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Table 2
Ranges of a and M implied by the discoseismic models of the 3:2 QPOs.
| GRS 1915+105 | XTE J1550-564 | GRO J1655-40 | ||
| Frequencies | a | M/M⊙ [10.0−18.0] | M/M⊙ [8.4−10.8] | M/M⊙ [5.1−6.6] |
|
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| νU = νg, νL = νc | 0.70–0.78 | 6.4−9.0 | 3.9−5.5 | 2.4−3.3 |
| νU = νc, νL = νg | 0.90-0.94 | 12.8−19.1 | 7.8−11.6 | 4.8−7.1 |
|
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| νU = νp, νL = νc | 0.30–0.63 | 1.1−5.0 | 0.7−3.0 | 0.4−1.8 |
| νU = νc, νL = νp | 0.50–0.82 | 1.7−8.6 | 1.0−5.2 | 0.6−3.2 |
|
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| νU = νg, νL = νp | 0.00–0.82 | 3.9−9.7 | 2.4−5.8 | 1.5−3.6 |
| νU = νp, νL = νg | — | — | — | — |
Notes. The values in the brackets indicate the referential interval of M for each microquasar.
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