Micorrização e respiração microbiana do solo sob o cultivo de maracujá e pinhão manso em diferentes regimes hídricos / Mycorrization and microbial respiration in soil under passion fruit and jatropha in different water regimes

Os fungos micorrízicos arbusculares (FMAs) e a população microbiana do solo ocupam papel de destaque em amenizar os efeitos causados pelo estresse hídrico em diversas culturas, entretanto se faz necessário estabelecer parâmetros sobre a dinâmica da interação desses microrganismos com as plantas em condições de estresse. Diante do exposto, o trabalho teve por objetivo avaliar a micorrização ea respiração microbiana do solo cultivado com mudas de maracujá amarelo e pinhão manso submetidas a diferentes níveis de água. O experimento foi realizado em vasos na casa de vegetação localizada na Universidade Estadual de Goiás, unidade de Ipameri. O delineamento utilizado foi inteiramente casualizado, e analisado em um esquema fatorial 2 x 7 sendo duas espécies de plantas (maracujá e pinhão manso) e sete níveis de fornecimento de água (25%, 50%, 75%, 100%, 125%, 150% e 175%) em relação a capacidade de campo (CC) do solo com cinco repetições, totalizando 70 parcelas experimentais de cultivo. Foram avaliadas a respiração microbiana do solo (RM), número de esporos micorrízicos (ESP) e colonização micorrízica (CM). Em termos de RM os solos responderam de forma distinta a alteração da umidade do solo, onde a microbiota do solo com pinhão manso se mostrou mais adaptada até aos 175% da CC que do maracujá. A condição de excesso hídrico provocou uma diminuição no ESP do solo de ambas a culturas, porém com efeito sendo mais significativo na cultura do maracujá que apresentou uma média de 77,2 esporos 50g-1 de solo. A CM do pinhão manso e do maracujazeiro foram afetadas negativamente com o aumento dos níveis de umidade do solo, porém o pinhão manso apresentou em média uma taxa de CM 38,5% maior que o maracujá. De maneira geral a microbiota do solo e os FMAs sob mudas de pinhão manso responderam melhor ao estresse hídrico.(AU)

Arbuscular mycorrhizal fungi (AMF) and the soil microbial population occupy a prominent role in mitigating the effects caused by water stress in several crops. However, it is necessary to establish parameters on the dynamics of the interaction of these microorganisms with plants under stress conditions. Given the above, this study aimed to evaluate the mycorrhization and microbial respiration of soil cultivated with yellow passion fruit and jatropha seedlings subjected to different water levels. The experiment was carried out in pots in a greenhouse located at the State University of Goiás, Ipameri unit. The design used was completely randomized and analyzed in a 2x 7 factorial scheme with two plant species (passion fruit and Jatropha curcas) and seven levels of water supply (25%, 50%, 75%, 100%, 125%, 150% and,175%) in relation to the field capacity (FC) of the soil with five replications, totaling 70 experimental cultivation plots. In addition, soil microbial respiration (MR), number of mycorrhizal spores (SPO) and mycorrhizal colonization (MC) were also evaluated. In terms of MR, the soils responded differently to changes in soil moisture, where the microbiota of the soil with Jatropha curcaswas more adapted up to 175% of CC than that of passion fruit. The excess water condition caused a decrease in the SPOof the soil of both crops, but with an effect being more significant in the passion fruit crop, which presented an average of 77.2 spores 50g-1of soil. The MC of Jatropha curcasand passion fruit were negatively affected with the increase of soil moisture levels, however,the Jatropha curcaspresented an average rate of MC 38.5% higher than the passion fruit. In general, the soil microbiota and the AMF under Jatropha seedlings responded better to water stress.(AU)

