Policy Brief Subsoil Compaction – a Threat to Sustainable Food Production and Soil Ecosystem Services
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Topic: Soil Classification
Programme: M.Sc.(Environmental Science) Course: Soil Science Semester: IV Code: MSESC4007E04 Topic: Soil Classification Prof. Umesh Kumar Singh Department of Environmental Science School of Earth, Environmental and Biological Sciences Central University of South Bihar, Gaya Note: These materials are only for classroom teaching purpose at Central University of South Bihar. All the data/figures/materials are taken from several research articles/e-books/text books including Wikipedia and other online resources. 1 • Pedology: The origin of the soil , its classification, and its description are examined in pedology (pedon-soil or earth in greek). Pedology is the study of the soil as a natural body and does not focus primarily on the soil’s immediate practical use. A pedologist studies, examines, and classifies soils as they occur in their natural environment. • Edaphology (concerned with the influence of soils on living things, particularly plants ) is the study of soil from the stand point of higher plants. Edaphologist considers the various properties of soil in relation to plant production. • Soil Profile: specific series of layers of soil called soil horizons from soil surface down to the unaltered parent material. 2 • By area Soil – can be small or few hectares. • Smallest representative unit – k.a. Pedon • Polypedon • Bordered by its side by the vertical section of soil …the soil profile. • Soil profile – characterize the pedon. So it defines the soil. • Horizon tell- soil properties- colour, texture, structure, permeability, drainage, bio-activity etc. • 6 groups of horizons k.a. master horizons. O,A,E,B,C &R. 3 Soil Sampling and Mapping Units 4 Typical soil profile 5 O • OM deposits (decomposed, partially decomposed) • Lie above mineral horizon • Histic epipedon (Histos Gr. -
Basic Soil Science W
Basic Soil Science W. Lee Daniels See http://pubs.ext.vt.edu/430/430-350/430-350_pdf.pdf for more information on basic soils! [email protected]; 540-231-7175 http://www.cses.vt.edu/revegetation/ Well weathered A Horizon -- Topsoil (red, clayey) soil from the Piedmont of Virginia. This soil has formed from B Horizon - Subsoil long term weathering of granite into soil like materials. C Horizon (deeper) Native Forest Soil Leaf litter and roots (> 5 T/Ac/year are “bio- processed” to form humus, which is the dark black material seen in this topsoil layer. In the process, nutrients and energy are released to plant uptake and the higher food chain. These are the “natural soil cycles” that we attempt to manage today. Soil Profiles Soil profiles are two-dimensional slices or exposures of soils like we can view from a road cut or a soil pit. Soil profiles reveal soil horizons, which are fundamental genetic layers, weathered into underlying parent materials, in response to leaching and organic matter decomposition. Fig. 1.12 -- Soils develop horizons due to the combined process of (1) organic matter deposition and decomposition and (2) illuviation of clays, oxides and other mobile compounds downward with the wetting front. In moist environments (e.g. Virginia) free salts (Cl and SO4 ) are leached completely out of the profile, but they accumulate in desert soils. Master Horizons O A • O horizon E • A horizon • E horizon B • B horizon • C horizon C • R horizon R Master Horizons • O horizon o predominantly organic matter (litter and humus) • A horizon o organic carbon accumulation, some removal of clay • E horizon o zone of maximum removal (loss of OC, Fe, Mn, Al, clay…) • B horizon o forms below O, A, and E horizons o zone of maximum accumulation (clay, Fe, Al, CaC03, salts…) o most developed part of subsoil (structure, texture, color) o < 50% rock structure or thin bedding from water deposition Master Horizons • C horizon o little or no pedogenic alteration o unconsolidated parent material or soft bedrock o < 50% soil structure • R horizon o hard, continuous bedrock A vs. -
Making Soils a Resource Through Microbial Labor
