comparison of proximal isovelocity surface area method

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458 JACC Vol. 26, No. 2 August 1995:458-65 Comparison of Proximal Isoveiocity Surface Area Method With Pressure Half-Time and Planimetry in Evaluation of Mitral Stenosis ROBERT D. RIFKIN, MD, FACC, KATHLEEN HARPER, DO, DENNIS TIGHE, MD, FACC Spn'ngfield, Massachusetts Objectives. This study sought to 1) compare the accuracyof the proximal isovelocity surface area (PISA) and Doppler pressure half-time methods and planimetry for echocardiographic estima- tion of mitrol valve area; 2) evaluate the effect of atrial fibrillation on the accuracy of the PISA method; and 3) assess factors used to correct PISA area estimates for leaflet angulation. Background.Despite recognizedlimitations of traditional echo. cardiographic methods for estimating mitral valve area, there has been no systematic comparison with the PISA method in a single cohort. Metl;ods. Area estimates were obtained in patients with mitral steaosis by the Gorlin hydraulic formula, PISA and pressure half-time method in 48 patients and by planimetry in 36. Two different factors were used to correct PISA estimates for leaflet angle (0): 1) plane-angle factor (01180 I0 in degrees]); and 2) solid-angle factor [1 - cos(0/2)1. Resu/ts. After exclusion of patients with significant mitrai regurgitation, the correlation between Goriin and PlSA areas (0.88) was significantly greater (p < 0.04) than that between Coffin and pressure half-time (0.78) or Gorlin and planimetry (0.72). The correlation between Gorlin and PISA area estimates was lower in atrial fibrillation than sinus rhythm (0.69 vs. 0.93), but the standard error of the estimate was only slightly greater (0.24 vs. 0.19 cm2).The average ratio of the solid- to the plane-augle correction factors was approximately equal to previously reported values of the orifice contraction coefficient for tapering stenosis. Conclusions. 1) The accuracy of PlSA area estimates in mitral stenosis is at least comparable to those of planimetry and pressure half.time. 2) Reasonable accuracy of the PISA method is possible in irregular rhythms. 3) A simple leaflet angle correction factor, 01180(Oin degrees), yields the physicalorifice area because it overestimates the vena contracta area by a factor approximately equal to the contraction coefficient for a tapering stenosis. (J Am Coil Cardio11995;26:458-65) Recent studies have demonstrated that current cchocardio- graphic tedmiques for estimating valve area in mitral stenosis have important limitations. In particular, the reliability of the pressure half-time method is reduced by conditions that alter left ventricular compliance, or preload (1-5). Similarly, leaflet calcification and poor parasternal windows impair the accuracy and feasibility of orifice planimetry (6,7). Although mitral pressure gradient is accurately measured by Doppler (8), the gradient depends quadratically on valvular flow and is there- fore also affected by cardiac output and mitral regurgitation. The proximal isovelocity surface area (PISA) method for estimating valve area is a new technique based on the conti- nuity principle (9,10) that may circumvent the limitations of the traditional methods. Therefore, the purpose of the pres~-nt study was 1) to compare the PISA method with planimetry and pressure half-time for estimation of valve area in mitral stenosis using the Goflin hydraulic formula as the reference method; 2) to assess the impact of mitral regurgitation and atrial fibrillation on the accuracy of the PISA method; 3) to From the Department of Medicine,Baystate Medical Center, Tufts Univer- sity School of Medicine, Springfield, Massachusetts. Manuscriptreceived October 21,1994; revised manuscriptreceived March 9, 1995, accepted March 14, 1995. Addres.~ for eorresnondeny~.: Dr. Robert D. Rifkin, CardiologyDivision, BaystateMedical Center, 759 Chestnut Street, Springfield, Massachusetts 01199. 01995 by the American College of Cardiology compare two alternative geometric factors to correct the calculation of proximal isovelocity surface flow for different degrees of leaflet angulation; and 4) to test the hypothesis that the magnitude of the difference in area estimates with these two correction factors is similar to the difference between physical orifice cross-sectional area and vena contracta cross- sectional area. Methods patients. We studied 48 consecutive patients (9 men, 39 women; mean age 68 years, range 44 to 85) with native valve mitral stenosis by two-dimensional echocardiography, in whom valve area could be calculated by the Gorlin hydraulic formula. Five patients had calcific annular mitral valve disease and 43 had rheumatic heart disease. We classified mitral regurgitation severity as follows: 1+ = mild; 2+ = mild-moderate; 3+ = moderate; 4+ = moderate to severe; and 5+ = severe. Equipment. A Hewlett-Packard Sonos 1500 revision 0.1 and 0.4 or Sonos 1000 revision L was used. Images were obtained with a 2.5-MHz transducer. Theory and assumptions of PISA method. Blood flow converging toward an orifice in a flat plate forms isovelocity shells that are hemispheric in shape over a certain range of velocities (Fig. 1). Shell radius R can be measured from the orifice to an aliasing boundary created by setting an appropri- 0735-1097/95/$9.50 0735-1097(95)00173-2

