Non-destructive elemental analysis of large meteorite samples by prompt gamma-ray neutron activation analysis with the internal mono-standard method

• Published in: Analytical and bioanalytical chemistry Vol. 405; no. 27; pp. 8749 - 8759
• Main Authors: Latif, Sk. A., Oura, Y., Ebihara, M., Nakahara, H.
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 01-11-2013; Springer; Springer Nature B.V
• Subjects: Alloys; Aluminum; Analytical Chemistry; Biochemistry; Canyons; Characterization and Evaluation of Materials; Chemical composition; Chemistry; Chemistry and Materials Science; Food Science; Gamma rays; Geological surveys; Geology; Laboratory Medicine; Magnesium; Manganese; Mathematical analysis; Meteorites; Meteors & meteorites; Monitoring/Environmental Analysis; Neutrons; Nickel; Properties; Radioactivity; Research Paper; Slabs; Stony meteorites; Titanium; Trace elements; Japan; Prompt gamma-ray neutron activation analysis (PGNAA); Large samples; Neutron activation analysis; Meteorites; Internal monostandard method
• ISSN: 1618-2642; 1618-2650
• DOI: 10.1007/s00216-013-7331-1

Prompt gamma-ray neutron activation analysis (PGNAA) using the internal mono-standard method was tested for its applicability to analyzing large solid samples including irregularly shaped meteorite samples. For evaluating the accuracy and precision of the method, large quantities of the Geological Survey of Japan standardized rock powders (JB-1a, JG-1a, and JP-1) were analyzed and 12 elements (B, Na, Mg, Al, Cl, K, Ca, Ti, Mn, Fe, Sm, and Gd) were determined by using Si as an internal standard element. Analytical results were mostly in agreement with literature values within 10 %. The precision of the method was also shown to be within 10 % (1σ) for most of these elements. The analytical procedure was then applied to four stony meteorites (Allende, Kimble County, Leedey, Lake Labyrinth) and four iron meteorites (Canyon Diablo, Toluca (Mexico), Toluca (Xiquipilco), Squaw Creek) consisting of large chunks or single slabs. For stony meteorites, major elements (Mg, Al, Si, S, Ca, and Ni), minor elements (Na and Mn) and trace element (B, Cl, K, Ti, Co, and Sm) were determined with adequate accuracy. For iron meteorites, results for the Co and Ni mass fractions determined are all consistent with corresponding literature values. After the analysis, it was confirmed that the residual radioactivity remaining in the sample after PGNAA was very low and decreased down to the background level. This study shows that PGNAA with the internal mono-standard method is highly practical for determining the elemental composition of large, irregularly shaped solid samples including meteorites.