Biochar News by Country

Brazil

  • The ceramic artifacts in archaeological black earth (terra preta) from lower Amazon region, Brazil: Mineralogy
    Marcondes Lima da Costa, Dirse Clara Kern, Alice Helena Eleotério Pinto, Jorge Raimundo da Trindade Souza, Acta Amazonica. vol.34 no.2 Manaus 2004

    ABSTRACT

    Several archaeological black earth (ABE) sites occur in the Amazon region. They contain fragments of ceramic artifacts, which are very important for the archaeological purpose. In order to improve the archaeological study in the region we carried out a detailed mineralogical and chemical study of the fragments of ceramic artifacts found in the two ABE sites of Cachoeira-Porteira, in the Lower Amazon Region. Their ceramics comprise the following tempers: cauixi, cariapé, sand, sand +feldspars, crushed ceramic and so on and are composed of quartz, clay equivalent material (mainly burned kaolinite), feldspars, hematite, goethite, maghemite, phosphates, anatase, and minerals of Mn and Ba. Cauixi and cariapé, siliceous organic compounds, were found too. The mineralogical composition and the morphology of their grains indicate a saprolite (clayey material rich on quartz) derived from fine-grained felsic igneous rocks or sedimentary rocks as source material for ceramic artifacts, where silica-rich components such cauixi, cariapé and/or sand (feldspar and rock fragments) were intentionally added to them. The high content of (Al,Fe)-phosphates, amorphous to low crystalline, must be product of the contact between the clayey matrix of pottery wall and the hot aqueous solution formed during the daily cooking of animal foods (main source of phosphor). The phosphate crystallization took place during the discharge of the potteries put together with waste of organic material from animal and vegetal origin, and leaving to the formation of the ABE-soil profile.

  • I INTERNATIONAL WORKSHOP ON ANTHROPOGENIC TERRA PRETA SOILS [NOVOTEL], MANAUS, BRAZIL, 13-19 JULY 2002.
    Organized by INPA, EMBRAPA, UA, MPEG, USP

    Program

    Publications

  • Black Carbon Increases Cation Exchange Capacity in Soils
    Liang et al. Soil Sci Soc Am J.2006; 70: 1719-1730

    Authors:
    B. Liang, J. Lehmann, D. Solomon, J. Kinyangi, J. Grossman, B. O'Neill, J. O. Skjemstad, J. Thies, F. J. Luizão, J. Petersen and E. G. Neves

    Abstract:

    Black Carbon (BC) may significantly affect nutrient retention and play a key role in a wide range of biogeochemical processes in soils, especially for nutrient cycling. Anthrosols from the Brazilian Amazon (ages between 600 and 8700 yr BP) with high contents of biomass-derived BC had greater potential cation exchange capacity (CEC measured at pH 7) per unit organic C than adjacent soils with low BC contents. Synchrotron-based near edge X-ray absorption fine structure (NEXAFS) spectroscopy coupled with scanning transmission X-ray microscopy (STXM) techniques explained the source of the higher surface charge of BC compared with non-BC by mapping cross-sectional areas of BC particles with diameters of 10 to 50 µm for C forms. The largest cross-sectional areas consisted of highly aromatic or only slightly oxidized organic C most likely originating from the BC itself with a characteristic peak at 286.1 eV, which could not be found in humic substance extracts, bacteria or fungi. Oxidation significantly increased from the core of BC particles to their surfaces as shown by the ratio of carboxyl-C/aromatic-C. Spotted and non-continuous distribution patterns of highly oxidized C functional groups with distinctly different chemical signatures on BC particle surfaces (peak shift at 286.1 eV to a higher energy of 286.7 eV) indicated that non-BC may be adsorbed on the surfaces of BC particles creating highly oxidized surface. As a consequence of both oxidation of the BC particles themselves and adsorption of organic matter to BC surfaces, the charge density (potential CEC per unit surface area) was greater in BC-rich Anthrosols than adjacent soils. Additionally, a high specific surface area was attributable to the presence of BC, which may contribute to the high CEC found in soils that are rich in BC.

