Effects of nutrient (N, P, K) fertilization on the dynamics of fine roots in tropical rain forests with different soil texture in the Colombian Pacific region / Efectos de la fertilización con nutrientes (N, P, K) sobre la dinámica de raíces finas en bosques húmedos tropicales con diferente textura del suelo en la región del Pacífico colombiano

Abstract Introduction: Fine root dynamics include production, turnover and decomposition; they are crucial to forest health, affect the entire biogeochemical complex of the ecosystem, and consequently, they substantially affect carbon balance. However, the influence of environmental factors and soil nutrient limitation on fine roots presents considerable uncertainties and has not been studied in tropical forests with more than 7 000 mm annual rainfall. Objective: To measure the effect of fertilization on fine roots in the high precipitation Chocó forest. Methods: We worked in two sites of the Chocó region, Colombia (August 2014-May 2015), where rainfall exceeds 10 000 mm per year. We applied five fertilization treatments (N, P, K, NPK and Control) to two soil type plots. Soil cylinders were removed at pre-established intervals to measure roots. Results: Phosphorus applications increased fined roots; and more fine roots were produced in sandy than in loam soil. The effects of fertilization were related, but not clearly determined by edaphic conditions. Conclusions: In this Chocó forest, the production of fine roots was higher in sandy and nutrient-rich soils but belowground net primary productivity was limited by the content of edaphic Phosphorus.

Resumen Introducción: La dinámica de las raíces finas incluye producción, rotación y descomposición; son cruciales para la salud de los bosques, afectan todo el complejo biogeoquímico del ecosistema y, en consecuencia, afectan sustancialmente el balance de carbono. Sin embargo, la influencia de los factores ambientales y la limitación de nutrientes del suelo en las raíces finas presenta incertidumbres considerables y no se ha estudiado en bosques tropicales con más de 7 000 mm de precipitación anual. Objetivo: Medir el efecto de la fertilización en las raíces finas en el bosque chocoano de alta precipitación. Métodos: Se trabajó en dos sitios de la región del Chocó, Colombia (agosto 2014-mayo 2015), donde las precipitaciones superan los 10 000 mm anuales. Se aplicaron cinco tratamientos de fertilización (N, P, K, NPK y Control) a dos parcelas por tipo de suelo. Los cilindros de suelo se retiraron a intervalos preestablecidos para medir las raíces. Resultados: Las aplicaciones de fósforo aumentaron las raíces finas; y se produjeron más raíces finas en suelos arenosos que en francos. Los efectos de la fertilización estuvieron relacionados, pero no claramente determinados por las condiciones edáficas. Conclusiones: En este bosque chocoano, la producción de raíces finas fue mayor en suelos arenosos y ricos en nutrientes, pero la productividad primaria neta subterránea estuvo limitada por el contenido de fósforo edáfico.

Effects of phosphate, carbonate, and silicate anions on CO2 emission in a typical oxisol from cerrado region / Efeitos dos ânions fosfato, carbonato e silicato na emissão de CO 2 em um latossolo típico da região do cerrado

The effects of agricultural practices on greenhouse gases emissions (e.g. CO2) at the soil-atmosphere interface have been highlighted worldwide. The use of ground limestone has been considered as the main responsible for CO2 emission from soils. However, liming is need as conditioner of acidic soils and the CO2 emission can be compensated due to carbon sequestration by plants. This study simulated under laboratory conditions the effects of two common agricultural practices in Brazil (P-fertilization and liming) on soil CO2 emission. Columns made of PVC tubes containing 1 kg of a typical Dystrophic Red Latosol from Cerrado region were incubated with CaCO3 (simulating liming), CaSiO3 (simulating slag), and different doses of KH2PO4 (simulating P-fertilization). The soil columns were moistened to reach the field capacity (0.30 cm3cm-3) and, during 36 days, CO2 emissions at the soil surface were measured using a portable Licor LI-8100 analyzer coupled to a dynamic chamber. The results showed that CO2 emission was influenced by phosphate, carbonate, and silicate anions. When using CaSiO3, accumulated CO2 emission (36-day period) was 20% lower if compared to the use of CaCO3. The same amount of phosphate and liming (Ca-carbonate or Ca-silicate) added to the soil provided the same amount of CO2 emission. At the same P dose, as Si increased the CO2emission increased. The highest CO2 emission was observed when the soil was amended with the highest phosphate and silicate doses. Based on this experiment, we could oppose the claim that the use of limestone is a major villain for CO2 emission. Also, we have shown that other practices, such as fertilization using P + CaSiO3, contributed to a higher CO2 emission. Indeed, it is important to emphasize that the best practices of soil fertility management will undoubtedly contribute to the growth of crops and carbon sequestration.

