Development of a Spatial Model for Soil Quality Assessment Under Arid and Semi-Arid Conditions
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Digital Mapping of Soil Properties in the Western-Facing Slope of Jabal
JJEES (2020) 11 (3): 193-201 JJEES ISSN 1995-6681 Jordan Journal of Earth and Environmental Sciences Digital Mapping of Soil Properties in the Western-Facing Slope of Jabal Al-Arab at Suwaydaa Governorate, Syria Alaa Khallouf 1,4, Sami AlHinawi2, Wassim AlMesber3, Sameer Shamsham4,Younis Idries5 1General Commission for Scientific Agricultural Research (GCSAR), Damascus, Syria 2Suwayda Research Center- GCSAR, Suwayda, Syria 3Damascus University, Faculty of Agriculture, Department of Soil Science, Syria 4Al-Baath University, Faculty of Agriculture, Department of Soil and Land reclamation, Syria 5General Organization of Remote Sensing (GORS), Syria Received 28 December 2019; Accepted 10 April 2020 Abstract Digital soil mapping has been increasingly used to produce statistical models of the relationships between environmental variables and soil properties. This study aimed at determining and representing the spatial distribution of the variability in soil properties of western face-sloping of Jabal Al-Arab, Suwaydaa governorate. pH, organic matter (OM), total nitrogen (N), phosphorus (P, as P2O5), potassium (K, as K2O), iron (Fe), boron (B) and zinc (Zn) were studied, thus, Forty-five surface soil samples (0 to 30 cm) were collected and analyzed. Descriptive statistics demonstrated that most of the measured soil variables (except pH, P2O5, and Zn) were skewed and ab-normally distributed, and logarithmic transformation was then applied. Kriging was used- as geostatistical tool- in ArcGIS to interpolate observed values for those variables, and the digital map layers were produced based on each soil property. Geostatistical interpolation recognized a strong spatial variability for pH, P2O5 & Zn, moderate for OM, N, Fe & B, and weak for K2O. -
Digital Soil Mapping in the Bara District of Nepal Using Kriging Tool in Arcgis
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Agronomy & Horticulture -- Faculty Publications Agronomy and Horticulture Department 10-26-2018 Digital soil mapping in the Bara district of Nepal using kriging tool in ArcGIS Dinesh Panday University of Nebraska-Lincoln, [email protected] Bijesh Maharjan University of Nebraska-Lincoln, [email protected] Devraj Chalise Nepal Agricultural Research Council Ram Kumar Shrestha Institute of Agriculture and Animal Science, Lamjung, Nepal Bikesh Twanabasu Westfalische Wilhelms Universitat, Munster Follow this and additional works at: https://digitalcommons.unl.edu/agronomyfacpub Part of the Agricultural Science Commons, Agriculture Commons, Agronomy and Crop Sciences Commons, Botany Commons, Horticulture Commons, Other Plant Sciences Commons, and the Plant Biology Commons Panday, Dinesh; Maharjan, Bijesh; Chalise, Devraj; Shrestha, Ram Kumar; and Twanabasu, Bikesh, "Digital soil mapping in the Bara district of Nepal using kriging tool in ArcGIS" (2018). Agronomy & Horticulture -- Faculty Publications. 1130. https://digitalcommons.unl.edu/agronomyfacpub/1130 This Article is brought to you for free and open access by the Agronomy and Horticulture Department at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Agronomy & Horticulture -- Faculty Publications by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. RESEARCH ARTICLE Digital soil mapping in the Bara district of Nepal using kriging tool in ArcGIS 1 1 2 3 Dinesh PandayID *, Bijesh Maharjan , Devraj Chalise , Ram Kumar Shrestha , Bikesh Twanabasu4,5 1 Department of Agronomy and Horticulture, University of Nebraska-Lincoln, Lincoln, Nebraska, United States of America, 2 Nepal Agricultural Research Council, Lalitpur, Nepal, 3 Institute of Agriculture and Animal Science, Lamjung Campus, Lamjung, Nepal, 4 Hexa International Pvt. -
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. -
Good Practices for the Preparation of Digital Soil Maps
