Micromorphology of Soils Micromorphology of Soils
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Tillage and Soil Ecology: Partners for Sustainable Agriculture
Soil & Tillage Research 111 (2010) 33–40 Contents lists available at ScienceDirect Soil & Tillage Research journal homepage: www.elsevier.com/locate/still Review Tillage and soil ecology: Partners for sustainable agriculture Jean Roger-Estrade a,b,*, Christel Anger b, Michel Bertrand b, Guy Richard c a AgroParisTech, UMR 211 INRA/AgroParisTech., Thiverval-Grignon, 78850, France b INRA, UMR 211 INRA/AgroParisTech. Thiverval-Grignon, 78850, France c INRA, UR 0272 Science du sol, Centre de recherche d’Orle´ans, Orle´ans, 45075, France ARTICLE INFO ABSTRACT Keywords: Much of the biodiversity of agroecosystems lies in the soil. The functions performed by soil biota have Tillage major direct and indirect effects on crop growth and quality, soil and residue-borne pests, diseases Soil ecology incidence, the quality of nutrient cycling and water transfer, and, thus, on the sustainability of crop Agroecosystems management systems. Farmers use tillage, consciously or inadvertently, to manage soil biodiversity. Soil biota Given the importance of soil biota, one of the key challenges in tillage research is understanding and No tillage Plowing predicting the effects of tillage on soil ecology, not only for assessments of the impact of tillage on soil organisms and functions, but also for the design of tillage systems to make the best use of soil biodiversity, particularly for crop protection. In this paper, we first address the complexity of soil ecosystems, the descriptions of which vary between studies, in terms of the size of organisms, the structure of food webs and functions. We then examine the impact of tillage on various groups of soil biota, outlining, through examples, the crucial effects of tillage on population dynamics and species diversity. -
Soil As a Huge Laboratory for Microorganisms
Research Article Agri Res & Tech: Open Access J Volume 22 Issue 4 - September 2019 Copyright © All rights are reserved by Mishra BB DOI: 10.19080/ARTOAJ.2019.22.556205 Soil as a Huge Laboratory for Microorganisms Sachidanand B1, Mitra NG1, Vinod Kumar1, Richa Roy2 and Mishra BB3* 1Department of Soil Science and Agricultural Chemistry, Jawaharlal Nehru Krishi Vishwa Vidyalaya, India 2Department of Biotechnology, TNB College, India 3Haramaya University, Ethiopia Submission: June 24, 2019; Published: September 17, 2019 *Corresponding author: Mishra BB, Haramaya University, Ethiopia Abstract Biodiversity consisting of living organisms both plants and animals, constitute an important component of soil. Soil organisms are important elements for preserved ecosystem biodiversity and services thus assess functional and structural biodiversity in arable soils is interest. One of the main threats to soil biodiversity occurred by soil environmental impacts and agricultural management. This review focuses on interactions relating how soil ecology (soil physical, chemical and biological properties) and soil management regime affect the microbial diversity in soil. We propose that the fact that in some situations the soil is the key factor determining soil microbial diversity is related to the complexity of the microbial interactions in soil, including interactions between microorganisms (MOs) and soil. A conceptual framework, based on the relative strengths of the shaping forces exerted by soil versus the ecological behavior of MOs, is proposed. Plant-bacterial interactions in the rhizosphere are the determinants of plant health and soil fertility. Symbiotic nitrogen (N2)-fixing bacteria include the cyanobacteria of the genera Rhizobium, Free-livingBradyrhizobium, soil bacteria Azorhizobium, play a vital Allorhizobium, role in plant Sinorhizobium growth, usually and referred Mesorhizobium. -
Soil and Litter Invertebrates and Heterotrophic Process: 1997 Revision
