Influence of Soil Type on the Reliability of the Prediction Model
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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. -
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. -
Distribution of Nematodes in Vertisol Aggregates Under a Permanent Pasture in Martinique
Applied Soil Ecology ELSEVIER Applied Soil Ecology 4 (1996) 193-200 Distribution of nematodes in vertisol aggregates under a permanent pasture in Martinique Patrick Quénéhervé, Jean-Luc Chotte * Laboratoire de Nhnatologie et Laboratoire de Matière Organique des Sols Tropicaux, Centre ORSTOM, B.P. 8006,97259 Fort de France Cedex, Martinique Accepted 13 May 1996 Abstract This study reports on the distribution of nematodes in different soil habitats under a permanent pasture of digitgrass (Digitaria decuinbens Stent. cv. 'Pangola') in Martinique. The objectives were (i) to evaluate a gentle fractionation method compatible with further soil nematode extraction and (ii) to assess the respective soil microhabitats of plant-feeding nematodes and free-living nematodes. This study indicated that gentle soil fractionation can effectively separate soil habitats and allow the recovery of associated nematodes. Plant-feeding nematodes were equally distributed between inter-aggregate pores, habitats constituted of aggregated fine silt + clay particles and roots + rhizosphere. Most of free-living nematodes (53%) resided in inter-aggre- gate pores. Irrespective of the food resource, densities of nematodes (number per gram of habitat) were similar in habitats coarser than 1000 pm (A5000, A2000, and A1000). Habitats with the finest soil (A200) were not favourable sites because of the rarity of roots (for plant-feeding nematodes) and physical constraints. Keywords: Nematode; Pasture; Soil aggregates; Soil fractionation; Soil habitats; Soil porosity; Vertisol 1. Introduction indicated that carbon concentration controls the dis- tribution of soil microorganisms. Griffin (1981) Soils consist of an assemblage of solid particles demonstrated the importance of water suction in and air-filled or water-filled pores of different sizes microbial metabolism. -
Changes in Soil Properties in a Fluvisol (Calcaric) Amended with Coal Fly Ash A
Changes in soil properties in a fluvisol (calcaric) amended with coal fly ash A. Riehl, F. Elsass, J. Duplay, F. Huber, M. Trautmann To cite this version: A. Riehl, F. Elsass, J. Duplay, F. Huber, M. Trautmann. Changes in soil properties in a fluvisol (calcaric) amended with coal fly ash. Geoderma, Elsevier, 2010, 155 (1-2), pp.67-74. 10.1016/j.geoderma.2009.11.025. halsde-00546980 HAL Id: halsde-00546980 https://hal.archives-ouvertes.fr/halsde-00546980 Submitted on 30 May 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. Geoderma 155 (2010) 67–74 Contents lists available at ScienceDirect Geoderma journal homepage: www.elsevier.com/locate/geoderma Changes in soil properties in a fluvisol (calcaric) amended with coal fly ash A. Riehl a, F. Elsass b, J. Duplay a,⁎, F. Huber a, M. Trautmann c a Laboratoire d'Hydrologie et de Géochimie de Strasbourg, UMR 7517 CNRS, 1 rue Blessig 67084 Strasbourg Cedex, France b Institut National de Recherche Agronomique, route de Saint-Cyr 78026Versailles, France c UMS 830 UDS/CNRS, Laboratoire d'Analyses des Sols et des Formations Superficielles, 3 rue de l'Argonne 67083 Strasbourg Cedex, France article info abstract Article history: Fluidized bed combustion ash (FBC) is a by-product from coal-fired power stations used for many decades in Received 25 March 2009 concrete, cement and brick manufacturing and more recently for trace metal immobilization and pesticide Received in revised form 17 November 2009 retention in soils. -
Integrated Management of Vertisols for Crop Production in Ethiopia: a Review
Journal of Biology, Agriculture and Healthcare www.iiste.org ISSN 2224-3208 (Paper) ISSN 2225-093X (Online) Vol.6, No.24, 2016 Integrated Management of Vertisols for Crop Production in Ethiopia: A Review Tadesse Debele 1 Haile Deressa 2 1.Department of Plant Sciences, College of Agriculture and Veterinary Sciences, Ambo University, P.O.Box – 19, Ambo, Ethiopia 2.Deutsche Gesellschaft für Internationale Zusammenarbeit (GIZ) GmbH, P.O.Box 100009, Addis Ababa, Ethiopia Abstract In Ethiopia, Vertisols account for 12.6 million hectares, of which about 7.6 million ha found in the highlands and are generally waterlogged due to abundant rainfall during the growing period. These soils are generally hard when dry and sticky when wet, a very low infiltration rate when the surface is sealed, very low saturated hydraulic conductivity and compaction as a result of swelling, and therefore presents serious limitations to their use. Crop production on these soils is limited because of impeded drainage, difficulty of land preparation, soil erosion and low fertility. Long-term adaptations to climate changes on Vertisols management require structural changes to overcome the harsh conditions. Vertisols have considerable productive potential, but they are usually underutilized in the traditional production system. Hence, achieving sustainable and improved management of Vertisols has been a major challenge for Ethiopian farmers for many years. Vertisols management technologies essentially early planting, drainage using BBM, improved variety, and fertilizers application were developed to effectively and efficiently utilize these soils. Early planting of short maturing wheat and teff varieties opened an opportunity for double cropping; excess water drained from the furrows would be utilized for supplemental irrigation. -
