Biochar Role in the Sustainability of Agriculture and Environment
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Topic: Soil Classification
Programme: M.Sc.(Environmental Science) Course: Soil Science Semester: IV Code: MSESC4007E04 Topic: Soil Classification Prof. Umesh Kumar Singh Department of Environmental Science School of Earth, Environmental and Biological Sciences Central University of South Bihar, Gaya Note: These materials are only for classroom teaching purpose at Central University of South Bihar. All the data/figures/materials are taken from several research articles/e-books/text books including Wikipedia and other online resources. 1 • Pedology: The origin of the soil , its classification, and its description are examined in pedology (pedon-soil or earth in greek). Pedology is the study of the soil as a natural body and does not focus primarily on the soil’s immediate practical use. A pedologist studies, examines, and classifies soils as they occur in their natural environment. • Edaphology (concerned with the influence of soils on living things, particularly plants ) is the study of soil from the stand point of higher plants. Edaphologist considers the various properties of soil in relation to plant production. • Soil Profile: specific series of layers of soil called soil horizons from soil surface down to the unaltered parent material. 2 • By area Soil – can be small or few hectares. • Smallest representative unit – k.a. Pedon • Polypedon • Bordered by its side by the vertical section of soil …the soil profile. • Soil profile – characterize the pedon. So it defines the soil. • Horizon tell- soil properties- colour, texture, structure, permeability, drainage, bio-activity etc. • 6 groups of horizons k.a. master horizons. O,A,E,B,C &R. 3 Soil Sampling and Mapping Units 4 Typical soil profile 5 O • OM deposits (decomposed, partially decomposed) • Lie above mineral horizon • Histic epipedon (Histos Gr. -
Dendrometric Analysis of Early Development of Eucalyptus Urophylla X Eucalyptus Grandis with Gypsum Use Under Subtropical Conditions
Floresta e Ambiente 2020; 27(1): e20190095 https://doi.org/10.1590/2179-8087.009519 ISSN 2179-8087 (online) Original Article Silviculture Dendrometric Analysis of Early Development of Eucalyptus urophylla x Eucalyptus grandis with Gypsum use Under Subtropical Conditions Carla Fernanda Ferreira1, Marcos Vinicius Martins Bassaco2 , Milena Pereira3, Volnei Pauletti3, Stephen Arthur Prior4 , Antonio Carlos Vargas Motta3 1Departamento de Agronomia, Centro de Ensino Superior dos Campos Gerais – CESCAGE, Ponta Grossa/PR, Brasil 2 Departamento de Engenharia Florestal, Faculdades FATI-FAJAR, Jaguariaíva/PR, Brasil 3Departamento de Solos e Engenharia Agrícola, Universidade Federal do Paraná – UFPR, Curitiba/PR, Brasil 4ARS National Soil Dynamics Laboratory, Auburn, USA ABSTRACT Gypsum can be used as a source for calcium (Ca) and sulphurum (S) for plants, as well as an acid, that is, a natural soil conditioner. Aiming to determine the influence of gypsum on the development of Eucalyptus urograndis in Brazil, an experiment was conducted at two locations in Paraná State. Experiments were conducted with rates of 0, 0.3, 0.6, 1.2, 2.4, 4.8 and 9.6 Mg ha-1 to verify the method of broadcast planting in a randomized block design with four repetitions. Diameter and height of plants were measured every six months and volume was determined after 36 months. There was a difference in Eucalyptus growth between the two areas, possibly related to differences in planting season and climate. Gypsum did not influence on the dendrometric growth of Eucalyptus trees. The lack of a response to gypsum, as a source of Ca, S and soil conditioner, was discussed based on soil type, Eucalyptus tolerance to soil acidity, and climatic conditions in the period evaluated. -
Soils Section
Soils Section 2003 Florida Envirothon Study Sections Soil Key Points SOIL KEY POINTS • Recognize soil as an important dynamic resource. • Describe basic soil properties and soil formation factors. • Understand soil drainage classes and know how wetlands are defined. • Determine basic soil properties and limitations, such as mottling and permeability by observing a soil pit or soil profile. • Identify types of soil erosion and discuss methods for reducing erosion. • Use soil information, including a soil survey, in land use planning discussions. • Discuss how soil is a factor in, or is impacted by, nonpoint and point source pollution. Florida’s State Soil Florida has the largest total acreage of sandy, siliceous, hyperthermic Aeric Haplaquods in the nation. This is commonly called Myakka fine sand. It does not occur anywhere else in the United States. There are more than 1.5 million acres of Myakka fine sand in Florida. On May 22, 1989, Governor Bob Martinez signed Senate Bill 525 into law making Myakka fine sand Florida’s official state soil. iii Florida Envirothon Study Packet — Soils Section iv Contents CONTENTS INTRODUCTION .........................................................................................................................1 WHAT IS SOIL AND HOW IS SOIL FORMED? .....................................................................3 SOIL CHARACTERISTICS..........................................................................................................7 Texture......................................................................................................................................7 -
Pacific Biochar What Is Biochar?