ES/ER/TM-126/R2 Toxicological Benchmarks for Contaminants of Potential Concern for Effects on Soil and Litter Invertebrates and Heterotrophic Process: 1997 Revision This document has been approved by the East Tennessee Technology Park Technical Information Office for release to the public. Date: ES/ER/TM-126/R2 Toxicological Benchmarks for Contaminants of Potential Concern for Effects on Soil and Litter Invertebrates and Heterotrophic Process: 1997 Revision R. A. Efroymson M. E. Will G. W. Suter II Date Issued—November 1997 Prepared for the U.S. Department of Energy Office of Environmental Management under budget and reporting code EW 20 LOCKHEED MARTIN ENERGY SYSTEMS, INC. managing the Environmental Management Activities at the East Tennessee Technology Park Oak Ridge Y-12 Plant Oak Ridge National Laboratory Paducah Gaseous Diffusion Plant Portsmouth Gaseous Diffusion Plant under contract DE-AC05-84OR21400 for the U.S. DEPARTMENT OF ENERGY PREFACE This report presents a standard method for deriving benchmarks for the purpose of “contaminant screening,” performed by comparing measured ambient concentrations of chemicals. The work was performed under Work Breakdown Structure 1.4.12.2.3.04.07.02 (Activity Data Sheet 8304). In addition, this report presents sets of data concerning the effects of chemicals in soil on invertebrates and soil microbial processes, benchmarks for chemicals potentially associated with United States Department of Energy sites, and literature describing the experiments from which data were drawn for benchmark derivation. iii ACKNOWLEDGMENTS The authors would like to thank Carla Gunderson and Art Stewart for their helpful reviews of the document. In addition, the authors would like to thank Christopher Evans and Alexander Wooten for conducting part of the literature review. -
The Nature and Dynamics of Soil Organic Matter: Plant Inputs, Microbial Transformations, and Organic Matter Stabilization
Soil Biology & Biochemistry 98 (2016) 109e126 Contents lists available at ScienceDirect Soil Biology & Biochemistry journal homepage: www.elsevier.com/locate/soilbio Review paper The nature and dynamics of soil organic matter: Plant inputs, microbial transformations, and organic matter stabilization Eldor A. Paul Natural Resource Ecology Laboratory and Department of Soil and Crop Sciences, Colorado State University, Fort Collins, CO 80523-1499, USA article info abstract Article history: This review covers historical perspectives, the role of plant inputs, and the nature and dynamics of soil Received 19 November 2015 organic matter (SOM), often known as humus. Information on turnover of organic matter components, Received in revised form the role of microbial products, and modeling of SOM, and tracer research should help us to anticipate 31 March 2016 what future research may answer today's challenges. Our globe's most important natural resource is best Accepted 1 April 2016 studied relative to its chemistry, dynamics, matrix interactions, and microbial transformations. Humus has similar, worldwide characteristics, but varies with abiotic controls, soil type, vegetation inputs and composition, and the soil biota. It contains carbohydrates, proteins, lipids, phenol-aromatics, protein- Keywords: Soil organic matter derived and cyclic nitrogenous compounds, and some still unknown compounds. Protection of trans- 13C formed plant residues and microbial products occurs through spatial inaccessibility-resource availability, 14C aggregation of mineral and organic constituents, and interactions with sesquioxides, cations, silts, and Plant residue decomposition clays. Tracers that became available in the mid-20th century made the study of SOM dynamics possible. Soil carbon dynamics Carbon dating identified resistant, often mineral-associated, materials to be thousands of years old, 13 Humus especially at depth in the profile. -
Soil Fauna: Key to New Carbon Models Authors
SOIL Discuss., doi:10.5194/soil-2016-19, 2016 Manuscript under review for journal SOIL Published: 14 April 2016 c Author(s) 2016. CC-BY 3.0 License. 1 1 2 Soil fauna: key to new carbon models 3 4 Authors 5 6 Juliane Filser1*, Jack H. Faber2, Alexei V. Tiunov3, Lijbert Brussaard4, Jan Frouz5, 7 Gerlinde De Deyn4, Alexei V. Uvarov3, Matty P. Berg6, Patrick Lavelle7, Michel Loreau8, 8 Diana H. Wall9, Pascal Querner10, Herman Eijsackers11, Juan José Jiménez12 9 10 1Center for Environmental Research and Sustainable Technolgy, University of Bremen, General and Theoretical 11 Ecology, Leobener Str. – UFT, D-28359 Bremen, Germany. 