How Valuable Is the Soil Resource? How Can We Measure It? How Can We Communicate Its Value to the Public? ISRIC Spring School 2019
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Soil Quality: Why and How?
Geoderma 114 (2003) 145–156 www.elsevier.com/locate/geoderma Soil quality: why and how? Douglas L. Karlena,*, Craig A. Ditzlerb, Susan S. Andrewsa a USDA-ARS National Soil Tilth Laboratory, 2150 Pammel Drive, Ames, IA 50011-4420, USA b National Soil Survey Center, 100 Centennial Mall North, Lincoln, NE 68508-3866, USA Abstract The soil quality concept evolved throughout the 1990s in response to increased global emphasis on sustainable land use and with a holistic focus emphasizing that sustainable soil management requires more than soil erosion control. The concept includes two areas of emphasis—education and assessment—both based soundly on principles of soil science. Soil quality test kits, farmer-based scorecards, visual assessment procedures, fact sheets, and video presentations were developed as educational materials because many people have no basis to recognize, understand or appreciate the complexity of soil resources. Assessment tools for indexing soil quality at various scales were pursued to show the multiple functions (e.g. nutrient and water cycling, filtering and buffering of contaminants, decomposition of crop residues and other organic matter sources, and recycling of essential plant nutrients) that soils provide as the foundation for sustainable land management. Worldwide research and technology transfer efforts have increased awareness that soil resources have both inherent characteristics determined by their basic soil formation factors and dynamic characteristics influenced by human decisions and management practices. Soil quality assessment and education are intended to provide a better understanding and awareness that soil resources are truly living bodies with biological, chemical, and physical properties and processes performing essential ecosystem services. -
Poster Presentation Schedule
20WCSS_Poster Schedule(vol.6) Abstract Date Time Code-N Session Name Country Affiliation Final Type Abstract Title No Folk Soil Knowledge for Soil Myriel Milicevic and June 9(Mon) All day Art Poster Taxonomy and Assessment-art Ruttikorn Vuttikorn Folk Soil Knowledge for Soil Autonomous University of CHARACTERIZATION AND CLASSIFICATION OF SOILS IN MEXICALI June 9(Mon) 15:30~16:20 P1-1 AF2388 Monica Aviles Mexico Poster Taxonomy and Assessment Baja California VALLEY, BAJA CALIFORNIA, MEXICO Folk Soil Knowledge for Soil UNIVERSITY OF CUIABA - Relationship between phytophysiognomy and classes of wetland soil June 9(Mon) 15:30~16:20 P1-2 AF2892 Leo Adriano Chig Brazil Poster Taxonomy and Assessment UNIC/INAU - NATIONAL of northern Pantanal Mato Grosso - Brazil Folk Soil Knowledge for Soil Luiz Felipe Moreira USE OF SIG TOOLS IN THE TREATMENT OF DATA AND STUDY OF June 9(Mon) 15:30~16:20 P1-3 AF2934 Brazil Universidade de Brasilia Poster Taxonomy and Assessment Cassol THE RELATIONSHIP BETWEEN SOIL, GEOLOGY AND Folk Soil Knowledge for Soil Universidad Michoacana de FARMER'S KNOWLEDGE OF LAND AND CLASSES OF CORN OF June 9(Mon) 15:30~16:20 P1-4 AF2977 Maria Alcala Mexico Poster Taxonomy and Assessment San Nicolas de Hidalgo MICHOACAN, MEXICO Folk Soil Knowledge for Soil Technological Educational June 9(Mon) 15:30~16:20 P1-5 AF2979 Pantelis E. Barouchas Greece Poster Soil mass balance for an Alfisol in Greece Taxonomy and Assessment Institute of Western Greece Critical Issues of Radionuclide Center for Land Use June 9(Mon) All day Art Poster Behavior -
Pedometric Mapping of Key Topsoil and Subsoil Attributes Using Proximal and Remote Sensing in Midwest Brazil