Soil Health & Carbon Farming Charlie McIntosh, Pacific Biochar What is Biochar? Biochar: biomass charcoal when used or found in soils Biochar + Soil Health SOIL ORGANIC MATTER ! Biochar is a natural component of soil organic matter ! Seasonal fires deposit biochar in soils where it accumulates over time ! People have used biochar to improve soils for millenia (ex. Terra Preta soils of the Amazon Basin) ! Fertile soils around the world often contain high levels of biochar ~30-50% of SOM Photo courtesy of Julie Major and Bruno Glaser Biochar forms a portion of the “Stabilized Organic Matter” pool in soils Biochar + Soil Health SOIL BIOLOGY ! Biochar provides an ideal micro- habitat for soil organisms ! Porous surfaces retain air, water and nutrients available for microorganisms and root hairs ! Studies consistently demonstrate enhanced biological activity in soils & composting using biochar Photo showing microstructure of biochar particle and Photo showing the organic coating formed on biochar fungal hyphae extending from spore, courtesy of Ogawa surfaces and pores, courtesy of Yoshizawa Biochar + Soil Health WATER & NUTRIENT CONSERVATION ! Biochar acts like a sponge ! Micropores retain moisture while macropores allow drainage ! Improves plant available water in sandy and heavy clay soils ! Biochar acts like a filter ! Reduces leaching & volatilization of nutrients, especially nitrogen Biochar + Compost COMPOST QUALITY ! Biochar-amended compost improves compost quality and maturity while the biochar is improved by microbe colonization and -
Artificial Chinampas Soils of Mexico City
!"#$%&$'()Chinampas)*+$(,)+-) ./0$&+)1$#23)#4/$")5"+6/"#$/,) '78)*'($7$9'#$+7):'9'"8, Suelos artificiales de chinampas de la Ciudad de México: propiedades y riesgos de salinización Solos artificiais da cidade do México - Chinampas: propriedades e riscos de salinização AUTHORS Received: 24.03.2011 Revised: 02.06.2011 Accepted: 24.06.2011 1 Ramos Bello, R. ABSTRACT García Calderón, 1 N.E. !e chinampas agriculture is a traditional land use practice in the Valley of Mexico since Pre-Hispa- nic time. !e chinampas soils were constructed by excavation of lake sediments that resulted in the Ortega Escobar, 2 H.M. creation of a system of islands separated by channels. !e agricultural productivity of these artificial soils was high; also the land use practices included forestry, fish breeding and hunting. Nowadays, 3@ Krasilnikov, P. the chinampas soils are affected by excessive salinity. We studied 10 representative soil profiles in the pavel.krasilnikov@ gmail.com chinampas zone of Mexico City in order to characterize their properties and origin, to provide their classification, and to evaluate soil salinization, vertical distribution of the salts and their chemical composition. !e soils are characterized by a layered structure, uniform dark grey colour, irregular vertical distribution of organic carbon and clay, and high percentage of carbon. Some soils show an @ Corresponding Author increase in organic matter with depth, and other profiles have maximum organic matter content in the surficial layers and in the subsoil. !e dynamics of sedimentation resulted in the decrease in 1 Facultad de Ciencias, organic matter in the upper layers of lacustrine sediments, because of recent increase in erosion rate UNAM, México. -
Opens in a New Windowguidelines for Pesticide Registration
GUIDELINES FOR PESTICIDE REGISTRATION CONTROL OF PLANTS ACT, CHAPTER 57A. Control of Plants (Registration of Pesticides) Rules. General Information A. All agricultural pesticide1 products used in the cultivation of plants intended for sale must be registered with the Singapore Food Agency (SFA).These include pesticide-containing biostimulant/fertilizer/soil conditioner. Biostimulant/fertilizer/soil conditioner which does not contain pesticide, or pesticide products for other purposes, including export, and industrial, public hygiene, landscaping and household uses, do not require registration with SFA. Pesticides used for the formulation of pesticide products also do not require registration with SFA. B. Any person who manufactures, imports, distributes, supplies or sells any pesticide products and who is conducting business in Singapore which is registered under the Business Names Registration Act 2014, or any company incorporated under the Companies Act, may apply for the registration of pesticide products for use in the agricultural farms in Singapore. C. Before applying for registration of a pesticide product with SFA, applicants are required to check whether the import of the pesticide for local use is allowed by the following agencies: i) Pollution Control Department (PCD) of the National Environment Agency (NEA) for import, export and sale of chemical pesticides that are listed as hazardous substances ii) Plant Health Services of the National Parks Board (NParks) for import of biological pesticides and organic fertilizers [Please check with NEA if you intend to register pesticides for vector control purposes.] D. If applicants are dealing with pesticides that are listed in the Environmental Protection and Management Act (EPMA), a copy of the Hazardous Substances Licence issued by the PCD/NEA must accompany the application. -