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Page 1: Comparison of proximal isovelocity surface area method

458 JACC Vol. 26, No. 2 August 1995:458-65

Comparison of Proximal Isoveiocity Surface Area Method With Pressure Half-Time and Planimetry in Evaluation of Mitral Stenosis

R O B E R T D. RIFKIN, MD, FACC, KATHLEEN H A R P E R , DO, DENNIS TIGHE, MD, FACC

Spn'ngfield, Massachusetts

Objectives. This study sought to 1) compare the accuracy of the proximal isovelocity surface area (PISA) and Doppler pressure half-time methods and planimetry for echocardiographic estima- tion of mitrol valve area; 2) evaluate the effect of atrial fibrillation on the accuracy of the PISA method; and 3) assess factors used to correct PISA area estimates for leaflet angulation.

Background. Despite recognized limitations of traditional echo. cardiographic methods for estimating mitral valve area, there has been no systematic comparison with the PISA method in a single cohort.

Metl;ods. Area estimates were obtained in patients with mitral steaosis by the Gorlin hydraulic formula, PISA and pressure half-time method in 48 patients and by planimetry in 36. Two different factors were used to correct PISA estimates for leaflet angle (0): 1) plane-angle factor (01180 I0 in degrees]); and 2) solid-angle factor [1 - cos(0/2)1.

Resu/ts. After exclusion of patients with significant mitrai

regurgitation, the correlation between Goriin and PlSA areas (0.88) was significantly greater (p < 0.04) than that between Coffin and pressure half-time (0.78) or Gorlin and planimetry (0.72). The correlation between Gorlin and PISA area estimates was lower in atrial fibrillation than sinus rhythm (0.69 vs. 0.93), but the standard error of the estimate was only slightly greater (0.24 vs. 0.19 cm2). The average ratio of the solid- to the plane-augle correction factors was approximately equal to previously reported values of the orifice contraction coefficient for tapering stenosis.

Conclusions. 1) The accuracy of PlSA area estimates in mitral stenosis is at least comparable to those of planimetry and pressure half.time. 2) Reasonable accuracy of the PISA method is possible in irregular rhythms. 3) A simple leaflet angle correction factor, 01180 (O in degrees), yields the physical orifice area because it overestimates the vena contracta area by a factor approximately equal to the contraction coefficient for a tapering stenosis.

(J Am Coil Cardio11995;26:458-65)

Recent studies have demonstrated that current cchocardio- graphic tedmiques for estimating valve area in mitral stenosis have important limitations. In particular, the reliability of the pressure half-time method is reduced by conditions that alter left ventricular compliance, or preload (1-5). Similarly, leaflet calcification and poor parasternal windows impair the accuracy and feasibility of orifice planimetry (6,7). Although mitral pressure gradient is accurately measured by Doppler (8), the gradient depends quadratically on valvular flow and is there- fore also affected by cardiac output and mitral regurgitation.

The proximal isovelocity surface area (PISA) method for estimating valve area is a new technique based on the conti- nuity principle (9,10) that may circumvent the limitations of the traditional methods. Therefore, the purpose of the pres~-nt study was 1) to compare the PISA method with planimetry and pressure half-time for estimation of valve area in mitral stenosis using the Goflin hydraulic formula as the reference method; 2) to assess the impact of mitral regurgitation and atrial fibrillation on the accuracy of the PISA method; 3) to

From the Department of Medicine, Baystate Medical Center, Tufts Univer- sity School of Medicine, Springfield, Massachusetts.

Manuscript received October 21,1994; revised manuscript received March 9, 1995, accepted March 14, 1995.

Addres.~ for eorresnondeny~.: Dr. Robert D. Rifkin, Cardiology Division, Baystate Medical Center, 759 Chestnut Street, Springfield, Massachusetts 01199.

01995 by the American College of Cardiology

compare two alternative geometric factors to correct the calculation of proximal isovelocity surface flow for different degrees of leaflet angulation; and 4) to test the hypothesis that the magnitude of the difference in area estimates with these two correction factors is similar to the difference between physical orifice cross-sectional area and vena contracta cross- sectional area.

M e t h o d s

patients. We studied 48 consecutive patients (9 men, 39 women; mean age 68 years, range 44 to 85) with native valve mitral stenosis by two-dimensional echocardiography, in whom valve area could be calculated by the Gorlin hydraulic formula. Five patients had calcific annular mitral valve disease and 43 had rheumatic heart disease. We classified mitral regurgitation severity as follows: 1+ = mild; 2+ = mild-moderate; 3+ = moderate; 4+ = moderate to severe; and 5+ = severe.

Equipment. A Hewlett-Packard Sonos 1500 revision 0.1 and 0.4 or Sonos 1000 revision L was used. Images were obtained with a 2.5-MHz transducer.

