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{{distinguish|Rutheniumruthenium}}
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{{infobox rubidium}}
'''Rubidium''' is a [[chemical element]]; it has [[Symbol (chemistry)|symbol]] '''Rb''' and [[atomic number]] 37. It is a very soft, whitish-grey solid in the [[alkali metal]] group, similar to [[potassium]] and [[caesium]].<ref>{{Ullmann |doi=10.1002/14356007.a23_473.pub2 |title=Rubidium and Rubidium Compounds |year=2010 |last1=Lenk |first1=Winfried |last2=Prinz |first2=Horst |last3=Steinmetz |first3=Anja |isbn=978-3527306732 }}</ref> Rubidium is the first [[alkali metal]] in the group to have a density higher than [[Properties of water|water]]. On Earth, natural rubidium comprises two [[isotope]]s: 72% is a stable isotope <sup>85</sup>Rb, and 28% is slightly [[radioactive]] <sup>87</sup>Rb, with a [[half-life]] of 48.8 billion years—more than three times as long as the estimated [[age of the universe]].
 
German chemists [[Robert Bunsen]] and [[Gustav Kirchhoff]] discovered rubidium in 1861 by the newly developed technique, [[Atomic emission spectroscopy#Flame emission spectroscopy|flame spectroscopy]]. The name comes from the [[Latin]] word {{lang|la|rubidus}}, meaning deep red, the color of its emission spectrum. Rubidium's compounds have various chemical and electronic applications. Rubidium metal is easily vaporized and has a convenient spectral absorption range, making it a frequent target for [[laser]] manipulation of [[atom]]s.<ref>{{Cite web |title=Rubidium (Rb) {{!}} AMERICAN ELEMENTS ® |url=https://www.americanelements.com/rb.htm |access-date=2024-03-27 |website=American Elements: The Materials Science Company |language=en}}</ref> Rubidium is not a known nutrient for any [[organism|living organisms]]. However, rubidium [[ion]]s have similar properties and the same charge as potassium ions, and are actively taken up and treated by [[animal cell]]s in similar ways.
 
==Characteristics==
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Rubidium is a very soft, [[ductility|ductile]], silvery-white metal.<ref name="Ohly" /> It is the second most [[Electronegativity|electropositive]] of the stable alkali metals and melts at a temperature of {{convert|39.3|°C|°F}}. Like other alkali metals, rubidium metal reacts violently with water. As with potassium (which is slightly less reactive) and caesium (which is slightly more reactive), this reaction is usually vigorous enough to ignite the [[hydrogen]] gas it produces. Rubidium has also been reported to ignite spontaneously in air.<ref name="Ohly">{{cite book | chapter = Rubidium | title = Analysis, detection and commercial value of the rare metals | last = Ohly | first = Julius | publisher = Mining Science Pub. Co. | date = 1910 | chapter-url = https://books.google.com/books?id=dGUuAQAAIAAJ}}</ref> It forms [[amalgam (chemistry)|amalgams]] with [[mercury (element)|mercury]] and [[alloy]]s with [[gold]], [[iron]], [[caesium]], [[sodium]], and [[potassium]], but not [[lithium]] (even though rubidium and lithium are in the same group).<ref name="HollemanAF">{{cite book |publisher = Walter de Gruyter |date = 1985 |edition = 91–100 |pages = 953–955 |isbn = 978-3-11-007511-3 |title = Lehrbuch der Anorganischen Chemie |first1 = Arnold F. |last1 = Holleman |last2 = Wiberg |first2 = Egon |last3 =Wiberg |first3 = Nils |chapter = Vergleichende Übersicht über die Gruppe der Alkalimetalle| language = de}}</ref>
[[File:Rb&Cs crystals.jpg|left|thumb|Rubidium crystals (silvery) compared to [[caesium]] crystals (golden)]]
Rubidium has a very low [[ionization energy]] of only 406&nbsp;kJ/mol.<ref>{{cite book | url = https://books.google.com/books?id=ZOm8L9oCwLMC&pg=PA259 | page =259 | title = Principles of Chemistry: The Molecular Science | isbn = 978-0-495-39079-4 | author1 = Moore, John W | author2 = Stanitski, Conrad L | author3 = Jurs, Peter C | date = 2009| publisher =Cengage Learning }}</ref> Rubidium and potassium show a very similar purple color in the [[flame test]], and distinguishing the two elements requires more sophisticated analysis, such as spectroscopy.{{citation needed|date=December 2021}}<ref>{{Cite journal |last1=Ahrens |first1=L. H |last2=Pinson |first2=W. H |last3=Kearns |first3=Makgaret M |date=1952-01-01 |title=Association of rubidium and potassium and their abundance in common igneous rocks and meteorites |url=https://dx.doi.org/10.1016/0016-7037%2852%2990017-3 |journal=Geochimica et Cosmochimica Acta |volume=2 |issue=4 |pages=229–242 |doi=10.1016/0016-7037(52)90017-3 |bibcode=1952GeCoA...2..229A |issn=0016-7037}}</ref><!-- As a symmetrical effect of rubidium metal's high reactivity toward oxidation and tendency to subsequent formation of the rubidium cation Rb<sup>+</sup>, this cation, once formed, is very stable, and is normally unreactive toward further oxidative or reductive chemical reactions.{{citation needed|date=December 2010}}--><!--ionization energy 10.1103/PhysRevA.49.1646 --><!-- https://books.google.com/books?id=mDXzAAAAMAAJ&q=Rubidium+coordination&dq=Rubidium+coordination&hl=de&ei=5GB9Tc7pJ4f2sgax7ZTsBw&sa=X&oi=book_result&ct=result&resnum=1&ved=0CDIQ6AEwAA the coordination is at least six and even nine is possible 10.1007/BF00745739 or twelve http://scripts.iucr.org/cgi-bin/paper?a04757-->
 
