It is generally accepted that for aqueous solutions the pH value falls within the range of 0–14: acidic solutions pH < 7, alkaline solutions pH > 7, neutral solutions pH = 7. Typically, surface waters have a pH in the range of 6.5–8.5, which meets the requirements for drinking water.
In the case of living water, pH does not play a special role, because the water adapts to the needs of our body. The body receives as many alkaline or acidic ions from the water as it requires to restore balance. Our water restores equilibrium—and this is what really matters, whether the water is alkaline or acidic.
The same applies to Redox potential. It is discussed in the context of restoring the body’s acid-base balance. Its specific value in active water does not matter, because for the body the crucial factor is the ability to donate or accept electrons, which in turn restores balance. A negative redox potential indicates an excess of electrons available to be taken up. In our water, there is no need to define the potential, because we are not artificially supplying electrons. Instead, the water “cooperates” with the body to restore acid-base balance, allowing the organism’s pH to reach the level most suitable for it.
In other words: by working together with the water, the body achieves the pH it needs. This value can differ from person to person. That is the true advantage of active water—it responds to individual needs.