12 email: [email protected] 13 * Corresponding author 14 15 2Alterra, Wageningen UR, Droevendaalsesteeg 3, 6708 PB Wageningen, The Netherlands 16 email: [email protected] 17 3Laboratory of Soil Zoology, Institute of Ecology & Evolution, Russian Academy of Sciences, Leninsky prospekt 33, 18 119071 Moscow, Russia 19 email: [email protected] 20 email: [email protected] 21 4Dept. of Soil Quality, Wageningen University, P.O. Box 47, 6700 AA Wageningen, The Netherlands 22 email: [email protected] 23 email: [email protected] 24 5Institute for Environmental Studies, Charles University in Prague, Faculty of Science, Benátská 2, 128 43 Praha 2, 25 Czech Republic 26 email: [email protected] 27 6Vrije Universiteit Amsterdam, Department of Ecological Science, De Boelelaan 1085, 1081 HV Amsterdam, The 28 Netherlands 29 email: [email protected] 30 7Université Pierre et Marie Curie, Centre IRD Ile de France, 32, rue H. Varagnat, 93143 Bondy Cedex, France 31 email: [email protected] 32 8Centre for Biodiversity Theory and Modelling, Station d'Ecologie Théorique et Expérimentale, UMR 5321 CNRS & 33 Université Paul Sabatier, 2, route du CNRS, 09200 Moulis, France 34 email: [email protected] 35 9School of Global Environmental Sustainability & Dept. -
Fundamentals in Soil Science Course a Course Offered by the Soil Science Society of America
Fundamentals in Soil Science Course A course offered by the Soil Science Society of America. This course is divided into six modules: Fundamentals of Soil Genesis, Classification, and Morphology, Fundamentals in Soil Chemistry and Mineralogy, Fundamentals in Soil Fertility and Nutrient Management, Soil Biology and Soil Ecology, Influences and Management of Soil Physical Properties and Soil and Land Use Management. Each module contains 2 lessons. Lectures are approximately two hours. To maximize learning, students will be expected to spend time reading and studying outside of the recorded lesson. Course Description The Soil Science Fundamentals Review Course is designed to provide an overview of the fundamental concepts in soil science: Genesis, Classification and Morphology, Physics, Chemistry, Fertility, Biology, and Land Use. Instructors will use the Fundamentals Performance Objectives (POs) as a guide for discussing topics within each section, but will not go through each objective individually. However, students are encouraged to ask questions regarding specific POs if needed. The objective of the course is to provide the student with a formalized way to build their fundamental knowledge and skills within the different areas of soil science to enhance their professional skills and/or to prepare to take the Fundamentals of Soil Science Exam. Lecture material is supplemented with additional readings and practical examples to illustrate the concepts and provide practical examples of how the concepts are used in practice. This course is not designed to teach a student how to take the Fundamentals Exam, but instead is designed to complement the students existing knowledge of soil science and help the student understand the principles behind the POs. -
Soil Fauna: Key to New Carbon Models
SOIL, 2, 565–582, 2016 www.soil-journal.net/2/565/2016/ doi:10.5194/soil-2-565-2016 SOIL © Author(s) 2016. CC Attribution 3.0 License. Soil fauna: key to new carbon models Juliane Filser1, Jack H. Faber2, Alexei V. Tiunov3, Lijbert Brussaard4, Jan Frouz5, Gerlinde De Deyn4, Alexei V. Uvarov3, Matty P. Berg6, Patrick Lavelle7, Michel Loreau8, Diana H. Wall9, Pascal Querner10, Herman Eijsackers11, and Juan José Jiménez12 1Center for Environmental Research and Sustainable Technology, University of Bremen, General and Theoretical Ecology, Leobener Str. – UFT, 28359 Bremen, Germany 2Wageningen Environmental Research (Alterra), P.O. Box 47, 6700 AA Wageningen, the Netherlands 3Laboratory of Soil Zoology, Institute of Ecology & Evolution, Russian Academy of Sciences, Leninsky prospekt 33, 119071 Moscow, Russia 4Dept. of Soil Quality, Wageningen University, P.O. Box 47, 6700 AA Wageningen, the Netherlands 5Institute for Environmental Studies, Charles University in Prague, Faculty of Science, Benátská 2, 128 43 Praha 2, Czech Republic 6Vrije Universiteit Amsterdam, Department of Ecological Science, De Boelelaan 1085, 1081 HV Amsterdam, the Netherlands 7Université Pierre et Marie Curie, Centre IRD Ile de France, 32, rue H. Varagnat, 93143 Bondy CEDEX, France 8Centre for Biodiversity Theory and Modelling, Station d’Ecologie Théorique et Expérimentale, UMR5321 – CNRS & Université Paul Sabatier, 2, route du CNRS, 09200 Moulis, France 9School of Global Environmental Sustainability & Dept. Biology, Colorado State University, Fort Collins, CO 80523-1036, USA 10University of Natural Resources and Life Sciences, Department of Integrated Biology and Biodiversity Research, Institute of Zoology, Gregor-Mendel-Straße 33, 1180 Vienna, Austria 11Wageningen University and Research Centre, P.O. -
Articles, and the Creation of New Soil Habitats in Other Scientific fields Who Also Made Early Contributions Through the Weathering of Rocks (Puente Et Al., 2004)