Os efeitos das práticas agrícolas nas emissões de gases de efeito estufa (e.g., CO2) na interface solo-atmosfera têm sido destacados em todo o mundo. O uso de calcário tem sido considerado oprincipal responsável pela emissão de CO2 em solos. Entretanto, a calagem é necessária como condicionador de solos ácidos e a emissão de CO2 pode ser compensada devido ao sequestro de carbono pelas plantas. Este estudo simulou, em condições de laboratório, os efeitos de duas práticas agrícolas comuns no Brasil (adubação fosfatada e calagem) na emissão de CO2 do solo. Colunas de tubos de PVC, contendo 1 kg de amostra de um Latossolo Vermelho Distrófico típico da região de Cerrado, foram incubadas com CaCO3 (simulando calagem), CaSiO3 (simulando escória) e diferentes doses de KH2PO4 (simulando fertilização com P). As colunas de soloforam umedecidas para atingir a capacidade de campo (0,30 cm3 cm-3) e, durante 36 dias, as emissões de CO2na superfície do solo foram medidas usando um analisador portátil Licor LI-8100 acoplado a uma câmara dinâmica. Os resultados mostraram que a emissão de CO2 foi influenciada pelos ânions fosfato, carbonato esilicato. Ao usar CaSiO3, a emissão de CO2 acumulada (período de 36 dias) foi 20% menor se comparado ao uso de CaCO3. A mesma quantidade de fosfato e calcário (Ca-carbonato ou Ca-silicato) adicionado ao solo proporcionou a mesma quantidade de emissão de CO2. Na mesma dose de P, o Si aumentou a emissão de CO2. A maior emissão de CO2 foi observada quando o solo foi alterado com as maiores doses de fosfato e silicato. Com base neste experimento, nega-se que o uso de calcário em solos é um grande vilão para a emissão de CO2. Além disso, foi mostrado que outras práticas, como a fertilização usando P + CaSiO3, contribuíram para uma maior emissão de CO2. Assim, é importante enfatizar que práticas adequadas de manejo da fertilidade do solo, sem dúvida, contribuirão para o crescimento das culturas e o sequestro de carbono.

Maize Productivity, Mycorrhizal Assessment, Chemical and Microbiological Soil Attributes Influenced by Maize-Forage Grasses Intercropping

Abstract Mycorrhizae are important components of agroecosystems and the diversification of crops stimulates the abundance of arbuscular mycorrhizal fungi and the participation of symbiosis in plant growth. This experiment examined mycorrhizal assessment, chemical and microbiological soil attributes in a maize-forage grasses intercropping compared to a maize-monocropping system. A complete randomized block design was used with crop systems installed under no-till management with three replicates, as follow: Maize (Zea mays L.); Panicum maximum Jacq. cv. Aruana; Urochloa humidicola (Rendle.) Schweickerdt.; Maize-P. maximum intercropping and Maize-U. humidicola intercropping. In 2015/2016 season, intercropping maize with Panicum maximum Jacq. cv. Aruana or Urochloa humidicola (Rendle.) Schweickerdt. promoted similar effects (Tukey test, p<0.05) to monocropped maize under no-till system on soil chemical and biochemical parameters related to carbon cycling in the soil surface layer, as well as the dynamics of arbuscular mycorrhizal symbiosis in tropical soils, managed for a period of more than six years. Similar grain yield was verified among maize crop systems. This result indicates that intercropping maize-tropical forage grasses represents an alternative for monocropped grains, a very common practice that is used in intensive management, being able to guarantee equivalent productivities and to combine grain production with crop-livestock systems. As a result, intercropping promotes the diversification of the property's income source, adding environmental gains, such as more efficient land use by cultivated plants, keeping soil constantly cultivated, storing carbon and contributing to minimize the impact of climate change on agricultural systems and the sustainability of food production.

