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| − | '''Oxygen''' is a chemical [[element]]. Its atomic number, derived from number of [[proton]]s and [[electron]]s it contains, is 8. Oxygen's atomic mass is slightly under 16, since it also has 8 [[neutron]]s (a slight amount of mass is "lost" in the energy contianed in the subatomic bonds).
| + | {{Element | name=Oxygen | symbol=O | anumber=8 | amass=15.994 amu | state=gas | class=Non-metal | cstructure=Cubic | color=Colorless | date=1774 | discname=[[Joseph Priestley]] | origname=From the Greek words ''oxus'' (acid) and ''gennan'' (generate) | uses=Supports life | obtained=From liquid air}} |
| | + | '''Oxygen''' is the third most abundant element in the universe by mass and is essential to life on Earth. |
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| − | Under [[normal condition]]s it is a colorless, odorless [[gas]] consisting of two oxygen [[atom|atoms]] which has the chemical formula O<sub>2</sub>. This means it is diatomic. Approximately 20% of the [[atmosphere]] is made up of oxygen. Oxygen also forms a triatomic molecule called [[ozone]] (O<sub>3</sub>), which although unstable under normal conditions, is a very important ingredient in the upper atmosphere.
| + | ==Chemical Properties== |
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| − | Oxygen is highly reactive, and in many other elements and compounds undergo [[exothermic reaction]]s with it (they [[combustion|burn]] or rust). If it were not for its continual replenishment as a waste product of plant [[photosynthesis]], the atmospheric oxygen would disappear, forming compounds with other chemicals at the earth's surface.
| + | At normal [[atmospheric pressure]] oxygen melts at 54.36 [[Kelvin]] (K) and boils at 90.2 K; on Earth it essentially exists only as a gas. It readily dissolves in water, which makes aquatic life possible. Under normal conditions oxygen forms molecules consisting of two oxygen atoms each sharing two electrons in the 2p subshell; this form of oxygen is known as O<sub>2</sub>. O<sub>2</sub> is a colorless, odourless gas. In liquid form (below -193 degrees Celsius) it is pale blue. |
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| − | Many animals depend upon oxygen as a highly efficient ingredient for breaking down food for energy, due to its reactivity. Those that do not are called "anaerobic", meaning "without air", and include many important bacteria.
| + | ==Isotopes== |
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| − | [[Category:Chemistry]] | + | There are three stable and 14 radioactive isotopes of oxygen. The stable isotopes are <sup>16</sup>O, <sup>17</sup>O and <sup>18</sup>O, with <sup>16</sup>O being by far the most common. Radioisotopes range from <sup>10</sup>O to <sup>26</sup>O, with the two most stable being <sup>15</sup>O and <sup>14</sup>O. This gives oxygen an atomic weight of slightly below 16.<ref>http://education.jlab.org/itselemental/iso008.html</ref> |
| − | [[Category:Elements]] | + | |
| − | [[Category: hydrogen economy]] | + | ==Compounds== |
| − | [[Category:gasses]] | + | |
| | + | Oxygen is highly reactive. It reacts readily with most metals and many other elements, either through combustion or oxidation. As a result, many naturally occurring compounds contain oxygen. |
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| | + | ==Occurrence in Nature== |
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| | + | Oxygen is the third most abundant element in the universe by mass after [[hydrogen]] and [[helium]]; approximately 5.9% of the mass of our [[solar system]] consists of oxygen. However, due to the large disparity in atomic weight between all isotopes of oxygen compared with <sup>1</sup>H and <sup>4</sup>He, less than 0.5% of the atoms in the solar system are oxygen atoms.{{fact}} |
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| | + | Due to its reactivity free oxygen is extremely rare in nature and would not exist on Earth without the process of [[photosynthesis]]. Geologists and paleontologists believe that free oxygen first appeared during the "Great Oxygenation Event" around 2.4 billion years ago. Young-Earth creationists reject this timescale. |
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| | + | {{Periodic table}} |
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| | + | ==References== |
| | + | {{Reflist}} |