| Volume 5 Special Issue 1 2011Soil Organic Matter: Brazilian Perspectives
   ISBN 978-4-903313-83-2
 How to reference:  Leite LFC,  Sagrilo E,  Maciel GA, Iwata BF (2011) Simulation model to estimate carbon sequestration under management systems in tropical soils of Brazil. In: Leite LF, Madari BE (Eds) Soil Organic Matter: Brazilian Perspectives. Dynamic Soil, Dynamic Plant 5 (Special Issue 1), 1-6
 
 Guest Editors Luiz F. LeiteEmbrapa Mid-North, Brazil
 www.cpamn.embrapa.br
 Beata E. MadariEmbrapa Rice and Beans, Brazil
 www.cnpaf.embrapa.br
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 CONTENTS AND ABSTRACTS Luiz Fernando Carvalho Leite, Edvaldo Sagrilo, Giovana Alcântara Maciel, Bruna de Freitas Iwata (Brazil) Simulation Model to Estimate Carbon Sequestration under Management Systems in Tropical Soils of Brazil (pp 1-6)
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   ABSTRACT Invited  Mini-Review: Soil organic carbon (SOC) represents a  major pool of carbon within the biosphere and acts as source and a sink for  carbon and nutrients. Several simulation models have been developed and  evaluated to estimate SOC stocks in different agroecosystems such as, CENTURY  or ROTHC which are considered mechanistic, complex and based on qualitative  concepts rather than measurable entities. Because of this complexity, it is  important that simpler but mechanistic SOC models, like CQESTR (a contraction  of C sequestration), be developed and tested under several soil and climate  conditions. CENTURY and CQESTR have been evaluated to estimate SOC stocks in  different management systems. Particularly in tropical soils, both models have  estimated an increase in the SOC stocks in the no-tillage compared to  conventional tillage system. However, it is necessary to improve the model  accuracy including important variables to tropical areas like soil structure or  soil mineralogy.    Edvaldo Sagrilo, Luiz  Fernando Carvalho Leite, Giovana Alcântara Maciel (Brazil) Soil Organic Matter as  Affected by Green Manure at Brazilian Conditions (pp 7-11) 
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   ABSTRACT Invited  Mini-Review: The use of green manure has been  associated with increasing soil organic matter (SOM), which is an essential  component of high-quality agricultural soils, especially in tropical  environments such as Brazil.  The aim of this review was to present evidence of the effectiveness that green  manures use has on the improvement of Brazilian SOM stocks. The contribution of  soil aggregation to SOM stabilization, the importance of returning high amounts  of plant residues to the soil, and the effectiveness of including N-fixing  legumes in the cropping systems are all summarized. Soil aggregation is highly  dependent on the continual addition of crop residues to the soil, and creates  favorable conditions for SOM accumulation. SOM build-up is directly correlated  to the amount of crop residues added to the soil and it is closely dependent on  the duration, in the long-term, of this soil residue input. Moreover, the  quality of these crop residues is of major importance, considering not only the  high content of C directly added to the soil by the green manures, but also  their N content, which is a determinant in the growth of subsequent crops, resulting  in increased amounts of residue-derived C returned to the soil. The inclusion  of green manures in cropping systems, especially legume species, in association  with appropriate soil management practices, is a feasible and sustainable way  to increase long-term SOM stocks in Brazilian tropical conditions.    Vanderlise Giongo, Sandra Regina da Silva Galvão,  Alessandra Monteiro Salviano Mendes, Carlos Alberto Tuão Gava, Tony Jarbas  Ferreira Cunha (Brazil) Soil  Organic Carbon in the Brazilian Semi-arid Tropics (pp 12-20)
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 ABSTRACT Invited  Mini-Review: The Brazilian semi-arid tropics occupies  an area of 969,589 km2 that represents 11% of the national territory  and the Caatinga is its most representatives Biome with an area of 844.453 km².  However, approximately 46% of this area is deforested. The conversion of  Caatinga preserved vegetation in degraded areas has contributed to global  climatic changes; therefore, a series of scientific research studies has as its  objective to quantify the C reservoirs in different semi-arid regions of the  world, as well as to identify the factors that control its dynamic. Recently,  network research studies for measuring C stock and balance in natural  vegetation and disturbed areas, firstly related to livestock and dry land  farming that are dominant activities in the region, and secondly related to  irrigated agricultural exploitation due to its high impact in the productive  system, have been developed. The studies comprise C determination in soil,  plant, micro-organism and atmosphere systems, involving C and energy balance  and the effect of land use on C stock relations. C stocks in the Brazilian  semi-arid tropics varies from 20 to 48.4 t ha-1 at 0-20 cm soil  layer, while for the aerial part of natural vegetation the values vary from 1 to  80 mg ha-1. It can be observed, for the same soil and vegetation  type, that changes in land use decrease soil C stock and that plant cover  management can behave as C source.    Beáta Emöke Madari, Tony Jarbas Ferreira Cunha,  Ricardo Soares (Brazil) Organic Matter of the  Anthropogenic Dark Earths of Amazônia (pp 21-28) 