This is a repository copy of Nonhuman labor and the making of resources: making soils a resource through microbial labor. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/152381/ Version: Published Version Article: Krzywoszynska, A. orcid.org/0000-0002-8304-0440 (2020) Nonhuman labor and the making of resources: making soils a resource through microbial labor. Environmental Humanities, 12 (1). pp. 227-249. ISSN 2201-1919 https://doi.org/10.1215/22011919-8142319 Reuse This article is distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs (CC BY-NC-ND) licence. This licence only allows you to download this work and share it with others as long as you credit the authors, but you can’t change the article in any way or use it commercially. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ Nonhuman Labor and the Making of Resources Making Soils a Resource through Microbial Labor ANNA KRZYWOSZYNSKA Department of Geography, University of Sheffield, UK Abstract With soils increasingly seen as living ecosystems, the understanding of the rela- tionship between soils and agricultural labor is changing. A shift from working the soil to working with the soil is hoped to deliver a true ecological modernization of capitalist agri- culture, making the production of ever-growing yields and the maintenance of healthy eco- systems co-constitutive. -
National University of Engineering Ge111
NATIONAL UNIVERSITY OF ENGINEERING COLLEGE OF ENVIRONMENTAL ENGINEERING ENVIRONMENTAL ENGINEERING PROGRAM GE111 – EDAPHOLOGY I. GENERAL INFORMATION CODE : GE111 – Edaphology SEMESTER : 5 CREDITS : 03 HOURS PER WEEK : 04 (Theory – Practices – Laboratory) PREREQUISITES : GE102 – Geography CONDITION : Mandatory II. COURSE DESCRIPTION Concept and importance of edaphological soil and its interest for Engineering. Detailed knowledge of the components, physical and chemical properties, genesis, classification and principles of cartography, of natural soils and anthropogenic urban soils. Principle of soil evaluation, as a starting point in studies of environmental planning, territorial planning and environmental impact assessment. Finally, it is intended that students understand the importance of soil as a non-renewable resource and the degradations to which its inappropriate use leads; It is also intended to train in the corrective and rehabilitating measures of degraded soils. III. COURSE OUTCOMES At the end of the course the student will: Organizes data for proper analysis and interpretation and calculations (soil densities, physical chemical and biological properties). Explains and determines the genesis of the soil, the physical properties of the soil, geo reference, physiographic units. Understand and apply densities, to determine the consistency of the soil, the probability of resistance in an earthquake. Interpret and perform types of soil sampling to take to the laboratory to determine their physical, chemical, and biological characteristics. Build models to determine the degree of contamination, is determined by the parameters, using the LMOs, ECAs, In soils. IV. LEARNING UNITS 1. SOIL GENESIS / 4 HOURS Objective of soil science: Interest in Engineering. Genesis. Pedological and edaphological approach. Factors of soil formation. Climate action. Properties of the soil affected by the climate. -
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. -
Demonstration of Physical Separation/Leaching Methods for the Remediation of Heavy Metals Contaminated Soils at Small Arms Ranges
84 4 0 ,;*v , DEMONSTRATION OF PHYSICAL ftsJS1:3«*s SEPARATION/LEACHING METHODS FOR THE REMEDIATION OF HEAVY waBHi METALS CONTAMINATED SOILS AT SMALL ARMS RANGES m &r<&S?GtXl WBTMBUTION BTATEMEHTT Approved for pntfelie r*l«u«*f Dürtrlbattoa UnHmtaKl M£3 SEPTEMBER 1997 19980M 177 flTIC QUALITY DTS^EOTED S This Document Contains Missing Page/s That Are Unavailable In The Original Document AEC Form <t5, 1 Feb 93 replaces THAMA Form <t5 which is obsolete. Form Approved REPORT DOCUMENTATION PAGE OMB No. 0704-0188 Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden, to Weshington Headquarters Services, Directorate for Information Operations and Reports, 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302, and to the Office of Management and Budget, Paperwork Reduction Project (0704-0188), Washington, DC 20503. 1. AGENCY USE ONLY (Leave blank) REPORT DATE 3. REPORT TYPE AND DATES COVERED September 1997 Technology Demonstration, Nov 1995-Sep 1997 4. TITLE AND SUBTITLE 5. FUNDING NUMBERS Demonstration of Physical Separation/Leaching Methods for the Remediation of Heavy Metals Contaminated Soils at Small Arms Ranges 6. AUTHOR(S) BDM Engineering Services Company 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) 8. PERFORMING ORGANIZATION BDM Engineering Services Company REPORT NUMBER 1801 Randolph Road, S.E. -
Behavior of Pesticides in Soils and Water 1