UNIVERSIDADE DE BRASÍLIA FACULDADE DE AGRONOMIA E MEDICINA VETERINÁRIA PROGRAMA DE PÓS-GRADUAÇÃO EM AGRONOMIA PEDOMETRIC MAPPING OF KEY TOPSOIL AND SUBSOIL ATTRIBUTES USING PROXIMAL AND REMOTE SENSING IN MIDWEST BRAZIL RAÚL ROBERTO POPPIEL TESE DE DOUTORADO EM AGRONOMIA BRASÍLIA/DF MARÇO/2020 UNIVERSIDADE DE BRASÍLIA FACULDADE DE AGRONOMIA E MEDICINA VETERINÁRIA PROGRAMA DE PÓS-GRADUAÇÃO EM AGRONOMIA PEDOMETRIC MAPPING OF KEY TOPSOIL AND SUBSOIL ATTRIBUTES USING PROXIMAL AND REMOTE SENSING IN MIDWEST BRAZIL RAÚL ROBERTO POPPIEL ORIENTADOR: Profa. Dra. MARILUSA PINTO COELHO LACERDA CO-ORIENTADOR: Prof. Titular JOSÉ ALEXANDRE MELO DEMATTÊ TESE DE DOUTORADO EM AGRONOMIA BRASÍLIA/DF MARÇO/2020 ii iii REFERÊNCIA BIBLIOGRÁFICA POPPIEL, R. R. Pedometric mapping of key topsoil and subsoil attributes using proximal and remote sensing in Midwest Brazil. Faculdade de Agronomia e Medicina Veterinária, Universidade de Brasília- Brasília, 2019; 105p. (Tese de Doutorado em Agronomia). CESSÃO DE DIREITOS NOME DO AUTOR: Raúl Roberto Poppiel TÍTULO DA TESE DE DOUTORADO: Pedometric mapping of key topsoil and subsoil attributes using proximal and remote sensing in Midwest Brazil. GRAU: Doutor ANO: 2020 É concedida à Universidade de Brasília permissão para reproduzir cópias desta tese de doutorado e para emprestar e vender tais cópias somente para propósitos acadêmicos e científicos. O autor reserva outros direitos de publicação e nenhuma parte desta tese de doutorado pode ser reproduzida sem autorização do autor. ________________________________________________ Raúl Roberto Poppiel CPF: 703.559.901-05 Email: [email protected] Poppiel, Raúl Roberto Pedometric mapping of key topsoil and subsoil attributes using proximal and remote sensing in Midwest Brazil/ Raúl Roberto Poppiel. -- Brasília, 2020. -
Impact of Heathland Restoration and Re-Creation Techniques on Soil Characteristics and the Historical Environment
Natural England Research Report NERR010 Impact of heathland restoration and re-creation techniques on soil characteristics and the historical environment www.naturalengland.org.uk Natural England Research Report NERR010 Impact of heathland restoration and re-creation techniques on soil characteristics and the historical environment Hawley, G.1, Anderson, P. 1, Gash, M. 1, Smith, P. 1, Higham, N. 2, Alonso, I. 3, Ede, J.3 & Holloway, J.3 1 Independent consultant, 2 University of Manchester and 3 Natural England Published on 28 March 2008 The views in this report are those of the authors and do not necessarily represent those of Natural England. You may reproduce as many individual copies of this report as you like, provided such copies stipulate that copyright remains with Natural England, 1 East Parade, Sheffield, S1 2ET ISSN 1754-1956 © Copyright Natural England 2008 Project details This report results from research commissioned by Natural England in order to provide information on the impact of heathland restoration and re-creation activities on the soils and archaeology. The work was undertaken under Natural England contract FST20-84-010 by the following team: Penny Anderson (Managing Director Penny Anderson Associates Ltd (PAA); Gerard Hawley (Senior Soil Scientist, PAA); Mark Gash (Ecologist, PAA); Phil Smith (Senior Ecologist, PAA) and Nick Higham (Professor of Early Medieval and Landscape History, University of Manchester). Isabel Alonso (Heathland Ecologist, Natural England), Joy Ede (Historic Environment Advisor, Natural England) and Julie Holloway (Senior Soil Specialist, Natural England) provided contacts, information, references and edited the report. A summary of the findings covered by this report, as well as Natural England's views on this research, can be found within Natural England Research Information Note RIN010: Impact of heathland restoration and re-creation techniques on soil characteristics and the historical environment. -
Agricultural Resources Assessment
2017 Agricultural Resources Assessment CHINO PARCEL DELIVERY FACILITY PROJECT PREPARED BY: T&B PLANNING, INC. Agricultural Resources Assessment for the Chino Parcel Delivery Facility Project City of Chino, California Prepared For: Scannell Properties 800 East 96th Street, Suite 175 Indianapolis, IN 46077 Prepared By: T&B Planning, Inc. 17542 East 17th Street, Suite 100 Tustin, CA 92780 October 4, 2017 Abstract The Chino Parcel Delivery Facility Project site is located in the City of Chino, San Bernardino County, California. The Project proposes the construction of industrial land uses on a 74.4-acre property, and is subject to review under the California Environmental Quality Act (CEQA). In this report, the California Land Evaluation and Site Assessment (LESA) Model