Laboratory Tests on the Production of High Quality Zeolite

International Mineral Processing Congress
Gülay Bulut Olgaç Kangal Mustafa Özer Mustafa Tarkan Yunus Emre Benkli Istanbul Technical University
Organization:
International Mineral Processing Congress
Pages:
1
File Size:
102 KB
Publication Date:
Jan 1, 2003

Abstract

"Zeolites are naturally occurring as hydrated aluminosilicate minerals. They belong to the class of minerals known as “tectosilicates” and are related to the common minerals feldspar and quartz. Seven natural zeolites that occur in large, commercially exploitable deposits, are: clinoptilolite, chabazite, mordenite, phillipsite, erionite, analcite, and ferrierite. Among them, clinoptilolite is the most abundant one and is not the best known, but is one of the more useful natural zeolite. Clinoptilolite [(Na3K3) (Al6Si30O72) 24 H2O] is very closely related to heulandite and is currently being considered for disuse it self as it may just be a variety of heulandite. It differs from heulandite significantly only in its enrichment in potassium and slightly more silica and it is argued that a separate mineral is not needed.There are large zeolite deposits in western part of Turkey. The sample used in this study was taken from the Gördes region of these deposits. Screen, chemical, XRD and mineralogical analyses were used to determine properties of the natural zeolite sample used in this work.According to the size distribution of the sample, it is found that the zeolite sample used in this study is below 1 mm in size and almost 80% of it is below 0.5 mm. X-Ray Diffraction (XRD) and mineralogical analyses show that the natural zeolite is found to be in the forms of clinoptilolite and heulandite. Clinoptilolite forms as a devitrification product of volcanic glass in tuffs. Quartz, clay minerals, orthoclase, plagioclase, biotite, seruzite-muskovite and epidote were observed as impurities. XRD analysis also shows that the sample contains approximately 58-60% clinoptilolite, 5% quartz, 5% feldspar, 10% smectite, 5- 10% illite and mica and remaining volcanic tuffs. Several types of mineral processing methods were performed in order to remove impurities from the natural zeolite sample to produce high purity zeolite. Gravity separation methods such as shaking table and superpanner were carried out for separating heavy minerals, while high intensity dry magnetic separation was used for discarding magnetic minerals."
Citation

APA: Gülay Bulut Olgaç Kangal Mustafa Özer Mustafa Tarkan Yunus Emre Benkli Istanbul Technical University  (2003)  Laboratory Tests on the Production of High Quality Zeolite

MLA: Gülay Bulut Olgaç Kangal Mustafa Özer Mustafa Tarkan Yunus Emre Benkli Istanbul Technical University Laboratory Tests on the Production of High Quality Zeolite. International Mineral Processing Congress, 2003.

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