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. 2022 Mar 15;82(3):226. doi: 10.1140/epjc/s10052-022-10161-y

Fig. 1.

Fig. 1

Baseline-removed and pole-zero corrected waveforms from PONaMa-1 events, taken with the TUBE scanning system. Both the bulk γ event (in blue) and the surface α event, taken with the source incident at r=-7.5 mm (in red), have 2615 keV of energy. The waveform regions used to calculate the DCR parameter for each waveform, determined as described in Sect. 2.4, are indicated by the shaded boxes, shown in the same color as the waveform they correspond to