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Gait & Posture 6 (I 997) 27 38
Extracting gravity line displacement from stabilographic recordings
Received‘9 August 1995;accepted 6 August19%
Abstract
Three algorithmsfor determininggravity line (GL) location from center of pressure(COP) and horizontal force {F,) recordings are suggesled.The afgorithms are designedto study upright standing postureand are basedon the following premises:(a) the font(feet) is 2~solid body and doesnot move, (b) the axis of rotation of the anklejoint doesnot dispface,and (c) the forcesand momentsactmg at the ankle joint can be reduced to a resultant force through the axis of rotation and i? force couple. The algorithmsare: ( 1) Single-pendululum algorithm.The human body is modeledasan inverted pendulumoscillatingaround the ankle joint(s). Becausethe oscillationsare small,the equationsof movementcan be linearized and the horizontal position of the gravity line (GLP) located. (2) Trend-eradication algorithm. The second integral of the horizontal force calculated and an initial integration constant (.?, the initial horizontal GL velocity) is found from the trend of the displacementcurve, (3) Zero-poitrr-toxro-point integration. When the horizontal force is zero, the horizontal position of the gravity line (GLP) passesthrough the COP. The instantaneousGLP and its velocity are determinedby integrating F, from one zero point to another zctropomt. k7 I’N7 Elscvier ScienceB.V. ki*,r~rorc/~~: Stabilography: Posturography:Gravity line: Center of pressure;Center of gravity
Since the pioneer study of Hellebrandt [l] posturographic recordings from force platforms are commonly used for examining a person’s ability to maintain balance [2--71. As a representative measure of balance, the center of pressure (COP), or the resulting torque on the ground plane, is usually analyzed [8-13). A variety of methods have been employed to analyze COP 114-161. The methods range from specially designed techniques like the length of the path traveled by the COP [17,18] to routine procedures of signal processing such as parameters of statistical distribution (means, standard deviations [14,19,20]), ranges and areas of variation [12,13,2 I 231, velocities of COP migration [21,23,24], transfer f-unctions 1257,spectral characteristics [25-291, and autocorrelation and autoregression analysis [30-361. During the last few years several new approaches have been used, including evolutionary spectral analysis * Corresponding author. Tel.:
t I 814
8653445;
fax:
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X657441, 0966-6362.97, S:17.004’ 1947 Elsevier PII Sl~‘)hh-6~h?i96101 lo! -0
Science
B.V. All rightsreserved
[37], fractal dimensions [38,39], Grassberger-Procaccia coefficients developed to study dimensionality of chaotic processes [40-421, random walk analysis [40.41,43- -451. and time-to-contact measures 146,471. For review, see also Carrol and Freedman [48] and Prieto et al. [49]. Some of these procedures have been used for purely descriptive purposes, though, in many cases the researchers assumed that the COP directly portrays body displacement (‘body sway’) and :or the efficacy of the neural control of upright stance. Center of pressure.however, is an indirect measureof body sway. As early as 1959 Thomas and Whitney [SO] reported that the COP measured by the force platform and the horizontal position of the gravi[y line (GLP) did not coincide. The gravity line is 21 vertical line passing through the center of gravity. COG. of the body. This difference has been confirmed by Murray et al. [Sl] who estimated the GLP from filming. Winter and colleagues have provided a tremendous body of research on both COP and COG characteristics in o
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variety of tasks [.52-55,16]. In particular, Eng and Winter [52] compared COP and GLP displacement curves during a balance task which required raising a horizontally oriented light weight rod held between the hands and found that the two curves were very different. The COP and the GLP or COG variables can differ in amplitude, phase, and frequency [50,56-601. Only in pure static cases is the COP identical to the GLP [l]. Stabilographic recordings contain not only a static component depending solely on GLP but also a dynamic component due to inertial forces [50,62-651. The higher the frequency of body oscillation, the greater the acceleration, and the larger the contribution of inertial forces to the stabilogram. Even during quiet stance, the contribution of the acceleration terms is substantial [53,66]. According to estimates by Gurfinkel [63], at a frequency of 0.2 Hz the forces due to body acceleration contribute 10% to the stabilographic recordings; this contribution increases to about 50% at a frequency of 0.5 Hz and at a frequency larger than 1 Hz the stabilographic recordings reflect mainly inertial forces. Spectral density analysis [67] have revealed that the mean frequency during quiet standing is approximately 0.7 Hz. At this frequency, the inertial forces may determine more than 50% of the COP displacement. Furthermore, this could be important in many pathologies where the mean frequency of the COP oscillation increases to 1 Hz or even higher. For example, increased power spectrum values have been reported around a frequency of 1 Hz in patients suffering from Friedrech’s ataxia [68] and tubes dorsalis [69], as well as in patients with local lesions of the brain [70]. Similar