Abstract
<h3>Objectives</h3> A VMAT technique using a rotatable tabletop for TBI in supine position is newly applied at UMC Utrecht. We aimed to assess the dose distribution robustness against daily isocenter shifts. <h3>Methods</h3> The tabletop enables rotation from head-first (HF) to feet-first (FF) supine position while the patient remains immobilized in an individualized whole-body vacuum matrass and a thermoplastic facemask. The treatment plan was optimized on the HF and FF CT-scans, co-registered on the overlapping anatomical region (20 cm longitudinal). Depending on patient-length, 4 to 6 isocenters with overlapping arcs (4 cm longitudinal) were used. Prescription dose (PD) was 12Gy in 6 fractions with mean dose constraints for lungs/kidneys <10Gy and lenses <8Gy. Daily patient-position verification procedure (PV) comprised: pelvic HF-iso3 (CBCT + online corrected); thoracic HF-iso2 (CBCT only, no correction); knee region FF-iso (CBCT + online corrected). Brain HF-iso1 and FF-iso4 or -iso5 (patient length dependent) not imaged. HF (FF) radiation delivery followed HF (FF)-PV. After each fraction, the dose distribution of the first 3 treated patients (length range 110-195 cm) was recalculated applying the registered isocenter corrections/shifts. Then, the 6-fraction rigidly accumulated dose distribution was compared to the original. <h3>Results</h3> The maximum shift for HF-iso2 was 0.4 cm lateral, 0.8 cm longitudinal and 0.9 vertical and for the knee region FF-iso 0.7 cm lateral, 0.4 cm longitudinal and 0.5 cm vertical over all patients/fractions. Over all patients, the differences in PTV volume receiving 80%, 90% and 120% PD between accumulated and original dose distribution were <1%, while a +3% V110% PD maximum difference was found. The maximum mean dose difference for lenses, lungs and kidneys between accumulated and original dose distributions was +1.0 Gy, +0.2 Gy and +0.6 Gy, respectively. <h3>Conclusion</h3> The dose distribution of the described VMAT technique for TBI, is proven to be robust against daily observed isocenter shifts.
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