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CALCIUM |
| Physical Properties |
Atomic Number:
20
Atomic Weight:
40.08
Electron Configuration:
1s22s22p63s23p64s2
First Ionization
Energy: 590 kJ/mol
Second Ionization Energy: 1145 kJ/mol
Crystal Structure: Face-Centered Cubic
Density: 1.55 g/cm3
Melting Point: 839oC
Atomic Radius: 197 pm
Ionic Radius: 99 pm
Standard Reduction Potential: -2.87 V (Ca2+ + 2e-= Ca)
| Occurrence and Properties |
Calcium is the third lightest member of the alkaline earth metals. Calcium is more reactive than magnesium. It is silvery in appearance, but when exposed to the air it quickly develops a white coating of calcium oxide. The calcium in the photo above is slightly tarnished due to exposure to siar. Calcium does not occur in nature in elemental form but it is widely distributed in compound form. Some common calcium ores include calcite (calcim carbonate), dolomite (calcium magnesium carbonate), gypsum (calcium sulfate dihydrat) and fluorite (calcium fluorite)
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Optical Calcite Calcite is one form of calcium carbonate. |
| Reactions of Calcium |
Calcium is generally more reactive than magnesium but not as reactive as sodium or potassium. Calcium will react quite vigorously with water to form calcium hydroxide and hydrogen gas.
Ca + 2H2O = Ca(OH)2 + H2
Calcium slowly oxidizes upon exposure to air, forming calcium oxide.
2Ca + O2 = 2CaO
Calcium will react with the halogens to form the corresponding halide.
When heated, it will react with nitrogen to form calcium nitride and with
hydrogen to form calcium nitride and with sulfur to form calcium sulfide.
| Calcium Compounds |
Calcium has no tendency to form covalent compounds and
all calcium compounds are ionic in nature. In general, calcium compounds
tend to be less soluble than the corresponding magnesium compounds. Calcium
sulfate, carbonate, chromate, and oxalate are all insoluble compounds.
Several calcium compounds are common household chemicals. Gypsum, used
in the manufacture of wallboard, is calcium sulfate dihydrate. Plaster
of paris is calcium sulfate hemihydrate (hemihydrate = half-hydrate). Calcium
oxide is called lime or quicklime. It reacts with water to produce calcium
hydroxide, and is often used to raise the pH of acidic soils.
CaO + H2O = 2Ca(OH)2
Calcium hydroxide is known as slaked lime, and solutions of calcium hydroxide are known as limewater. When carbon dioxide is bubbled through a solution of limewater, a precipitate of calcium carbonate is produced. In this case a precipitate is produced becasue calciumc carbonate is insoluble. Other hydroxides may be used; on space missions the air is "scrubbed" by passing it through a solution of lthium hydroixde (lithium is used because it is ligter).
CO2 + Ca(OH)2 = CaCO3
+ H2O
Limerock (or limestone) and coral are both composed prmarily of calcium
carbonate. There are two forms of calcium carbonate, the calcite form and
the aragonite form. Calcium carbonate deposited on land is primarily the
calcite form, while calcium carbonate deposited in the sea, such as coral,
is primarily the aragonite form.
Although considered to be insoluble, small amounts of calcium carbonate
will dissolve in water and water obtained in areas where the bedrock is
primarily limerock is said to be "hard" due to the presence of
dissolved calcium and magnesium. This solubiliy decreases with increasing
temperature; in boilers this is a problem because heating causes the dissolved
calcium and magnesium carbonates to be deposited as "bouiler scale."
All carbonates, including calcium and magnesium carbonate, react with acids
to expel carbon dioxide gas.
CaCO3 + 2HCl = CaCl2 + H2O + CO2