The Business Side of Ecosystem Services of Soil Systems
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Age and Pedogenic Reconstruction of a Paleo–Relict Chernozem Soil from Central Transylvanian Basin
AGE AND PEDOGENIC RECONSTRUCTION OF A PALEO–RELICT CHERNOZEM SOIL FROM CENTRAL TRANSYLVANIAN BASIN F. PENDEA1, Z. SZÁNTÓ2, A. S. BADARAU1 and S. DEZSI1 1Babes–Bolyai University, Faculty of Geography, Cluj–Napoca Clinicilor street no 5–7, 3400 Cluj–Napoca, Romania 2Institute of Nuclear Research, Laboratory of Environmental Studies, H 4001 Debrecen P.O Box 51, Hungary Abstract: The “chernozem” area of Transylvanian Lowland has been of much debate in the last two centuries. The paper presents pedological and geochronological evidence that the chernozem soils of the Central Transylvania have relict Late Glacial–Early Holocene features and at least partially must be clasiffied as paleo–relict in the sense of Reuter (2000). Key words: radiocarbon dating, pedogenic carbonates, paleo–relict features, Central Transylvania During the last century a much debated issue for Romanian pedological and botanical scientific communities was the age and origin of the Central Transylvanian Mollisol cover in conjunction with the associated forest–steppe vegetation. In this study we have found at least partial evidence that the chernozem soil cover in Central Transylvanian was a stable feature long before the ascent of human activities and that, in the Late Holocene, they have suffered a degradation process to the present state of Haplic and Luvic chernozem. The process is somewhat similar with that inferred for Central and Southern Germany, where chernozems formed in the dry steppe or forest–steppe conditions were degraded to brown earths, the resulting polygenetic cover being named Braunerde (Parabraunerde)–Tschernozem (Catt 1989). Because the nature and properties of different soil horizons can hold information with respect to the time pedogenic factor an investigation was undertaken to determine if the typical chernozem features were indeed Late Holocene (Post–Neolithic) as it has been accepted before. -
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 -
REGENERATIVE AGRICULTURE and the SOIL CARBON SOLUTION SEPTEMBER 2020
REGENERATIVE AGRICULTURE and the SOIL CARBON SOLUTION SEPTEMBER 2020 AUTHORED BY: Jeff Moyer, Andrew Smith, PhD, Yichao Rui, PhD, Jennifer Hayden, PhD REGENERATIVE AGRICULTURE IS A WIN-WIN-WIN CLIMATE SOLUTION that is ready for widescale implementation now. WHAT ARE WE WAITING FOR? Table of Contents 3 Executive Summary 5 Introduction 9 A Potent Corrective 11 Regenerative Principles for Soil Health and Carbon Sequestration 13 Biodiversity Below Ground 17 Biodiversity Above Ground 25 Locking Carbon Underground 26 The Question of Yields 28 Taking Action ACKNOWLEDGMENTS 30 Soil Health for a Livable Future Many thanks to the Paloma Blanca Foundation and Tom and Terry Newmark, owners of Finca Luna Nueva Lodge and regenerative farm in 31 References Costa Rica, for providing funding for this paper. Tom is also the co-founder and chairman of The Carbon Underground. Thank you to Roland Bunch, Francesca Cotrufo, PhD, David Johnson, PhD, Chellie Pingree, and Richard Teague, PhD for providing interviews to help inform the paper. EXECUTIVE SUMMARY The environmental impacts of agricultural practices This introduction is co-authored by representatives of two The way we manage agricultural land 140 billion new tons of CO2 contamination to the blanket of and translocation of carbon from terrestrial pools to formative organizations in the regenerative movement. matters. It matters to people, it matters to greenhouse gases already overheating our planet. There is atmospheric pools can be seen and felt across a broad This white paper reflects the Rodale Institute’s unique our society, and it matters to the climate. no quarreling with this simple but deadly math: the data are unassailable. -
Chernozems Kastanozems Phaeozems
Chernozems Kastanozems Phaeozems Peter Schad Soil Science Department of Ecology Technische Universität München Steppes dry, open grasslands in the mid-latitudes seasons: - humid spring and early summer - dry late summer - cold winter occurrence: - Eurasia - North America: prairies - South America: pampas Steppe soils Chernozems: mostly in steppes Kastanozems: steppes and other types of dry vegetation Phaeozems: steppes and other types of medium-dry vegetation (till 1998: Greyzems, now merged to the Phaeozems) all steppe soils: mollic horizon Definition of the mollic horizon (1) The requirements for a mollic horizon must be met after the first 20 cm are mixed, as in ploughing 1. a soil structure sufficiently strong that the horizon is not both massive and hard or very hard when dry. Very coarse prisms (prisms larger than 30 cm in diameter) are included in the meaning of massive if there is no secondary structure within the prisms; and Definition of the mollic horizon (2) 2. both broken and crushed samples have a Munsell chroma of less than 3.5 when moist, a value darker than 3.5 when moist and 5.5 when dry (shortened); and 3. an organic carbon content of 0.6% (1% organic matter) or more throughout the thickness of the mixed horizon (shortened); and Definition of the mollic horizon (3) 4. a base saturation (by 1 M NH4OAc) of 50% or more on a weighted average throughout the depth of the horizon; and Definition of the mollic horizon (4) 5. the following thickness: a. 10 cm or more if resting directly on hard rock, a petrocalcic, petroduric or petrogypsic horizon, or overlying a cryic horizon; b. -
