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Isotopic and elemental fractionation of solar wind implanted in the Genesis concentrator target characterized and quantified by noble gases
Authors:Veronika S HEBER  Roger C WIENS  Amy J G JUREWICZ  Nadia VOGEL  Daniel B REISENFELD  Heinrich BAUR  Kevin D McKEEGAN  Rainer WIELER  Donald S BURNETT
Institution:1. Institute for Geochemistry and Petrology, ETH Zurich, 8092 Zurich, Switzerland;2. Department of Earth and Space Sciences, UCLA, 595 Charles Young Drive East, Los Angeles, California 90095–1567, USA;3. Los Alamos National Laboratory, Los Alamos, New Mexico 87544, USA;4. Center for Meteorite Studies, Arizona State University, Tempe, Arizona 85287, USA;5. Department of Physics and Astronomy, University of Montana, Missoula, Montana 87544, USA;6. California Institute of Technology, Pasadena, California 91109, USA
Abstract:Abstract– We report concentrations and isotopic compositions of He, Ne, and Ar measured with high spatial resolution along a radial traverse of a silicon carbide (SiC) quadrant of the Genesis mission concentrator target. The Ne isotopic composition maps instrumental fractionation as a function of radial position in the target: the maximum observed isotopic fractionation is approximately 33‰ per mass unit between the center and periphery. The Ne fluence is enhanced by a factor of 43 at the target center and decreases to 5.5 times at the periphery relative to the bulk solar wind fluence. Neon isotopic profiles measured along all four arms of the “gold cross” mount which held the quadrants in the concentrator target demonstrate that the concentrator target was symmetrically irradiated during operation as designed. We used implantation experiments of Ne into SiC and gold to quantify backscatter loss and isotopic fractionation and compared measurements with numerical simulations from the code “stopping and range of ions in matter.” The 20Ne fluence curve as a function of radial distance on the target may be used to construct concentration factors relative to bulk solar wind for accurate corrections for solar wind fluences of other light elements to be measured in the concentrator target. The Ne isotopic composition as a function of the radial distance in the SiC quadrant provides a correction for the instrumental mass‐dependent isotopic fractionation by the concentrator and can be used to correct measured solar wind oxygen and nitrogen isotopic compositions to obtain bulk solar wind isotopic compositions.
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