Research Article
Identification of Asbestos Using Laser-Induced Breakdown Spectroscopy: A Viable Alternative to the Conventional Approach?
Table 2
Spectral peak intensities for various elements and spectral lines measured in six forms of asbestos.
| Element | Wavelength | Actinolite | Amosite | Anthophyllite | Chrysotile | Crocidolite | Tremolite |
| Ca | 397.01 nm | 829 | 174 | 0 | 357 | 239 | 2275 | Ca | 423.17 nm | 1829 | 864 | 0 | 498 | 844 | 4351 | Fe | 438.67 nm | 1035 | 3720 | 372 | 0 | 1768 | 586 | Fe | 440.73 nm | 697 | 2487 | 237 | 0 | 1128 | 0 | Mg | 517.51 nm | 3704 | 7007 | 6097 | 6205 | 2171 | 16009 | Mg | 518.64 nm | 5217 | 9106 | 8440 | 8979 | 2916 | 21897 | Na | 589.73 nm | 2405 | 825 | 712 | 440 | 9944 | 2145 | Si | 634.71 nm | 963 | 431 | 578 | 937 | 346 | 3564 | Si | 636.91 nm | 594 | 270 | 332 | 567 | 0 | 1983 | H | 656.21 nm | 1025 | 391 | 844 | 4021 | 0 | 2581 | Na | 744.74 nm | 445 | 1058 | 0 | 1424 | 0 | 1036 | K | 766.83 nm | 317 | 515 | 383 | 0 | 405 | 388 | O | 777.44 nm | 3780 | 1337 | 1840 | 10990 | 890 | 9562 |
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