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Chemical differences between white and gray mineral trioxide aggregate.
Saeed Asgary1, Masoud Parirokh, Mohammad Jafar Eghbal
1Endodontic Department, Shahid Beheshti Dental School, Tehran, Iran.
Journal of Endodontics
|January 27, 2005
Summary
Gray and white mineral trioxide aggregate (MTA) share key compounds like lime and silica. However, gray MTA contains significantly higher concentrations of aluminum oxide, magnesium oxide, and iron oxide compared to white MTA.
Area of Science:
- Biomaterials Science
- Dental Materials Science
- Materials Chemistry
Background:
- Mineral trioxide aggregate (MTA) is a widely used dental material.
- Understanding the compositional differences between white MTA and gray MTA is crucial for material selection and application.
- Previous analyses have established the primary components, but detailed comparative data on trace elements and oxides is essential.
Purpose of the Study:
- To quantitatively compare the elemental composition of white mineral trioxide aggregate (WMTA) and gray mineral trioxide aggregate (GMTA).
- To identify and quantify significant compositional variations between the two types of MTA.
Main Methods:
- Electron probe microanalysis (EPMA) was employed to determine the elemental composition.
- Quantitative analysis of major and minor oxide components in both WMTA and GMTA samples.
Main Results:
- Lime (CaO), silica (SiO2), and bismuth oxide (Bi2O3) were identified as dominant compounds in both WMTA and GMTA, present at comparable levels.
- Significant differences in oxide concentrations were observed: Al2O3 (+122%), MgO (+130%), and FeO (+1000%) were notably higher in GMTA compared to WMTA.
Conclusions:
- The primary chemical constituents of WMTA and GMTA are similar.
- The substantial increase in aluminum oxide, magnesium oxide, and particularly iron oxide content in GMTA accounts for the observed color and potential performance differences.
- These compositional variations highlight the need for careful consideration of MTA type based on clinical requirements.