UNIVERSIDAD DE COSTA RICA CENTRO DE INVESTIGACIONES AGRONÓMICAS FACULTAD DE CIENCIAS AGROALIMENTARIAS GOOD PRACTICES FOR THE PREPARATION OF DIGITAL SOIL MAPS Resilience and comprehensive risk management in agriculture Inter-american Institute for Cooperation on Agriculture University of Costa Rica Agricultural Research Center UNIVERSIDAD DE COSTA RICA CENTRO DE INVESTIGACIONES AGRONÓMICAS FACULTAD DE CIENCIAS AGROALIMENTARIAS GOOD PRACTICES FOR THE PREPARATION OF DIGITAL SOIL MAPS Resilience and comprehensive risk management in agriculture Inter-american Institute for Cooperation on Agriculture University of Costa Rica Agricultural Research Center GOOD PRACTICES FOR THE PREPARATION OF DIGITAL SOIL MAPS Inter-American institute for Cooperation on Agriculture (IICA), 2016 Good practices for the preparation of digital soil maps by IICA is licensed under a Creative Commons Attribution-ShareAlike 3.0 IGO (CC-BY-SA 3.0 IGO) (http://creativecommons.org/licenses/by-sa/3.0/igo/) Based on a work at www.iica.int IICA encourages the fair use of this document. Proper citation is requested. This publication is also available in electronic (PDF) format from the Institute’s Web site: http://www.iica. int Content Editorial coordination: Rafael Mata Chinchilla, Dangelo Sandoval Chacón, Jonathan Castro Chinchilla, Foreword .................................................... 5 Christian Solís Salazar Editing in Spanish: Máximo Araya Acronyms .................................................... 6 Layout: Sergio Orellana Caballero Introduction .................................................. 7 Translation into English: Christina Feenny Cover design: Sergio Orellana Caballero Good practices for the preparation of digital soil maps................. 9 Printing: Sergio Orellana Caballero Glossary .................................................... 15 Bibliography ................................................. 18 Good practices for the preparation of digital soil maps / IICA, CIA – San Jose, C.R.: IICA, 2016 00 p.; 00 cm X 00 cm ISBN: 978-92-9248-652-5 1. -
Progressive and Regressive Soil Evolution Phases in the Anthropocene
Progressive and regressive soil evolution phases in the Anthropocene Manon Bajard, Jérôme Poulenard, Pierre Sabatier, Anne-Lise Develle, Charline Giguet- Covex, Jeremy Jacob, Christian Crouzet, Fernand David, Cécile Pignol, Fabien Arnaud Highlights • Lake sediment archives are used to reconstruct past soil evolution. • Erosion is quantified and the sediment geochemistry is compared to current soils. • We observed phases of greater erosion rates than soil formation rates. • These negative soil balance phases are defined as regressive pedogenesis phases. • During the Middle Ages, the erosion of increasingly deep horizons rejuvenated pedogenesis. Abstract Soils have a substantial role in the environment because they provide several ecosystem services such as food supply or carbon storage. Agricultural practices can modify soil properties and soil evolution processes, hence threatening these services. These modifications are poorly studied, and the resilience/adaptation times of soils to disruptions are unknown. Here, we study the evolution of pedogenetic processes and soil evolution phases (progressive or regressive) in response to human-induced erosion from a 4000-year lake sediment sequence (Lake La Thuile, French Alps). Erosion in this small lake catchment in the montane area is quantified from the terrigenous sediments that were trapped in the lake and compared to the soil formation rate. To access this quantification, soil processes evolution are deciphered from soil and sediment geochemistry comparison. Over the last 4000 years, first impacts on soils are recorded at approximately 1600 yr cal. BP, with the erosion of surface horizons exceeding 10 t·km− 2·yr− 1. Increasingly deep horizons were eroded with erosion accentuation during the Higher Middle Ages (1400–850 yr cal. -
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. -
A New Soil Quality Index (SQI) for Assessing Forest Soil Health
