| Literature DB >> 29936216 |
Thomas Sanford1, Adam J Gadzinski2, Thomas Gaither2, E Charles Osterberg2, Greg P Murphy2, Peter R Carroll2, Benjamin N Breyer2.
Abstract
BACKGROUND: Genital numbness and erectile dysfunction in cyclists may result from repeated perineal impacts on the bicycle saddle (micro-trauma) that occur during routine cycling. AIM: To evaluate the relationship between oscillation forces and perineal pressures among cyclists in a simulated laboratory setting.Entities:
Keywords: Cycling; Micro-Trauma; Perineum; Saddle
Year: 2018 PMID: 29936216 PMCID: PMC6085221 DOI: 10.1016/j.esxm.2018.05.002
Source DB: PubMed Journal: Sex Med ISSN: 2050-1161 Impact factor: 2.491
Figure 1Experimental design. Pressure mat was cut into strips and attached to the bicycle saddle with double-sided tape and suture. The 15 × 16 matrix of integer values that was taken at 100 Hz was summed for the total pressure measurement. There was 1 oscillation event every 5 seconds. The maximum pressure change for each 5-second interval was defined as the maximum pressure value minus the baseline value for that 5 seconds. The baseline was defined as all the values that did not exceed 1 SD from the median value.
Subject demographics
| Total, N = 39 | Men, N = 29 | Women, N = 10 | Men vs women, | |
|---|---|---|---|---|
| Age, y, mean (range) | 30 (18–44) | 30 (18–44) | 31 (28–35) | .77 |
| Height, cm, mean (range) | 175 (155–193) | 178 (163–193) | 165 (155–173) | <.01 |
| Weight, kg, mean (range) | 73.9 (45.4–111.1) | 78.5 (56.7–111.1) | 60.8 (45.4–78.0) | <.01 |
| BMI, mean (range) | 24.0 (17.7–31.3) | 24.1 (18.8–31.3) | 22.1 (17.7–29.5) | .06 |
| Ischial tuberosity distance, cm, mean (range) | 5.2 (4.2–7) | 5.1 (4.2–7) | 5.1 (4.5–6) | .98 |
| Commute, N (%) | 12 (31%) | 8 (28%) | 4 (40%) | .69 |
| Commute, min, mean (range) | 44 (15–180) | 52 (20–180) | 23 (15–40) | .20 |
| Ride recreationally, N (%) | 23 (59%) | 15 (52%) | 8 (80%) | .15 |
| Median min/weekly recreational ride, mean (range) | 110 (2–420) | 101 (2–240) | 126 (30–420) | .63 |
BMI = body mass index.
Figure 2Average of maximal changes. There was an increase in perineal pressure as the amount of oscillation increased from 0.8–1.5g. This pressure was mitigated by the presence of a shock absorber in the stationary group. The shock absorber had less of an effect in the riding group. The trends remained after correcting the amount of pressure by the oscillation.
Figure 3Relationship between pressure and oscillation. There is a linear direct relationship among small, medium, and large oscillation events with r of 0.8.
Changes in perineal pressure above baseline with standard saddle
| Percent pressure change | Percent pressure change | ||
|---|---|---|---|
| Size oscillation | Percent change pressure (95% CI) | Size oscillation | Percent change pressure (95% CI) |
| Small | 10.3 (7.7–12.7) | Small | 19.8 (16.4–23.2) |
| Medium | 16.3 (12.9–19.5) | Medium | 24.6 (19.8–29.4) |
| Large | 19.4 (15.1–23.7) | Large | 26.9 (22.8–31.0) |
| <.01 | <.01 | ||
ANOVA = analysis of variance.
Changes in perineal pressure above baseline with addition of seatpost shock absorber
| Condition | Size oscillation | No shock | Shock | Decrease | |||
|---|---|---|---|---|---|---|---|
| % Change pressure | Stationary | Small | 10.3 | 6.5 | 58% | <.01 | |
| Stationary | Medium | 16.3 | 10.4 | 57% | <.01 | ||
| Stationary | Large | 19.4 | 12.2 | 59% | <.01 | ||
| Riding | Small | 19.8 | 16.8 | 18% | .11 | ||
| Riding | Medium | 24.6 | 21.3 | 15% | .23 | ||
| Riding | Large | 26.9 | 24.6 | 9% | .41 | ||
| % Change pressure | Stationary | Small | 18.6 | 11.6 | 60% | <.01 | |
| * | Stationary | Medium | 37.9 | 21.1 | 80% | <.01 | |
| Correction factor | Stationary | Large | 53.6 | 34.9 | 53% | <.01 | |
| Riding | Small | 35.5 | 31.8 | 12% | .62 | ||
| Riding | Medium | 58.7 | 45.8 | 28% | .24 | ||
| Riding | Large | 79.5 | 76.4 | 4.0% | .81 | ||
Figure 4Points of maximal pressure in men and women. For men and women, the distribution of the maximum pressure averaged across all participants. The increases in pressure were absorbed by relatively small areas corresponding to known bony landmarks.