  • SOLOS DE TERRA PRETA PODEM SER SOLUÇÃO PARA A AGRICULTURA NA AMAZÔNIA

    Pesquisadores de vários países correm contra o tempo para descobrir como se formou
    um dos solos mais férteis do mundo: a Terra Preta Arqueológica
    http://www.museu-goeldi.br/destaqueamazonia/tpa.htm
    Até onde se sabe, os solos de terra preta arqueológica existem principalmente na Amazônia. Extremamente fértil, a terra preta está derrubando o mito de que os solos da região são pobres e impróprios para a agricultura.

  • Isolating Unique Bacteria from Terra Preta Systems: Using Culturing and Molecular Tools for Characterizing Microbial Life in Terra Preta
    O'Neill, Brendan Grossman, Julie Tsai, S.M. Gomes, Jose Elias Garcia, Carlos Eduardo Solomon, Dawit Liang, Biqing Lehmann, Johannes Thies, Janice
    Poster presentation from the 2006 World Congress of Soil Science in Philadelphia, PA
    16-Aug-2006

    The greater fertility of Terra Preta (TP) soils is thought to be due to their high black carbon (BC) content, which contributes to increased nutrient and moisture retention, and increased pH.

  • Green Charcoal by Pronatura International, France

    Two billion people around the world use wood for household energy needs. This contributes significantly to the world's deforestation activities as well as increasing the risk of droughts and desertification. In an attempt to reduce deforestation, Pro-Natura has developed Green-Charcoal.

  • Black C Effects on the Biogeochemical Cycling of Soil Nutrients and Organic C in Amazonian Dark Earths (Terra Preta De Indo)
    Biqing Liang, Graduate Student, Department of Crop and Soil Sciences, Cornell University, 9/21/2006,Crop and Soil Sciences Seminar Series, Cornell University. College of Agriculture and Life Sciences.

    Abstract:

  • Charcoal as Soil Conditioner Studies in the humid Tropics
    Christoph Steiner1, W. G. Teixeira2, J. Lehmann3and W. Zech1

    1Institute of Soil Science, University of Bayreuth, Germany
    2EmbrapaAmazoniaOcidental, Manaus, Brazil
    3 Department of Crop and Soil Sciences, Cornell University, USA

  • Long term Effects of manure, charcoal and mineral fertilization on crop production and fertility on a highly weathered Central Amazonian upland soil January 2007
    Christoph Steiner · Wenceslau G. Teixeira · Johannes Lehmann ·Thomas Nehls · Jeferson Luis Vasconcelos de Macêdo · Winfried E. H. Blum · Wolfgang Zech

    Abstract

  • Cornell University: Bio-Char Projects 2007

    Bio-char Projects

    Currently (January 2007) we conduct experiments to evaluate the effects of bio-char on nutrient adsorption, nutrient leaching, water percolation, soil water availability and carbon cycling as well as the stability and mobility of bio-char itself with research in our Ithaca lab, in Colombia, Brazil, Zambia and Kenya.

  • Charcoal as Soil Conditioner: Studies in the humid Tropics
    Christoph Steiner1, W. G. Teixeira2, J. Lehmann3and W. Zech1, U Georgia TP 2004

  • BBC: The Secret of El Dorado
    December 19, 2006

    In 1542, the Spanish Conquistador, Francisco de Orellana ventured along the Rio Negro, one of the Amazon Basin's great rivers. Hunting a hidden city of gold, his expedition found a network of farms, villages and even huge walled cities. At least that is what he told an eager audience on his return to Spain.

    "No one ever saw again what Orellana described"
    Dr James Petersen, University of Vermont

  • Advanced Brazilian Beehive Kiln
    Ken Newcomber, Katoomba Working Group, Rio de Janerio, Brazil 2001
    Advanced Brazilian Beehive KilnAdvanced Brazilian Beehive Kiln

  • Slash and Char as Alternative to Slash and Burn: soil charcoal amendments maintain soil fertility and establish a carbon sink
    Christoph Steiner, www.biochar.org Summary of Dissertation, Faculty of Biology, Chemistry and Geosciences University of Bayreuth, Germany, Institute of Soil Science and Soil Geography, University of Bayreuth, D-95440 Bayreuth, Germany (email: Christoph.Steiner@uni-bayreuth.de)