Archaea diversity in vegetation gradients from the Brazilian Cerrado

Abstract We used 16S rRNA sequencing to assess the archaeal communities across a gradient of Cerrado. The archaeal communities differed across the gradient. Crenarcheota was the most abundant phyla, with Nitrosphaerales and NRPJ as the predominant classes. Euryachaeota was also found across the Cerrado gradient, including the classes Metanocellales and Methanomassiliicoccaceae.

Dinámica de raíces finas y su relación con la fertilidad edáfica en bosques pluviales tropicales del Chocó biogeográfico colombiano / Fine root dynamics and its relationship with soil fertility in tropical rainforests of Chocó

Resumen:Las raíces finas juegan un papel importante en la adquisición de agua y minerales del suelo, el balance global del carbono y la mitigación del cambio climático. La dinámica (productividad-PRF y recambio-RRF) de raíces finas es esencial para el ciclo de nutrientes y balance de carbono de los ecosistemas forestales. La disponibilidad de agua y nutrientes determina de manera significativa la PRF y el RRF. Se ha planteado la hipótesis de que la dinámica de raíces finas aumenta con la disponibilidad de los recursos del suelo en bosques tropicales. Para probar esta hipótesis en las selvas tropicales del Chocó (ecosistemas con las más altas tasas de precipitación en el mundo), se establecieron cinco parcelas permanentes de una hectárea en las localidades de Opogodó y Pacurita, donde la PRF y RRF se midieron a 0-10 cm y 10-20 cm de profundidad. La medición de la PRF se realizó por el método de cilindros de crecimiento. La tasa de RRF se midió como la PRF/ biomasa media anual. Además, se midieron los parámetros de fertilidad del suelo (pH, nutrientes y textura) y se evaluó su asociación con PRF y RRF. Se encontró que ambos sitios presentan suelos pobres en nutrientes. Las localidades difieren en características edáficas; Opogodó tiene suelos arenosos y topografía plana, y Pacurita tiene suelos arcillosos, ricos en aluminio y topografía montañosa. En Opogodó la PRF fue (media ± DE) de 6.50 ± 2.62 t/ha.año. En Pacurita la PRF fue 3.61 ± 0.88 t/ha.año. Igualmente, en Opogodó el RRF fue mayor que en Pacurita (1.17 /año y 0.62 /año, respectivamente). El RRF y la PRF fueron mayores en la superficie del suelo (10 cm de profundidad). La PRF y el RRF mostraron correlación positiva con el pH, MO, N total, K, Mg, y arena; mientras que, las correlaciones fueron negativas con la CICE, Al, limo y arcilla. El porcentaje de arena fue el parámetro que mejor explica la variación en la PRF. La tasa negativa de la RRF fue explicada por la disponibilidad de Al. Los resultados evidenciaron un aumento en la dinámica de las raíces finas con la fertilidad del suelo a escala local, lo que sugiere que en selvas tropicales con suelos oligotróficos, las raíces finas tienden a proliferar rápidamente en pequeños parches de suelo ricos en arena y nutrientes.

Abstract:The fine roots play an important role in the acquisition of water and minerals from the soil, the global carbon balance and mitigation of climate change. The dynamics (productivity and turnover) of fine roots is essential for nutrient cycling and carbon balance of forest ecosystems. The availability of soil water and nutrients has significantly determined the productivity and turnover of fine roots. It has been hypothesized that fine roots dynamics increases with the availability of soil resources in tropical forest ecosystems. To test this hypothesis in tropical rainforests of Chocó (ecosystems with the highest rainfall in the world), five one-ha permanent plots were established in the localities of Opogodó and Pacurita, where the productivity and turnover of fine roots were measured at 0-10 cm and 10-20 cm depth. The measurement of the fine root production was realized by the Ingrowth core method. The fine root turnover was measured like fine roots production divided mean annual biomass. In addition, soil fertility parameters (pH, nutrients, and texture) were measured and their association with productivity and turnover of fine roots was evaluated. It was found that the sites had nutrient-poor soils. The localities also differ in soil; Opogodó has sandy soils and flat topography, and Pacurita has clay soils, rich in aluminum and mountainous topography. In Opogodó fine root production was 6.50 ± 2.62 t/ha.yr (mean ± SD). In Pacurita, fine root production was 3.61 ± 0.88 t/ha.yr. Also in Opogodó, the fine root turnover was higher than in Pacurita (1.17 /y and 0.62 /y, respectively). Fine root turnover and production in the upper soil layers (10 cm upper soil) was considerably higher. Productivity and turnover of fine roots showed positive correlation with pH and contents of organic matter, total N, K, Mg, and sand; whereas correlations were negative with ECEC and contents of Al, silt, and clay. The percentage of sand was the parameter that best explained the variations of fine root production. The fine root turnover was negatively explained by soil Al availability. Results suggested the increase of fine root dynamics with soil fertility at a local scale, which also indicates that under the oligotrophic conditions of soils in tropical rainforests, fine roots tend to proliferate rapidly in small patches of soil rich in sand and nutrients. Rev. Biol. Trop. 64 (4): 1709-1719. Epub 2016 December 01.