Editorial SOIL, 1, 117–129, 2015 www.soil-journal.net/1/117/2015/ doi:10.5194/soil-1-117-2015 SOIL © Author(s) 2015. CC Attribution 3.0 License. The interdisciplinary nature of SOIL E. C. Brevik1, A. Cerdà2, J. Mataix-Solera3, L. Pereg4, J. N. Quinton5, J. Six6, and K. Van Oost7 1Department of Natural Sciences, Dickinson State University, Dickinson, ND, USA 2Departament de Geografia, Universitat de València, Valencia, Spain 3GEA-Grupo de Edafología Ambiental , Departamento de Agroquímica y Medio Ambiente, Universidad Miguel Hernández, Avda. de la Universidad s/n, Edificio Alcudia, Elche, Alicante, Spain 4School of Science and Technology, University of New England, Armidale, NSW 2351, Australia 5Lancaster Environment Centre, Lancaster University, Lancaster, UK 6Department of Environmental Systems Science, Swiss Federal Institute of Technology, ETH Zurich, Tannenstrasse 1, 8092 Zurich, Switzerland 7Georges Lemaître Centre for Earth and Climate Research, Earth and Life Institute, Université catholique de Louvain, Louvain-la-Neuve, Belgium Correspondence to: J. Six ([email protected]) Received: 26 August 2014 – Published in SOIL Discuss.: 23 September 2014 Revised: – – Accepted: 23 December 2014 – Published: 16 January 2015 Abstract. The holistic study of soils requires an interdisciplinary approach involving biologists, chemists, ge- ologists, and physicists, amongst others, something that has been true from the earliest days of the field. In more recent years this list has grown to include anthropologists, economists, engineers, medical professionals, military professionals, sociologists, and even artists. This approach has been strengthened and reinforced as cur- rent research continues to use experts trained in both soil science and related fields and by the wide array of issues impacting the world that require an in-depth understanding of soils. -
Cartoon History of Soil Microbiology, a (JNRLSE)
A Cartoon History of Soil Microbiology M. S. Coyne* ABSTRACT particularly endearing because they convey their message Students reviewing the history of soil microbiology may see while making us laugh (either inwardly or outwardly). Gary great microbiologists as icons rather than real people. I employ Larsen's portrayal of science and weird science in The Far cartoons to present a historical perspective of soil microbiolo- Side cartoon and Sidney Harris' sophisticated analyses of gy that makes this information more entertaining and conse- industrial science are classic examples of the genre. They're quently more palatable to introductory students. Basic histori- funny while simultaneously conveying either the principles, cal facts and major accomplishments of the pioneering soil foibles, or stereotypes of scientists and their science. microbiologists are present in a factual but tongue-in-cheek Much of the humor in these cartoons lies in knowing survey. The material is either presented as a slide show in class enough science to appreciate the jokes. For several years or as a part of a manual students may read at their leisure. I've been using cartoons to illustrate microbial principles for Comments about this approach have generally been favorable, students taking introductory soil microbiology at the but it lacks a rigorous test demonstrating whether it achieves University of Kentucky. What follows is a presentation I use its intended goal. This type of multimedia presentation should to introduce these students to the history of soil microbiolo- have potential application to a wider range of introductory gy and the key players who made the discipline what it is course material. -
Sustainable Soil Management
Top of Form ATTRAv2 page skip navigation 500 500 500 500 500 0 Search Bottom of Form 800-346-9140 Home | Site Map | Who We Are | Contact (English) Us | Calendar | Español | Text Only 800-411-3222 (Español) Home > Master Publication List > Sustainable Soil Management What Is Sustainable Soil Management Sustainable Agriculture? The printable PDF version of the Horticultural By Preston Sullivan entire document is available at: Crops NCAT Agriculture Specialist http://attra.ncat.org/attra- © NCAT 2004 pub/PDF/soilmgmt.pdf Field Crops ATTRA Publication #IP027/133 31 pages — 1.5 mb Download Acrobat Reader Soils & Compost Water Management Pest Management Organic Farming Livestock Marketing, Business & Risk Abstract Soybeans no-till planted into Management wheat stubble. This publication covers