is used as an evaluation tool to determine if the subject property qualifies as an important agricultural resource. Based on the methodology established by the California LESA Model, this report concludes that the Project site is an important agricultural resource. Agricultural Resources Assessment Chino Parcel Delivery Facility City of Chino TABLE OF CONTENTS Section Number/Title Page 1.0 Introduction ...................................................................................................................................................................1 1.1 Document Purpose .................................................................................................................................................1 1.2 Project Location .......................................................................................................................................................1 -
Indicators of Agricultural Soil Genesis Under Varying Conditions of Land Use, Steppe Crimea
Geoderma 239–240 (2015) 304–316 Contents lists available at ScienceDirect Geoderma journal homepage: www.elsevier.com/locate/geoderma Indicators of agricultural soil genesis under varying conditions of land use, Steppe Crimea Fedor Lisetskii a, Vladimir F. Stolba b,⁎,OlgaMarininа a a Belgorod State National Research University, 308015, Belgorod, ul. Pobedy 85, Russia b Aarhus University, Nordre Ringgade 1, DK-8000 Aarhus C, Denmark article info abstract Article history: This study investigates the effects of agricultural exploitation of soils of the north-western Crimea, the active and Received 12 May 2014 large-scale cultivation of which began with the Greek colonization of the area. In order to compare soils using a Received in revised form 29 October 2014 wide spectrum of physical and chemical properties, the studied objects (virgin land, post-antique idle land, con- Accepted 8 November 2014 tinually plowed land, modern-day plowed land, idle land of the modern era) have been grouped into a Available online 20 November 2014 chronosequence. This makes it possible to apply the method of factor sequences of agrogenic transformations Keywords: in soils, which takes into account different periods of human activities. The other factors involved in soil forma- Soil formation tion are considered to be relatively invariable. From the mass of physiochemical properties of these soils that Idle lands have endured long-term agricultural stress, the most informative indicators of agrogenesis have been identified. Agrogenic soils The authors propose a procedure for calculating an integral agrophysical soil indicator based on five parameters Chronosequence that can be used to determine the soil structure and cloddiness as well as water-stability, the amount of water- Agrogenic indicators stable aggregates and their mean mass-weighted diameter. -
Economic Valuation of Soil Functions: Phase 1
Economic Valuation of Soil Functions Phase 1: Literature Review and Method Development Prepared for: Defra Prepared by: David Harris, ADAS Boxworth, Battlegate Road, Boxworth, Cambridge, CB3 8NN Dr. Bob Crabtree, CJC Consulting, Oxford John King, ADAS Boxworth Paul Newell-Price, ADAS Gleadthorpe Date: July 2006 Copyright The proposed approach and methodology is protected by copyright and no part of this document may be copied or disclosed to any third party, either before or after the contract is awarded, without the written consent of ADAS. 0936648 Economic Valuation of Soil Functions Phase 1: Literature Review and Method Development Glossary of Terms ALC Agricultural Land Classification AONB Area of Outstanding Natural Beauty BMP Best Management Practice generally defined by being within the Codes of Good Agricultural Practice for Air, Water and Soil, COGAP (Defra) Brickfield series An imperfectly drained soil with a fine loamy texture CAP Common Agricultural Policy Clifton series An imperfectly drained, medium to coarse-textured soil with a perched water table Cu Copper CV Contingent valuation DE Direct energy used in fuel for field operations Defra Department for Environment, Food and Rural Affairs DoE Department of the Environment (now part of Defra and distinct from the Environment Agency) Dunkeswick series A poorly drained soil with a fine loamy topsoil, and a clay subsoil beginning at between 40 and 80 cm depth ELS Entry Level Scheme of Environmental Stewardship Scheme ESA Environmentally Sensitive Area FIOs Faecal indicator organisms -
