Incidencia del manejo agronómico convencional y orgánico sobre la biodiversidad en sistemas productivos de aguacate (Persea americana Mill.) en el estado de Michoacán, México

La pérdida de la biodiversidad que genera la disminución de interacciones bióticas y procesos ecosistémicos es uno de los principales problemas ecológicos en la actualidad. Esta situación se ha relacionado a la simplificación de los sistemas naturales y a la intensificación de los sistemas productivos agrícolas, prácticas que incluso pueden ir en detrimento del rendimiento de los campos de cultivo. Sin embargo, las huertas podrían ser reservorios de biodiversidad y recursos alimenticios que provean hábitats de alta calidad para muchos organismos. En este trabajo, se relaciona el tipo de manejo agronómico (convencional y orgánico) en huertas aguacateras con la riqueza y la composición de las comunidades de visitantes florales, acarreadores de polen y plantas herbáceas con el fin de estudiar la diversidad asociada a dichos sistemas y la incidencia del manejo agronómico sobre estas comunidades. El trabajo se compone de 3 capítulos. El primer capítulo plantea la relación entre el manejo agronómico y la diversidad de visitantes florales y plantas herbáceas a partir de la generación de Unidades Básicas de Clasificación (UBC). En el segundo capítulo, se aborda la ecología reproductiva del aguacatero, en donde se estimó la oferta floral, la diversidad de la comunidad de visitantes florales y acarreadores de polen, su eficiencia de estos en el acarreo de polen y su contribución a la producción de frutos bajo el manejo agronómico orgánico y convencional. En el tercer capítulo, se construyeron y analizaron seis redes de interacción de polen acarreado-acarreador en dos momentos del cultivo: i) durante la floración del aguacatero y ii) en ausencia de floración del aguacatero. El estudio se llevó a cabo durante dos años consecutivos en el pico de floración 2010/2011 y 2011/2012 en 6 huertas orgánicas y 4 convencionales (...) Los resultados de este trabajo mostraron como el manejo agronómico puede influir en la estructura de la comunidad de visitantes, acarreadores de polen y herbáceas. Considerando que el cultivo del aguacatero presenta la floración en una época específica del año, es importante que existan de forma continua otros recursos florales para los acarreadores como son las herbáceas. Los recursos provenientes de estas plantas pueden mantener durante el año la funcionalidad de la comunidad de visitantes y acarredores, proporcionando el servicio ecosistémico de la polinización de plantas silvestres y de las cultivadas. A su vez, la tesis contribuye al fortalecimiento del conocimiento de patrones que proponen que la disponibilidad de recursos florales en las huertas derivados de manejos agronómicos más integrales y menos intensivos que favorecen el incremento de la riqueza de visitantes de flores y acarreadores de polen nativos

Distribution of Uranium Contamination in Weathered Fractured Saprolite/Shale and Ground Water

The objective of this study was to determine how structure, stratigraphy, and weathering influence fate and transport of contaminants (particularly U) in the ground water and geologic material at the Department of Energy (DOE) Environmental Remediation Sciences Department (ERSD) Field Research Center (FRC). Several cores were collected near four former unlined adjoining waste disposal ponds. The cores were collected, described, analyzed for U, and compared with ground water geochemistry from surrounding multilevel wells. At some locations, acidic U-contaminated ground water was found to preferentially flow in small remnant fractures weathering the surrounding shale (nitric acid extractable U [UNA] usually <50 mg kg–1) into thin (

