Soil Quality: Why and How?
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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. -
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. -
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 -
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. -
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). -
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 -
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. -
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 -
Lead and Arsenic Contamination by a Smelter Plant Located in the Mexico-USA Boundary Area
Lead and Arsenic Contamination by a Smelter Plant Located in the Mexico-USA Boundary Area F.E. Porras Hernández 1, M.T. Alarcón Herrera 2, A. Granados Olivas 1, and I.R. Martin Domínguez 2. 1Civil and Environmental Engineering Department, Autonomous University of Ciudad Juarez (UACJ), Autonomous University of Ciudad Juarez, Ave of Charro 450 North Ciudad Juárez, México 2Environment and Energy Department, Advanced Materials Research Center (CIMAV), Chihuahua, Mexico Key Words: contamination, soil, arsenic, lead, smelting Summary The ASARCO smelter, located in El Paso del Norte border region between Chihuahua (Mexico) and Texas and New Mexico (United States of America), was working for approximately 100 years, mainly in the casting of metals. The direct impacts to soil and water due to the emissions coming out from the smelter are considered in this study. It is assumed that during the period of its operation, the plant continuously released lead, cadmium and arsenic to the atmosphere. This research is limited to an area enclosed in 5 km-perimeter circle, Ciudad Juarez included. A geospatial analysis, using a digital-thematic cartography, is presented. The types of soil in the area of interest included variables such as: geology, topography, surface hydrology and regional climate. Taking the main chimney of the smelter as a center, the study area is enclosed into concentric circles with radii that range from 500 m up to 5000 m. Within this area, 160 soil samples of 0.60 m depth and 160 soil samples of 0.05 m were collected. The lab analysis of the samples showed that after the closing of the plant, 10 years ago, the pollution of soil by arsenic and lead still remains in some points near the main Chimney.