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   ABSTRACT Invited  Review: The anthropogenic dark earths (ADE, Terra Preta de  Índio or terra preta arqueológica, as are often referred to in Portuguese)  feature unique properties that are interesting not only from a pedological  point of view but have important agronomic and economic relevance. Among other  properties, the organic matter (SOM) of these soils is considerably different  from that of other mineral soils. Besides the quantity of SOM, its origin,  composition and, consequently, function in the soil is different. Carbonized  biomass (pyrogenic carbon) is a principal constituent of ADE that was, to our  best knowledge, gradually incorporated into these soils, 4 to 10 thousand years  ago, by native dwellers of the Amazon region. The carbon of pyrogenic origin  was not only accumulated in ADE, but it also played important role in the  transformation of organic matter and the humification process. As a result of  this, the SOM of ADE is relatively stable, compared to the SOM of adjacent  ferralsols, and at the same time it has chemical reactivity that is the major  responsible for the higher cation exchange capacity and good buffer properties  of these soils. These properties have very important environmental and  agronomic relevance in the tropics due to organic carbon conservation in the  soil and enhanced soil fertility. The ADE soils are excellent model for the  development of modern soil fertility management practices.    Giovana Alcantara Maciel, Sandro Manuel Carmelino  Hurtado, Luiz Fernando Carvalho Leite, Edvaldo Sagrilo, Adriana Monteiro da  Costa (Brazil) Influence of  Integrated Crop-Livestock-Forest Systems on Soil Organic Matter in Tropical  Regions (pp 29-35)
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   ABSTRACT Invited  Mini-Review: Soil organic matter (SOM) plays important  functions in soil physical, chemical and biological processes. A reduction of  SOM enhances the soil degradation process by reducing the biomass production  and causing the loss of nutrients, water and soil. A mix of annual crops, tree  species and pasture on the same area in an Integrated Crop-Livestock-Forest  System (ICLFS) ensures abundant supplies of residues and an elevated amount of  accumulated organic material in the soil thus constituting a promising  alternative for tropical regions. Land areas aimed at fodder production, if  well managed, produce large quantities of residues, which associated with a  non-disturbed soil, favor the accumulation of SOM. In ICLFS, the cultivation of  grain crops prior to the use of the land for pastures ensures more efficient  use of residual nutrients by the plants, thus increasing the productivity of  pastures. The adoption of technologies aiming at sustainability, as an improved  soil management system, with better use of natural resources, increases the  soil carbon levels. This condition results in the economic feasibility of  cropping systems, through the improvement of soil, water and consequently, the  environment quality. This chapter discusses the main advantages of integrated  production systems and the influence of ICLFS on the supply and maintenance of  SOM in tropical and subtropical regions.    Cristiane Pereira de Assis, Francisco Alisson da  Silva Xavier, Stoécio Malta Ferreira Maia, Rafaella Silva Nogueira, Guilherme  Viana de Alencar, Teógenes Senna de Oliveira (Brazil) Soil Organic Matter Changes in Agroforestry and Organic Farming in the  Semi-Arid Region of Northeastern Brazil (pp 36-44)
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   ABSTRACT Invited  Review: The development of  management strategies aiming to increase soil quality in Brazilian semi-arid  regions, including the improvement of soil organic matter (SOM) status, is  still scarce. In general, most  of the traditional farming practices adopted in agricultural fields in Northeast Brazil (semi-arid) contribute to a reduction of  in SOM levels, thus alternative management practices must be implemented to  improve soil quality in different agricultural production systems. Within this  context, agroforestry and organic farming have been considered suitable  management options to cope with the semi-arid climate despite of its  environmental constraints. This study aimed at presenting results from well  established experiments on agroforestry and organic farming performed in  Sobral, Guaraciaba do Norte and Ubajara counties, all located in the State of Ceará, Brazil.  