The Soil Food Web
THE SOIL FOOD WEB HEALTHY SOIL HEALTHY ENVIRONMENT The Soil Food Web Alan Sundermeier Extension Educator and Program Leader, Wood County Extension, The Ohio State University. Vinayak Shedekar Postdoctural Researcher, The Ohio State University. A healthy soil depends on the interaction of many organisms that make up the soil food web. These organisms live all or part of their life cycle in the soil and are respon- sible for converting energy as one organism consumes another. Source: Soil Biology Primer The phospholipid fatty acid (PLFA) test can be used to measure the activity of the soil food web. The following chart shows that mi-crobial activity peaks in early summer when soil is warm and moisture is adequate. Soil sampling for detecting soil microbes should follow this timetable to better capture soil microbe activity. The soil food web begins with the ener- gy from the sun, which triggers photo- synthesis in plants. Photosynthesis re- sults in plants using the sun’s energy to fix carbon dioxide from the atmosphere. This process creates the carbon and organic compounds contained in plant material. This is the first trophic level. Then begins building of soil organic matter, which contains both long-last- ing humus, and active organic matter. Active organic matter contains readily available energy, which can be used by simple soil organisms in the second trophic level of the soil food web. Source: Soil Biology Primer SOILHEALTH.OSU.EDU THE SOIL FOOD WEB - PAGE 2 The second trophic level contains simple soil organisms, which Agriculture can enhance the soil food web to create more decompose plant material. -
Culman-2009-AGEE-Inpress.Pdf
G Model AGEE-3535; No of Pages 12 Agriculture, Ecosystems and Environment xxx (2009) xxx–xxx Contents lists available at ScienceDirect Agriculture, Ecosystems and Environment journal homepage: www.elsevier.com/locate/agee Long-term impacts of high-input annual cropping and unfertilized perennial grass production on soil properties and belowground food webs in Kansas, USA S.W. Culman a,*, S.T. DuPont b,1, J.D. Glover c, D.H. Buckley a, G.W. Fick a, H. Ferris b, T.E. Crews d a Department of Crop and Soil Sciences, Cornell University, Ithaca, NY 14853, United States b Department of Nematology, University of California, Davis, CA 95616, United States c The Land Institute, 2440 E. Water Well Road, Salina, KS 67401, United States d Environmental Studies, Prescott College, Prescott, AZ 86301, United States ARTICLE INFO ABSTRACT Article history: Soil ecosystem properties and processes which simultaneously maintain native fertility and sustain Received 10 May 2009 plant yields are of principal interest in sustainable agriculture. Native prairies in Kansas are relevant in Received in revised form 2 November 2009 this context, as some have been annually harvested for hay for over 75 years with no fertilization or Accepted 5 November 2009 detectable decline in yield or soil fertility. In contrast, annual crop production has resulted in significant Available online xxx reductions in soil fertility and now requires intensive inputs to maintain yields. Soil food webs were compared between hayed native grasslands and adjacent annual croplands in order to determine the Keywords: long-term effects of these two production systems on soil ecosystem properties. -
Appendices Soil Quality/Soil Health Cards
Appendices Appendices v Soil Quality/Soil Health Cards 1. Willamette Valley Soil Quality Card 2. Maryland Soil Quality Assessment Book v Readings (not included in Web version) 1. Farmer/Scientist Focus Sessions: A How-to Guide (1993). D. McGrath, L.S. Lev, H. Murray, R.D. William. Oregon State University Extension Service, EM 8554. 2. How Farmers Assess Soil Health and Quality (1995). D.E. Romig, M.J. Garlynd, R.F. Harris, K. McSweeney. Journal of Soil and Water Conservation. 50(3): 229- 236. 3. The Changing Concept of Soil Quality (1995). B.P. Warkentin. Journal of Soil and Water Conservation. 50(3): 226-228 Permission for reprints in this guide was obtained from authors and publishers. v NRCS State Technical Notes 1. Maryland Soil Quality Assessment Book Technical Note 2. NRCS State Technical Note: Oregon Soil Quality Cards v Soil Quality Card User Guide (not included in Web version) Sample of the Willamette Valley Soil Quality Card Guide (1998). J. Burket et al. Oregon State University Extension Service, EM 8710. (Contact OSUES at: http://osu.orst.edu/extension/, or by faxing 541-737-0817.) v Take-home Training Materials Materials provided to (and added to the Guide by) participants in training sessions. 104 Soil Quality Card Design Guide Willamette Valley Soil Quality Assessment Card The Willamette Valley Soil Quality Assessment Card is a standard paper size (8.5” x 11”) pad, which includes user instructions, an assessment calendar, and multiple soil assessment cards (printed on Rite- in-the-Rain paper). The card was also produced as a fold-out brochure for convenient display and distribution. -
