(2006) World Reference Base for Soil Resources
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Soil Properties and Pre-Columbian Settlement Patterns in The
SOIL, 1, 65–81, 2015 www.soil-journal.net/1/65/2015/ doi:10.5194/soil-1-65-2015 SOIL © Author(s) 2015. CC Attribution 3.0 License. Soil properties and pre-Columbian settlement patterns in the Monumental Mounds Region of the Llanos de Moxos, Bolivian Amazon U. Lombardo1,2, S. Denier1, and H. Veit1 1Universität Bern, Geographisches Institut, Hallerstrasse 12, 3012 Bern, Switzerland 2CaSeS research group, IMF-CSIC, C/Egipciaques, 15-08001 Barcelona, Spain Correspondence to: U. Lombardo ([email protected]) Received: 5 May 2014 – Published in SOIL Discuss.: 15 May 2014 Revised: – – Accepted: 26 September 2014 – Published: 6 January 2015 Abstract. In the present paper we explore to what degree soil properties might have influenced pre-Columbian settlement patterns in the Monumental Mounds Region (MMR) of the Llanos de Moxos (LM), Bolivian Amazon. Monumental mounds are pre-Hispanic earth buildings and were preferentially built on mid- to late Holocene palaeolevees of the Grande River (here denominated PR1), while levees of older palaeorivers (PR0) were only sparsely occupied. We dug two transects across PR0 and PR1 levee–backswamp catenas and analysed them for grain size, pH, cation exchange capacity (CEC) and Corg. Our data show that PR1 soils, where the density of mounds is higher, have far greater agricultural potential than PR0 soils, which are affected by aluminium toxicity in the backswamps and by high levels of exchangeable sodium in the levees. This study provides new data on the soil properties of the south-eastern Bolivian Amazon and reinforces the hypothesis that environmental constraints and opportunities exerted an important role on pre-Columbian occupation patterns and the population density reached in the Bolivian Amazon. -
NRCS Keys to Soil Taxonomy
United States Department of Agriculture Keys to Soil Taxonomy Ninth Edition, 2003 Keys to Soil Taxonomy By Soil Survey Staff United States Department of Agriculture Natural Resources Conservation Service Ninth Edition, 2003 The United States Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, gender, religion, age, disability, political beliefs, sexual orientation, and marital or family status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at 202-720-2600 (voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326W, Whitten Building, 14th and Independence Avenue, SW, Washington, DC 20250-9410, or call 202-720-5964 (voice and TDD). USDA is an equal opportunity provider and employer. Cover: A natric horizon with columnar structure in a Natrudoll from Argentina. 5 Table of Contents Foreword .................................................................................................................................... 7 Chapter 1: The Soils That We Classify.................................................................................. 9 Chapter 2: Differentiae for Mineral Soils and Organic Soils ............................................... 11 Chapter 3: Horizons and Characteristics Diagnostic for the Higher Categories ................. -
Soil Taxonomy" in Particular ,
1. CONTROL NUMBER 2. SUBECT CLASSIFICATION (695) BIBLIOGRAPItlC DATA SHEET IN-AAJ-558 AF26-0000-0000 3. TITLE ANt) SUBTITLE (240) Experimental designs for predicting crop productivity with environmental and economic inputs for al rotcchnology transfer 4. PERSON.\I. AUTHORS (10P) Silva, J. A. 5. CORPORATE AUTHORS (101) Hawaii Univ. College of Tropical Agriculture 6. IDOCUMEN2< DATE (110)7. NUMBER OF PAGES (120) 8.ARC NUMBER [7 1981 13n631.5.S586b __ 9. R FRENCE ORGANIZATION (130) Hawaii 10. SUPI'PLEMENTARY NOTES (500) (In Departmental paper 49) 11. ABSTRACT (950) 12. DESCRIPTORS (920) 13. PROJECT NUMBER (150) Agricultural production Agricultural technology 931582C00 Technology transferi!Techoloy tansferYieldY e d14. CONTRACT NO.(I It)) 15. CONTRACT Soil fertility Experimentation TYPE (140) Tropics Productivity AID/ta-C-1108 Forecasting 16. TYPE OF DOCUMENT (160) AM 590-7 (10-79) Departmental Paper 49 Experimental Designs for Predicting Crop Productivity with Environmental and Economic Inputs for Agrotechnology Transfer Edited by James A. Silva ...... ,..,... *** .......... ....* ...... .... .. 00400O 00€€€€*00 .. ...