Evaluation of Megathyrsus maximus genotypes under water stress conditions

The objective was to evaluate the production of Megathyrsus maximusgenotypes (Syn. Panicum maximum), under different levels of water in the soil. This was a 5x5 factorial completely randomized design conducted in a greenhouse, combining five genotypes of M. maximus(B55, C10 and PM30, cv. Massai and cv. BRS Tamani) and five levels of soil field capacities (20%, 40%, 60%, 100% and 140%), with three replications. Dry matter production was evaluated: leaf, stem, dead material, root, shoot and total dry matters, as well as the number of tillers and leaf:stem and aboveground:root ratios. The qualitative factor (genotypes) was subjected to Duncan test at 5% probability. The quantitative factor (% field capacity) was subjected to regression, adopting 5% as a critical level of probability. There was no interaction between the factors for any of the evaluated characteristics. Significant differences amongthe genotypes were detected for tiller number, dead material dry mass, root and total dry mass and leaf:stem ratio. There was no significant effect of the percentage of field capacity on most of the characteristics, except for leaf:stem and aboveground:root ratios. Cultivar Massai showed the best forage production compared to the other genotypes, regardless of the percentage of field capacity evaluated. In general, the evaluated genotypes were more tolerant to excess water stress than to water deficit.(AU)

Determination of field capacity in the Chibunga and Guano rivers micro-basins.

Background: The micro-basins of the Chibunga and Guano rivers are located within the sub-basin of the Chambo River, which starts at the thaw of the Chimborazo, crosses the cities of Guano and Riobamba, and ends in the Chambo River. These rivers are considered fluvial hydrological forces and geological limits of the aquifer, located in this sub-basin. For this reason, our investigation addressed the field capacity in the micro-basins of Chibunga and Guano rivers, to determine the maximum retention potential, i.e., the saturation of water in the soil. Methods: We investigated the change of precipitation to runoff through the correlations between the characteristics of the soil and its vegetation. We applied the Curve Number (CN) method introduced by the United States Soil Conservation Service (USSCS); this represents an empirical model, which relates the vegetation cover to the geological and topographic conditions of the soil. Along with the geographic information system, the model allows to represent the variation of runoffs for each micro-basin, according to the different land use categories, over the time frame from 2010 to 2014. Results: We found that the maximum retention potential is directly affected by CN values, representing the runoff potential. Highest values of 100 belong to the wetlands, urban area, snow, and water, as rain is converted directly into runoff, being impervious areas. The Guano river micro-basin possesses clay soil with CN of 78, the soil texture for eucalyptus forest is clay loam, and its CN value, 46, is the lowest of the data set. Knowledge of field capacity allows to properly evaluate the storage capacity of soil and water conservation. Conclusions: Results of this work will be useful in the quantification of the water balance, to determine the water supply and demand.

A comprehensive evaluation of pedotransfer functions for predicting soil water content in environmental modeling and ecosystem management.

Many pedotransfer functions (PTFs) have been developed for predicting the soil water content at different matric potentials. The use of these functions has been encouraged because of the time and work typically required for measuring it, while the PTFs require commonly measured soil properties such as sand, silt, clay, organic matter content, or bulk density for predicting water retention. In addition, several environmental and ecosystem management simulation models such as DRAINMOD, HYDRUS, EPIC, SPAW, and WEPP use PTFs for computing soil hydraulic properties. Because of the increasing use of the PTFs and their effect in many soil water simulation and transport models, this study revised and tested 13 different PTFs for predicting soil water content at -33 and -1500 kPa, values usually known as field capacity and wilting point. Three of these PTFs were derived from tropical soils while the rest were developed with soil samples collected across the United States. These PTFs were evaluated in Chilean soils as an independent dataset and their improvement after calibration was assessed with this new data. The results demonstrate that the PTFs performance depends on the soils used for their development as the estimates showed a significant improvement after calibration. When predicting water content, Rawls et al. (2004) was the best function before calibration (RMSE = 0.08 for -33 and -1500 kPa), while Gupta and Larson (1979) was the best after calibration (RMSE of 0.06 and 0.05, and r2 values of 0.69 and 0.66 at -33 and -1500 kPa, respectively). Nonlinear PTFs performed better than linear PTFs when predicting water content at field capacity. Finally, bulk density proved to be the key variable and can be used as footprint for soils changes through time. Organic matter content was also a significant input but improved the estimates for some specific matric potentials and PTFs.

