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Formación De Neologismos En Ciencia Del Suelo
Formación de neologismos en Ciencia del Suelo Formation of Soil Science neologisms Formação de neologismos em Ciência do Solo AUTORES Received: 01.06.2012 Revised: 19.06.2012 Accepted: 20.06.2012 @ 1 Porta J. [email protected]. cat RESUMEN 2 Desde el Congreso de Roma de 1924, en el que la comunidad cientí!ca decidió utilizar la expresión Villanueva D. Soil Science en lugar de Pedology o Edaphology, no se ha llegado a establecer criterios para la formación en español de neologismos referentes! "# al estudio del suelo."$%#& En inglés, los nuevos términos se forman dando prioridad a la raíz griega ! " frente a la raíz # . Este criterio, que se ha consolidado !!"#" con el uso, no tiene en cuenta que en griego el término se"$%#& re!ere al suelo sobre el que se anda y @ Corresponding no al suelo en el que crecen las plantas, expresado por el término # . En el presente trabajo, desde Author una perspectiva etimológica, semántica y de pragmática lingüística, se proponen criterios para la 1 Sociedad Española formación de neologismos en español o al establecer equivalencias en español de voces introducidas de la Ciencia del en inglés. El análisis se basa en voces de autoridad; en elementos etimológicos; en aspectos de am- Suelo. Universitat de Lleida. Rovira Roure bigüedad fonética y ortográ!ca; en la revisión de equivalencias entre términos similares en español, 191, 25198 Lleida, inglés y francés; en el ámbito universitario; en la denominación de las sociedades y revistas cientí!cas; España. y en aspectos de buen gusto idiomático en determinados ámbitos geográ!cos del español. -
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. -
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. -
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. -
Soils and Soil-Forming Material Technical Information Note 04 /2017 30Th November 2017
Soils and Soil-forming Material Technical Information Note 04 /2017 30th November 2017 Contents 1. Introduction to Soils ........................................................................................................................ 2 2. Components and Properties of Soil ................................................................................................ 7 3. Describing and Categorising soils .................................................................................................. 29 4. Policy, Regulation and Roles ......................................................................................................... 34 5. Soil Surveys, Handling and Management ..................................................................................... 40 6. Recommended Soil Specifications ................................................................................................ 42 7. References .................................................................................................................................... 52 “Upon this handful of soil our survival depends. Husband it and it will grow our food, our fuel, and our shelter and surround us with beauty. Abuse it and the soil will collapse and die, taking humanity with it.” From Vedas Sanskrit Scripture – circa 1500 BC The aim of this Technical Information Note is to assist Landscape Professionals (primarily landscape architects) when considering matters in relation to soils and soil-forming material. Soil is an essential requirement for providing -
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. -
Soil Classification Following the US Taxonomy: an Indian Commentary
See discussions, stats, and author profiles for this publication at: http://www.researchgate.net/publication/280114947 Soil Classification Following the US Taxonomy: An Indian Commentary ARTICLE · JULY 2015 DOI: 10.2136/sh14-08-0011 DOWNLOADS VIEWS 21 27 1 AUTHOR: Tapas Bhattacharyya International Crops Research Institute for Se… 110 PUBLICATIONS 848 CITATIONS SEE PROFILE Available from: Tapas Bhattacharyya Retrieved on: 19 August 2015 provided by ICRISAT Open Access Repository View metadata, citation and similar papers at core.ac.uk CORE brought to you by Published July 17, 2015 Review Soil Classification Following the US Taxonomy: An Indian Commentary T. Bhattacharyya,* P. Chandran, S.K. Ray, and D.K. Pal More than 50 yr ago US soil taxonomy was adopted in India. Since then many researchers have contributed their thoughts to enrich the soil