Soil Vital Signs: A New Soil Quality Index (SQI) for Assessing Forest Soil Health Michael C. Amacher, Katherine P. O’Neill, and Charles H. Perry May 2007 United States Forest Service Rocky Mountain Research Paper Department Research Station RMRS-RP-65WWW of Agriculture Amacher, Michael C.; O’Neil, Katherine P.; Perry, Charles H. 2007. Soil vital signs: A new Soil Quality Index (SQI) for assessing forest soil health. Res. Pap. RMRS-RP-65WWW. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 12 p. Abstract __________________________________________ The Forest Inventory and Analysis (FIA) program measures a number of chemical and physical properties of soils to address specific questions about forest soil quality or health. We developed a new index of forest soil health, the soil quality index (SQI), that integrates 19 measured physical and chemical properties of forest soils into a single number that serves as the soil’s “vital sign” of overall soil quality. Regional and soil depth differences in SQI values due to differences in soil properties were observed. The SQI is a new tool for establishing baselines and detecting forest health trends. Keywords: forest soil health, Forest Inventory and Analysis, soil indicator database, soil quality index The Authors Michael C. Amacher is a research soil scientist with the Forest and Woodland Program Area at the Forestry Sciences Laboratory in Logan, UT. He holds a B.S. and a M.S. in chemistry and a Ph.D. in soil chemistry, all from The Pennsylvania State University. He joined the Rocky Mountain Research Station in 1989. -
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 -
Sustaining the Pedosphere: Establishing a Framework for Management, Utilzation and Restoration of Soils in Cultured Systems
Sustaining the Pedosphere: Establishing A Framework for Management, Utilzation and Restoration of Soils in Cultured Systems Eugene F. Kelly Colorado State University Outline •Introduction - Its our Problems – Life in the Fastlane - Ecological Nexus of Food-Water-Energy - Defining the Pedosphere •Framework for Management, Utilization & Restoration - Pedology and Critical Zone Science - Pedology Research Establishing the Range & Variability in Soils - Models for assessing human dimensions in ecosystems •Studies of Regional Importance Systems Approach - System Models for Agricultural Research - Soil Water - The Master Variable - Water Quality, Soil Management and Conservation Strategies •Concluding Remarks and Questions Living in a Sustainable Age or Life in the Fast Lane What do we know ? • There are key drivers across the planet that are forcing us to think and live differently. • The drivers are influencing our supplies of food, energy and water. • Science has helped us identify these drivers and our challenge is to come up with solutions Change has been most rapid over the last 50 years ! • In last 50 years we doubled population • World economy saw 7x increase • Food consumption increased 3x • Water consumption increased 3x • Fuel utilization increased 4x • More change over this period then all human history combined – we are at the inflection point in human history. • Planetary scale resources going away What are the major changes that we might be able to adjust ? • Land Use Change - the world is smaller • Food footprint is larger (40% of land used for Agriculture) • Water Use – 70% for food • Running out of atmosphere – used as as disposal for fossil fuels and other contaminants The Perfect Storm Increased Demand 50% by 2030 Energy Climate Change Demand up Demand up 50% by 2030 30% by 2030 Food Water 2D View of Pedosphere Hierarchal scales involving soil solid-phase components that combine to form horizons, profiles, local and regional landscapes, and the global pedosphere. -
The Use of Proximal Soil Sensor Data Fusion and Digital Soil Mapping For
The use of proximal soil sensor data fusion and digital soil mapping for precision agriculture Wenjun Ji, Viacheslav Adamchuk, Songchao Chen, Asim Biswas, Maxime Leclerc, Raphael Viscarra Rossel To cite this version: Wenjun Ji, Viacheslav Adamchuk, Songchao Chen, Asim Biswas, Maxime Leclerc, et al.. The use of proximal soil sensor data fusion and digital soil mapping for precision agriculture. Pedometrics 2017, Jun 2017, Wageningen, Netherlands. 298 p. hal-01601278 HAL Id: hal-01601278 https://hal.archives-ouvertes.fr/hal-01601278 Submitted on 2 Jun 2020 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. Distributed under a Creative Commons Attribution - ShareAlike| 4.0 International License Abstract Book Pedometrics 2017 Wageningen, 26 June – 1 July 2017 2 Contents Evaluating Use of Ground Penetrating Radar and Geostatistic Methods for Mapping Soil Cemented Horizon .................................... 13 Digital soil mapping in areas of mussunungas: algoritmos comparission .......... 14 Sensing of farm and district-scale soil moisture content using a mobile cosmic ray probe (COSMOS Rover) .................................... 15 Proximal sensing of soil crack networks using three-dimensional electrical resistivity to- mography ......................................... 16 Using digital microscopy for rapid determination of soil texture and prediction of soil organic matter ..................................... -
