Efeito de diferentes materiais no pH do solo

A grande maioria dos solos agrícolas brasileiros apresenta alta acidez (pH H2O < 5,5) sendo um dos principais responsáveis pela baixa produtividade das culturas. Estes solos exigem a aplicação de corretivos para elevar o seu pH, neutralizar os efeitos dos elementos tóxicos, fornecer Ca e Mg como nutrientes e aumentar a produtividade das culturas. Com o objetivo de verificar o efeito de diferentes materiais (calcário calcinado e dolomítico, escória e gesso) no pH do solo, em função da dose aplicada (2, 4 e 6 t/ha) e do tempo de incubação (25, 50 e 75 dias), foi conduzido trabalho em condições de laboratório. Após o período de incubação e determinação do pH em água, concluiu-se que: a) todos os materiais, com exeção do gesso, foram eficientes para elevar o pH do solo. b) o efeito corretivo do material foi função do seu poder de neutralização (PN), ou seja, para uma mesma dose e tempo, quando maior o PN, maior o efeito do material no pH do solo; c) dentre os materiais estudados, o calcário calcinado foi o que provocou o maior aumento de pH, seguido do calcário dolomítico e da escória; d) a maior dose aplicada de cada corretivo correspondeu maior elevação de pH do solo.The great majority of Brazilian agricultural soils presents high acidity (pH H2O < 5,5) which is one of the main causes of low crop yields. These soils demand lime materials to increase their pH, to neutralize the toxic element effects, to supply calcium and magnesium as nutrients and to increase crop yields. This laboratory experiment was carried out to evaluate the effect of different materials (calcinated and dolomitic limestone, scoria and gypsum) on soil pH, as affected by the applied dosis (2, 4 and 6 tons per hectare) and the incubation time (25, 50 and 75 days). It was concluded that: a) all materials, except gypsum, were efficient in increasing the soil pH; b) the lime material effect was related to its neutralization power, i.e., for the same dosis and time, the highest neutralization power had the highest effect on soil pH; c) among the used materials, the calcinated limestone determined the highest increase in soil pH, followed by the dolomitic limestone and scoria; d) the highest dosis for each material corresponded to the highest pH increase

A simulation toolkit for electroluminescence assessment in rare event experiments

A good understanding of electroluminescence is a prerequisite when optimising double-phase noble gas detectors for Dark Matter searches and high-pressure xenon TPCs for neutrinoless double beta decay detection. A simulation toolkit for calculating the emission of light through electron impact on neon, argon, krypton and xenon has been developed using the Magboltz and Garfield programs. Calculated excitation and electroluminescence efficiencies, electroluminescence yield and associated statistical fluctuations are presented as a function of electric field. Good agreement with experiment and with Monte Carlo simulations has been obtained

Molecular Characterization Reveals No Functional Evidence for Naturally Occurring Cross-Kingdom RNA Interference in the Early Stages of Botrytis Cinerea–Tomato Interaction

[Abstract] Plant immune responses are triggered during the interaction with pathogens. The fungus Botrytis cinerea has previously been reported to use small RNAs (sRNAs) as effector molecules capable of interfering with the host immune response. Conversely, a host plant produces sRNAs that may interfere with the infection mechanism of an intruder. We used high-throughput sequencing to identify sRNAs produced by B. cinerea and Solanum lycopersicum (tomato) during early phases of interaction and to examine the expression of their predicted mRNA targets in the other organism. A total of 7042 B. cinerea sRNAs were predicted to target 3185 mRNAs in tomato. Of the predicted tomato target genes, 163 were indeed transcriptionally down-regulated during the early phase of infection. Several experiments were performed to study a causal relation between the production of B. cinerea sRNAs and the down-regulation of predicted target genes in tomato. We generated B. cinerea mutants in which a transposon region was deleted that is the source of c.10% of the fungal sRNAs. Furthermore, mutants were generated in which both Dicer-like genes (Bcdcl1 and Bcdcl2) were deleted and these displayed a >99% reduction of transposon-derived sRNA production. Neither of these mutants was significantly reduced in virulence on any plant species tested. Our results reveal no evidence for any detectable role of B. cinerea sRNAs in the virulence of the fungus.The research of S.Q. was supported by a scholarship from the China Scholarship Council

