Making the Most of Microbes for Soil Restoration and Function

Total Page:16

File Type:pdf, Size:1020Kb

Making the Most of Microbes for Soil Restoration and Function Earth and Environment ︱ Dr Mary Ann Bruns MANAGEMENT “TARGET” NATIVE MICROBIAL HABITAT UNDERSTUDIED PRACTICE SOIL PROPERTY CONDITIONS METABOLIC REACTIONS Greater retention of CO Biophysical 2 Heterotrophic CO2 and volatile compounds integrity assimilation within the soil More varied biochemical High proportion of Making the most Reduced/ gradients and micro-site macroaggregate No tillage heterogeneity volume (Eh, pH, pO2, pCO2, volatile organics) Macropore Cover crop connectivity Facilitated diffusion of microbes for soil H2 Oxidation and tortuosity of gases and volatile compounds Increased proportion Crop High root density of rhizosphere-affected DNRA rotations and turnover restoration and function soil and particulate carbon substrates umans have drastically transformed types of soil systems can enhance Organic Mary Ann Bruns is Associate Increased supply Earth’s protective soil layers, with soil functionality by improving living amendments Long periods Professor of Soil Microbiology of root exudation of labile carbon in the Department of Ecosystem Hagriculture and mining being conditions for microbes. They define substrates among the most damaging land uses. functionality as the soil’s biologically Science and Management at Diversified root More varied supply of Atypical nosZ- Penn State University. The Severe disturbances to soils result in driven ability to capture, retain, exudates labile carbon substrates denitrification Bruns research group aims their failure to hold water and recycle and recycle water and nutrients. nutrients, two critical soil functions to to understand how beneficial High concentration functions of soil microorganisms mitigate biogeochemical and hydrological The team’s restoration research recognises and diverse carbon - Fungal NO3 can be promoted through better imbalances on a global scale. Bruns that soil functionality depends on sources Uptake management of agricultural explains: “Well-established interactions sustaining microbial viability and activity. Figure 2. Microbe-informed soil management can promote beneficial microbial processes (from Bhowmiket al., 2017.) Respective colours of text, and mining-impacted lands. among plant roots, fungi, bacteria A schematic from their recent paper (Fig. connecting arrows, and lines are blue (for physical structure improvement); green (for increased plant inputs); and red (for more diverse organic inputs). The group focuses on microbial and micro- and macrofauna are all 2) depicts how microbe-informed soil processes important in nutrient destroyed once vegetation is removed management can promote beneficial and other microbes. During degradation microbial conversion of highly mobile soils are mostly comprised of rocky cycling and water retention. and soil is upturned, buried, or eroded microbial processes through reduced of organic compounds, microbes also nitrates to ammonium. subsoils that have been stockpiled Their goal is to identify away. We want to know how functional disturbance and continued provision produce secretions that combine with less and redistributed. Microbes in these practices (Fig 1) which sustain microbial-root networks can be brought of organic residues. Here, we take a closer degradable residues to create stabilized Bruns hypothesises that moister, more soils have extremely poor living microbially assisted delivery back most effectively in altered soils look at their research which states the organic matter. Because it acts as a water energy-rich conditions in soils will conditions, with very low organic matter of water and nutrients to plants to improve nutrient recycling, water case for taking microbes into account and nutrient-retaining sponge, stabilized and result in more cost-effective retention, and plant productivity.” when managing agricultural and mining- organic matter improves microbial habitat. and lasting restoration. impacted soils, respectively. Thus, microbial degradative activity exerts The team’s restoration research recognises Agricultural and mining-impacted soils positive feedbacks on soil bio-function. that