The 87Rb-86Sr system is a widely used long-lived isotope geochronometer. 87Rb, the naturally occurring radioactive isotope of Rb, undergoes beta-decay to stable 87Sr with a half-life of approximately 50 Ga. Decay of 87Rb to 87Sr results in variable 87Sr/86Sr in minerals with different Rb/Sr, and measurement of 87Rb/86Sr and 87Sr/86Sr allows for the determination of the age of the rock. Accurate ages depend both on the quality of the isotopic analysis and on the accuracy of the 87Rb decay constant, lambda87. Although the currently accepted value for lambda87 of 1.42 × 10-11a-1 has been in use for over 30 years, there is growing evidence that it is not accurate. Recent attempts to refine lambda87 and its precision have not reached a consensus. This thesis describes a new experiment to measure lambda87 by 87Sr accumulation over a period of about 30 years, and the preparation of a 84-86Sr double-spike in conjunction with that experiment. Radiogenic 87Sr produced in aliquots of a RbClO4 salt was measured by isotope dilution thermal ionization mass spectrometry. An average of 31 measurements yields a value of 1.398 ± 0.003 × 10-11a-1 . This requires a substantial revision from the previously accepted decay constant and makes Rb-Sr ages calculated with it 1.5% older. A Rb-Sr and U-Pb isotopic chronometry study was carried out on thirteen ordinary chondrites – the most common type of meteorite, the origin and history of which are still unclear. Some meteorites appear disturbed, possibly by recent shock during breakup of the parent body, whereas others yielded accurate and precise U-Pb and Pb-Pb ages. For example, L5 Elenovka yielded distinct ages for silicates (4555 Ma) and phosphates (4535 Ma), allowing the cooling rate of this meteorite from approximately 1055 K to 759 K to be constrained to 15 ± 3 K/Ma. Rb-Sr yielded less precise ages than U-Pb, but using the new decay constant allows accurate comparison between the two methods. This study creates a firm foundation for future studies in thermal history of chondrites and terrestrial metamorphic complexes using Rb-Sr together with other isotopic chronometers.

ABSTRACT EXCHANGES OF STRONTIUM ON CLINOPTILOLITE ZEOLITE G&Uuml / L, &Ouml / zkan MS, Department of Chemical Engineering Supervisor: Prof. Dr. Hayrettin Y&uuml / cel November 2003, 110 Pages Sr-90 and Cs-137, nuclear fission products, are the major sources of medium-level radioactive waste which must be decontaminated. Inorganic ion exchangers are the preferred materials to eliminate radioisotopes from aqueous nuclear waste because of their high selectivity, radiation and thermal stability, low cost and likely compatibility with cement containment. Clinoptilolite and other zeolites are widely used in nuclear industry for the removal of radioisotopes from aqueous nuclear waste. In this study, the performance of local clinoptilolite zeolite from G&ouml / rdes region has been investigated so as to determine the conditions under which it can be used effectively in the column for strontium and cesium removal. It was found that under different loading conditions, breakthrough capacity varied from 0 to 0.4078 meq/g for strontium removal, breakthrough capacity varied from 0.1178 to 0.7800 meq/g for cesium removal. It was also determined that the increase of the flow rate reduced the exchange capacity of the bed. Effect of cationic form of the zeolite (Na-CLI: Sodium form of clinoptilolite and Original-CLI: Original form of clinoptilolite) on the breakthrough capacity was also searched. It was observed that Na-CLI performed much better for the removal of strontium and cesium with respect to its original form. In addition, effect of presence of calcium in the feed solution on the breakthrough capacity was investigated and it was found that presence of calcium in the feed solution makes strontium removal essentially impossible, in the case of cesium, presence of calcium in the feed solution decreases breakthrough capacity significantly.

