World Soil Property Estimates for Broad-Scale Modelling (Wise30sec)
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Eletrochemical Changes in Gleysol of the Amazon Estuary
http://dx.doi.org/10.4322/rca.1796 ORIGINAL ARTICLE George Rodrigues da Silva1* Paulo Augusto Lobato da Silva2 Sérgio Brazão e Silva1 Mário Lopes da Silva Junior1 Eletrochemical changes in Gleysol of the Marcos André Piedade Gama1 Antonio Rodrigues Fernandes1 Amazon estuary Alterações eletroquímicas em Gleissolo do estuário 1 Universidade Federal Rural da Amazônia – UFRA, Instituto de Ciências Agrárias, Av. Presidente Tancredo Neves, 2501, 66077-830, Belém, PA, amazônico Brasil 2 Empresa de Assistência Técnica e Extensão Rural do Estado do Pará – EMATER/PA, Rodovia BR- 316, km 12, s/n, 67105-970, Ananindeua, PA, ABSTRACT: Electrochemical reactions are intensified by soil flooding, which changes Brasil the dynamics of nutrients and negatively affects plant growth. In this work, we aimed to Corresponding Author: evaluate the changes in the redox potential (Eh), pH and nutrient availability in a Haplic E-mail: [email protected] Gleysol soil from a floodplain of the Guamá River, Belém, Pará State. During the period of floods (61 days), samples soils were collected on alternate days and analyzed in dry and wet conditions. Flooding resulted in higher pH values and decreased Eh, which stabilized after 32 days of flooding and did not affect the values of total nitrogen. An increase in the KEYWORDS Oxidation-reduction concentrations of phosphorus, sulfur, iron, manganese, copper and zinc were observed, and Availability of nutrients they were subsequently reduced with time of submergence. The reduction of sulfur occurred Waterlogged soils at low Eh and pH values near neutrality. The results show that nitrogen and sulfur do not limit agricultural production in the lowland soils of the Guamá River. -
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. -
Some Features of Soil Contamination Based on Soil Monitoring System in Slovakia
SOME FEATURES OF SOIL CONTAMINATION BASED ON SOIL MONITORING SYSTEM IN SLOVAKIA Jozef Kobza National Agricultural and Food Centre – Soil Science and Conservation Research Institute Bratislava, Regional working place Banská Bystrica, Mládežnícka 36, 974 04 Banská Bystrica, Slovakia, e-mail: [email protected] Identification of factors in relation to soil contamination 1. Natural (physical-geographical) factors include: V climatic conditions (temperature, precipitation, evapotranspiration, speed and directions of wind) V soil - lithological conditions (geology, soil type, texture, occurrence of geochemical anomalies, etc.) V vegetation (type of vegetation, rooting, etc.) V topography (slope, relief, elevation/altitude) 2. Anthropogenic factors include: V land use and farming system (crop land, grassland, forest) V use of fertilisers and organic manures V irrigation, melioration practices V other sources (sealing, mining, waste disposal, pollutant emissions) Measured risk elements in soil monitoring network in Slovakia • Cd, Pb, Cu, Zn, Ni, Cr, Se, Co, As (aqua regia) • Hg (total content, AMA 254) • Fw (watersoluble fluorine measured by ionselective electrode) Mean content of risk elements on agricultural soils in Slovakia Soils As Cd Co Cr Cu Ni Pb Zn Se Hg FM 10.8 0.7 8.8 39.1 34.0 37.0 54.3 122.8 - 0.2 ČA 10.0 0.4 7.8 42.9 22.7 29.6 21.1 75.6 0.2 0.06 ČM 10.0 0.4 7.8 42.9 22.7 29.6 21.1 75.6 0.3 0.1 HM 9.2 0.2 10.0 41.5 22.9 32.6 19.7 68.8 0.1 0.05 LM+PG 9.9 0.3 9.7 42.8 17.0 23.3 24.2 66.7 0.2 0.07 KM 14.8 0.3 12.6 52.2 28.9 29.2 27.0 -
Influence of Soil Type on the Reliability of the Prediction Model
agronomy Article Influence of Soil Type on the Reliability of the Prediction Model for Bioavailability of Mn, Zn, Pb, Ni and Cu in the Soils of the Republic of Serbia Jelena Maksimovi´c*, Radmila Pivi´c,Aleksandra Stanojkovi´c-Sebi´c , Marina Jovkovi´c,Darko Jaramaz and Zoran Dini´c Institute of Soil Science, Teodora Drajzera 7, 11000 Belgrade, Serbia; [email protected] (R.P.); [email protected] (A.S.