Archival copy: for current recommendations see http://edis.ifas.ufl.edu or your local extension office. SL 40 Behavior of Pesticides in Soils and Water 1 P.S.C. Rao and A.G. Hornsby2 During the past twenty years, concern has arisen applied, and to show how this information can be as to the presence of pesticides in the environment used, along with other factors, to select the proper and the threat they pose to wildlife and mankind. pesticide. Certainly, pesticides have improved longevity and the quality of life, chiefly in the area of public health. PATHWAYS OF PESTICIDE LOSS The use of pesticides also constitutes an important There are basically two ways properly-applied aspect of modern agriculture. Florida's temperate to pesticides may reach surface and ground waters- subtropical climate favors growth of many harmful through runoff and leaching. Runoff is the physical insects, weeds and diseases, thus making this state transport of pollutants over the ground surface by particularly dependent on pesticides for economical rainwater which does not penetrate the soil. Leaching crop management. is a process whereby pollutants are flushed through Unfortunately, pesticides are poisons and can be the soil by rain or irrigation water as it moves particularly dangerous when misused. Fish-kills, downward. In many areas of Florida, soils are sandy reproductive failure in birds, and acute illnesses in and permeable and leaching is likely to be a more people have all been attributed to exposure to or serious problem than runoff. We now have ingestion of pesticides - usually as a result of technology to help estimate the potential misapplication or careless disposal of unused contamination of water from a given pesticide. -
Nitrate Leaching from Intensive Organic Farms to Groundwater
Open Access Hydrol. Earth Syst. Sci., 18, 333–341, 2014 Hydrology and www.hydrol-earth-syst-sci.net/18/333/2014/ doi:10.5194/hess-18-333-2014 Earth System © Author(s) 2014. CC Attribution 3.0 License. Sciences Nitrate leaching from intensive organic farms to groundwater O. Dahan1, A. Babad1, N. Lazarovitch2, E. E. Russak3, and D. Kurtzman4 1Department of Environmental Hydrology & Microbiology, Zuckerberg Institute for Water Research, Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Midreshet Ben-Gurion, Israel 2Wyler Department of Dryland Agriculture, French Associates Institute for Agriculture and Biotechnology of Drylands, Jacob Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Midreshet Ben-Gurion, Israel 3Geological and Environmental Sciences, Ben-Gurion University of the Negev, Beer Sheva, Israel 4Institute of Soil, Water and Environmental Sciences, Agricultural Research Organization, The Volcani Center, Bet Dagan, Israel Correspondence to: O. Dahan ([email protected]) Received: 18 June 2013 – Published in Hydrol. Earth Syst. Sci. Discuss.: 29 July 2013 Revised: 8 December 2013 – Accepted: 11 December 2013 – Published: 27 January 2014 Abstract. It is commonly presumed that organic agriculture productive agriculture must inherently include the leaching causes only minimal environmental pollution. In this study, of excess lower quality water below the root zone to the un- we measured the quality of percolating water in the vadose saturated zone and ultimately to the groundwater (Shani et zone, underlying both organic and conventional intensive al., 2007; Dudley et al., 2008). As such, maintaining the del- greenhouses. Our study was conducted in newly established icate balance between productive agriculture and groundwa- farms where the subsurface underlying the greenhouses has ter quality requires a broad perspective over different time been monitored continuously from their establishment. -
Assessment and Governance of Sustainable Soil Management
sustainability Editorial Assessment and Governance of Sustainable Soil Management Katharina Helming 1,2,*, Katrin Daedlow 3, Bernd Hansjürgens 4 and Thomas Koellner 5 1 Leibniz Centre for Agricultural Landscape Research (ZALF) e.V., 15374 Müncheberg, Germany 2 Eberswalde University for Sustainable Development, 16225 Eberswalde, Germany 3 Division Agriculture and Food Policy, Humboldt-Universität zu Berlin, 10099 Berlin, Germany; [email protected] 4 Helmholtz Centre for Environmental Research—UFZ, Permoserstraße 15, 04315 Leipzig, Germany; [email protected] 5 Professorship of Ecological Services, Faculty of Biology, Chemistry and Earth Sciences, BayCEER, University of Bayreuth, Universitaetsstr. 