soil functionality depends on differ not only in nutrient and water RESTORING BIO-FUNCTIONS availability for plants, they provide starkly TO AGRICULTURAL SOILS Management practices that help restore sustaining microbial viability and activity. contrasting habitats for microbial life. Before being converted to agriculture, bio-functionality to agricultural soils Bruns’s team aims to learn how microbe- soils are endowed with vital stocks include reduced tillage, crop rotations with enhance the abilities of soil microbes to and little access to water and air due informed management for both of organic matter, a dark, amorphous perennial legumes, and cover cropping retain N in its less mobile forms and keep to heavy compaction by equipment. substance built up over decades, if not (Fig. 3). Winter cover crops, planted in it from being lost so quickly to the centuries, by microbial decomposition late summer or fall, add organic carbon environment. This is an important goal of plant, animal, and microbial residues. and provide a protective soil cover. Bruns for improving soil functionality, because Agricultural crop harvesting, however, and her colleagues are evaluating changes on average, less than 50% of fertilizer N is prevents most plant residues from being in soil microbial processes in response taken up by agricultural crops worldwide. returned to the soil, and tillage (e.g., to these practices in a USDA-funded plowing) disrupts and aerates soils, cropping systems experiment. RESTORING PRODUCTIVITY causing rapid microbial oxidation of TO MINING-IMPACTED LANDS organic matter. These practices, combined The Bruns group is particularly In the U.S. Appalachian region, strip with wind and water erosion, have caused interested in the relationship between mining to access near-surface coal native organic matter stocks to be lowered soil functionality and predominant forms seams has impacted millions of hectares. by half in agricultural soils worldwide. of plant-available nitrogen (N). They Although government legislation in the propose that N in its less mobile forms 1970s mandated reclamation of strip- To restore soil functionality, continued (i.e., ammonium, amino acids, proteins) mined lands, legal requirements are supply of fresh root exudates or organic predominate in well-functioning soils, based on minimum plant cover rather residues is essential. Additions of organic resulting in longer soil N residence than on soil properties, with the result Figure 1. Reduced tillage, cover cropping, matter sustain microbial degradation times and increased probability of crop that previous levels of land productivity and extended residue cover build soil Figure 3. Roots of a cover crop, organic matter and protect against erosion. of energy-rich carbon compounds to N uptake. An example of a potentially are rarely achieved post-reclamation. coated with rhizosphere soil. make mineral nutrients available to plants beneficial process under study is the Poor plant productivity persists because www.researchoutreach.org www.researchoutreach.org Whereas strip-mined lands are extensive in area, smaller “kill zones” result when Behind the Research highly acidic mine waters burst out of abandoned underground mines. As mineral-rich acid mine drainage (AMD) Mary Ann Bruns, Ph.D. emerges and flows overland, acidic metal precipitates are deposited on E: [email protected] T: +1 814 863 0779 https://ecosystems.psu.edu/directory/mvb10 http://sites.psu.edu/soilmicrobiology/photos/ the land, killing all vegetation in its wake. W: W: W: https://www.researchgate.net/profile/Maryann_Bruns A characteristic feature of a barren kill zone is a red-orange surface layer of iron oxide precipitates (below pH 3) that Research Objectives References prohibits vascular plant growth. Left unattended, kill zones remain barren for Dr Mary Ann Bruns’ work aims to learn how soil microbiome Bhowmik, Arnab, Mara Cloutier, Emily Ball, Mary Ann Bruns. 