PubMed · 4861473
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S De Rysky. [Schreinemacker's method for complete dentures].. https://pubmed.ncbi.nlm.nih.gov/4861473/
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Two methods for radon emanation factor determination were performed and compared regarding their measuring accuracy: (a) by hermetically closing the sample in an airtight container and measuring the induced radon activity, and (b) by mixing charcoal and sealing the sample hermetically and after placing the sample in an open vessel with no charcoal addition, measuring each time the 226Ra content using gamma-spectrometry. Measurements of radon emanation factor of cement and pozzolanic additives, i.e. fly ash and phosphogypsum were also performed.
A complete investigation of the phonon mixing in the nu3(SO4(2-)) frequency region was made, under experimental geometry where the reflecting crystal plane and the plane of incidence contain two principal dielectric axes. It was shown that although it is monoclinic, in the frequency region under inspection, gypsum could be treated as an orthorhombic crystal. More sophisticated model dielectric functions were introduced for the explanation of the Evans holes in the reflectance spectra. Using the model dielectric function, an appearance of the shoulder at the higher frequency part of the reflectance band was explained in terms of longitudinal and quasilongitudinal phonons. A possibility for Evans type interaction was encountered between the nu3(SO4(2-)) Au symmetry type mode and probably some of the combination modes.
Electron spin resonance (ESR) was used to date the formation and most recent recrystallization of three types of gypsum samples (massive, bedded and fracture filling gypsum) from the Sakarya Formation at Eskişehir in the middle of Turkey. The ESR spectra had the signals of Fe3+ and Mn2+ in addition to those of the G1 and G2 sensitive centers (g = 2.002 and 2.008) to artificial gamma-irradiation. ESR intensities of G1 and G2 were enhanced by gamma-ray irradiation to give equivalent doses DE) for each sample. The ESR ages derived from the annual doses of 238U, 232Th and 40K contents of the samples determined by thermal neutron activation analysis (TNAA) were between 43 +/- 18 ka (massive gypsum) and 1100 +/- 466 ka (bedded gypsum) as minimal and maximal values. The ages fall into the upper Miocene-Pliocene Epoch of the geological time scale, which agreed with the stratigraphy.