A Systemic Approach for Modeling Soil Functions
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Soil Survey
The Soil Survey The soil survey delineates the basal soil pattern of an area and characterises each kind of soil so that the response to changes can be assessed and used as a basis for prediction. Although in an economic climate it is necessarily made for some practical purpose, it is not subordinated to the parti cular need of the moment, but is conducted in a scientific way that provides basal information of general application and eliminates the necessity for a resurvey whenever a new problem arises. It supplies information that can be combined, analysed, or amplified for many practical purposes, but the purpose should not be allowed to modify the method of survey in any fundamental way. According to the degree of detail required, soil surveys in New Zealand are classed as general, . district, or detailed. General surveys produce sufficient detail for a final map on the scale of 4 miles to an inch (1 :253440); they show the main sets of soils and their general relation to land forms; they are an aid to investigations and planning on the regional or national scale. District surveys, for maps, on the scale of 2 miles to an inch (1: 126720), show soil types or, where the pattern is detailed, combinations of types; they are designed to show the soil pattern in sufficient detail to allow the study of local soil problems and to provide a basis for assembling and distributing information in many fields such as agriculture, forestry, and engineering. Detailed surveys, mostiy for maps on the scale of 40 chains to an inch (1 :31680), delineate soil types and land-use phases, and show the soil pattern in relation to farm boundaries and subdivisional fences. -
Soil Contamination and Human Health: a Major Challenge For
Soil contamination and human health : A major challenge for global soil security Florence Carre, Julien Caudeville, Roseline Bonnard, Valérie Bert, Pierre Boucard, Martine Ramel To cite this version: Florence Carre, Julien Caudeville, Roseline Bonnard, Valérie Bert, Pierre Boucard, et al.. Soil con- tamination and human health : A major challenge for global soil security. Global Soil Security Sympo- sium, May 2015, College Station, United States. pp.275-295, 10.1007/978-3-319-43394-3_25. ineris- 01864711 HAL Id: ineris-01864711 https://hal-ineris.archives-ouvertes.fr/ineris-01864711 Submitted on 30 Aug 2018 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. Human Health as another major challenge of Global Soil Security Florence Carré, Julien Caudeville, Roseline Bonnard, Valérie Bert, Pierre Boucard, Martine Ramel Abstract This chapter aimed to demonstrate, by several illustrated examples, that Human Health should be considered as another major challenge of global soil security by emphasizing the fact that (a) soil contamination is a worldwide issue, estimations can be done based on local contamination but the extent and content of diffuse contamination is largely unknown; (b) although soil is able to store, filter and reduce contamination, it can also transform and make accessible soil contaminants and their metabolites, contributing then to human health impacts. -
Evolution of Loess-Derived Soil Along a Topo-Climatic Sequence in The
European Journal of Soil Science, May 2017, 68, 270–280 doi: 10.1111/ejss.12425 Evolution of loess-derived soil along a climatic toposequence in the Qilian Mountains, NE Tibetan Plateau F. Yanga,c ,L.M.Huangb,c,D.G.Rossitera,d,F.Yanga,c,R.M.Yanga,c & G. L. Zhanga,c aState Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, NO. 71 East Beijing Road, Xuanwu District, Nanjing 210008, China, bKey Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, No. 11(A), Datun Road, Chaoyang District, Beijing 100101, China, cUniversity of the Chinese Academy of Sciences, No.19(A) Yuquan Road, Shijingshan District, Beijing 100049, China, and dSchool of Integrative Plant Sciences, Section of Soil and Crop Sciences, Cornell University, Ithaca NY 14853, USA Summary Holocene loess has been recognized as the primary source of the silty topsoil in the northeast Qinghai-Tibetan Plateau. The processes through which these uniform loess sediments develop into diverse types of soil remain unclear. In this research, we examined 23 loess-derived soil samples from the Qilian Mountains with varying amounts of pedogenic modification. Soil particle-size distribution and non-calcareous mineralogy were changed only slightly because of the weak intensity of chemical weathering. Accumulation of soil organic carbon (SOC) and leaching of carbonate were both identified as predominant pedogenic responses to soil forming processes. Principal component analysis and structural analysis revealed the strong correlations between soil carbon (SOC and carbonate) and several soil properties related to soil functions. -