Avaliação da higroscopicidade de fertilizantes e corretivos

Visando determinar a quantidade de água absorvida em função da umidade do ambiente e do tempo de exposição por alguns fertilizantes simples, misturas de fertilizantes e corretivos, foram colocadas em três ambientes de umidade relativa constante de 70,4%, 80,5% e 88,8% . As amostras foram pesadas após 0, 3, 6, 24, 48 e 72 horas determinando a porcentagem de água absorvida. A absorção de água pelos produtos aumentou com o aumento da umidade relativa do ar e do tempo de exposição. Todos os materiais absorveram alguma umidade no menor tempo e na menor umidade relativa estudados, isto é, 3 horas de 70,4%, porém essa absorção foi insignificante nos casos do sulfato de amônio, fosfato diamônico, fosfato natural parcialmente acidulado, cloreto de potássio, sulfato de potássio, calcário calcinado. Os fertilizantes nitrogenados, uréia e nitrocálcio, foram os que apresentaram maior higroscopicidade dentre os materiais estudados. Foi possível verificar também que a presença de 5% de calcário calcinado ou de vermiculita nas misturas de grânulos diminuiu sensivelmente sua higroscopicidade.The percentual of water absorbed by fertilizer materials, bulk blend fertilizer mixtures and agricultural liming materials was determined as a function of the environment relative humidity and time of exposition. Samples of these were exposed to three relative humidity environments: 70,4%, 80,5% and 77,8%, during 3, 6, 12, 24, 48, 72 hours, after drying at 50&deg;C for 24 hours. The water absorbed by all products increased with air relative humidity and exposition time. All the materials absorbed some humidity for the lowest exposition time and lowest relative humidity (3 hours and 70,4%) but was insignificant in the case of ammonium sulphate, diammonium phosphate, natural phosphate parcially acidulated, potassium chloride, potassium sulphate, limestone and hidrated lime. The urea and calcium nitrate presented major higroscopicity among the materials studied. The presence of 5% hidrated lime or vermiculite in bulk blend mixtures decreases significatively the higroscopicity

Evaluation of turbulent dissipation rate retrievals from Doppler Cloud Radar

Turbulent dissipation rate retrievals from cloud radar Doppler velocity measurements are evaluated using independent, in situ observations in Arctic stratocumulus clouds. In situ validation data sets of dissipation rate are derived using sonic anemometer measurements from a tethered balloon and high frequency pressure variation observations from a research aircraft, both flown in proximity to stationary, ground-based radars. Modest biases are found among the data sets in particularly low- or high-turbulence regimes, but in general the radar-retrieved values correspond well with the in situ measurements. Root mean square differences are typically a factor of 4-6 relative to any given magnitude of dissipation rate. These differences are no larger than those found when comparing dissipation rates computed from tetheredballoon and meteorological tower-mounted sonic anemometer measurements made at spatial distances of a few hundred meters. Temporal lag analyses suggest that approximately half of the observed differences are due to spatial sampling considerations, such that the anticipated radar-based retrieval uncertainty is on the order of a factor of 2-3. Moreover, radar retrievals are clearly able to capture the vertical dissipation rate structure observed by the in situ sensors, while offering substantially more information on the time variability of turbulence profiles. Together these evaluations indicate that radar-based retrievals can, at a minimum, be used to determine the vertical structure of turbulence in Arctic stratocumulus clouds

Low-diffusion Xe-He gas mixtures for rare-event detection: electroluminescence yield

High pressure xenon Time Projection Chambers (TPC) based on secondary scintillation (electroluminescence) signal amplification are being proposed for rare event detection such as directional dark matter, double electron capture and double beta decay detection. The discrimination of the rare event through the topological signature of primary ionisation trails is a major asset for this type of TPC when compared to single liquid or double-phase TPCs, limited mainly by the high electron diffusion in pure xenon. Helium admixtures with xenon can be an attractive solution to reduce the electron diffu- sion significantly, improving the discrimination efficiency of these optical TPCs. We have measured the electroluminescence (EL) yield of Xe–He mixtures, in the range of 0 to 30% He and demonstrated the small impact on the EL yield of the addition of helium to pure xenon. For a typical reduced electric field of 2.5 kV/cm/bar in the EL region, the EL yield is lowered by ∼ 2%, 3%, 6% and 10% for 10%, 15%, 20% and 30% of helium concentration, respectively. This decrease is less than what has been obtained from the most recent simulation framework in the literature. The impact of the addition of helium on EL statistical fluctuations is negligible, within the experimental uncertainties. The present results are an important benchmark for the simulation tools to be applied to future optical TPCs based on Xe-He mixtures. [Figure not available: see fulltext.]