Theory and assumptions of PISA method. Blood flow converging toward an orifice in a flat plate forms isovelocity shells that are hemispheric in shape over a certain range of velocities (Fig. 1). Shell radius R can be measured from the orifice to an aliasing boundary created by setting an appropri-

0735-1097/95/$9.50 0735-1097(95)00173-2

Page 2: Comparison of proximal isovelocity surface area method

JACC Vol. 26, No. 2 RIFKIN ET AL. 459 August 1995:458-65 MITRAL VALVE AREA BY ECHOCARDIOGRAPHY

Left Ventricle

t

R ~ R r l t Alias

Lett Atrium Figure 1. Schematic of aliasing boundary. R = distance from orifice to boundary; # = angle between domed mittal leaflets. Isovelocity surface area is reduced from that of a hemisphere by leaflet angulation.

ate color flow Nyquist limit (11,12). Streamlines of flow cross this shell perpendicularly. AccoIdingly, the instantaneous flow rate across this boundary is the product of its surface area (21rR 2) and the aliasing velocity at the shell (V,). By continu- ity, this flow equals the instantaneous flow across the orifice, given by the product of orifice area A and peak velocity Vp. Thus, 2~'R 2" V, = A" Vp, and A = 21rR 2" (VnNp).

As a result of leaflet doming in rheumatic mitral stenosis, a correction to these formulas is required because flow crosses only that fraction of the hemispheric isovelocity shell given by the ratio of the solid angle ,'~, subtended by the leaflet funnel, to the solid angle 27r, subtended by a hemisphere. If 0 is the plane angle between the leaflets, tilen I'I/27r = I - cos(O/2), which is hereinafter referred to as the solid-angle correction factor (Appendix 1). Thus, A = (VnNp) • (2~rR2) • [1 - cos(0/ 2)]. A simpler correction factor, 0/180 (0 in degrees), referred to subsequently as the plane-angle correction factor, has also been used (9), resulting in an alternative formula for orifice area: A = (Vp.Np) • (2IrR2) • (0/180 t0 in degrees]).

Calculations. We calculated the PISA valve area for each patient using both the solid- and plane-angle correction factors according to the preceding formulas and by the Gorlin hydrau- lic formula A = (CO/DFP)/(37.6. G1/2), where CO = cardiac output; DFP = diastolic filling period; G = mean pressure gradient; and 37.6 = the Gorlin hydraulic constant for the mitral valve (13). Cardiac output was determined by thermodi- lution.

Comparison of plane- and solid-angle correction factors. In the 30 patients with 0 to 2+ mitral regurgitation, we determined the regression slope of the Gorlin area (y variate) onto the PISA area (x variate) separately for the plane- and solid-angle correction factors. We compared the ratio of these slopes with published values of the orifice contraction coeffi- cient Co, which describes the ratio of the vena contracta cross.sectional area to the physical orifice cross-sectional area for free jets emerging from an orifice into a stationary reservoir (14). To further elucidate the two different correction factors, we graphed 0/180 (0 in degrees) and 1 - cos(0/2) as a function of 0.

Image acquisition. Magnified color flow images of the mitral leaflets and orifice were used to maximize frame rate

and limit measurement error. The apical four-chamber view was used in all patients. An isovelocity boundary was formed by color Doppler baseline shift to an aliasing velocity between 18 and 30 cm/s. Transducer orientation was adjusted in real time to maximize aliasing radius. Images were then captured on digital eine loop for immediate frame by frame analysis. Orifice velocity, pressure half-time and mean gradient were measured by continuous wave Doppler immediately after radius mea- surements.

Image evaluation. Early diastole was examined frame by frame to find the aliasing boundary with maximal radius corresponding to E wave continuous wave peak velocity. Repeated capture and measurement of zones was performed until at least five were obtained with <15% variation in radius. Zones with irregular or fragmented borders, sig'aificant asym- metry or inability to identify orifice were rejected. The orifice was located by 1) point of maximal narrowing of color flow jet in the region of leaflet tips; and 2) leaflet tip position on the cine loop image with the color flow m~p turned off. Leaflet angle was evaluated using cine loop images with the color map both off and on (Fig. 2). Measurement of aliasing radii and leaflet angles was performed by an observer without knowl- edge of the planimetric, pressure half-time or hemodynamic estimates of valve area.

In atrial fibrillation, because of significant variation in E wave velocity and maximal aliasing radius associated with RR interval variations, we collected the maximal aliasing radii and continuous wave Doppler peak E wave velocities for a series of 6 to 8 beats with the longest RR intervals. The two series were arranged in order of descending values. E wave velocities and aliasing radii were matched according to this ordering, and valve area was calculated separately for each matched pair. These were averaged to obtain a final area estimate.

Statistical analysis. Linear regression and correlation (15) were performed between each echocardiographie method and the Gorlin areas. Because the Gorlin area was common to each correlation calculation, the correlation coefficients were not independent. Accordingly, we tested for significant differences using the method of Olkin and Finn (16) by which, for a trivariate normal distribution, the variance of the difference between any pair of the three nonindependeut correlation coefficients r13, r~ and rlz is given by

var(rt3 - rz3) = var(r13) + var(rz~) - 2 • cov(r13,rz~),

where

var(r,j) = (I - rii2)Z/n;

and

cov( r13 , rz0 =

[(2 • rn - r13 " r~) • (1 - r132 - r~ 2 - vn:) + rn3]/(2n).

