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Time-of-flight-based mass analysis of charged water fragments have been used to measure the dissociative and the nondissociative reaction pathways of water formed during collisions with 150.3em0exto0.3em0ex1000.3em0exkeV and 5000.3em0exto0.3em0ex35000.3em0exkeV H⁺ projectiles and with 80.3em0exto0.3em0ex1000.3em0exkeV H⁰ projectiles. The fragmentation pathways resulting from the ionization and the electron capture collisions with the incident H⁺ and H⁰ projectiles, as well as collisions involving projectile electron loss by the incident H⁰ projectiles, were separately recorded by detecting the target product ions in coincidence with either the ejected target electrons or the charge-analyzed projectiles. The fragmentation profile shows that at high collision energies the ionization of water arises mainly through outer shell processes. At lower energies valence electron capture and ionization dominate and transfer ionization leads to substantially different fragmentation patterns. H⁰ and H⁺ projectiles are found to be equally efficient at ionizing the water molecule. These results are of particular interest to workers in astrophysics and those involved in cancer therapy with heavy particle ion beams.
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Luna et al. (2007) studied this question.
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