A Future for Soil Ecology ? Connecting the System Levels
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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 Ecology
LSC 322 Laboratory 10 LAB #10: SOIL ECOLOGY Soil is one of the earth’s most important resources. For a community of plants and animals to become established on land, soil must first be present. Further, soil quality is often a limiting factor for growth many systems. Soil is a complex mixture of inorganic and organic materials, microorganisms, water and air. The weathering of bedrock produces small grains of rock that accumulate as a layer on the surface of the earth. There they are altered by biology, becoming mixed with organic matter, which results from the decomposition of the waste products and dead tissue of living organisms to form humus. The soil formation process is very slow (hundreds to thousands of years), so it can be very detrimental to a community if the soil is lost through erosion or its quality degraded by pollution or misuse. Soil Sampling As a class, we will identify interesting soil ecosystems on campus that we would like to examine further. Your small group will be assigned to collect one of those samples. Using a trowel, you will scoop the top 5 cm (this is where most of the biological “action” happens) into a ziplock bag. Also, take notes to record the environmental surroundings. What is the land usage? What plants are growing here? What is the soil moisture? These environmental characteristics will influence many aspects of the soil. Questions - Describe the environment from which you took your soil sample. Include all of the information from your notes. - How do these conditions relate to the soil characteristics measured during the lab exercise (texture, nutrients, pH, and biota)? After samples are collected, we will return to the lab and measure the following characteristics: Soil Texture Soil texture refers to the proportion of sand, silt, and clay present in a soil, which differ in their particle size. -
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. -
Dynamics of Carbon 14 in Soils: a Review C
Radioprotection, Suppl. 1, vol. 40 (2005) S465-S470 © EDP Sciences, 2005 DOI: 10.1051/radiopro:2005s1-068 Dynamics of Carbon 14 in soils: A review C. Tamponnet Institute of Radioprotection and Nuclear Safety, DEI/SECRE, CADARACHE, BP. 1, 13108 Saint-Paul-lez-Durance Cedex, France, e-mail: [email protected] Abstract. In terrestrial ecosystems, soil is the main interface between atmosphere, hydrosphere, lithosphere and biosphere. Its interactions with carbon cycle are primordial. Information about carbon 14 dynamics in soils is quite dispersed and an up-to-date status is therefore presented in this paper. Carbon 14 dynamics in soils are governed by physical processes (soil structure, soil aggregation, soil erosion) chemical processes (sequestration by soil components either mineral or organic), and soil biological processes (soil microbes, soil fauna, soil biochemistry). The relative importance of such processes varied remarkably among the various biomes (tropical forest, temperate forest, boreal forest, tropical savannah, temperate pastures, deserts, tundra, marshlands, agro ecosystems) encountered in the terrestrial ecosphere. Moreover, application for a simplified modelling of carbon 14 dynamics in soils is proposed. 1. INTRODUCTION The importance of carbon 14 of anthropic origin in the environment has been quite early a matter of concern for the authorities [1]. When the behaviour of carbon 14 in the environment is to be modelled, it is an absolute necessity to understand the biogeochemical cycles of carbon. One can distinguish indeed, a global cycle of carbon from different local cycles. As far as the biosphere is concerned, pedosphere is considered as a primordial exchange zone. Pedosphere, which will be named from now on as soils, is mainly located at the interface between atmosphere and lithosphere. -
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. -
Dynamics of Soil Nitrogen and Carbon Accumulation for 61 Years After Agricultural Abandonment
Ecology, 81(1), 2000, pp. 88±98 q 2000 by the Ecological Society of America DYNAMICS OF SOIL NITROGEN AND CARBON ACCUMULATION FOR 61 YEARS AFTER AGRICULTURAL ABANDONMENT JOHANNES M. H. KNOPS1 AND DAVID TILMAN Department of Ecology, Evolution and Behavior, University of Minnesota, St. Paul, Minnesota 55108 USA Abstract. We used two independent methods to determine the dynamics of soil carbon and nitrogen following abandonment of agricultural ®elds on a Minnesota sand plain. First, we used a chronosequence of 19 ®elds abandoned from 1927 to 1982 to infer soil carbon and nitrogen dynamics. Second, we directly observed dynamics of carbon and nitrogen over a 12-yr period in 1900 permanent plots in these ®elds. These observed dynamics were used in a differential equation model to predict soil carbon and nitrogen dynamics. The two methods yielded similar results. Resampling the 1900 plots showed that the rates of accumulation of nitrogen and carbon over 12 yr depended on ambient carbon and nitrogen levels in the soil, with rates of accumulation declining at higher carbon and nitrogen levels. A dynamic model ®tted to the observed rates of change predicted logistic dynamics for nitrogen and carbon accumulation. On average, agricultural practices resulted in a 75% loss of soil nitrogen and an 89% loss of soil carbon at the time of abandonment. Recovery to 95% of the preagricultural levels is predicted to require 180 yr for nitrogen and 230 yr for carbon. This model accurately predicted the soil carbon, nitrogen, and carbon : nitrogen ratio patterns observed in the chronosequence of old ®elds, suggesting that the chronose- quence may be indicative of actual changes in soil carbon and nitrogen. -
