Protective effect of divalent cations against aluminum toxicity in soybean

A large proportion of soybean fields in Brazil are currently cultivated in the Cerrado region, where the area planted with this crop is growing considerably every year. Soybean cultivation in acid soils is also increasing worldwide. Since the levels of toxic aluminum (Al) in these acid soils is usually high it is important to understand how cations can reduce Al rhizotoxicity in soybean. In the present study we evaluated the ameliorative effect of nine divalent cations (Ca, Mg, Mn, Sr, Sn, Cu, Zn, Co and Ba) in solution culture on Al rhizotoxicity in soybean. The growth benefit of Ca and Mg to plants in an acid Inceptisol was also evaluated. In this experiment soil exchangeable Ca:Mg ratios were adjusted to reach 10 and 60 % base saturation, controlled by different amounts of CaCl2 or MgCl2 (at proportions from 100:0 up to 0:100), without altering the soil pH level. The low (10 %) and adequate (60 %) base saturation were used to examine how plant roots respond to Al at distinct (Ca + Mg)/Al ratios, as if they were growing in soils with distinct acidity levels. Negative and positive control treatments consisted of absence (under native soil or undisturbed conditions) or presence of lime (CaCO3) to reach 10 and 60 % base saturation, respectively. It was observed that in the absence of Aluminum, Cu, Zn, Co and Sn were toxic even at a low concentration (25 µmol L-1), while the effect of Mn, Ba, Sr and Mg was positive or absent on soybean root elongation when used in concentrations up to 100 µmol L-1. At a level of 10 µmol L-1 Al, root growth was only reverted to the level of control plants by the Mg treatment. Higher Tin doses led to a small alleviation of Al rhizotoxicity, while the other cations reduced root growth or had no effect. This is an indication that the Mg effect is ion-specific and not associated to an electrostatic protection mechanism only, since all ions were divalent and used at low concentrations. An increased exchangeable Ca:Mg ratio (at constant soil pH) in the acid soil almost doubled the soybean shoot and root dry matter even though treatments did not modify soil pH and exchangeable Al3+. This indicates a more efficient alleviation of Al toxicity by Mg2+ than by Ca2+. The reason for the positive response to Mg2+ was not the supply of a deficient nutrient because CaCO3 increased soybean growth by increasing soil pH without inducing Mg2+ deficiency. Both in hydroponics and acid soil, the reduction in Al toxicity was accompanied by a lower Al accumulation in plant tissue, suggesting a competitive cation absorption and/or exclusion of Al from plant tissue stimulated by an Mg-induced physiological mechanism.

Influence of the (111) twinning on the formation of diamond cubic/diamond hexagonal heterostructures in Cu-catalyzed Si nanowires

The occurrence of heterostructures of cubic silicon/hexagonal silicon as disks defined along the nanowire (111) growth direction is reviewed in detail for Si nanowires obtained using Cu as catalyst. Detailed measurements on the structural properties of both semiconductor phases and their interface are presented. We observe that during growth, lamellar twinning on the cubic phase along the (111) direction is generated. Consecutive presence of twins along the (111) growth direction was found to be correlated with the origin of the local formation of the hexagonal Si segments along the nanowires, which define quantum wells of hexagonal Si diamond. Finally, we evaluate and comment on the consequences of the twins and wurtzite in the final electronic properties of the wires with the help of the predicted energy band diagram.

Silicon nanocluster sensitization of erbium ions under low-energy optical excitation

The sensitizing action of amorphous silicon nanoclusters on erbium ions in thin silica films has been studied under low-energy (long wavelength) optical excitation. Profound differences in fast visible and infrared emission dynamics have been found with respect to the high-energy (shortwavelength) case. These findings point out to a strong dependence of the energy transfer process on the optical excitation energy. Total inhibition of energy transfer to erbium states higher than thefirst excited state (4I13/2) has been demonstrated for excitation energy below 1.82 eV (excitation wavelength longer than 680 nm). Direct excitation of erbium ions to the first excited state (4I13/2)has been confirmed to be the dominant energy transfer mechanism over the whole spectral range of optical excitation used (540 nm¿680 nm).