Selection and Use of Soil Characteristics in Digital Soil Mapping in Tanzania
Selection and use of soil characteristics in digital soil mapping in Tanzania A M. Kilasara ASokoine University of Agriculture, P.O. Box 3008 Morogoro, Tanzania, Email [email protected], [email protected] Abstract A study of soil characteristics was conducted in three different agro-ecological zones representing the humid, sub humid and semi-arid-sub humid zones in East Africa. The selected sites correspond to high potential medium and near-marginal areas for the production of maize. Emphasis was put on the topsoil characteristics which largely influence the performance of soils in terms of crop production in the inter-tropical African region. Topsoil depth, available water capacity, organic carbon content, pH, and bulk density, cation exchange capacity are among the key characteristics that influence the functioning of the studied soils. In certain cases, a few key characteristics determine the soils behaviour while in others the same do not. The selection of which ones are critical for a given soil requires detailed analysis supported by field evidence such as experimental data. Spatial heterogeneity in magnitude of individual soil characteristics was common in all sites. In the future digital soil mapping should provide room for subsequent upgrading of the soil information as more data become available. A digital soil map should be prepared such that it provides a possibility to extract information at various resolutions according to needs. Key Words Soil characterisatiation, digital soil map. Introduction The publication of the soil map of the World in 1981 paved the way for classifying soils using a widely accepted harmonised criteria and nomenclature at the global scale. -
Soil Quality 1
START FARMINGSOIL QUALITY 1 introduction to soils Soil Quality Culman Steve ealthy soils yield healthy crops, But what is healthy soil and how do we Healthy, high-quality soil has: Hachieve it? • Good soil tilth • Sufficient depth Soil health is the foundation of productive farming practices. Fertile soil provides essential nutrients to • Sufficient, but not excessive, nutrient supply plants. Important physical characteristics of soil-like • Small population of plant pathogens and insect structures and aggregation allow water and air to pests infiltrate, roots to explore, and biota to thrive. Diverse • Good soil drainage and active biological communities help soil resist • Large population of beneficial organisms physical degradation and cycle nutrients at rates to • Low weed pressure meet plant needs. Soil health and soil quality are terms • No chemicals or toxins that may harm the crop used interchangeably to describe soils that are not • Resilience to degradation and unfavorable only fertile but also possess adequate physical and conditions biological properties to “sustain productivity, maintain —from Soil Health Training Manual environmental quality and promote plant and animal health” (Doron 1994). According to the (USDA) Natural Resource Remember, soil fertility is only one component Conservation Service, “Soil quality is how well soil does of soil quality. Fertile soils are able to provide the what we want it to do.” In order to grow our crops, we nutrients required for plant growth. These are the want the soil to hold water and nutrients like a sponge chemical components of soil. Some plants need certain where they are readily available for plant roots to take nutrients in large amounts, like nitrogen, phosphorus, them up, suppress pests and weeds that may attack and potassium, which are called macronutrients.