Structural changes in latosols of the cerrado region: I - relationships between soil physical properties and least limiting water range

The agricultural potential of Latosols of the Brazilian Cerrado region is high, but when intensively cultivated under inappropriate management systems, the porosity can be seriously reduced, leading to rapid soil degradation. Consequently, accelerated erosion and sedimentation of springs and creeks have been observed. Therefore, the objective of this study was to evaluate structural changes of Latosols in Rio Verde, Goiás, based on the Least Limiting Water Range (LLWR), and relationships between LLWR and other physical properties. Soil samples were collected from the B horizons of five oxidic Latosols representing the textural variability of the Latosols of the Cerrado biome. LLWR and other soil physical properties were determined at various soil compaction degrees induced by uniaxial compression. Soil compaction caused effects varying from enhanced plant growth due to higher water retention, to severe restriction of edaphic functions. Also, inverse relationships were observed between clay content and bulk density values (Bd) under different structural conditions. Bd values corresponding to critical soil macroporosity (BdcMAC) were more restrictive to a sustainable use of the studied Latosols than the critical Bd corresponding to LLWR (BdcLLWR). The high tolerable compression potential of these oxidic Latosols was related to the high aeration porosity associated to the granular structure.

Highlands of the upper Jequitinhonha valley, Brazil: II - mineralogy, micromorphology, and landscape evolution¹

Palm swanp formations, the so-called veredas, typically occur in the Brazilian biome known as "Cerrado" (savanna-like vegetation), especially on flattened areas or tablelands (chapadas). The aim of this study was to characterize the mineralogy and micromorphology of soil materials from a representative toposequence of the watershed of the vereda Lagoa do Leandro, located in Minas Novas, state of Minas Gerais, Brazil, on plains in the region of the upper Jequitinhonha valley, emphasizing essential aspects of their genesis and landscape evolution. The toposequence is underlain by rocks of the Macaúbas group and covered with detrital and metamorphic rocks (schists of Proterozoic diamictites). The soil profiles were first pedologically described; samples of the disturbed and undisturbed soils were collected from all horizons for further micromorphological and mineralogical analyses. The mineralogical analysis was mainly based on powder X ray diffractometry (XRD) and micromorphological descriptions of thin sections under a petrographic microscope. The soils from the bottom to the top of this toposequence were classified as: Typic Albaquult (GXbd), Xanthic Haplustox, gray color, here called "Gray Haplustox" ("LAC"), Xanthic Haplustox (LA) and Typic Haplustox (LVA). The clay mineralogy of all soils was found to be dominated by kaolinite. In soil of LA and LVA, the occurrence of goethite, gibbsite, and anatase was evidenced; "LAC" also contained anatase and the GXbd, illite, anatase, and traces of vermiculite. The micromorphological analyses of the LVA, LA and "LAC" soils showed the prevalence of a microaggregate-like or granular microstructure, and aggregate porosity has a stacked/packed structure, which is typical of Oxisols. A massive structure was observed in GXbd material, with the presence of illuviation cutans of clay minerals and iron compounds. Paleogleissolos, which are strongly weathered, due to the action of the excavating fauna , and resulted in the present "LAC". The GXbd at the base of the vereda preserved the physical, mineralogical and micromorphological properties that are typical of a pedogenesis with a strong influence of long dry periods.

Inter-relation between soybean yield and soil compaction under degraded pasture in Brazilian Savannah

The Cerrado (Brazilian Savannah) plays an important economic and financial role in the nation, since the pastures of this biome feed cattle for half of the domestic bovine meat productivity, and its agricultural fields produce a third of the country's grain. The variability and spatial dependence between the soil physical attributes and soybean yield were evaluated in a crop rotation planted on a degraded brachiaria pasture, on a dystroferric Red Latosol of an experimental farm of the State University of São Paulo (UNESP), in the 2005/2006 growing season. The linear and spatial correlations between these attributes were also studied, to determine conditions that would allow increased agricultural productivity. In the above pasture area, a grid was installed with 124 plots, spaced 10.0 x 10.0 m and 5.0 x 5.0 m apart, in a total area of 7,500 m². From the linear and spatial point of view, the high grain yield can be explained by the number of grains per plant and soil macroporosity. The high variability observed for most soil properties indicated that the crop - livestock integration system results in environmental heterogeneity of the soil.