findings have been reported for normal people whose leg muscle afferents were blocked by ischemia [27,71,72]. ‘The one-hertz phenomenon’ [73] is thought to be due to vestibular reflexes [68,69,73]. Higher frequencies - between 2 and 4 Hz - have been reported for patients with anterior lobe atrophy [68]. At such high frequencies, the COP does not represent GLP displacement. The horizontal ground reaction force may provide more useful information than the COP [7,16,52,58,75771. Horizontal force is proportional to the horizontal acceleration of the COG of the body and after normalization by body mass its second integral is equal to the displacement of the GLP. Hence, if body sway is an object of interest, analyzing horizontal force rather than COP appears attractive. While this COG-horizontal force relationship is well established it has not been used widely in practical research because the initial constants of integration (position and velocity) are usually not known. Shimba [78] proposed estimating the initial integration constants through a curve fit of two different functions. Specifically the method requires knowing S(r), which is the second integral of the horizontal
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ground reaction force, and E(t) = xP + zJ;oX]FOz), where x,, is the x-coordinate of the point of application of the ground reaction force, zG is the vertical component of the position vector of the COG of the body, and F,, and F,, are the horizontal and vertical components of the ground reaction force. According to Shimba [78] (page 56) ‘the curve fitting of S(t) with E(t)’ is done using ‘least squares with three unknowns’. Note that this approach requires knowledge of both the horizontal and vertical forces. Benda et al. [79] estimated the GL migration by filtering the COP time history data. This method does not require the knowledge of integration constants and is based on the presumption that the COP fluctuates about the GLP and contains higher frequency components. Though the postulations are rational, the method is unable to accommodate phase differences between the GLP and COP time histories and, thus, can only be applied when the frequency of body sway is low. Also, the outcome of this methods depends on the filtering cutoff frequency which is selected arbitrarily. The aim of this paper is to show several different ways of estimating GL location from force platform recordings.
1. Main model
For a standing person, the following assumptions are made: (1) the feet do not move and are considered solid bodies; (2) the axis of ankle joint rotation is fixed (this assumption is confirmed by the studies of Inman [80] and Bogert et al. [Sl]); and (3) all of the forces and moments acting at the ankle joint can be replaced by a resultant force acting through the joint axis of rotation and a couple. The forces and couples acting on the foot in a single-pendulum model of a standing person are illustrated in Fig. 1. The origin of the reference system is the intersection of the supporting surface and the vertical line passing through the ankle joint center. The following forces and couples are acting on the foot: Fz,,, CF,,,, and T, are the forces and couple (torque) at the ankle joint; F,,,, F.+, and T, are the external forces and external torque; and IV’ is the weight of the foot. Because the foot system is in equilibrium, the sum of the forces and the sum of the moments are zero. The equations in scalar form (sagittal projection) are: r;,,, = - Fx,, Fz,e = - ( W- + F,,,) M,=F3,exd,+T,+F,,,xh,+
Wfxdf
(1)
The horizontal ground reaction force, F& and the vertical force acting at the ankle joint, Fz,,, pass through the origin, 0, and do not contribute to the moment about this point. The moment due to the
D.L.
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weight of the foot is constant. Thus the equation COP location can be written as:
for
(2)
During standing, ankle joint height, h,, is constant and fluctuations in the vertical forces are so insignificant that they can be confused with ballistocardiographic (501 signals. Hence, ankle joint torque and horizontal force are the primary determinants of COP location. Since F, r = - F, a the horizontal force acting at the ankle joint(s). F,.,,, is easily determined. Thus, the con-
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tribution of the ankle joint torque. I’;,. 1s &he only undetermined variable. According to classical mechanics. the sum of the moments about a fixed point A of ah external forces acting on a system is equal to the time rate of change of the total angular momentum of the system about point A. Consider rotation around the ankle ,joint center fii,, = 1 M,, = mgd,y.,, + 7:,
or
7, --: B,
- /iI,~d,..(,
(3)
where tiU is the time rate of change of the angular momentum about the ankle joint center. IV!,: is a moment taken with respect to the ankle joint, and dp,<,is the moment arm of the force of gravity applied at the COG of the system. From Eq. (3) rt follows that the ankle joint torque is an algebraic turn of a ‘static’ moment. rrz,qd+,, which is a product of the system‘s weight times the corresponding moment arm, and a ‘kinetic’ moment. I?<,, which is numerically equal to the time rate of the change of the anguiar momentum of the system, Only the static moment is of mtcrest, however. The difficulties encountered by the presence of & in Eq. (3) need to be overcome. In essence. this is the premise of the suggested algorithms.
