DOCSLIB.ORG

Soil Memory: Types of Record, Carriers, Hierarchy and Diversity

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Soil Memory: Types of Record, Carriers, Hierarchy and Diversity Revista Mexicana de Ciencias Geológicas,Soil memory: v. 21, núm.Types 1, of 2004, record, p. carriers,1-8 hierarchy and diversity 1 Soil memory: Types of record, carriers, hierarchy and diversity Victor O. Targulian* and Sergey V. Goryachkin Institute of Geography, Russian Academy of Sciences, Staromonetny per.29, Moscow, 119029, Russia. * [email protected] ABSTRACT The concept of palimpsest-wise soil memory and record is generally characterized in comparison with the book-wise memory and record of sedimentary rocks. Soil systems have a capacity for storing information about environmental factors and pedogenic processes that have been acting for a period of pedogenesis. The main mechanisms of soil memory and record formation are those sets of pedogenic processes that generate the solid phase products and features within the multiphase soil system. The main types of solid-phase carriers of soil memory and their spatial/temporal hierarchy within the soil system are briefly described. The phenomena of isomorphism and polymorphism of soil record carriers in regard to the pedogenic processes should be realized when we try to decode and understand the information stored in soil memory. Each specific type of climate could not be imprinted in only one type of pedon. When reading the record in the soil system under one type of climate, it is obligatory to account for the diversity of solid phase soil horizons and pedons induced by the diversity of parent materials (lithodiversity), topography (topodiversity), biota (biodiversity) and duration of pedogenesis (chronodiversity). Key words: soil memory, solid phase carriers, isomorphism, polymorphism. RESUMEN El concepto de registro y memoria palimpséstica en suelos es generalmente caracterizado en comparación con la memoria y registro en forma de libro presente en rocas sedimentarias. Los sistemas de suelos tienen capacidad para almacenar información sobre los factores ambientales y los procesos que han estado actuando durante un periodo de pedogénesis. Los principales mecanismos de memoria del suelo y formación de registro son aquellos conjuntos de procesos pedogenéticos que generan los productos de fase sólida y los rasgos dentro del sistema de suelo multifásico. Se describen brevemente los principales tipos de portadores en fase sólida de la memoria del suelo y su jerarquía espacio-temporal. Los fenómenos de isomorfismo y polimorfismo de los portadores del registro del suelo, en relación con los procesos pedogenéticos, deben ser considerados cuando tratamos de descifrar y entender la información almacenada en la memoria del suelo. Cada tipo específico de clima podría no estar marcado o grabado en un solo tipo de pedón. Cuando se lee el registro en el sistema de suelo bajo un tipo de clima, es obligatorio tener en cuenta la diversidad de los horizontes de suelo de fase sólida y los pedones inducida por la diversidad de materiales parentales (litodiversidad), topografía (topodiversidad), biota (biodiversidad) y duración de la pedogénesis (cronodiversidad). Palabras clave: memoria del suelo, portadores de fase sólida, isomorfismo, polimorfismo. 2 Targulian and Goryachkin TYPES OF ENVIRONMENT RECORDING IN interactions of soil-forming factors in time. Solid carriers EARTH LAND SURFACE SYSTEMS of soil memory can be developed from any kind of solid parent materials: igneous or sedimentary, natural or Soil memory is both: (i) a capacity of the complex anthropogenic. Soil records are forming in situ within the multiphase soil system to record environmental phenomena body of parent material due to its gradual transformation through pedogenic processes acting in situ in each point of by the interacting climatic, biotic, hydrological vertical and the land surface of the Earth, and (ii) a record itself of this lateral fluxes and cycles (including the anthropogenic ones). environmental and process information on the resistant soil Parent material changes, that resulted in new composition solid-phase carriers in situ. and/or arrangement of substances, could be perceived There are three main fundamentally different simultaneously as soil formation and as the soil recording pathways of recording of environmental and process of environment. information on the time-resistant and long-living solid Due to in-situ formation of soil memory, in each carriers. The first one is a very specific way of recording in ‘point’ of land surface it records very local, even ‘point’, glaciers where the individual ice layers record regional and combinations of environmental factors and pedogenic global climatic conditions, as well as chemical and dust processes at the levels of small-area ecosystems, variations composition of the atmosphere (Petit et al., 1990). Records of microclimate, microrelief, parent rocks mosaics, etc. in glaciers have very high temporal resolution and follow Therefore, soil memory has much more exact space exactly the seasonal and annual snow precipitation. But this resolution than sedimentary memory. On the other hand, way of recording is realized only in several very cold regions soil record is forming usually in one volume and thickness