Soil Life in Reconstructed Ecosystems: Initial Soil Food Web Responses After Rebuilding a Forest Soil Profile for a Climate Change Experiment
Soil life in reconstructed ecosystems: Initial soil food web responses after rebuilding a forest soil profile for a climate change experiment Paul T. Rygiewicza,*, Vicente J. Monleonb, Elaine R. Inghamc, Kendall J. Martind, Mark G. Johnsona ABSTRACT Disrupting ecosystem components. while transferring and reconstructing them for experiments can produce myriad responses. Establishing the extent of these biological responses as the system approaches a new equilibrium allows us more reliably to emulate comparable native systems. That is, the sensitivity of analyzing ecosystem processes in a reconstructed system is improved by excluding the period when observed phenomena are primarily responses caused by establishing the experiment rather than effects of imposed treatments; achieved by determining the extent of any pulse of activity caused by preparatory procedures. A native forest soil was physically disrupted when it was collected. sieved. and then rebuilt in lysimeters in a controlled-environment study evaluating the influence of elevated atmospheric CO2 concentration and elevated atmospheric temperature on the reconstructed soil that was planted with Douglas-fir (Pseudotsugo menziesii Mirb. Franco) seedlings. Generally. soil food web populations responded in two phases during the exposure as indicated by preliminary evaluation of the 4.5-year dataset. Also. previous work indicated that relatively elevated soil CO2 effluxes occurred during the first phase. suggesting that food web populations may have responded to carbon sources made available when the soil was harvested and its profile reconstructed in the lysimeters, Results are presented for bacterial and fungal biomass. numbers of protozoa and nematodes to gain insight on whether the first phase responses are attributable to the acute stress of physically disrupting the soil. -
Sustainable Soil Management
Top of Form ATTRAv2 page skip navigation 500 500 500 500 500 0 Search Bottom of Form 800-346-9140 Home | Site Map | Who We Are | Contact (English) Us | Calendar | Español | Text Only 800-411-3222 (Español) Home > Master Publication List > Sustainable Soil Management What Is Sustainable Soil Management Sustainable Agriculture? The printable PDF version of the Horticultural By Preston Sullivan entire document is available at: Crops NCAT Agriculture Specialist http://attra.ncat.org/attra- © NCAT 2004 pub/PDF/soilmgmt.pdf Field Crops ATTRA Publication #IP027/133 31 pages — 1.5 mb Download Acrobat Reader Soils & Compost Water Management Pest Management Organic Farming Livestock Marketing, Business & Risk Abstract Soybeans no-till planted into Management wheat stubble. This publication covers basic soil Photo by: Preston Sullivan Farm Energy properties and management steps toward building and maintaining healthy soils. Part I deals with basic Education soil principles and provides an understanding of living soils and how they work. In this section you will find answers to why soil organisms Other Resources and organic matter are important. Part II covers management steps to build soil quality on your farm. The last section looks at farmers who Master have successfully built up their soil. The publication concludes with a Publication List large resource section of other available information. Table of Contents Top of Form Part I. Characteristics of Sustainable Soils o Introduction o The Living Soil: Texture and Structure o The Living Soil: The Importance of Soil Organisms 1011223551022 o Organic Matter, Humus, and the Soil Foodweb o Soil Tilth and Organic Matter oi o Tillage, Organic Matter, and Plant Productivity o Fertilizer Amendments and Biologically Active Soils Go o Conventional Fertilizers Enter your o Top$oil—Your Farm'$ Capital email above o Summary of Part I and click Go. -
Soil Microbiology
