Use of Biochar-Compost for Phosphorus Availability to Maize in a Concretionary Ferric Lixisol in Northern GHANA
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Phosphorus Biofertilizers from Ash and Bones—Agronomic Evaluation of Functional Properties
Journal of Agricultural Science; Vol. 8, No. 6; 2016 ISSN 1916-9752 E-ISSN 1916-9760 Published by Canadian Center of Science and Education Phosphorus Biofertilizers from Ash and Bones—Agronomic Evaluation of Functional Properties Magdalena Jastrzębska1, Marta K. Kostrzewska1, Kinga Treder1, Wiesław P. Jastrzębski2 & Przemysław Makowski1 1 Department of Agroecosystems, University of Warmia and Mazury in Olsztyn, Olsztyn, Poland 2 Department of Botany and Nature Protection, University of Warmia and Mazury in Olsztyn, Olsztyn, Poland Correspondence: Magdalena Jastrzębska, Department of Agroecosystems, University of Warmia and Mazury in Olsztyn, Plac Łódzki 3, Olsztyn 10-718, Poland. Tel: 48-89-523-4829. E-mail: [email protected] Received: March 16, 2016 Accepted: April 25, 2016 Online Published: May 15, 2016 doi:10.5539/jas.v8n6p58 URL: http://dx.doi.org/10.5539/jas.v8n6p58 Abstract Renewable raw materials could be a valuable source of phosphorus for plants. The bioavailability of this element can be enhanced by phosphorus-solubilizing bacteria. Suspension biofertilizers have been produced from sewage sludge ash and animal bones and enriched with the bacteria Bacillus megaterium. The functional properties of these preparations were compared in field experiments (northeast Poland, 2014, four replications) on spring wheat (Triticum aestivum ssp. vulgare Mac Key) to conventional fertilizers (superphosphate, phosphorite), ash-water solution (without microorganisms) and a control treatment without P fertilization. The soil type and cultivation regime were adjusted to the requirements of spring wheat in line with good agricultural practice. The effects of biofertilizers on the following were investigated: wheat yield, ear density, number of grains in the ear, the weight of 1000 grains, harvest index, weed infestation, the weight and structure of crop residues, and the pH of soil. -
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 Organic Matter As Sole Indicator of Soil Degradation
Environ Monit Assess (2017) 189:176 DOI 10.1007/s10661-017-5881-y Soil organic matter as sole indicator of soil degradation S.E. Obalum & G.U. Chibuike & S. Peth & Y. Ouyang Received: 27 July 2016 /Accepted: 7 March 2017 # Springer International Publishing Switzerland 2017 Abstract Soil organic matter (SOM) is known to play properties as well. Thus, functions of SOM almost al- vital roles in the maintenance and improvement of many ways affect various soil properties and processes and soil properties and processes. These roles, which largely engage in multiple reactions. In view of its role in soil influence soil functions, are a pool of specific contribu- aggregation and erosion control, in availability of plant tions of different components of SOM. The soil func- nutrients and in ameliorating other forms of soil degra- tions, in turn, normally define the level of soil degrada- dation than erosion, SOM has proven to be an important tion, viewed as quantifiable temporal changes in a soil indicator of soil degradation. It has been suggested, that impairs its quality. This paper aims at providing a however, that rather than the absolute amount, temporal generalized assessment of the current state of knowl- change and potential amount of SOM be considered in edge on the usefulness of SOM in monitoring soil its use as indicator of soil degradation, and that SOM degradation, based on its influence on the physical, may not be an all-purpose indicator. Whilst SOM re- chemical and biological properties and processes of mains a candidate without substitute as long as a one- soils. -
Seção V - Gênese, Morfologia E Classificação Do Solo