of the Earth (Antarctic, Arctic, and high-mountain glaciers). of the parent materials and rocks having been penetrated in The second pathway (Figure 1) is a well-known situ by atmo-hydro-biogenic forces, fluxes, and cycles. When recording by the Earth sedimentary systems, both these factors are changing in time, their records in soil are continental and marine. These systems reflect a much more changing thereafter and are superimposing on the previous complex set of environmental factors and processes: records in the same volume. Such superimposing can lead climatically, biologically and geologically controlled to different and complex combinations of older and newer mobilization of solid particles and solutions from records in the same soil volume and thickness: addition, watersheds, their mechanical and geochemical transfer, and juxtaposition, plexus, or obliteration of the features of each sedimentation, diagenesis and epigenesis of sediments record. (Strachov, 1963). Sedimentary records are very diverse: they Such sophistication of soil records leads, in the case could be biogenic (fossil plants, animal bones, phytoliths, of environmental evolution in time, to less exact time spores and pollen, coal, humus, etc.), lithogenic (mineral resolution of soil memory compared with sedimentary grains, rock debris), or geochemical (salts, carbonates, Fe, memory. In contrast with book-wise sedimentary memory Al, Si oxides precipitation). Sedimentary records are always and record, the soil memory and record could be called formed in individual lithological layers stacked up in vertical palimpsest-wise, which is a the term proposed for the sedimentary sequence, which reflects the temporal changes geomorphic systems (Allaby and Allaby, 1990). in environment and lithogenesis. Therefore, this type of Sedimentary and soil records are the two main record has high and exact time resolution and resembles a complementary ways of environmental records within the book-wise memory. At the same time, the sedimentary record upper part of the land lithosphere. The first one occurrs always accumulates the environmental and process both in terrestrial and marine environments, but only in areas information of the specific catchment area (or an area of of accretion; land areas without accretion do not have eolian transfer) and therefore memorizes the environment sedimentary memory. In such land areas, the main systems and geomorphic processes of some territory, but not of an recording the interaction of climate and biota with individual site. So, sedimentary records have usually low lithosphere are the soil and weathering systems developing space resolution because they are not on-site specific. They in situ (Martini and Chesworth, 1992). Moreover, soil summarize the results of bioclimatic and geomorphic records can be formed within the sedimentary rocks, being processes and factors, which are acting on some territory superimposed on the sedimentary memory as the memory not only in situ but also laterally, along the land surface. of the latest existing environment events (epilithogenic In contrast with sedimentary memory and record, soils pedogenesis). In several cases, the rates of slow terrestrial and weathering mantles* have a quite different type of sedimentation are comparable to the rates of soil formation, memory and record, which was proposed to be called soil and so called synlithogenic pedogenesis takes place. In such memory (Targulian and Sokolov, 1978; Targulian and cases the processes of solid particle deposition are closely Goryachkin, 2001). Soil memory and soil record (Figure 1) combined with the humification, weathering, leaching, and are forming in situ, in each specific place of on site other pedogenic processes within the forming soil body (many alluvial soils, Fluvisols, and volcanic-ash soils, * We consider the weathering mantle of all kinds of rocks as well as the Andosols). More often in areas of terrestrial sedimentation, soil to represent in-situ formed exogenic records on the land surface. the stratigraphic lacunae are imprinted by soil and/or Soil memory: Types of record, carriers, hierarchy and diversity 3 Figure 1. Formation of sedimentary (book-wise) and soil (palimsest-wise) memory. weathering profiles that record the environment conditions pedogenesis. Later, in the 1970s, Targulian and Sokolov, during the break of sedimentation (loess-soil, tephra-soil
Load more

Recommended publications
  • Engineering Behavior and Classification of Lateritic Soils in Relation to Soil Genesis Erdil Riza Tuncer Iowa State University
    Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1976 Engineering behavior and classification of lateritic soils in relation to soil genesis Erdil Riza Tuncer Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Civil Engineering Commons Recommended Citation Tuncer, Erdil Riza, "Engineering behavior and classification of lateritic soils in relation to soil genesis " (1976). Retrospective Theses and Dissertations. 5712. https://lib.dr.iastate.edu/rtd/5712 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. INFORMATION TO USERS This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1. The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image.
    [Show full text]
  • 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.