    ABSTRACT

    Introduction

  • Terra Preta: Homepage about Anthrohumox in Brazilian Lowland
    Gerhard Bechtold, University of Bayreuth/Munchen, Germany, November 2007
    Consultant for National (Geo-)Information Systems and Database Setup, for Natural
    Resources Assessments


    GIS MAP of Terra Preta Sites in the Amazon
    Summary of Thesis about Anthrohumox in Brazilian Lowland (2007)


    In the Amazon lowland, Oxisol developed in scattered areas to ‘Indian Black Earth’ (Portuguese: ‘ Terra Preta’). High content of C (more than 9%) and ceramics are characteristics. Furthermore, they show weak acidity (but pH not over 6.5), low solum weight and high cation exchange capacity. The very most soil parameters are correlating with the percentage of C.


    Terra Preta soil patterns can be found in the Amazon lowland ( map, based on literature research). Visited TP spots in Belterra (close to Santarem) show characteristics about their extension (seldom more than 2 acre), their depth (till about 50 cm with black color of value 3 or lower, in traces till 2-3 m depth) and their transition to the surrounding Oxisols (some few km). Size is correlating with intensity (low value – large areas) and frequency of ceramics in most cases. Due to oxic horizon in the lower Terra Preta, great group ‘Anthrohumox’ is proposed.


    There are various theories about their origin. It is proved indeed, that Terra Preta is man made (high phosphate content, ceramics, situation on former village sites). About 1500-2800 years ago the Indios of the area had a strong influence on the Oxisols by their garbage, kitchen, compost and/or mulch ‘farming’ for a couple of hundreds years on their dwelling sites. C14 tests of the samples showed ages of 1780 (+ 270) and of 2260 (+ 280) years, thus dating back to between 800 BC and 500 AD.


    Intensive activity of organisms and bioturbation cause a breaking up, a lowering of the solum weight, the loss of some hundred kg soil material per square m and of fine particles (‘only’ 65-80 % clay). High sand content indicates high C content (not in terms relative to other areas). All those characteristics decrease with increasing soil depth.


    Strong impact of humic acids react a strong weathering of Si, Al and Fe. Different leaching ratios are discussed in the paper. They show a stronger weathering in the Terra Preta than in the Oxisol (lower Si, higher Al and Fe content). Al occurs mainly as 1:1 mineral (the main parent material), Fe as hematite or –favored by organic material – as goethite (over 70 % Fe d:Fe t).


    Strong weathering (Aw climate) causes some characteristics at the depth functions of Si, Al, Fe, but leaching and cristallization is retarded by strong chelation (humic acids complex with metal ions). M o:M d relations quote always high (especially in Al and Mn, less in Fe). Very pronounced peaks of Al o (and of Fe o) are difficult to explain. Illuviation and podzolation seem to be very active. Different chelating groups (M(OH)++ or M(OH)2+) with different stabilities are more reasonable.
    Very strong is the influence of the organic material on the content of Mn, Ca, Mg in the upper layers existing a manifold content, compared to the lower horizons, more than 10 times at Ca, due to the exchange sites of the organic substance (high solubility and erosion). At Mg existing fixation in anorganic compounds, e.g. Mg-Al-hydroxydes, at K in mineral interlayers are responsible for the lower percentages of the exchangeable to the total.


    The vertical transition to the Oxisol depends on the element: Terra Preta and Oxisol have an almost identical C content at a depth of 1.50 – 2.00 m, an identical solum weight at 2.30 m depth, identical texture only at depths of more than 4 m, identical acidity and Si content at 2 m, Mn and K 40 – 50 cm, Ca and Mg at 1.50 m.


    An exceptional profile with nodular laterite concretions (plinthic, plateau laterite) on a slope was analysed. It was found to have high C content and plenty of ceramics (therefore, Terra Preta), but in acidity and exchange capacity (content of K, Ca, Mg) it is more similar to Oxisols. In a different TP profile, burned charcoal induced high C contents and other characteristics of the upper horizons of Terra Preta.


    At many elements it is possible to recognize, beside the organic influence, a ‘basic content’ (very low at nutrients) of Ca with 200 – 300 ppm, Mg with 180 – 190 ppm, K with 200 – 300 ppm, K with 50 ppm etc. A melioration by mobilization of these reserves is impossible.