2. Algorithms
Buckground. For this algorithm, t&o additional assumptions are made: (1) joint motion is only in the ankle joint(s) and (2) body sway is small. Thus, the body is modeled as an inverted pendulum (Fig. 1). Similar single-pendulum models have been used previously by other researchers [63,6X75,82 -841. Small magnitudes of body sway permit linearizing the equations - instead of sin B the value of (1 can he used. The model can be described by the fol?owing equation: T, = I$ - mC cos cl + (mi - mgr sin H )
(J!
where I is the moment of inertia of the ‘whole body minus the foot(feet)’ system with respect to its center of mass, I’ is the distance from the ankle to the system’s center of mass, and 0, is the angle of the longitudinal axis of the body to the vertical. Eq. (4) can be linearized and written as: T, = I.$ - mgr0
-d,-
Fzfe -c-+ Fig
1. Single-pendulum
model.
(5)
where I<, is the moment of inertia with respect to the ankle joint(s), I, - I+ mr’. Eq. (5) is identical to Eq. (3), fit, = I,(?. Since angular and linear acceleriltions are interrelated for a single pendulum and the angle (1 is small for the system under discussion, ii can be found from the known values of .i:.
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Algorithm: Step 1. Determine the moment generated by the weight of the foot. According to Zatsiorsky and Seluyanov [85], the mass of the foot is 1.371 + 0.155% of the body mass, and the foot’s center of mass is located at 44.1 +_3.6% of foot length. Using these coefficients and measuring the horizontal distance of the ankle joint center to the heel, the moment arm of the weight of the foot, dr- is calculated and its moment is determined. However, the moment is small, on the order of 0.99 Nm, and can be neglected. If higher accuracy is required, the calculated value of the moment can be included in Eq. (1) and taken into account in Eq. (2). Step 2. Calculate the torque in the ankle joint(s). The moment generated by the horizontal force acting at the ankle joint(s) is subtracted from the moment of the ground reaction force (see Eq. (2)).
T, = F,!, x d, - F,+ x h,
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2.2. Second algorithm technique
(GL-2): Trend-eradication
Background. The GLP displacement, x,,,(t), is the second integral of the horizontal acceleration of the COG. Considering only the anterior-posterior component, it follows that:
Initial constants for integration, x(t,) and i(t,), are, however, not known. If an arbitrary value, for instance zero, of x(t,) were selected there would be a constant shift of the calculated GLP with respect to the actual GLP. This would affect the mean value of the GLP. Typically, though, the mean is not an important variable in posturographic studies and any value within the range of the COG travel can be used for x(t,). Arbitrary selection of i(to) will result in an erroneous linear ‘drift’ of the calculated GLP. This drift, (ia,,., &&to)). t, where &,(tJ is an arbitrary value of the initial velocity constant and Irea, is the real value of the initial velocity, would accumulate over time and bring the estimated GLP far from the real area of GLP travel. The rate of this linear trend of the GLP displacement is used as an estimation of the initial velocity, i(r,). This method is based on the assumption that the GLP migration over the period of observation, T, is stationary. It was assumed that when the linear trend is calculated over a large time interval error due to small differences between the initial and final CL positions does not affect the estimation of the initial velocity?
Step 3. Calculate the static moment in the ankle joint(s). Eq. (5) is used. The product I,8 is calculated and then subtracted from the ankle joint torque, T,. Subsrep 2. The angular acceleration # is estimated as T/r. The vertical component of the acceleration of the center of gravity is being disregarded. The distance from the ankle joint(s) to the system’s COG, Y, is estimated. According to data from Kozyrev [86], on average, the whole body COG is located at 57.1 + 0.127% (2 + m) of body height in males and 55.9 + 0.106% of body height in females. The height of the foot’s COG is approximately 40% of ankle joint height, h,, and the two feet together are approximately 2.75% of body weight. Using these values, the location of the COG of the ‘whole body minus the foot (feet)’ system is 58.71% of body height for males and 57.48% of body height for females. The difference, Y= h, - h,, is now calculated. Substep 2. The moment of inertia, I,, is estimated. Segmental moments of inertia are determined from regression equations based on body height and mass [85]. Using segment lengths determined from body height [87] and segment COG locations determined from regression equations [85], the moment of inertia of the ‘whole body minus the foot (feet)’ system is calculated. Accuracy can be improved by measuring individual body segment lengths. Substep 3. From Eq. (4). the static moment, mgr /3, is estimated as
Algorithm: Step 1. Calculate the second integral of the horizontal acceleration, i(t) = F,(t)/m, using n(t,) = 0 as the arbitrary initial velocity value. Stop integrating when t is large, not less than 30 s. To be consistent start and stop at peak values of COP. The horizontal acceleration must fluctuate about zero. If the mean of Z(t) is not zero, either due to a short period of observation or asymmetric error of the force plate, an accumulating error of the GLP during integration will accrue. Step 2. Estimate i(t,) as a regression coefficient (linear trend) of the time series. Step 3. Determine the time course of the GLP migration using the estimated i(t,) value as the integration constant.