Initial pH of medium affects organic acids production but do not affect phosphate solubilization

The pH of the culture medium directly influences the growth of microorganisms and the chemical processes that they perform. The aim of this study was to assess the influence of the initial pH of the culture medium on the production of 11 low-molecular-weight organic acids and on the solubilization of calcium phosphate by bacteria in growth medium (NBRIP). The following strains isolated from cowpea nodules were studied: UFLA03-08 (Rhizobium tropici), UFLA03-09 (Acinetobacter sp.), UFLA03-10 (Paenibacillus kribbensis), UFLA03-106 (Paenibacillus kribbensis) and UFLA03-116 (Paenibacillus sp.). The strains UFLA03-08, UFLA03-09, UFLA03-10 and UFLA03-106 solubilized Ca3(PO4)2 in liquid medium regardless of the initial pH, although without a significant difference between the treatments. The production of organic acids by these strains was assessed for all of the initial pH values investigated, and differences between the treatments were observed. Strains UFLA03-09 and UFLA03-10 produced the same acids at different initial pH values in the culture medium. There was no correlation between phosphorus solubilized from Ca3(PO4)2 in NBRIP liquid medium and the concentration of total organic acids at the different initial pH values. Therefore, the initial pH of the culture medium influences the production of organic acids by the strains UFLA03-08, UFLA03-09, UFLA03-10 and UFLA03-106 but it does not affect calcium phosphate solubilization.

Simulation of use and management effects on the soil organic matter pools of the atlantic forest biome, Brazil / Simulação dos efeitos do uso e manejo sobre os compartimentos da matéria orgânica no solo no bioma da florestal atlântica, Brasil

Soil organic matter simulation in areas under long term use provides an important tool to test future scenarios, enabling the adoption of less impressive management to environment. The purposes of the present study were: a) to simulate, with the Century model, the impacts on soil organic matter, according to the adoption of different crop management, with forage purposes, in two different soils and; b) to validate the Century model for these managements and soils by comparing the simulated values with those measured in the field. The following treatments were evaluated: in the Oxisol area ­ brachiaria pasture with fertilizer (BPw) and without fertilizer (BPwo), the Incept area ­ corn for silage (CS), Coast Cross pasture (CC) and sugar cane field (SC). The microbial biomass represented the active compartment of carbon and nitrogen, the particle free light fraction represented the slow compartment of carbon and nitrogen and the passive pools were determined by the difference of the total minus the active and the slow pools (passive = total ­ (active + slow)). The Century model showed great potential to simulate the dynamics of the total C and N stocks for tropical soils, which was confirmed by similarity between the simulated values and those measured in the field.

Simulação da matéria orgânica no solo em longo prazo é uma ferramenta importante para testar cenários futuros, permitindo a adoção de uma gestão menos impactante ao meio ambiente. Os objetivos do presente estudo foram: (a) simular o modelo do CENTURY, com os impactos sobre a matéria orgânica do solo em função do manejo diferente em culturas com fins de forragem em dois solos diferentes e, (b) comparar o estoque simulado com os reais de matéria orgânica, medidos no campo. Foram avaliados os seguintes tratamentos: na área de Latossolo Vermelho em uso de pastagem com fertilizantes (BPW) e sem fertilizante (BPwo), no Cambissolo - testou os usos com milho para silagem (CS), e pastagem com coast cross (CC) e um plantio de cana-de-açúcar (SC). A biomassa microbiana ativa representa compartimento de carbono e do nitrogênio, a fração leve livre de partículas representada o compartimento lento do carbono e de nitrogênio e os compartimentos passivos foram determinadas pela diferença do total menos o ativo e os compartimentos lentos (Passivo Total = - Ativo + Lento). O modelo Century demonstrou grande potencial para simular a dinâmica do C total e estoques de N para solos tropicais, o que foi comprovado por semelhança entre os valores simulados e medidos no campo.