EVALUATION OF MORPHOLOGICAL, PHYSICAL AND CHEMICAL CHARACTERISTICS... 573 SEÇÃO V - GÊNESE, MORFOLOGIA E CLASSIFICAÇÃO DO SOLO EVALUATION OF MORPHOLOGICAL, PHYSICAL AND CHEMICAL CHARACTERISTICS OF FERRALSOLS AND RELATED SOILS(1) E. KLAMT(2) & L. P. VAN REEUWIJK(3) SUMMARY Morphological, physical and chemical data of 58 soil profiles of Ferralsols and low activity clay Cambisols, Lixisols, Acrisols and Nitisols and of Alisols of the International Soil Reference and Information Centre (ISRIC) collection, described and sampled in eighteen different countries of tropical and subtropical regions, were selected to analyse their consistency and, or, variability and to search for properties to better describe and differentiate them. The soil profile descriptions were based on the guidelines of FAO and the FAO endorsed analytical methods of ISRIC. Frequence diagrams of the data show an asymmetric positively skewed and leptokurtic distribution for sand and silt fractions, specific surface, exchangeable bases and cation exchange capacity. Clustering soil colour hues, values and chromas rendered four distinct clusters, respectively of Rhodic, Rhodic/Xanthic (Haplic), Xanthic and Humic properties. The same technique applied to particle size distribution also originated four clusters, respectively of fine loamy, fine silty, clayey and fine clayey soils. Most of the soils analysed are acid, with low base saturation, except for Rhodic Nitisols and Rhodic Ferralsols, which present low exchangeable aluminium. Higher and variable values of this property are found in the other soil classes studied. Cation exchange capacity is also low and related to the kaolinitic and oxihydroxydic composition of the clay material. Regression analysis applied to cation exchange capacity resulted in low correlations with clay and silt content and higher with organic carbon and specific surface and clay content. -
Soil Classification Based on Spectral and Environmental Variables
https://doi.org/10.5194/soil-2019-77 Preprint. Discussion started: 20 November 2019 c Author(s) 2019. CC BY 4.0 License. Soil classification based on spectral and environmental variables Andre Carnieletto Dotto1, Jose A. M. Demattê1, Raphael Viscarra Rossel2, and Rodnei Rizzo1 1Department of Soil Science, College of Agriculture Luiz de Queiroz, University of São Paulo, Piracicaba, SP, 13418-900, Brazil 2School of Molecular and Life Sciences, Curtin University, Perth, WA, 6102, Australia Correspondence: Jose A. M. Demattê ([email protected]) Abstract. Given the large volume of soil data, it is now possible to obtain a soil classification using spectral, climate and terrain attributes. The idea was to develop a soil series system, which intends to discriminate soil types according to several variables. This new system was called Soil-Environmental Classification (SEC). The spectra data was applied to obtain information about the soil and climate and terrain variables to simulate the pedologist knowledge in soil-environment interactions. The most 5 appropriate numbers of classes were achieved by the lowest value of AIC applying the clusters analysis, which was defined with 8 classes. A relationship between the SEC and WRB-FAO classes was found. The SEC facilitated the identification of groups with similar characteristics using not only soil but environmental variables for the distinction of the classes. Finally, the conceptual characteristics of the 8 SEC were described. The development of SEC conducted to incorporate applicable soil data for agricultural management, with less interference of personal/subjective/empirical knowledge (such as traditional taxonomic 10 systems), and more reliable on automation measurements by sensors. -
Prediction of Soil Properties for Agricultural and Environmental Applications from Infrared and X-Ray Soil Spectral Properties
Institute of Plant Production and Agroecology in the Tropics and Subtropics University of Hohenheim Field: Global Food Security Prof. Dr. Georg Cadisch (Supervisor) Prediction of soil properties for agricultural and environmental applications from infrared and X-ray soil spectral properties Dissertation Submitted in fulfillment of the requirements for the degree "Doktor der Agrarwissenschaften" (Dr.sc.agr. / Ph.D. in Agricultural Sciences) to the Faculty of Agricultural Sciences presented by Towett, Erick Kibet Born on October 3 rd 1981 in Kericho, Kenya 2013 This thesis was accepted as a doctoral dissertation in fulfillment of the requirements for the degree "Doktor der Agrarwissenschaften” by the Faculty of Agricultural Sciences at University of Hohenheim on 31/10/2013 Date of oral examination: 09/12/2013 Examination Committee Supervisor and Review: Prof. Dr. Georg Cadisch Co-Reviewer: Prof. Dr. Torsten Müller Additional examiners: Prof. Dr. Karl Stahr Head of the Committee: Prof. Dr.-Ing. Stefan Böttinger. i Contents Abbreviations and acronyms .......................................................................................................v 1.0 Introduction to the thesis .......................................................................................................2 1.1 Background and rationale....................................................................................................2 1.2 Overview of soils in African context ...................................................................................3 -
Application of the Crystallinity Ratio of Free Iron Oxides for Dating Soils
第 四 紀 研 究(The Quaternary Research)41(16)p.485-493 Dec. 2002 Application of the Crystallinity Ratio of Free Iron Oxides for Dating Soils Developed on the Raised Coral Reef Terraces of Kikai and Minami-Daito Islands, Southwest Japan Yuji Maejima*1, Shizuo Nagatsuka*2 and Teruo Higashi*3 Absolute ages of soils developed on the raised coral reef terraces in Kikai Island in the Ryukyus, Southwest Japan were estimated by using the mean rate of tectonic up- lift and glacio-eustatic curve during late Quaternary in the previous paper. In order to estimate the soil age of other areas where the similar soils as those existed in Kikai Island were formed by using the index of soil age, which was highly correlated with some physico-chemical properties of soil itself, total iron (Fet), iron and aluminum extractable by dithionite-citrate (Fed, Ald) and by acid ammonium oxalate (Feo, Alo) were determined for all horizons of the six profiles in Kikai Island. The results obtained are as follows: The crystallinity ratio of free iron oxides [(Fed-Feo)/Fet] gradually increased with the stage of soil development, while the activity ratio (Feo/Fed) decreased. There was a highly positive correlation between the soil age and (Fed-Feo)/Fet. By using this relationship, the ages of Minami-Daito Island soils, Lateritic Red soil and Lateritic Yellow soil whose age had not been determined, were estimated from the mean values of (Fed-Feo)/Fet, as 500±60 ka and 630±110ka, respectively. Therefore, it was concluded that the crystallinity ratio of free iron oxides could be a good index of the degree of soil development and age of Red-colored soils. -
Phosphate Solubilizing Microbes: Sustainable Approach for Managing
Sharma et al. SpringerPlus 2013, 2:587 http://www.springerplus.com/content/2/1/587 a SpringerOpen Journal REVIEW Open Access Phosphate solubilizing microbes: sustainable approach for managing phosphorus deficiency in agricultural soils Seema B Sharma1*, Riyaz Z Sayyed2, Mrugesh H Trivedi1 and Thivakaran A Gobi3 Abstract Phosphorus is the second important key element after nitrogen as a mineral nutrient in terms of quantitative plant requirement. Although abundant in soils, in both organic and inorganic forms, its availability is restricted as it occurs mostly in insoluble forms. The P content in average soil is about 0.05% (w/w) but only 0.1% of the total P is available to plant because of poor solubility and its fixation in soil (Illmer and Schinner, Soil Biol Biochem 27:257-263, 1995). An adequate supply of phosphorus during early phases of plant development is important for laying down the primordia of plant reproductive parts. It plays significant role in increasing root ramification and strength thereby imparting vitality and disease resistance capacity to plant. It also helps in seed formation and in early maturation of crops like cereals and legumes. Poor availability or deficiency of phosphorus (P) markedly reduces plant size and growth. Phosphorus accounts about 0.2 - 0.8% of the plant dry weight. To satisfy crop nutritional requirements, P is usually added to soil as chemical P fertilizer, however synthesis of chemical P fertilizer is highly energy intensive processes, and has long term impacts on the environment in terms of eutrophication, soil fertilility depletion, carbon footprint. Moreover, plants can use only a small amount of this P since 75–90% of added P is precipitated by metal–cation complexes, and rapidly becomes fixed in soils. -
