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Isotope geochemistry of strontium in carbonate and evaporite rocks of marine origin /Tremba, Edward Louis, 1943- January 1973 (has links)
No description available.
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Ground state properties of strontium nuclides by laser spectroscopyRamsay, Eric Barnaby January 1988 (has links)
Isotope shifts of twenty-two isotopes of strontium, $ sp{78}$Sr to $ sp{100}$Sr excluding $ sp{99}$Sr, and three isomers of strontium, $ sp{83 rm m,85m,87m}$Sr, have been measured using laser spectroscopy. The nuclear spins, magnetic and quadrupole moments, have been extracted from the data for all odd isotopes. The changes in mean square charge radii have also been evaluated for all isotopes and isomers. / The changes in mean square charge radii, which are compared to the predictions of the droplet model and Hartree-Fock plus B.C.S. calculations, show a pronounced shell effect at the closed neutron shell at N = 50 and a sharp increase at N = 60. The theoretical analysis suggests that the change in mean square charge radii for N = 60, 62 is due to the onset of a large static deformation. For the remaining isotopes, the changes are attributed to a change in size, a change in the predominantly dynamic deformation, and a change in the diffuseness of the nuclear charge distribution.
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Ground state properties of strontium nuclides by laser spectroscopyRamsay, Eric Barnaby January 1988 (has links)
No description available.
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Solute Inputs to Soil and Stream Waters in a Seasonally Snow-Covered Mountain Catchment Determined Using Ge/Si, ⁸⁷SR/⁸⁶SR and Major Ion Chemistry: Valles Caldera, New MexicoPorter, Courtney January 2012 (has links)
Weathering releases lithogenic elements to soil and stream waters that support life in catchment ecosystems. Seasonal and inter-annual variations in hydrologic conditions change subsurface flowpaths, modifying the influence of weathering on stream waters. This study, over two climatically variable years, determined seasonal and inter-annual changes in solute sources to streams using a multi-tracer approach including major cations, strontium isotopes, germanium (Ge)/silica ratios, carbon species, and trace metals. Stream water cations display constant concentrations although discharge response was highly variable, suggesting that there is a consistent subsurface water supply. However, Sr isotope ratios, and concentrations of Ge, Fe, Al, and dissolved organic carbon, which originate from shallow soil waters, increase with the hydrograph during a wet winter snowmelt. This indicates that during a year with a thick snowpack, stream waters contain components of both shallow soilwater and groundwater during snowmelt, whereas during all other times groundwater contributes predominantly to the stream.
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Strontium isotopes as a tracer for the origin of Mississippi valley-type sulfide deposits from the southeast Missouri and tri-state district of MissouriLange, Steven L January 2011 (has links)
Typescript (photocopy). / Digitized by Kansas Correctional Industries
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Etude de la reaction 89Y (d,a) 87Sr.Brien, Marcel January 1971 (has links)
No description available.
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Decay of 86 m Y and 83 Y.Simpson, Margaret Louise January 1972 (has links)
No description available.
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Etude de la reaction 89Y (d,a) 87Sr.Brien, Marcel January 1971 (has links)
No description available.
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Strontium isotope and geochronological studies of the basic igneous province of N.E. ScotlandPankhurst, Robert J. January 1968 (has links)
No description available.
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Decay of 86 m Y and 83 Y.Simpson, Margaret Louise January 1972 (has links)
No description available.
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