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. -
Soils and Soil-Forming Material Technical Information Note 04 /2017 30Th November 2017
Soils and Soil-forming Material Technical Information Note 04 /2017 30th November 2017 Contents 1. Introduction to Soils ........................................................................................................................ 2 2. Components and Properties of Soil ................................................................................................ 7 3. Describing and Categorising soils .................................................................................................. 29 4. Policy, Regulation and Roles ......................................................................................................... 34 5. Soil Surveys, Handling and Management ..................................................................................... 40 6. Recommended Soil Specifications ................................................................................................ 42 7. References .................................................................................................................................... 52 “Upon this handful of soil our survival depends. Husband it and it will grow our food, our fuel, and our shelter and surround us with beauty. Abuse it and the soil will collapse and die, taking humanity with it.” From Vedas Sanskrit Scripture – circa 1500 BC The aim of this Technical Information Note is to assist Landscape Professionals (primarily landscape architects) when considering matters in relation to soils and soil-forming material. Soil is an essential requirement for providing -
REGENERATIVE AGRICULTURE and the SOIL CARBON SOLUTION SEPTEMBER 2020
REGENERATIVE AGRICULTURE and the SOIL CARBON SOLUTION SEPTEMBER 2020 AUTHORED BY: Jeff Moyer, Andrew Smith, PhD, Yichao Rui, PhD, Jennifer Hayden, PhD REGENERATIVE AGRICULTURE IS A WIN-WIN-WIN CLIMATE SOLUTION that is ready for widescale implementation now. WHAT ARE WE WAITING FOR? Table of Contents 3 Executive Summary 5 Introduction 9 A Potent Corrective 11 Regenerative Principles for Soil Health and Carbon Sequestration 13 Biodiversity Below Ground 17 Biodiversity Above Ground 25 Locking Carbon Underground 26 The Question of Yields 28 Taking Action ACKNOWLEDGMENTS 30 Soil Health for a Livable Future Many thanks to the Paloma Blanca Foundation and Tom and Terry Newmark, owners of Finca Luna Nueva Lodge and regenerative farm in 31 References Costa Rica, for providing funding for this paper. Tom is also the co-founder and chairman of The Carbon Underground. Thank you to Roland Bunch, Francesca Cotrufo, PhD, David Johnson, PhD, Chellie Pingree, and Richard Teague, PhD for providing interviews to help inform the paper. EXECUTIVE SUMMARY The environmental impacts of agricultural practices This introduction is co-authored by representatives of two The way we manage agricultural land 140 billion new tons of CO2 contamination to the blanket of and translocation of carbon from terrestrial pools to formative organizations in the regenerative movement. matters. It matters to people, it matters to greenhouse gases already overheating our planet. There is atmospheric pools can be seen and felt across a broad This white paper reflects the Rodale Institute’s unique our society, and it matters to the climate. no quarreling with this simple but deadly math: the data are unassailable. -
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. -
The Soil Food Web
THE SOIL FOOD WEB HEALTHY SOIL HEALTHY ENVIRONMENT The Soil Food Web Alan Sundermeier Extension Educator and Program Leader, Wood County Extension, The Ohio State University. Vinayak Shedekar Postdoctural Researcher, The Ohio State University. A healthy soil depends on the interaction of many organisms that make up the soil food web. These organisms live all or part of their life cycle in the soil and are respon- sible for converting energy as one organism consumes another. Source: Soil Biology Primer The phospholipid fatty acid (PLFA) test can be used to measure the activity of the soil food web. The following chart shows that mi-crobial activity peaks in early summer when soil is warm and moisture is adequate. Soil sampling for detecting soil microbes should follow this timetable to better capture soil microbe activity. The soil food web begins with the ener- gy from the sun, which triggers photo- synthesis in plants. Photosynthesis re- sults in plants using the sun’s energy to fix carbon dioxide from the atmosphere. This process creates the carbon and organic compounds contained in plant material. This is the first trophic level. Then begins building of soil organic matter, which contains both long-last- ing humus, and active organic matter. Active organic matter contains readily available energy, which can be used by simple soil organisms in the second trophic level of the soil food web. Source: Soil Biology Primer SOILHEALTH.OSU.EDU THE SOIL FOOD WEB - PAGE 2 The second trophic level contains simple soil organisms, which Agriculture can enhance the soil food web to create more decompose plant material.