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Introduction |
Contents |
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9
The Kinetics
of Acetylcholinesterase Inhibition and the Influence
of Fluoride and Fluoride Complexes on the
Permeability of Erythrocyte Membranes - Page 7.
B.
Effect of Fluoride on the Permeability of the
Erythrocyte Membranes for
Na+,
K+, Ca2+, F-, HPO42-,
and Glucose
Exerting an influence on the
permeability for the cations and anions at the cell
membrane always has effects on the function of the
effected cells. The effect can either support or
hinder their cellular function. In the case of nerve
cells, for example, a depolarizing effect, which is
the result of affecting the (Na+-K+)
permeability of the membrane, can increase the
excitability of the cell to a certain extent when
the resting potential moves closer to the threshold
potential without exceeding it. If the latter arises
it leads to a constant depolarization and thereby
un-excitability. The distribution of the (Na+-K+)
ions is especially important because the
polarization of the cell is the result of an unequal
distribution of these ions between the intra- and
extracellular spaces. We therefore tried, with the
help of the radioactive isotopes Na-24 and K-42, to
study the influence of the smallest F concentrations
possible on the distribution of these ions across
the cell membrane. The erythrocytes served as a
model for the large number of other cells on which
studies can only be carried out with a considerably
larger experimental effort.
The separation of the (Na+-K+)
ions at the membrane is an entropy reducing
process. The necessary energy is taken from the
splitting of ATP. SEN and POST (30) found that per
split Mol of ATP, 3 Mol of Na+
are exported, and 2 Mol K+ are imported.
The cell in turn extracts the ATP from glycolysis (Embden-Meyerhoff
degradation) as well as the following
respiratory chains. Erythrocytes are, however,
because of missing sub-cellular particles, only
capable of glycolysis. Every effect on the
metabolism of ATP can therefore also have effects on
active transport. Such an effect arises, for example
a) with an increase in the F-
concentration (21)
b) with an increase in the Ca2+
concentration (31)
c) with a decrease in the Mg
concentration
d) with a decrease in the
glucose concentration
e) with a decrease in the
potassium concentration (32)
f) with an increase in the
sodium concentration (32)
Due to this variety of mechanisms
one must study the effects of fluoride on as many
parameters of the cellular medium as possible,
whereby one must take great pains to match the
remaining controlled variables as closely as
possible to the natural conditions of the cell. We
therefore studied the effect of fluoride on the
variables listed above.
Description of the Isotopes Used
We carried out all subsequent
studies with the help of radioactively labeled
substances. The overwhelming portion of the tracers
we used are commercially available (from
Amersham-Buchler, Braunschweig). The isotopes
18F and 31Si are, because of their
short life spans, not sold. We obtained the 18F
in cooperation with the physics institute at the
University of Hamburg (Prof. H. Neuert’s study group
kindly took charge of 18F for us) while
we produced the 31Si with the help of our
institute's neutron generator. For now we could only
study the production of 31Si from which
we developed the basis for further studies (eg,
resorption of hexafluorosilicates). The 18F
was so far only twice available to us, because of
which only a few orienting preliminary experiments
could be carried out with it. In the following table
we give an overview of the most important
characteristics of the isotopes that were used.
|
Isotope |
Half-Life |
Type of Radiation |
Max Energy
MeV
|
Production Process |
|
14C |
5730 years |
b- |
0.156 |
14N(n,p)
14C |
|
18F |
1.83 hours |
b+
g |
0.65
0.51 |
16O(3He,
p) 18F |
|
24Na |
15.5 hours |
b-
g |
1.39
2.76
1.38 |
23
Na(n,g)
24Na |
|
31Si |
2.62 hours |
b-
g |
1.48
1.26 |
31P(n,p)
31Si |
|
32P |
14.3 days |
b- |
1.74 |
31P(n,g)
32P |
|
42K |
12.4 hours |
b-
g |
3.58; 2.04
1.51; 0.32 |
41K(n,g)
42K |
|
45Ca |
165 days |
b- |
0.25 |
44Ca(n,g)
45Ca |
Production of 31Si
Since we saw from the example of
AChE that silicon compounds could be of biological
importance, and since Si, like F, is probably one of
the essential elements (daily release in the urine
around 10mg), we undertook the task of developing a
tracer method that would allow us to follow the path
of Si in the body. The processes involved in
resorption of SiF62- were of
particular interest to us. Since radioactive
isotopes of this element are not commercially sold,
we developed a method to obtain carrier-free 31Si.
Using our institute's neutron generator, which
generates neutrons with an energy of 10-14 MeV at a
maximum flow of 109 particles/sec and cm2,
we exposed the purest red phosphorus to the neutron
beam for 15 hours. An analysis of the
g-spectrum
of the specimen showed that only 28Al
(half-life 2.31 min.) and 31Si had
formed.
31P(n,p)
31Si
s
= 0.077b
31P(n,
a)
28Al
s
= 0.15 b
The 28Al isotope did
not, however, disrupt the experiment because of its
relatively short half-life in comparison to 31Si.
The following decay curve was derived by recording
from a piece of the activated specimen in the liquid
scintillation counter.
Figure 32
- Decay Curve of a Phosphorus Specimen After 15
Hours of Activation
The mathematical expression for
the curve in figure 32 forms the equation for the
radioactive decay. In logarithmic form it reads:
(equation 28)
The following relationship
develops between the decay constant, which is
identical to the slope of the line here, and the
half-life t1/2:
(equation 29)
By inserting the value for the
slope of the line from figure 32 one derives the
half life as:

This value agrees exactly with
the half life for 31Si (see table 3),
which is an additional proof that only this
radioactive isotope is present. Next we carried out
a series of experiments to separate the red
phosphorus from the carrier. We would like to
briefly describe two of these experiments.
1.)
We agitated a specimen of the activated
phosphorus with 30% hydrofluoric acid. The Si, which
due to the high degree of dispersion could be
oxidized to SiO2 using the oxygen in the
air, was supposed to react with the HF.
The hexafluorosilicic acid
thereby went into solution. After a reaction time of
one hour we separated the precipitates from the
solution and determined the radioactivity in both
the precipitate and the solution. Result: 15.5% of
the total radioactivity was found in the solution.
2.) We agitated another specimen
together with a 1% solution of MgSiF6 in
water.
Result: After one hour 67% of the
31Si had gone into solution. So, a
relatively fast exchange takes place on the
phosphate carrier between the stable 30Si
and the radioactive 31Si. This is,
therefore, a very convenient method for separating
the 31Si from the carrier, whereby a
labeled SiF62- solution
simultaneously forms and can be directly implemented
in further experiments.
Unfortunately, the activities
that can be derived in this way are too limited for
many studies on biological systems (especially for
studies on living animals). For this reason, in
further studies we will have to rely on the
production of this isotope from 30Si
(over n,
g
reaction) in the reactor. The derived
radioactivities (around 5 µCi) are, however,
sufficient for measuring the permeability
characteristics of fluorosilicate complexes of
various biological membranes.
Introduction |
Contents |
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2 |
3 |
4 |
5 |
6 |
7 |
8 |
9 |