Conclusions
Solution of the salt Zr(SO4)2 leads to a long-wave shift of the extrema of the Kronig structure in the x-ray K absorption spectrum of zirconium. Primary and secondary hydration both make a contribution to the shift. The magnitude of the shifts increases with increasing distance into the short-wave region from the K edge and is due to an increase in the distance of the zirconium atom from its immediate environment.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Fizika, No. 10, pp. 120–122, October, 1972.
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Petrov, É.V. X-ray K absorption spectrum of zirconium in crystalline hydrate Zr(SO4)2·nH2O. Soviet Physics Journal 15, 1488–1490 (1972). https://doi.org/10.1007/BF00892102
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DOI: https://doi.org/10.1007/BF00892102