Metais poluentes e micronutrienes em solos, sob pecuária leiteira em sistema de pastejo direto, no alto da bacia do Rio Paranaíba, Goiás, Brasil / Heavy metals and micronutrients in soils under dairy grazing right on top of the river paranaíba basin in the state of Goiás, Brazil

A preocupação quanto à contaminação do ambiente por meio da atividade leiteira está relacionada ao fato dos dejetos destes bovinos apresentarem metais poluentes em sua constituição; na criação desses animais no sistema de pastejo direto questiona-se a possibilidade da ocorrência de contaminação por estes metais nas aguadas, área onde esses animais se aglomeram em determinados períodos do dia para beberem água e onde defecam. O presente estudo objetivou avaliar os teores dos metais cobre, ferro, manganês, zinco, cádmio, chumbo e cromo em áreas de aguadas e em áreas preservadas (testemunha) de 28 propriedades, agrupadas em seis Ottobacias hidrográficas formadoras do alto da bacia do Rio Paranaíba, no Estado de Goiás. As amostras simples de solos foram coletadas em três profundidades (0-10, 10-20 e 20-30 cm), a partir destas foram obtidas uma amostra composta para cada profundidade nas áreas de aguadas e preservadas. Pela análise de PCA os metais poluentes analisados nos solos de aguada não indicou a ocorrência de contaminação nestes ambientes quando comparados à área preservada. A distribuição aleatória dos teores médios dos metais nas três profundidades estudadas em todos os tratamentos dificulta a definição do potencial de contaminação do solo pelos dejetos originados da atividade leiteira em áreas de aguadas, sob pastejo direto.

In Brazil, the agricultural activity is among the most competitive sectors of national economy, in which milk production has a very significant contribution. Concern about environmental contamination by this activity is related to the fact that dairy cattle manure heavy metals present in the constitution; the creation of such animals in the grazing system directly questions the possibility of any contamination by these metals in the watery, area where these animals congregate at certain times of day for drinking water and where they defecate. This study aimed to evaluate the content of copper, iron, manganese, zinc, cadmium, lead and chromium in watery areas and in conservation areas (control) of 28 properties, grouped into six "otto-basins" forming the upper basin of the Paranaíba River in the State of Goiás. The simple soil samples were collected at three depths (0-10, 10-20 and 20-30 cm) obtained from such a composite sample for each depth in the areas watered and preserved. The analysis of PCA metals pollutants in soils watery areas analyzed did not indicate the occurrence of contamination in these environments when compared to the preserved area. Observed random distribution of average levels of metals in the three studied depths in all treatments, which complicates the definition of the potential for soil contamination by feces of dairy farming originated in watery areas, under rotational grazing.

Influência dos constituintes do esgoto no colapso de um solo arenoso / The influence of sewage constituents in sandy soil collapse

Este trabalho analisa o comportamento colapsível de um solo tropical arenoso inundado com diferentes fluidos de saturação que constituem o esgoto doméstico. Para tal análise, foram levados em consideração parâmetros físicos e químicos e aspectos estruturais do solo no âmbito do fenômeno da colapsibilidade dos solos, assim como as principais características dos fluidos de inundação de água destilada, esgoto doméstico e algumas soluções à base de substâncias que compõem os esgotos e as deformações axiais do solo a um metro de profundidade em ensaios edométricos. As propriedades físicas e químicas dos fluidos de inundação e dos solos, bem como a combinação entre tais propriedades, desempenham relevante papel na compreensão do fenômeno do colapso, mostrando que a sua ocorrência não pode ser atribuída a um ou outro parâmetro do solo ou do fluido isoladamente.

This article evaluates the collapsible behavior of a tropical sandy soil when exposed to different sewage constituent fluids as wetting fluids. The analysis considers the physical, chemical and structural properties of the soil, as well as soil collapsible behavior, the properties of wetting fluids distilled water, domestic sewage, and some solutions composed by substances that constitute sewage, measuring soil deformation in axial compression edometric tests. The physical and chemical properties of fluids and of the soil, as well as their combination, play a relevant role in the comprehension of collapse phenomena, which shows that its occurrence can not be attributed to isolated parameters of soil or fluid.