mgrB = T, - I,#
2.3. Third algorithm integration
(7)
Since the product mgr is constant, the moment depends on the angle 8 alone and therefore represents the GLP.
i-(&J.
(GL-3): Zero-point-to-zero-point
Background. This algorithm is based on premises that when F,= 0, the COP and the GLP coincide. This is due to the assumption that at the instant when the
horizontal force, F,. is zero. the kinetic term of the ankle joint torque is zero. A/gorithrn: Step 1. Determine the location of the COP at the instant when the horizontal ground reaction force is zero. .~,,,(r~,)lF, = 0. When using digital computers. F, is almost never exactly zero. A threshold range, + fi, around zero must be used to determine the zero crossing, - rS
3. Experimental methods
Prior to the stabilographic experiments the distance from the ankle joint center (talocrural) to the ground, h,,. was measured. The axis of rotation of this joint runs just distal to the tips of the malleoli [80]. Viewing from medial to lateral. the axis is directed posteriorly (on average 6” as reported by Inman [SO]; 6.8 ~fr.8.1” according to Bogert et al. [81]) and inclined downward (8“ -Inman [80]: 7.0 * 5.4” -~- Bogert et al. [Sl]). Ankle height. Iz,, was determined as the mean height of the medial and lateral malleoli. A Bertec force platform (model 4060s Bertec Inc., Worthington, OH, USA) was used for data collection. In different experiments the subjects were asked either to stand quietly with their eyes open or closed, or to perform intentionally exaggerated body sway. The sway was performed at different frequencies around either
the ankle joints (single-pendulum movement pattern. the ankle strategy [10,74]), or both the hip and ankle joints (double-pendulum movemrpr pattern, the hip strategy [10,74]). The vertical and horizontal i;lntrrior-postcric,r! ground reaction forces, as well as COP. were usccl for the analyses. Data were collected on II -186~(36persona! computer with a 12 bit National Insiruments model AT-M lo-64F-5 data acquisition hozir-d (National instruments Corporation, Dallas. T?i. l’S,4! kit a sam-. pling frequency of 200 Hz for 30 s. Spvclai \otiware was developed using the Lab-View softwitr:: package (N:\tional Instruments Corpor;llion) ,f;lr ci;ll:i ~.~~ilti~tion ,lnd analysis.
4. Results and discussion
Example results of slow intentional ankle sway. t&t intentional hip sway. and quiet standing eyes closed are presented in Fig. 2. Fig. 3 and Fig. 4. respectively. The coefficients of correlation between the estimations from the three different algorithms are grearcr than 0.95 fol both slow ankle sway and quiet standing eyes closed. During the fast hip sway. however, the GL-i is quite different from the GL-2 and GL-3 merhodx. Due to the low frequency
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Time (set)
z .E 80
100
-
50
--
0
Time (set) 0
-50
t-
Time (set)
Fig. 2. Slow ankle sway (frequency of sway was approximately 0.3 Hz). All of the three methods are in relatively good agreement with each other. The GL migrates strictly in phase with the COP and out of phase with the horizontal force. The coefficients of correlation are: F, versus GL-1, r = - 0.88; F, versus GL-2, r = - 0.87; F, versus GL-3, r = - 0.85; GL-1 versus GL-2, r = 0.97; GL-1 versus GL-3, r = 0.96; GL-2 versus GL-3, r = 0.95. All of the correlation coefficients in this figure and Figs. 3 and 4 are for 30-s trials. The data are from the same subject (male, height 162 cm, weight 70 kg; during the experiment the subject wore soft walking shoes).