    Melioration is imaginable by pH raising (of soil and vegetation), addition of organic substances without fast mineralization and higher bioturbation.


    Further research about Terra Preta, surrounding conditions of their development and analytics are described in the paper.

  • Studies of the Compositions of Humic Acids from Amazonian Dark Earth Soils
    Etelvino H. Novotny, Eduardo R. de Azevedo, Tito J. Bonagamba, Tony J. F. Cunha, Beta E. Madari, Vinícius de M. Benites, and Michael H.B. Hayes, Environmental Science and Technology, December 8, 2006

    Abstract:
    The compositions of humic acids (HAs) isolated from cultivated and forested "Terra Preta de Índio" or Amazonian Dark Earth soils (anthropogenic soils) were compared with those from adjacent non-anthropogenic soils (control soils) using elemental and thermogravimetric analyses, and a variety of solid-state nuclear magnetic resonance techniques. The thermogravimetric index, which indicates the molecular thermal resistance, was greater for the anthropogenic soils than for the control soils suggesting polycyclic aromatic components in the former. The cultivated anthropogenic soils were more enriched in C and depleted in H than the anthropogenic soils under forest, as the result of the selective degradation of aliphatic structures and the possible enrichment of H-deficient condensed aromatic structures. The combination of variable amplitude cross-polarization (VACP) and chemical shift anisotropy with total suppression of spinning sidebands experiments with composite pulses could be used to quantify the aromaticity of the HAs from the anthropogenic soils. From principal component analysis, using the VACP spectra, it was possible to separate the different constituents of the HAs, such as the carboxylated aromatic structures, from the anthropogenic soils and plant derived compounds. The data show that the HAs from anthropogenic soils have high contents of aryl and ionisable oxygenated functional groups, and the major functionalities from adjacent control soils are oxygenated functional groups from labile structures (carbohydrates, peptides, and with evidence for lignin structures). The anthropogenic soils HAs can be considered to be more recalcitrant, and with more stable reactive functional groups which may, in part, explain their more sustainable fertility due to the organic matter contribution to the soil cation exchange capacity.

    Environ. Sci. Technol., 41 (2), 400 -405, 2007. 10.1021/es060941x S0013-936X(06)00941-2
    Web Release Date: December 8, 2006

    Authors: Embrapa Solos, R. Jardim Botânico, 1.024, Rio de Janeiro-RJ, Brazil, 22460-000, Chemical and Environmental Sciences, University of Limerick, Ireland, Instituto de Física de São Carlos, Universidade de São Paulo, São Carlos-SP, Brazil, Embrapa Semi-rido Cx.P. 23. Petrolina-PE, Brazil, 56300-970, and Embrapa Arroz e Feijão, Cx.P. 179. Santo Antônio de Gois-GO, Brazil, 75375-000

Burkina Faso

  • Microcatchment Rainwater Harvesting Systems: Zai Planting Holes Section 2.1
    Olufunke Cofie, Boubacar Barry, Deborah Bossio, International Water Management Institute, Ghana and Sri Lanka, Nobember 22-25, 2004

    Zai Planting pit, Sandy Soil, NigerZai Planting pit, Sandy Soil, Niger

    "Human Resources as a driver of Bright Spots: the case of rainwater harvesting in West Africa", Conference Paper 19, NEPAD/IGAD Regional Conference: Agricultural Successes in the Greater Horn of Africa, Nairobi 22-25, 2004

    2.1 Micro-catchment rainwater harvesting systems

    "There are many types including: terraces, earth or rock bunds, tied ridges, rock dikes, stone lines, planting pits or basins and their modifications used in different parts of West Africa. Stone and earth bunds have been used for several years to trap water for crops during the rainy season. Around Upper West Region in Ghana, these bunds have been developed into a terrace system on the slopes. The bunds are square, or rectangular shape, and their slopes are not along the contour. Millet is the main crop grown under this system in Ghana. The height of the stone bunds depends on available stone or soil depth in the neighborhood. In some places stone lines are used. These are made up of continuous lines of stones in a field along the contour to slow down the flow of rainwater, thus enhancing infiltration and to facilitate to some extent the deposition of vegetable debris and fine soil particles which increase soil fertility in the long run. Planting Pit or Basin is commonly used in the sub-region with various modifications including the zai in Burkina and in Mali, and also Tassa and half moon in Niger. In Ghana, stones are removed to create pits for collection of water in areas with high clay content in the subsoil (Kranjac-Berisavljevic et al 2002).

    Perhaps the most sucessful of these techniques is the zai ("water pocket") in Burkina Faso Zai is an ancestral planting pit developed in the Yatenga province, North Western part of Burkina Faso (where average rainfall is about 600 mm, with recurrent droughts and where soils are heavily encrusted. The Yatenga province has a hig population density (80 hbts/km2), and sufferred from recurrent droughts in the late 1960's and early 1970's. Since the early 1980's, "zai" has been rapidly revived and adopted by farmers, resulting in 1989, over 8000 hectares of degraded land in over 400 vilages in Burkina, being brought back to productivity. Large areas of the province are covered with lateritic soils of low infiltration capacity. the objective of the Zai practice is to regenerate the most degraded part of the field. It consists of digging holes or 'basins' of around 20-20 cm in diameter and 10-15 cm in depth. (Bandre and batta, 2002). The holes store rainwater, for plant growth. Generally the density is about 10,000-15,000 holes/ha depending on the crop chosen and the spacing between holes. Farmers use stone contour bunds to reduce the speed of runoff allowing infiltration into the zai which collect and concentrate the runoff. The larger the planting pits, and the bigger the spacing, the more water can be harveted from the uncultivated micro-catchments. Organic manure is put in the holes at a rate of about 3-4 t/ha. Sorghum is the preferred crop because of its greater adaptation to possible temporary hydromorphic conditions in the hole.

    According to Fatondji (2002) working in Naimey (Niger), the Zai technique assured a substantial total dry matter (TDM) increase (3086 kg ha-1) compared to flat planting (991 kg ha-1) with cattle manure application under 20 mm irrigation regime. He also observed that the quality of the amendment in Zai played a significant role. Low TDM as well as grain yield was produced with crop residue and compost of low quality. He observed for instance at the three study sites in Niger, that TDM produced on average with crop residue application was 756 at Sadore; 925 at Damari and 2185 kh ha-1 at Kakassi in 1999, compared to 3957, 4600 and 5030 kg ha-1 respectively with same rate of manure application. The grain yield was 151 kg ha-1 at Damari and 393 kg ha-1 at Kakassi with crop residue application, while it was 987 and 778 kg ha with manure application.

    Ftondji (2002) observed that the Zai planting technique induced a higher water use efficiency than flat planting at three sites in Niger. Combination of Zai with manure improved considerably water use efficiency in three different sites. Therefore it is imperative to promote technologies that can on one hand help increase potential water availability and on the other hand consequently help rehabilitate degraded lands. "Zai" enhanced soil water storage and increased plant water availability, though most of this water could be drained out in soil with low water holding capacity as in Sadore and Damari in Niger. Nevertheless, the use of good quality organic amendment (manure) promoted rapid and deep root growth and helped limit water loss by drainage.

    See also:

    Southern and East Africa Rainwater Network Searnet
    IWMI Research in Africa Best Practices Zai Holes

    ECHO Dryland techniques and Mulches

    Drylands Coordination Group Integrated Plant Nutrition

    Drylands Coordination Group Integrated Plant Nutrition Management in Mali pdf
    Summary Report 1998-2004

Burundi

Canada

  • Canadian conference on "Greenhouse Gases: Mitigation and Utilization" 8-12 July 2007
    Duane Pendergast, February 16, 2007

    I recently received a conference notice of potential interest to Terra Preta researchers and developers.

    The conference scope provides for papers on the carbon balance, CO2 sequestration in soil and biomass, mitigation of N2O and methane, enhanced agriculture and forestry, regulatory frameworks for carbon capture and
    storage and science for policy development and public understanding.

    CHEMRAWN-XVII and ICCDU-IX Conference on GREENHOUSE GASES Mitigation and Utilization
    8-12 July 2007 Kingston, Ontario, Canada

    www.chem.queensu.ca/greenhouse/