* Y Y*b***S4....... ~~~.eeeeeoeeeeeU ........ o .. *.4.............*e............ :0 ooee............. ........... ....... nae of T c.e Haw i. ns..ut. CollegeofTrpclgr.cut a UnversityoHa B....EMAR.SO University of Hawaiio~ee BENCHMAR SO I Le~eSPoJECTU/ADCotac o.t-C1 14.. C4 '4 t 10 wte IA:A 77 d E/ Adt , I 26Esi ',. ,~ )~'I *3-! * Ire ~ -I ~ 0 1 N Koel4 'I M M Experimental Designs for Predicting Crop Productivity with Environmental and Economic Inputs for Agrotechnology Transfer Edited by James A. Silva Benchmark Soils Project UH/AiD Contract No. to-C-1108 The Author James A. Silva is Soil Scientist and Principal Investigator, Benchmark Soils Project/Hawaii, Department of Agronomy and Soil Science, College of Tropical Agriculture and Human Resources, University of Hawaii, Honolulu. -
81421371.Pdf
View metadata, citation and similar papers at core.ac.uk brought to you by CORE ORIGINAL SCIENTIFIC PAPER 187 Clay and Humus Contents Have the Key Impact on Physical Properties of Croatian Pseudogleys Vedran RUBINIĆ ( ) Stjepan HUSNJAK Summary Pseudogleys (Stagnosols according to WRB-2014) represent the second most widespread soil type in Croatia, developed almost exclusively in its Pannonian region. Although most Croatian Pseudogleys are found on agricultural land or in agro- ecosystems, they usually have numerous constraints for agricultural production. Primarily, this is due to their unfavorable water/air regime (precipitation water periodically stagnates on/in the poorly permeable subsoil horizon). Th e aim of this study was to determine which signifi cant diff erences in physical properties and humus content exist between the eluvial horizon (Eg) and the illuvial horizon (Btg) in Croatian Pseudogleys. Total of 33 Pseudogley profi les were investigated at 11 forest sites across the Pannonian region of Croatia. Properties of Eg horizon signifi cantly diff ered from the properties of Btg horizon. Compared with the Eg horizon, the Btg horizon had more clay, higher bulk density, less pores, and lower capacity for air. However, the stability of microaggregates was higher in the Btg horizon than in the Eg horizon. Contents of clay and humus have the key impact on most soil physical properties. Th ese results should be borne in mind, both when converting natural Pseudogleys into arable soils and when ameliorating arable Pseudogleys that contain the Eg horizon below the Ap horizon. Key words stagnosols, Pannonian region of Croatia, forest soils, soil physical properties, humus University of Zagreb Faculty of Agriculture, Svetošimunska 25, 10000 Zagreb, Croatia e-mail: [email protected] Received: June 4, 2016 | Accepted: November 17, 2016 Agriculturae Conspectus Scientifi cus . -
The Soil Map of the Flemish Region Converted to the 3 Edition of the World Reference Base for Soil Resources
Ontwikkelen en toepassen van een methodiek voor de vertaling van de Belgische bodemclassificatie van de kustpolders naar het internationale WRB systeem en generaliseren van de WRB-bodemkaart voor gans Vlaanderen naar het 1 : 250 000 schaalniveau The soil map of the Flemish region converted to the 3 rd edition of the World Reference Base for soil resources Stefaan Dondeyne, Laura Vanierschot, Roger Langohr Eric Van Ranst and Jozef Deckers Oct. 2014 Opdracht van de Vlaamse Overheid Bestek nr. BOD/STUD/2013/01 Contents Contents............................................................................................................................................................3 Acknowledgement ...........................................................................................................................................5 Abstract............................................................................................................................................................7 Samenvatting ...................................................................................................................................................9 1. Background and objectives.......................................................................................................................11 2. The soil map of Belgium............................................................................................................................12 2.1 The soil survey project..........................................................................................................................12 -
