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- 2012 (2) (entfernen)
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- Englisch (2)
Referierte Publikation
- ja (2)
Schlagworte
In this study, we address the question of the
provenance and origin of the Dead Sea Scrolls manuscripts.
A characteristic low ratio of chlorine to bromine, corresponding
to that of the Dead Sea water, may serve as an indicator for
local production. For this aim we developed a non-destructive
procedure to determine the Cl/Br ratio in the parchment of
these manuscripts. Micro-X-ray fluorescence (µ-XRF) measurements
of a large number of parchment and leather
fragments from the Dead Sea Scrolls were analyzed with a
routine we developed based on fundamental parameter
quantification. This routine takes into account the absorption
of the collagen matrix and the influence of the different sample
thicknesses. To calculate the representative Cl/Br ratio for each
fragment, we investigated the lateral homogeneity and
determined the total mass deposition using the intensity of
the inelastically scattered, characteristic tube radiation. The
distribution of the Cl/Br ratios thus obtained from the µ-XRF
measurements make it possible to distinguish fragments
whose origin lies within the Dead Sea region from those
produced in other locations.
A new approach for chemical speciation in stratified systems using 3D Micro-XAFS spectroscopy is developed by combining 3D Micro X-ray Fluorescence Spectroscopy (3D Micro-XRF) and conventional X-ray Absorption Fine Structure Spectroscopy (XAFS). A prominent field of application is stratified materials within which depth-resolved chemical speciation is required. Measurements are collected in fluorescence mode which in general lead to distorted spectra due to absorption effects. Developing a reliable reconstruction algorithm for obtaining undistorted spectra for superficial and in-depth layers is proposed and validated. The developed algorithm calculates the attenuation coefficients of the analyte for the successive layers facilitating a new spectroscopic tool for three-dimensionally resolved nondestructive chemical speciation.