In agroforestry, agrosilvopastoral and silvopastoral designs may be considered  as important options to increase soil organic C stocks, with consequences in  the different SOM pools, including labile C. Organic farming has been implemented  in both small and large scale agriculture, and it too represents a good  strategy to increase the status of SOM, even in sandy soils as observed at  Ubajara county. Obviously, agronomic,  economic and social aspects should be linked to the environmental benefits brought about through the  adoption of agroforestry and/or organic cultivation. Notwithstanding, the  discussion involving the improvement of food production in Brazilian semi-arid  must regard both types of agroecosystems as suitable options to increase the  status of SOM, which represents the starting point for recovering soil quality,  and consequently, enhancing productivity.    Francisco Alisson da Silva Xavier, Eduardo de Sá  Mendonça (Brazil) Agroforestry for Recovering Soil Organic Matter: A Brazilian Perspective  (pp 45-52)
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   ABSTRACT Invited  Review: The recovery of soil organic matter (SOM) can be  considered as one of the most important goals in recovering soil quality. The  evaluation of changes in SOM levels as a result of soil management practices is  essential to identify strategies to increase agricultural production, avoid  soil degradation, and decrease the emission of greenhouse gases. Agroforestry  systems are considered to be a suitable land use alternative to maintain SOM  levels through the supply of litter and root residues. In Brazil, no-tillage is widely  accepted as a soil management alternative to enhance soil organic carbon (C)  sequestration in different ecosystems. Nevertheless, only few studies have been  conducted to evaluate the effect of agroforestry on SOM recovering. Interest in  agroforestry has increased in the last decade, especially its adoption by  smallholding agriculture. The most consistent Brazilian agroforestry  experiences have been developed basically in three main macro-regions of the  country: the North, Northeast and Southeast Regions. In the North, multistrata  agroforestry designs are preferentially adopted in the Amazonian Region,  whereas silvopastoral, agrosilvopastoral and alley cropping are mainly adopted  in the Northeast Region. Coffee-agroforestry systems are examples of well  established agroforestry experiences in the Southeast. The potential of soil C  sequestration by agroforestry systems in Brazil varies substantially among  the different regions. The potential of organic C storage depends on the design  of the systems, tree species, climate and soil characteristics. The biomass  production (through litterfall) in some Brazilian agroforestry systems may vary  from 1.39 to 25.92 Mg ha-1 year-1 and the respective  potential for organic C storage from 0.62 to 11.66 Mg ha-1 year-1.    Claudia Maria B. F. Maia, Beata E. Madari, Etelvino  H. Novotny (Brazil) Advances in Biochar Research in Brazil (pp 53-58) 
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   ABSTRACT Invited  Mini-Review: To mitigate global warming, major changes  in the global carbon balance are expected as the world’s larger economies  migrate to energy matrices that emit less greenhouse gases (GHG). Alternatives  of carbon-neutral technologies have led to significant alterations in the  global balance of carbon. One example is biochar, which is any source of  biomass previously heated under low or no oxygen supply with the purpose of  application on soil. This review aims to give an overview about the research  carried out in Brazil  on biochar-to-soil technology, from its structural characterization to field  trials all over the country.    Lilian B. P. Zaidan, Maria Angela M. Carvalho (Brazil) Nitrogen  Effects on Growth and Fructan Production in Vernonia herbacea (Vell.)  Rusby, an Asteraceae from the Brazilian Cerrado (pp 59-64)
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   ABSTRACT Invited  Mini-Review: The Cerrado, second  largest biome in Brazil,  hosts a high biodiversity and is listed as one of the most endangered  ecosystems (hotspots) of the world. The cerrado soils are old, deep, with low  water retention, poor in nutrients and with high levels of aluminum. Although  plants native to the cerrado are well adapted to oligotrophic soils, growth and  productivity can be increased by addition of mineral nutrients. Vernonia  herbacea is a perennial herb accumulating about 80% of inulin-type fructans  in the underground organs, thus being considered an alternative source for  inulin production. The present review is focused on the role of nitrogen in  growth, biomass allocation and inulin production in plants of V. herbacea grown in the field and under glasshouse conditions. The studies here reported  summarize the efforts towards the understanding of the physiology and  biochemistry of this promising species of the Cerrado and could contribute to  the sustainable use of this biome.    Gooty Jaffer Mohiddin, Mandala Srinivasulu, Mekapogu Madakka, Kondeti  Subramanyam, Vengatampalli Rangaswamy (India) Influence of Selected Insecticides on Enzyme  Activities in Groundnut (Arachis hypogaea L.) Soils (pp 65-69)
