Author: Ahmad Hosseini
Supervisors: Dr. Reza Maddahian, Dr. Sajad Khodadadi
This study models urine flow in the human ureter, both with and without blockages, using the Immersed Boundary Method (IBM). The simulation, which is cost-effective and independent of geometry, shows only a 1% error compared to analytical solutions.
It explores how different blockage percentages, peristaltic wavelengths, and wave amplitudes affect kidney stone movement and urine flow. Findings suggest that less blockage or increased wavelength and amplitude reduce stone excretion time.
However, more obstruction, higher amplitude, and shorter wavelength increase the risk of backflow and reflux. Wave amplitude has the most significant impact on stone movement and urine flow rate.
The human ureter, part of the upper urinary tract, transports urine from the kidney to the bladder using peristaltic pumping. This study simulates peristaltic flow in the ureter, with and without obstructions, using the Immersed Boundary Method (IBM), which is cost-effective and geometry-independent.
The simulation shows a 1% error compared to analytical solutions in estimating flow rate reduction due to reverse pressure. It examines how blockage percentage (0-60%), peristaltic wavelength (30-90 mm), and wave amplitude (1-2.5 mm) affect kidney stone dynamics and urine flow. Results indicate that stone excretion time decreases with less blockage or increased wavelength and amplitude.
Increased obstruction, higher amplitude, and shorter wavelength raise backflow and reflux risk. Among these parameters, wave amplitude significantly impacts stone movement and urine flow rate.
The innovations of the present work can be listed as follows:
When a microbubble is situated within an infinite environment and initially subjected to a pressure, the bubble's radius will exhibit a continuous fluctuation due to the symmetry of the system. This ensures that the bubble will not fail. The simulation geometry is a two-dimensional, symmetrical semicircle.
| Test case | Blockage ratio | Wavelength (mm) | Wave amplitude (mm) | Stone diameter (mm) | Mass (g) |
|---|---|---|---|---|---|
| TC2 | 0 | 60 | 1.5 | 0 | 0 |
| TC3 | 10 | 60 | 1.5 | 2.21 | 0.012433 |
| TC4 | 40 | 60 | 1.5 | 4.42 | 0.099466 |
| TC5 | 60 | 60 | 1.5 | 5.42 | 0.183403 |
| TC6 | 20 | 60 | 1 | 3.13 | 0.035322 |
| TC7 | 20 | 60 | 2.5 | 3.13 | 0.035322 |
| TC8 | 20 | 30 | 1.5 | 3.13 | 0.035322 |
| TC9 | 20 | 90 | 1.5 | 3.13 | 0.035322 |
| Test case | Changes in the time of stone exit | Changes in the Average mass flow rate passing through the inlet in the stage (V) | Changes in the Maximum flow rate | Changes in the maximum return movement of the stone |
|---|---|---|---|---|
| TC8 | 9.05% | -29.5% | 24% | -11.25% |
| TC9 | -2.02% | 21.9% | -13.3% | 2.5% |
This paper investigates urine transport in both normal and obstructed ureters using numerical simulations. It examines how blockage percentage, wavelength, and amplitude of peristaltic waves affect kidney stone dynamics and urine flow rate. The simulations, performed with a modified immersed boundary solver in OpenFOAM, consider three degrees of freedom. Key findings include: