Sugar Cane Response to Potassium Fertilization on Andisol, Entisol, and Mollisol Soils of Guatemala
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Soils Section
Soils Section 2003 Florida Envirothon Study Sections Soil Key Points SOIL KEY POINTS • Recognize soil as an important dynamic resource. • Describe basic soil properties and soil formation factors. • Understand soil drainage classes and know how wetlands are defined. • Determine basic soil properties and limitations, such as mottling and permeability by observing a soil pit or soil profile. • Identify types of soil erosion and discuss methods for reducing erosion. • Use soil information, including a soil survey, in land use planning discussions. • Discuss how soil is a factor in, or is impacted by, nonpoint and point source pollution. Florida’s State Soil Florida has the largest total acreage of sandy, siliceous, hyperthermic Aeric Haplaquods in the nation. This is commonly called Myakka fine sand. It does not occur anywhere else in the United States. There are more than 1.5 million acres of Myakka fine sand in Florida. On May 22, 1989, Governor Bob Martinez signed Senate Bill 525 into law making Myakka fine sand Florida’s official state soil. iii Florida Envirothon Study Packet — Soils Section iv Contents CONTENTS INTRODUCTION .........................................................................................................................1 WHAT IS SOIL AND HOW IS SOIL FORMED? .....................................................................3 SOIL CHARACTERISTICS..........................................................................................................7 Texture......................................................................................................................................7 -
Stabilization and Destabilization of Soil Organic Matter: Mechanisms and Controls
13F7H GEODERLIA ELSEVIER Geoderma 74 (1996) 65-105 • Stabilization and destabilization of soil organic matter: mechanisms and controls Phillip Sollins, Peter Homann, Bruce A. Caldwell Department of Forest Science Oregon State University Corvallis, OR 97331, USA Receed 1 December 1993; revised 26 July 1995; accepted 3 April 1996 Abstract We present a conceptual model of the processes by which plant leaf and root litter is transformed to soil organic C and CO 2. Stabilization of a portion of the litter C yields material that resists further transformation; destabilization yields material that is more susceptible to microbial respiration. Stability of the organic C is viewed as resulting from three general sets of characteristics. Recalcitrance comprises, molecular-level characteristics of organic substances, including elemental composition, presence of functional groups, and molecular conformation, that influence their degradation by microbes and enzymes. Interactions refers to the inter-molecular interactions between organics and either inorganic substances or other organic substances that alter the rate of degradation of those organics or synthesis of new organics. Accessibility refers to the location of organic substances with respect to microbes and enzymes. Mechanisms by which these three characteristics change through time are reviewed along with controls on those mechanisms. This review suggests that the following changes in the study of soil organic matter dynamics would speed progress: (1) increased effort to incorporate results -
The Hidden Ecological Resource of Andic Soils in Mountain Ecosystems: Evidence from Italy
Solid Earth, 9, 63–74, 2018 https://doi.org/10.5194/se-9-63-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. The hidden ecological resource of andic soils in mountain ecosystems: evidence from Italy Fabio Terribile1,2, Michela Iamarino1, Giuliano Langella1, Piero Manna2,3, Florindo Antonio Mileti1, Simona Vingiani1,2, and Angelo Basile2,3 1Department of Agricultural Sciences, University of Naples Federico II, Via Università 100, 80055 Portici (Naples), Italy 2CRISP, Interdepartmental Research Centre on the Earth Critical Zone, University of Naples Federico II, Via Università 100, 80055 Portici (Naples), Italy 3Institute for Mediterranean Agricultural and Forestry Systems, National Research Council of Italy, Via Patacca 85, 80056 Ercolano (Naples), Italy Correspondence: Fabio Terribile ([email protected]) Received: 9 June 2017 – Discussion started: 9 August 2017 Revised: 1 November 2017 – Accepted: 20 November 2017 – Published: 31 January 2018 Abstract. Andic soils have unique morphological, physical, 1 Introduction and chemical properties that induce both considerable soil fertility and great vulnerability to land degradation. More- Andic soils (i.e. soils with evident andosolization process) over, they are the most striking mineral soils in terms of are known to have a unique set of morphological, physi- large organic C storage and long C residence time. This is cal, and chemical soil properties. Andosolization (Ugolini especially related to the presence of poorly crystalline clay et al., 1988; Shoji et al., 1993) is a major soil-forming pro- minerals and metal–humus complexes. Recognition of andic cess regardless of whether these soils meet or do not meet soils is then very important. -
