“…Based on animal studies and studies during retrograde pyelography in humans, pyelotubular backflow occurs at 20–30 mmHg (27–41 cmH 2 O), pyelovenous backflow at 30–50 mmHg (41–68 cmH 2 O), and forniceal rupture at 70–200 mmHg (95–272 cmH 2 O) [ 1 , 2 ]. Newer studies using dynamic gadolinium-enhanced MRI have suggested, however, that IRB may occur at considerably lower pressures, starting at mean pressures as low as 15 mmHg (20 cmH 2 O) [ 13 ]. Thus, it seems logic that IRB happens as a continuous function of pressure, initially appearing in the center of the medullary pyramid, where the collecting ducts are less protected against reflux, compared to the peripheral ducts that end on the oblique part of the papillary surface.…”