Soil residue analysis and degradation of saflufenacil as affected by moisture content and soil characteristics.

BACKGROUND: Saflufenacil dissipation in soils under different moisture conditions is not available in the scientific literature. The objective of this study was to evaluate saflufenacil degradation and persistence in soils from rice regions under field capacity (non-flooded) and saturated (flooded) conditions. RESULTS: The accelerated solvent extraction (ASE) residue analytical method developed to conduct the study resulted in recovery greater than 80% for the combinations of soils and moisture conditions. Saflufenacil degradation was faster at field capacity for all soils, except for Morey soil. Herbicide half-life was 28.6, 15.0 and 23.1 days under field capacity treatments and 58.8, 36.9 and 79.7 under saturated conditions for Nada, Crowley and Gilbert soils respectively. A half-life no longer than 80 days was observed for the combination of soils and moisture treatments. CONCLUSION: An ASE method was developed and used to extract saflufenacil from soil samples. Half-life averaged among soils was 59 and 33 days for saturated and field capacity respectively. Saflufenacil persistence in the environment was 2-3 times longer under flooded conditions for most of the soils studied.

Exigências de uma semeadora-adubadora de precisão variando a velocidade e a condição da superfície do solo

The objective of the work was to evaluate the performance of a set tractor-four lines seeder, when and operating at different tractor gears and soil tillage, on corn crop planting. The sowing was carried out through in dark-red Oxisoil, eutrophic. The treatments designs had been composites of tillage systems (conventional, reduced and no-tillage) and marches of the set tractor-seeder (5.9 and 7.0km h-1). The experimental delineation was in a randomized blocks design in factorial array of 3 x 2 with 4 replications. The analyzed variables had been: forward speed, field operational capacity, hourly and area fuel consumption, wheels lip, draft force and drawbar power. The speed, the wheels lip and fuel consumption had been higher for gear M2 (7.0km.h-1) when operating in soil prepared by reduced soil tillage also presented greater values fuel consumption and lower speed of sowing.

O objetivo do trabalho foi avaliar o desempenho de um conjunto trator-semeadora-adubadora de quatro linhas, variando as marchas do trator e preparo do solo. A semeadura foi realizada em Latossolo Vermelho Eutroférrico. Os tratamentos foram: preparo do solo (convencional, reduzido e plantio direto) e marchas do trator (5,9km h-1 e 7,0km h-1), em delineamento de blocos casualizados em fatorial 3 x 2 com quatro repetições. Foram analisadas: velocidade de deslocamento, capacidade de campo operacional, consumo de combustível horário e por área, patinagem, força de tração e potência na barra. A velocidade, a patinagem e os consumos de combustível horário e por área foram maiores para a marcha M2 (7,0km h-1) e o conjunto trabalhando em área cujo preparo do solo foi realizado com escarificador apresentou maiores valores para os consumos de combustível horário e por área e também menor velocidade operacional.

Exigências de uma semeadora-adubadora de precisão variando a velocidade e a condição da superfície do solo

The objective of the work was to evaluate the performance of a set tractor-four lines seeder, when and operating at different tractor gears and soil tillage, on corn crop planting. The sowing was carried out through in dark-red Oxisoil, eutrophic. The treatments designs had been composites of tillage systems (conventional, reduced and no-tillage) and marches of the set tractor-seeder (5.9 and 7.0km h-1). The experimental delineation was in a randomized blocks design in factorial array of 3 x 2 with 4 replications. The analyzed variables had been: forward speed, field operational capacity, hourly and area fuel consumption, wheels lip, draft force and drawbar power. The speed, the wheels lip and fuel consumption had been higher for gear M2 (7.0km.h-1) when operating in soil prepared by reduced soil tillage also presented greater values fuel consumption and lower speed of sowing.

