Araştırma Makalesi
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INVESTIGATION OF NATURAL ANALCIME-RICH ZEOLITE TUFF FROM TURKEY: A COMBINED XRD, XRF, FT-IR AND SEM STUDY

Yıl 2021, , 36 - 41, 24.12.2021
https://doi.org/10.20290/estubtdb.1010189

Öz

In this study, chemical and structural properties of natural analcime-rich zeolite tuff from Turkey and that of ion-exchanged forms investigated. The microporous structure and the presence of extra-framework cations are of great importance for characterizing the unique properties of zeolites. Ion-exchanged forms (K+, H+ and Ca2+) of analcime zeolite were prepared with 1 M KNO3,1 M Ca(NO3)2 and 1 M HCl solutions in a shaker for 6 hours at 80 °C. The obtained samples were characterized by X-ray diffraction (XRD), X-ray fluorescence (XRF), Fourier transform infrared spectroscopy (FT-IR) and scanning electron microscopy (SEM) techniques. Quantitative XRD analysis showed that the major component of the natural zeolite was analcime, together with varying amounts of quartz, feldspar and clay mineral.

Destekleyen Kurum

Eskişehir Teknik Üniversitesi Bilimsel Araştırma Projesi

Proje Numarası

20ADP231

Teşekkür

Financial support by Eskişehir Teknik University via Scientific Research Projects (No. 20ADP231 ) is acknowledged.

Kaynakça

  • [1] Dyer A. An Introduction to Zeolite Molecular Sieves, John Willey and Sons Press, 1988.
  • [2] Gottardi G, Galli E. Natural Zeolites, Berlin: Springer-Verlag, 1985.
  • [3] Deer WA, Howie RA, Zussman J. An Introduction to the Rockforming Minerals, London: Longman, 1992.
  • [4] Tsitsishvili V, Dolaberidze N, Urotadze S, Alelishvili M, Mirdzveli N, Nijaradze M. Ion exchange properties of Georgian natural zeolites. Chem. J. Moldova 2017; 12(1): 95-101.
  • [5] Ataman G, Gündoğdu N. Analcimic zones in the Tertiary of Anatolia and their geological positions. Sediment Geol 1982; 31: 89-99.
  • [6] Esenli F, Özpeker I. Gördes çevresindeki neojen havzasının zeolitik diyajenezi ve höylandit klinoptilolitlerin mineralojisi, Türkiye Jeoloji Kurultayı Bülteni, 1993. pp. 8-18.
  • [7] Gündoğdu MN, Yalçın H, Temel A, Clauer N. Geological, mineralogical and geochemical characteristics of zeolite deposits associated with borates in the Bigadiç, Emet ve Kırka Neeogene Lacustrine basins, Western Turkey. Miner Deposit 1996; 31: 492-513.
  • [8] Esenli F, Uz B, Suner F, Esenli V, Ece ÖI, Kumbasar I. Zeolitization of tuffaceous rocks in the Keşan region, Thrace, Turkey. Geologia 2005;58: 51-161.
  • [9] Harada K, Tanaka K, Nagashima K. New data on the analcime-wairakite series. Am Mineral 1972; 57: 924-931.
  • [10] Hernandez MA, Petranovskii V, Avalos M, Portillo R, Rojas F, Lara VH. Influence of the Si/Al framework ratio on the microporosity of dealuminated mordenite as determined from N2 adsorption. Sep Sci Technol 2006; 41(9): 1907–1925.
  • [11] Garcia-Basabe Y, Rodriguez-Iznaga I, de Menorval L, Llewellyn P, Maurin G, Lewisf DW, Binionsf R, Autieg MA, Ruiz-Salvadora R. Step-wise dealumination of natural clinoptilolite: structural and physicochemical characterization. Microporous Mesoporous Mater 2010; 135(1–3): 187–196.
  • [12] Pechar F, Rykl D (1983) A complex study of vibrational spectra of natural analcime. Chem Pap, 37:757-765.
  • [13] Mozgawa W, Sitarz M, Rokita M. Spectroscopic studies of different aluminosilicate structures. J Mol Struct 1999; 511-512: 251-257.
  • [14] Mozgawa W. The relation between structure and vibrational spectra of natural zeolites. J Mol Struct 2001; 596: 129-137.
  • [15] Ma X, Yang J, Ma H, Liu C. Zhang P. Synthesis and characterization of analcime using quartz syenite powder by alkali‐hydrothermal treatment. Microporous Mesoporous Mater 2015; 201:134–140.
  • [16] Sandoval MV, Henao JA, Rios CA, Williams CD, Apperley DC. Synthesis and characterization of zeolite type Ana framework by hydrothermal reaction of natural clinker. Fuel 2009; 88:272–281.

