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Principles of Modern Radar - Volume 2 1891121537

Principles of Modern Radar - Volume 2 1891121537

Principles of Modern Radar - Volume 2 1891121537

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714 CHAPTER 16 Human Detection With <strong>Radar</strong>: Dismount DetectionRV = v/HT. The parameter RLc can be expressed in terms <strong>of</strong> RV as RLc = 1.346 √ RV,leading to the following simplification in the expression for Dc:Dc = 1.346 √RV(s) (16.5)The duration <strong>of</strong> support, Ds, the duration <strong>of</strong> double support, Dds, and duration <strong>of</strong>balance are all linearly dependent upon the cycle duration and are given asDs = 0.752Dc − 0.143 (s) (16.6)Dds = 0.252Dc − 0.143 (s) (16.7)Db = 0.248Dc + 0.143 (s) (16.8)A relative time parameter, t%, is defined ast% = t(16.9)Dcwhile the relative duration <strong>of</strong> support, Ds%, is defined asDs% = Ds(16.10)DcIn both (16.9) and (16.10), the term “relative” refers to the time elapsed as being a percentage<strong>of</strong> the overall walking cycle duration.These temporal values are used in the parametric model, which produces the 3-Dkinematic equations for the time-varying change in position <strong>of</strong> certain points on the bodyas well as the time-varying angular motion <strong>of</strong> elbow, knee, and ankle joints. All motionis described relative to the origin, defined at the bottom <strong>of</strong> the spine, OS (as shown inFigure 16-3). Note that the thigh height, which is a critical parameter in the model, isdefined as the distance between the ground and the top <strong>of</strong> the thigh bones, while OS islocated higher up at the base <strong>of</strong> the spine. The kinematics governing pelvic rotations andflexing at the hip are thus also modeled.Consider the equations given by the Boulic-Thalmann model for the periodic trajectoriesthat govern the motion <strong>of</strong> the origin, OS, for the duration <strong>of</strong> one walking cycle:Vertical translation:OS V = 0.015RV (sin 2π (2t% − 0.35) − 1) (16.11)Lateral translation:⎧⎨ −0.032 for RV > 0.5OS L = A L sin 2π (t% − 0.1) , where A L =⎩−0.128RV 2 + 0.128RV for RV < 0.5(16.12)Forward/backward translation:OS FB = A FB sin 2π (2t% − 2φ FB ) (16.13){−0.021 for RV > 0.5where φ FB = 0.625 − Ds% and A FB =−0.084RV 2 + 0.084RV for RV < 0.5A plot <strong>of</strong> the trajectories <strong>of</strong> OS for varying values <strong>of</strong> RV is shown in Figure 16-4. Thesecurves are significant because when these components are combined to form the overall

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