Principles of buffering:
HA ⇌ H+ + A−
OH− + HA → H2O + A−
OH− + H+ → H2O
Once the acid is more than 95%
deprotonated, the pH rises rapidly because most of the added alkali is consumed in the neutralization reaction.
Buffer capacity is a quantitative measure of the resistance to change of pH of a solution containing a buffering agent with respect to a change of acid or alkali concentration. It can be defined as follows:
What's essentially happening throughout the growing phase, is that your "buffer" is always getting smaller and smaller, (as acids are deprotonated) so if you build in a "reserve" buffer, during the mixing phase (when soil is created) you should have more overhead, while still maintaining excellent pH values. (an offset) that can absorb and bind all the broken down acids, so that the soil pH remains healthy, and constant.
This is how I understand it anyhow.