Lithosphere & Pedosphere Observation Requirements Table
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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. -
The Muencheberg Soil Quality Rating (SQR)
The Muencheberg Soil Quality Rating (SQR) FIELD MANUAL FOR DETECTING AND ASSESSING PROPERTIES AND LIMITATIONS OF SOILS FOR CROPPING AND GRAZING Lothar Mueller, Uwe Schindler, Axel Behrendt, Frank Eulenstein & Ralf Dannowski Leibniz-Zentrum fuer Agrarlandschaftsforschung (ZALF), Muencheberg, Germany with contributions of Sandro L. Schlindwein, University of St. Catarina, Florianopolis, Brasil T. Graham Shepherd, Nutri-Link, Palmerston North, New Zealand Elena Smolentseva, Russian Academy of Sciences, Institute of Soil Science and Agrochemistry (ISSA), Novosibirsk, Russia Jutta Rogasik, Federal Agricultural Research Centre (FAL), Institute of Plant Nutrition and Soil Science, Braunschweig, Germany 1 Draft, Nov. 2007 The Muencheberg Soil Quality Rating (SQR) FIELD MANUAL FOR DETECTING AND ASSESSING PROPERTIES AND LIMITATIONS OF SOILS FOR CROPPING AND GRAZING Lothar Mueller, Uwe Schindler, Axel Behrendt, Frank Eulenstein & Ralf Dannowski Leibniz-Centre for Agricultural Landscape Research (ZALF) e. V., Muencheberg, Germany with contributions of Sandro L. Schlindwein, University of St. Catarina, Florianopolis, Brasil T. Graham Shepherd, Nutri-Link, Palmerston North, New Zealand Elena Smolentseva, Russian Academy of Sciences, Institute of Soil Science and Agrochemistry (ISSA), Novosibirsk, Russia Jutta Rogasik, Federal Agricultural Research Centre (FAL), Institute of Plant Nutrition and Soil Science, Braunschweig, Germany 2 TABLE OF CONTENTS PAGE 1. Objectives 4 2. Concept 5 3. Procedure and scoring tables 7 3.1. Field procedure 7 3.2. Scoring of basic indicators 10 3.2.0. What are basic indicators? 10 3.2.1. Soil substrate 12 3.2.2. Depth of A horizon or depth of humic soil 14 3.2.3. Topsoil structure 15 3.2.4. Subsoil compaction 17 3.2.5. Rooting depth and depth of biological activity 19 3.2.6. -
Progressive and Regressive Soil Evolution Phases in the Anthropocene
Progressive and regressive soil evolution phases in the Anthropocene Manon Bajard, Jérôme Poulenard, Pierre Sabatier, Anne-Lise Develle, Charline Giguet- Covex, Jeremy Jacob, Christian Crouzet, Fernand David, Cécile Pignol, Fabien Arnaud Highlights • Lake sediment archives are used to reconstruct past soil evolution. • Erosion is quantified and the sediment geochemistry is compared to current soils. • We observed phases of greater erosion rates than soil formation rates. • These negative soil balance phases are defined as regressive pedogenesis phases. • During the Middle Ages, the erosion of increasingly deep horizons rejuvenated pedogenesis. Abstract Soils have a substantial role in the environment because they provide several ecosystem services such as food supply or carbon storage. Agricultural practices can modify soil properties and soil evolution processes, hence threatening these services. These modifications are poorly studied, and the resilience/adaptation times of soils to disruptions are unknown. Here, we study the evolution of pedogenetic processes and soil evolution phases (progressive or regressive) in response to human-induced erosion from a 4000-year lake sediment sequence (Lake La Thuile, French Alps). Erosion in this small lake catchment in the montane area is quantified from the terrigenous sediments that were trapped in the lake and compared to the soil formation rate. To access this quantification, soil processes evolution are deciphered from soil and sediment geochemistry comparison. Over the last 4000 years, first impacts on soils are recorded at approximately 1600 yr cal. BP, with the erosion of surface horizons exceeding 10 t·km− 2·yr− 1. Increasingly deep horizons were eroded with erosion accentuation during the Higher Middle Ages (1400–850 yr cal. -
A New Soil Quality Index (SQI) for Assessing Forest Soil Health
Soil Vital Signs: A New Soil Quality Index (SQI) for Assessing Forest Soil Health Michael C. Amacher, Katherine P. O’Neill, and Charles H. Perry May 2007 United States Forest Service Rocky Mountain Research Paper Department Research Station RMRS-RP-65WWW of Agriculture Amacher, Michael C.; O’Neil, Katherine P.; Perry, Charles H. 2007. Soil vital signs: A new Soil Quality Index (SQI) for assessing forest soil health. Res. Pap. RMRS-RP-65WWW. