Isotopic and elemental fractionation of solar wind implanted in the Genesis concentrator target characterized and quantified by noble gases
نویسندگان
چکیده
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 Ne 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.
منابع مشابه
Genesis , Five Years After
Introduction: Almost five years after the crash-landing of the sample return capsule of the Genesis solar wind collection mission, many of the originally defined high-priority goals [1] have been reached or prospects are very good that they will be reached within the next few years. None of the major goals had to be abandoned as a consequence of the crash. This contribution reviews some of the ...
متن کاملSolar Wind Neon in the Genesis Concentrator Gold Cross by Uv Laser Ablation: First Preliminary Data
Introduction: To determine the oxygen isotopic composition of the present day solar wind is one of the key goals of the Genesis solar wind (SW) collection mission, as the solar wind is a proxy for the solar nebula. In order to increase the number of atoms to be analysed and hence analytical precision on O isotopes, SW ions in the mass range up to 28 amu were accelerated and focussed onto a "con...
متن کاملFractionation Processes in the Solar Wind Revealed by Noble Gases Collected by Genesis Regime Targets
Introduction: Genesis collected solar wind (SW) ions with one major objective being to obtain abundances and isotopic composition of ultra-volatile elements. The SW is a proxy for the composition of the solar outer convective zone (OCZ) and, hence for the solar nebula. For most elements accurate values for the isotopic composition of sun can be inferred from meteorites. Carbonaceous chondrites ...
متن کاملPreliminary Genesis Bulk Solar Wind Ar, Kr, and Xe Abundances in Comparison to Young Lunar Regolith and Solar Photosphere Data
Introduction: A major objective of GENESIS is to constrain the present day solar wind (SW) Ar, Kr, and Xe isotopic and elemental compositions by direct measurements of SW irradiated artificial samples [1]. Due to the low abundances of heavy noble gases in the SW, until now these compositions could only be inferred from regolith samples which were irradiated by the SW over large time spans [e.g....
متن کاملThe Genesis solar wind sample return mission: Past, present, and future
The Genesis Discovery mission returned solar matter in the form of the solar wind with the goal of obtaining precise solar isotopic abundances (for the first time) and greatly improved elemental abundances. Measurements of the light noble gases in regime samples demonstrate that isotopes are fractionated in the solar wind relative to the solar photosphere. Theory is required for correction. Mea...
متن کامل