Tenencia de la tierra y tecnología en productores de soja de Santiago del Estero : comparación con productores bonaerenses

p.155-171

El precio de la tierra en pradera pampeana y su relación con los commodities agropecuarios : periodo 1988 - 2008

El presente trabajo se focaliza en el estudio del valor de la tierra en pradera pampeana y su relación con los commodities agropecuarios para el período comprendido entre los años 1988 y 2008. En la década de 1990 se ha producido un nuevo escenario en el mercado inmobiliario rural argentino, principalmente en la zona conocida como Pradera Pampeana. Los motivos principales que lo han desencadenado fueron la adaptación de la siembra directa y el uso de variedades transgénicas, acompañado por todo un paquete tecnológico hasta entonces desconocido en el país. El valor de la tierra está determinado por la productividad de los factores y el instrumento que se utilizó para cuantificar el mismo fue el método de flujo de fondos y del valor residual descontado por la tasa de corte imperante en cada período bajo análisis. En el presente trabajo se buscó verificar el comportamiento del valor de equilibrio (técnico)de la tierra en la pampa húmeda y su relación con el valor de mercado. El valor de la tierra en las distintas zonas de la pampa húmeda constituye un sistema de vasos comunicantes que se expresa a través de la correlación que existe entre los valores de las distintas zonas. Se produce una revalorización de los campos por arbitraje o arrastre al variar los precios de algunos commodities más que otros. Finalmente se demostró que el precio relativo de los granos a nivel internacional, la tecnología aplicada, las políticas públicas vigentes y la tasa de corte son determinantes del valor técnico de la tierra; el cual, sumado a las expectativas de valoración genera el valor de mercado. Las encuestas realizadas a expertos en el mercado inmobiliario rural reflejan que el valor de la tierra se debe a lo dicho, además de ser un factor escaso y un refugio contra la desvalorización del dólar y el peso.

Distribución de la tierra : interacción entre la política pública y la globalización económica

p.237-246

Determinación del precio de la tierra en el partido de Pergamino : algunos aspectos metodológicos

p.105-112

Indicadores de calidad de la tierra en distintas posiciones de la cuenca del Río Santa María

p.111-115

Tierra, población y producción agrícola en América Latina y el Caribe

p.103-106

Influencia del uso de la tierra sobre la erosión entre surcos en un argiudol típico de Argentina

p.333-340

Investigación dirigida: medición del radio de la Tierra

La génesis de este artículo fue la experiencia realizada con (y por) nuestros alumnos para que conocieran el procedimiento seguido por Eratóstenes para medir el radio de la Tierra y lo repitiesen. Es decir, un primer y claro objetivo de la experiencia era que los alumnos aprendieran un método clásico e ilustrativo de la rigurosidad e ingenio científicos; sin embargo, también nos planteamos un segundo objetivo que, a nuestro entender, es mucho más interesante y formativo: ver cómo los alumnos eran capaces de investigar por su cuenta con unas pocas indicaciones, con el fin de conocerlos mejor y tratar de fomentar las capacidades especificas de cada uno.

Modelling collisions of rail vehicles with deformable objects

This study utilized the latest computing techniques to analyze the driver's cab of a railroad vehicle colliding with deformable objects. It explored the differences between a collision with a deformable object and a collision with a rigid object. It also examined the differences between a collision with a large simple shaped object and a collision with a life-like object. Tools of analysis included vehicle dynamics analysis and finite element analysis.

Late Holocene climatic changes in Tierra del Fuego based on multiproxy analyses of peat deposits

A ca. 1400-yr record from a raised bog in Isla Grande, Tierra del Fuego, Argentina, registers climate fluctuations, including a Medieval Warm Period, although evidence for the 'Little Ice Age' is less clear. Changes in temperature and/or precipitation were inferred from plant macrofossils, pollen, fungal spores, testate amebae, and peat humification. The chronology was established using a C-14 wiggle-matching technique that provides improved age control for at least part of the record compared to other sites. These new data are presented and compared with other lines of evidence from the Southern and Northern Hemispheres. A period of low local water tables occurred in the bog between A.D. 960-1020, which may correspond to the Medieval Warm Period date range of A.D. 950-1045 generated from Northern Hemisphere tree-ring data. A period of cooler and/or wetter conditions was detected between ca. A.D. 1030 and I 100 and a later period of cooler/wetter conditions estimated at ca. cal A.D. 1800-1930, which may correspond to a cooling episode inferred from Law Dome, Antarctica. (C) 2004 University of Washington. All rights reserved.