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   ABSTRACT Original  Research Paper: The influence of acephate  and imidacloprid on important soil enzyme activities, such as dehydrogenase and  urease in two groundnut (Arachis hypogaea L.) soils, collected from  Anantapur District of Andhra Pradesh, India, was studied under laboratory conditions.  The activity of dehydrogenase, in terms of formazan formed from triphenyl  tetrazolium chloride, was more pronounced in both soils treated with 2.5 kg ha-1 of the acephate and imidacloprid. But higher concentrations (5.0, 7.5 and 10 kg  ha-1) were toxic to dehydrogenase activity. The activity of urease  in terms of ammonia formed from hydrolysis of urea was higher in both soils,  treated with acephate and imidacloprid at 5.0 kg ha-1, but higher  levels (7.5 and 10 kg ha-1) were toxic or innocuous to urease  activity.    Mekapogu Madakka, Gooty Jaffer Mohiddin, Mandala Srinivasulu, Vengatampalli  Rangaswamy (India) Influence of  Pesticides, Alone and in Combination, on Phosphatase Activity in Soils of  Groundnut (Arachis hypogaea L.) Fields (pp 70-74)
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   ABSTRACT Original  Research Paper: Pesticides such as thiram  and difenoconazole (fungicides), and deltamethrin and profenofos (insecticides),  alone and in combination with insecticides viz., profenofos (organophosphate) +  cypermethrin (synthetic pyrethroid) and deltamethrin (synthetic pyrethroid) +  endosulfan (organochlorine) were applied at five concentrations (0.0, 1.0, 2.5,  5.0, 7.5 and 10.0 kg ha-1) to test their non-target effects towards  the activity of phosphatase in black clay and red sandy clay soils of groundnut  (Arachis hypogaea L.) fields under laboratory conditions. Phosphatase  activity was more pronounced in soil samples treated with 2.5 kg ha-1 of the insecticide combinations and individual pesticides. The activity of  phosphatase was increased with increasing concentration of insecticide  combinations up to 2.5 kg ha-1. Higher levels of these pesticides  and insecticide combinations eliminated phosphatase activity. Soil samples  receiving 2.5 kg ha-1 of insecticide combinations profenofos +  cypermethrin and deltamethrin + endosulfan accumulated para-nitrophenol  most after 20 days of incubation; enzyme activity decreased as the period of  incubation increased. Results of this study suggest that enzyme activity is  influenced by the concentration of profenofos + cypermethrin and deltamethrin +  endosulfan combinations.    Mekapogu Madakka, Mandala Srinivasulu, Gooty Jaffer  Mohiddin, Vengatampalli Rangaswamy (India) Effect of Pesticides on Microbial Diversity  and Urease in Groundnut (Arachis hypogaea L.) Soil (pp 75-82)
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   ABSTRACT Original  Research Paper: The  influence of four pesticides viz., profenofos, deltamethrin, thiram and difenoconazole  and two insecticide combinations viz., profenofos + cypermethrin and  deltamethrin + endosulfan at 0.0, 1.0, 2.5, 5.0, 7.5 and 10.0 kg ha-1 were  assessed for their effects on the activity of urease (measured in terms of  hydrolysis of urea by sodium hypochlorite method) and microbial populations  like bacteria, fungi and actinomycetes in two agricultural soils, collected  from a fallow groundnut (Arachis hypogaea Linn.) fields of Anantapur  district. The effects of selected pesticides profenofos, deltamethrin, thiram  and difenoconazole and profenofos + cypermethrin and deltamethrin + endosulfan  on microbial population and urease activity were dose dependent. Urease  activity and microbial populations increased with increasing concentrations of  the pesticides up to 5.0 kg ha-1. Higher rates (7.5, 10.0 kg ha-1)  of these pesticides were either toxic or innocuous to the urease activity and microbial  population. The significant stimulation in the activity of urease was  associated with 2.5 kg ha-1 of pesticides in black soil, where as in  red soil it was 5.0 kg ha-1 of profenofos, 2.5 kg ha-1 of  deltamethrin, thiram, difeneconozole. In the insecticide combinations urease  activity was 5.0 kg ha-1 profenofos + cypermethrin, 5.0 kg ha-1 of deltamethrin + endosulfan in black clay soils whereas in red sandy  clay soils, population of microorganisms increased with 2.5 to 5.0 kg ha-1 of pesticides. With further incubation the activity of urease was significantly  more at day 20 and enzyme activity decreased progressively with increasing  incubation period.    S. Viveka, B. Leena Grace (India) Utilization of Weeds as Substrates for  Vermifertilizer (pp 83-86)
