil degra- tions, in turn, normally define the level of soil degrada- dation than erosion, SOM has proven to be an important tion, viewed as quantifiable temporal changes in a soil indicator of soil degradation. It has been suggested, that impairs its quality. This paper aims at providing a however, that rather than the absolute amount, temporal generalized assessment of the current state of knowl- change and potential amount of SOM be considered in edge on the usefulness of SOM in monitoring soil its use as indicator of soil degradation, and that SOM degradation, based on its influence on the physical, may not be an all-purpose indicator. Whilst SOM re- chemical and biological properties and processes of mains a candidate without substitute as long as a one- soils.