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. -
Advanced Crop and Soil Science. a Blacksburg. Agricultural
DOCUMENT RESUME ED 098 289 CB 002 33$ AUTHOR Miller, Larry E. TITLE What Is Soil? Advanced Crop and Soil Science. A Course of Study. INSTITUTION Virginia Polytechnic Inst. and State Univ., Blacksburg. Agricultural Education Program.; Virginia State Dept. of Education, Richmond. Agricultural Education Service. PUB DATE 74 NOTE 42p.; For related courses of study, see CE 002 333-337 and CE 003 222 EDRS PRICE MF-$0.75 HC-$1.85 PLUS POSTAGE DESCRIPTORS *Agricultural Education; *Agronomy; Behavioral Objectives; Conservation (Environment); Course Content; Course Descriptions; *Curriculum Guides; Ecological Factors; Environmental Education; *Instructional Materials; Lesson Plans; Natural Resources; Post Sc-tondary Education; Secondary Education; *Soil Science IDENTIFIERS Virginia ABSTRACT The course of study represents the first of six modules in advanced crop and soil science and introduces the griculture student to the topic of soil management. Upon completing the two day lesson, the student vill be able to define "soil", list the soil forming agencies, define and use soil terminology, and discuss soil formation and what makes up the soil complex. Information and directions necessary to make soil profiles are included for the instructor's use. The course outline suggests teaching procedures, behavioral objectives, teaching aids and references, problems, a summary, and evaluation. Following the lesson plans, pages are coded for use as handouts and overhead transparencies. A materials source list for the complete soil module is included. (MW) Agdex 506 BEST COPY AVAILABLE LJ US DEPARTMENT OFmrAITM E nufAT ION t WE 1. F ARE MAT IONAI. ItiST ifuf I OF EDuCATiCiN :),t; tnArh, t 1.t PI-1, t+ h 4t t wt 44t F.,.."11 4. -
A New Era of Digital Soil Mapping Across Forested Landscapes 14 Chuck Bulmera,*, David Pare´ B, Grant M
CHAPTER A new era of digital soil mapping across forested landscapes 14 Chuck Bulmera,*, David Pare´ b, Grant M. Domkec aBC Ministry Forests Lands Natural Resource Operations Rural Development, Vernon, BC, Canada, bNatural Resources Canada, Canadian Forest Service, Laurentian Forestry Centre, Quebec, QC, Canada, cNorthern Research Station, USDA Forest Service, St. Paul, MN, United States *Corresponding author ABSTRACT Soil maps provide essential information for forest management, and a recent transformation of the map making process through digital soil mapping (DSM) is providing much improved soil information compared to what was available through traditional mapping methods. The improvements include higher resolution soil data for greater mapping extents, and incorporating a wide range of environmental factors to predict soil classes and attributes, along with a better understanding of mapping uncertainties. In this chapter, we provide a brief introduction to the concepts and methods underlying the digital soil map, outline the current state of DSM as it relates to forestry and global change, and provide some examples of how DSM can be applied to evaluate soil changes in response to multiple stressors. Throughout the chapter, we highlight the immense potential of DSM, but also describe some of the challenges that need to be overcome to truly realize this potential. Those challenges include finding ways to provide additional field data to train models and validate results, developing a group of highly skilled people with combined abilities in computational science and pedology, as well as the ongoing need to encourage communi- cation between the DSM community, land managers and decision makers whose work we believe can benefit from the new information provided by DSM. -
Improving Soil and Soil Functions
IMPROVING SOIL AND SOIL FUNCTIONS BAMPA FRANCESCA AND CREAMER RACHEL (WUR) AGRIRESEARCH CONFERENCE, INNOVATING FOR THE FUTURE OF FARMING AND RURAL COMMUNITIES BRUXELLES, 3RD MAY 2018 This project has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement No 635201. SOILS ARE A FINITE RESOURCE compaction loss of biodiversity salinisation loss of organic matter flooding contamination landslides erosion sealing ...FROM THREATS TO FUNCTIONS 2 www.landmark2020.eu email [email protected] twitter @Landmark2020 02/05/2018 DEMANDS ON OUR LAND How do we increase our productivity? I want to grow my milk output by 50% DEMANDS ON OUR LAND 3 www.landmark2020.eu email [email protected] twitter @Landmark2020 02/05/2018 DEMANDS ON OUR LAND We need better water regulation by our land… 4 www.landmark2020.eu email [email protected] twitter @Landmark2020 02/05/2018 DDEMANDSEMANDS