1999•AIP conference proceedingsRequires access

Positron annihilation in opals: Evidence of positronium formation

Jagoda M. Urban-Klaehn, Carroll A. Quarles

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Abstract

Natural opal samples have been studied with positron annihilation spectroscopy methods: Lifetime spectroscopy (LT) and Doppler Broadening (DB) spectroscopy. Additionally, samples have been examined by the Scanning Electron Microscope (SEM) and the BET method. The mean lifetimes and DB spectra shape of opals have been compared to other rocks by constructing the quotient spectra. Unusual properties of opals have been explained by positronium formation in the three-dimensional tektosilicate framework structure (SiO2*nH2O) of the opals.

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What this paper is about

Natural opal samples have been studied with positron annihilation spectroscopy methods: Lifetime spectroscopy (LT) and Doppler Broadening (DB) spectroscopy. Additionally, samples have been examined by the Scanning Electron Microscope (SEM) and the BET method. The mean lifetimes and DB spectra shape of opals have been compared to other rocks by constructing the quotient spectra. Unusual properties of opals have been explained by positronium formation in the three-dimensional tektosilicate framework structure (SiO2*nH2O) of the opals.

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Available abstract

Natural opal samples have been studied with positron annihilation spectroscopy methods: Lifetime spectroscopy (LT) and Doppler Broadening (DB) spectroscopy. Additionally, samples have been examined by the Scanning Electron Microscope (SEM) and the BET method. The mean lifetimes and DB spectra shape of opals have been compared to other rocks by constructing the quotient spectra. Unusual properties of opals have been explained by positronium formation in the three-dimensional tektosilicate framework structure (SiO2*nH2O) of the opals.

Key concepts: Positronium, Positron annihilation spectroscopy, Spectroscopy, Scanning electron microscope, Materials science, Annihilation, Positron, Doppler broadening

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