Literature Review on Soil Health and Conservation
AUG 30, 2017 Methods to Assess Co-Benefits of California Climate Investments Soil Health and Conservation Center for Resource Efficient Communities, UC-Berkeley Agreement #15TTD002, Project Order #1, Task 2 Literature Review Primary Author: Bill Eisenstein and Sara Litke I. Background Under California’s Cap-and-Trade program, the State’s portion of the proceeds from Cap-and-Trade auctions is deposited in the Greenhouse Gas Reduction Fund (GGRF). The Legislature and Governor enact budget appropriations from the GGRF for State agencies to invest in projects that help achieve the State’s climate goals. These investments are collectively called California Climate Investments (CCI). Senate Bill 862 requires the California Air Resources Board (CARB) to develop guidance on reporting and quantification methods for all State agencies that receive appropriations from the GGRF. Guidance includes developing quantification methodologies for greenhouse gas (GHG) emission reductions and other social, economic, and environmental benefits of projects, referred to as “co-benefits.” This document is one of a series that reviews the available methodologies for assessing selected co-benefits for CCI projects at two phases: estimating potential project-level co-benefits prior to project implementation (i.e., forecasting of co-benefits), and measuring actual co-benefits after projects have been implemented (i.e. tracking of co-benefits). The assessment methodology at each of these phases may be either quantitative or qualitative. As with CARB’s existing GHG -
California Revised Storie Index (CA)—Tehama County, California (Old Russell Farm Package) 122° 22' 15'' W 122° 21' 13'' W
California Revised Storie Index (CA)—Tehama County, California (Old Russell Farm Package) 122° 22' 15'' W 15'' 22' 122° W 13'' 21' 122° 553700 553800 553900 554000 554100 554200 554300 554400 554500 554600 554700 554800 554900 555000 40° 6' 32'' N 40° 6' 32'' N 4440000 4440000 4439900 4439900 4439800 4439800 4439700 4439700 4439600 4439600 4439500 4439500 4439400 4439400 4439300 4439300 4439200 4439200 Soil Map may not be valid at this scale. 40° 6' 1'' N 4439100 40° 6' 1'' N 4439100 553700 553800 553900 554000 554100 554200 554300 554400 554500 554600 554700 554800 554900 555000 Map Scale: 1:6,730 if printed on A landscape (11" x 8.5") sheet. Meters N 0 50 100 200 300 122° 22' 15'' W 15'' 22' 122° W 13'' 21' 122° Feet 0 300 600 1200 1800 Map projection: Web Mercator Corner coordinates: WGS84 Edge tics: UTM Zone 10N WGS84 Natural Resources Web Soil Survey 3/2/2018 Conservation Service National Cooperative Soil Survey Page 1 of 4 California Revised Storie Index (CA)—Tehama County, California (Old Russell Farm Package) MAP LEGEND MAP INFORMATION Area of Interest (AOI) Grade 5 - Very Poor The soil surveys that comprise your AOI were mapped at Area of Interest (AOI) 1:20,000. Grade 6 - Nonagricultural Soils Not rated Warning: Soil Map may not be valid at this scale. Soil Rating Polygons Enlargement of maps beyond the scale of mapping can cause Grade 1 - Excellent Not rated or not available misunderstanding of the detail of mapping and accuracy of soil Grade 2 - Good Water Features line placement. -
For Peer Review Only
ORE Open Research Exeter TITLE Comparison of methods for evaluating the suitability of Vertisols for Gossypium hirsutum (Bt cotton) in two contrasting agro-ecological regions AUTHORS Karthikeyan, , K; Vasu, , D; Tiwary, , P; et al. JOURNAL Archives of Agronomy and Soil Science DEPOSITED IN ORE 20 November 2018 This version available at http://hdl.handle.net/10871/34827 COPYRIGHT AND REUSE Open Research Exeter makes this work available in accordance with publisher policies. A NOTE ON VERSIONS The version presented here may differ from the published version. If citing, you are advised to consult the published version for pagination, volume/issue and date of publication Archives