Cronología de la regeneración del bosque tropical seco en Santa Rosa, Guanacaste, Costa Rica: II. La vegetación en relación con el suelo

Chronology of tropical dry forest regeneration in Santa Rosa, Guanacaste, Costa Rica. II. Vegetation in relation to the soil. Tropical dry forest (TDF) succession was monitored in Santa Rosa, Costa Rica. We analyzed the effect of soil type on forest structure and diversity. Eight seasonally-dry TDF sites located along a successional chrono-sequence (10, 15, 20, 40, 60 and >100 years) were examined in relation to 17 soil pedons and six soil orders. Soils had moderate to high fertility and were classified as Entisols and Vertisols, although Mollisols, Alfisols, Inceptisols and Ultisols were also present. One-hundred and thirty 500 m2 plots were established, 20 plots in secondary and 10 plots in mature TDFsites. Diameter at breast height (dbh) and total tree height were measured for saplings (dbh ≥1 and <5 cm), shrubs and trees (dbh ≥5 cm). With the exception of two sites (40 and 60 years), soil type did not have significant effects on forest structure. However, tree diversity measured with Shannon-Wiener’s H’ and Fisher’s α rarefaction curves, showed substantial differences among soil types, which became accentuated in mature forests. This pattern might be explained by non-random distributions of TDF trees, the scale of the study, the plot shape, and the use of systematic sampling designs. Low-fertility sites in general had higher species richness, consistent with idea that more restrictive soils reduce competition among trees and allow co-existence of species with contrasting growth rates. Changes in soil properties along a chrono-sequence of Entisols indicated that trees may experience more severe water stress as succession progresses, which may require adjustments in biomass allocation and phenological behavior of the dominant species. Our results suggest that edaphic specialization is more pronounced in mature TDF forests, and that most TDF trees are generalists in relation to soil type, highly tolerant to site heterogeneity, and show little physiological specializations in response to edaphic heterogeneity. Rev. Biol. Trop. 57 (3): 817-836. Epub 2009 September 30.

Se estudió la sucesión del bosque tropical seco (BTS) de Santa Rosa, Guanacaste, Costa Rica, en cinco sitios boscosos secundarios y tres bosques maduros. Se analizó el efecto de la clase de suelo sobre la estructura del bosque y la diversidad de especies arbóreas. Los ocho sitios sucesionales estaban localizados a lo largo de una cronosecuencia de regeneración (10, 15, 20, 40, 60 and >100 años) en la que se identificaron 17 pedones y seis órdenes de suelos con moderada a alta fertilidad, clasificados como Entisoles y Vertisoles, aunque los Mollisoles, Alfisoles, Inceptisoles y Ultisoles estuvieron presentes también. Se establecieron 130 parcelas de 10 por 50 m (0.05 ha), 20 en cada bosque secundario y 10 en cada bosque antiguo (6.5 ha en total), de acuerdo con la topografía. Se midió el diámetro a la altura de pecho (dap) de todos los individuos presentes en cada parcela, la altura dominante y el área basal (m2ha-1), usando dos poblaciones: latizales (dap ≥ 1 y < 5 cm) y árboles (dap ≥ 5 cm). Cada bosque presentó al menos dos pedones de suelo bien diferenciados. La alta variación edáfica encontrada se debió posiblemente al origen piroclástico de la meseta ignimbrítica de Santa Rosa, las variaciones en los tiempos de deposición del material parental, y los patrones de erosión. A excepción de dos sitios, no se presentaron diferencias importantes en la estructura del bosque entre las clases de suelos examinadas, según la densidad de individuos, el área basal y la altura dominante. La diversidad de especies arbóreas medida según el índice Shannon-Wiener y las curvas de rarefacción construidas con el índice α de Fisher, presentaron diferencias considerables entre las clases de suelos. Esta tendencia se explicó por la influencia de las características edáficas sobre las distribuciones no aleatorias de las especies arbóreas, la escala de medición del estudio, la forma de la parcela, y el muestreo sistemático utilizado. En general, los suelos de menor fertilidad presentaron mayor riqueza de especies, indicando que los sitios más restrictivos redujeron la competencia y permitieron la coexistencia de individuos con tasas de crecimiento disímiles. Los cambios en las propiedades físicas encontrados a lo largo de una cronosecuencia de Entisoles indicaron que los árboles podrían experimentar estrés hídrico más severo conforme la sucesión avanza, lo que podría requerir ajustes en el comportamiento fenológico y en las propiedades ecofisiológicas de las especies dominantes. En general, nuestros resultados sugieren que la especialización edáfica es más pronunciada en BTS maduros, y que la mayoría de las especies del BTS son generalistas en relación con la clase de suelo, altamente tolerantes a la heterogeneidad de los sitios, y muestran poca especialización fisiológica para responder a la variabilidad edáfica en distancias cortas.

