Calcium
The chemical element Calcium (Ca), atomic number 20, is the fifth element and the third most abundant metal in the earth’s crust. The metal is trimorphic, harder than sodium, but softer than aluminium. As well as beryllium and aluminium, and unlike the alkaline metals, it doesn’t cause skin-burns. It is less chemically reactive than alkaline metals and than the other alkaline-earth metals.
Calcium
ions solved in water form deposits in pipes and boilers and when the water is
hard, that is, when it contains too much calcium or magnesium. This can be
avoided with the water softeners. In the industry, metallic calcium is separated from the melted
calcium chloride by electrolysis. This is obtained
by treatment of carbonated minerals with chlorhydric acid, or like a sub
product of the carbonates Solvay process.
In contact with air, calcium develops an oxide and nitride
coating, which protects it from further corrosion. It burns in the air at a
high temperature to produce nitride.
The
commercially produced metal reacts easily with water and acids and it
produces hydrogen which contains remarkable amounts of ammonia and hydrocarbides as impurities.
Applications
The metal
is used in aluminium alloys for bearings, as a
helper in the bismuth removal form lead, as well as in controlling graphitic
carbon in melted iron. It is also used as a deoxidizer in the manufacture of
many steels; as a reducing agent in the preparation of metals as chromium, thorium, zirconium and uranium,
and as separating material for gaseous mixtures of nitrogen
and argon.
Calcium is an alloying used in the production of aluminium, beryllium,
copper, lead and magnesium alloys. It is also used in making cements and mortar that are used in builldings.
The calcium
oxide, CaO, is produced by thermal decomposition of
carbonated minerals in furnaces, applying a continuous bed process. The oxide is used in high intensity light
arcs (lime light) for its unusual spectral characteristics and as dehydrating
industrial agent. The metallurgic industry extensively uses the oxide during
the reduction of ferrous alloys.
The calcium
oxide, Ca(OH)2, has many applications in
which the hydroxyl ion is necessary. In the process of calcium hydroxide
quenching, the volume of blown out lime [Ca(OH)2]
expends to double the initial quantity of quick lime (CaO),
fact that makes it useful to break down rocks or wood.
The quick lime is an excellent absorbent for the carbon dioxide,
because it produces carbonate, which is very insoluble.
The calcium
silicate, CaSi, prepared in an electric oven from
lime, silica and reducing carbonated agents, is useful as a steel-deoxidizing
agent. Calcium carbide, CaC2, is produces when heating up a
mixture of lime and carbon at 3000ºC in an electric oven and it is an acetylate which produces
acetylene by hydrolysis. The acetylene is the base material of a great number
of important chemicals for the organic industrial chemistry.
The pure
calcium carbonate occurs in two crystalline forms: calcite, hexagonal shaped,
which possesses birrefringent properties, and
aragonite, rhombohedric. The natural carbonates are
the most abundant calcium minerals. The Iceland spar and the calcite are
essentially pure carbonate forms, whilst the marble is impure and much more
compact, reason why it can be polished. It’s very demanded as construction
material. Although the calcium carbonate is very little soluble in water, it
is quite soluble if the water contains dissolved carbon dioxide, for in these
solutions it forms bicarbonate when dissolving. This fact explains the cave
formation, where the lime stone deposits have been in contact with acid
waters.
The calcium halogenures include
phosphorescent fluoride, which is the calcium compound more abundant and with
important applications in spectroscopy. The calcium chloride possesses, in the anhydric form, great deliquescence capacity, which makes
it useful as industrial dehydrating agent and as sand whirl control factor in
roads. Calcium hypochlorite (whitening powder) is produced in the industry
when passing chlorine through a lime solution, and has been used as a
whitening agent and as water purifier.
The
dehydrated calcium sulphate is the mineral gypsum,
constitutes the bigger portion of
Calcium
in the environment
Calcium is
the fifth element and the third most abundant metal in the earth’s crust. The
calcium compounds account for 3.64% of the earth’s crust. The distribution of
calcium is very wide; it is found in almost every terrestrial area in the
world. This element is essential for the life of plants and animals, for it is present in the animal’s skeleton, in
tooth, in the egg’s shell, in the coral and in many soils. Seawater contains
0.15% of calcium chloride.
Calcium cannot be found alone in nature. Calcium is found mostly
as limestone, gypsum and fluorite. Stalagmites and stalactites contain
calcium carbonate.
Calcium is
always present in every plant, as it is essential for its growth. It is
contained in the soft tissue, in fluids within the tissue and in the
structure of every animal’s skeleton. The vertebrate’s bones contain calcium
in the form of calcium fluoride, calcium carbonate and calcium phosphate.
Health effects of calcium
Calcium is
the most abundant metal in the human
body: is the main constituent of bones and teeth and it has key metabolic
functions.
Calcium is sometimes referred to as lime. It is most commonly found in milk
and milk products, but also in vegetables, nuts and beans. It is an essential
component for the preservation of the human skeleton and teeth. It also
assists the functions of nerves and muscles.
The use of more than 2,5 grams of calcium per day without a medical necessity
can lead to the development of kidney stones and sclerosis of kidneys and
blood vessels.
A lack of calcium is one of the main causes of osteoporosis. Osteoporosis is
a disease in which the bones become extremely porous, are subject to
fracture, and heal slowly, occurring especially in women following menopause
and often leading to curvature of the spine from vertebral collapse.
Unlike most
of the people think, there is an intense biological activity inside our
bones. They are being renewed constantly by new tissue replacing the old one.
During childhood and adolescence, there’s more production of new tissue than
destruction of the old one, but at some point, somewhere around the 30 or 35 years of age,
the process is inverted and we start to lose more tissue than what we can
replace. In women the process is accelerated after the menopause (the period
marked by the natural and permanent cessation of menstruation, occurring
usually between the ages of 45 and 55); this is because their bodies stop
producing the hormone known as estrogen, one of which functions is to
preserve the osseous mass.
Evidence
suggests that we need a daily intake of 1,000 milligrams of calcium in order
to preserve the osseous mass in normal conditions. This is both for man and
pre-menopausic women. The recommended daily intake
rises to 1,500 for menopausic woman.
The main
calcium sources are the dairy products, but also nuts, some green vegetables
like spinach, and cauliflower, beans, lentils…
Calcium
works together with magnesium to create new osseous mass. Calcium should be
taken together with magnesium in a 2:1 rate, that is to say, if you ingest
1000 mg of calcium, you should also ingest 500 mg of magnesium. Some
magnesium sources in the diet are seafood, whole-grains, nuts, beans, wheat
oats, seeds and green vegetables.
Other
important measures to prevent osteoporosis are:
Other
triggers for osteoporosis are the hereditary factor and the stress.
Environmental Effects of Calcium
Calcium phosphide is very toxic to aquatic organisms.