2017. Underexplored microbial metabolisms for enhanced decades, only permitting growth of acid- Figure 4. Acid mine drainage “kill zone” prior to the reclamation experiment. functions can be promoted to improve nitrogen recycling The 50-year-old barrens was created by overland flow of discharge from an nutrient recycling in agricultural soils. AIMS Microbiology 3(4): tolerant mosses or lichens. and water retention in agricultural and mined land soils. abandoned underground coal mine. 826-845. https://DOI:10.3934/microbiol.2017.4.826. Lupton, Mary Kay, Claudia Rojas, Patrick J Drohan, Mary Ann Bruns and her team have conducted Detail Bruns. 2013. Vegetation and soil development in compost- research on an accessible AMD barrens Countering expectations, all plots were CONCLUSIONS amended iron oxide precipitates at a 50-year-old acid mine in the Appalachian Plateau about 100 successfully revegetated, although To improve soil functionality, we can Mary Ann Bruns, Ph.D. drainage barrens. Restoration Ecology 21:320-328. https://doi. km from her university (Fig. 4). Most each zone supported very different make the most of resident soil microbes Associate Professor of Soil Microbiology Dept. of Ecosystem org/10.1111/j.1526-100X.2012.00902.x of the barrens is no longer inundated plant communities. Their treatment by ameliorating their living conditions, Science and Management Rojas, CR, RM Gutierrez, MA Bruns. 2016. Bacterial and eukaryal and comprises three zones differing in proved effective, even in the most providing sufficient,
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Microorganisms and Soil Fertility
    Microorganisms and Soil Fertility By WALTER BENO BOLLEN Professor of Bacteriology, Oregon State College Bacteriologist, Oregon Agricultural Experiment Station OREGON STATE COLLEGE CORVALLIS, OREGON. PRINTED AT THE COLLEGE PRESS,1959. OREGON STATE MONOGRAPHS Studies in Bacteriology Number 1 1959 Sigma Xi Award Lecture Published by Oregon State College Corvallis, Oregon Table of Contents Page Table of Contents iii List of Illustrations iii List of Tables iii Editor's Preface iv The Soil as a Culture Medium 6 The Carbon Cycle 8 Organic Matter and Nitrogen 9 The Nitrogen Cycle 14 Denitrification 16 Assimilation 17 Soil Fertility and Management 18 Ecology of Soil Microorganisms 19 Bibliography 20 List of Illustrations Figure Page 1 Constitution of the Pedosphere 5 2Composition of the Spheres of Nature in Relation to Organisms and Their Environment 5 3 The Carbon Cycle 8 4 Annual Total Agricultural Nitrogen Situation in the United States in Tons of 2,000 Pounds, 1957 12 5The Nitrogen Cycle 14 List of Tables Table Page 1 Annual Balance of Plant Nutrients in Soils of the United States, 1930 2 2Living Organisms in Fertile Soil 3 3Factors of Environment and Their Approximate Cardinal Values for General Microbology Activity in Soil 6 iii Editor's Preface Sharp-eyed readers will at once notice what appears to be a consistent typographical error throughout this MONOGRAPH. Since the word "microbology" is not one commonly found in dictionaries, it requires a note of explanation. As used here the term microbology refers to that segment of life that may be generally classified as microbes. Itis microbe-ology rather than micro- biology.
    [Show full text]
  • Soil Health—A New Challenge for Microbiologists and Chemists
    REVIEW ARTICLE INTERNATIONAL MICROBIOLOGY (2005) 8:13-21 www.im.microbios.org M. Enriqueta Arias1* Soil health—a new challenge José A. González-Pérez2 Francisco J. González-Vila2 for microbiologists and Andrew S. Ball3 chemists 1Department of Microbiology and Parasitology, University Summary. Soil health refers to the biological, chemical, and physical features of of Alcalà (Madrid), Spain soil that are essential to long-term, sustainable agricultural productivity with min- 2Natural Resources and imal environmental impact. Thus, soil health provides an overall picture of soil Agrobiology Institute of Sevilla, functionality. Although it cannot be measured directly, soil health can be inferred CSIC, Spain by measuring specific soil properties (e.g. organic matter content) and by observ- 3Department of Biological ing soil status (e.g. fertility). There is also increased interest in studying soil Sciences, University of Essex, microorganisms in their particular environments, as microbial diversity is intimate- Colchester, UK ly related to soil structure and function. One of the key objectives in determining soil health is to acquire indicators that can be used to evaluate the soil’s current sta- tus and hence to develop sustainable agricultural systems. In this regard, significant progress has been made over the last few years in the development of specific bio- markers and macromolecular probes, enabling rapid and reliable measurements of soil microbial communities. In addition, modern molecular biological techniques, such as fluorescence
    [Show full text]
  • The Soil Food Web Seasonal Microbial Activity
    '-, The Soil Food Web Arthropods Predators Birds Nematodes Fungal- and 1 101 bacterial-feeders Fungi Mycorrhizal fungi Saprophytic fungi Plants Shoots and roots Organic Protozoa Matter Amoebae, flagellates, and ciliates Waste, residue and o metabolites from Animals plants, animals and Bacteria microbes. I First trophic level : Second trophic level : Third trophic level : Fourth trophic level : Fifth and higher Photosynthesizers Decomposers Mutualists Shredders Higher level predators trophic levels : Pathogens, Parasites Predators Higher level predators Root-feeders Grazers Composting is a Seasonal Microbial Activity great way to "see" early Q summer soil organisms in V o \ a late ~ ° summer first action, breaking _ \ frost last ,a 0) down manure on C v frost the farm or leaves d V v M in the yard . S: January Month December FIGURE 2-13 The rhizosphere . The mucigel is a mixture of gelatinous and other plant products, bacterial cells and; their metabolic products, colloidal minerals, and organic matter, which together with other plant exudates, lysates, and secretions form a gradient of carbon that is most concentrated near the root surface and decreases with increasing distance away from the root . Because of this gradient, the rhizosphere is a zone of intense microbial activity. Original drawing by Kim Luoma . FIGURE 1-1 A soil habitat containing mineral soil particles (sand-Sa, silt-Si, and clay-C), organic matter (OM), water (W), plant root with root hairs (R), and soil organisms (bacteria-B, actinomycetes-A, mycorrhizal spores and hyphae-My, hyphae of a saprophytic fungus-H, a nematode-N, ciliate protozoa-CP, flagellate protozoa-FP, and a mite-M .) This soil can be a habitat of enormous complexity and diversity even over small distances .
    [Show full text]
  • Soil Organisms, Bacteria, Fungi, Protozoa, Nematodes and Rotifers
    .* .’ . SOIL ORGANISMS, BACTERIA, FUNGI, PROTOZOA, NEMATODES AND ROTIFERS Prepared By Dr. E. R. Ingham Oregon State University :’ _’ : 1995 INTERIOR COLUMBIA BASIN ECOSYSTEM MANAGEMENT PROJECT . -d-l&e* i..“, SOIL ORGANISMS: BACTERIA; FUNGI, PROTOZOA, NEMATODES, AND ROTIFERS Prepared by: Dr. E. R. Ingham Department of Botany and Plant Pathology Oregon State University Corvallis, OR 97331-2902 e-mail: [email protected] This report consists of: - a brief introduction,. - a table which summarize critical soil foodweb organisms in majo ecosystem-types found in the Columbia River Basin (Table l), - a table which summarizes critical genera or species of each soi foodweb group in each ecosystem-type (Table 2), - an overview of critical soil foodweb components responses to majo disturbances, (watershed document) and - summary reports, in the requested format, for each soil foodweb group a. Beneficial Bacteria: N-fixers - Rhizobium vd+l”.> / b. Beneficial bacteria: Cyanobacteria and crust-forming communitie Competitive bacteria: Bacillus 2 Competitive bacteria: Pseudomonas -e. Bacteria: N-immobilizers f. Bacterial pathogens VAM fungi 2: Ectoycorrhizal mat-forming fungi i. Saprophytic fungi Fungal pathogens 2: Protozoa: bacterial predators 1. Bacterial-feeding nematodes m. Fungal-feeding nematodes n. Plant-feeding nematodes 0. Rotifers INTRODUCTION The study of the community structure of soil organisms, their functiona roles in controlling ecosystem productivity and structure are only now bein investigated. Soil ecology has just begun to identify the importance o understanding soil foodweb structure and how it can control plant vegetation and how, .in turn, plant community structure affects soil organic matte quality, root exudates and therefore, alters soil foodweb structure. Sine this field is relatively new, not all the relationships have been explored nor is the fine-tuning within ecosystems well understood.