Comparison of Polycyclic Aromatic Hydrocarbon (PAHs) concentrations in urban and natural forest soils in the Atlantic Forest (São Paulo State)

Studies about pollution by Polycyclic Aromatic Hydrocarbons (PAHs) in tropical soils and Brazil are scarce. A study was performed to examine the PAHs composition, concentrations and sources in red-yellow Oxisols of remnant Atlantic Forest of the São Paulo State. Sampling areas were located in an urban site (PEFI) and in a natural one (CUNHA).The granulometric composition, pH, organic matter content and mineralogical composition were determined in samples of superficial soils. The sum of PAHs (ΣHPAs) was 4.5 times higher in the urban area than in the natural one. Acenaphthylene, acenaphthene, fluorene, phenanthrene and fluoranthene have been detected in the soils of both areas and presented similar concentrations. Acenaphthene and fluorene were the most abundant compounds. Pyrene was twice more abundant in the soils of natural area (15 µg.kg-1) than of the urban area and fluoranthene was the dominant compound (203 µg.kg-1) in urban area (6.8 times higher than in the natural area). Some compounds of higher molecular weight, which are tracers of vehicular emissions showed significant concentrations in urban soils. Pyrene represented 79 percent of ΣPAHs whereas it has not been detected in natural soils. The results showed that forest soils in urban area are characterized by the accumulation of high molecular weight compounds of industrial and vehicular origin.

Estudos sobre a poluição por Hidrocarbonetos Policíclicos Aromáticos (HPAs) são escassos em solos tropicais e no Brasil. Um estudo foi realizado para examinar a composição, as concentrações e fontes de HPAs encontrados em Latossolos vermelho-amarelo (Oxissolos), remanescentes de Mata Atlântica no Estado de São Paulo. As áreas de estudos localizaram-se em um sítio urbano (PEFI) e um natural (CUNHA). A composição granulométrica, pH, teor de matéria orgânica e composição mineralógica foram determinados em amostras de solo superficial. A soma dos HPAs analisados (ΣHPAs) foi 4,5 vezes mais elevada na área urbana do que na área natural. Acenaftileno, acenafteno, fluoreno, fenantreno e fluoranteno foram detectados, em concentrações similares, nos solos das duas áreas. Acenafteno e fluoreno foram os compostos mais abundantes. O pireno foi duas vezes mais abundante no solo da área natural (15 µg.kg-1), e o fluoranteno foi o composto dominante (203 µg.kg-1) na área urbana (6,8 vezes mais elevado que na área natural). Alguns compostos de alto peso molecular, traçadores de emissões veiculares, foram detectados em quantidades significativas no solo da área urbana. O pireno representou 79 por cento da ΣHPAs, enquanto que não foi detectado na área natural. Estes resultados evidenciaram que os solos de floresta em áreas urbanas são caracterizados pela acumulação de HPAs pesados oriundos de emissões industriais e veiculares.

Carbono orgânico nas frações granulométricas e substâncias húmicas de um Latossolo Vermelho Amarelo distrófico - LVAd sob diferentes agrossistemas

This study aimed to assess the total organic carbon content in chemical and granulometric fraction of an Oxisol from four different land use systems. The soil samples were collected in Juruena and Juara, Mato Grosso (Brazil), and prepared for the physical and chemical fractionations. The results indicated that different land use systems caused significative carbon content changing in both humic substances and granulometric fraction. It was observed from the differentiated concentration of humine and free fulvic acids for each system. The distribution of total organic carbon in the granulometric fraction 53 m was higher than fraction > 53 m for all land use, indicating greater presence of organic material in the silt and clay.

