Avances en el estudio del "torrao" o cribado del tomate

El "torrao" es una enfermedad presente en nuestro país desde 2001, que sigue presentándose en cada campaña de tomate con mayor o menor incidencia según el año. Las plantas afectadas muestran necrosis en la parte basal de los foliolos que puede evolucionar a cribado, manchas longitudinales en los peciolos y manchas necróticas en fruto, que terminan por rajarlo. El presente trabajo es la continuación del publicado en el número 32 de esta revista titulado "Necrosis del tomate: "torrao" o cribado" y surge de los resultados obtenidos tras la reciente publicación de la identificación y caracterización del nuevo virus "Tomato torrado virus" (ToTV) como agente implicado en la enfermedad conocida como "torrao". En este estudio se seleccionaron 94 muestras procedentes de prospecciones realizadas en invernaderos de Murcia durante los años 2003 a 2006. La aplicación RT-PCR e hibridación molecular para la detección de ToTV ha permitido detectar la presencia de esta nueva virosis en 87 de las muestras analizadas. En 83 de ellas, se encontró la presencia conjunta de este nuevo virus con el Pepino mosaic virus (PepMV), mayoritariamente con el aislado tipo Chileno 2 (Accesión number: DQ00095). Se plantean nuevos estudios para determinar la implicación de ambos virus, ToTV y PepMV, en el desarrollo del síndrome conocido como "torrao" del tomate.

Historia del Instituto de Estudios Norteamericanos de Barcelona (1951-62)

Esta ponencia deriva del estudio previo: "la Historia del Instituto Norteamericano de Barcelona, 1951-1962", y sostiene como hipótesis de partida que esta institución, cultural y académica, impulsada desde la sociedad cívica catalana, fue, en su etapa preformativa como en la inmediatamente previa a su consolidación, un fiel reflejo y termómetro del giro político de los Estados Unidos de América respecto del Estado Español en el anterior siglo XX. Su centro de interés radica a nuestro entender en el estudio de la metabolización de ese cambio en un segmento de la sociedad catalana y en la mutua instrumentalización, que no por desigual, ambas partes pusieron en práctica, eso sí, con finalidades ya distintas, coincidentes u opuestas.

Reexposure and advection of C-14-depleted organic carbon from old deposits at the upper continental slope

Outcrops of old strata at the shelf edge resulting from erosive gravity-driven flows have been globally described on continental margins. The reexposure of old strata allows for the reintroduction of aged organic carbon (OC), sequestered in marine sediments for thousands of years, into the modern carbon cycle. This pool of reworked material represents an additional source of C-14-depleted organic carbon supplied to the ocean, in parallel with the weathering of fossil organic carbon delivered by rivers from land. To understand the dynamics and implications of this reexposure at the shelf edge, a biogeochemical study was carried out in the Gulf of Lions (Mediterranean Sea) where erosive processes, driven by shelf dense water cascading, are currently shaping the seafloor at the canyon heads. Mooring lines equipped with sediment traps and current meters were deployed during the cascading season in the southwestern canyon heads, whereas sediment cores were collected along the sediment dispersal system from the prodelta regions down to the canyon heads. Evidence from grain-size, X-radiographs and Pb-210 activity indicate the presence in the upper slope of a shelly-coarse surface stratum overlying a consolidated deposit. This erosive discontinuity was interpreted as being a result of dense water cascading that is able to generate sufficient shear stress at the canyon heads to mobilize the coarse surface layer, eroding the basal strata. As a result, a pool of aged organic carbon (Delta C-14 = -944.5 +/- 24.7%; mean age 23,650 +/- 3,321 ybp) outcrops at the modern seafloor and is reexposed to the contemporary carbon cycle. This basal deposit was found to have relatively high terrigenous organic carbon (lignin = 1.48 +/- 0.14 mg/100 mg OC), suggesting that this material was deposited during the last low sea-level stand. A few sediment trap samples showed anomalously depleted radiocarbon concentrations (Delta C-14 = -704.4 +/- 62.5%) relative to inner shelf (Delta C-14 = -293.4 +/- 134.0%), mid-shelf (Delta C-14 = -366.6 +/- 51.1%), and outer shelf (Delta C-14 = -384 +/- 47.8%) surface sediments. Therefore, although the major source of particulate material during the cascading season is resuspended shelf deposits, there is evidence that this aged pool of organic carbon can be eroded and laterally advected downslope.

Amorphous silicon thin film solar cells deposited entirely by Hot-Wire Chemical Vapour Deposition at low temperature (<150 ºC)

Amorphous silicon n-i-p solar cells have been fabricated entirely by Hot-Wire Chemical Vapour Deposition (HW-CVD) at low process temperature < 150 °C. A textured-Ag/ZnO back reflector deposited on Corning 1737F by rf magnetron sputtering was used as the substrate. Doped layers with very good conductivity and a very less defective intrinsic a-Si:H layer were used for the cell fabrication. A double n-layer (μc-Si:H/a-Si:H) and μc-Si:H p-layer were used for the cell. In this paper, we report the characterization of these layers and the integration of these layers in a solar cell fabricated at low temperature. An initial efficiency of 4.62% has been achieved for the n-i-p cell deposited at temperatures below 150 °C over glass/Ag/ZnO textured back reflector.