LAURA ANNE GERMAN the Dynamics of Terra Preta
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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. -
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. -
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. -
Effects of Biochar Application on Nitrogen Leaching, Ammonia Volatilization and Nitrogen Use Efficiency in Two Distinct Soils
Journal of Soil Science and Plant Nutrition, 2017, 17 (2), 515-528 RESEARCH ARTICLE Effects of biochar application on nitrogen leaching, ammonia volatilization and nitrogen use efficiency in two distinct soils Zunqi Liu1,2 Tianyi He1,2 Ting Cao1,2 Tiexing Yang1,2 Jun Meng2*, and Wenfu Chen1,2 1Agronomy College, Shenyang Agricultural University, Shenyang, China. 2Liaoning Biochar Engineering & Technology Research Centre, Shenyang, China. *Corresponding author: [email protected] Abstract This study was conducted to determine the effect of biochar application on nitrogen (N) leaching, ammonia (NH3) volatilization, and fertilizer N use efficiency (NUE) in two soils with different properties (loamy and sandy). Ryegrass (Lolium perenne L.) incubation experiments (with 15N-enriched urea applied) and an N loss simulation study were conducted at biochar application rates of 2% and 4%. The results showed that 15N utilization increased by 8.83–9.06% following the addition of biochar to sandy soil during the first season compared with the control. However, this significant effect was not observed in the loamy soil, in which significantly more urea-N was retained in the soil following biochar application. Furthermore, based on the results of the N leaching and NH3 volatilization experiments, 29.19% and 28.65% NO3-N leaching reductions were induced by 2% and 4% biochar amendments in loamy soil, decreasing the total inorganic N that was leached (NH4+-N plus NO3-N) by 26.46% and 26.82%, respectively. However, although the amount of leached NH4+-N decreased in biochar-amended sandy soil, the cumulative NH3 volatilizations were 14.18–20.05% higher than in the control, and 22.55% more NO3--N was leached from biochar-amended sandy soil, resulting in a negative effect on N retention. -
Paleosols Can Promote Root Growth of Recent Vegetation – a Case Study from the Sandy Soil–Sediment Sequence Rakt, the Netherlands
SOIL, 2, 537–549, 2016 www.soil-journal.net/2/537/2016/ doi:10.5194/soil-2-537-2016 SOIL © Author(s) 2016. CC Attribution 3.0 License. Paleosols can promote root growth of recent vegetation – a case study from the sandy soil–sediment sequence Rakt, the Netherlands Martina I. Gocke1,2, Fabian Kessler1, Jan M. van Mourik3, Boris Jansen4, and Guido L. B. Wiesenberg1 1Department of Geography, University of Zurich, Winterthurerstr. 190, 8057 Zurich, Switzerland 2Institute of Crop Science and Resource Conservation, University of Bonn, Nussallee 13, 53115 Bonn, Germany 3IBED-Paleoecology, University of Amsterdam, P.O. Box 94240, Amsterdam 1090 GE, the Netherlands 4IBED-Earth Surface Science, University of Amsterdam, P.O. Box 94240, Amsterdam 1090 GE, the Netherlands Correspondence to: Martina I. Gocke ([email protected]) Received: 3 November 2015 – Published in SOIL Discuss.: 14 December 2015 Accepted: 15 September 2016 – Published: 21 October 2016 Abstract. Soil studies commonly comprise the uppermost meter for tracing, e.g., soil development. However, the maximum rooting depth of various plants significantly exceeds this depth. We hypothesized that deeper parts of the soil, soil parent material and especially paleosols provide beneficial conditions in terms of, e.g., nutrient contents, thus supporting their utilization and exploitation by deep roots. We aimed to decipher the different phases of soil formation in Dutch drift sands and cover sands. The study site is located at Bedafse Bergen (south- eastern Netherlands) in a 200-year-old oak stand. A recent Podzol developed on drift sand covering a Plaggic Anthrosol that was piled up on a relict Podzol on Late Glacial eolian cover sand. -
Terras Pretas: Approaches to Formation Processes in a New Paradigm
Received: 6 April 2016 Revised: 14 June 2017 Accepted: 19 June 2017 DOI: 10.1002/gea.21647 REVIEW ARTICLE Terras pretas: Approaches to formation processes in a new paradigm Dirse Clara Kern1 Helena Pinto Lima2 Jucilene Amorim da Costa3 Herdjania Veras de Lima4 Anna Browne Ribeiro5 Bruno Marcos Moraes6 Nestor Kämpf7 1Museu Paraense Emílio Goeldi, Av. Perimetral, 1901 – Terra Firme – Telefone: 55 91 3075 6272 Abstract -Cep:66077-530–Belém-PA-Brasil,Pará, Terras pretas (Amazonian Dark Earths) are a remarkable kind of archaeological site found in the Brazil Amazon region. Rich in cultural artifacts and other occupational debris, these dark anthropogenic 2 Museu Paraense Emílio Goeldi, Pará, Brazil soil matrices are very fertile, presenting high levels of organic carbon, phosphorus, calcium, mag- 3 Universidade Federal do Amapá, Rod. Juscelino nesium, zinc, and manganese. Their high nutrient levels come from decomposed organic matter, Kubitscheck, 3296-3364 – Jardim Equatorial, including remains of fish, shellfish, game, and other refuse, while their dark color has been linked Macapá – AP,68903-419, Amapá, Brazil to residual charcoal from intentional fires associated with daily activities and landscape manage- 4Universidade Federal Rural da Amazônia, Av. Perimetral, 2501 – Terra Firme, Belém – PA, ment. Studies of anthropogenic earths in the Amazon have a deep history, as much in the geo- 66077-830, Pará, Brazil sciences as in archaeology and other historical sciences. Terras pretas have been studied as evi- 5University of Louisville, Lutz Hall Room 228, dence of a major shift in human–environment relations, but also within the lens of environmen- Louisville, Kentucky 40292 tal resiliency and sustainability. -