THE EFFECTS of PHOSPHORUS DEFICIENCY and RHIZOBACTERIA on PHOSPHORUS CONTENTS of TWO SOYBEAN (Glycine Max L.) CULTIVARS GROWN at LOW WATER SUPPLY
Scientific Papers. Series A. Agronomy, Vol. LVII, 2014 ISSN 2285-5785; ISSN CD-ROM 2285-5793; ISSN Online 2285-5807; ISSN-L 2285-5785 THE EFFECTS OF PHOSPHORUS DEFICIENCY AND RHIZOBACTERIA ON PHOSPHORUS CONTENTS OF TWO SOYBEAN (Glycine max L.) CULTIVARS GROWN AT LOW WATER SUPPLY Vladimir ROTARU1, Simion TOMA1, Ana BIRSAN2 1Institute of Genetics, Physiology and Plant Protection, Moldavian Academy of Sciences 20 Padurii str., MD 2002, Chisinau, Republic of Moldova 2State University of Moldova, 60 Mateevici str., MD 2009, Chisinau, Republic of Moldova Corresponding author email: [email protected] Abstract Phosphorus (P) deficiency and low water supply are major environmental constraints for agricultural production in many regions. Compared to cereal crops, the soybean (Glycine max.L.) is more susceptible to phosphorus insufficiency and drought. A soil pot experiment was conducted in the greenhouse to investigate the effects of phosphorus deficiency and pseudomonas florescence and azotobacter chroococcum strains on phosphorus uptake by soybean grown under temporary drought conditions. Soybean cultivars Zodiac and Horboveanca were grown on soil-sand mixture with P deficiency at two water regimes - 70% water holding capacity of soil (WHC) and 35% WHC. Plants were harvested and analyzed for P contents in each organ after 12 days of water deficit at the setting pod stage. Phosphorus deficiency significantly decreased nutrient uptake by all plant parts especially in drought conditions. Leaves have shown a higher sensitivity to P deficiency than roots. Application of rhizobacteria induced P uptake in both cultivars but their effects were more pronounced in Horboveanca under both well watered and dry soil conditions. Phosphorus fertilization alone of plants significantly increased P accumulation irrespective of soil moisture regime and Horboveanca displayed a higher response than Zodiac cultivar. -
Lunnyu Soils in the Lake Victoria Basin of Uganda: Link to Toposequence and Soil Type
African Journal of Environmental Science and Technology Vol. 5(1), pp. 15 - 24, January 2011 Available online at http://www.academicjournals.org/AJEST ISSN 1996-0786 ©2011 Academic Journals Full Length Research Paper Lunnyu soils in the Lake Victoria basin of Uganda: Link to toposequence and soil type Fungo B. 1* , Grunwald S. 2, Tenywa M. M.3, Vanlauwe B. 4 and Nkedi-Kizza P. 2 1Department of Forest Biology and Ecosystems Management, Faculty of Forestry and Nature Conservation, Makerere University, Kampala-Uganda 2Soil and Water Science Department, Institute of Food and Agricultural Science, University of Florida, Geinsville, Florida, USA. 3Makerere University Agricultural Research Institute, Kabanyolo, Kampala-Uganda. 4Tropical Soil Biology and Fertility (TSBF) International Center for Tropical agriculture (CIAT), Nairobi, Kenya. Accepted 6 December, 2010 We compared the physico-chemical characteristics of Lunnyu soils using soil type and slope position in order to explain their variability in the Lake Victoria basin of Uganda. Lunnyu patches located on four different soil types (chromic lixisol, mollic gleysols and plinthic ferralsols) were selected. At each patch, the slope was divided into shoulder, back-slope and foot-slope. Five locations along the contour of each landscape position and at distance of 20 to 30 m were located and soil samples taken at two depths (0 to 20 cm and 20 to 40 cm). The soils were analyzed for pH, available P, texture, and exchangeable bases. Lunnyu patches on chromic lixisol and mollic gleysols had higher pH, P, sand, clay and silt compared to those on plinthic ferralsols and petrifferic lixisol. Neither of the soil properties was influenced by landscape position. -
