Scopus
YÖKSİS DOI Eşleşti
SJR Q1
Application of ATR-FTIR spectroscopy in tandem with chemometrics for assessing the firing conditions of Hellenistic and Roman ceramic shards excavated from the ancient city of Stratonikeia in South-Western Turkey
Microchemical Journal · Mart 2021
YÖKSİS Kayıtları
Application of ATR-FTIR spectroscopy in tandem with chemometrics for assessing the firing conditions of Hellenistic and Roman ceramic shards excavated from the ancient city of Stratonikeia in South-Western Turkey
Microchemical Journal · 2021 SCI-Expanded
Doç. Dr. İLKER IŞIK →
Application of ATR-FTIR spectroscopy in tandem with chemometrics for assessing the firing conditions of Hellenistic and Roman ceramic shards excavated from the ancient city of Stratonikeia in South-Western Turkey
Microchemical Journal · 2021 SCI-Expanded
Doç. Dr. İSMAİL TARHAN →
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Application of ATR-FTIR spectroscopy in tandem with chemometrics for assessing the firing conditions of Hellenistic and Roman ceramic shards excavated from the ancient city of Stratonikeia in South-Western Turkey
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Makale Bilgileri
Dergi
Microchemical Journal
ISSN0026265X
Yayın TarihiMart 2021
Cilt / Sayfa162
Scopus ID2-s2.0-85098127165
Özet
The use of attenuated total reflectance (ATR) Fourier transform infrared (FTIR) spectra combined with chemometrics were tested to assess the firing conditions of the shard samples excavated from the ancient city of Stratonikeia. Totally thirty-six principal component analysis (PCA) models were compared according to their ability to classify fifty-five shard samples. The PCA model using normal FTIR spectra ranged between 825 and 400 cm−1 with 25 smoothing points showed the best classification results by dividing the shard samples into five different groups (A, B, C, D, E) based on their different spectral information. To determine the firing conditions and the mineralogical compositions of the shard groups, the second-derivative ATR-FTIR spectra (two polynomial degrees and 11 smoothing points of Savitzky-Golay) between 1700 and 400 cm−1 was successfully used. It was determined that the minerals of pseudo-amorphous structure of meta-smectite, quartz, muscovite, gehlenite, and gypsum were the main phases in the shard samples fired in the oxidizing atmospheric conditions. The obtained findings indicate that the firing temperature is about 800–950 °C and 600–800 °C for the shard groups of A, B, C, and D and E, respectively.
Yazarlar (3)
1
İsmail Tarhan
ORCID: 0000-0003-3353-8635
2
İlker Işık
3
Bilal Söğüt
Anahtar Kelimeler
Ceramic
Chemometrics
Firing temperature
FTIR spectroscopy
Mineral characterization
PCA
Kurumlar
Pamukkale Üniversitesi
Denizli Turkey
Selçuk Üniversitesi
Selçuklu Turkey
Scimago Dergi (ISSN Eşleşmesi)
Microchemical Journal
Q1
SJR Skoru0,750
H-Index117
YayıncıElsevier Inc.
ÜlkeUnited States
Analytical Chemistry (Q1)
Spectroscopy (Q1)
Metrikler
16
Atıf
3
Yazar
6
Anahtar Kelime