Uranium removal from contaminated groundwater by synthetic resins

Synthetic resins are shown to be effective in removing uranium from contaminated groundwater. Batch and field column tests showed that strong-base anion-exchange resins were more effective in removing uranium from both near-neutral-pH (6.5)- and high-pH (8)-low-nitrate-containing groundwaters, than metal-chelating resins, which removed more uranium from acidic-pH (5)-high-nitrate-containing groundwater from the Oak Ridge Reservation (ORR) Y-12 S-3 Ponds area in Tennessee, USA. Dowex 1-X8 and Purolite A-520E anion-exchange resins removed more uranium from high-pH (8)-low-nitrate-containing synthetic groundwater in batch tests than metal-chelating resins. The Dowex™ 21K anion-exchange resin achieved a cumulative loading capacity of 49.8 mg g^-1 before breakthrough in a field column test using near-neutral-pH (6.5)-low-nitrate-containing groundwater. However, in an acidic-pH (5)-high-nitrate-containing groundwater, metal-chelating resins Diphonix and Chelex-100 removed more uranium than anion-exchange resins. In 15 mL of acidic-pH (5)-high-nitrate-containing groundwater spiked with 20 mg L^-1 uranium, the uranium concentrations ranged from 0.95 mg L^-1 at 1-h equilibrium to 0.08 mg L^-1 at 24-h equilibrium for Diphonix and 0.17 mg L^-1 at 1-h equilibrium to 0.03 mg L^-1 at 24-h equilibrium for Chelex-100. Chelex-100 removed more uranium in the first 10 min in the 100 mL of acidic-(pH 5)-high-nitrate-containing groundwater (~5 mg L^-1 uranium); however, after 10 min, Diphonix equaled or out-performed Chelex-100. This study presents an improved understanding of the selectivity and sorption kenetics of a range of ion-exchange resins that remove uranium from both low- and high-nitrate-containing groundwaters with varying pHs..

Speciation of Uranium in Sediments before and after In situ Biostimulation

The success of sequestration-based remediation strategies will depend on detailed information, including the predominant U species present as sources before biostimulation and the products produced during and after in situ biostimulation. We used X-ray absorption spectroscopy to determine the valence state and chemical speciation of U in sediment samples collected at a variety of depths through the contaminant plume at the Field Research Center at Oak Ridge, TN, before and after approximately 400 days of in situ biostimulation, as well as in duplicate bioreduced sediments after 363 days of resting conditions. The results indicate that U(VI) in subsurface sediments was partially reduced to 10–40% U(IV) during biostimulation. After biostimulation, U was no longer bound to carbon ligands and was adsorbed to Fe/Mn minerals. Reduction of U(VI) to U(IV) continued in sediment samples stored under anaerobic condition at <4 °C for 12 months, with the fraction of U(IV) in sediments more than doubling and U concentrations in the aqueous phase decreasing from 0.5-0.74 to <0.1 µM. A shift of uranyl species from uranyl bound to phosphorus ligands to uranyl bound to carbon ligands and the formation of nanoparticulate uraninite occurred in the sediment samples during storage.

Deposition of Uranium Precipitates in Dolomitic Gravel Fill

Uranium-containing precipitates have been observed in a dolomitic gravel fill near the Department of Energy (DOE) S-3 Ponds former waste disposal site as a result of exposure to acidic (pH 3.4) groundwater contaminated with U (33 mg L-1), Al3+ (900 mg L-1), and NO3- (14?000 mg L-1). The U containing precipitates fluoresce a bright green under ultraviolet (UV) short-wave light which identify U-rich coatings on the gravel. Scanning electron microscopy (SEM) microprobe analysis show U concentration ranges from 1.6-19.8% (average of 7%) within the coatings with higher concentrations at the interface of the dolomite fragments. X-ray absorption near edge structure spectroscopy (XANES) indicate that the U is hexavalent and extended X-ray absorption fine structure spectroscopy (EXAFS) shows that the uranyl is coordinated by carbonate. The exact nature of the uranyl carbonates are difficult to determine, but some are best described by a split K+-like shell similar to grimselite [K4Na(UO2)(CO3)3·H2O] and other regions are better described by a single Ca2+-like shell similar to liebigite [Ca2(UO2)(CO3)3·11(H2O)] or andersonite [Na2CaUO2(CO3)3 · 6H2O]. The U precipitates are found in the form of white to light yellow cracked-formations as coatings on the dolomite gravel and as detached individual precipitates, and are associated with amorphous basalumnite [Al4(SO4)(OH)10·4H2O].