Conventional 3D staging PET/CT in CT simulation for lung cancer: impact of rigid and deformable target volume alignments for radiotherapy treatment planning

Objective: Positron emission tomography (PET)/CT scans can improve target definition in radiotherapy for non-small cell lung cancer (NSCLC). As staging PET/CT scans are increasingly available, we evaluated different methods for co-registration of staging PET/CT data to radiotherapy simulation (RTP) scans.

Methods: 10 patients underwent staging PET/CT followed by RTP PET/CT. On both scans, gross tumour volumes (GTVs) were delineated using CT (GTVCT) and PET display settings. Four PET-based contours (manual delineation, two threshold methods and a source-to-background ratio method) were delineated. The CT component of the staging scan was co-registered using both rigid and deformable techniques to the CT component of RTP PET/CT. Subsequently rigid registration and deformation warps were used to transfer PET and CT contours from the staging scan to the RTP scan. Dice’s similarity coefficient (DSC) was used to assess the registration accuracy of staging-based GTVs following both registration methods with the GTVs delineated on the RTP PET/CT scan.

Results: When the GTVCT delineated on the staging scan after both rigid registration and deformation was compared with the GTVCT on the RTP scan, a significant improvement in overlap (registration) using deformation was observed (mean DSC 0.66 for rigid registration and 0.82 for deformable registration, p50.008). A similar comparison for PET contours revealed no significant improvement in overlap with the use of deformable registration.

Conclusions: No consistent improvements in similarity measures were observed when deformable registration was used for transferring PET-based contours from a staging PET/CT. This suggests that currently the use of rigid registration remains the most appropriate method for RTP in NSCLC.

Postglacial vegetation dynamics of western Tierra del Fuego

The southern fringes of the South American landmass provide a rare opportunity to examine the development of moorland vegetation with sparse tree cover in a wet, cool temperate climate of the Southern Hemisphere. We present a record of changes in vegetation over the past 17,000 years, from a lake in extreme southern Chile (Isla Santa Inés, Magallanes region, 53°38.97S; 72°25.24W), where human influence on vegetation is negligible. The western archipelago of Tierra del Fuego remained treeless for most of the Lateglacial period; Lycopodium magellanicum, Gunnera magellanica and heath species dominated the vegetation. Nothofagus may have survived the last glacial maximum at the eastern edge of the Magellan glaciers from where it spread southwestwards and established in the region at around 10,500 cal. yr BP. Nothofagus antarctica was likely the earlier colonizing tree in the western islands, followed shortly after by Nothofagus betuloides. At 9000 cal. yr BP moorland communities expanded at the expense of Nothofagus woodland. Simultaneously, Nothofagus species shifted to dominance of the evergreen Nothofagus betuloides and the Magellanic rain forest established in the region. Rapid and drastic vegetation changes occurred at 5200 cal. yr BP, after the Mt Burney MB2 eruption, including the expansion and establishment of Pilgerodendron uviferum and the development of mixed Nothofagus-Pilgerodendron-Drimys woodland. Scattered populations of Nothofagus, as they occur today in westernmost Tierra del Fuego may be a good analogue for Nothofagus populations during the Lateglacial in eastern sites.

A bond model for DEM simulation of cementitious materials and deformable structures

There is an increasing use of the discrete element method (DEM) to study cemented (e.g. concrete and rocks) and sintered particulate materials. The chief advantage of the DEM over continuum based techniques is that it does not make assumptions about how cracking and fragmentation initiate and propagate, since the DEM system is naturally discontinuous. The ability for the DEM to produce a realistic representation of a cemented granular material depends largely on the implementation of an inter-particle bonded contact model. This paper presents a new bonded contact model based on the Timoshenko beam theory which considers axial, shear and bending behaviour of the bond. The bond model was first verified by simulating both the bending and dynamic response of a simply supported beam. The loading response of a concrete cylinder was then investigated and compared with the Eurocode equation prediction. The results show significant potential for the new model to produce satisfactory predictions for cementitious materials. A unique feature of this model is that it can also be used to accurately represent many deformable structures such as frames and shells, so that both particles and structures or deformable boundaries can be described in the same DEM framework.