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Dr. Chris Meletis N. D.
Chloride: The Forgotten Essential Mineral
Chloride is an “essential” mineral for humans. It is abundant in
ionic trace mineral preparations. It is a major mineral nutrient
that occurs primarily in body fluids. Chloride is a prominent negatively
charged ion of the blood, where it represents 70% of the body’s total
negative ion content. On average, an adult human body contains
approximately 115 grams of chloride, making up about 0.15% of total body
weight.1
The suggested amount of chloride intake ranges from 750 to 900 milligrams
per day, based on the fact that total obligatory loss of chloride in the
average person is close to 530 milligrams per day. As the principle
negatively charged ion in the body, chloride serves as one of the main
electrolytes of the body. Chloride, in addition to potassium and sodium,
assist in the conduction of electrical impulses when dissolved in bodily
water. Potassium and sodium become positive ions as they lose an electron
when dissolved and chloride becomes a negative ion as it gains an electron
when dissolved. A positive ion is always accompanied by a negative ion,
hence the close relationship between sodium, potassium and chloride. The
electrolytes are distributed throughout all body fluids including the blood,
lymph, and the fluid inside and outside cells.2
The negative charge of chloride balances against the positive charges of
sodium and potassium ions in order to maintain serum osmolarity.
Pivotal Roles of Chloride in the Body
In addition to its functions as an electrolyte, chloride combines with
hydrogen in the stomach to make hydrochloric acid, a powerful digestive
enzyme that is responsible for the break down of proteins, absorption of
other metallic minerals, and activation of intrinsic factor, which in turn
absorbs vitamin B12. Chloride is specially transported into the gastric
lumen, in exchange for another negatively charged electrolyte (bicarbonate),
in order to maintain electrical neutrality across the stomach membrane.
After utilization in hydrochloric acid, some chloride is reabsorbed by the
intestine, back into the blood stream where it is required for maintenance
of extracellular fluid volume. Chloride is both actively and passively
absorbed by the body, depending on the current metabolic demands. A
constant exchange of chloride and bicarbonate, between red blood cells and
the plasma helps to govern the pH balance and transport of carbon dioxide, a
waste product of respiration, from the body. With sodium and potassium,
chloride works in the nervous system to aid in the transport of electrical
impulses throughout the body, as movement of negatively charged chloride
into the cell propagates the nervous electrical potential.
Deficiency of Chloride
Deficiency of chloride is rare. However, when it does occur, it results in
a life threatening condition known as alkalosis, in which the blood becomes
overly alkaline. A tedious balance between alkalinity and acidity is in
constant flux, and must be vigilantly maintained throughout the entire body.
Alkalosis may occur as a result of excessive loss of sodium, such as heavy
sweating during endurance exercise, and in cases of prolonged vomiting and
diarrhea. Symptoms include muscle weakness, loss of appetite, irritability,
dehydration, and profound lethargy. Hypochloremia may result from water
overload, wasting conditions, and extensive bodily burns with sequestration
of extracellular fluids.
In a situation in which infants were inadvertently fed chloride-deficient
formula, many experienced failure to thrive, anorexia, and weakness in their
first year of life.3
Excess Intake?
Excessive intakes of dietary chloride only occur with the ingestion of large
amounts of salt and potassium chloride. The toxic effects of such diets,
such as fluid retention and high blood pressure, are attributed to the high
sodium and potassium levels.4
Chloride toxicity has not been observed in humans except in the special case
of impaired sodium chloride metabolism, e.g. in congestive heart failure.5
Healthy individuals can tolerate the intake of large quantities of chloride
provided that there is a concomitant intake of fresh water. Other situations
in which increased blood levels of chloride are seen include diseases of
improper waste elimination that occur in kidney diseases. Excess chloride is
normally excreted in the urine, sweat, and bowels. In fact, excess urinary
excretion of chloride occurs in high salt diets. Excessive intakes of
chloride can occur in a person with compromised health in addition to an
unhealthy diet. However, those that follow a healthy diet and lead an
active lifestyle may need to consider supplementing their diet with this
important mineral.
Chloride vs. Chlorine
The mineral supplement chloride is very different from
the gas chlorine. While elemental chlorine is a dangerous gas that does not
exist in the free elemental state in nature because of its reactivity,
although it is widely distributed in combination with other elements.
Chloride is related to chlorine however, as one of the most common chlorine
compounds is common salt, NaCl. Chloride is a by-product of the reaction
between chlorine and an electrolyte, such as potassium, magnesium, or
sodium, which are essential for human metabolism. Chloride salts are
essential for sustaining human metabolism and have none of the effects of
isolated chlorine gas.
Sources of Chloride
Chloride occurs naturally in foods at levels normally less than 0.36
milligrams per gram of food. The average intake of chloride during a
salt-free diet is approximately 100 milligrams per day. Unfortunately,
chloride is found commonly combined with undesirable dietary sources. The
most common of these negative sources is table salt. Table salt is made
from a combination of sodium and chloride ions. Other unhealthful sources
include yeast extracts, processed lunchmeats, and cheeses. Healthier sources
of chloride include kelp (seaweed), ionic trace minerals, olives,
rye, tomatoes, lettuce, and celery,
although not in large enough amounts to supply the needs of an active adult.6
In its original form, however, chloride is leached from various rocks into
soil and water by years of weathering processes. The chloride ion is highly
mobile and is transported to closed basins, such as the
Great Salt Lake,
or oceans.7
Summary
Chloride is a highly important, vital mineral required for both human and
animal life. Without chloride, the human body would be unable to maintain
fluids in blood vessels, conduct nerve transmissions, move muscles, or
maintain proper kidney function. As a major electrolyte mineral of the
body, chloride performs many roles, and is rapidly excreted from the body.
Active adults that eat a healthy diet devoid of salt and illnesses in which
vomiting and/or diarrhea are profuse warrant the supplementation of
additional chloride. Replacement of chloride is essential on a daily basis
to maintain regular metabolic function. Chloride is safely utilized by the
body, without negative health effects. Of the negative health effects that
have been associated with diets high in chloride, these are mainly
attributable to the accompanying sodium and potassium, two other electrolyte
minerals to which chloride is often attached
1
Wesson LG. Physiology of the human kidney. New York, NY, Grune and
Stratton, 1969: 591
2
Weast RC, ed. CRC handbook of chemistry and physics, 67th ed. Boca
Raton, FL, CRC Press, 1986.
3
Kaleita TA. Neurologic/behavioral syndrome associated with ingestion of
chloride-deficient infant formula. Pediatrics 1986 Oct;78(4):714-5
4
Beard TC. A salt-hypertension hypothesis. J Cardiovasc Pharmacol 1990;16
Suppl 7:S35-8
5
Seelig M.
Cardiovascular consequences of magnesium deficiency and loss:
pathogenesis, prevalence and manifestations--magnesium and chloride loss
in refractory potassium repletion. Am J Cardiol 1989 Apr
18;63(14):4G-21G
6 Altschul AM, Grommet JK. Food
choices for lowering sodium intake. Hypertension 1982 Sep-Oct;4(5 Pt
2):III116-20
7 Gelb SB,
Anderson MP. Sources of chloride and sulfate in ground water beneath an
urbanized area in Southeastern Wisconsin (Report WIS01 NTIS). Chemical
abstracts, 1981, 96(2):11366g.
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