Adsorption of Heavy Metals on Soil Collected from Lixisol of Typical Karst Areas in the Presence of Caco3 and Soil Clay and Their Competition Behavior
sustainability Article Adsorption of Heavy Metals on Soil Collected from Lixisol of Typical Karst Areas in the Presence of CaCO3 and Soil Clay and Their Competition Behavior 1, 2, 2 3 4, Guandi He y, Zhenming Zhang y , Xianliang Wu , Mingyang Cui , Jiachun Zhang * and Xianfei Huang 5,* 1 The Key Laboratory of Plant Resources Conservation and Germplasm Innovation in Mountainous Region (Ministry of Education), Institute of Agro-Bioengineering and College of Life Sciences, Guizhou University, Guiyang 550025, China; [email protected] 2 Guizhou Institute of Biology, Guizhou Academy of Sciences, Guiyang 550009, China; [email protected] (Z.Z.); [email protected] (X.W.) 3 College of Life Science, Guizhou University, Guiyang 550025, China; [email protected] 4 Guizhou Botanical Garden, Guizhou Academy of Sciences, Guiyang 550004, China 5 Guizhou Provincial Key Laboratory for Information Systems of Mountainous Areas and Protection of Ecological Environment, Guizhou Normal University, Guiyang 550001, China * Correspondence: [email protected] (J.Z.); [email protected] (X.H.) These authors contributed equally to this work. y Received: 8 July 2020; Accepted: 1 September 2020; Published: 7 September 2020 Abstract: The content of heavy metals in the soil in Guizhou Province, which is a high-risk area for heavy metal exposure, is significantly higher than that in other areas in China. Therefore, the objective of this study was to evaluate the ability of CaCO3 and clay to accumulate heavy metals in topsoil sample collected from Lixisol using the method of indoor simulation. The results showed that the contents of Cu, Zn, Cd, Cr, Pb, Hg and As in the soil sample were 10.8 mg/kg, 125 mg/kg, 0.489 mg/kg, 23.5 mg/kg, 22.7 mg/kg, 58.3 mg/kg and 45.4 mg/kg, respectively. -
Essential Nutrients for Plant Growth: Nutrient Functions and Deficiency Symptoms
Plant Nutrient Management in Hawaii’s Soils From: Plant Nutrient Management in Hawaii’s Soils, Approaches for Tropical and Subtropical Agriculture J. A. Silva and R. Uchida, eds. College of Tropical Agriculture and Human Resources, University of Hawaii at Manoa, ©2000 Chapter 3 Essential Nutrients for Plant Growth: Nutrient Functions and Deficiency Symptoms R. Uchida lants, like all other living things, need food for their their function in plants, symptoms of their deficien- Pgrowth and development. Plants require 16 essen- cies, and recommended nutrient levels in plant tissues tial elements. Carbon, hydrogen, and oxygen are de- of selected crops. rived from the atmosphere and soil water. The remain- ing 13 essential elements (nitrogen, phosphorus, po- Nitrogen – tassium, calcium, magnesium, sulfur, iron, zinc, man- symbol: N; available to plants as nitrate (NO3 ) , and + ganese, copper, boron, molybdenum, and chlorine) are ammonium (NH4 ) ions. supplied either from soil minerals and soil organic Nutrient functions matter or by organic or inorganic fertilizers. N is biologically combined with C, H, O, and S to For plants to utilize these nutrients efficiently, light, • create amino acids, which are the building blocks of heat, and water must be adequately supplied. Cultural proteins. Amino acids are used in forming proto- practices and control of diseases and insects also play plasm, the site for cell division and thus for plant important roles in crop production. growth and development. Each type of plant is unique and has an optimum Since all plant enzymes are made of proteins, N is nutrient range as well as a minimum requirement level. • needed for all of the enzymatic reactions in a plant.