Drought impact on rainfed common bean production areas in Brazil.

Common bean production in Goiás, Brazil is concentrated in the same geographic area, but spread acrossthree distinct growing seasons, namely, wet, dry and winter. In the wet and dry seasons, common beansare grown under rainfed conditions, whereas the winter sowing is fully irrigated. The conventional breed-ing program performs all varietal selection stages solely in the winter season, with rainfed environmentsbeing incorporated in the breeding scheme only through the multi environment trials (METs) wherebasically only yield is recorded. As yield is the result of many interacting processes, it is challengingto determine the events (abiotic or biotic) associated with yield reduction in the rainfed environments(wet and dry seasons). To improve our understanding of rainfed dry bean production so as to produceinformation that can assist breeders in their efforts to develop stress-tolerant, high-yielding germplasm,we characterized environments by integrating weather, soil, crop and management factors using cropsimulation models. Crop simulations based on two commonly grown cultivars (Pérola and BRS Radi-ante) and statistical analyses of simulated yield suggest that both rainfed seasons, wet and dry, can bedivided in two groups of environments: highly favorable environment and favorable environment. Forthe wet and dry seasons, the highly favorable environment represents 44% and 58% of production area,respectively. Across all rainfed environment groups, terminal and/or reproductive drought stress occursin roughly one fourth of the seasons (23.9% for Pérola and 24.7% for Radiante), with drought being mostlimiting in the favorable environment group in the dry TPE. Based on our results, we argue that eventhough drought-tailoring might not be warranted, the common bean breeding program should adapttheir selection practices to the range of stresses occurring in the rainfed TPEs to select genotypes moresuitable for these environments.

AVALANCHAS EN LA SIERRA VOLCANICA CENTRAL. EL CASO DE RIO CIRUELAS

El dia 20 de julio de 1988, en la tarde, se produjo una avalancha considerable en el rio Ciruelas, localizado en la ladera suroeste del volcán Barva, Heredia, Costa Rica, causando daños enormes en la población de San Bosco de Santa Bárbara.  El área afectada se dividió en tres grandes sectores, descritos a continuación: I.        SECTOR SUPERIOR (DESLIZAMIENTOS)Comprendido entre las cotas de 2.600m y 2.800 m, o sea cerca de la cima del Barva, caracterizado por desprendimientos de materiales poco consolidados (cenizas gruesas) con un ancho de aproximadamente 30m-40m y una profundidad de aproximadamente 4m-5m en casi todos los afluentes del rio Ciruelas. II.      SECTOR INTERMEDIO (TRANSITO)Comprendido entre las cotas de 2.600m y 1.600m, caracterizado por profundización erosiva del cauce en areas de materiales poco resistentes y por la ocurrencia de pequeños deslizamientos secundarios causados por la profundización del cauce. III.    SECTOR BAJO ( SEDIMENTACION)De 1.600m hasta 950m, caracterizado por la sedimentación en los primeros kilómetros de material grueso(bloques mayores de 2m). El pueblo de San Bosco esta situado sobre un abanico aluvial de materiales de eventos similares. En lo9s siguientes kilómetros se presenta la sedimentación de materiales mas finos.  La causa de esta desastre es únicamente la presencia de lluvias de alta intensidad provocadas por un frente de brisa, que en este dia ocurrieron en el sector I, provocando los deslizamientos y por ende las avalanchas de rocas y lodo que llegaron a los lugares mas bajos. Por estar el sector superior totalmente y el sector intermedio parcialmente en la selva virgen del Parque Nacional Braulio Carrillo se puede excluir definitivamente algún impacto humano que haya causado la desestabilización de las laderas. Por los vestigios de eventos antiguos de este tipo( acumulaciones cerca de San Bosco) se puede derivar que estos fenómenos también ocurrieron en tiempos pasados , sin embargo, se estima la probabilidad de una repetición pronta como muy baja. SUMMARYA big avalanche  that occurred the 20 th of july in the afternoon in the (rio ciruelas) watershed situated on the sowthwestern slope of the Volcano Barva, Costa Rica, caused big losses in the village of San Bosco de Santa Barbarbara. Based on field observations we distinguished three sectors analysed below: I.                    SUPERIOR SECTOR (LAND SLIDES)Localed in altitude between 2.600m and 2.800m near the peak of the volcano, characterized by landslides of poorly consolidated ashes, with a  width of between 30m-40m and a depth of about 4m to 5m, found in nearly and all of the affluents of the (Rio Ciruelas). II.                  MEDIUM SECTOR (TRANSIT)Between 2.600m and 1.600m, characterized by deep erosion in area of materials of low resistivity and by secondary(small) landslides provoked by the destruction of the support. III.                LOWER SECTOR ( SEDIMENTATION)Between 1.600m and 950m, characterized by sedimentation, in the first kilometers of coarse material (sometimes<2m).The village of San Bosco was constructed exactly above the detrictic cone of anterior events. In the subsequent kilometers we found the sedimentation of fine materials. As the cause of this desastre we analysed high intensity rainfalls provoked by a local front in the zone of the firt sector, causing landslides and then avalanches in the lower part of the primary forest of the national park <<Braulio Carrillo>>.The sediments of older events(the San Bosco cone) prove that avalanches ocurr in this area with a certain frecuency, but with relatively long recurrence intervals.