ANTHROSOLS Profound Changes in Soil Properties (From the Greek, Meaning Soil)
JRC Soils Atlas 24/6/05 11:32 am Page 28 The soil of Europe The major soil types of Europe Soil with subsurface accumulation of low activity clay Acid soil with a bleached horizon penetrating a clay ACRISOLS minerals and low base saturation (from the Latin, acris, ALBELUVISOLS accumulation horizon (from the Latin, albus, meaning meaning very acid). white and eluere, meaning to wash out). An Acrisol is a highly weathered soil occurring in warm temperate regions and the wetter parts Albeluvisols have an accumulation of clay in the subsoil with an irregular or broken upper of the tropics and subtropics. Acrisols have poor chemical properties, low levels of plant boundary and deep penetrations or ‘tonguing’ of bleached soil material into the illuviation nutrients, high levels of aluminium and high susceptibility to erosion. These conditions are horizon. The typical “albeluvic tongues” are generally the result of freeze-thaw processes in strong limitations for agricultural use. Acrisols are similar to the Red-Yellow Podzolic soil of periglacial conditions and often show a polygonal network in horizontal cuts. Albeluvisols occur Indonesia), Red and Yellow Earths and are related to several subgroups of Alfisols and Ultisols mainly in the moist and cool temperate regions. Also known as Podzoluvisols (FAO), Ortho- (Soil Taxonomy). podzolic soil (Russia) and several suborders of the Alfisols (Soil Taxonomy). Left: Sheet and rill erosion on Left: Albeluvisols develop Acrisols; mostly under forest vegetation; Below: a natural Acrisol profile Below: Albeluvic tongues are exposed by deep gully erosion; clearly visible penetrating the The map shows the location of bleached illuvial horizon; The areas in Europe where Acrisols map shows the location of are the dominant soil type. -
Terra Preta Ancient Amazonian Technique For
TERRA PRETA ANCIENT AMAZONIAN TECHNIQUE FOR URBAN FARMING PRESENTED IN THE GERMAN PAVILION By Xi Fang Germany presents its Pavilion at Expo 2015 as the Fields of Ideas, where a variety of innovations oriented to face the challenge of future human nutrition are showcased. The expositions concern various aspects related to food production and consumption in an urban world: soil, water, climate and biodiversity. TerraBoGa is one of the innovations promoted in the Pavilion. It is a research and project carried out in the Botanical Garden of Freie Universität Berlin, applying an ancient Amazonian agricultural technique Terra Preta, with the objective to find a universal solution for sustainable resource use and urban agriculture applicable in all around the world. TerraBoGa project uses the old Terra Preta technology, which was used by the indigenous peoples in the Amazon region centuries ago to produce very nutrient-rich humus out of sewage and other organic waste. Terra Preta (black earth) is a black soil created by humans with a much higher capacity to store water and nutrients than soils that have developed naturally. The high fertility of Terra Preta is due to more than 10 percent chemically and biologically inert carbon (charcoal-like material). There is a major difference between Terra Preta technology and conventional composting. Terra Preta technology is based on improved composting and on lactic acid fermentation using charcoal, with which, more carbon dioxide (CO2) is removed from the atmosphere for a longer period of time than in conventional composting. The highly nutrient-rich soil that is produced can be used as a substitute for fertilizer. -
Classification of Soil Systems on the Basis of Transfer Factors of Radionuclides from Soil to Reference Plants
IAEA-TECDOC-1497 Classification of soil systems on the basis of transfer factors of radionuclides from soil to reference plants Proceedings of a final research coordination meeting organized by the Joint FAO/IAEA Programme of Nuclear Techniques in Food and Agriculture and held in Chania, Crete, 22–26 September 2003 June 2006 IAEA-TECDOC-1497 Classification of soil systems on the basis of transfer factors of radionuclides from soil to reference plants Report of the final research coordination meeting organized by the Joint FAO/IAEA Programme of Nuclear Techniques in Food and Agriculture held in Chania, Crete, 22–26 September 2003 June 2006 The originating Section of this publication in the IAEA was: Food and Environmental Protection Section International Atomic Energy Agency Wagramer Strasse 5 P.O. Box 100 A-1400 Vienna, Austria CLASSIFICATION OF SOIL SYSTEMS ON THE BASIS OF TRANSFER FACTORS OF RADIONUCLIDES FROM SOIL TO REFERENCE PLANTS IAEA, VIENNA, 2006 IAEA-TECDOC-1497 ISBN 92–0–105906–X ISSN 1011–4289 © IAEA, 2006 Printed by the IAEA in Austria June 2006 FOREWORD The IAEA Basic Safety Standards for Radiation Protection include the general requirement to keep all doses as low as reasonably achievable, taking account of economic and social considerations, within the overall constraint of individual dose limits. National and Regional authorities have to set release limits for radioactive effluent and also to establish contingency plans to deal with an uncontrolled release following an accident or terrorist activity. It is normal practice to assess radiation doses to man by means of radiological assessment models. In this context the IAEA published (1994), in cooperation with the International Union of Radioecologists (IUR), a Handbook of Parameter Values for the Prediction of Radionuclide Transfer in Temperate Environments to facilitate such calculations.