In this paper we briefly describe the present experimental set-up used for
ionoluminescence (IL) measurements. As one of the first applications of the
IL method we studied the IL of femoral cross-sections of ancient human bon
es in order to get more information about diagenetic alteration of bone min
eral. With increasing distance from the periosteal edge of the bone, a chan
ge of the luminescence from orange to blue was found. The TL spectra consis
t of two broad bands centred at lambda = 440 and lambda = 590 nm, respectiv
ely. The intensity of the latter one corresponds well with the Mn content o
btained by mu PIXE measurements. Therefore, the luminescence band at 590 nm
most likely results from luminescence activation by Mn2+ ions incorporated
into the bone mineral, possibly due to the ion exchange process Ca2+ <-> M
n2+ which occurred during the time that the bone was buried in the soil. (C
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