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. -
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 -
Sustaining the Pedosphere: Establishing a Framework for Management, Utilzation and Restoration of Soils in Cultured Systems
Sustaining the Pedosphere: Establishing A Framework for Management, Utilzation and Restoration of Soils in Cultured Systems Eugene F. Kelly Colorado State University Outline •Introduction - Its our Problems – Life in the Fastlane - Ecological Nexus of Food-Water-Energy - Defining the Pedosphere •Framework for Management, Utilization & Restoration - Pedology and Critical Zone Science - Pedology Research Establishing the Range & Variability in Soils - Models for assessing human dimensions in ecosystems •Studies of Regional Importance Systems Approach - System Models for Agricultural Research - Soil Water - The Master Variable - Water Quality, Soil Management and Conservation Strategies •Concluding Remarks and Questions Living in a Sustainable Age or Life in the Fast Lane What do we know ? • There are key drivers across the planet that are forcing us to think and live differently. • The drivers are influencing our supplies of food, energy and water. • Science has helped us identify these drivers and our challenge is to come up with solutions Change has been most rapid over the last 50 years ! • In last 50 years we doubled population • World economy saw 7x increase • Food consumption increased 3x • Water consumption increased 3x • Fuel utilization increased 4x • More change over this period then all human history combined – we are at the inflection point in human history. • Planetary scale resources going away What are the major changes that we might be able to adjust ? • Land Use Change - the world is smaller • Food footprint is larger (40% of land used for Agriculture) • Water Use – 70% for food • Running out of atmosphere – used as as disposal for fossil fuels and other contaminants The Perfect Storm Increased Demand 50% by 2030 Energy Climate Change Demand up Demand up 50% by 2030 30% by 2030 Food Water 2D View of Pedosphere Hierarchal scales involving soil solid-phase components that combine to form horizons, profiles, local and regional landscapes, and the global pedosphere. -
Distribution and Classification of Volcanic Ash Soils
83 Distribution and Classification of Volcanic Ash Soils 1* 2 Tadashi TAKAHASHI and Sadao SHOJI 1 Graduate School of Agricultural Science, Tohoku University 1-1, Tsutsumidori, Amamiya-machi, Aoba-ku, Sendai, 981-8555 Japan e-mail: [email protected] 2 Professor Emeritus, Tohoku University 5-13-27, Nishitaga, Taihaku-ku, Sendai, 982-0034 Japan *corresponding author Abstract Volcanic ash soils are distributed exclusively in regions where active and recently extinct volcanoes are located. The soils cover approximately 124 million hectares, or 0.84% of the world’s land surface. While, thus, volcanic ash soils comprise a relatively small extent, they represent a crucial land resource due to the excessively high human populations living in these regions. However, they did not receive worldwide recognition among soil scientists until the middle of the 20th century. Development of international classification systems was put forth by the 1978 Andisol proposal of G. D. Smith. The central concept of volcanic ash soils was established after the finding of nonallophanic volcanic ash soils in Japan in 1978. Nowadays, volcanic ash soils are internationally recognized as Andisols in Soil Taxonomy (United States Department of Agriculture) and Andosols in the World Reference Base for Soil Resources (FAO, International Soil Reference and Information Centre and International Society of Soil Science). Several countries including Japan and New Zealand have developed their own national classification systems for volcanic ash soils. Finally correlation of the international and domestic classification systems is described using selected volcanic ash soils. Key words: Andisols, Andosols, Japanese Cultivated Soil Classification, New Zealand Soil Classification, Soil Taxonomy, World Reference Base for Soil Resources (WRB) 1. -
Iron and Aluminum Association with Microbially Processed Organic Matter Via Meso-Density Aggregate Formation Across Soils: Organo- Metallic Glue Hypothesis
