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Updated: Aug 5, 2026

Real-Time Void Spot Assay
Published on: February 10, 2023
Development of an Imaging-Based Method for Analyzing Voided Urine Flow Using Conventional and High-Speed Video
Masahiro Goto1, Tomonori Minagawa1, Hiroaki Hara1
1Department of Urology, Shinshu University School of Medicine, Matsumoto, Japan.
Voided urine form parameters, length to first twist (LFT) and length to scattered water (LSW), offer new insights into lower urinary tract pathology independent of traditional uroflowmetry. Dynamic voided urine velocity and cross-sectional area (CA) can also be measured non-invasively.
Area of Science:
- Urology
- Biomedical Engineering
- Fluid Dynamics
Background:
- Conventional uroflowmetry is the standard for assessing lower urinary tract symptoms.
- There is a need for independent parameters to evaluate urinary tract pathology.
- Novel methods for dynamic urine flow analysis are being explored.
Purpose of the Study:
- To determine if voided urine form parameters can independently assess lower urinary tract pathology.
- To evaluate a new method for dynamically measuring urine velocity and cross-sectional area (CA).
Main Methods:
- A male urethral phantom model was used with a high-speed video camera (HSVC) to record voided water.
- Voided water form parameters (LFT, LSW, VWA) were measured alongside uroflowmetry.
- Urethral deformities were simulated using silicone tube attachments.
- Dynamic velocity and CA of voided water were analyzed.
Main Results:
- Length to first twist (LFT) and length to scattered water (LSW) increased with pump speed and were sensitive to urethral strictures.
- Voided water angle (VWA) showed minor increases with simulated urethral deformity.
- Dynamic voided water velocity and CA increased with pump speed but were unaffected by simulated deformities at fixed flow rates.
Conclusions:
- LFT and LSW are novel parameters for evaluating lower urinary tract pathology, distinct from conventional uroflowmetry.
- Combining uroflowmetry with HSVC allows for non-invasive measurement of voided water velocity and CA.
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