    [Show full text]
  • Zborník Abstraktov Sborník Abstraktů Abstract Proceedings
    Sponzori/Sponzoři/Sponsors Výskumný ústav pôdoznalectva a ochrany pôdy Bratislava Jaroslava Sobocká, Bořivoj Šarapatka (eds.) Ejkelkamp PD Kalná nad Hronom EKOTECHNIKA spol. s r. o. Ing. Juraj Varšányi, CSc. Mokropeská 1832 Červenej armády 179 252 28 Černošice 935 32 Kalná nad Hronom Zborník abstraktov Slovenská spoločnosť PD Podolie Sborník abstraktů pre poľnohospodárske, lesnícke, Ing. Ján Gučík potravinárske a veterinárske vedy Podolie 824 pri SAV Abstract proceedings Radlinského 9 812 37 Bratislava 1 Pôda v modernej informačnej spoločnosti Půda v moderní informační společnosti Soil in modern information society Laboratoř MORAVA s. r. o. A.KTI, s. r. o., Bučovická ul. lesnická a zemědělská 1. Konferencia Českej pedologickej spoločnosti a Societas pedologica slovaca 742 13 Studénka projekční kancelář 1. Konference České pedologické společnosti a Societas pedologica slovaca B. Antonínové 36/1 1st Conference of the Czech Society of Soil Science and Societas pedologica slovaca 621 00 Brno-Mokrá Hora ISBN 978-80-89128-34-1 20.-23. 8. 2007 Rožnov pod Radhoštěm Jaroslava Sobocká, Bořivoj Šarapatka (eds.) Zborník abstraktov Sborník abstraktů Abstract proceedings Pôda v modernej informačnej spoločnosti Půda v moderní informační společnosti Soil in modern information society 1. Konferencia Českej pedologickej spoločnosti a Societas pedologica slovaca 1. Konference České pedologické společnosti a Societas pedologica slovaca 1st Conference of the Czech Soil Science Society and Societas pedologica slovaca Rožnov pod Radhoštěm, 2007 Zborník abstraktov
    [Show full text]
  • Living Soils: the Role of Microorganisms in Soil Health
    20 June 2017 Living Soils: The Role of Microorganisms in Soil Health Christopher Johns Research Manager, Northern Australia and Land Care Research Program Key Points • Fertile soils teem with microorganisms, which directly contribute to the biological fertility of that soil. • Biological fertility is under-studied and our scientific knowledge of it is incomplete. • In addition to fertility, soil microorganisms also play essential roles in the nutrient cycles that are fundamentally important to life on the planet. • In the past, agricultural practices have failed to promote healthy populations of microorganisms, limiting production yields and threatening sustainability. • Scientific research is exploring new and exciting possibilities for the restoration and promotion of healthy microbial populations in the soil. ‘Soil is essential for the maintenance of biodiversity above and below ground. The wealth of biodiversity below ground is vast and unappreciated: millions of microorganisms live and reproduce in a few grams of topsoil, an ecosystem essential for life on earth…’ From: Australian Soils and Landscape, An Illustrated Compendium Summary Soil fertility comprises three interrelated components: physical fertility, chemical fertility and biological fertility. Biological fertility, the organisms that live in the soil and interact with the other components, varies greatly depending upon conditions and it is highly complex and dynamic. It is the least well-understood fertility component. In addition to soil fertility, soil microorganisms play essential roles in the nutrient cycles that are fundamental to life on the planet. Fertile soils teem with soil microbes. There may be hundreds of millions to billions of microbes in a single gram of soil. The most numerous microbes in soil are the bacteria, followed in decreasing numerical order by the actinomycetes, the fungi, soil algae and soil protozoa.
    [Show full text]