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. -
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. -
Soil Management Requirements KSLA November 22, 2011
Soil management requirements KSLA November 22, 2011 by Mats Olsson Department of Soil and Environment, SLU matlts.olsson@ @lslu.se Land use and land management must be sustainable That means e.g. • All ecosystem services have to be considered in a long term ppperspective Land use and land management must be sustainable That means e.g. • All ecosystem services has to be considered in a long term ppperspective • Use and management must be site adapted Soil is a diverse concept – and so is soil management Cryosols Leptosols Cambisols Arenosols Acrisols Calcisols Ferralsols Properties are set by: Gleyso ls Luvisols Podzols Kastanozems Lixisols 1. Topography Fluvisols Histosols 2. Climate Vertisols Albeluvisols Regosols 3. Geology Solonchaks Chernozems 4. Biota and land use Alisols Nitisols 5. Time Phaeozems Stagnosols Solonetz Planosols Andosols Gypsisols Umbrisols Global: 15 300 Mha Plinthosols Durisols Technosols From: World Reference Base for Anthrosols Soil Resources, 2006 Land use and land management must be sustainable That means e.g. • All ecosystem services has to be considered in a long term ppperspective • Use and management must be site adapted • A system analyses ppperspective should be applied Wheat production at different N fertilizing rates, SdSweden, k/h*kg/ha*yr From Lennart Mattsson, 2004 Wheat production at different N fertilizing rates, SdSweden, k/h*kg/ha*yr • Low margilinal impact on production • High negative environmental consequences From Lennart Mattsson, 2004 Fertilizer use, kg perha*yr Netherlands Vietnam Japan -
The Muencheberg Soil Quality Rating (SQR)
The Muencheberg Soil Quality Rating (SQR) FIELD MANUAL FOR DETECTING AND ASSESSING PROPERTIES AND LIMITATIONS OF SOILS FOR CROPPING AND GRAZING Lothar Mueller, Uwe Schindler, Axel Behrendt, Frank Eulenstein & Ralf Dannowski Leibniz-Zentrum fuer Agrarlandschaftsforschung (ZALF), Muencheberg, Germany with contributions of Sandro L. Schlindwein, University of St. Catarina, Florianopolis, Brasil T. Graham Shepherd, Nutri-Link, Palmerston North, New Zealand Elena Smolentseva, Russian Academy of Sciences, Institute of Soil Science and Agrochemistry (ISSA), Novosibirsk, Russia Jutta Rogasik, Federal Agricultural Research Centre (FAL), Institute of Plant Nutrition and Soil Science, Braunschweig, Germany 1 Draft, Nov. 2007 The Muencheberg Soil Quality Rating (SQR) FIELD MANUAL FOR DETECTING AND ASSESSING PROPERTIES AND LIMITATIONS OF SOILS FOR CROPPING AND GRAZING Lothar Mueller, Uwe Schindler, Axel Behrendt, Frank Eulenstein & Ralf Dannowski Leibniz-Centre for Agricultural Landscape Research (ZALF) e. V., Muencheberg, Germany with contributions of Sandro L. Schlindwein, University of St. Catarina, Florianopolis, Brasil T. Graham Shepherd, Nutri-Link, Palmerston North, New Zealand Elena Smolentseva, Russian Academy of Sciences, Institute of Soil Science and Agrochemistry (ISSA), Novosibirsk, Russia Jutta Rogasik, Federal Agricultural Research Centre (FAL), Institute of Plant Nutrition and Soil Science, Braunschweig, Germany 2 TABLE OF CONTENTS PAGE 1. Objectives 4 2. Concept 5 3. Procedure and scoring tables 7 3.1. Field procedure 7 3.2. Scoring of basic indicators 10 3.2.0. What are basic indicators? 10 3.2.1. Soil substrate 12 3.2.2. Depth of A horizon or depth of humic soil 14 3.2.3. Topsoil structure 15 3.2.4. Subsoil compaction 17 3.2.5. Rooting depth and depth of biological activity 19 3.2.6. -
Drained Organic Soils Under Agriculture
Geoderma 355 (2019) 113911 Contents lists available at ScienceDirect Geoderma journal homepage: www.elsevier.com/locate/geoderma Drained organic soils under agriculture — The more degraded the soil the higher the specific basal respiration T ⁎ Annelie Säuricha,1, Bärbel Tiemeyera, , Axel Dona, Sabine Fiedlerb, Michel Bechtolda,2, Wulf Amelungc, Annette Freibauera,3 a Thünen Institute of Climate-Smart Agriculture, Bundesallee 65, 38116 Braunschweig, Germany b Institute for Geography, Johannes Gutenberg-University Mainz, 55099 Mainz, Germany c University of Bonn, Institute of Crop Science and Resource Conservation, Soil Science and Soil Ecology, Nussallee 13, 53115 Bonn, Germany ARTICLE INFO ABSTRACT Handling Editor: Ingrid Kögel-Knabner Drained peatlands are hotspots of carbon dioxide (CO2) emissions from agricultural soils. As a consequence of Keywords: both drainage-induced mineralisation and anthropogenic mixing with mineral soils, large areas of former Carbon dioxide peatlands under agricultural use underwent a secondary transformation of the peat (e.g. formation of ag- Peatland agriculture gregates). These soils show contents of soil organic carbon (SOC) at the boundary between mineral and organic Heinemeyer incubation soils. However, the carbon (C) dynamics of such soils have rarely been studied so far. The aim of the present Anthropogenic disturbance study was to evaluate the vulnerability of soil organic matter (SOM) to decomposition over the whole range of − Peat-sand-mixing peat-derived soils under agriculture including very carbon rich mineral soils (76–526 g kg 1 SOC). A total of 62 soil samples covering a broad range of soil and site characteristics were selected from the sample set of the German Agricultural Soil Inventory. -
Topsoil Characterization for Sustainable Land Management 1
DRAFT FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS TOPSOIL CHARACTERIZATION FOR SUSTAINABLE LAND MANAGEMENT Land and Water Development Division Soil Resources, Management and Conservation Service Rome 1998 2 ACKNOWLEDGEMENTS This study is based upon earlier work by O.C. Spaargaren "Framework for Characterization and Classification of Topsoils in the World" (1992 unpublished) and A. Hebel "Soil Characterization and Evaluation System (SCE) with Emphasis on Topsoils and their Fertility-related Characteristics" (1994 unpublished). We would also like to acknowledge the cooperation of the University of Hohenheim, especially Dr. Gaiser and Prof. Stahr for testing the system, and various contributions, suggestions and constructive criticism received from Ms L.M. Jansen, Ms A Bot, Mr F. Nachtergaele, and last but not least, Mr M.F. Purnell. CONTENTS 1. Introduction 1 2. Topsoil Characterization Within Existing Soil Classification Systems 3 2.1 Introduction 3 2.2 Fertility Capability Classification (FCC) 3 2.3 Soil Classification Systems 3 3. Factors Influencing Topsoil Properties 7 3.1 Climate 7 3.2 Vegetation and Organic Matter 7 3.3 Topography and Physiography 8 3.4 Mineralogical Soil Constituents 9 3.5 Surface Processes 9 3.6 Biological Activity 10 3.7 Human Activity 10 4. Definition of Topsoil Properties and Modifiers 13 4.1 Texture 13 4.2 Organic Material 13 4.3 Organic Matter Status 14 4.4 Physical Features 16 4.5 Chemical Features 18 4.6 Biological Features 20 4.7 Drainage Features 21 4.8 Land Use 21 4.9 Erosion or Degradation 23 4.10 External Physical Conditions 25 4.11 Slope 26 4.12 Examples of Topsoil Characterization 26 5. -
Managing Crop Residues and Nitrogen Fertiliser to Improve Wheat Yield
Managing crop residues and nitrogen fertiliser to improve wheat yield potential in water-limited environments Thesis submitted to The University of Adelaide in fulfilment of the requirements for the degree of Doctor of Philosophy Maria del Pilar Muschietti Piana School of Agriculture, Food and Wine The University of Adelaide October 2020 TABLE OF CONTENTS Abstract…………………………………………………………………………..v Declaration……………………………………………………………………….viii Publications and presentations arising from this thesis………………………….ix Acknowledgements……………………………………………………………....xi Structure of the Thesis…………………………………………………………...xiii CHAPTER 1. General introduction and literature review Introduction………………………………………………………...................2 Drivers of wheat nitrogen demand……………………………………….5 Soil nitrogen supply for wheat crop……………………………………...9 Management of in-season nitrogen supply for wheat crop………..........18 Residues as a source of nitrogen………………………..............18 The effect of break crops on wheat yield ………………..........23 Fertiliser as a source of nitrogen…………………………..........24 Identifying the source of nitrogen available for wheat uptake using 15N-labelled techniques…………………….………………………………….……....27 Towards improved nitrogen management for wheat crop via quantification of in- season nitrogen mineralisation……………………………….................28 Research aims………………………………………………...................30 Theoretical framework and methods……………………………………31 Significance and contribution to the discipline………………………………32 References……………………………………………………………............33 ii CHAPTER 2. Combined