Thus, z = (r13 - r2a)/[var(rl3 - r23)11/2 is a standard normal variate (mean 0, variance 1) and can be used for testing the significance of r t3 - r23.

Differences in standard errors of the estimate were tested by the F ratio for variances with n - 2 degrees of freedom for

Page 3: Comparison of proximal isovelocity surface area method

460 RIFKIN ET AL. JACC Vol. 26, No. 2 MITRAL VALVE AREA BY ECHOCARDIOGRAPHY August 1995:458-65

Figure 2. Zoom-magnified images of the flow convergence zone. Top, Color flow map of the aliasing boundary. Bottom, Same frame with pixel coloration turned off to optimally display leaflets. The orifice location and leaflet angle were determined from these two displays.

each variate (15). Interpretation of regression slopes was based on our recent analysis of regression and correlation in medical method comparison studies (17) (Appendix 2). The analysis of Altman and Bland (18) was used to supplement the conven- tional methods for assessment of error and bias.

R e s u l t s

Area by PlSA compared with pressure half.time, planim- etry and mitral gradient. Planimetry was obtained for 36 (75%) of 48 patients. Pressure h~lf-time and PISA methods were obtained for all patients (Fig. 3).

When all 48 patients were included for analysis, and PISA areas were computed by the plane-angle correction factt, r (Table 1), the correlation and regression statistics were similar among the three methods and showed only a modest agree- ment with Gorlin valve areas. However, when patients with significant mitral regurgitation were excluded from analysis, agreement between the PISA and Gorlin areas improved markedly. In particular, in the subgroup with 0 to 2+ mitral

5

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>=

<C

o g w

5

rr"

,9 Z - i

O (9 >- CO <c

2.5

1.5

0.5

0

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."5

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5 2 n-

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Q O 0 Ill • •

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AREA BY PISA USING PLANE ANGLE (sq cm)

• O-2+MR, n = 3 0 /

• 3 + MR, n = I O o / o ~ /

o 4-5+MR, n = 8 o ~ e ~

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AREA BY PRESSURE HALF TiME (sq c m )

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o 4-5+MR, n = 6 o ~

• • • •

Q Q I 0 •

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0.5 1 1.5 2 2,5

AREA BY PLANIMETRY (sq c m )

Figure 3. Scatterpiots of the Gorlin valve area versus echocardio- graphic estimates of area using (a) proximal isovelocity surface area ~PISA) method with plane-angle correction factor; (b) pressure half- time method; (e) planimetry. Light lines = lines of identity; bold lines = least-squares regression lines from Table 1. MR = mitral regurgitation.

regurgitation (Table 2), the correlation between PISA and Gorlin areas increased from 0.78 to 0.85, and the standard error of the estimate decreased from 0.33 to 0.23 cm 2. By contrast, agreement between the other two methods and

Page 4: Comparison of proximal isovelocity surface area method

JACC Vol. 26, No. 2 RIFKIN ET AL. 461 August 1995:458-6~ MITRAL VALVE AREA BY ECHOCARDIOGRAPHY

Table 1. Regression of Gorlin Valve Area Onto Area by Proximal isovelocity Surface Area, Pressure Half-Time and Planimetry

Methods Compared

x y No. of Corr Coeff SEE Variate Variate Pts (r) (area fern2]) Intercept Slope

PISA, tflane angle Gorlin formula 48 0.78 0.33 0.27 0.72 Pressure half-time Gorlin formula 48 0.73 0.36 0.02 0.73 Planimetry Gorlin formula 36 0.75 0.33 0.18 0.71

Con" Coeff = correlation coetticient; PISA = proxima! isoveloeity surface area; Pts = patientg.

Gorlin areas improved to a much lesser extent. Thus, in 23 patients with 0 to 2+ mitral regurgitation in whom planimetry was obtained, PISA area estimates showed a significantly higher (p < 0.05) correlation with Gorlin areas (r = 0.85, not shown in tables) than did the planimetric estimates (r = 0.72). Similarly, in 40 patients with 0 to 3+ mitral regurgitation (not shown in tables), the correlation between PISA and Gorlin estimates (r = 0.88) was significantly higher (p < 0.04) than the correlation between pressure half-time and Gorlin estimates (r = 0.78).

Although the correlation between PISA and Gorlin areas was good, and the standard error of the estimate was small in the 30 patients with 0 to 2+ mitral regurgitation, the regression slope (0.84) was substantially < 1. However, rather than imply- ing systematic bias, a slope <1 is the expected finding when the reference method (Gorlin valve area) is subject to measure- ment error with respect to true valve areas (Appendix 2). In fact, the regression slope was slightly less than the correlation coefficient (0.85) (Table 2), which is consistent with the absence of systematic bias in the PISA method for estimation of true valve area when the reference test is superior to the new test (Appendix 2). Absence of bias is further supported by analysis of our data according to ;he method of Altman and Bland (18) (Fig. 4). The mean difference between the Gorlin and PISA areas was only 0.01 cm 2, and the regression slope of the difference in area onto the mean value of area was only -0.011.