30, 95440 Bayreuth, Germany; [email protected] * Correspondence: [email protected]; Tel.: +49-(0)33432-82155 Received: 5 November 2018; Accepted: 7 November 2018; Published: 27 November 2018 Abstract: The globally increasing demand for food, fiber, and bio-based products interferes with the ability of arable soils to perform their multiple functions and support sustainable development. Sustainable soil management under high production conditions means that soil functions contribute to ecosystem services and biodiversity, natural and economic resources are utilized efficiently, farming remains profitable, and production conditions adhere to ethical and health standards. Research in support of sustainable soil management requires an interdisciplinary approach to three interconnected challenges: (i) understanding the impacts of soil management on soil processes and soil functions; (ii) assessing the sustainability impacts of soil management, taking into account the heterogeneity of geophysical and socioeconomic conditions; and (iii) having a systemic understanding of the driving forces and constraints of farmers’ decision-making on soil management and how governance instruments may, interacting with other driving forces, steer sustainable soil management. -
Global Soil Governance: Status and Future Perspectives
Global soil governance: Status and future perspectives Wednesday 25th August 2021 (11:30 - 13:00 CEST) Virtual format (Zoom) Soils are essential to life on Earth. It is a key provider of ecosystem services, such as regulating climate change and water flows, providing clean water, food, feed, and fuel, supporting human infrastructure, and buffering and filtering contaminants. Their protection and sustainable management is of the utmost importance to ensure the future of food systems and sustainable development. However, due to the crosscutting nature of soil resources and the different stakeholders that benefit from them, soil governance is generally addressed in a dispersed manner in current national and international legal frameworks, ranging from agricultural legislation to regulations on mining, urban development and environmental protection. Soil has commonly been considered in a scattered way across the European and international legislation, as a tool to achieve secondary goals in related environmental policies. Currently, EU and international Environmental Law are still apprehending soil and related environmental concerns in a sectoral and compartmentalized manner rather than a set of interconnected problems. As a result, both international and European environmental governance are still lacking a soil specific instrument along with soil specific policies incorporated within the existing and relevant legislation, while soils play a central role in achieving the many set environmental goals. Approximately, ten years ago soils were not in the global agenda as soils were usually taken by granted. Today, however, after advocacy and awareness raising efforts from different initiatives (Global Soil Partnership, EU Soil Thematic Strategy, Global Soil Biodiversity Initiative, Global Soil Week, etc.) soils are in the decision making agenda. -
Leaching of Heavy Metals in Soils Conditioned with Biosolids from Sewage Sludge
Floresta e Ambiente 2019; 26(Spec No 1): e20180399 https://doi.org/10.1590/2179-8087.039918 ISSN 2179-8087 (online) Original Article Silviculture Leaching of Heavy Metals in Soils Conditioned with Biosolids from Sewage Sludge Thaís Campos1 , Guilherme Chaer2, Paulo dos Santos Leles1, Marcelo Silva1, Felipe Santos1 1Universidade Federal Rural do Rio de Janeiro, Seropédica/RJ, Brasil 2Empresa Brasileira de Pesquisa Agropecuária, Seropédica/RJ, Brasil ABSTRACT A promising use of biosolids is as organic fertilizer in agricultural and forestry activities. However, its composition might contain several pollutants, especially heavy metals, which may result in an increase in the concentrations of these elements in the soil and the risk of groundwater contamination. This study aimed to determine the leaching levels of ions in a Ferralsol (clayey texture) and in a Planosol (sandy texture). The experiment was conducted in a greenhouse at Embrapa Agrobiologia, Seropédica, Rio de Janeiro state. Soils were packed in PVC columns and received 2 L/column of biosolids. The concentrations of heavy metals present in the biosolids composition were below the limits established by the legislation (CONAMA 375). In addition, the performed simulations showed the absence of contamination risk of soil or groundwater and surface water, according to the limits allowed by CONAMA 375. However, it should be emphasized the potential of nitrate leaching. Keywords: contamination risk, chemical elements percolation, test with columns, risk analysis. Creative Commons License. All the contents of this journal, except where otherwise noted, is licensed under a Creative Commons Attribution License. 2/10 Campos T, Chaer G, Leles PS, Silva M, Santos F Floresta e Ambiente 2019; 26(Spec No 1): e20180399 1. -
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