https://doi.org/10.5194/soil-2020-32 Preprint. Discussion started: 11 June 2020 c Author(s) 2020. CC BY 4.0 License. Iron and aluminum association with microbially processed organic matter via meso-density aggregate formation across soils: organo- metallic glue hypothesis 5 Rota Wagai1, Masako Kajiura1, Maki Asano2 1National Agriculture and Food Research Organization, Institute for Agro-Environmental Sciences. 3-1-3 Kan-nondai, Tsukuba, Ibaraki, 305-8604, Japan 2Faculty of Life and Environmental Sciences, University of Tsukuba, 1-1-1 Tennodai, Tsukuba, Ibaraki 305-8572, Japan Correspondence to: Rota Wagai ([email protected]) 10 Abstract. Global significance of iron (Fe) and aluminum (Al) for the storage of organic matter (OM) in soils and surface sediments is increasingly recognized. Yet specific metal phases involved or the mechanism behind metal-OM correlations frequently shown across soils remain unclear. We identified density fraction locations of major metal phases and OM using 23 soil samples from 5 climate zones and 5 soil orders (Andisols, Spodosols, Inceptisols, Mollisols, Ultisols), including several subsurface horizons and both natural and managed soils. Each soil was separated to 4 to 7 density fractions using sodium 15 polytungstate with mechanical shaking, followed by the sequential extraction of each fraction with pyrophosphate (PP), acid oxalate (OX), and finally with dithionite-citrate (DC) to estimate pedogenic metal phases of different solubility and crystallinity. The extractable Fe and Al concentrations (per fraction) generally showed unique unimodal distribution along particle density gradient for each soil and each extractable metal phase. Across the studied soils, the maximum metal concentrations were always at meso-density range (1.8-2.4 g cm-3) within which PP-extractable metals peaked at 0.3-0.4 g cm- 20 3 lower density range relative to OX- and DC-extractable metals. -
Soil Properties Database of Spanish Soils. Volumen
65°^ e 0 6,2.1 Centro de Investigaciones Energeticas, Medioambientales y Tecnoldgicas Miner A, is /X Base de Dates de Propiedades Edafoldgicas de los Suelos Espanoles. VolumenXI. CASTHIA-LEON(b): Palentia, Valladolid y Avila C. Trueba RMillan T. Schmid received C. Lago JUL 121999 C. Roquero M. Magister OSTl MormesTecnicosCiemat 898 julio,1999 1. -a;:' ' > DISCLAIMER Portions of this document may be illegible in electronic image products. Images are produced from the best available original document. Informes T ecnicos Ciemat 898 julio, 1999 Base de Dates dePropiedades Edafologicas de los Suelos Espanoles. VohnnenXL CASHLLA-LEON(b): Palencia, Valladolid y Avila C. Trueba (*) R. Millan(*) T. Schmid (*) C. Lago (*) C. Roquero (**) M.Magister (**) (*) CIEMAT (**)UPM Departamento de Impacto Ambiental de la Energia Toda correspondenica en relation con este trabajo debe dirigirse al Servicio de Information y Documentation, Centro de Investigaciones Energeticas, Medioambientales y Tecnoldgicas, Ciudad Universitaria, 28040-MADRID, ESPANA. Las solicitudes de ejemplares deben dirigirse a este mismo Servicio. Los descriptores se ban seleccionado del Thesauro del DOE para describir las materias que contiene este informe con vistas a su recuperation. La catalogacidn se ha hecho utilizando el documento DOE/TIC-4602 (Rev. 1) Descriptive Cataloguing On-Line, y la clasificacion de acuerdo con el documento DOE/TIC.4584-R7 Subject Categories and Scope publicados por el Office of Scientific and Technical Information del Departamento de Energia de los Estdos Unidos. Se autoriza la reproduction de los resumenes analiticos que aparecen en esta publication. Deposito Legal: M -14226-1995 ISSN: 1135-9420 NIRO: 238-99-003-5 Editorial CIEMAT CLASIFICACION DOE Y DESCRIPTORES 540230 SOILS; SOIL CHEMISTRY; SOIL MECHANICS; RADIONUCLIDE MIGRATION; DATA BASE MANAGEMENT; DATA COMPILATION; SPAIN; “Base de Dates de Propiedades Edafologicas de los Suelos Espanoles. -
Soil Andic Properties As Powerful Factors Explaining Deep Soil Organic Carbon Stocks Distribution: the Case of a Coffee Agrofore