Mitral inflow gradient and stenosis severity. Both mean and peak mitral inflow gradients correlated poorly with the Godin valve area. f'or 0 to 2+ mitral regurgitation (n = 30), the correlation coefficient and standard error of the estimate for mean gradient (x variate) versus Gorlin area (y variate) were r = 0.60 and SEE 0.35 cm 2, whereas for 3 to 5+ mitral

regurgitation (n = 18) these values were r = 0.43 and SEE 0.59 cm 2. For peak gradient versus Gorlin area in 0 to 2+ mitral regurgitation (n = 30), the correlation coefficient and standard error of the estimate were r = 0.55 and SEE 0.36 cm 2, whereas for 3 to 5 + mitral regurgitation, these values were r = 0.41 and SEE 0.60 cm 2. Thus, correlation between gradient and Gorlin valve area improved in patients with less mitral regurgitation but remained poor.

PISA accuracy in sinus rhythm versus atrial fibrillation. For the study group as a whole, the correlation between the Gorlin and PISA methods was very similar for patients with sinus rhythm and atrial fibrillation; however, for patients with 0 to 2+ mitral regurgitation and atrial fibrillation, the corre- lation was much lower (Table 3, Fig. 5). Nevertheless, the standard error of the estimate was enly slightly higher for patients with 0 to 2+ mitral regu-gitation and atrial fibrillation (0.24 cm 2) than for patients with 0 to 2+ mitral regurgitation and sinus rhythm (0.19 cm2). Thus, the lower correlation associated with atrial fibrillation is partly due to a smaller spread of valve areas in thi~ ,3roup. In particular, the standard deviation of Gorlin valve areas was 0.49 cm 2 for patients with sinus rhythm and 0 to 2+ mitral regurgitation compared with 0.40 cm z for those with 0 to 2+ mitral regurgitation and atrial fibriUation. If adjusted for this difference (Appendix 3), the correlation coefficient for atrial fibrillation would be 0.87 versus 0.93 for sinus rhythm.

Plane-angle versus solid-angle correction factor. For any leaflet angle 0, the difference in area predicted by the plane- and solid-angle correction factors is directly related to the difference between 0/180 (0 in degrees) and 1 - cos(0/2) (Fig. 6). The solid-angle factor is always smaller, but for 0 between 150 ° and 180 °, seen in 8% of our patients, the difference is <12%. For 0 from 111 ° to 150 °, seen in 83% of our patients,

Table 2. Comparison of Methods for Patients With 0 to 2+ Mitral Regurgitation

Methods Compared

x y No. of Corr Coeff SEE Variate Varia~e Pts (r) (area fern"l)

PISA, plane angle Gorlin formula 30 0.85 0.23 Pressure half-time Gorlin formula 30 0.75 0.29 Planimetw Gorlin formula 23 0.72 0.32 PISA, solid angle Gorlin formula 30 0.84 0.24

Abbreviations as in Table 1.

Intercept Slope

0.18 0.84 0.12 0.64 0.30 0.60 0.19 1.05

Page 5: Comparison of proximal isovelocity surface area method

462 RIFKIN El" AL. JACC Vol. 26, No. 2 MITRAL VALVE AREA BY ECHOCARDIOGRAPHY August 1995:458-65

0.8

uJ 0.6 ~c <C < r~ 0.4

J

< uu 0.2 t r

Z .~ 0 t r O o

-0.2 II

uJ t~ -0.4 Z I , L l

r r LLI ~. -0.6

-0.8

0 - 2 + MR.n = 30 MEAN DIFFERENCE = .01 S.D. DIFFERENCE = .24

CORRELATION COEFF = .02 SLOPE =-.011. INTERCEPT = .024

STANDARD ERROR = .24

. . . . . . . . . . . . . . e ~ u . . . . •

- • •

• • •

e

0.5 1 1.5 2

M E A N = ( G O R L I N A R E A + P I S A A R E A ) / 2

I 2,5

Figure 4. Analysis of Altman and Bland (18) for proximal isoveloeity surface area (PISA) estimates in patients with 0 to 2+ mitral regurgitation (MR) using the plane-angle correction factor. The slope and intercept (inset) for regression of the differ- ence (y values) onto the mean (x values) of Gorlin and PISA areas is essentially zero, indicating ab- sence of bias in the PISA method. COEFF = coefficient.

the solid-angle estimate is 12% to 30% smaller and, for 0 < 110 ° , seen in 9% of our patients, the solid-angle factor is over 30% less. The mean (__.SD) leaflet angle in our 48 patients was 128 ° +_ 15 °. For this average angle, the solid-angle factor is 79% of the plane-angle factor. Thus, averaged over all 48 patients, solid-angle correction resulted in valve areas that were 79% of that using the plane-angle factor.