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   ABSTRACT Original  Research Paper: Aquatic weeds interfere  with the normal functioning of water bodies. Among the aquatic weeds, water  hyacinth is considered to be the most obnoxious weed ranked eighth in the  world. Ipomoea carnea is a cosmopolitan species of weed in disturbed  habitats. Compost is known to improve crop production by improving soil  fertility and soil physical properties. Earthworms make important contributions  in the decomposition of organic material. In the present study, Lampito  mauritii, an indigenous earthworm, was utilized for the decomposition of  commonly available aquatic weeds viz., Eichhornia crassipes and I. carnea for the production of good  quality vermicompost. After the completion of vermicomposting the cocoons,  juveniles, non-clitellated and adult earthworms were separated and counted.  Physico-chemical parameters of the compost were analyzed in the initial and  final stages of vermicomposting. Bacterial and fungal density and their generic  and species level identification analysis were also carried out. The pH value  increased in the final stage and was 7.2. The EC improved from initial  (0.82,0.85) to final stages (1.43,0.99) in both Eichhornia- and Ipomoea-based  composts. The temperature in the final stage of Eichhornia- and Ipomoea-based  vermicompost was 28.9 and 28.7°C, respectively. Bulk density decreased  significantly with increasing water holding capacity and porosity. N, P, K and  organic carbon values were higher in both Eichhornia- and Ipomoea-based  vermicompost than the initial state. Bacterial density of Eichhornia and Ipomoea composts was 2.16 ´ 107 and 2.83 ´ 107 CFU/g, respectively. The  fungal density of Eichhornia and Ipomoea composts were 2.76 ´ 104 and 2.30 ´ 104CFU/g, respectively. E.  crassipes and I. carnea,  bothweeds, could be effectively utilized as substrates for  vermicomposting.    Mojtaba Zeraat Pishe, Farhad Khormali, Ali Shahriari (Iran) The  Relationship between Specific Surface Area and Soil Organic Carbon in Loess-Derived  Soils of Northern Iran (pp 87-89)
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   ABSTRACT Short  Communication: Soil organic carbon (SOC)  can act as a sink or source of atmospheric carbon dioxide, therefore, it is  important to understand the amount and composition of SOC in terrestrial  ecosystems, the spatial variation in SOC, and the underlying mechanisms that  stabilize SOC. Relationships between minerals specific surface area and organic  carbon (OC) concentration were examined for sediments and soil A-horizons from  throughout the world. The organic compositions can be absorbed by  minerals surface, and also exist a positive relation between specific surface  area (SSA) and OC. Much of our current understanding is based on laboratory  experiments, the results of which often do not support observations made in the  field. The present study attempted to demonstrate the relationship between  specific surface area, SOC rate and clay content in the pasture soils, in  Golestan province. 7 soil profiles formed under different moisture regimes  (udic, xeric and aridic regimes) were sampled from their surface horizons (0-30  cm depth). Correlation and linear regressions  were performed between SOC, SSA and particle clay size. Results indicate that  the content of clay showed significant liner correlations with SSA (R2 = 0.63, P < 0.05) but SOC did not show significant liner correlations  with SSA (R2 = 0.50, P < 0.07). The results demonstrated  that mean residence time of organic carbon in soil increase with higher  specific surface area. Soils with high clay levels show greater SOC than soils  with high sand contents.    Mojtaba Zeraat Pishe, Farhad Khormali (Iran) Estimation of Organic Carbon Loss Potential  in a Climosequence in Golestan Province, Northern Iran (pp 90-93)
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   ABSTRACT Short  Communication: Soil carbon oxidized by  neutral KMnO4 has been used as index of labile C by several workers.  Study area a climosequence (udic-xeric-aridic regimes) with loess parent  material in Golestan province, Iran.  Samples from 7 different soil orders with pasture land use (Mollisols,  Inceptisols, Aridisols and Entisols) were collected at (0-20 cm) depth. Permanganate-oxidizable  carbon (POC), an index of soil labile carbon, was used to show soil potential  loss of organic carbon (OC). This index shows the maximum loss of OC in a given  soil. Maximum loss of OC for each soil was estimated through POC and bulk  density. The potential losses of OC were estimated between 1930.6 and 69180.9  Kg ha-1 C. The lowest organic C loss was related to Entisols because  of containing the lowest OC, and maximum potential loss of OC has been detected  in Mollisols mainly due to having a lot of fresh organic tissue in mollic  epipedon. In addition, the total amount of OC which were oxidised by KMnO4 ranged from 15.6 to 60.73% of the total C. The effect of soil texture on POC  was examined, clay + silt/OC, silt/OC and clay/OC accounts for 63, 68 and 51%,  respectively, of the variability in soil POC (P < 0.05). And also soil POC  of 7 soil sample were regressed with their total C contents and were found to  be highly correlated (R2 = 0.94, P < 0.01). Stable organic  constituents in the soil include humic substances and other organic  macromolecules that are intrinsically resistant against microbial attack, or  that are physically protected by adsorption on mineral surfaces or entrapment  within clay and mineral aggregates.    |