COG is oriented vertically and is not accelerating horizontally. In general, the acceleration of the COG can be
represented as both radial (centripetal) and tangential accelerations. Since the angular velocity of the COG is
3CG
I 3
Tme (ser
Fig, 3. Fast hip sway (approximately 4.0 Hz). The correlation between GL-2 and GL-3 is I = 0.75. The correlations between COP and OLP range from ( - 0.6, COP versus GL-I, and 0.74, COP versus GL-2). The large horizontal forces influenced the high correlation between F, and GL,-1 (I = 0.99).
small, the centripetal force is negligible. Hence, F, is essentially an account of the tangential acceleration of the COG. Due to the small inclination angle, B, of the COG from vertical, the magnitude of the tangential
acceleration of the COG and its horizontal projection practically coincide. Theoretically, the analysis of GLP travel rather than COP displacement seems attractive, especially in popu-
34
10
Time (set)
Time (see)
19 -z 6 ';
0
Time (set)
r; -10
-20 20 10 z E ?
0
:__i\,j
Time (set)
ti -10 -20 20
-.
10 -z zC-Y
0
Time (set)
i; -10 -20
Fig. 4. Quiet standing eyes closed. The GL-1, GL-2, and GL-3 estimations follow similar paths, r 2 0.96, and are highly correlated with COP (r 2 0.94).
with high frequency of body sway. In these conditions, the COP trajectory does not resemble the trajectory of the GLP and cannot be used for estimating body sway. Center of pressure and GLP have not been used concurrently to study representative groups and have not been compared systematically with either lations
parametric (mean, standard deviation, etc.) or nonparametric methods (spectral power, etc.) methods. Depending on the outcome of these comparisons, the attitudes toward the analysis of the GLP instead of the COP, will be different. If analysis of GLP provides additional information that cannot be gained with more
Fig. 5. Determining zero crossings at different sampling frequencies with different thresholds. The graphs are a one tecond portion of a horizontal force time history during a 30 s quiet standing trial. The black squares represent zero crossings and the horizontal hncs short the different threshold ranges.
traditional stabilographic methods, the suggested techniques may be well received. At this time, however, the real merit of the suggested algorithms remains to be investigated.
5. Nomenclature
Vectors are printed in bold O-XYZ
an absolute system of coordinates with the origin, 0, at the intersection of the supporting surface and the frontal plane passing through the ankle joint center force and couple (torque) at the ankle joint(s) ground reaction force and torque (external force and torque) weight of the foot horizontal and vertical components of the external force horizontal and vertical components of the force acting at the ankle joint(s) the moment of the resultant Force about the origin of coordinates 0 the height of the ankle joint COP location along the X-axis, the distance from the COG of the foot to the Z-axis (moment arm) mass velocity and acceleration along the
X-axis. acceleration aLong the %aXiS
time rate of change of the angular momentum about the irnkle joint center the moment arm of thz gravity force of the system ‘the whole body except the footifeet’ u-irh respect to the ankle joint the distance from the ankle to the system’s center of mass the body inclination; the angle of the longitudinal axis of the body to the vertical :mgular acceleration moment of inertia 1ime the horizontal location t)f the GL, and it’s velocity at / = 0 lrariables of integration horizontal location of COP and second integral of horizontal acceleration
arbitrary initial velocity integration constant and real initial veLocit> constant ‘under condition that’ zero range threshold
Acknowledgements
The authors thank Drs. R.(.‘. Nelson.
X4.1,. L,atash
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D.A. Rosenbaum and B.V. Lazareva for helpful comments on an early draft of the manuscript.
Appendix A. Determining
zero crossing points
With digital signals the horzontal force is rarely exactly zero. To determine instances when F, = 0, it is necessary to use a threshold range around zero and estimate F, = 0 by 6 < F, < 6, where + b is the threshold. The threshold must be chosen considering both sampling frequency and frequency of oscillaion. Improper selection of the zero range threshold can cause true zero values to be missed or non zero values to be included. For example, if the threshold is too large the GLP and COP will be forced to coincide in places when J’, is truly not zero. During swaying tasks, F, clearly passes through zero and an appropriate threshold is easily determined. During quiet standing, though, F, hovers about zero and is rarely greater than + 1 N. Fig. 5 illustrates that it is possible to determine zero crossings during quiet standing by adjusting the threshold to the sampling frequency. At a frequency of 120 Hz and a threshold hold of + 0.2 N, there are many false zero crossings. In some instances, the signal quickly changes from positive to negative (or vice versa) so that F, is less than - 0.05 N at sampling time ti and is greater than 0.5 N at the next sampling ti+ I. As a result, these zero crossing points would not be recognized by the computer. At 30 Hz and a threshold of k 0.2 N, the zero crossings have been reasonably determined. At a threshold of k 0.05 N, however, all zero crossings have been missed. These examples represent extremes, however, it is apparent that by adjusting the zero-crossing threshold to the sampling frequency it is possible to determine zero crossings during quiet standing. References [II Hellebrandt FA. Standing
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