The Lamb shift in muonic hydrogen and the proton radius

By means of pulsed laser spectroscopy applied to muonic hydrogen (μ− p) we have measured the 2S F = 1 1/2 − 2PF = 2 3/2 transition frequency to be 49881.88(76) GHz. By comparing this measurement with its theoretical prediction based on bound-state QED we have determined a proton radius value of rp = 0.84184 (67) fm. This new value is an order of magnitude preciser than previous results but disagrees by 5 standard deviations from the CODATA and the electronproton scattering values. An overview of the present effort attempting to solve the observed discrepancy is given. Using the measured isotope shift of the 1S-2S transition in regular hydrogen and deuterium also the rms charge radius of the deuteron rd = 2.12809 (31) fm has been determined. Moreover we present here the motivations for the measurements of the μ 4He + and μ 3He + 2S-2P splittings. The alpha and triton charge radii are extracted from these measurements with relative accuracies of few 10 − 4. Measurements could help to solve the observed discrepancy, lead to the best test of hydrogen-like energy levels and provide crucial tests for few-nucleon ab-initio theories and potentials

Search for direct production of charginos and neutralinos in events with three leptons and missing transverse momentum in √s = 7 TeV pp collisions with the ATLAS detector

A search for the direct production of charginos and neutralinos in final states with three electrons or muons and missing transverse momentum is presented. The analysis is based on 4.7 fb−1 of proton–proton collision data delivered by the Large Hadron Collider and recorded with the ATLAS detector. Observations are consistent with Standard Model expectations in three signal regions that are either depleted or enriched in Z-boson decays. Upper limits at 95% confidence level are set in R-parity conserving phenomenological minimal supersymmetric models and in simplified models, significantly extending previous results

Jet size dependence of single jet suppression in lead-lead collisions at sqrt(s(NN)) = 2.76 TeV with the ATLAS detector at the LHC

Measurements of inclusive jet suppression in heavy ion collisions at the LHC provide direct sensitivity to the physics of jet quenching. In a sample of lead-lead collisions at sqrt(s) = 2.76 TeV corresponding to an integrated luminosity of approximately 7 inverse microbarns, ATLAS has measured jets with a calorimeter over the pseudorapidity interval |eta| < 2.1 and over the transverse momentum range 38 < pT < 210 GeV. Jets were reconstructed using the anti-kt algorithm with values for the distance parameter that determines the nominal jet radius of R = 0.2, 0.3, 0.4 and 0.5. The centrality dependence of the jet yield is characterized by the jet "central-to-peripheral ratio," Rcp. Jet production is found to be suppressed by approximately a factor of two in the 10% most central collisions relative to peripheral collisions. Rcp varies smoothly with centrality as characterized by the number of participating nucleons. The observed suppression is only weakly dependent on jet radius and transverse momentum. These results provide the first direct measurement of inclusive jet suppression in heavy ion collisions and complement previous measurements of dijet transverse energy imbalance at the LHC.Comment: 15 pages plus author list (30 pages total), 8 figures, 2 tables, submitted to Physics Letters B. All figures including auxiliary figures are available at http://atlas.web.cern.ch/Atlas/GROUPS/PHYSICS/PAPERS/HION-2011-02

Measurement of the polarisation of W bosons produced with large transverse momentum in pp collisions at sqrt(s) = 7 TeV with the ATLAS experiment

This paper describes an analysis of the angular distribution of W->enu and W->munu decays, using data from pp collisions at sqrt(s) = 7 TeV recorded with the ATLAS detector at the LHC in 2010, corresponding to an integrated luminosity of about 35 pb^-1. Using the decay lepton transverse momentum and the missing transverse energy, the W decay angular distribution projected onto the transverse plane is obtained and analysed in terms of helicity fractions f0, fL and fR over two ranges of W transverse momentum (ptw): 35 < ptw < 50 GeV and ptw > 50 GeV. Good agreement is found with theoretical predictions. For ptw > 50 GeV, the values of f0 and fL-fR, averaged over charge and lepton flavour, are measured to be : f0 = 0.127 +/- 0.030 +/- 0.108 and fL-fR = 0.252 +/- 0.017 +/- 0.030, where the first uncertainties are statistical, and the second include all systematic effects.Comment: 19 pages plus author list (34 pages total), 9 figures, 11 tables, revised author list, matches European Journal of Physics C versio