Module 5 TAKING CARE OF OUR PLANET • Unit 1 PLANET EARTH IS IN THE DANGER ZONE SOIL MICROBIOLOGY 1 Read the following text and decide which of these adjectives could be used instead of those underlined in the passage: abundant, available, better, big, dangerous, entire, minute, productive, several, supreme, useful, vital. Inorganic constituents (minerals, water, process that crop residues, grass clippings, air), dead organic matter and soil life are leaves, organic wastes, etc., are decomposed the components that make up the total soil and converted to forms useable for plant environment. The living portion of the soil can growth as well as converted to stable soil be divided into macro- and micro-organisms. organic matter called ‘humus’. Macro-organisms play an important role in The large organisms function as grinders in organic decomposition by chewing plant that they reduce the particle size of organic and animal residues into fine particles. residues making them more accessible and Though the micro-organic portion represents decomposable by the soil microbes. The soil considerably less than 1% of the soil mass, it microbial population also further decomposes is on this tiny fraction that the continued re- the waste products of the larger animals. cycling of nutrients mainly depends. Thus, the activities of different groups of soil Normal, fertile soils teem with soil microbes. organisms are linked in complex “food webs”. The most numerous microbes in soil are the One beneficial process carried out exclusively bacteria followed by the actinomycetes, the by soil microbes is called nitrogen fixation, the fungi, soil algae and cyanobacteria (“blue- capture of inert N2 gas (dinitrogen) from the air green algae”) and soil protozoa. -
Guidebook for Field Excursions Xllth International Symposium and Field Seminar on Paleopedology
'1 ■ I VJ 1 ■ ’ »■ " ' . ... !■ 1|Щ 11 ■ Institute of Geography, Russian Academy of Sciences Moscow State University, Soil Science Institute V.V. Dokuchaev Soil Science Institute Institute of History and Material Culture, Russian Academy of Sciences Kursk State University Upetsk State University W. Alekhin Centrul-Chemozemic State Biospheric Reserve Natural Architectural-Archaeological Museum-Resort "Dhmogorid' Guidebook for Field Excursions Xllth International Symposium and Field Seminar on Paleopedology ‘Paleosols, pedosediments and landscape morphology as archives of environmental evolution” 10 -15 August, 2013, Kursk, Russia Moscow 2013 ■ ....... ... - Guidebook for Field Excursions Xllth International Symposium and Field Seminar on Paleopedology CONTENTS Introduction (S.A. Sycheva) 5 1. General characterization of the environment and soils of the Central Russian Upland (S.A. Sycheva, I. V. Kovda, A. V.Kashkin) 9 1.1. Geology and relief 9 1.2. Climate 10 1.3. Hydrology 11 1.4. Vegetation 11 1.5. Soils 12 1.6. Human history and agricultural development of landscapes 12 KURSK SITE 14 2. Aleksandrov Quarry (S.A. Sycheva, E. D. Sheremetskaya, T.M. Grigorieva, M.A. Bronnikova, S.N. Sedov, V.S. Gunova, A.N. Siniakova, P.R.Pushkina) 14 2.1. General characteristics, geochronology and stratigraphy 14 2.2. Description of the composite generalized stratigraphic section 15 2.2.1. Morphology 15 2.2.2. Analytical data 20 2.3. Ryshkov (Mikulino) paleosols and paleocatena (MIS 5e) 23 2.3.1. Ryshkov paleosol on the paleoslope (section 15): interpretation of properties 23 2.3.2. Ryshkov pedolithocomplex in the bottom 27 2.4. Early Valdai Kukuev and Streletsk paleosols (MIS 5 & MIS 5a) 28 2.4.1. -
Structural State of Chernozem After Long-Term Post-Agrogenic Transformation Demydenko O
UDC 631.434 © 2019 Structural state of chernozem after long-term post-agrogenic transformation Demydenko O. Cherkasy State Agricultural Research Station of the National Institute of Agriculture of NAAS, 13 Dokuchaieva Str., Holodnianske village, Smilianskyi district, Cherkasy oblast, Ukraine, 20731; e-mail: [email protected] The purpose. To determine the main laws of transformation and regulatory parameters of the structural state change of chernozems of the forest-steppe zone in conditions of long-term post-agrogenic transformation according to the results of dry sieving of soil samples and statistical analysis of the data using the method of principal components, factor and non-parametric analysis. Methods. Laboratory analytical, experimental field, statistical. Results. The performed statistical processing of results of the analysis of dry sieving of the structure of chernozems in the long-term post-agrogenic state demonstrates the promise of using factor, cluster and non-parametric analysis methods. An important role in the restoration of the structure of chernozems is played by a combination of structural units 3.0—0.5 mm in size, with which the additional density in the humus horizon is inversely proportional, and with the humus content, it is directly proportional. The carried out clustering indicates that the content of the presented chernozems in the state of virgin soil and long-term deposits is the separated and not similar state of soil objects. But there is a general pattern of formation of a set of structural units of 3.0-0.5 mm similar to chernozems in the state of virgin soil, which content exceeds 40-50% of the content of parts in the agronomically valuable interval.