Estudio de la reaccion de sulfurizacion de precursores Cu/In para la formacion de capas delgadas policristalinas de CuInS2 para celulas solares

En este trabajo se presenta un estudio detallado de los procesos implicados en la sulfurización de capas metálicas de Cu-In para la fabricación de células solares de CuInS2. Con este objeto, se ha desarrollado un experimento de sulfurización parcial de las capas, que han sido sometidas posteriormente a un tratamiento de selenización. El estudio de estas estructuras mediante Espectroscopía Raman y Espectroscopía de Electrones Auger (AES) ha permitido conocer algunos de los detalles de la reacción química, en concreto la identificación del frente de crecimiento de la reacción de sulfurización. Paralelamente, se ha desarrollado un sistema experimental que ha hecho posible investigar in-situ la reacción de sulfurización por Espectroscopía Raman, lo cual ha permitido un seguimiento preciso de la evolución estructural del material durante el proceso. Los resultados experimentales demuestran que la reacción de sulfurización se inicia en la superficie de la capa, dando lugar a la formación de CuInS2, coexistiendo dos estructuras cristalinas polimórficas (calcopirita y orden catiónico CuAu). Posteriormente la reacción química continúa asistida por la difusión de los metales hacia la superficie, que reaccionan con la atmósfera de azufre, de forma simultánea se produce una transformación de la fase CuAu del compuesto en la estructura calcopirita.

Calcineurin A of Candida albicans: involvement in antifungal tolerance, cell morphogenesis and virulence.

The azole antifungal fluconazole possesses only fungistatic activity in Candida albicans and, therefore, this human pathogen is tolerant to this agent. However, tolerance to fluconazole can be inhibited when C. albicans is exposed to fluconazole combined with the immunosuppressive drug cyclosporin A, which is known to inhibit calcineurin activity in yeast. A mutant lacking both alleles of a gene encoding the calcineurin A subunit (CNA) lost viability in the presence of fluconazole, thus making calcineurin essential for fluconazole tolerance. Consistent with this observation, tolerance to fluconazole was modulated by calcium ions or by the expression of a calcineurin A derivative autoactivated by the removal of its C-terminal inhibitory domain. Interestingly, CNA was also essential for tolerance to other antifungal agents (voriconazole, itraconazole, terbinafine, amorolfine) and to several other metabolic inhibitors (caffeine, brefeldin A, mycophenolic acid, fluphenazine) or cell wall-perturbing agents (SDS, calcofluor white, Congo red), thus indicating that the calcineurin pathway plays an important role in the survival of C. albicans in the presence of external growth inhibitors. Several genes, including PMC1, a vacuolar calcium P-type ATPase, were regulated in a calcineurin- and fluconazole-dependent manner. However, PMC1 did not play a direct role in the survival of C. albicans when exposed to fluconazole. In addition to these different properties, calcineurin was found to affect colony morphology in several media known to modulate the C. albicans dimorphic switch. In particular, calcineurin was found to be essential for C. albicans viability in serum-containing media. Finally, calcineurin was found to be necessary for the virulence of C. albicans in a mice model of infection, thus making calcineurin an important element for adequate adaptation to the conditions of the host environment.

Model for the emission of Si+ ions during oxygen bombardment of Si(100) surfaces

The variation in the emission of Si+ ions from ion-beam-induced oxidized silicon surfaces has been studied. The stoichiometry and the electronic structure of the altered layer has been characterized using x-ray photoelectron spectroscopy (XPS). The XPS analysis of the Si 2p core level indicates the strong presence of suboxide chemical states when bombarding at angles of incidence larger than 30 °. Since the surface stoichiometry or degree of oxidation varies with the angle of incidence, the corresponding valence-band structures also differ among each other. A comparison between experimental measurements and theoretically calculated Si and SiO2 valence bands indicates that the valence bands for the altered layers are formed by a combination of those two. Since Si-Si bonds are present in the suboxide molecules, the top of the respective new valence bands are formed by the corresponding 3p-3p Si-like subbands, which extend up to the Si Fermi level. The changes in stoichiometry and electronic structure have been correlated with the emission of Si+ ions from these surfaces. From the results a general model for the Si+ ion emission is proposed combining the resonant tunneling and local-bond-breaking models.

