A COMPARISON OF VALVE RESISTANCE, THE CONTINUITY EQUATION, AND THE GORLIN FORMULA AGAINST DIRECTLY OBSERVED ORIFICE AREA IN BIOPROSTHETIC VALVES IN THE MITRAL POSITION - AN IN-VITRO STUDY
Jb. Chambers et al., A COMPARISON OF VALVE RESISTANCE, THE CONTINUITY EQUATION, AND THE GORLIN FORMULA AGAINST DIRECTLY OBSERVED ORIFICE AREA IN BIOPROSTHETIC VALVES IN THE MITRAL POSITION - AN IN-VITRO STUDY, Journal of heart valve disease, 5(2), 1996, pp. 136-143
Background and aims of the study: There is no consensus over how to de
scribe forward flow through valves in the mitral position. There are t
hree main candidate hydraulic formulae; resistance, the Gorlin formula
and the continuity equation, However, virtually no work has been perf
ormed to validate resistance and the continuity equation for valves in
the mitral position. The aim of this study, therefore, was to compare
the three formulae against an independent standard provided by direct
ly observed orifice areas. Materials and methods: Five bioprosthetic v
alves with orifice areas between 0.14 cm(2) and 2.33 cm(2) were studie
d in a pulse simulator at up to 20 different stroke volume/rate combin
ations using quasi-physiologic flow curves. Orifice areas were measure
d using a video camera, pressure difference using strain gauge transdu
cers and Doppler signals using a 1.9 MHz Pedoff probe with a Vingmed S
D50 system. Results: The Gorlin ratio (flow/root mean Delta P) had a d
irect curvilinear relationship with the orifice area (log(y) = 0.31 0.36x; r = 0.94, SEE 0.08 cm(2), p < 0.0001). Resistance (mean Delta P
/flow) had an indirect curvilinear relationship (log(y) = 0.19 - 0.55x
, r = -0.93, SEE 0.13 cm(2), p < 0.0001). The continuity equation was
directly related to observed orifice area although with high scatter (
y = 1.13 + 0.79x; r = 0.90, SEE 0.23 cm(2), p < 0.0001). Although both
the Gorlin ratio and resistance changed with flow, there was also a t
endency for observed orifice areas to increase with flow. Empirical ef
fective orifice areas calculated using the regression equations closel
y resembled observed orifice areas and agreement was reasonable, with
95% limits of -0.33 cm(2) to +0.33 cm(2) (Gorlin), -0.41 cm(2) to +0.4
2 cm(2) (resistance) and -0.40 cm(2) to +0.48 cm(2) (continuity). Conc
lusion: In conclusion, no single formula adequately predicted all obse
rved orifice areas although a resistance and the Gorlin formula gave u
seful predictions after empirical correction.