of Agronomy and Soil Science For Peer Review Only Comparison of methods for evaluating the suitability of Vertisols for Gossypium hirsutum (Bt cotton) in two contrasting agro-ecological regions Journal: Archives of Agronomy and Soil Science Manuscript ID GAGS-2018-0638.R2 Manuscript Type: Original Article Agro-ecological regions, Land suitability evaluation, Soil quality index, Keywords: Vertisols, Principal component analysis URL: http://mc.manuscriptcentral.com/GAGS E-mail: [email protected] Page 1 of 34 Archives of Agronomy and Soil Science Comparison of methods for evaluating the suitability of Vertisols for Gossypium hirsutum (Bt cotton) in two contrasting agro-ecological regions Karunakaran Karthikeyana, Duraisamy Vasua, Pramod Tiwarya, Andrew M. Cunliffeb, Padikkal Chandrana, Sankar Mariappanc, Surendra K Singhd For Peer Review Only aDivision of Soil -
Introduction to Soils and Pedology
Introduction to Soils and Pedology • Coined in mid 19th Century by French scientist • DidDerived from Gree k: pedon=ground, log ia = discour se • “The study, in situ, of the biogeochemical processes that form and dbdistribute soil”ls” • An observational, vs. an experimental, science - nature is the laboratory • Origins attributed to two centers: Russia (Dokuchaev) and Berkeley (Hilgard) Definition of Soils • Many definitions •Soil is part of a continuum of materials at earth’ surface –Soil vs. non-soil at bottom and top –Different soils laterally •Need to divide continuum into systems, or discrete seggyments, for study •Hans Jenny (1930’s) conceptualized soils as physical systems amenable and susceptible to physical variables (STATE FACTORS) ElEcological functions of soil • Supports plant growth • Recycles nutrients and waste • Controls the flow and purity of water • Provid es habit a t for soil organisms • Functions as a building material/base Role of Pedology in Scientific and Societal Problems •Carbon and nitrogen cycles •Are soils part of an unidentified sink for CO2? •What is the effect of agricultural on soil C (and atm CO2)? •Will soils store excess N from human activity? •Chemi st ry of natural waters •How do soils release elements with time and space? •Earth history •‘Paleosols’ and evolution of land plants, atmospheric CO2 records, human evolution •Soils and archaeology •Biodiversity •Is soil diversity analogous to, and complementary to, biodiversity •Microorganisms in soil represent unknown biodiversity resources Soils as a -
Soils As Pacemakers and Limiters of Global Silicate Weathering
Originally published as: Dixon, J. L., von Blanckenburg, F. (2012): Soils as pacemakers and limiters of global silicate weathering. ‐ Comptes Rendus Geoscience, 344, 11 ‐ 12, 597‐609 DOI: 10.1016/j.crte.2012.10.012 Soils as pacemakers and limiters of global silicate weathering Jean L. Dixon1,2 and Friedhelm von Blanckenburg1 1 Helmholtz Centre Potsdam, GFZ German Centre for Geosciences, Telegraphenberg, 14473 Potsdam, Germany 2 Department of Geography, University of California, Santa Barbara, CA 93106, USA Keywords: chemical weathering, soil production, speed limits, erosion, regolith, river fluxes Comptes rendus – Geosciences 344, 597-609, 2012 Abstract The weathering and erosion processes that produce and destroy regolith are widely recognized to be positively correlated across diverse landscapes. However, conceptual and numerical models predict some limits to this relationship that remain largely untested. Using new global data compilations of soil production and weathering rates from cosmogenic nuclides and silicate weathering fluxes from global rivers, we show that the weathering- erosion relationship is capped by certain ‘speed limits’. We estimate a soil production speed limit of between 320 to 450 t km-2 y-1 and the associated weathering rate speed limit of roughly 150 t km-2 y-1. These limits appear to be valid for a range of lithologies, and also extend to mountain belts, where soil cover is not continuous and erosion rates outpace soil production. We argue that the presence of soil and regolith is a requirement for high weathering fluxes from a landscape, and that rapidly eroding, active mountain belts are not the most efficient sites for weathering.