INVESTIGATION OF NATURAL ANALCIME-RICH ZEOLITE TUFF FROM TURKEY: A COMBINED XRD, XRF, FT-IR AND SEM STUDY

Yıl 2021, , 36 - 41, 24.12.2021
https://doi.org/10.20290/estubtdb.1010189

Öz

In this study, chemical and structural properties of natural analcime-rich zeolite tuff from Turkey and that of ion-exchanged forms investigated. The microporous structure and the presence of extra-framework cations are of great importance for characterizing the unique properties of zeolites. Ion-exchanged forms (K+, H+ and Ca2+) of analcime zeolite were prepared with 1 M KNO3,1 M Ca(NO3)2 and 1 M HCl solutions in a shaker for 6 hours at 80 °C. The obtained samples were characterized by X-ray diffraction (XRD), X-ray fluorescence (XRF), Fourier transform infrared spectroscopy (FT-IR) and scanning electron microscopy (SEM) techniques. Quantitative XRD analysis showed that the major component of the natural zeolite was analcime, together with varying amounts of quartz, feldspar and clay mineral.

Proje Numarası

20ADP231

Kaynakça

  • [1] Dyer A. An Introduction to Zeolite Molecular Sieves, John Willey and Sons Press, 1988.
  • [2] Gottardi G, Galli E. Natural Zeolites, Berlin: Springer-Verlag, 1985.
  • [3] Deer WA, Howie RA, Zussman J. An Introduction to the Rockforming Minerals, London: Longman, 1992.
  • [4] Tsitsishvili V, Dolaberidze N, Urotadze S, Alelishvili M, Mirdzveli N, Nijaradze M. Ion exchange properties of Georgian natural zeolites. Chem. J. Moldova 2017; 12(1): 95-101.
  • [5] Ataman G, Gündoğdu N. Analcimic zones in the Tertiary of Anatolia and their geological positions. Sediment Geol 1982; 31: 89-99.
  • [6] Esenli F, Özpeker I. Gördes çevresindeki neojen havzasının zeolitik diyajenezi ve höylandit klinoptilolitlerin mineralojisi, Türkiye Jeoloji Kurultayı Bülteni, 1993. pp. 8-18.
  • [7] Gündoğdu MN, Yalçın H, Temel A, Clauer N. Geological, mineralogical and geochemical characteristics of zeolite deposits associated with borates in the Bigadiç, Emet ve Kırka Neeogene Lacustrine basins, Western Turkey. Miner Deposit 1996; 31: 492-513.
  • [8] Esenli F, Uz B, Suner F, Esenli V, Ece ÖI, Kumbasar I. Zeolitization of tuffaceous rocks in the Keşan region, Thrace, Turkey. Geologia 2005;58: 51-161.
  • [9] Harada K, Tanaka K, Nagashima K. New data on the analcime-wairakite series. Am Mineral 1972; 57: 924-931.
  • [10] Hernandez MA, Petranovskii V, Avalos M, Portillo R, Rojas F, Lara VH. Influence of the Si/Al framework ratio on the microporosity of dealuminated mordenite as determined from N2 adsorption. Sep Sci Technol 2006; 41(9): 1907–1925.
  • [11] Garcia-Basabe Y, Rodriguez-Iznaga I, de Menorval L, Llewellyn P, Maurin G, Lewisf DW, Binionsf R, Autieg MA, Ruiz-Salvadora R. Step-wise dealumination of natural clinoptilolite: structural and physicochemical characterization. Microporous Mesoporous Mater 2010; 135(1–3): 187–196.
  • [12] Pechar F, Rykl D (1983) A complex study of vibrational spectra of natural analcime. Chem Pap, 37:757-765.
  • [13] Mozgawa W, Sitarz M, Rokita M. Spectroscopic studies of different aluminosilicate structures. J Mol Struct 1999; 511-512: 251-257.
  • [14] Mozgawa W. The relation between structure and vibrational spectra of natural zeolites. J Mol Struct 2001; 596: 129-137.
  • [15] Ma X, Yang J, Ma H, Liu C. Zhang P. Synthesis and characterization of analcime using quartz syenite powder by alkali‐hydrothermal treatment. Microporous Mesoporous Mater 2015; 201:134–140.
  • [16] Sandoval MV, Henao JA, Rios CA, Williams CD, Apperley DC. Synthesis and characterization of zeolite type Ana framework by hydrothermal reaction of natural clinker. Fuel 2009; 88:272–281.
Toplam 16 adet kaynakça vardır.

