Sodium feedback and two brakes
Put the three gating equations together with the membrane equation and you have four coupled ordinary differential equations. A small depolarisation lets the fast sodium activation catch up, sodium current flows in, and the voltage rises faster. Nothing stops this step, and the voltage heads for the sodium reversal potential.
The brakes come from two slower processes. The sodium inactivation variable shuts the sodium channels within about a millisecond, while the potassium activation opens the potassium channels. The voltage falls, overshoots rest, stays for a while about 11 mV below it, and slowly returns.
Hodgkin and Huxley integrated these equations step by step with Hartree’s method (p. 523 of the paper), with steps of 0.02 ms on the rising phase. We integrate with a fourth-order Runge–Kutta scheme; halving the step changes the peak by less than .
Source: A. L. Hodgkin and A. F. Huxley · W. Gerstner
The threshold lies between 6 and 7 nC/cm²
Hodgkin and Huxley computed a series of initial depolarisations at 6 °C: 6 mV gave no spike and 7 mV did (Figs. 12 and 21 of the paper). Bisection in our model at 6.3 °C puts the threshold at ; a second integrator, written independently in the paper’s own signs, gives 6.504.
Above threshold, a larger shock hardly changes the peak. Table 4 lists a 102.1 mV peak for a 7 mV start, 105.4 mV for 15 mV and 108.5 mV for 90 mV. The starts differ by more than ten times and the peaks by 6%. That is what all or none means.
The threshold is not a fixed voltage. Right after a spike most sodium channels are inactivated and the potassium channels are still open, so the same shock again gives no spike; this is the refractory period (Fig. 20). Conversely, hold the membrane 30 mV below rest and release it suddenly: part of the sodium inactivation has been removed and the potassium channels are shut, so the membrane fires on its own. This is anode break (Fig. 22).
Source: A. L. Hodgkin and A. F. Huxley · W. Gerstner
Worked example: one 15 nC/cm² shock
Problem. At 6.3 °C a resting membrane receives an instantaneous shock of 15 nC/cm². Find the peak, the maximum rate of rise and the extra sodium that enters and potassium that leaves, and compare them with Tables 4 and 5 of 1952. How much sodium would it take just to charge the capacitor to the peak, and how does that compare with the sodium that actually enters?
Model. Integrate Eq. (26) from . As in the paper, integrate the movements up to the third return to the resting level after the peak, then subtract the flux that would have flowed at rest over the same time. That subtraction is our inference from the numbers; the paper does not say so.
Numbers. The peak is against 105.4 printed in Table 4; the maximum rate of rise is against 311; the peak conductance is against 37.0. The extra sodium entry is against 14.46 in Table 5, and the extra potassium exit 14.33 against 14.32. Charging to 105 mV needs only .
Explanation. Thirteen times more sodium enters than charging requires. During the second half of the rise the potassium channels are already open, so most of the charge sodium brings in is cancelled by potassium leaving at the same time, and only a small part stays on the capacitor. A spike is cheap in charge and expensive in ions, and pumps must later move all that sodium and potassium back.
Check. Repeat the calculation at 18.5 °C: the model gives 96.9 mV and 563 V/s against 96.8 and 564 in Table 4, and extra sodium and potassium of 4.01 and 4.10 pmol/cm² against 3.99 and 4.07 in Table 5. The largest difference is the potassium of the anode-break row, 16.59 in the model against 16.77 printed, 1.1%.
Source: A. L. Hodgkin and A. F. Huxley · W. Gerstner