A Sustainable Approach for Improving Soil Properties and Reducing N2O Emissions Is Possible Through Initial and Repeated Biochar Application
agronomy Article A Sustainable Approach for Improving Soil Properties and Reducing N2O Emissions Is Possible through Initial and Repeated Biochar Application Ján Horák 1,* , Tatijana Kotuš 1, Lucia Toková 1, Elena Aydın 1 , Dušan Igaz 1 and Vladimír Šimanský 2 1 Department of Biometeorology and Hydrology, Faculty of Horticulture and Landscape Engineering, Slovak University of Agriculture, 949 76 Nitra, Slovakia; [email protected] (T.K.); [email protected] (L.T.); [email protected] (E.A.); [email protected] (D.I.) 2 Department of Soil Science, Faculty of Agrobiology and Food Resources, Slovak University of Agriculture, 949 76 Nitra, Slovakia; [email protected] * Correspondence: [email protected] Abstract: Recent findings of changing climate, water scarcity, soil degradation, and greenhouse gas emissions have brought major challenges to sustainable agriculture worldwide. Biochar application to soil proves to be a suitable solution to these problems. Although the literature presents the pros and cons of biochar application, very little information is available on the impact of repeated application. In this study, we evaluate and discuss the effects of initial and reapplied biochar (both in rates of 0, 10, and 20 t ha−1) combined with N fertilization (at doses of 0, 40, and 80 kg ha−1) on soil properties and N O emission from Haplic Luvisol in the temperate climate zone (Slovakia). Results showed that 2 biochar generally improved the soil properties such as soil pH(KCl) (p ≤ 0.05; from acidic towards Citation: Horák, J.; Kotuš, T.; Toková, moderately acidic), soil organic carbon (p ≤ 0.05; an increase from 4% to over 100%), soil water L.; Aydın, E.; Igaz, D.; Šimanský, V. -
Agricultural Soil Compaction: Causes and Management
October 2010 Agdex 510-1 Agricultural Soil Compaction: Causes and Management oil compaction can be a serious and unnecessary soil aggregates, which has a negative affect on soil S form of soil degradation that can result in increased aggregate structure. soil erosion and decreased crop production. Soil compaction can have a number of negative effects on Compaction of soil is the compression of soil particles into soil quality and crop production including the following: a smaller volume, which reduces the size of pore space available for air and water. Most soils are composed of • causes soil pore spaces to become smaller about 50 per cent solids (sand, silt, clay and organic • reduces water infiltration rate into soil matter) and about 50 per cent pore spaces. • decreases the rate that water will penetrate into the soil root zone and subsoil • increases the potential for surface Compaction concerns water ponding, water runoff, surface soil waterlogging and soil erosion Soil compaction can impair water Soil compaction infiltration into soil, crop emergence, • reduces the ability of a soil to hold root penetration and crop nutrient and can be a serious water and air, which are necessary for water uptake, all of which result in form of soil plant root growth and function depressed crop yield. • reduces crop emergence as a result of soil crusting Human-induced compaction of degradation. • impedes root growth and limits the agricultural soil can be the result of using volume of soil explored by roots tillage equipment during soil cultivation or result from the heavy weight of field equipment. • limits soil exploration by roots and Compacted soils can also be the result of natural soil- decreases the ability of crops to take up nutrients and forming processes. -
Terra Preta Amazonian Dark Earth Terra Preta
Terra Preta Amazonian Dark Earth Terra Preta EPi’s Carbon Char residue offers a wide variety of uses, although much of this choice is determined by the type of material to be processed and the conditions applied by the process. As a smokeless fuel it can provide high levels of energy, acting as a substitute for naturally occurring resources such as coal or gas. Although high levels of inert will have a detrimental affect to the overall calorific value of the fuel. Char created from processing plant and cellulosic material will present opportunities to convert the char into Activated Carbon, used in the air and water purification industries. But more recently, scientists around the world have become aware of its potential as a soil conditioner and fertiliser with extensive horticultural and environmental benefits. This high quality, energy rich carbon char, is the residual solid that remains after processing organic material using EPi’s unique technology. There is minimal