ESTIMATION OF IRON AND MANGANESE CARBONATE VALUES IN DOLOMITES USING X-RAY DIFFRACTION METHOD

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.

KHASHEI M.; MIRAB SHABESTARI GH.; ZARRINKOUB M.H.

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

Journal Paper

Paper Information

Journal: Iranian Journal of Crystallography and Mineralogy Year:2012 | Volume:20 | Issue:3 Page(s): 583-592

Download Full-Text

Persian Verion

View:

1,390

Download:

Cites:

Information Journal Paper

Title

ESTIMATION OF IRON AND MANGANESE CARBONATE VALUES IN DOLOMITES USING X-RAY DIFFRACTION METHOD

Author(s)

KHASHEI M. | MIRAB SHABESTARI GH. | ZARRINKOUB M.H. | Issue Writer Certificate

Keywords

XRDQ2

DOLOMITEQ2

FERROAN DOLOMITEQ2

MANGANESE DOLOMITEQ2

Abstract

The aim of this research was to estimate iron and manganese carbonate values in DOLOMITEs using XRD technique. This method is done easily and with less cost than the conventional chemical methods which are used to determine the amount of iron and manganese.For this purpose, total number of 20 samples from four different formations with various ages and locations, including Soltanieh, Sibzar, Shotori and Mozduran Formations, were selected and their iron and manganese contents were measured using atomic absorption spectrophotometery technique. Then all samples were analyzed by XRD. Finally, with drawn cell space values versus amounts of iron and manganese, the graph was obtained and the function of mol% FeCO3+MnCO3=1271.5 d104 - 3667.2 (r2=0.897) was obtained from it. This function can be used to estimate iron and manganese carbonate contents in the other unknown DOLOMITE samples which have only been studied using XRD method.

Cites

No record.

References

APPLICATION OF GEOCHEMICAL DATA IN RECOGNIZING ORIGIN OF SOLTANIEH DOLOMITE AND DETERMINING TEMPERATURE OF DOLOMITE FORMATION, IN NORTH OF SEMNAN

Cite

APA: Copy

KHASHEI, M., MIRAB SHABESTARI, GH., & ZARRINKOUB, M.H.. (2012). ESTIMATION OF IRON AND MANGANESE CARBONATE VALUES IN DOLOMITES USING X-RAY DIFFRACTION METHOD. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 20(3), 583-592. SID. https://sid.ir/paper/4100/en

Vancouver: Copy

KHASHEI M., MIRAB SHABESTARI GH., ZARRINKOUB M.H.. ESTIMATION OF IRON AND MANGANESE CARBONATE VALUES IN DOLOMITES USING X-RAY DIFFRACTION METHOD. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2012;20(3):583-592. Available from: https://sid.ir/paper/4100/en

IEEE: Copy

M. KHASHEI, GH. MIRAB SHABESTARI, and M.H. ZARRINKOUB, “ESTIMATION OF IRON AND MANGANESE CARBONATE VALUES IN DOLOMITES USING X-RAY DIFFRACTION METHOD,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 20, no. 3, pp. 583–592, 2012, [Online]. Available: https://sid.ir/paper/4100/en

Related Journal Papers