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 12 p. Abstract __________________________________________ The Forest Inventory and Analysis (FIA) program measures a number of chemical and physical properties of soils to address specific questions about forest soil quality or health. We developed a new index of forest soil health, the soil quality index (SQI), that integrates 19 measured physical and chemical properties of forest soils into a single number that serves as the soil’s “vital sign” of overall soil quality. Regional and soil depth differences in SQI values due to differences in soil properties were observed. The SQI is a new tool for establishing baselines and detecting forest health trends. Keywords: forest soil health, Forest Inventory and Analysis, soil indicator database, soil quality index The Authors Michael C. Amacher is a research soil scientist with the Forest and Woodland Program Area at the Forestry Sciences Laboratory in Logan, UT. He holds a B.S. and a M.S. in chemistry and a Ph.D. in soil chemistry, all from The Pennsylvania State University. He joined the Rocky Mountain Research Station in 1989. -
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. -
Zinc Redistribution in a Soil Developed from Limestone During Pedogenesis C
Zinc Redistribution in a Soil Developed from Limestone During Pedogenesis C. Laveuf, Sophie Cornu, Denis Baize, Michel Hardy, Olivier Josière, Sylvain Drouin, Ary Bruand, F. Juillot To cite this version: C. Laveuf, Sophie Cornu, Denis Baize, Michel Hardy, Olivier Josière, et al.. Zinc Redistribution in a Soil Developed from Limestone During Pedogenesis. Pedosphere, Elsevier, 2009, 19 (3), pp.292-304. 10.1016/S1002-0160(09)60120-X. insu-00403877 HAL Id: insu-00403877 https://hal-insu.archives-ouvertes.fr/insu-00403877 Submitted on 21 Nov 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Zinc Redistribution in a Soil Developed from Limestone During Pedogenesis∗1 C. LAVEUF1,∗2,S.CORNU1, D. BAIZE1, M. HARDY1, O. JOSIERE1, S. DROUIN2, A. BRUAND2 and F. JUILLOT3 1INRA, UR0272 Science du Sol, Centre de recherche d’Orl´eans, 45075 Orl´eans cedex 2 (France) 2ISTO, UMR 6113, CNRS, Universit´ed’Orl´eans, 45071 Orl´eans cedex 2 (France) 3IMPMC, UMR CNRS 7590, Universit´e Paris 6 et 7, IPGC, 75252 Paris cedex 05 (France) (Received November 20, 2008; revised March 23, 2009) ABSTRACT The long-term redistribution of Zn in a naturally Zn-enriched soil during pedogenesis was quantified based on mass balance calculations. -
Soil Quality 1
START FARMINGSOIL QUALITY 1 introduction to soils Soil Quality Culman Steve ealthy soils yield healthy crops, But what is healthy soil and how do we Healthy, high-quality soil has: Hachieve it? • Good soil tilth • Sufficient depth Soil health is the foundation of productive farming practices. Fertile soil provides essential nutrients to • Sufficient, but not excessive, nutrient supply plants. Important physical characteristics of soil-like • Small population of plant pathogens and insect structures and aggregation allow water and air to pests infiltrate, roots to explore, and biota to thrive. Diverse • Good soil drainage and active biological communities help soil resist • Large population of beneficial organisms physical degradation and cycle nutrients at rates to • Low weed pressure meet plant needs. Soil health and soil quality are terms • No chemicals or toxins that may harm the crop used interchangeably to describe soils that are not • Resilience to degradation and unfavorable only fertile but also possess adequate physical and conditions biological properties to “sustain productivity, maintain —from Soil Health Training Manual environmental quality and promote plant and animal health” (Doron 1994). According to the (USDA) Natural Resource Remember, soil fertility is only one component Conservation Service, “Soil quality is how well soil does of soil quality. Fertile soils are able to provide the what we want it to do.” In order to grow our crops, we nutrients required for plant growth. These are the want the soil to hold water and nutrients like a sponge chemical components of soil. Some plants need certain where they are readily available for plant roots to take nutrients in large amounts, like nitrogen, phosphorus, them up, suppress pests and weeds that may attack and potassium, which are called macronutrients. -
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 Organic Carbon in a Changing World
