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Blood pH and Life


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The movement of life stems from the constant change of one element into another.



How Our Bodies Regulate pH

Biological Transmutations

by Professor C. Louis Kervan

Member of the New York Academy of Science
Director of Conferences of Paris University
Member of Conseil d'Hygiene de la Seine

Translation and Adaptation by Michel Abehsera
Copyright 1989

If there is abundant literature showing that the presence of K is dependent on the availability of oxygen, there are also several experiments showing its relation to hydrogen, for according to our reaction, K + H = Ca. In other words, if K is too abundant in the presence of H, it will give Ca.

The presence of H is linked to acidity ( low pH ). An excess of H ions signifies an acidity that might become dangerous for the cell. However, in that case K can join an H nucleus to produce Ca, thereby establishing alkalinity and an optimum Ca/K ratio. The agent of equilibrium is thus K. The effects between K and Ca are opposite in appearance only; they are in fact complementary.

Hoagland writes that there is a clear tendency toward acidification of the of the cellular medium, freezing H+ ions; the addition of K+ ions leads to the alkalinization of the cellular liquids.

Reinberg notices that "the alkalinization of the cellular liquids with K is well known by arboriculturists, who use potassium nitrate to speed up fruit maturation."

It is of interest to point out that the proportions of K and Ca are of the same order in animal life — in the plasma as well as in seawater, where life began.

...

Darrow pointed out that a K increase in the cell decreases the cell's acidity because it causes a decrease in H. Thus the alkalinization takes place when K takes H to give Ca. Ca is taken back by the outside liquid and excreted, producing a negative Ca balance sheet. More Ca is excreted than ingested, but the main source of Ca is Mg.

The internal equilibrium of the animal cell postulates a large K content and a small Ca content. The reactions with H help to reduce acidification, since H is taken away.

It has been found that micro-organisms in the soil excrete H ions which acidify the soil; however, K neutralizes this acidity when it comes in contact with the roots.

If the calcium concentration in the nutritive medium is increased, there is a smaller absorption of K. This can be explained by the fact of reversibility.

...

This specific reaction allows a biological equilibrium to be maintained.




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