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Friction, lubrication and wear in lower kinematic pairs  157

















                     Figure 4.56

                                 road moves with a velocity V = o)R 0, where co denotes the angular velocity
                                 of the wheel and R 0 is the effective rolling radius. During a braked rolling
                                period, the band velocity of the tyre increases to the road velocity a)R 0 at
                                the entrance to the contact zone and is steady until approximately one-half
                                of the contact length has been traversed (Fig. 4.56, case (a)). From that
                                moment onwards the tyre band velocity decreases in a non-linear way
                                towards the rear of the contact. As a result of that a variable longitudinal
                                slip velocity is produced in the forward direction. The slip velocity increases
                                with the speed of the vehicle and plays a particularly significant role in
                                promoting skidding on a wet road surface. A similar slip velocity pattern is
                                established in the rear of the contact but this time in a backward direction
                                (Fig. 4.56, case (b)).


                                4.14.6. Tyre performance on a wet road surface
                                Figure 4.57 shows, in a schematic way, a pneumatic tyre in contact with a
                                wet surface of the road. The contact area length is divided into three regions.
                                It is convenient to assume that the centre of the rolling tyre is stationary and
                                the road moves with velocity V. Approximately, it can be said there is no
                                relative motion between the tyre and the road within the front part of the
                                contact zone when the former traverses the contact length. Due to the
                                geometrical configuration, a finite wedge angle can be distinguished
                                between the tyre and the water surface just ahead of the contact zone (Fig.
                                4.57), and, under conditions of heavy flooding, a hydrodynamic upward
                                thrust P h is generated as a result of the change in momentum of the water
                                within the converging gap. The magnitude of this upward lift increases in
                                proportion to the forward velocity of the tyre relative to the road surface.











                     Figure 4.57
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