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Polycapillary halflenses are widely used to focus X-ray radiation onto a small spot. Additionally they can reduce the field of view of a semiconductor detector when placed in front of one. In 3D micro X-ray fluorescence spectroscopy (3D Micro-XRF) with synchrotron radiation, two polycapillary halflenses are used in a confocal geometry. Up until now, characterization measurements in the focal plane have only been performed in the case of the lens focusing parallel radiation. Assumptions have been made, that in the other case, when isotropic radiation from a spot source is transported to a detector, the acceptance distribution in the focal plane is also Gaussian. We performed measurements with an electron beam as well as a proton beam which confirm this assumption. In addition, a comparison between measurements in collecting and focusing mode show differences in spot size and transmission. These differences exemplify the fact that there is not one global spot size or transmission function of a polycapillary halflens. Illumination and divergence effects can alter both characteristic lens parameters.
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.