In the 30 patients with 0 to 2+ mitral regurgitation, the correlation coefficient was 0.84, standard error of the estimate was 0.24, and slope was 1.05 for regression of the Gorlin areas onto PISA areas using solid-angle correction. Thus, the corre- lation coefficient and standard error of the estimate with solid-angle correction were nearly identical to those using plane-angle correction (Table 2), but the regression slope was 125% greater. Accordingly, if each area based on the plane- angle correction factor was multiplied by 0.8, or, conversely, if each solid-angle area was multiplied by 1.25, the plane- and solid-angle regressions would be nearly identical (because the

Table 3. Influence of Rhythm on Estimation of Gorlin Valve Area (y variate) by Proximal Isovelocity Surface Area Method (x variate): Sinus Rhythm Versus Atrial Fibrillation

COlT No. of Coeff SEE

Group (x variate) Pts (r) (area [emZ]) Intercept Slope

Sinus rhythm 22 0.75 0,43 0.28 0.71 Atrial fibrillation 26 0.79 0.24 0.26 0.73 Sinus rhythm and 11 0.93 0.19 0.01 0,99

0 to 2+ MR

Atrial fibrillation 17 0.69 0.24 0.41 0.60 and 0 to 2+ MR

MR = mitral regurgitation; other abbreviations as in Table 1.

correlation and standard error of the estimate are not changed by multiplication of all data by the same factor).

D i s c u s s i o n

Accuracy and feasibility of PISA compared with pressure half-time and planimetry. In the present study, the PISA method correlated better with calculation of mitral valve area by the Gorlin equation than did Doppler pressure half-time or planimetry. Notably, ag!,:cment between the latter two meth- ods and Godin valve area in our patients was lower than previously reported (6,19,20). Planimetry was feasible in 75%

Figure 5. Scatterplot for patients with 0 to 2+ mitral regurgitation (MR) in normal sinus rhythm (NSR) and atrial fibrillation (A FIB). There is greater variation in patients with atrial fibrillation. PISA = proximal isovelocity surface area.

2.b

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Page 6: Comparison of proximal isovelocity surface area method

.I'ACC Vol. 26, No. 2 RIFKIN El" AL 463 August 1995:458-65 r' 5rltRAL ~¢ALVE AREA B'¢ ECHOCARDIOGRAPHY

1.2

1.0 ,=,=,

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17 SOLID ANGLE FACTOR 1-cosla~lglel2~

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0 30 60 90 120 150 180

LEAFLET ANGLE Figure 6. Comparison of plane-angle and solid-angle correction fac- tors for leaflet angulatie,~. The solid-angle factor is always smaller and leads to smaller area estimates.

(36 of 48) of patients, also a somewhat lower figure than in earlier reports (6,19,20). However, the mean age of our patients was 68 years, which is considerably older than that in previous studies. It i~as i'eceuLly been recognized (21) that the pressure half-time method is less accurate in the elderly. This finding is consistent with theoretic (22) and clinical studies (1-5) showing that ventricular compliance declines with age. Similarly, greater valvular thickening and calcification in the elderly would be expected to reduce the feasibility and accu- racy of planimetry. Of note, in our study group there were no false positive valve areas <1 cm 2 by the pressure half-time method. Thus, evidence of significant narrowing by this tech- nique may be reliable, even in the elderly.

A purported advantage of pressure half-time and planim- etry methods over the mean gradient in assessing stenosis severity is their independence of valvular flow and therefore of cardiac output and severity of mitral regurgitation. The PISA method, in principle, compensates for variations in transvalvu- lar flow. Our data support this and suggest further that with significant mitral regurgitation, PISA area estimates may be more accurate than the Gorlin formula, which tends to under- estimate area in these patients.

Accuracy of flow convergence method in atrial fibrillation. With current technology, orifice velocity and PISA radius must be measured in different beats. Peak continuous wave Doppler E wave velocity, and the maximal early diastolic color flow aliasing radius provide suitable corresponding moments for measurement. Nevertheless, due to limited color Doppler frame rates, the maximal aliasing radius can be missed, causing underestimation of aliasing radius. Because PISA area de- pends on radius squared, both area underestimation and beat-to-beat variations in area are magnified. This effect can be minimized by measuring the radius in multiple beats until a consistent set of values is obtained. However, in atrial fibrilla- tion, variations are even greater due to changing RR intervals,

resulting in the ~educed accuracy that we encountered, how- ever, we fou~,d that if sufficient time is allo~.'ed, only a modest decrease in accuracy occurs with irregular rhythm. Our data suggest that the accuracy of the Pi~iA method in atrial fibril- lation is as ~ood as, or better 'than, pressure half-tirae and planimetry, which may also be less aceuxate in this .~,ituation.

Plane-angle versus so!id-angle correction factor. If leaflet angulation is axially symmetric ~,nd the PISA surface is spheric, the solid-angle correction faetoz expresses the correct fraction of a hemispheric surface available for flow. By contrast, the plane-angle factor corrects for nan'owing along only one geometric dimension. Yet, in our data, solid-angle correction underestimated the Gorlin valve area, whereas both our esti- mates, and those in a previous report ,[9), which also used the plane-angle correction factor, agreed well with the Go~'lin area.