Characterization and classification of soils in the Taquari river basin - Pantanal region, state of Mato Grosso do Sul, Brazil

Among the soils in the Mato Grosso do Sul, stand out in the Pantanal biome, the Spodosols. Despite being recorded in considerable extensions, few studies aiming to characterize and classify these soils were performed. The purpose of this study was to characterize and classify soils in three areas of two physiographic types in the Taquari river basin: bay and flooded fields. Two trenches were opened in the bay area (P1 and P2) and two in the flooded field (P3 and P4). The third area (saline) with high sodium levels was sampled for further studies. In the soils in both areas the sand fraction was predominant and the texture from sand to sandy loam, with the main constituent quartz. In the bay area, the soil organic carbon in the surface layer (P1) was (OC) > 80 g kg-1, being diagnosed as Histic epipedon. In the other profiles the surface horizons had low OC levels which, associated with other properties, classified them as Ochric epipedons. In the soils of the bay area (P1 and P2), the pH ranged from 5.0 to 7.5, associated with dominance of Ca2+ and Mg2+, with base saturation above 50 % in some horizons. In the flooded fields (P3 and P4) the soil pH ranged from 4.9 to 5.9, H+ contents were high in the surface horizons (0.8-10.5 cmol c kg-1 ), Ca2+ and Mg² contents ranged from 0.4 to 0.8 cmol c kg-1 and base saturation was < 50 %. In the soils of the bay area (P1 and P2) iron was accumulated (extracted by dithionite - Fed) and OC in the spodic horizon; in the P3 and P4 soils only Fed was accumulated (in the subsurface layers). According to the criteria adopted by the Brazilian System of Soil Classification (SiBCS) at the subgroup level, the soils were classified as: P1: Organic Hydromorphic Ferrohumiluvic Spodosol. P2: Typical Orthic Ferrohumiluvic Spodosol. P3: Typical Hydromorphic Ferroluvic Spodosol. P4: Arenic Orthic Ferroluvic Spodosol.

N2O emissions from a cultivated mollisol: optimal time of day for sampling and the role of soil temperature

The correct use of closed field chambers to determine N2O emissions requires defining the time of day that best represents the daily mean N2O flux. A short-term field experiment was carried out on a Mollisol soil, on which annual crops were grown under no-till management in the Pampa Ondulada of Argentina. The N2O emission rates were measured every 3 h for three consecutive days. Fluxes ranged from 62.58 to 145.99 ∝g N-N2O m-2 h-1 (average of five field chambers) and were negatively related (R² = 0.34, p < 0.01) to topsoil temperature (14 - 20 ºC). N2O emission rates measured between 9:00 and 12:00 am presented a high relationship to daily mean N2O flux (R² = 0.87, p < 0.01), showing that, in the study region, sampling in the mornings is preferable for GHG.

Filiação entre arenitos da formação Guará e sua cobertura pedológica no Rio Grande Do Sul

As regiões oeste e sudoeste do Rio Grande do Sul, RS, destacam-se pela ocorrência de extensas áreas com solos frágeis desenvolvidos sobre sedimentos arenosos continentais do Mesozoico da Bacia do Paraná. O uso inadequado das terras tem acelerado o processo de arenização sobre essas áreas. Nesse caso, o conhecimento dos solos é fundamental para a seleção de práticas adequadas de manejo visando a sua sustentabilidade. Os objetivos deste trabalho foram entender a evolução e estabelecer a relação, em termos de filiação, entre a rocha e sua respectiva cobertura pedológica por meio de perfis desenvolvidos sobre os arenitos da Formação Guará no RS. Foram realizadas análises químicas, físicas, mineralógicas e morfológicas em dois perfis de Cambissolos Háplicos e um perfil de Argissolo Vermelho. Verificaram-se indícios de adição externa de materiais aos perfis estudados, principalmente ilmenita, oriunda da alteração de áreas com rochas vulcânicas básicas circunvizinhas. O aporte de material alóctone nos perfis estudados é responsável pela pedogênese de horizontes B com incremento de argila, característicos de Argissolos e Cambissolos. Os dados sugerem a identificação e interpretação de um sexto componente pedogenético definido como contexto geológico do entorno.