taxonomy. The National Bureau of Soil Survey and Land Use Planning (NBSS & LUP) (Indian Council of Agricultural Research) as a premier soil survey institute has been consistently using benchmark soil series to understand the rationale of the soil taxonomy, keeping in view the soil genesis from different rock systems under various physiographic locations in tropical India. The present review is a humble effort to present this information. ne of the fundamental requirements of any natural science minerals, higher categories of soil classification were conceptu- Ois to classify the proposed bodies or the objects stud- alized (Duchaufour, 1968). The concept of genetic profiles was ied (Joel, 1926). Soils do not exist as discrete objects like plants used in early and current Russian soil classification schemes and animals but occur in nature as a complex and dynamic (Gerasimov, 1975; Gorajichkin et al., 2003). -
Basic Soil Properties
Soil: Definition and Basic Properties Allen Hayes, Soil Scientist, NCDA, Division of Soil & Water Conservation Soil Defined: USDA-Natural Resources Conservation Service ▪ “Soil…is a natural body comprised of solids (minerals and organic matter), liquid, and gases that occurs on the land surface, occupies space, and is characterized by one or both of the following: ▪ horizons, or layers, that are distinguishable from the initial material as a result of additions, losses, transfers, and transformations of energy and matter ▪ or the ability to support rooted plants in a natural environment.” (Soil Survey Staff, 1999) Soil Defined: USDA-Natural Resources Conservation Service ▪ “…a natural body…” ▪ Forms naturally in terrestrial ecosystems ▪ Not man-made Soil Defined: USDA-Natural Resources Conservation Service ▪ “comprised of solids (minerals and organic matter), liquid, and gases…” Soil Defined: USDA-Natural Resources Conservation Service ▪ “…occurs on the land surface,…” ▪ “…occupies space…” ▪ Has “horizons, or layers, that are distinguishable from the initial material as a result of additions, losses, transfers, and transformations of energy or matter, or ▪ Has “the ability to support rooted plants in a natural environment” Soil Formation (briefly) ▪ Soil vs. Dirt ▪ Soil forming factors ▪ Parent material, climate, biology, relief and time ▪ North Carolina has about 400 soil series ▪ United States has about 20,000 soil series Soil Defined ▪ “Nature has endowed the Earth with glorious wonders and vast resources that man may use for his own ends. Regardless of our tastes or our way of living, there are none that present more variations to tax our imagination than the soil, and certainly none so important to our ancestors, to ourselves, and to our children.” -Dr. -
Role of Arthropods in Maintaining Soil Fertility
Agriculture 2013, 3, 629-659; doi:10.3390/agriculture3040629 OPEN ACCESS agriculture ISSN 2077-0472 www.mdpi.com/journal/agriculture Review Role of Arthropods in Maintaining Soil Fertility Thomas W. Culliney Plant Epidemiology and Risk Analysis Laboratory, Plant Protection and Quarantine, Center for Plant Health Science and Technology, USDA-APHIS, 1730 Varsity Drive, Suite 300, Raleigh, NC 27606, USA; E-Mail: [email protected]; Tel.: +1-919-855-7506; Fax: +1-919-855-7595 Received: 6 August 2013; in revised form: 31 August 2013 / Accepted: 3 September 2013 / Published: 25 September 2013 Abstract: In terms of species richness, arthropods may represent as much as 85% of the soil fauna. They comprise a large proportion of the meso- and macrofauna of the soil. Within the litter/soil system, five groups are chiefly represented: Isopoda, Myriapoda, Insecta, Acari, and Collembola, the latter two being by far the most abundant and diverse. Arthropods function on two of the three broad levels of organization of the soil food web: they are plant litter transformers or ecosystem engineers. Litter transformers fragment, or comminute, and humidify ingested plant debris, which is deposited in feces for further decomposition by micro-organisms, and foster the growth and dispersal of microbial populations. Large quantities of annual litter input may be processed (e.g., up to 60% by termites). The comminuted plant matter in feces presents an increased surface area to attack by micro-organisms, which, through the process of mineralization, convert its organic nutrients into simpler, inorganic compounds available to plants. Ecosystem engineers alter soil structure, mineral and organic matter composition, and hydrology.