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Hydrochemical and environmental isotope based investigation of the Masama Ntane Sandstone Aquifer, BotswanaMofokeng, Thelma January 2017 (has links)
A research report submitted to the Faculty of Science school of Geosciences in partial fulfillment of the requirements for the degree of Masters of Science in Hydrogeology. Johannesburg, June 2017. / The Masama Sandstone Aquifer is located in a semi-arid region of south-eastern Botswana
where there are no perennial rivers. Groundwater is the main source of water supply for the
communities. Historically many water drilling programs have been carried out in this area and
the hydrogeological system has been conceptualized. An integrated approach coupling
environmental isotopes, radioisotopes and multivariate statistical analysis of the hydrochemical
variables was employed to study the origin, age, recharge conditions, rock-water interaction and
the hydrological link between the aquifer and geological structures. The major ions in this area
are Na+, Ca2+, Mg2+ and HCO-3. Groundwater in the Masama area fall in the transition from a
Na-HCO-3 –type through Ca-Na-HCO-3 to Ca-Mg-HCO-3 -type waters from the western to the
eastern part of the area. The water types are as a result of cation exchange, carbonate dissolution
and rock-weathering processes. The δ18O and δ2H values vary spatially depending on the source
of moisture, rainfall season, geology, topography and groundwater circulation depth. Deep
circulating groundwaters are isotopically depleted whilst shallow circulating groundwaters are
isotopically enriched with respect to winter rain. Low tritium values < 0.8TU and 14C values <
80pmc testifies for recharge. Recent rainfall amount in the area is not sufficient enough to make
a profound replenishment in the aquifer. Tritium, 14C and Chloride Mass Balance helped in
identifying recharge location and hydrologic connections between structures and the sandstone
aquifer elucidating that recharge zones are in the NE and NW of the study area. High recharge
rates occur in the north-eastern part and the Makhujwane fault act as a conduit for groundwater
recharge. This study provides a better understanding of the aquifer and the information contained
herein can be incorporated into future works for sustainable use of the groundwater resource. / XL2017
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The size dependence of radiophosphorus bioaccumulation in the freshwater plankton /Vézina, Alain January 1984 (has links)
No description available.
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Autoradiographic studies of GABA-ergic neurons in mouse cerebellum / GABA-ergic neurons in mouse cerebellum.Mpinga, Manuel Mikeseni 03 June 2011 (has links)
Ball State University LibrariesLibrary services and resources for knowledge buildingMasters ThesesThere is no abstract available for this thesis.
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An autoradiographic study of pentosan deposition in the cell walls of Populus tremuloides MichxMullis, Ralph H. 01 January 1975 (has links)
No description available.
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THE EARLY PRODUCTS OF RADIOACTIVE PHOSPHATE ESTERIFICATION BY BARLEY ROOTSElbagouri, Ismael Hamdi Mahmoud, 1938- January 1966 (has links)
No description available.
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THE SYNTHESIS OF SPECIFICALLY DEUTERATED AMINO ACIDS AND PEPTIDES FOR USE IN BIOPHYSICAL STUDIESUpson, Donald Allen, 1946- January 1975 (has links)
No description available.
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The size dependence of radiophosphorus bioaccumulation in the freshwater plankton /Vézina, Alain January 1984 (has links)
Body size influences virtually all aspects of the autecology of material flow by organisms. Thus, size classes may be considered as alternatives to grouping by trophic level, function or taxonomy to describe the structure and function of communities. The general intent of this thesis is to assess the role of body size in the dynamics of radiophosphorus in the freshwater plankton. To calculate a priori estimates of the fluxes of phosphorus through size classes of plankton, the rates of assimilation and excretion of laboratory cultures of algae and cladocerans were measured, and regressed on body mass (W). In both groups, assimilation increased as W('0.75). The turnover of body phosphorus was described as a two-compartment system. The turnover rates of the small (2-5% of body P) fast turnover pool, the large (95-98%) slow turnover pool, and that of the body phosphorus fell proportionately to W('- 1/4) in algae and W('- 1/2) in zooplankton. Field tests of allometric models of radiophosphorus flow were conducted by following the redistribution of radioactivity among 11 size fractions of enclosed epilimnetic assemblages over 5 to 6 days. Concentration of the tracer in the biomass declined with size soon after addition and gradually shifted to a uniform distribution within 3 days. A model that makes no a priori assumptions as to the trophic structure of the system, i.e. all size classes are at the same trophic level, predicted these dynamics better than one that assumes trophic position to increase with size. Further analyses indicated that explicit treatment of the physiological allometry and size distribution of broad functional groups of plankton are needed to improve the descriptive power of the model further.
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Determination of alkyllead compounds and synthesis of alkyllead radiotracersBlais, Jean-Simon January 1987 (has links)
No description available.
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A determination of air-sea gas exchange and upper ocean biological production from five noble gases and tritiugenic helium-3Stanley, Rachel H. R. January 2007 (has links)
Thesis (Ph. D.)--Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 2007. / "September 2007". "Joint Program in Oceanography/Applied Ocean Science and Engineering"--Cover. Title from Web page (viewed on Mar. 24, 2008). Includes bibliographical references (p. 215-225).
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An isotope washout technique to study skin perfusion pressure and vascular resistance in diabetes, hypertension and peripheral vascular disease /Duncan, Henry J. January 1986 (has links) (PDF)
Thesis (M.D.)--University of Adelaide, 1987. / Includes bibliographical references (leaves 140-190).
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