    [Show full text]
  • Soil Physics and Agricultural Production
    Conference reports Soil physics and agricultural production by K. Reichardt* Agricultural production depends very much on the behaviour of field soils in relation to crop production, physical properties of the soil, and mainly on those and to develop effective management practices that related to the soil's water holding and transmission improve and conserve the quality and quantity of capacities. These properties affect the availability of agricultural lands. Emphasis is being given to field- water to crops and may, therefore, be responsible for measured soil-water properties that characterize the crop yields. The knowledge of the physical properties water economy of a field, as well as to those that bear of soil is essential in defining and/or improving soil on the quality of the soil solution within the profile water management practices to achieve optimal and that water which leaches below the reach of plant productivity for each soil/climatic condition. In many roots and eventually into ground and surface waters. The parts of the world, crop production is also severely fundamental principles and processes that govern limited by the high salt content of soils and water. the reactions of water and its solutes within soil profiles •Such soils, classified either as saline or sodic/saline are generally well understood. On the other hand, depending on their alkalinity, are capable of supporting the technology to monitor the behaviour of field soils very little vegetative growth. remains poorly defined primarily because of the heterogeneous nature of the landscape. Note was According to statistics released by the Food and taken of the concept of representative elementary soil Agriculture Organization (FAO), the world population volume in defining soil properties, in making soil physical is expected to double by the year 2000 at its current measurements, and in using physical theory in soil-water rate of growth.
    [Show full text]
  • 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.
    [Show full text]
  • Characterization of Ecoregions of Idaho
    1 0 . C o l u m b i a P l a t e a u 1 3 . C e n t r a l B a s i n a n d R a n g e Ecoregion 10 is an arid grassland and sagebrush steppe that is surrounded by moister, predominantly forested, mountainous ecoregions. It is Ecoregion 13 is internally-drained and composed of north-trending, fault-block ranges and intervening, drier basins. It is vast and includes parts underlain by thick basalt. In the east, where precipitation is greater, deep loess soils have been extensively cultivated for wheat. of Nevada, Utah, California, and Idaho. In Idaho, sagebrush grassland, saltbush–greasewood, mountain brush, and woodland occur; forests are absent unlike in the cooler, wetter, more rugged Ecoregion 19. Grazing is widespread. Cropland is less common than in Ecoregions 12 and 80. Ecoregions of Idaho The unforested hills and plateaus of the Dissected Loess Uplands ecoregion are cut by the canyons of Ecoregion 10l and are disjunct. 10f Pure grasslands dominate lower elevations. Mountain brush grows on higher, moister sites. Grazing and farming have eliminated The arid Shadscale-Dominated Saline Basins ecoregion is nearly flat, internally-drained, and has light-colored alkaline soils that are Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and America into 15 ecological regions. Level II divides the continent into 52 regions Literature Cited: much of the original plant cover. Nevertheless, Ecoregion 10f is not as suited to farming as Ecoregions 10h and 10j because it has thinner soils.
    [Show full text]
  • Irrigation of Wi in Rapes
    42 NO VEMBER/DECEMBER 2001 WINEGR OWING ative. The same can be said of a plant's water potential. For example, when more water is Irrigation lost from a leaf via transpiration than moves into the leaf from the vascular tissue, its water potential will become more negative due to a relative increase in its solute concentration. of w i rapes This is important as water in plants and soils moves from regions where water potential is relatively high to regions where water potential is rela- tively low. Such differences in water in potential will result in movement of water from cell to cell within a plant or from regions within the soil profile that Cal Lorry E. WIIIIams y.t portion of the growing season in contain more moisture to those with Department of Viticulture Enology these areas and vineyard water use less. University of California-Qavis, and can be greater than the soil's water One way to measure the water Kearney Agricultural Center reservoir after the winter rainfall, potential of a plant organ in the field supplemental irrigation of vineyards (such as a leaf) is by using a pressure SYNOPSIS: How much irrigation water is may be required at some point dur- chamber. required to grow quality winegrapes ing summer months. The leaf's petiole is cut and the leaf depends upon site, the stage of vine quickly placed into the chamber with growth, row spacing, size of the vine's IRRIGATION MANAGEMENT the cut end of the petiole protruding canopy, and amount of rainfall occur- No matter where grapevines are out of the chamber.
    [Show full text]
  • 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.