===Compounds===
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===Occurrence===
Rubidium is not abundant, being one of 56 elements that combined make up 0.05% of the twentyEarth's crust; at roughly the 23rd <!--third verified in USGS ref -->[[Abundance of elements in Earth's crust|most abundant element in the Earth's crust]], roughlyit asis more abundant asthan [[zinc]] and rather more common thanor [[copper]].<ref name="USGS">{{cite web |url = http://pubs.usgs.gov/of/2003/of03-045/of03-045.pdf |publisher = United States Geological Survey |access-date = 2010-12-04 |title = Mineral Commodity Profile: Rubidium |first1 = William C. |last1 = Butterman |first2 = William E. |last2 = Brooks |first3 = Robert G. Jr. |last3 = Reese |date=2003}}</ref>{{rp|4}} It occurs naturally in the minerals [[leucite]], [[pollucite]], [[carnallite]], and [[zinnwaldite]], which contain as much as 1% rubidium [[oxide]]. [[Lepidolite]] contains between 0.3% and 3.5% rubidium, and is the commercial source of the element.<ref>{{Cite journal |title =Trace element chemistry of lithium-rich micas from rare-element granitic pegmatites |volume = 55
| issue = 13 |date = 1995 |doi = 10.1007/BF01162588 |pages = 203–215 |journal = Mineralogy and Petrology |first = M. A. |last = Wise |bibcode = 1995MinPe..55..203W |s2cid = 140585007
}}</ref> Some [[potassium]] minerals and [[potassium chloride]]s also contain the element in commercially significant quantities.<ref>{{cite book |last=Norton |first=J. J. |date=1973 |chapter=Lithium, cesium, and rubidium—The rare alkali metals |editor=Brobst, D. A. |editor2=Pratt, W. P. |title=United States mineral resources |publisher=U.S. Geological Survey Professional |volume=Paper 820 |pages=365–378 |chapter-url=https://pubs.er.usgs.gov/usgspubs/pp/pp820 |access-date=2010-09-26 |archive-date=2010-07-21 |archive-url=https://web.archive.org/web/20100721060544/http://pubs.er.usgs.gov/usgspubs/pp/pp820 |url-status=dead }}</ref>
 
[[Seawater]] contains an average of 125&nbsp;µgμg/L of rubidium compared to the much higher value for potassium of 408&nbsp;mg/L and the much lower value of 0.3&nbsp;µgμg/L for caesium.<ref>{{cite journal |last1 = Bolter |first1 = E. |last2 = Turekian |first2 = K. |last3 = Schutz |first3 = D. |title = The distribution of rubidium, cesium and barium in the oceans |journal = Geochimica et Cosmochimica Acta |volume = 28 |issue = 9 |pages = 1459 |date = 1964 |doi = 10.1016/0016-7037(64)90161-9 |bibcode = 1964GeCoA..28.1459B }}</ref> Rubidium is the 18th most abundant element in seawater.<ref>{{Cite book |last1=Hart |first1=William A. Hart|url=https://doi.org/10.1016/C2013-0-05695-2 |title=The Chemistry of Lithium, Sodium, Potassium, Rubidium, Caesium,Cesium and Francium |last2=Beumel Jr. |first2=O.F . |last3=Whaley |first3=Thomas P. |date=1973 |publisher=Elsevier |isbn=978-0-08-018799-0 |page=371 |doi=10.1016/c2013-0-05695-2}}</ref>
 