-S.); [email protected] (M.J.); [email protected] (D.J.); [email protected] (Z.D.) * Correspondence: [email protected] Abstract: The principles of sustainable agriculture in the 21st century are based on the preservation of basic natural resources and environmental protection, which is achieved through a multidisciplinary approach in obtaining solutions and applying information technologies. Prediction models of bioavailability of trace elements (TEs) represent the basis for the development of machine learning and artificial intelligence in digital agriculture. Since the bioavailability of TEs is influenced by the physicochemical properties of the soil, which are characteristic of the soil type, in order to obtain more reliable prediction models in this study, the testing set from the previous study was grouped based on the soil type. The aim of this study was to examine the possibility of improvement in the prediction of bioavailability of TEs by using a different strategy of model development. After the training set was grouped based on the criteria for the new model development, the developed basic models were compared to the basic models from the previous study. The second step was to develop Citation: Maksimovi´c,J.; Pivi´c,R.; models based on the soil type (for the eight most common soil types in the Republic of Serbia—RS) Stanojkovi´c-Sebi´c,A.; Jovkovi´c,M.; and to compare their reliability to the basic models. -
GYPSISOLS, DURISOLS, and CALCISOLS
GYPSISOLS, DURISOLS, and CALCISOLS Otto Spaargaren ISRIC – World Soil Information Wageningen The Netherlands Definition of Gypsisols Soils having z A gypsic or petrogypsic horizon within 100cm from the soil surface z No diagnostic horizons other than an ochric or cambic horizon, an argic horizon permeated with gypsum or calcium carbonate, a vertic horizon, or a calcic or petrocalcic horizon underlying the gypsic or petrogypsic horizon Gypsic horizon Results from accumulation of secondary gypsum (CaSO4.2H2O). It contains ≥ 15 percent gypsum (if ≥ 60 percent gypsum, horizon is called hypergypsic), and has a thickness of at least 15cm. Petrogypsic horizon The petrogypsic horizon z contains ≥ 60 percent gypsum z is cemented to the extent that dry fragments do not slake in water and the horizon cannot be penetrated by roots z has a thickness of 10cm or more Genesis of Gypsisols Main soil-forming factor is: Arid climate Main soil-forming process is: – Precipitation of gypsum from the soil solution when this evaporates. Most Gypsisols are associated with sulphate-rich groundwater that moves upward in the soil through capillary action and evaporates at the surface. Classification of Gypsisols (1) z Strong expression qualifiers: hypergypsic and petric z Intergrade qualifiers: calcic, duric, endosalic, leptic, luvic, and vertic z Secondary characteristics qualifiers, related to defined diagnostic horizons, properties or materials: aridic, hyperochric, takyric, and yermic Classification of Gypsisols (2) z Secondary characteristics qualifiers, not related to defined diagnostic horizons, properties or materials: arzic, skeletic, and sodic z Haplic qualifier, where non of the above applies: haplic Example of a Gypsisol (1) Yermi-Calcic Gypsisol (Endoskeletic and Sodic), Israel 0-2cm 2-6cm 6-21cm 21-38cm 38-50cm % gypsum 50-78cm % CaCO3 78-94cm 94-126cm 126-150cm 020406080 % Example of a Gypsisol (2) Yermi-Epipetric Gypsisol, Namibia Distribution of Gypsisols (1) Distribution of Gypsisols (2) Gypsisols cover some 100M ha or 0.7 % of the Earth’s land surface. -
Management of Carbon Sequestration by Identification of Soil Limitation Factors That Affect Plants Growing
Management of Carbon Sequestration by Identification of Soil Limitation Factors That Affect Plants Growing Ziba Nalbandi Ghareghiye Abstract Organic matter plays an important role in many soil properties. So it is necessary to identify management systems which maintain or increase its concentrations. Different types of soil with its cover plants have different potential in carbon sequestration. For this goal, four sites with different soils (Saline soil, Gypsisol, Calcic soil, Forest Acidic soil) and their vegetation have been studied. In each sites, 12 to 15 points were sampled and analyzed some relative factors that reflect crucial characteristics of each soil. The results show that EC, gypsum and lime are limited factors in arid and semi-arid sites and only tolerant plant as Halophytes and Gypsophytes can be stable. Also, in forest site, soil acidic condition shows limiting for plants growth more than climatic factors. But the amount of growing plants in arid and semi-arid sites depends on climatic factors Mostly. Therefore, identification of