variation in the composition of the residual char resulting from various materials treated by our process, because the organic content will always be reduced to carbon. Any volatile matter (PAH’s, VOCs & SVOCs) that may have been present within the original material, is completely destroyed by exposure to high temperatures during our process. Only the inert material remains unchanged . “Terra preta” (which means Dark Soil in Portuguese) refers to vast expanses of very dark soils found in the Amazon Basin, also known as "Amazonian Dark Earth" or "Indian Black Earth". In Portuguese its full name is “Terra preta de indio”. These soils are highly fertile and nutrient rich and it is thought that they were formed by the early Aztec and Mayan civilisations, who fertilised the land with charcoal and pottery shards, together with various plant and animal residues. -
A Review of Four Soil Amendments
Die Bodenkultur: Journal of Land Management, Food and Environment Volume 69, Issue 3, 141–153, 2018. 10.2478/boku-2018-0013 ISSN: 0006-5471 online, © De Gruyter, www.degruyter.com/view/j/boku Research Article Sustainable intensification of agricultural production: a review of four soil amendments Nachhaltige Intensivierung der landwirtschaftlichen Produktion: ein Überblick vier verschiedener Bodenzusätze Katharina Maria Keiblinger1,* Rosana Maria Kral2 1 University of Natural Resources and Life Sciences Vienna, Austria, Institute of Soil Research, Peter-Jordan-Straße 82, 1190 Vienna, Austria 2 University of Natural Resources and Life Sciences Vienna, Austria, Centre for Development Research, Peter-Jordan-Straße 82, 1190 Vienna, Austria * Corresponding author: [email protected] Received: 22 June 2018, received in revised form: 10 September 2018, accepted: 21 September 2018 Summary Dwindling natural resources, growing population pressure, climate change, and degraded soils threaten agricultural production. In order to feed the growing world population, we have to develop strategies to sustainably intensify current agricultural production while reducing the adverse effects of agriculture. Currently, a number of amendments have come into focus for improving structure and fertility of soils. Zeolites, biochar (BC), lime, and nitrification inhibitors (NIs) are reviewed for their properties. Zeolites and BC share many characteristics, such as a high cation exchange capacity (CEC), high specific surface area, and high porosity. Lime, on the other hand, works above all through its buffering capacity and can improve aggregate stability. Although the latter amend- ments change soil physicochemical characteristics, NIs do not act on soil properties but constrain a chemical/enzymatic reaction directly. These amendments are potential strategies to mitigate ongoing soil degradation and to secure soil fertility, under the global challenges. -
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. -
Agricultural Soil Carbon Credits: Making Sense of Protocols for Carbon Sequestration and Net Greenhouse Gas Removals
Agricultural Soil Carbon Credits: Making sense of protocols for carbon sequestration and net greenhouse gas removals NATURAL CLIMATE SOLUTIONS About this report This synthesis is for federal and state We contacted each carbon registry and policymakers looking to shape public marketplace to ensure that details investments in climate mitigation presented in this report and through agricultural soil carbon credits, accompanying appendix are accurate. protocol developers, project developers This report does not address carbon and aggregators, buyers of credits and accounting outside of published others interested in learning about the protocols meant to generate verified landscape of soil carbon and net carbon credits. greenhouse gas measurement, reporting While not a focus of the report, we and verification protocols. We use the remain concerned that any end-use of term MRV broadly to encompass the carbon credits as an offset, without range of quantification activities, robust local pollution regulations, will structural considerations and perpetuate the historic and ongoing requirements intended to ensure the negative impacts of carbon trading on integrity of quantified credits. disadvantaged communities and Black, This report is based on careful review Indigenous and other communities of and synthesis of publicly available soil color. Carbon markets have enormous organic carbon MRV protocols published potential to incentivize and reward by nonprofit carbon registries and by climate progress, but markets must be private carbon crediting marketplaces. paired with a strong regulatory backing. Acknowledgements This report was supported through a gift Conservation Cropping Protocol; Miguel to Environmental Defense Fund from the Taboada who provided feedback on the High Meadows Foundation for post- FAO GSOC protocol; Radhika Moolgavkar doctoral fellowships and through the at Nori; Robin Rather, Jim Blackburn, Bezos Earth Fund.