SOIL Discuss., https://doi.org/10.5194/soil-2019-14 Manuscript under review for journal SOIL Discussion started: 23 April 2019 c Author(s) 2019. CC BY 4.0 License. Soil andic properties as powerful factors explaining deep soil organic carbon stocks distribution: the case of a coffee agroforestry plantation on Andosols in Costa Rica Tiphaine Chevallier1, Kenji Fujisaki1, Olivier Roupsard1,2, Florian Guidat3, Rintaro Kinoshita3,5, Elias de 5 Melo Viginio Filho3, Peter Lehner4, Alain Albrecht1 1 Eco&Sols, IRD, CIRAD, INRA, Montpellier SupAgro, Univ Montpellier, Montpellier, France 2 CIRAD, UMR Eco&Sols, LMI IESOL, B.P. 1386 CP 18524, Dakar, Senegal 3 CATIE, Tropical Agricultural Centre for Research and Higher Education, 7170 Turrialba, Costa Rica 4 Cafetalera Aquiares S.A., PO Box 362-7150, Turrialba, 7150, Costa Rica 10 5 Research Center for Global Agromedicine, Obihiro University of Agriculture and Veterinary Medecine, Obihiro, Hokkaido 080-8555, Japan Correspondence to: Tiphaine Chevallier ([email protected]) Abstract. Soil organic carbon (SOC) constitutes the largest terrestrial carbon stock. Both distribution and variation of SOC stocks are needed to constitute reference baseline for studies on temporal SOC change. Specifically, in volcanic areas, the 15 spatial variation of soil andic properties usually explains the spatial variation of topsoil SOC contents, but SOC data for deeper soil layers are needed. We measured the andic properties (e.g. pyrophosphate extractable aluminium and allophane contents) and SOC stocks down to 200-cm depth in a 1 km2 micro-watershed covered by Arabica coffee agroforestry in Costa Rica. We used diffuse reflectance mid-infrared (MIR) spectroscopy to allow a large number of soil analysis. -
Relationships Between Land Use, Fertility and Andisol Behaviour: Examples from Volcanic Islands
144 Land use, fertility,and Andisol behaviour Soil Use and Management (1999) 15, 144^149 Relationships between land use, fertility and Andisol behaviour: examples from volcanic islands S. Perret1 & M. Dorel Abstract. Soils developed on volcanic parent materials have many intrinsic qualities favourable to cropping. However, fertility decreases dramatically when they are badly managed. A short review and case studies from Re¨ union and Guadeloupe highlight the special characteristics of these soils, and their response to management. The interplay of cropping systems and physical characteristics of Andisols is first considered through the example of Pelargonium and food crop systems in Re¨ union. Progressive decrease in production and cropping potential shows in falling yields as well as in the overall decline of the system.The example of banana production in Guadeloupe highlights the increase in inputs needed to realise the land's potential and to maintain yields, in particular more tillage and pest treatment. In both cases, these trends are connected to the co-evolution of soil characteristics and cropping systems.They lead to an increase of risks with less security and less scope in the choice of cropping systems.Technical solutions in the form of erosion-control measures, rotation and planting techniques have been developed and prove to be relevant and consistent in their benefit. Keywords : Andisols, cropping systems, soil fertility,Pelargonium, bananas, Re¨ union, Guadeloupe INTRODUCTION ments of Re¨ union, Guadeloupe and Martinique. ndisols are found mostly in volcanic zones at high Soils with andic behaviour and properties can develop Aaltitudes and are widespread throughout the world in from massive basaltic lavas under heavy rainfall conditions, these environments. -
Soil Quality Indicators in an Andisol Under Different Tree Covers in Disturbed Nothofagus Forests
RESEARCH Soil quality indicators in an Andisol under different tree covers in disturbed Nothofagus forests Marianela Alfaro1, 2, Francis Dube2*, and Erick Zagal3 1Universidad de Costa Rica, Facultad de Ingeniería, Casilla 11501-2060, San José, Costa Rica. 2Universidad de Concepción, Facultad de Ciencias Forestales, Victoria 631, Concepción, Chile. *Corresponding author ([email protected]). 3Universidad de Concepción, Facultad de Agronomía, Av. Vicente Méndez 595, Chillán, Chile. Received: 3 October 2017; Accepted: 16 November 2017; doi:10.4067/S0718-58392018000100106 ABSTRACT Non-systemic logging, cattle browsing and grazing with the site natural vegetation can modify tree covers in native forests and alter the quantity and quality of organic matter entering the soil and hence its overall quality. The objective of this study was to evaluate the effect of modifying tree covers by uncontrolled logging and grazing processes on soil quality, in a mature and unmanaged roble (Nothofagus obliqua (Mirb.) Blume) forest. Soil quality was evaluated under partly-closed (PC), partly-open (PO), and open (OP) forest covers, and two soil depths. The indicators used were soil organic C (SOC), potential net N mineralization (N-min), and nitrification (N-NO3), soil microbial respiration (SMR), microbial biomass C (MBC), soil aggregates, and light fraction (LF). At 0-5 cm soil depth SMR and MBC in PC cover was approximately 12% higher than in PO and OP covers. For the same soil depth N-min in PC cover was 68% and 95% higher than in PO and OP covers, respectively; and for N-NO3 PC cover was 45% higher than PO cover. OP tree cover presented a negative N-NO3 (immobilization).