Partição de substâncias húmicas em solos brasileiros

As substâncias húmicas (SH) representam o principal reservatório de carbono orgânico total do solo (COT) e sua partição entre diferentes frações de solubilidade em meio alcalino ou ácido pode guardar relação com o tipo de solo e manejo adotado. O objetivo deste trabalho foi comparar a partição das SHs, de acordo com profundidade, tipo de solo, bioma e uso do solo no Brasil. Revisou-se a literatura, incluindo teses, dissertações, artigos e resumos em anais de eventos, em busca de dados sobre o teor de COT, sua porcentagem como ácidos húmicos (AH), ácidos fúlvicos (AF) e humina (HU) e a razão AH/AF. Os dados foram estratificados por intervalos comparáveis de profundidades (0-5, 5-10, 0-20, 20-50, 50-100 e >100 cm), biomas (Mata Atlântica, Cerrado, Amazônia, Pampa e Caatinga), ordem de solo (Argissolo, Latossolo, Cambissolo, Planossolo, Neossolo, Gleissolo e Organossolo) e principais usos do solo (florestas nativas, pastagem natural, pastagem plantada, eucalipto, culturas perenes e anuais). Os dados foram analisados por estatística descritiva, correlações de Spearman e análise de componentes principais (ACP). Nos Argissolos, Latossolos e Organossolos, a fração HU contribuiu com metade do COT, tendendo a diminuir em profundidade. Para Latossolos e Organossolos, a fração AF tendeu a aumentar em profundidade. Em Neossolos, a fração AH aumentou em profundidade, embora tenha diminuído em Gleissolos e Planossolos. A razão AH/AF geralmente diminui em profundidade. Pela ACP, não foi possível identificar um padrão de agrupamento das amostras em razão do tipo de bioma e uso do solo, sugerindo que a partição das SHs tem baixo potencial como indicador de efeitos do manejo ou condições ambientais, embora seja útil para discriminar processos de humificação em algumas ordens de solo.

Impacts of deforestation on water balance components of a watershed on the Brazilian East Coast

The Brazilian East coast was intensely affected by deforestation, which drastically cut back the original biome. The possible impacts of this process on water resources are still unknown. The purpose of this study was an evaluation of the impacts of deforestation on the main water balance components of the Galo creek watershed, in the State of Espírito Santo, on the East coast of Brazil. Considering the real conditions of the watershed, the SWAT model was calibrated with data from 1997 to 2000 and validated for the period between 2001 and 2003. The calibration and validation processes were evaluated by the Nash-Sutcliffe efficiency coefficient and by the statistical parameters (determination coefficient, slope coefficient and F test) of the regression model adjusted for estimated and measured flow data. After calibration and validation of the model, new simulations were carried out for three different land use scenarios: a scenario in compliance with the law (C1), assuming the preservation of PPAs (permanent preservation areas); an optimistic scenario (C2), which considers the watershed to be almost entirely covered by native vegetation; and a pessimistic scenario (C3), in which the watershed would be almost entirely covered by pasture. The scenarios C1, C2 and C3 represent a soil cover of native forest of 76, 97 and 0 %, respectively. The results were compared with the simulation, considering the real scenario (C0) with 54 % forest cover. The Nash-Sutcliffe coefficients were 0.65 and 0.70 for calibration and validation, respectively, indicating satisfactory results in the flow simulation. A mean reduction of 10 % of the native forest cover would cause a mean annual increase of approximately 11.5 mm in total runoff at the watershed outlet. Reforestation would ensure minimum flows in the dry period and regulate the maximum flow of the main watercourse of the watershed.