basic soil Photo by: Preston Sullivan Farm Energy properties and management steps toward building and maintaining healthy soils. Part I deals with basic Education soil principles and provides an understanding of living soils and how they work. In this section you will find answers to why soil organisms Other Resources and organic matter are important. Part II covers management steps to build soil quality on your farm. The last section looks at farmers who Master have successfully built up their soil. The publication concludes with a Publication List large resource section of other available information. Table of Contents Top of Form Part I. Characteristics of Sustainable Soils o Introduction o The Living Soil: Texture and Structure o The Living Soil: The Importance of Soil Organisms 1011223551022 o Organic Matter, Humus, and the Soil Foodweb o Soil Tilth and Organic Matter oi o Tillage, Organic Matter, and Plant Productivity o Fertilizer Amendments and Biologically Active Soils Go o Conventional Fertilizers Enter your o Top$oil—Your Farm'$ Capital email above o Summary of Part I and click Go. -
Soil Microbiology
Module 5 TAKING CARE OF OUR PLANET • Unit 1 PLANET EARTH IS IN THE DANGER ZONE SOIL MICROBIOLOGY 1 Read the following text and decide which of these adjectives could be used instead of those underlined in the passage: abundant, available, better, big, dangerous, entire, minute, productive, several, supreme, useful, vital. Inorganic constituents (minerals, water, process that crop residues, grass clippings, air), dead organic matter and soil life are leaves, organic wastes, etc., are decomposed the components that make up the total soil and converted to forms useable for plant environment. The living portion of the soil can growth as well as converted to stable soil be divided into macro- and micro-organisms. organic matter called ‘humus’. Macro-organisms play an important role in The large organisms function as grinders in organic decomposition by chewing plant that they reduce the particle size of organic and animal residues into fine particles. residues making them more accessible and Though the micro-organic portion represents decomposable by the soil microbes. The soil considerably less than 1% of the soil mass, it microbial population also further decomposes is on this tiny fraction that the continued re- the waste products of the larger animals. cycling of nutrients mainly depends. Thus, the activities of different groups of soil Normal, fertile soils teem with soil microbes. organisms are linked in complex “food webs”. The most numerous microbes in soil are the One beneficial process carried out exclusively bacteria followed by the actinomycetes, the by soil microbes is called nitrogen fixation, the fungi, soil algae and cyanobacteria (“blue- capture of inert N2 gas (dinitrogen) from the air green algae”) and soil protozoa. -
Faunal Activities and Soil Processes : Adaptive Strategies That Determine
F Faunal Activities .and Soil Processes: Adaptive Strategies That Determine Ecosystem Function P . LAVELLE I . Summary ................................................. 93 II . Introduction ............................................... 94 III . The role of invertebrates in the soil system ....................... 96 N . Adaptive strategies of soil organisms: the sleeping beauty and the ecosystem engineers ........................................ 97 V . Microfauna: microbial regulation in micro-foodwebs ...............101 A . The composition of micro-foodwebs ........................ 101 B., Distribution and dispersal of microsites ..................... 103 C. Evidence for the functional importance of micro-foodwebs: effects on SOM dynamics ...................104 VI . Saprophagous arthropoda: the litter transformers ..................105 A . Niche .............................................. 105 B . Structures ............................................ 105 C. Effects on physical parameters of soil ...................... 106 D . SOM dynamics ....................................... 106 E. Effects on plant growth in microcosms ..................... 108 VII. Termites and earthworms: the ecosystem engineers ................108 A . Roles ............................................... 108 B . Effects on physical structure ............................. 109 C. Effects on SOM dynamics ............................... 115 D. Effects on plant growth ................................. 118 Vm . Conclusions .............................................