No presente estudo foram avaliados os teores de carbono orgânico total nas frações húmicas e granulométricas de um Latossolo Vermelho Amarelo distrófico sob quatro sistemas de uso: Floresta nativa (FL), agrossilvopastoril (SS), agroflorestal (SA) e pastagem (PA), na região norte mato-grossense. As amostras do solo foram coletadas em Juruena e Juara, Mato Grosso e preparadas para posterior fracionamento físico e químico. Os resultados indicaram que os diferentes sistemas de uso do solo influenciaram diretamente na quantidade de carbono orgânico total das frações granulométricas e das substâncias húmicas dos solos. O sistema agrossilvopastoril apresentou pronunciada diferenciação em relação aos demais sistemas estudados, principalmente quanto à concentração de humina e ácidos fúlvicos livres. A distribuição do carbono orgânico total na fração granulométrica fina ( 53 m) foi superior a da fração grosseira (> 53 m) para todos os agrossistemas, indicando maior presença de material orgânico agregado ao silte e argila.

Relationship between the mass of organic matter and carbon in soil

The quantity of soil organic matter (SOM) was estimated through the determination of soil organic carbon (SOC) times a factor, which assumes that 58 percent of the SOM was formed by carbon. A number of soil samples with wide range of SOC content collected in the state of Paraná, Brazil were evaluated in the laboratory. SOC was measured by Walkley-Black method and the total SOM by loss on ignition. The SOC was positively correlated with SOM. The SOM/SOC ratio varied from 1.91 to 5.08 for the soils. It shows that Brazilian SOM has greater oxidation degree. Although, the SOM and SOC decreased with soil depth the SOM/SOC ratio increased. It showed that SOM in the subsoil contained more oxygen but less carbon than the SOM in the upper soil surface. The CEC/SOC also increased with depth indicating that the functional groups of the SOM increased per unity of carbon.

O teor de matéria orgânica do solo (MOS) é estimado pelo conteúdo de carbono orgânico do solo (COS) vezes um fator, decorrente do pressuposto de que 58 por cento da MOS é formada por carbono. Amostras de solos apresentando grande variação no teor de COS foram avaliadas no laboratório. O COS foi determinado pelo método de Walkley-Black (WB) e a MOS pela perda de massa por ignição (PMI). A MOS foi positivamente correlacionada com o COS. A relação MOS/COS variou de 1,91 a 5,08. Este resultado mostra que a MOS brasileiros apresentam maior grau de oxidação. Embora a MOS e o COS tenham diminuído a relação MOS/COS aumentou com a profundidade do solo. Este resultado demonstrou que a MOS da subsuperfície contem mais oxigênio e menos carbono que a MOS da superfície do solo. A relação CTC/COS também aumentou com a profundidade, indicando um aumento nos grupos funcionais da MOS por unidade de carbono.

Amazon landforms and soils in relation to biological diversity

Thirteen main landform units are distinguished for the whole of the forested Amazon region, each with its specific soil pattern and vegetation structure. These landform-soil-vegetation units are delineated on a small-scale map and illustrated by a schematic cross-section. Floristic diversity of the gamma type is to be highest on the steepland-and-valley complexes of the Andean fringe, on the crystalline shield uplands, on the inselberg complexes, and on the eutric variant of the western sedimentary plains. Endemism is expected to be highest on the sandy plains, and parts of the table lands and inselberg complexes. Speciation, linked to the concept of forest refuge areas, is likely to be highest on the sandstone table lands, on the stretches of Amazon planalto, and in the areas of relict valleys, in view of the prolonged geomorphological stability of these units.

Foram distinguidas treze unidades de paisagens maiores, em toda região Amazônica florestada, cada unidade com padrão de solos e estrutura de cobertura vegetal específica. Estas unidades de paisagem-solos-vegetação foram delineadas num mapa geral da região e ilustradas por um corte transversal esquemático. A diversidade florística, do tipo gamma, deve ser a mais alta no complexo paisagístico da Selva Alta, bordeando a Cordilheira Andina; nas terras firmes colinosas dos escudos cristalinos; no complexo de inselbergs, e no variante eutrico das terras firmes sedimentárias ocidentais. Estima-se que o endemismo seja mais alto nas planícies arenosas, e em partes dos complexos de chapadões e de inselbergs. Especiação, ligada com o conceito de refúgios florestais, é provavelmente mais alta nos chapadões de areniscos antigos, nas extensões do planalto Amazônico, e nas áreas de vales relictos, considerando a estabilidade geomorfológica prolongada destas unidades.