Calcium
Calcium is a chemical element with the symbol Ca and atomic number 20. It stands as an alkaline earth metal that forms a dark oxide-nitride layer when exposed to air. Its physical properties closely mirror those of its heavier homologues strontium and barium. This substance ranks fifth in abundance within Earth's crust, making it the third most abundant metal after iron and aluminium. The most common calcium compound on our planet exists as calcium carbonate found inside limestone or fossils of early sea life. Other sources include gypsum, anhydrite, fluorite, and apatite minerals. A pure sample appears as a very ductile silvery metal sometimes described as pale yellow. Calcium crystals are often stored in mineral oil to prevent rapid reaction with atmospheric oxygen.
Lime served as a building material for statues around 7000 BC long before chemistry understood its makeup. The first dated lime kiln dates back to 2500 BC and was discovered at Khafajah in Mesopotamia. Dehydrated gypsum appeared simultaneously during construction of the Great Pyramid of Giza. Ancient Romans utilized lime mortars made by heating limestone known scientifically as calcium carbonate. Joseph Black proved in 1755 that this process involved loss of carbon dioxide gas unrecognized by earlier civilizations. Antoine Lavoisier suspected lime might be an oxide of an element in his table from 1789 listing five salifiable earths including chaux. Humphry Davy isolated pure calcium via electrolysis of its oxide in 1808 naming the new element. He used mercury(II) oxide mixed with respective metal oxides on a platinum plate acting as anode while cathode remained submerged in liquid mercury. Distilling off the mercury yielded the metal though no commercial bulk production method existed until over a century later.
Natural calcium consists of a mixture containing five stable isotopes plus one isotope considered stable due to extreme longevity. Calcium-40 makes up 96.941% of natural calcium produced through silicon-burning fusion processes involving alpha particles. It represents the heaviest stable nuclide possessing equal proton and neutron numbers. Another common isotope accounts for roughly 2.806% formed when unstable titanium decays via electron captures into stable calcium-44. Four lighter isotopes comprise less than 1% each primarily products of oxygen burning or silicon burning leaving heavier ones created via neutron capture. Calcium-48 stands out as doubly magic nucleus featuring twenty protons and twenty-eight neutrons arranged within closed shells. This configuration renders it extremely stable despite being very neutron-rich for such light elements. Its beta decay remains hindered by gross mismatch of nuclear spin preventing standard transformation pathways. When calcium-48 does eventually decay it proceeds via double beta decay transforming into titanium instead becoming the lightest known nuclide undergoing this process. Experimental lower limits place half-lives at values exceeding hundreds of millions of years suggesting practical stability.
China produces approximately ten thousand to twelve thousand tonnes annually while Russia yields six thousand to eight thousand tonnes yearly. The United States generates between two thousand and four thousand tonnes per year according to recent data from 2005 showing total global output around twenty-four thousand tonnes. About half extracted worldwide goes toward American usage with eighty percent consumed each calendar year. In Russia and China electrolysis applies directly to molten calcium chloride rather than oxide mixtures used historically elsewhere. U.S. facilities reduce lime using aluminium powder mixed compacted into briquettes placed inside sealed retorts heated near one thousand two hundred degrees Celsius. These operations release calcium vapor condensing over roughly eight hours forming pieces weighing between twenty-four and thirty-four kilograms. Metallic calcium finds largest application in steelmaking where strong chemical affinity removes oxygen sulfur impurities creating liquid aluminate sulfide inclusions improving castability cleanliness mechanical properties. Automotive batteries utilize small amounts containing zero point one percent calcium lead alloys reducing water loss self-discharging compared traditional antimony alternatives. Calcium also strengthens aluminum bearings controls graphitic carbon cast iron removing bismuth impurities from pure lead sources.
Mountain building exposes calcium bearing rocks like basalt granodiorite triggering chemical weathering releasing ions into surface waters. Transported rivers carry these dissolved species oceans reacting carbon dioxide form limestone settling sea floor incorporated new geological formations. Each released ion ultimately removes single molecule atmospheric ocean soil living organisms storing it carbonate rocks lasting hundreds millions years. Weathering processes scrubbing CO2 exert long term effects climate regulation through natural cycles connecting tectonics atmosphere biosphere geosphere. Seawater pH converts most dissolved carbon immediately back bicarbonate ions resulting net transport one molecule per cycle lithospheric storage systems. Skulan DePaolo observed 1997 that seawater concentration changes reflect mineral precipitation rates exceeding input inputs demonstrating dynamic non steady state conditions marine environment. These fluctuations hold important climatological implications linking calcium cycling directly global carbon balance mechanisms operating over deep time scales billions of years human history.
Calcium ranks as the fourth most abundant element lunar highlands yet remains essential life forms requiring large quantities daily intake levels vary age groups ranging seven hundred milligrams infants up thirteen hundred adolescents aged nine eighteen years old adults need thousand milligram amounts pregnancy lactation maintain similar thresholds. The Ca2+ ion acts electrolyte vital muscular circulatory digestive system health indispensable bone building hydroxyapatite supporting blood cell synthesis function regulating contraction muscles nerve conduction clotting blood tightly controlled intra extracellular concentrations. Calcium binds carboxyl glutamic acid residues interacting phosphorylated serine tyrosine threonine chelated gamma-carboxylated amino acids enabling complex formation proteins enzymes trypsin osteocalcin activating phospholipid layer anchoring surface associated molecules solubility ranges monocalcium phosphate highly soluble dicalcium phosphate moderate tricalcium phosphate low allowing diverse biological roles skeletal organic matrix interactions maintaining homeostasis critical metabolic processes throughout organism lifespan.
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Common questions
What is calcium and how abundant is it in Earth's crust?
Calcium is a chemical element with the symbol Ca and atomic number 20 that ranks fifth in abundance within Earth's crust. It stands as an alkaline earth metal and serves as the third most abundant metal after iron and aluminium.
When was pure calcium first isolated by Humphry Davy?
Humphry Davy isolated pure calcium via electrolysis of its oxide in 1808 naming the new element. He used mercury(II) oxide mixed with respective metal oxides on a platinum plate acting as anode while cathode remained submerged in liquid mercury.
Which countries produce the most calcium annually according to recent data from 2005?
China produces approximately ten thousand to twelve thousand tonnes annually while Russia yields six thousand to eight thousand tonnes yearly. The United States generates between two thousand and four thousand tonnes per year showing total global output around twenty-four thousand tonnes.
How does calcium cycling affect climate regulation over deep time scales?
Weathering processes scrubbing CO2 exert long term effects climate regulation through natural cycles connecting tectonics atmosphere biosphere geosphere. Seawater pH converts most dissolved carbon immediately back bicarbonate ions resulting net transport one molecule per cycle lithospheric storage systems lasting hundreds millions years.
What are the daily intake levels for calcium across different age groups?
Daily intake levels vary age groups ranging seven hundred milligrams infants up thirteen hundred adolescents aged nine eighteen years old adults need thousand milligram amounts pregnancy lactation maintain similar thresholds. Calcium ranks as the fourth most abundant element lunar highlands yet remains essential life forms requiring large quantities daily.