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Calcium

Calcium is a chemical Potassium - Calcium - Scandium element in the periodic table that has the symbol Mg Ca and atomic number 20. Ca Calcium is a soft grey SrÊÊ [Image:Ca-TableImage.png] alkaline earth metal that Ê Full table is used as a reducing Ê agent in the extraction of General thorium, zirconium and uranium. This element is Name, Symbol, Number Calcium, Ca, 20 also the fifth most Series Alkaline earth metal abundant element in the Group, Period, Block 2 (IIA), 4, s earth's crust and is an essential element for Density, Hardness 1550 kg/m3, 1.75 living organisms. Appearance silvery white Atomic Properties Atomic weight 40.078 amu Atomic radius (calc.) 180 (194) pm Covalent radius 174 pm van der Waals radius no information Electron configuration [Ar]4s2 e- 's per energy level 2, 8, 8, 2 Notable Characteristics Oxidation states (Oxide) 2 (strong base) Calcium is a rather hard Crystal structure Cubic face centered element that is purified Physical Properties by electrolysis from State of matter solid (paramagnetic) calcium fluoride that burns with a yellow-red Melting point 1115 K (1548¡F) flame and forms a white Boiling point 1757 K (2703¡F) nitride coating when exposed to air. It reacts Molar volume 26.20 ×103 m3/mol with water displacing Heat of vaporization 153.6 kJ/mol hydrogen and forming Heat of fusion 8.54 kJ/mol calcium hydroxide. Vapor pressure 254 Pa at 1112 K Applications Speed of sound 3810 m/s at 293.15 K Calcium is an important Other component of a healthy Electronegativity 1.00 (Pauling scale) diet. Its minor deficit Specific heat capacity 0.632 J/(kg*K) can affect bone and teeth formation. Its excess can Electrical conductivity 29.8 106/m ohm lead to kidney stones. Thermal conductivity 201 W/(m*K) Vitamin D is needed to absorb calcium. Dairy 1st ionization potential 589.8 kJ/mol products are an excellent 2nd ionization potential 1145.4 kJ/mol source of calcium. Other uses include: 3rd ionization potential 4912.4 kJ/mol * Reducing agent in the Most Stable Isotopes extraction of other iso NA half-life DM DE MeV DP metals such as uranium, zirconium, 40Ca 96.941% Ca is stable with 20 neutrons and thorium. 41Ca {syn.} 103,000y epsilon 0.421 41K * Deoxidizer, desulfurizer, or 42Ca 0.647% Ca is stable with 22 neutrons decarburizer for 43Ca 0.135% Ca is stable with 23 neutrons various ferrous and nonferrous alloys. 44Ca 2.086% Ca is stable with 24 neutrons * Alloying agent used in the production of 46Ca 0.004% Ca is stable with 26 neutrons aluminum, beryllium, 48Ca 0.187% >6×1018y beta- 4.272 48Ti copper, lead, and magnesium alloys. SI units & STP are used except where noted. History (Latin calx, lime) Lime was prepared and used by the Romans as early as the 1st century, but calcium was not discovered until 1808. After learning that Berzelius and Pontin prepared calcium amalgam by electrolyzing lime in mercury, Sir Humphry Davy was able to isolate the impure metal. Occurrence Calcium is the fifth most abundant element in the earth's crust (forming more than 3%) and is an essential part of leaves, bones, teeth, and shells. Due to its chemical reactivity with air and water, calcium is never found in nature unbound to other elements. This metallic element is found in quantity in limestone, gypsum, and fluorite. Apatite is the fluorophosphate or chlorophosphate of calcium. Electrolysis of molten calcium chloride (CaCl2) can be used to isolate pure calcium. Isolation (* follow): cathode: Ca2+* + 2e- --> Ca anode: Cl-* --> *Cl2 (gas) + e- Compounds Quicklime (CaO) is used in many chemical refinery processes and is made by heating and carefully adding water to limestone. When CaO is mixed with sand it hardens into a mortar and is turned into plaster by carbon dioxide uptake. Mixed with other compounds, CaO forms an important part of Portland cement. When water percolates through limestone or other soluble carbonate rocks, it partially disolves part of the rock and causes cave formation and characteristic stalactites and stalagmites and also forms hard water. Other important calcium compounds are nitrate, sulfide, chloride, carbide, cyanamide, and hypochlorite. Isotopes Calcium has six stable isotopes, two of which occur in nature: stable Ca-40 and radioactive Ca-41 with a half-life = 103,000 years. 97% of the element is in the form of Ca-40. Ca-40 is one of the daughter products of K-40 decay, along with Ar-40. While K-Ar dating has been used extensively in the geological sciences, the prevalence of Ca-40 in nature has impeded its use in dating. Techniques using mass spectrometry and a double spike isotope dilution have been used for K-Ca age dating. Unlike cosmogenic isotopes that are produced in the atmosphere, Ca-41 is produced by neutron activation of Ca-40. Most of its production is in the upper meter or so of the soil column where the cosmogenic neutron flux is still sufficiently strong. Ca-41 has received much attention in stellar studies because Ca-41 decays to K-41, a critical indicator of solar-system anomalies.

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