Our resuhs suggest that this finding; relates to the difference between physical orifice area and vena contracta jet area (14), which is well known to be s~,ailer than the physical orifice. The PISA method, based on continuity, measures the vena con- tracta area. Cohen and Gorlin (13) determined the constant in the Gorlin formula by comparison of hemodynamic data with anatomic specimens of stenotic raitral valves; therefore, the Gorlin formula gives the physical orifice area. The ratio of vena contracta alea to physical orifice area is defined :.~s the coefficient of contraction: Cc = ,~ct/m~ritice. For orifices in flat plates, C~ is ~0.6 (23). Segal et al. (24) measured C~ in two tapering orifices with 56% and 79% reductions in area relative ;.o the inlet, representing mild and severe mitral stenosis, respectively, and found C¢ to be between 0.75 to 0.85 over a wide range of flows.

In the 30 patients with 0 to 2+ mitral ~egurgitation, we found that if each PISA area ,~sing solid-angle correction was increased by a factor of 1.25, or, equivalendy, if plane-angle areas were reduced by a fitctor of 0.8 (1/1.25 = 0.8), the regression statistics for plane- and solid-angle correction be- come nearly identical. The factor (0.8) is within the range of values of C c reported by Segal et al. (24) for tapering stenoses, suggesting that PISA areas usin~; plane-angle correction agree with Gorlin areas because, for most angles encountered in mitral stenosis, plane-angle PISA overestimates vena contracta area by approximately the diffelence between physical orifice and vena contracta areas. Similarly, it also explains the agree- ment between PISA areas and planimetry in earlier studies that u~ed the plane-angle colxection tactor (9,12). However, for the narrowest leaflet angles, for which there is a very large disparity between the two correction factons, the existence of some ~.;ym- metry of the leaflet funnel may also be required to explain the accuracy of the plane angle correction factor.

Previous work. Rodriguez et ai. (9) found a correlation coefficient of 0.86, slope 0.89 and standard error of the estimate of 0.24 cm 2 for regression of PISA areas (3, variate) onto Gorlin ~reas (x variate) in 25 patients. When the x and y variates are exchanged to correspond to ours (Appendix 3), the slope, standard error of the estimate of Gorlin areas and correlation coefficient become 0.83, 0.23 cmz and 0.86, respec- tively, which agrees well with our values. Notably, only 2 of

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4 6 4 RIFlrdN El" AL. JACC Vol. 26, No. 2 MITRAL VALVE A R E A BY E C H O C A R D I O G R A P H Y August 1995:458-65

their 25 patients were in atrial fibrillation. Hence, their results reflect primarily patients in regular rhythm. Additionally, 13 of their patients had mitral regurgitation of unspecified severity. These differences impede comparison with our data. By eval- uating rhythm and degree of mitral regurgitation separately, we were better able to assess the accuracy of the PISA method.

Deng et al. (12) recently reported that an aliasing limit of 21 cm/s was optimal for the PISA method in mitral stenosis, but used pressure half-time and planimetry as the reference methods rather than Gorlin valve areas. The aliasing limits we used were between 18 and 30 era/s, which would yield no more than a 12% error in area estimates based on the results of Deng et al. (12).

Study limitations, The size of the ~tudy group was limited by the small number of patients with mitral stenosis who underwent hemodynamic study. Thus, statistically significat~t differences in regression variables between the Gorlin and the three echocardiographic methods tested were found only in the group with moderate or tess mitral regurgitation.

Our study group was biased in that it included primarily elderly hospital inpatients. The mean age of the patients studied using planimet .ry by Deng et al. (12) and Wann et al. (25) was 39 and 43 years, respectively, compared with 68 years in our study. Extrapolation of our observations on the relative accuracy and feasibility of PISA versus traditional echocardio- graphic methods to other age groups may be invalid.

Clinical implications a n d c o n c l u s i o n s . Despite possible bias due to the age of our patients, the PISA method appears

- ~.o provide valve area estimates that are at least comparable in accuracy and possibly superior to traditional echocardio- graphic methods in certain groups, such as the elderly and patients in unstable condition or those with concomitant heart disease. In patients w:ah significant mitral regurgitation, the PISA method may yield more accurate valve area estimates than catheterization. Reasonable, albeit reduced, accuracy of the PISA method is maintained in atrial fibrillation. Correction of hemispheric flow for leaflet angulation can be accomplished by using a simple factor, 0/180 (0 in degrees).

The PlSA method is technically demanding and more time-consuming than the pressure half-time approach. Many aspects of the PISA method require meticulous technique, and a significant learning curve exists for the use of this approach. As with the other methods, clinically important deviations from the Gorlin area can occur, and the results of the PISA method still need to be interpreted in the context of other echocardiographic and clinical data.

