2023
DOI: 10.3390/ma16072628
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Material Evidence of Sediments Recovered from Ancient Amphorae Found at the Potaissa Roman Fortress

Abstract: Methods for material investigation are powerful tools that allow specialists to elucidate important aspects regarding ancient artifacts such as the Roman amphorae deposits discovered at Potaissa Fortress in Turda, Romania. Archeological debate states that the deposit contained olive oil and wine amphorae, but no material evidence has been presented until now. The current research is focused on the most representative large amphora fragments found in the Potaissa deposit, with a significant amount of sediment o… Show more

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Cited by 3 publications
(3 citation statements)
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“…Both original coins were subjected to the X-ray diffraction (XRD) investigation; the obtained patterns are presented in Figure 3. The XRD pattern for the original from 1620 is dominated by the Ag peaks, which are very well developed, and a single copper peak is visible (Figure 3); thus, applying the RIR method [10,24,25] results in a weight composition of 93.17% Ag and 6.83% Cu, fact in good agreement with EDS observation. The original coin issued in 1620 presents sharp details of the impression with significant wear marks on the top of the inscriptions (Figure 2a).…”
Section: Original 3-polkerssupporting
confidence: 74%
“…Both original coins were subjected to the X-ray diffraction (XRD) investigation; the obtained patterns are presented in Figure 3. The XRD pattern for the original from 1620 is dominated by the Ag peaks, which are very well developed, and a single copper peak is visible (Figure 3); thus, applying the RIR method [10,24,25] results in a weight composition of 93.17% Ag and 6.83% Cu, fact in good agreement with EDS observation. The original coin issued in 1620 presents sharp details of the impression with significant wear marks on the top of the inscriptions (Figure 2a).…”
Section: Original 3-polkerssupporting
confidence: 74%
“…Silanized quartz particles are evidenced by silicate-specific absorption bands at 1034 cm −1 , belonging to in-plane Si-O stretching; 815 cm −1 belongs to the Si-O stretching of quartz [ 45 , 46 , 47 ]. The polymer matrix is very well evidenced by specific chemical bonds such as 1162 cm −1 , related to C-O stretching; 1455 cm −1 , related to C-H bending; 1367 cm −1 , related to C=C stretching; 1720 cm −1 , related to C=O stretching within carboxylic units of Bis-GMA.…”
Section: Resultsmentioning
confidence: 99%
“…The slurry samples' minerals amount was determined using the reference intensity ratio method (RIR), which was previously described in the literature [36,37]. The obtained values were correlated with the particle sizes range measured on the MOM images and further centralized in Table 2.…”
Section: Microstructure and Composition Characterizationmentioning
confidence: 99%