Ayrıntılar

Birincil Dil İngilizce
Konular Mühendislik
Bölüm Makaleler
Yazarlar

Meryem Akbelen 0000-0003-2535-5003

Proje Numarası 20ADP231
Yayımlanma Tarihi 24 Aralık 2021
Yayımlandığı Sayı Yıl 2021

Kaynak Göster

APA Akbelen, M. (2021). INVESTIGATION OF NATURAL ANALCIME-RICH ZEOLITE TUFF FROM TURKEY: A COMBINED XRD, XRF, FT-IR AND SEM STUDY. Eskişehir Teknik Üniversitesi Bilim Ve Teknoloji Dergisi B - Teorik Bilimler, 9(Iconat Special Issue 2021), 36-41. https://doi.org/10.20290/estubtdb.1010189
AMA Akbelen M. INVESTIGATION OF NATURAL ANALCIME-RICH ZEOLITE TUFF FROM TURKEY: A COMBINED XRD, XRF, FT-IR AND SEM STUDY. Estuscience - Theory. Aralık 2021;9(Iconat Special Issue 2021):36-41. doi:10.20290/estubtdb.1010189
Chicago Akbelen, Meryem. “INVESTIGATION OF NATURAL ANALCIME-RICH ZEOLITE TUFF FROM TURKEY: A COMBINED XRD, XRF, FT-IR AND SEM STUDY”. Eskişehir Teknik Üniversitesi Bilim Ve Teknoloji Dergisi B - Teorik Bilimler 9, sy. Iconat Special Issue 2021 (Aralık 2021): 36-41. https://doi.org/10.20290/estubtdb.1010189.
EndNote Akbelen M (01 Aralık 2021) INVESTIGATION OF NATURAL ANALCIME-RICH ZEOLITE TUFF FROM TURKEY: A COMBINED XRD, XRF, FT-IR AND SEM STUDY. Eskişehir Teknik Üniversitesi Bilim ve Teknoloji Dergisi B - Teorik Bilimler 9 Iconat Special Issue 2021 36–41.
IEEE M. Akbelen, “INVESTIGATION OF NATURAL ANALCIME-RICH ZEOLITE TUFF FROM TURKEY: A COMBINED XRD, XRF, FT-IR AND SEM STUDY”, Estuscience - Theory, c. 9, sy. Iconat Special Issue 2021, ss. 36–41, 2021, doi: 10.20290/estubtdb.1010189.
ISNAD Akbelen, Meryem. “INVESTIGATION OF NATURAL ANALCIME-RICH ZEOLITE TUFF FROM TURKEY: A COMBINED XRD, XRF, FT-IR AND SEM STUDY”. Eskişehir Teknik Üniversitesi Bilim ve Teknoloji Dergisi B - Teorik Bilimler 9/Iconat Special Issue 2021 (Aralık 2021), 36-41. https://doi.org/10.20290/estubtdb.1010189.
JAMA Akbelen M. INVESTIGATION OF NATURAL ANALCIME-RICH ZEOLITE TUFF FROM TURKEY: A COMBINED XRD, XRF, FT-IR AND SEM STUDY. Estuscience - Theory. 2021;9:36–41.
MLA Akbelen, Meryem. “INVESTIGATION OF NATURAL ANALCIME-RICH ZEOLITE TUFF FROM TURKEY: A COMBINED XRD, XRF, FT-IR AND SEM STUDY”. Eskişehir Teknik Üniversitesi Bilim Ve Teknoloji Dergisi B - Teorik Bilimler, c. 9, sy. Iconat Special Issue 2021, 2021, ss. 36-41, doi:10.20290/estubtdb.1010189.
Vancouver Akbelen M. INVESTIGATION OF NATURAL ANALCIME-RICH ZEOLITE TUFF FROM TURKEY: A COMBINED XRD, XRF, FT-IR AND SEM STUDY. Estuscience - Theory. 2021;9(Iconat Special Issue 2021):36-41.