Refinements of equipment may facilitate use of the PISA method. Nevertheless, with practice and careful imaging, PISA can yield useful mitral area estimates at the present time and should now be included in the repertoire of techniques avail- able in the echocardiographic laboratory.

We acknowledge the technical assistance of Marianne Kalmbaeh, BS, RDCS, Janet D'Amoars, RDCS, Barbara Popowski, BS, RDCS and Pat Gilmette, RDCS.

Appendix 1

Derivation of Solid-Angle Correction Factor The mitral leaflet funnel is represented by a cone with its apex at the origin, its apex angle 0 representing the plane angle between the leaflets, its long axis coincident with the positive x-axis and its circular base of radius Rb defined by intersection of the cone with a sphere of radius 1~ centered at the origin. Let dl = R~. dr, be a differential element of are length along the sphere's st, dace, where a is the angle between the x-axis and the sphere's surface in the first quadrant of the x,y plane. Let dS = 2~rRb dl be the area of an infinitesimal ringlike element of the spheric surface subtended by the cone. Then, Rb = Rs sin(c 0, and dS = R~ sin(a)21rR~ da. The surface area of the section of the sphere subtended by the cone, representing the PISA surface, can be found by integrating dS over a from 0 to 0/2:

f~ [21rR~ 2 sin(a)] da = - 21r1~ 2 • [cos(0/2) - cos(0)] 0/2

=0 = 2'lrRs 2 " (1 - cos 0/2).

Because the surface area of the hemisphere is 2~r~ 2, the fraction of its surface area subtended by the cone is 21r~ 2" (1 - cos 0/2)/27rR~ 2 = 1 - cos 0/2.

Appendix 2

Effect of Imperfect Refe~?nce Test on Observed Slope and Correlation Coejfici:nt in Linear Regression It is commonly assumed that to prove a new test is free of bias (systematic underestimation or overestimation or both), the observed slope of regression of reference test value~ (y variate) on to new test values (x variate) should be close to 1. However, when the reference test itself is subject to random measurement error with respect to true values, this is not valid. We recently showed (17) that, for this case, the observed correlation coefficient Pttt 2 for the regression of the reference test (~tl) onto a new test (--t2) is given by the following expression:

0tlt 2 = 01 " 02 q" 0EIE 2 " (1 -- 0t2) 1/2 " (1 - 022) 1/2,

where 01 and 02 are the correlation with true values for t~ and t2,

respectively, and P~zP-~ is tt~e correlation between the test errors. We also showed that the slope (b.ttz) and intercept (atlt2) are

bttt2 -- (B2]BI) • 012 + (o'G/o~2)2

and

atlt2 = t t - t2 "b t l t 2,

where B1 and B 2 a r e the slopes of the regression of the true values onto the reference test and the new test, respectively and tl and t2 are mean values. For comparison of valve areas by echocardiographic and hydrodynamic methods, errors are likely to be uncorrelated (~tE2 = 0) because these methods are physiologically dtfferent. Thus, Pt,t2 = Pt" 02 and bht 2 = (B2/BI) • pl 2. Because 02 = Ptl,~/Pl, the value of 02 could be found from the observed value of Ptlt 2 if the value of pt is known.

It is also often assumed that Pt|t 2 at~d bqt ~ are surrogates fox 02 and B2; that is, Pitt2 ~" t'2 and bt,t2 ~ B2. Howcvex, the preceding equati, ms

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JACC Vol. 26, No. 2 RIFKIN ET AL. 465 August 1995:458-65 MITRAL VA1,VE AREA BY ECHOCARDIOGRAPHY

show this is a valid assumption only if p~ ~ I and B~ ~ B 2 or if BI/B 2 = pl 2, both unlikely conditions. In fact, because pt < 1, it follows that Pt,t2 := Pt" Pz < P2 in all cases and btjt2 < B 2 in almost all cases. These effects have been recognized previously (26). Thus, finding a slope <1 (bt,t2 < 1) is the expected result when the new test is unbiased. Moreover, because brat2 = Pitt2" 0rtt/trt2) (Appendix 3), the slope will be less than the correlation coefficient (brat2 < Pt~t2) whenever the refer- ence test is better than the new test 0rt~ < crt2 ) and B~ ~- B2. If B~ B2, and both tests are of equal diagnostic accuracy 0rt~ ~ trt:), then the slope will be approximately equal to the correlation coefficient (brat2

Appendix 3

Slope and Standard Error of the Estimate for Inverse Regression For n samples from a bivariate normal population,

and

SEF_~ 2 = (n - 1) • (I - rrx 2) • cry2/(n - 2), [2]

where Byx, ry~ and SEE~ are the known slope, correlation coefficient and standard error of the estimate, rcspcctivcly, for regression of y onto x, and cry and o'~ are unknown sample standard deviations.

For regression of x onto y values, r,~ = rr~. Solve equation 2 for ~ry, and substitute it into equation I to find ~r r Use this value of ~r~ in equation 2 for the new #y to obtain the new SEEdy of the invcrse regression, and calculate (crJcry) • r~y as in equation I to obtain the new value for slope (B~y).

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