Table 5.
Time ranges used to search for the second periodicity Pl.
| String # | HJD′range | Δt | n | PDM Po (d) | FAP | GLS Pl (d) | FAP |
|---|---|---|---|---|---|---|---|
| 1 | 16 200–19 300 | 3100 | 375 | 32.311918 ± 0.026102 | 0.005(5) | Not detected | NA |
| 2 | 24 000–26 100 | 2100 | 174 | 32.318880 ± 0.055707 | 0.009(9) | ∼700 | NA |
| 3 | 26 800–31 000 | 4200 | 632 | 32.324103 ± 0.010448 | 0.008(8) | 356 ± 8 | 0 ± 0 |
| 4 | 39 700–43 700 | 4000 | 648 | 32.338040 ± 0.010457 | 0.005(5) | 500 ± 16 | 0 ± 0 |
| 5 | 44 000–46 200 | 2200 | 524 | 32.310178 ± 0.031318 | 0.005(5) | 491 ± 27 | 0 ± 0 |
| 6 | 47 800–49 100 | 1300 | 231 | 32.324103 ± 0.262953 | 0.005(5) | ∼525 | NA |
| 7 | 52 600–59 000 | 6400 | 1900 | 32.348501 ± 0.005232 | 0.005(5) | 501± 44 | 0 ± 0 |
Notes. Δt is the range of days and n the number of data points. The orbital and long periods are given along with its false alarm probability (FAP); phase dispersion minimization (PDM) and generalized Lomb–Scargle periodograms (GLS) were used. For string 2 the residuals of the long-term tendency fitted with a third-order polynomial were used to determine the orbital period.
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