Pedosphere 27(5): 789{791, 2017 doi:10.1016/S1002-0160(17)60489-2 ISSN 1002-0160/CN 32-1315/P ⃝c 2017 Soil Science Society of China Published by Elsevier B.V. and Science Press Preface Soil Organic Carbon in a Changing World JIA Zhongjun1, Yakov KUZYAKOV2;3, David MYROLD4 and James TIEDJE5 1State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008 (China). E-mail: [email protected] 2Agro-Technology Institute, RUDN University, Moscow 115419 (Russia). E-mail: [email protected] 3Institute of Physicochemical and Biological Problems in Soil Science, RAS, Pushchino 142290 (Russia) 4Department of Crop and Soil Science, Oregon State University, Corvallis OR 97331 (USA). E-mail: [email protected] 5Center for Microbial Ecology, Michigan State University, East Lansing MI 48824-1325 (USA). E-mail: [email protected] Soil contains more than three times as much carbon like compounds. By characterizing soil organic matter (C) as either the atmosphere or terrestrial vegetation. species using solid-state 13C cross polarization magic Soil organic C (SOC) is essentially derived from in- angle spinning (CPMAS) nuclear magnetic resonance puts of plant and animal residues, which are processed (NMR) (13C CPMAS-NMR) spectroscopy of humic by the microbiota (bacteria, archaea, protists, fungi substances and density-based fractions in a forest eco- and viruses) that dominates SOC transformation and system, Ranatunga et al. observed greater fractions of turnover in complex terrestrial environments. A tiny alkyl C, O-alkyl C, and carbohydrate functional gro- change in the SOC pool would have profound impacts ups in response to burning. -
The Soil Story Curricular Guide
THE SOIL STORY CURRICULUM Rebuilding Healthy Soil for Carbon Cycle Balance Earth’s Systems Photosynthesis Healthy Soil Lead Authors: Whitney Cohen | Education Director, Life Lab Food & Farming Carrie Strohl, PhD | Educational Consultant Taking Action Contributors: Annie Martin | Business Program, Kiss the Ground Arlae Castellanos | Sustainability Tracking Program Manager, Green Schools Alliance Craig Macmillan, PhD | Technical Program Manager, Vinyard Team Didi Pershouse | Director, Learning Resources Don Smith | Storytelling Team, Kiss the Ground Emily Harris, PhD | Research Scientist, BSCS Science Learning Finian Makepeace | Co-Founder, Kiss the Ground Ilana Lowe | 5th Grade Lead Science Teacher, Main Street Elementary Jessica Handy, RDN | Education Program, Kiss the Ground Karen Rodriguez | Former Operations Manager, Kiss the Ground A Middle School Lauren Tucker | Executive Director, Kiss the Ground Curriculum by Leslie Rogers | Director of Education, Atlas Organics Liz Henry | Senior Consultant, Crecer Strategies Markos Major | Director, Climate Action Now Paul Hawken | Author and Environmentalist Designer: Michelle Uyeda | Graphic Designer, Kiss the Ground + Thank you to our sponsors: About 1 THE SOIL STORY CURRICULAR GUIDE The Soil Story Curricular Guide was created through a collaborative partnership between Kiss the Ground and Life Lab. It serves as a supplemental material for teaching middle schoolers Next Generation Science Standards. Kiss the Ground (KTG) is a nonprofit with a mission to inspire participation in the regeneration of the planet, beginning with soil. The organization creates educational curriculum, campaigns, and media to raise awareness and empower individuals to purchase food that supports health soils and a balanced climate. KTG also works with farmers, educators, non government organizations, scientists, students, and policymakers to advocate for regenerative agriculture, raise funds to train farmers, and help brands and businesses to invest in healthy soils. -
Willamette Valley Soil Quality Card Guide to Accompany the Willamette Valley Soil Quality Card, EM 8711
Willamette Valley Soil Quality Card Guide To accompany the Willamette Valley Soil Quality Card, EM 8711 EM 8710-E Reprinted February 2009 Contents Introduction ......................................................................................................................................3 Suggested assessment calendar ........................................................................................................4 Soil-quality indicators 1. Does the soil have good structure and tilth? ..........................................................................5 2. Is the soil free of compacted layers? ......................................................................................7 3. Is the soil worked easily? .......................................................................................................9 4. Is the soil full of living organisms? ......................................................................................11 5. Are earthworms abundant in the soil? .................................................................................13 6. Is plant residue present and decomposing? ..........................................................................15 7. Do crops/weeds appear healthy and vigorous? ....................................................................17 8. Do plant roots grow well? ....................................................................................................19 9. Does water infiltrate quickly? ..............................................................................................21