Because of its large [[ionic radius]], rubidium is one of the "[[incompatible element]]s".<ref>{{cite book |url = https://books.google.com/books?id=385nPZOXmYAC&pg=PA224 |page = 224 |title = Cosmochemistry |isbn = 978-0-521-87862-3 |author1 = McSween Jr., Harry Y |author2 = Huss, Gary R |date = 2010|publisher = Cambridge University Press }}</ref> During [[Fractional crystallization (geology)|magma crystallization]], rubidium is concentrated together with its heavier analogue caesium in the liquid phase and crystallizes last. Therefore, the largest deposits of rubidium and caesium are zone [[pegmatite]] ore bodies formed by this enrichment process. Because rubidium substitutes for [[potassium]] in the crystallization of magma, the enrichment is far less effective than that of caesium. Zone pegmatite ore bodies containing mineable quantities of caesium as [[pollucite]] or the lithium minerals [[lepidolite]] are also a source for rubidium as a by-product.<ref name="USGS" />
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Rubidium has been used for polarizing [[Helium-3|<sup>3</sup>He]], producing volumes of magnetized <sup>3</sup>He gas, with the nuclear spins aligned rather than random. Rubidium vapor is optically pumped by a laser, and the polarized Rb polarizes <sup>3</sup>He through the [[hyperfine structure|hyperfine]] interaction.<ref>{{Cite journal |url=http://www.ncnr.nist.gov/equipment/he3nsf/SEOP/nistSlowNeutronconf2005.pdf |journal=Journal of Research of the National Institute of Standards and Technology |title=Polarized <sup>3</sup>He spin filters for slow neutron physics |volume=110 |issue=3 |pages=299–304 |first1=T. R. |last1=Gentile |first2=W. C. |last2=Chen |first3=G. L. |last3=Jones |first4=E. |last4=Babcock |first5=T. G. |last5=Walker |doi=10.6028/jres.110.043 |pmid=27308140 |pmc=4849589 |year=2005 |access-date=2015-08-06 |archive-date=2016-12-21 |archive-url=https://web.archive.org/web/20161221234735/https://ncnr.nist.gov/equipment/he3nsf/SEOP/nistSlowNeutronconf2005.pdf |url-status=dead }}</ref> Such [[spin polarization|spin-polarized]] <sup>3</sup>He cells are useful for neutron polarization measurements and for producing polarized neutron beams for other purposes.<ref>{{Cite web |url=http://www.ncnr.nist.gov/AnnualReport/FY2002_html/pages/neutron_spin.htm |publisher=NIST Center for Neutron Research 2002 Annual Report |title=Neutron spin filters based on polarized helium-3 |access-date=2008-01-11}}</ref>
 
The resonant element in [[atomic clock]]s utilizes the [[hyperfine structure]] of rubidium's energy levels, and rubidium is useful for high-precision timing. It is used as the main component of secondary frequency references (rubidium oscillators) in cell site transmitters and other electronic transmitting, networking, and test equipment. These [[rubidium standard]]s are often used with [[Global Positioning System|GPSGNSS]] to produce a "primary frequency standard" that has greater accuracy and is less expensive than caesium standards.<ref>{{cite book |chapter-url = https://books.google.com/books?id=jmfkJYdEANEC&pg=PA32 |page = 32 |chapter = GPS |title = Measurement, control, and communication using IEEE 1588 |isbn = 978-1-84628-250-8 |author1 = Eidson, John C |date = 2006-04-11|publisher = Springer }}</ref><ref name="Clock">{{cite book |chapter-url = https://books.google.com/books?id=ttYt5bZqX0AC&pg=PA300 |page = 300 |chapter = Rubidium and crystal oscillators |title = Data network engineering |isbn = 978-0-7923-8594-3 |author1 = King, Tim |author2 = Newson, Dave |date = 1999-07-31|publisher = Springer }}</ref> Such rubidium standards are often mass-produced for the [[telecommunication]] industry.<ref>{{cite book |chapter-url = https://books.google.com/books?id=LesrjSVQMPQC&pg=PA72 |chapter = Rubidium Vapor Cell |title = Advances in electronics and electron physics |isbn = 978-0-12-014644-4 |author1 = Marton, L. |date = 1977-01-01|publisher = Academic Press }}</ref>
 
Other potential or current uses of rubidium include a working fluid in vapor turbines, as a [[getter]] in [[vacuum tube]]s, and as a [[photocell]] component.<ref>{{cite book |url = https://books.google.com/books?id=GEVt3kpFw64C&pg=PA274 |page = 274 |title = Introduction To Nuclear And Particle Physics |isbn = 978-81-203-3610-0 |author1 = Mittal |date = 2009|publisher = Prentice-Hall Of India Pvt. Limited }}</ref> Rubidium is also used as an ingredient in special types of glass, in the production of [[superoxide]] by burning in [[oxygen]], in the study of [[potassium]] [[ion channel]]s in biology, and as the vapor in atomic [[magnetometer]]s.<ref name="MAG">{{Cite journal |title=Parametric modulation of an atomic magnetometer |journal=Applied Physics Letters| volume=89| date=2006 |issue=13 |pages=23575531–23575533 |doi=10.1063/1.2357553 |last1=Li |first1=Zhimin |last2=Wakai |first2=Ronald T. |last3=Walker |first3=Thad G. |bibcode = 2006ApPhL..89m4105L |pmc=3431608 |pmid=22942436}}</ref> In particular, <sup>87</sup>Rb is used with other alkali metals in the development of spin-exchange relaxation-free [[SERF|(SERF) magnetometers]].<ref name="MAG" />
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[[Category:Reducing agents]]
[[Category:Chemical elements with body-centered cubic structure]]
[[Category:Pyrophoric materials]]