ONONOUROURLANDLAND We need to protect our We need to sequester carbon resources carbon 5 www.landmark2020.eu email [email protected] twitter @Landmark2020 02/05/2018 DEMANDS ON OUR LAND We need to find a home for our waste… 6 www.landmark2020.eu email [email protected] twitter @Landmark2020 02/05/2018 DEMANDS ON OUR LAND Soil biodiversity is the driver of many processes in soils Protect the home of biodiversity Lijbert Brussaard WHAT CAN OUR LAND SUPPLY? Water Provision Primary and purification Production Carbon sequestration Nutrient Cycling Habitat for biodiversity All soils / land perform all functions …but different parts of the land(scape) are better at delivering different functions Schulte et al., 2014 More info - interactive glossary http://landmark2020.eu/landmark-glossary/ 8 www.landmark2020.eu email [email protected] twitter @Landmark2020 02/05/2018 LAND MANAGEMENT: ASSESSMENT, RESEARCH, KNOWLEDGE BASE Objective: to quantify the supply of soil functions across the EU as determined by soil properties, land use and soil management practices. -
Evaluation of Digital Soil Mapping Approaches with Large Sets of Environmental Covariates
SOIL, 4, 1–22, 2018 https://doi.org/10.5194/soil-4-1-2018 © Author(s) 2018. This work is distributed under SOIL the Creative Commons Attribution 3.0 License. Evaluation of digital soil mapping approaches with large sets of environmental covariates Madlene Nussbaum1, Kay Spiess1, Andri Baltensweiler2, Urs Grob3, Armin Keller3, Lucie Greiner3, Michael E. Schaepman4, and Andreas Papritz1 1Institute of Biogeochemistry and Pollutant Dynamics, ETH Zürich, Universitätstrasse 16, 8092 Zürich, Switzerland 2Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Zürcherstrasse 111, 8903 Birmensdorf, Switzerland 3Research Station Agroscope Reckenholz-Taenikon ART, Reckenholzstrasse 191, 8046 Zürich, Switzerland 4Remote Sensing Laboratories, University of Zurich, Wintherthurerstrasse 190, 8057 Zürich, Switzerland Correspondence: Madlene Nussbaum ([email protected]) Received: 19 April 2017 – Discussion started: 9 May 2017 Revised: 11 October 2017 – Accepted: 24 November 2017 – Published: 10 January 2018 Abstract. The spatial assessment of soil functions requires maps of basic soil properties. Unfortunately, these are either missing for many regions or are not available at the desired spatial resolution or down to the required soil depth. The field-based generation of large soil datasets and conventional soil maps remains costly. Mean- while, legacy soil data and comprehensive sets of spatial environmental data are available for many regions. Digital soil mapping (DSM) approaches relating soil data (responses) to environmental -
Soil Organic Carbon Storage As a Key Function of Soils
Geoderma 333 (2019) 149–162 Contents lists available at ScienceDirect Geoderma journal homepage: www.elsevier.com/locate/geoderma Soil organic carbon storage as a key function of soils - A review of drivers and indicators at various scales T ⁎ Martin Wiesmeiera,b, , Livia Urbanskia, Eleanor Hobleya, Birgit Langc, Margit von Lützowa, Erika Marin-Spiottad, Bas van Wesemaele, Eva Rabotf, Mareike Ließf, Noelia Garcia-Francoa, Ute Wollschlägerf, Hans-Jörg Vogelf, Ingrid Kögel-Knabnera,g a Chair of Soil Sciences, TUM School of Life Sciences Weihenstephan, Technical University of Munich, Freising, Germany b Bavarian State Research Center for Agriculture, Institute for Organic Farming, Soil and Resource Management, Freising, Germany c Senckenberg Museum of Natural History Görlitz, Görlitz, Germany d Department of Geography, University of Wisconsin-Madison, 550 North Park Street, Madison, WI 53706, USA e Georges Lemaître Centre for Earth and Climate Research, Earth and Life Institute, Université Catholique de Louvain, 1348 Louvain-la-Neuve, Belgium f Helmholtz Centre for Environmental Research - UFZ, Halle, Germany g Institute for Advanced Study, Technical University of Munich, Garching, Germany ARTICLE INFO ABSTRACT Handling Editor: Junhong Bai The capacity of soils to store organic carbon represents a key function of soils that is not only decisive for climate ff ff Keywords: regulation but also a ects other soil functions. Recent e orts to assess the impact of land management on soil Clay mineralogy functionality proposed that an indicator- or proxy-based approach is a promising alternative to quantify soil Specific surface area functions compared to time- and cost-intensive measurements, particularly when larger regions are targeted. The Metal oxides objective of this review is to identify measurable biotic or abiotic properties that control soil organic carbon Microorganisms (SOC) storage at different spatial scales and could serve as indicators for an efficient quantification of SOC. -
What's Your Soil Type?
