Abstract
In 1887, the first recording of electrical activity of the human heart was done using Waller’s capillary meter. The recorded signal included four waves called A, B, C, and D. Einthoven mathematically modified this signal to correct the inertia associated with the movement of the mercury column in the capillary electrometer. To avoid confusion with Waller’s recording, Einthoven named the five identified deflections P, Q, R, S, and T having used the O point as the origin of the time scale (by mathematical convention O is used for the origin of the Cartesian coordinates). The interval QT was defined as the interval between the beginning of the QRS complex and the end of the T wave. The ventricular repolarization process of the heart begins in the early-activated myocardial cells while the rest of the ventricle is still depolarizing. This is why the entire duration of the ventricular repolarization is commonly associated with a measure including the QRS complex. It is also during the late 19th century that new discovery, including the electrical triggering of contraction during late refractory period, would open an entire field of quantitative electrocardiology focusing on a better understanding of the cardiac repolarization.
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Couderc, JP., Zareba, W. (2005). Assessment of Ventricular Repolarization From Body-Surface ECGs in Humans. In: Morganroth, J., Gussak, I. (eds) Cardiac Safety of Noncardiac Drugs. Humana Press. https://doi.org/10.1007/978-1-59259-884-7_6
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