La caverna de José Saramago: imagen platónica versus metafísica

La caverna de José Saramago tiene como referencia indudable la imagen de la caverna del libro VII de la República de Platón, y, sin embargo, Saramago no és un escritor idealista o metafísico. Este artículo muestra cómo, aprovechando la aplicabilidad con que Platón dotó a su imagen, Saramago defiende la necesidad de saber recibir los mensajes de la tierra, de la materia, de no convertirnos en prisioneros en las cavernas doradas de la sociedad occidental, y de ser libres en la naturaleza, phýsis, y no lejos o más allá, metá, de ella.

The Cave by José Saramago: Platonic image versus metaphysics

The cave by José Saramago has as a certain reference the image of the cave of book VII of Plato's Republic and, however, Saramago is not an idealistic or metaphysical writer. This article, taking advantage of the applicability with which Plato endowed his image, defends the urge to be open to the messages sent by the earth, by matter, the urge not to become prisoners in the golden caves of the Western society and, finally, the urge to find our freedom in Nature, phýsis, and not far or beyond, metá, it.

La caverna de José Saramago: imagen platónica versus metafísica

La caverna de José Saramago tiene como referencia indudable la imagen de la caverna del libro VII de la República de Platón, y, sin embargo, Saramago no és un escritor idealista o metafísico. Este artículo muestra cómo, aprovechando la aplicabilidad con que Platón dotó a su imagen, Saramago defiende la necesidad de saber recibir los mensajes de la tierra, de la materia, de no convertirnos en prisioneros en las cavernas doradas de la sociedad occidental, y de ser libres en la naturaleza, phýsis, y no lejos o más allá, metá, de ella.

Impacts of land leveling on lowland soil physical properties

The practice of land leveling alters the soil surface to create a uniform slope to improve land conditions for the application of all agricultural practices. The aims of this study were to evaluate the impacts of land leveling through the magnitudes, variances and spatial distributions of selected soil physical properties of a lowland area in the State of Rio Grande do Sul, Brazil; the relationships between the magnitude of cuts and/or fills and soil physical properties after the leveling process; and evaluation of the effect of leveling on the spatial distribution of the top of the B horizon in relation to the soil surface. In the 0-0.20 m layer, a 100-point geo-referenced grid covering two taxonomic soil classes was used in assessment of the following soil properties: soil particle density (Pd) and bulk density (Bd); total porosity (Tp), macroporosity (Macro) and microporosity (Micro); available water capacity (AWC); sand, silt, clay, and dispersed clay in water (Disp clay) contents; electrical conductivity (EC); and weighted average diameter of aggregates (WAD). Soil depth to the top of the B horizon was also measured before leveling. The overall effect of leveling on selected soil physical properties was evaluated by paired "t" tests. The effect on the variability of each property was evaluated through the homogeneity of variance test. The thematic maps constructed by kriging or by the inverse of the square of the distances were visually analyzed to evaluate the effect of leveling on the spatial distribution of the properties and of the top of the B horizon in relation to the soil surface. Linear regression models were fitted with the aim of evaluating the relationship between soil properties and the magnitude of cuts and fills. Leveling altered the mean value of several soil properties and the agronomic effect was negative. The mean values of Bd and Disp clay increased and Tp, Macro and Micro, WAD, AWC and EC decreased. Spatial distributions of all soil physical properties changed as a result of leveling and its effect on all soil physical properties occurred in the whole area and not specifically in the cutting or filling areas. In future designs of leveling, we recommend overlaying a cut/fill map on the map of soil depth to the top of the B horizon in order to minimize areas with shallow surface soil after leveling.