Ph. Vandervoort et al., COMPARISON OF INTRAVENOUS ADENOSINE TO INTRACORONARY PAPAVERINE FOR CALCULATION OF PRESSURE-DERIVED FRACTIONAL FLOW RESERVE, Catheterization and cardiovascular diagnosis, 39(2), 1996, pp. 120-125
For calculation of fractional flow reserve (FFR), simultaneous registr
ation of both aortic pressure (P-a) and transstenotic distal coronary
pressure (P-d) is necessary at steady-state maximum coronary hyperemia
. The aim of the present study was to compare the maximum transstenoti
c gradient (Delta Pmax) and pressure-derived myocardial fractional flo
w reserve (FFR(myo)), observed during intravenous adenosine infusion,
to Delta Pmax and FFR(myo) induced by intracoronary papaverine, which
is considered to be the gold standard for induction of coronary hypere
mia, but acts too short for steady-state hyperemic pressure recordings
and is associated with QT-prolongation. In 24 patients with coronary
stenoses of various degrees, P-a and P-d were measured simultaneously
by the diagnostic catheter and a high fidelity 0.018 '' fiberoptic pre
ssure monitoring guide wire, respectively. Excellent steady-state phas
ic intracoronary pressure recordings were obtained in all patients wit
hin 1 min after start of intravenous adenosine infusion at a rate of 1
40 mu g/kg/min, and compared to Delta Pmax obtained 30 sec after intra
coronary administration of papaverine (12 mg LCA, 10 mg RCA). Delta Pm
ax was 24 +/- 15 mmHg during adenosine infusion and 24 +/- 15 mmHg aft
er papaverine administration. Myocardial fractional flow reserve, calc
ulated from these pressure recordings, was 0.75 +/- 0.16 and 0.75 +/-
0.15, respectively, with an individual difference of 0.02 +/- 0.01 bet
ween both values (r = 0.99). No important side effects by intravenous
infusion of adenosine were observed. Thus intravenous adenosine infusi
on at a rate of 140 mu g/kg/min is an excellent and safe alternative f
or induction of steady-state maximum coronary hyperemia and therefore
is an ideal vasodilator for determination of fractional flow reserve b
ased upon pressure recordings. (C) 1996 Wiley-Liss, Inc.