Spatial variability of soil chemical properties after coffee tree removal

Assessing the spatial variability of soil chemical properties has become an important aspect of soil management strategies with a view to higher crop yields with minimal environmental degradation. This study was carried out at the Centro Experimental of the Instituto Agronomico, in Campinas, São Paulo, Brazil. The aim was to characterize the spatial variability of chemical properties of a Rhodic Hapludox on a recently bulldozer-cleaned area after over 30 years of coffee cultivation. Soil samples were collected in a 20 x 20 m grid with 36 sampling points across a 1 ha area in the layers 0.0-0.2 and 0.2-0.4 m to measure the following chemical properties: pH, organic matter, K+, P, Ca2+, Mg2+, potential acidity, NH4-N, and NO3-N. Descriptive statistics were applied to assess the central tendency and dispersion moments. Geostatistical methods were applied to evaluate and to model the spatial variability of variables by calculating semivariograms and kriging interpolation. Spatial dependence patterns defined by spherical model adjusted semivariograms were made for all cited soil properties. Moderate to strong degrees of spatial dependence were found between 31 and 60 m. It was still possible to map soil spatial variability properties in the layers 0-20 cm and 20-40 cm after plant removal with bulldozers.

Influence of litter layer removal on the soil thermal regime of a pine forest in a mediterranean climate

The removal of the litter layer in Portuguese pine forests would reduce fire hazard, but on the other hand this practice would influence the thermal regime of the soil, hence affecting soil biological activity, litter decomposition and nutrient dynamics. Temperature profiles of a sandy soil (Haplic Podzol) under a pine forest were measured with thermocouples at depths to 16 cm, with and without litter layer. The litter layer acted as a thermal insulator, reducing the amplitude of the periodic temperature variation in the mineral soil underneath and increasing damping depths, particularly at low soil water contents. At the mineral soil surface the reduction of amplitudes was about 2.5 ºC in the annual cycle and 5 to 6.7 ºC in the daily cycle, depending on the soil water content. When soil was both cold and wet, mean daily soil temperatures were higher (about 1 - 1.5 ºC) under the litter layer. Improved soil thermal conditions under the litter layer recommend its retention as a forest management practice to follow in general.

Entropy change of martensitic transformations in Cu-based shape-memory alloys

We have investigated the different contributions to the entropy change at the martensitic transition of different families of Cu-based shape-memory alloys. The total entropy change has been obtained through calorimetric measurements. By measuring the evolution of the magnetic susceptibility with temperature, the entropy change associated with conduction electrons has been evaluated. The contribution of the anharmonic vibrations of the lattice has also been estimated using various parameters associated with the anharmonic behavior of these alloys, collected from the literature. The results found in the present work have been compared to values published for the martensitic transition of group-IV metals. For Cu-based alloys, both electron and anharmonic contributions have been shown to be much smaller than the overall entropy change. This finding demonstrates that the harmonic vibrations of the lattice are the most relevant contribution to the stability of the bcc phase in Cu-based alloys.

Mobilidade de P, Cu e Zn em colunas de solo sob sistema de semeadura direta submetido às adubações mineral e orgânica

A retenção, no perfil do solo, de elementos minerais aplicados em sua superfície é fundamental para a manutenção da qualidade da água. Nesse sentido, o objetivo deste trabalho foi avaliar o efeito da aplicação de dejeto líquido de suíno e adubo mineral na lixiviação do P, Cu e Zn em colunas indeformadas de solo (25 cm de altura e 20,3 cm de diâmetro) retiradas de uma área de Latossolo Vermelho eutroférrico típico sob semeadura direta. A água foi aplicada nas colunas de forma ininterrupta, na quantidade correspondente a três volumes da porosidade total do solo (10.020 cm³), sendo a coleta e análise dos elementos subdivididas em cinco frações. Cada volume de poros (3.340 cm³) corresponde a um turno de água percolada, e o primeiro volume foi fracionado em três coletas. A concentração dos elementos no solo foi determinada nas camadas de 0 a 2,5, 2,5 a 10 e 10 a 20 cm. A retenção de P, Cu, e Zn no solo, em relação ao aplicado via dejeto líquido de suíno, foi de 99,6, 98,8 e 100 %, respectivamente. Para o P aplicado via adubo mineral, a retenção foi de 89,7 %. Independentemente do tipo de adubo, as concentrações de P, Cu e Zn no solo foram maiores na camada de 0 a 2,5 cm. Esses resultados indicam o baixo potencial de lixiviação desses elementos, o que sugere ser importante o uso de práticas de manejo e conservação do solo e da água que proporcionem a contenção e a infiltração do escoamento superficial.