SPATIAL VARIABILITY AND VITALITY OF EPIGEOUS TERMITE MOUNDS IN PASTURES OF MATO GROSSO DO SUL, BRAZIL

Epigeous termite mounds are frequently observed in pasture areas, but the processes regulating their population dynamics are poorly known. This study evaluated epigeous termite mounds in cultivated grasslands used as pastures, assessing their spatial distribution by means of geostatistics and evaluating their vitality. The study was conducted in the Cerrado biome in the municipality of Rio Brilhante, Mato Grosso do Sul, Brazil. In two pasture areas (Pasture 1 and Pasture 2), epigeous mounds (nests) were georeferenced and analyzed for height, circumference and vitality (inhabited or not). The area occupied by the mounds was calculated and termite specimens were collected for taxonomic identification. The spatial distribution pattern of the mounds was analyzed with geostatistical procedures. In both pasture areas, all epigeous mounds were built by the same species, Cornitermes cumulans. The mean number of mounds per hectare was 68 in Pasture 1 and 127 in Pasture 2, representing 0.4 and 1 % of the entire area, respectively. A large majority of the mounds were active (vitality), 91 % in Pasture 1 and 84 % in Pasture 2. A “pure nugget effect” was observed in the semivariograms of height and nest circumference in both pastures reflecting randomized spatial distribution and confirming that the distribution of termite mounds in pastures had a non-standard distribution.

Cambios en la vegetacion de un campo abandonado despues de un cultivo de trigo

La vegetación prístina de los campos altos del sur de Santa Fe (Argentina) son distintos tipos de flechillares caracterizados por la abundancia de varias especies del género Stipa. Cuando un campo agrícola se abandona suele revertir a las comunidades prístinas. El objeto de este trabajo es analizar los diez primeros años de la sucesión secundaria de un campo sometido a agricultura durante largo tiempo que se abandonó después de un cultivo de trigo (Triticum aestivum). En el primer año aparece trigo acompañado de malezas anuales (Chenopodium album y Portulaca oleracea); después del primer año una parcela fue colonizada por Baccharis salicifolia y las otras por Carduus acanthoides, Cerastium glomeratum, Ammi majus, etc. Los últimos años constituyen una etapa en la que disminuye la diversidad y se establece una fuerte dominancia de Baccharis salicifolia o Carduus acanthoides. El Sorgo de Alepo (Sorghum halepense) aparece en las etapas tempranas y perdura durante todo el período con valores altos de abundancia. Aún, prácticamente no han aparecido especies de los flechillares, por lo tanto se concluye que no ha transcurrido suficiente tiempo para que se regenere el flechillar, o porque sus especies no se encuentran en los bancos de semillas o en las proximidades.

Adaptabilidade e estabilidade do rendimento de grãos de genótipos de feijão

Efetuaram-se análises de adaptabilidade e estabilidade do rendimento de grãos de onze genótipos de feijão (Phaseolus vulgaris L.) de ensaios conduzidos em 23 municípios do Rio Grande do Sul, de 1988/89 a 1993/94, compreendendo 72 ambientes, visando identificar genótipos mais adequados para cultivo no Estado e utilização em programas de melhoramento. Foram avaliados os genótipos Rio Tibagi, Guateian 6662, EMPASC 201, FT 120, Macanudo, Pampa, Minuano, Macotaço, CNF 5491, Carioca e Iraí. Utilizou-se o método de regressão linear segmentada com estimação da junção dos segmentos. A ausência de alterações significativas das taxas de respostas lineares individuais dos genótipos indicou o método de regressão linear simples como mais apropriado. Os genótipos apresentaram desvios de regressão significativos, caracterizando instabilidade fenotípica. Iraí mostrou instabilidade superior às dos demais. Os genótipos diferiram quanto à produtividade média e à taxa de resposta, classificando-se como: Minuano, Macotaço, CNF 5491 e Macanudo, adaptabilidade geral; Rio Tibagi, Pampa e Iraí, pobremente adaptados a todos ambientes; Guateian 6662 e EMPASC201, adaptação específica a ambientes pobres e FT 120 e Carioca, adaptação média a todos ambientes. Destacaram-se Minuano, Macotaço, CNF 5491 e Macanudo, como mais produtivos e melhor adaptados aos ambientes considerados. Esses genótipos, aparentados, apresentaram adaptabilidade semelhante entre si e diferente dos demais e estabilidade não diferenciada em relação a alguns.

Avaliação de espaçamentos e populações de plantas de feijão visando à colheita mecanizada direta

O trabalho foi conduzido na safra 1992/93, no Centro Agropecuário Palma (CAP)/Universidade Federal de Pelotas (UFPel), objetivando avaliar o efeito da variação do espaçamento entre linhas e da população de plantas sobre características agronômicas relacionadas com a colheita mecanizada de feijoeiro (Phaseolus vulgaris L.). Foram testados três espaçamentos entre linhas (25, 50 e 75 cm) e quatro populações de plantas/ha (100, 200, 350 e 500 mil), utilizando como reagente a cultivar Pampa, de hábito de crescimento indeterminado, tipo II. O delineamento experimental foi em blocos casualizados, com quatro repetições. Somente ocorreu interação entre os fatores para o índice de acamamento, onde o aumento da população tendeu a reduzi-lo. A combinação do maior espaçamento com a menor população provocou o maior acamamento. A redução no espaçamento entre linhas, apesar de reduzir a altura de plantas, a altura de inserção de vagens e o rendimento de grãos, provocou aumento na altura da ponta da vagem mais baixa até o solo, e redução na porcentagem de plantas com vagens encostando no solo. O aumento na população de plantas, apesar de não afetar a maioria das características agronômicas das plantas, provocou redução na porcentagem de plantas com vagens encostando no solo, e não provocou modificações no rendimento de grãos.

Bases genéticas de milho e alterações no plano experimental

Resultados experimentais seguros exigem um plano experimental apropriado, obtido através da utilização de adequado tamanho e forma de parcelas, número de repetições e de amostras. O objetivo deste trabalho foi avaliar a influência de diferentes bases genéticas de milho, híbrido simples (DAS 9560), duplo (AG 6018), triplo (AG 303) e variedade cultivada (Pampa), sobre a estimativa do tamanho de parcela experimental e do número de repetições. O delineamento experimental foi de blocos ao acaso com quatro repetições e amostragem nas parcelas. As parcelas experimentais foram constituídas por oito fileiras com 12 metros de comprimento, formando 96 unidades básicas. O tamanho de parcela e o número de repetições foram estimados por meio dos métodos de Lessman & Atkins e de Hatheway. O tamanho ótimo de parcela variou entre 4,5 m² (híbrido simples) e 7,2 m² (híbrido duplo). A heterogeneidade do solo e a variabilidade genética influenciam no tamanho ótimo de parcela e número de repetições necessárias.

Detection of Rhynchosporium secalis in barley seeds from Argentina through polymerase chain reaction technique

Leaf scald of barley caused by Rhynchosporium secalis is an important disease in Argentina. The fungus is a necrotrophic pathogen which survives in stubble, seeds and weeds. Isolation of R. secalis from seeds on artificial media usually has not been successful due to the slow growth rate of the pathogen and strong inhibition by contaminants. The objective in this work was to detect R. secalis in different genotypes of barley seeds in Argentina using the polymerase chain reaction (PCR)-based diagnostic assay. Four barley genotypes were tested in 2004: Quilmes Ayelén, Quilmes Alfa, Barke and Maltería Pampa 1004. The previously described RS8 and RS9 primers were used for the detection of R. secalis in barley seeds. A 264-bp single band was obtained for each cultivar showing the presence of R. secalis. The use of specific primers was efficient in the detection of R. secalis in barley seeds in Argentina and could be used for routine diagnosis, epidemiology and seed transmission studies. This is the first report on the detection of R. secalis in barley seeds in Argentina.

What can and should be legalized in ecological restoration?

After listing the five key elements of ecological restoration, ecology, economics, social values, cultural values, and politics, I celebrate the fact that in Brazil there is legislation on how to perform ecological restoration of degraded tropical forests, as well as an ongoing dialogue among legislators and scientists about this legislation, and also a lively debate among scientists as the best way forward, referring to articles by Brancalion et al. (2010) and Durigan et al. (2010) in this issue of Revista Árvore. Legislators elsewhere, especially megadiversity countries, should take note. I do not take sides in the debate; I think both groups of authors make very good points. Instead I call on the scientists and legislators concerned with restoration to ponder five strategic tools: A. Start with clear concepts. B. Decide where you want to go and why. C. Negotiate who should benefit & how, and who should pay, how, & why. D. Work out how an honest cost-benefit analysis of restoration would look, regardless of the biome in which you are working. Finally, figure out how to make the restoration immediately attractive for private landowners. Otherwise, they will not cooperate as fully as they could or should, and restoration efforts will not achieve its full potential.