POSSIBILITY OF PRODUCING FORSTERITE FROM NATURAL SERPENTINE, IN ORDER TO USE IN REFRACTORIES INDUSTRY

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

DABIRI RAHIM; GHAFFARI MITRA; MOLLAI HABIB; MOSLEMPOUR MOHAMAD ELYAS

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: Journal of Advanced Processes in Materials Engineering Year:2015 | Volume:9 | Issue:1 (32) Page(s): 187-192

Download Full-Text

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Verion

View:

1,293

Download:

Cites:

Information Journal Paper

Title

POSSIBILITY OF PRODUCING FORSTERITE FROM NATURAL SERPENTINE, IN ORDER TO USE IN REFRACTORIES INDUSTRY

Author(s)

DABIRI RAHIM | GHAFFARI MITRA | MOLLAI HABIB | MOSLEMPOUR MOHAMAD ELYAS | Issue Writer Certificate

Keywords

FORSTERITEQ2

SERPENTINEQ2

REFRACTORYQ3

XRDQ2

DTA-TGQ2

Abstract

Petrography, XRD and DTA- TG studies indicate that SERPENTINE decomposition to FORSTERITE in high temperature. SERPENTINE has been expanded in Iranian ophiolitic rocks. Testing Iranian ophiolitic rocks shows that FORSTERITE has been produced from heating of SERPENTINE in 600 °C. Therefore it facilitates the usage of serpentinic rocks as primary material in REFRACTORY industry. The test results show that, Dehydration reactions on SERPENTINE started at approximately between 100 to 150 °C and dehydroxilation reactions started at approximately 550-700°C. As a result of thermal reaction the decomposition of SERPENTINE will take place and then changing in to olivine (FORSTERITE). Crystallization of olivine (FORSTERITE) will start at 600 °C.

Cites

No record.

References

No record.

Cite

APA: Copy

DABIRI, RAHIM, GHAFFARI, MITRA, MOLLAI, HABIB, & MOSLEMPOUR, MOHAMAD ELYAS. (2015). POSSIBILITY OF PRODUCING FORSTERITE FROM NATURAL SERPENTINE, IN ORDER TO USE IN REFRACTORIES INDUSTRY. ADVANCED PROCESSES IN MATERIALS, 9(1 (32)), 187-192. SID. https://sid.ir/paper/172560/en

Vancouver: Copy

DABIRI RAHIM, GHAFFARI MITRA, MOLLAI HABIB, MOSLEMPOUR MOHAMAD ELYAS. POSSIBILITY OF PRODUCING FORSTERITE FROM NATURAL SERPENTINE, IN ORDER TO USE IN REFRACTORIES INDUSTRY. ADVANCED PROCESSES IN MATERIALS[Internet]. 2015;9(1 (32)):187-192. Available from: https://sid.ir/paper/172560/en

IEEE: Copy

RAHIM DABIRI, MITRA GHAFFARI, HABIB MOLLAI, and MOHAMAD ELYAS MOSLEMPOUR, “POSSIBILITY OF PRODUCING FORSTERITE FROM NATURAL SERPENTINE, IN ORDER TO USE IN REFRACTORIES INDUSTRY,” ADVANCED PROCESSES IN MATERIALS, vol. 9, no. 1 (32), pp. 187–192, 2015, [Online]. Available: https://sid.ir/paper/172560/en

Related Journal Papers