What’s Your Soil Type? What’s Soil Made Of? Good soil is a well balanced mixture of inorganic matter, organic matter, water and air. Everything you do to manage plants depends on the soil. The soil inorganic mineral matter is determined by the parent rock of the local geology. Here in Wichita, Kansas, we have limestone & shale because this area was once a shallow inland sea that has been uplifted and then eroded by wind & water. The local soils have a high pH (alkaline a.k.a. base) and once you’re away from the river bottom land, the soil is more clay. Soil Texture Sand, silt and clay are the sizes of soil particles. Sand is the largest particle, and clay, being microscopic, is the smallest. The best soils are loams, which are a good balance between the three particle sizes. Soil texture is created by the amount each particle size mixed in a given soil. Texture is an important property of soil. It affects everything from crop productivity and nutrient requirements, to a soil’s potential for erosion. Texture determines the soil pore size, which is the space between soil particles. When you know the texture, then you know how fast a soil will absorb water, as well as, how much it will retain after the water is turned off. Jar Test Soil Amending The A jar test is a simple way to determine what type of soil you have. To conduct a jar test, you will need: A 1 quart or larger size glass jar with lid A paper or plastic bag Water A ruler 1. -
Unit 2.3, Soil Biology and Ecology
2.3 Soil Biology and Ecology Introduction 85 Lecture 1: Soil Biology and Ecology 87 Demonstration 1: Organic Matter Decomposition in Litter Bags Instructor’s Demonstration Outline 101 Step-by-Step Instructions for Students 103 Demonstration 2: Soil Respiration Instructor’s Demonstration Outline 105 Step-by-Step Instructions for Students 107 Demonstration 3: Assessing Earthworm Populations as Indicators of Soil Quality Instructor’s Demonstration Outline 111 Step-by-Step Instructions for Students 113 Demonstration 4: Soil Arthropods Instructor’s Demonstration Outline 115 Assessment Questions and Key 117 Resources 119 Appendices 1. Major Organic Components of Typical Decomposer 121 Food Sources 2. Litter Bag Data Sheet 122 3. Litter Bag Data Sheet Example 123 4. Soil Respiration Data Sheet 124 5. Earthworm Data Sheet 125 6. Arthropod Data Sheet 126 Part 2 – 84 | Unit 2.3 Soil Biology & Ecology Introduction: Soil Biology & Ecology UNIT OVERVIEW MODES OF INSTRUCTION This unit introduces students to the > LECTURE (1 LECTURE, 1.5 HOURS) biological properties and ecosystem The lecture covers the basic biology and ecosystem pro- processes of agricultural soils. cesses of soils, focusing on ways to improve soil quality for organic farming and gardening systems. The lecture reviews the constituents of soils > DEMONSTRATION 1: ORGANIC MATTER DECOMPOSITION and the physical characteristics and soil (1.5 HOURS) ecosystem processes that can be managed to In Demonstration 1, students will learn how to assess the improve soil quality. Demonstrations and capacity of different soils to decompose organic matter. exercises introduce students to techniques Discussion questions ask students to reflect on what envi- used to assess the biological properties of ronmental and management factors might have influenced soils. -
Articles, and the Creation of New Soil Habitats in Other Scientific fields Who Also Made Early Contributions Through the Weathering of Rocks (Puente Et Al., 2004)
Editorial SOIL, 1, 117–129, 2015 www.soil-journal.net/1/117/2015/ doi:10.5194/soil-1-117-2015 SOIL © Author(s) 2015. CC Attribution 3.0 License. The interdisciplinary nature of SOIL E. C. Brevik1, A. Cerdà2, J. Mataix-Solera3, L. Pereg4, J. N. Quinton5, J. Six6, and K. Van Oost7 1Department of Natural Sciences, Dickinson State University, Dickinson, ND, USA 2Departament de Geografia, Universitat de València, Valencia, Spain 3GEA-Grupo de Edafología Ambiental , Departamento de Agroquímica y Medio Ambiente, Universidad Miguel Hernández, Avda. de la Universidad s/n, Edificio Alcudia, Elche, Alicante, Spain 4School of Science and Technology, University of New England, Armidale, NSW 2351, Australia 5Lancaster Environment Centre, Lancaster University, Lancaster, UK 6Department of Environmental Systems Science, Swiss Federal Institute of Technology, ETH Zurich, Tannenstrasse 1, 8092 Zurich, Switzerland 7Georges Lemaître Centre for Earth and Climate Research, Earth and Life Institute, Université catholique de Louvain, Louvain-la-Neuve, Belgium Correspondence to: J. Six ([email protected]) Received: 26 August 2014 – Published in SOIL Discuss.: 23 September 2014 Revised: – – Accepted: 23 December 2014 – Published: 16 January 2015 Abstract. The holistic study of soils requires an interdisciplinary approach involving biologists, chemists, ge- ologists, and physicists, amongst others, something that has been true from the earliest days of the field. In more recent years this list has grown to include anthropologists, economists, engineers, medical professionals, military professionals, sociologists, and even artists. This approach has been strengthened and reinforced as cur- rent research continues to use experts trained in both soil science and related fields and by the wide array of issues impacting the world that require an in-depth understanding of soils.