First published online March 14, 2005
Journal of Experimental Biology 208, 1191-1200 (2005)
Published by The Company of Biologists 2005
doi: 10.1242/jeb.01485
In vivo muscle function vs speed II. Muscle function trotting up an incline
Steven J. Wickler1,*,
Donald F. Hoyt2,
Andrew A. Biewener3,
Edward A. Cogger1 and
Kristin L. De La Paz1
1 Equine Research Center, California State Polytechnic University, Pomona,
CA 91768-4032, USA
2 Biological Sciences Department, California State Polytechnic University,
Pomona, CA 91768-4032, USA
3 Concord Field Station, Department of Organismic and Evolutionary Biology,
Harvard University, Bedford, MA 01730, USA

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Fig. 1. Typical recordings for the entire stride for a forelimb and hindlimb during
trotting up an incline. The top graphs include tracings of accelerometer
records that were used to identify stance phase (gray shaded area with hoof
lift-off denoted by vertical arrow). EMG activity patterns are shown below the
accelerometer records to demonstrate when the muscle was active.
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Fig. 2. Normalized stance phase muscle lengths (means ± 1
S.E.M.) of the triceps and vastus for all
horses at all speeds (N=4). The grey curve represents the mean of the
same horses for locomotion over all speeds at 0% slope (from
Hoyt et al., 2005 ). On the
incline, both muscles shortened more than on the level.
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Fig. 3. Joint angles (broken lines) and normalized muscle lengths (solid lines,
where 1.0 = length at rest), at 3.25 m s-1 for the triceps (A) and
for the two patterns of muscle strain observed in the vastus (B; referred to
in Hoyt et al., 2005 ). Phases
(denoted by vertical broken lines and numbers), based on kinematics, were the
same as used in the analysis of the data obtained during level locomotion.
Mean duration of EMG activity is indicated by shaded gray bars.
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Fig. 4. Total strain (change in normalized muscle length) and strain rate
(L s-1) of the triceps (during phase 3) as a function of
trotting speed on a 10% incline (black symbols, mean ± 1
S.E.M.). Total strain on the level is denoted
by gray symbols (Hoyt et al.,
2005 ). Strain and strain rate during incline locomotion did not
change with speed but were greater than during level locomotion.
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Fig. 5. The average strain (change in normalized muscle lengths; means ± 1
S.E.M.) of the vastus for the three phases of
stance identified in Fig. 3
(phases 3-5). There was no overall effect of trotting speed. The muscle
contracted concentrically during all three phases and the total concentric
strain during the three phases was greater on an incline (black symbols) than
on the level (gray symbols).
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Fig. 6. Shortening rates (L s-1; means ± 1
S.E.M.) of the vastus for phases 3-5. For
phases 4 and 5 the shortening rates increased with speed and were greater on
the incline (black symbols) than on the level (gray symbols).
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Fig. 7. EMG patterns (means ± 1 S.E.M.) for
the triceps and vastus as a function of speed on the incline (black)
versus the level (gray; Hoyt et
al., 2005 ). (A) On an incline at low speeds, EMG activity of both
muscles started near the time of foot contact, but as speed increased the
muscle was activated earlier. (B) As speed increased on the incline, EMGs of
both muscles were active for a smaller percentage of stance, but for a larger
fraction than at the same speed on the level. (C) Integrated EMG activities of
both muscles increased with speed and were greater on the incline.
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Fig. 8. Stride parameters (means ± 1
S.E.M.) for both limbs measured on the
incline (black) versus on the level (gray;
Hoyt et al., 2005 ). (A) Stride
period decreased with speed and was longer on the incline than on the level,
and was not different between the limbs. There were differences between the
limbs for all the other parameters listed. (B) Swing time on the incline was
not different from that on level for the forelimb, but was shorter for the
hindlimb. (C) Time of contact on the incline was longer in the forelimb but
not different in the hind limb. (D) Step length on the incline was longer for
the forelimb but not different for the hindlimb. (E) The duty factor on the
incline was not different from that on the level.
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© The Company of Biologists Ltd 2005