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.