Tibial stress fractures are thought to result from a fatigue-failure process
where bone failure is highly dependent on peak strain magnitude. Little is
known regarding the mechanical loading environment of the tibia during graded
running despite the prevalence of this terrain. To probe the sensitivity of the
mechanical loading environment of the tibia to running grade, tibial strains
were quantified using a combined musculoskeletal-finite element modeling
routine during graded and level running. Seventeen participants ran on a
treadmill at ±10{\deg}, ±5{\deg}, and 0{\deg} while force and motion
data were captured. At each grade, participants ran at 3.33 m/s and a
grade-adjusted speed, that was 2.20 m/s and 4.17 m/s for uphill and downhill
conditions, respectively. Muscle and joint contact forces were estimated using
inverse-dynamics-based static optimization. These forces were applied to a
participant-informed finite element model of the tibia. 50th percentile
pressure-modified von Mises strain was lower (≤-130 με)
during downhill running compared to level and uphill running at 3.33 m/s.
However, neither 95th percentile strain (peak strain) nor the volume of bone
experiencing strains ≥4000 με (strained volume) were
different between grades (F(4)≤3.28, p≥0.01). In contrast, peak
strain and strained volume were highly sensitive to running speed
(F(1)≥10.61, p≤0.001), where a 1 m/s increase in speed resulting in a
9 % and 155 % increase in peak strain and strained volume, respectively.
Overall, these findings suggest that faster running speeds, but not changes in
running grade, may increase the risk of developing a tibial stress fracture