O objetivo do trabalho foi avaliar o desempenho de um conjunto trator-semeadora-adubadora de quatro linhas, variando as marchas do trator e preparo do solo. A semeadura foi realizada em Latossolo Vermelho Eutroférrico. Os tratamentos foram: preparo do solo (convencional, reduzido e plantio direto) e marchas do trator (5,9km h-1 e 7,0km h-1), em delineamento de blocos casualizados em fatorial 3 x 2 com quatro repetições. Foram analisadas: velocidade de deslocamento, capacidade de campo operacional, consumo de combustível horário e por área, patinagem, força de tração e potência na barra. A velocidade, a patinagem e os consumos de combustível horário e por área foram maiores para a marcha M2 (7,0km h-1) e o conjunto trabalhando em área cujo preparo do solo foi realizado com escarificador apresentou maiores valores para os consumos de combustível horário e por área e também menor velocidade operacional.

Soil spatial variability and the estimation of the irrigation water depth

The effects of soil water spatial variability previous to irrigation and of the field capacity on the estimation of irrigation water depth are evaluated. The experiment consisted of a common bean (Phaseolus vulgaris L.) crop established on a Kandiudalfic Eutrudox of Piracicaba, SP, Brazil, irrigated by central pivot, in which soil water contents were evaluated with a depth neutron gauge, in a grid of 20x4 points with lag of 0.5 m. In a given situation, the 80 calculated irrigation water depths presented a coefficient of variation of 29.3%, with an average water value of 18 mm, maximum of 41mm and minimum of 9 mm. It is concluded that the only practical way of irrigation is the use of an average water depth, due to the inherent variability of the soil, and that the search for better field capacity values does not imply in better water depth estimates.

A influência da variabilidade espacial da umidade do solo em uma situação pré-irrigação e da capacidade de campo é avaliada no cálculo da lâmina de irrigação. O experimento constou de cultura de feijão (Phaseolus vulgaris L.) estabelecida em um ARGISSOLO da região de Piracicaba, SP, irrigada por pivô central, tendo as medidas de umidade sido feitas com sonda de nêutrons, em uma malha de 20x4 pontos, espaçados de 0.5 m. Em determinada situação, os 80 valores de lâmina de irrigação calculados apresentaram um coeficiente de variação de 29.3%, para uma média de 18 mm, com valor mínimo de 9 mm e máximo de 41mm. É concluído que a única forma prática de irrigação é o uso de uma lâmina média devido à variabilidade inerente ao solo, e que a procura de melhores valores para a capacidade de campo não implica em melhores estimativas da lâmina de irrigação.

Soil spatial variability and the estimation of the irrigation water depth

The effects of soil water spatial variability previous to irrigation and of the field capacity on the estimation of irrigation water depth are evaluated. The experiment consisted of a common bean (Phaseolus vulgaris L.) crop established on a Kandiudalfic Eutrudox of Piracicaba, SP, Brazil, irrigated by central pivot, in which soil water contents were evaluated with a depth neutron gauge, in a grid of 20x4 points with lag of 0.5 m. In a given situation, the 80 calculated irrigation water depths presented a coefficient of variation of 29.3%, with an average water value of 18 mm, maximum of 41mm and minimum of 9 mm. It is concluded that the only practical way of irrigation is the use of an average water depth, due to the inherent variability of the soil, and that the search for better field capacity values does not imply in better water depth estimates.

A influência da variabilidade espacial da umidade do solo em uma situação pré-irrigação e da capacidade de campo é avaliada no cálculo da lâmina de irrigação. O experimento constou de cultura de feijão (Phaseolus vulgaris L.) estabelecida em um ARGISSOLO da região de Piracicaba, SP, irrigada por pivô central, tendo as medidas de umidade sido feitas com sonda de nêutrons, em uma malha de 20x4 pontos, espaçados de 0.5 m. Em determinada situação, os 80 valores de lâmina de irrigação calculados apresentaram um coeficiente de variação de 29.3%, para uma média de 18 mm, com valor mínimo de 9 mm e máximo de 41mm. É concluído que a única forma prática de irrigação é o uso de uma lâmina média devido à variabilidade inerente ao solo, e que a procura de melhores valores para a capacidade de campo não implica em melhores estimativas da lâmina de irrigação.