The 87Rb-86Sr system is a widely used long-lived isotope geochronometer. 87Rb, the naturally occurring radioactive isotope of Rb, undergoes beta-decay to stable 87Sr with a half-life of approximately 50 Ga. Decay of 87Rb to 87Sr results in variable 87Sr/86Sr in minerals with different Rb/Sr, and measurement of 87Rb/86Sr and 87Sr/86Sr allows for the determination of the age of the rock. Accurate ages depend both on the quality of the isotopic analysis and on the accuracy of the 87Rb decay constant, lambda87. Although the currently accepted value for lambda87 of 1.42 × 10-11a-1 has been in use for over 30 years, there is growing evidence that it is not accurate. Recent attempts to refine lambda87 and its precision have not reached a consensus. This thesis describes a new experiment to measure lambda87 by 87Sr accumulation over a period of about 30 years, and the preparation of a 84-86Sr double-spike in conjunction with that experiment. Radiogenic 87Sr produced in aliquots of a RbClO4 salt was measured by isotope dilution thermal ionization mass spectrometry. An average of 31 measurements yields a value of 1.398 ± 0.003 × 10-11a-1 . This requires a substantial revision from the previously accepted decay constant and makes Rb-Sr ages calculated with it 1.5% older. A Rb-Sr and U-Pb isotopic chronometry study was carried out on thirteen ordinary chondrites – the most common type of meteorite, the origin and history of which are still unclear. Some meteorites appear disturbed, possibly by recent shock during breakup of the parent body, whereas others yielded accurate and precise U-Pb and Pb-Pb ages. For example, L5 Elenovka yielded distinct ages for silicates (4555 Ma) and phosphates (4535 Ma), allowing the cooling rate of this meteorite from approximately 1055 K to 759 K to be constrained to 15 ± 3 K/Ma. Rb-Sr yielded less precise ages than U-Pb, but using the new decay constant allows accurate comparison between the two methods. This study creates a firm foundation for future studies in thermal history of chondrites and terrestrial metamorphic complexes using Rb-Sr together with other isotopic chronometers.

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<p>Coal fired power plants are ubiquitous in the United States and most developed countries around the world, providing affordable electricity to consumers. In the US, approximately six hundred power plants generate 136 million tons of Coal Combustion Residuals (CCRs) annually, encompassing fly ash, bottom ash, and flue gas desulfurization materials. The range and blends of CCRs varies substantially across coal-fired plants and depends on a unique set of circumstances for each plant and coal source. Current U.S. regulations mandate the installation of advanced capture technologies to reduce atmospheric pollution, but do not address the transfer and storage, or the potential impacts to water resources. Thus improved air quality is traded for significant enrichments of contaminants in the solid waste and effluent discharged from power plants. </p><p>This work examines the geochemical and isotopic characteristics of CCRs, as well as potential environmental impacts from CCRs. This investigation looks at several different aspects of CCR and environmental interactions from 1) the immediate impacts of the 2008 TVA coal ash spill in Kingston, TN, 2) the long-term (18-month) exposure of the spilled ash in the Emory and Clinch rivers, 3) impacts on waterways in North Carolina that receive CCR effluent from coal fired power plants, and 4) examination of boron and strontium isotopes of CCRs from leaching experiments and their application as tracers in the environment of the TVA spill and NC waterways. These investigations have illuminated several conclusions, including contact of surface water with CCRs leach high concentrations of leachable CCR contaminants, such as As, Se, B, Sr, Mo, and V in the surface waters; the dilution effect is critical in determining the concentration of contaminants from the CCRs in surface water (both at the spill and in waterways receiving CCR effluent); recycling of trace elements (such as As) through adsorption/desorption can impact water quality; and elevated boron and strontium concentrations, in addition to their isotopes, can trace CCR effluent in the environment. Combining the geochemical behavior and isotopic characteristics provides a novel tool for the identification CCR effluents in the environment.</p> / Dissertation

The aim in this thesis is to use carbon, nitrogen and sulfur isotope analysis on teeth and bone to track diet and mobility of the population as well as the individual level from the articulated and disarticulated individuals from the passage grave Frälsegården, situated in Gökhem parish in the region of Falbygden, western Sweden. 50 human samples were analyzed from tooth, mandibula and femur, together with 11 faunal samples from different bone elements of local wild and domestic animals. The results fall well in line with earlier stable isotope work done on passage grave individuals from Falbygden in stable isotopes: A homogenous group with a diet which was clearly terrestrial and lived on a pretty high trophic level. It also seems that the analyzed individuals deliberately focused their food intake to the cultural and natural, megalith and limestone landscape of Falbygden, and not to its surroundings, even if the passage grave is situated in the outermost areas of the region. A small study compares the sulfur results to with earlier work done on strontium isotopes. The results show that the different methods might provide a deeper understanding in the interpretation of the methods, and therefore suggesting that further work should be done to compare the methods.

