991 resultados para óxidos de Fe e Al


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Si bien existen estudios sobre el desarrollo de los prestadores de servicios agropecuarios de labores culturales -"contratistas" en la jerga nativa-, a lo largo del siglo XX, el crecimiento exponencial de esta actividad y las vertiginosas dinámicas de innovación tecnológica para el agro en relación a este rubro, han abierto nuevos interrogantes respecto de las características productivas y las identidades construidas por estos sujetos. El objetivo de este trabajo es dar cuenta de las distintas estrategias desplegadas respecto a la compra-venta de servicios por parte de estos actores de la producción agrícola, así como también comprender cómo estas estrategias se relacionan con el modelo productivo predominante. El acercamiento que proponemos a continuación, es en base a un relevamiento cuantitativo de hogares de productores agropecuarios (provincias de Buenos Aires y de Santa Fe) y a entrevistas cualitativas sobre trayectorias de vida y empresariales. A partir de la construcción de estos datos analizamos las características de aquellos que implementaron la prestación de servicios agrícolas, en base a las dimensiones materiales e identitarias estudiadas

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The Paleo- to Meso-Proterozoic Jabiluka unconformity related uranium mine is located within the Alligator River Uranium Field, found in the Northern Territories, Australia. The uranium ore is hosted in the late middle Paleoproterozoic Cahill Formation, which is unconformably overlain by a group of unmetamorphosed conglomerates known as the Kombolgie subgroup. The Kombolgie subgroup provided the source for oxidized basinal brines, carrying U as the mobile form U(VI), which interacted with reducing lithologies in the Cahill formation, thus reducing U(VI) to the solid U(IV), and leading to the precipitation of uraninite (UO2). In order to characterize fluid interaction with the ore body and compare that to areas without mineralization, several isotopic tracers were studied on a series of clay samples from drill core at Jabiluka as well as in barren areas throughout the ARUF. Among the potential tracers, three were selected: U (redox sensitive and recent fluid mobilization), Fe (redox sensitive), and Li (fractionated by hydrothermal fluids and adsorption reactions). δ238U values were found to be closely linked to the mineralogy, with samples with higher K/Al ratios (indicating high illite and low chlorite concentrations) having higher δ238U values. This demonstrates that 235U preferentially absorbs onto the surface of chlorite during hydrothermal circulation. In addition, δ234U values lie far from secular equilibrium (δ234U of 30‰), indicating there was addition or removal of 234U from the surface of the samples from recent (<2.5Ma) interactions of mobile fluids. δ57Fe values were found to be related to lithology and spatially to known uranium deposits. Decreasing δ57Fe values were found with increasing depth to the unconformity in a drill hole directly above the ore zone, but not in drill holes in the barren area. Similarly to δ238U, δ7Li is found to correlate with mineralogy, with higher δ7Li values associated with samples with more chlorite. In addition, higher δ7Li values are found at greater depth throughout the basin, indicating that the direction of the mineralizing fluid circulation was upwards from the Cahill formation to the Kombolgie subgroup.

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Si bien existen estudios sobre el desarrollo de los prestadores de servicios agropecuarios de labores culturales -"contratistas" en la jerga nativa-, a lo largo del siglo XX, el crecimiento exponencial de esta actividad y las vertiginosas dinámicas de innovación tecnológica para el agro en relación a este rubro, han abierto nuevos interrogantes respecto de las características productivas y las identidades construidas por estos sujetos. El objetivo de este trabajo es dar cuenta de las distintas estrategias desplegadas respecto a la compra-venta de servicios por parte de estos actores de la producción agrícola, así como también comprender cómo estas estrategias se relacionan con el modelo productivo predominante. El acercamiento que proponemos a continuación, es en base a un relevamiento cuantitativo de hogares de productores agropecuarios (provincias de Buenos Aires y de Santa Fe) y a entrevistas cualitativas sobre trayectorias de vida y empresariales. A partir de la construcción de estos datos analizamos las características de aquellos que implementaron la prestación de servicios agrícolas, en base a las dimensiones materiales e identitarias estudiadas

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Electron microprobe and thermomagnetic analyses of selected basalt samples from Hole 597C were performed. The main purpose of this work was to investigate and estimate the degree of oxidation of the samples using the ratios of Fe to Ti and the Curie temperatures obtained from thermomagnetic curves. The results show that the magnetic properties of samples from Hole 597C change at a sub-bottom depth of 100 m, and that low-temperature and high-temperature oxidation processes prevailed above and below 100 m, respectively.

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Hydrogenetic ferromanganese crusts were dredged from four seamounts in the western Pacific, OSM7, OSM2, Lomilik, and Lemkein, aligned in a NW-SE direction parallel to Pacific Plate movement. The crusts consist of four well-defined layers with distinct textural and geochemical properties. The topmost layer 1 is relatively enriched in Mn, Co, Ni, and Mo compared to the underlying layer 2, which is relatively enriched in Al, Ti, K, and Rb and Cu, Zn, and excess Ba. Textural and geochemical properties of layer 2 suggest growth conditions under high biogenic and detrital flux. Such conditions are met in the equatorial Pacific (i.e., between the Intertropical Convergence Zone (ITCZ) and equatorial high-productivity zone). Layer 2 likely formed when each seamount was beneath the equatorial Pacific along its back track path. On the other hand, layer 1 probably started to grow after seamounts moved northwest from the ITCZ. This interpretation is consistent with the thickness of layer 1 across the four crusts, which increases to the northwest. Ages of the layer 1-layer 2 boundary in each crust, a potential proxy for northern margin of the ITCZ, also increase to the northwest at 17, 11, 8, and 5 Ma for OSM7, OSM2, Lomilik, and Lemkein, respectively. Assuming Pacific Plate motion of 0.3°/Myr, the seamounts were located at 12°N, 11°N, 9°N, and 8°N at the time of boundary formation. This result suggests that the north edge of the ITCZ has shifted south since the middle Miocene in the western Pacific, which agrees with information from the eastern Pacific.

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