    [Show full text]
  • Prairie Wetland Soils: Gleysolic and Organic Angela Bedard-Haughn Department of Soil Science, University of Saskatchewan
    PS&C Prairie Soils & Crops Journal Agricultural Soils of the Prairies Prairie Wetland Soils: Gleysolic and Organic Angela Bedard-Haughn Department of Soil Science, University of Saskatchewan Summary Gleysolic and Organic soils are collectively referred to as “wetland soils”. They are found in wet low-lying or level landscape positions. Gleysolic soils are found throughout the agricultural Prairies, in association with Chernozemic and Luvisolic soils. In semi-arid regions, they are frequently tilled in dry years and can be very productive due to their relatively high levels of soil moisture and nutrients. In the Prairie Provinces, Organic soils tend to be mostly associated with the Boreal transition zones at the northern and eastern perimeter of the Prairies. With proper management, these can also provide productive agricultural land, particularly for forages. Introduction Soils of the Gleysolic and Organic orders are collectively referred to as “wetland soils”. Soil maps of the agricultural region of the Canadian Prairies seldom have areas mapped as dominantly Gleysolic8 or Organic9; however, these soils are found throughout the region wherever climate and/or topography have led to persistent water-saturated conditions. Gleysols are mineral soils with colors that reflect intermittent or prolonged anaerobic (i.e., saturated, low oxygen) conditions (Fig. 1A). Organic soils reflect permanent anaerobic conditions, which lead to soils that are made up of variably decomposed plant residues, mostly from water-tolerant (i.e., hydrophytic) vegetation (Fig. 1B). Figure 1: A) Humic Luvic Gleysol, Saskatchewan and B) Typic Fibrisol (Organic), Manitoba7. Of the some 100,000,000 ha covered by the Canada Land Inventory (CLI) in the Prairie Provinces12, Gleysolic soils occupy less than 15% of the Prairie ecoregions and up to 40% in the Mid-Boreal (boreal = “northern”) Upland (Alberta) and Interlake Plain (Manitoba) ecoregions12.
    [Show full text]
  • World Reference Base for Soil Resources 2014 International Soil Classification System for Naming Soils and Creating Legends for Soil Maps
    ISSN 0532-0488 WORLD SOIL RESOURCES REPORTS 106 World reference base for soil resources 2014 International soil classification system for naming soils and creating legends for soil maps Update 2015 Cover photographs (left to right): Ekranic Technosol – Austria (©Erika Michéli) Reductaquic Cryosol – Russia (©Maria Gerasimova) Ferralic Nitisol – Australia (©Ben Harms) Pellic Vertisol – Bulgaria (©Erika Michéli) Albic Podzol – Czech Republic (©Erika Michéli) Hypercalcic Kastanozem – Mexico (©Carlos Cruz Gaistardo) Stagnic Luvisol – South Africa (©Márta Fuchs) Copies of FAO publications can be requested from: SALES AND MARKETING GROUP Information Division Food and Agriculture Organization of the United Nations Viale delle Terme di Caracalla 00100 Rome, Italy E-mail: [email protected] Fax: (+39) 06 57053360 Web site: http://www.fao.org WORLD SOIL World reference base RESOURCES REPORTS for soil resources 2014 106 International soil classification system for naming soils and creating legends for soil maps Update 2015 FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2015 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO.
    [Show full text]
  • Correlation Between the Polish Soil Classification (2011) and International Soil Classification System World Reference Base for Soil Resources (2015)
    DE DE GRUYTER 88 OPEN CEZARY KABA£A, MARCIN ŒWITONIAK, PRZEMYS£AW CHARZYÑSKI SOIL SCIENCE ANNUAL DOI: 10.1515/ssa-2016-0012 Vol. 67 No. 2/2016: 88–100 CEZARY KABA£A1*, MARCIN ŒWITONIAK2, PRZEMYS£AW CHARZYÑSKI2 1 Wroc³aw University of Environmental and Life Sciences, Institute of Soil Science and Environmental Protection Grunwaldzka 53, 50-357 Wroc³aw, Poland 2 Nicolaus Copernicus University, Department of Soil Science and Landscape Management Lwowska 1, 87-100 Toruñ, Poland Correlation between the Polish Soil Classification (2011) and international soil classification system World Reference Base for Soil Resources (2015) Abstract: The recent editions of the Polish Soil Classification (PSC) have supplied the correlation table with the World Reference Base for Soil Resources (WRB), which is the international soil classification most commonly used by Polish pedologists. However, the latest WRB edition (IUSS Working Group WRB 2015) has introduced significant changes and many of the former correlations became outdated. The current paper presents the closest equivalents of the soil orders, types and subtypes of the recent edition of the PSC (2011) and WRB (IUSS Working Group WRB 2015). The proposals can be used for general correlation of soil units on maps and in databases, and may support Polish soil scientists to establish the most appropriate equivalents for soils under study, as well as make PSC more available for an international society. Keywords: Polish Soils Classification, WRB, equivalents, reference soil groups, soil types INTRODUCTION quantitative concept. Presently, the Soil Taxonomy is used in over 40 countries (Krasilnikov 2002) as a Pedology appeared in the second half of the 19th primary system for naming the soils.
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]