U. Leder et al., Temporal properties of high frequency Intra-QRS signals in myocardial infarction and healthy hearts, BIOMED TECH, 45(9), 2000, pp. 243-247
The prevalence of late potentials after myocardial infarction depends on th
e site of the infarction. This may be caused by the different activation on
sets of the anterior and inferior myocardial segments. Therefore, in anteri
or infarcts the high frequency signals may be concealed within the QRS wher
eas in the inferior infarcts they last beyond the end of the QRS. We compar
ed the timing and the spatial patterns of high frequency intra-QRS signals
(IQSs) in the different infarction sites.
We investigated 14 patients with anterior infarcts, 17 patients with inferi
or infarcts, and 10 healthy subjects. 31-lead magnetocardiograms were recor
ded in left precordial position and averaged. The QRS signals were smoothed
with a Savitzky-Golay filter. The smoothed QRS signals were subtracted fro
m the measured ones. The difference of the signals (frequency band of about
60-200 Hz) representing the high frequency components was quantified. The
percentage of the high frequency signals was calculated for the entire QRS,
for the first and for the second half, respectively.
We found that in patients with anterior infarcts the high frequency compone
nts predominantly appeared in the first half of the QRS whereas in inferior
infarcts these components predominantly appeared in the second half of the
QRS. The different infarction sites were associated with different spatial
patterns of the high frequency signals on the body surface. In healthy sub
jects there was not such a preferential association of time intervals and h
igh frequency signals.
Late potentials are the special case of high frequency signals appearing in
the terminal QRS. It is the general property of the myocardium to generate
high frequency signals associated with the depolarization of infarcted tis
sue. The timing of such signals and the spatial distribution patterns on th
e body surface may help to identify the location of the sources.