limitation factors of soil for different ecosystems can be help to manage their vegetation cover that adjusted the different soil conditions for carbon stocks. Keyword: Sequestration; Gypsisol; Calcic; Acidic; Halophytes; Gypsophytes; Published Date: 7/31/2019 Page.538-562 Vol 7 No 7 2019 DOI: https://doi.org/10.31686/ijier.Vol7.Iss7.1574 International Journal of Innovation Education and Research www.ijier.net Vol:-7 No-7, 2019 Management of Carbon Sequestration by Identification of Soil Limitation Factors That Affect Plants Growing Ziba Nalbandi Ghareghiye1: Post-Doctorate student at Atlantic International University (AlU)2 1: E-mail address of corresponding, [email protected] 2: Address of university: Pioneer Plaza, 900 Fort Street Mall 410, Honolulu, HI 96813 Tell: +989917804975 Abstract Organic matter plays an important role in many soil properties. -
Redalyc.Quaternary Pedostratigraphy of the Nevado De Toluca Volcano
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Solleiro Rebolledo, Elizabeth; Macías, José Luis; Gama Castro, Jorge Enrique; Sedov, Sergey; Sulerzhitsky, Leopold D. Quaternary pedostratigraphy of the Nevado de Toluca volcano Revista Mexicana de Ciencias Geológicas, vol. 21, núm. 1, 2004, pp. 101-109 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57221112 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de Ciencias Geológicas,Quaternary v. 21 pedostratigraphy núm. 1, 2004, p. of101-109 the Nevado de Toluca volcano 101 Quaternary pedostratigraphy of the Nevado de Toluca volcano Elizabeth Solleiro-Rebolledo1,*, José Luis Macías2, Jorge Gama-Castro1, Sergey Sedov1, and Leopold D. Sulerzhitsky3 1 Instituto de Geología, 2 Insituto de Geofísica, Universidad Nacional Autónoma de México, Cd. Universitaria, 04510 México, D.F., Mexico 3 Geological Institute, Russian Academy of Sciences,Pyzhevsky 7, 119017 Moscow, Russia * [email protected] ABSTRACT Paleosol sequences of the Nevado de Toluca volcano (NTV) preserve a detailed record of late Quaternary environmental change. In fact, some studies have been used the NTV paleosols to interpret paleoenvironmental conditions, however some uncertainties still remain concerning their stratigraphic position and correlation. In this paper, we present the results of the NTV pedostratigraphy by using different paleosol units and based on present day tephrostratigraphy. We recognized eight Pleistocene paleosols, labeled PT0–PT7 which cover the 100,000–10,000 yr BP interval. -
Detachment of Soil Organic Carbon by Rainfall Splash: Experimental Assessment on Three Agricultural Soils of Spain
Detachment of soil organic carbon by rainfall splash: experimental assessment on three agricultural soils of Spain Santiago Beguer´ıa∗ Estaci´onExperimental de Aula Dei (EEAD-CSIC), 1005 Avda. Monta~nana,Zaragoza, Spain Marta Angulo-Mart´ınez Department of Civil and Environmental Engineering, Pratt School for Engineering, Duke University, Durham, NC Leticia Gaspar Environmental Science Program, University of Northern British Columbia, 3333 University Way, Prince George, British Columbia, V2N 4Z9, Canada Ana Navas Estaci´onExperimental de Aula Dei (EEAD-CSIC), 1005 Avda. Monta~nana,Zaragoza, Spain Abstract An experiment was undertaken to measure the concentration of soil organic carbon (SOC) in particles mobilized by rainfall splash under natural precip- itation and to assess its relationship with soil and precipitation properties. Splash cups were deployed on three agricultural soils typical of the central Ebro Valley in Spain (a Cambisol, a Gypsisol, and a Solonchak), and the rainfall characteristics (intensity, kinetic energy) were measured by means of ∗Corresponding author Email address: [email protected] (Santiago Beguer´ıa) Preprint submitted to Geoderma Thursday 8th January, 2015 a disdrometer (optical spectro-pluviometer). Evidences of SOC enrichment, i.e. a significantly higher concentration in the splashed material with respect to the parent material, were found in the three soils under study. Differ- ences were found, too, between two particle size fractions (less than 0.05 mm and between 0.05 and 0.5 mm), with higher SOC enrichment in the coarsest fraction. While the amount of splash was clearly related to the erosivity of each rainfall event, no significant effect was found with respect to the SOC concentration. -
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.