Strontium pyrophosphate is a promising phosphate that is used widely in the industry as a result of its luminescent, fluorescent, dielectric, semi-conductor, catalyst, magnetic and ion exchange properties. Thermoluminescent dosimetry (TLD) is one of such areas. Recent researches in METU on thermoluminescence property of strontium pyrophosphate showed that strontium pyrophosphate could give enough intensity for radiation dosimetry when doped with oxides of some rare-earth elements. In this study strontium pyrophosphate was synthesized and the product was doped with copper-silver, copper-indium and manganese-praseodymium ions by solid-state reaction. In addition to these processes, characterization and the investigation of thermoluminescence properties of strontium pyrophosphate with and without dopants was conducted. Stoichiometric quantities of strontium carbonate and ammonium dihydrogen phosphate were weighed, mixed and ground by agate mortar. Afterwards, the mixture was heated at 900&amp / #730 / C for 14.5 hours. For doping process, synthesized strontium pyrophosphate and different amounts of copper oxide, indium oxide, silver nitrate, manganese oxide and praseodymium oxide were weighed and powdered together. Then, mixture was heated at 950&amp / #730 / C for 11 hours. For characterization of strontium pyrophosphate samples with and without dopants / X-ray Diffraction (XRD) was implemented. Fourier Transform Infrared Spectroscopy (FTIR) was used to determine whether the bond structures were affected from doping or not. Thermal properties of the samples were investigated with the help of Differential Thermal Analysis (DTA). Morphology of compounds was observed by Scanning Electron Microscope (SEM). Afterwards thermoluminescence (TLD) studies were carried out. XRD pattern of samples showed that the intensity of hkl-310 peak of strontium pyrophosphate increased with the inclusion of metal oxides, however none of the characteristic peaks of metal oxides was observed. Addition of metal oxides caused no change in FTIR meaning that the anionic part of matrix compound, which is strontium pyrophosphate, has structural stability. Thermal analysis and morphological investigation of this material were performed. TLD results were different for each sample, which has different content. The most significant peak, which is suitable for radiation dosimetry was observed at 160&amp / #730 / C in the glow curve with the sample doped with 7% manganese oxide and 1% praseodymium oxide.

We test the fidelity of shallow-water gastropod skeletons as multi-proxy archives of seasonal paleo-environmental change by performing isotopic and trace-metal analyses on specimens of Conus ermineus from the Gulf of Mexico. Four adult specimens were collected from Stetson Bank in the Flower Garden Banks National Marine Sanctuary during the summer of 2002. Shell samples were milled along axes of growth to produce time-series profiles spanning up to eight years. We corrected the profiles for growth rate effects and compared the tuned results with in situ temperature and salinity records at the reef surface and temperature profiles from nearby surface buoys. Examination of sample densities in &#948;18O cycles shows that shell growth is faster during summers and slower during winters. Tuning the profiles versus time yields &#948;18O values that co-vary closely with seasonal temperatures to a high degree of coherency (R2 = 0.84). The &#948;13C profiles show cyclic variation modified by ontogenetic decreases in &#948;13C. These ontogenetic trends are attributable to decreasing metabolic efficiency, while seasonal cycles reflect hydrographic changes in the gastropods’ habitat. Salinity and &#948;13C of dissolved inorganic carbon show a strong correlation at Stetson Bank (R2 = 0.80), and early summer shell &#948;13C minima coincide with local salinity minima during times of peak river discharge. The terminations of these &#948;13C minima occur during annual upcoast reversals of shelf currents in this area. These effects are augmented by summer stratification and productivity minima that further decrease seawater &#948;13C. Sr/Ca ratios increase through ontogeny, most likely due to decreasing metabolic efficiency. However, seasonal variations in Sr/Ca profiles show strong similarity with &#948;18O profiles, confirming the temperature dependence of Sr/Ca and minimal influence of salinity on shell &#948;18O at Stetson Bank. The results of this study show that tuned &#948;18O and Sr/Ca profiles can be used to reconstruct seasonal paleotemperatures. Carbon isotope profiles and environmental data also demonstrate the utility of Conus &#948;13C as a proxy for freshwater flux and shelf circulation.

De très nombreux oxyhalogénures de structures très diverses ont été mis en évidence pour les éléments de transitions ou certains éléments des sous-groupes III, IIIB, IVB, l'étude de leurs propriétés chimiques se révélant souvent extrêmement féconde. Nous ne citerons pour mémoire que les travaux relatifs aux oxyhalogénures d'alluminium et de fer effectués au laboratoire respectivement par...

Les besoins en matériaux fluorescents ont entrainé l'étude de "structures d'hôte" dans lesquelles des "ions actifs" sont susceptibles de s'introduire par substitution ou plus rarement par insertion. Ces ions actifs comportent des sous-couches d ou f non saturées ; ce sont également des lanthanides ou des actinides...