Integrated Evaluation of Petroleum Impacts to Soil
Integrated Evaluation of Petroleum Impacts to Soil Randy Adams, D. Marín, C. Avila, L. de la Cruz, C. Morales, and V. Domínguez Universidad Juárez Autónoma de Tabasco, Villahermosa, Mexico [email protected] 1.00 0.90 0.80 0.70 0.60 R2 = 0.9626 0.50 0.40 1-IAFcorr 0.30 0.20 0.10 0.00 0 1000 2000 3000 4000 5000 6000 7000 8000 9000 10000 Conc. hidrocarburos (mg/Kg) Actual Modelo BACKGROUND U J A T •Clean-up criteria for petroleum contaminated soils developed in US in 60’s and 70’s on drilling cuttings •1% considered OK – no or only slight damage to crops, only lasts one growing season •Bioassays confirmed low toxicity of residual oil •Subsequenty used as a basis for clean-up criteria for hydrocarbons in soils in many countries does not consider kind of hydrocarbons does not consider kind of soil SISTEMATIC EVALUATION U J A T •Selection of light, medium, heavy and extra-heavy crudes •Selection of 5 soil types common in petroleum producing region of SE Mexico •Contamination of soil at different concentrations •Measurement of acute toxicity (Microtox), and subchronic toxicity (28 d earthworm) •Measurement of impacts to soil fertility: water repellency, soil moisure, compaction, complemented with in situ weathering experiments •Measurement of plant growth: pasture, black beans Crude Petroleum Used in Study U J A T 100% 80% 60% Aliphatics Aromatics 40% Polars + Resins Asphaltenes 20% 0% Light Crude Medium Crude Heavy Crude Extra-heavy Crude 37 ºAPI 27 ºAPI 15 ºAPI 3 ºAPI U J A T FAO: FLUVISOL VERTISOL GLEYSOL ARENOSOL ACRISOL USDA: FLUVENT -
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. -
Diagnostic Horizons
Exam III Wednesday, November 7th Study Guide Posted Tomorrow Review Session in Class on Monday the 4th Soil Taxonomy and Classification Diagnostic Horizons Epipedons Subsurface Mollic Albic Umbric Kandic Ochric Histic Argillic Melanic Spodic Plaggen Anthropic Oxic 1 Surface Horizons: Mollic- thick, dark colored, high %B.S., structure Umbric – same, but lower B.S. Ochric – pale, low O.M., thin Histic – High O.M., thick, wet, dark Sub-Surface Horizons: Argillic – illuvial accum. of clay (high activity) Kandic – accum. of clay (low activity) Spodic – Illuvial O.M. accumulation (Al and/or Fe) Oxic – highly weathered, kaolinite, Fe and Al oxides Albic – light colored, elluvial, low reactivity Elluviation and Illuviation Elluviation (E horizon) Organic matter Clays A A E E Bh horizon Bt horizon Bh Bt Spodic horizon Argillic horizon 2 Soil Taxonomy Diagnostic Epipedons Diagnostic Subsurface horizons Moisture Regimes Temperature Regimes Age Texture Depth Soil Taxonomy Soil forming processes, presence or Order Absence of major diagnostic horizons 12 Similar genesis Suborder 63 Grasslands – thick, dark Great group 250 epipedons High %B.S. Sub group 1400 Family 8000 Series 19,000 Soil Orders Entisols Histosols Inceptisols Andisols Gelisols Alfisols Mollisols Ultisols Spodosols Aridisols Vertisols Oxisols 3 Soil Orders Entisol Ent- Recent Histosol Hist- Histic (organic) Inceptisol Incept- Inception Alfisol Alf- Nonsense Ultisol Ult- Ultimate Spodosol Spod- Spodos (wood ash) Mollisol Moll- Mollis (soft) Oxisol Ox- oxide Andisol And- Ando (black) Gelisol -
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. -
The Influence of Soil Compaction on Chemical Properties of Mollic Fluvisol Soil Under Lucerne (Medicago Sativa L.)
Pol. J. Environ. Stud. Vol. 22, No. 1 (2013), 107-113 Original Research The Influence of Soil Compaction on Chemical Properties of Mollic Fluvisol Soil under Lucerne (Medicago sativa L.) Tomasz Głąb1, Krzysztof Gondek2 1Institute of Machinery Exploitation, Ergonomics and Production Processes, University of Agriculture in Kraków, Poland 2Department of Agricultural and Environmental Chemistry, University of Agriculture in Kraków, Poland Received: 28 January 2012 Accepted: 3 August 2012 Abstract The purpose of this study was to determine the effects of soil compaction on the chemical properties of soil and herbage yield of lucerne (Medicago sativa L.). A field experiment was conducted on a silty loam Mollic Fluvisols soil in 2003-07. Four compaction treatments were applied three times annually by tractor using the following number of passes: control without experimental traffic, two passes, four passes, and six passes. This study confirmed the unfavorable effect of multiple tractor passes on lucerne dry matter produc- tion. The results showed that tractor traffic reduced the yields of lucerne, particularly during the second and third harvests in each year. Soil compaction caused by tractors changed some chemical properties of soil. Tractor passes resulted in increasing pH and EC. It also increased P and Zn content. Most of these changes were statistically significant only in the deeper 20-30 cm soil layer. This effect could be ascribed to higher soil density and lower air permeability. The upper (0-20 cm) soil layer was resistant to changes in chemical prop- erties, probably due to the dense root system that recovers the soil after compaction and improves physical properties.