Isotopes of lithium - wikipedia Isotopes of lithium Main isotopes of lithium Isotope Decay abundance half - life ( t ) mode product Li 7.59 % stable Li 92.41 % stable Li content may be as low as 3.75 % in natural samples. Li would therefore have a content of up to 96.25 %. Standard atomic weight ( A ) ( 6.938, 6.997 ) Conventional : 6.94 view talk Naturally occurring lithium ( Li ) is composed of two stable isotopes, lithium - 6 and lithium - 7, with the latter being far more abundant : about 92.5 percent of the atoms. Both of the natural isotopes have an unexpectedly low nuclear binding energy per nucleon ( ~ 5.3 MeV ) when compared with the adjacent lighter and heavier elements, helium ( ~ 7.1 MeV ) and beryllium ( ~ 6.5 MeV ). The longest - lived radioisotope of lithium is lithium - 8, which has a half - life of just 838 milliseconds. Lithium - 9 has a half - life of 178 milliseconds, and lithium - 11 has a half - life of about 8.6 milliseconds. All of the remaining isotopes of lithium have half - lives that are shorter than 10 nanoseconds. The shortest - lived known isotope of lithium is lithium - 4, which decays by proton emission with a half - life of about 6977909999999999999 ♠ 9.1 × 10 seconds, although the half - life of lithium - 3 is yet to be determined, and is likely to be much shorter, like helium - 2 ( diproton ) which undergoes proton decay within 6991100000000000000 ♠ 10 s. Lithium - 7 and lithium - 6 are two of the primordial nuclides that were produced in the Big Bang, with lithium - 7 to be 10 of all primordial nuclides and amount of lithium - 6 around 10. A small percentage of lithium - 6 is also known to be produced by nuclear reactions in certain stars. The isotopes of lithium separate somewhat during a variety of geological processes, including mineral formation ( chemical precipitation and ion exchange ). Lithium ions replace magnesium or iron in certain octahedral locations in clays, and lithium - 6 is sometimes preferred over lithium - 7. This results in some enrichment of lithium - 7 in geological processes. Lithium - 6 is an important isotope in nuclear physics because when it is bombarded with neutrons, tritium is produced. A chart showing the abundances of the naturally - occurring isotopes of lithium. Contents 1 Isotope separation 1.1 Colex separation 1.2 Vacuum distillation 2 Lithium - 4 3 Lithium - 6 4 Lithium - 7 5 Lithium - 11 6 Lithium - 12 7 List of isotopes 7.1 Notes 8 Decay chains 9 See also 10 References 11 External links Isotope separation Colex separation Main article : COLEX process ( isotopic separation ) Lithium - 6 has a greater affinity than lithium - 7 for the element mercury. When an amalgam of lithium and mercury is added to solutions containing lithium hydroxide, the lithium - 6 becomes more concentrated in the amalgam and the lithium - 7 more in the hydroxide solution. The colex ( column exchange ) separation method makes use of this by passing a counter-flow of amalgam and hydroxide through a cascade of stages. The fraction of lithium - 6 is preferentially drained by the mercury, but the lithium - 7 flows mostly with the hydroxide. At the bottom of the column, the lithium ( enriched with lithium - 6 ) is separated from the amalgam, and the mercury is recovered to be reused with fresh raw material. At the top, the lithium hydroxide solution is electrolyzed to liberate the lithium - 7 fraction. The enrichment obtained with this method varies with the column length and the flow speed. Vacuum distillation Lithium is heated to a temperature of about 550 ° C in a vacuum. Lithium atoms evaporate from the liquid surface and are collected on a cold surface positioned a few centimetres above the liquid surface. Since lithium - 6 atoms have a greater mean free path, they are collected preferentially. The theoretical separation efficiency is about 8.0 percent. A multistage process may be used to obtain higher degrees of separation. Lithium - 4 Lithium - 4 contains three protons and one neutron. It is the shortest - lived known isotope of lithium, with a half - life of about 91 yoctoseconds, 6977909999999999999 ♠ 9.1 × 10 seconds and decays by proton emission to helium - 3. Lithium - 4 can be formed as an intermediate in some nuclear fusion reactions. Lithium - 6 Lithium - 6 is valuable as the source material for the production of tritium ( hydrogen - 3 ) and as an absorber of neutrons in nuclear fusion reactions. Natural lithium contains about 7.5 percent lithium - 6, with the rest being lithium - 7. Large amounts of lithium - 6 have been separated out for placing into hydrogen bombs. The separation of lithium - 6 has by now ceased in the large thermonuclear powers, but stockpiles of it remain in these countries. Lithium - 6 is one of only three stable isotopes with a spin of 1 and has the smallest nonzero nuclear electric quadrupole moment of any stable nucleus. Lithium - 7 Lithium - 7 is by far the most - common isotope, making up about 92.5 percent of all natural lithium. A lithium - 7 atom contains three protons, four neutrons, and three electrons. Because of its nuclear properties lithium - 7 is less common than helium, beryllium, carbon, nitrogen, or oxygen in the Universe, even though the latter four all have heavier nuclei. The industrial production of lithium - 6 results in a waste product which is enriched in lithium - 7 and depleted in lithium - 6. This material has been sold commercially, and some of it has been released into the environment. A relative abundance of lithium - 7, as high as 35 percent greater than the natural value, has been measured in the ground water in a carbonate aquifer underneath the West Valley Creek in Pennsylvania, which is downstream from a lithium processing plant. In the depleted lithium, the relative abundance of lithium - 6 can be reduced to as little as 20 percent of its nominal value, giving an atomic mass for the discharged lithium that can range from about 6.94 Da to about 7.00 Da. Hence the isotopic composition of lithium can vary somewhat depending on its source. An accurate atomic mass for samples of lithium can not be measured for all sources of lithium. Lithium - 7 is used as a part of the molten lithium fluoride in molten salt reactors : liquid - fluoride nuclear reactors. The large neutron - absorption cross-section of lithium - 6 ( about 940 barns ) as compared with the very small neutron cross-section of lithium - 7 ( about 45 millibarns ) makes high separation of lithium - 7 from natural lithium a strong requirement for the possible use in lithium fluoride reactors. Lithium - 7 hydroxide is used for alkalizing of the coolant in pressurized water reactors. Some lithium - 7 has been produced, for a few picoseconds, which contains a lambda particle in its nucleus, whereas an atomic nucleus is generally thought to contain only neutrons, protons, and pions. Lithium - 11 Lithium - 11 is thought to possess a halo nucleus consisting of a core of three protons and eight neutrons, two of which are in a nuclear halo. It has an exceptionally large cross-section of 3.16 fm, comparable to that of Pb. It decays by beta emission to Be, which then decays in several ways ( see table below ). Lithium - 12 Lithium - 12 has a considerably shorter half - life of around 10 nanoseconds. It decays by neutron emission into Li, which decays as mentioned above. List of isotopes nuclide symbol Z ( p ) N ( n ) isotopic mass ( u ) half - life decay mode ( s ) daughter isotope ( s ) nuclear spin representative isotopic composition ( mole fraction ) range of natural variation ( mole fraction ) excitation energy Li 7000402719000000000 ♠ 4.027 19 ( 23 ) 6977909999999999999 ♠ 91 ( 9 ) × 10 s ( 6987966112421661000 ♠ 6.03 MeV ) p He 5 Li 7000501254000000000 ♠ 5.012 54 ( 5 ) 6978370000000000000 ♠ 370 ( 30 ) × 10 s ( ~ 6987240326473050000 ♠ 1.5 MeV ) p He 3 / 2 − 6 Li 7000601512279500000 ♠ 6.015 122 795 ( 16 ) Stable 1 + ( 6998759000000000000 ♠ 0.0759 ( 4 ) ) 6998722500000000000 ♠ 0.072 25 -- 6998771400000000000 ♠ 0.077 14 7 Li 7000701600343660000 ♠ 7.016 003 4366 ( 45 ) Stable 3 / 2 − ( 6999924100000000000 ♠ 0.9241 ( 4 ) ) 6999922750000000000 ♠ 0.922 75 -- 6999927860000000000 ♠ 0.927 86 8 Li 5 7000802248736000000 ♠ 8.022 487 36 ( 10 ) 6999840299999999999 ♠ 840.3 ( 9 ) ms β 8 Be 2 + 9 Li 6 7000902678950000000 ♠ 9.026 7895 ( 21 ) 6999178300000000000 ♠ 178.3 ( 4 ) ms β, n ( 50.8 % ) 8 Be 3 / 2 − β ( 49.2 % ) 9 Be 10 Li 7 7001100354810000000 ♠ 10.035 481 ( 16 ) 6979199999999999999 ♠ 2.0 ( 5 ) × 10 s ( 6987192261178440000 ♠ 1.2 ( 3 ) MeV ) n 9 Li ( 1 −, 2 − ) 10m1 Li 6986320435297400000 ♠ 200 ( 40 ) keV 6979370000000000000 ♠ 3.7 ( 15 ) × 10 s 1 + 10m2 Li 6986769044713760000 ♠ 480 ( 40 ) keV 6979135000000000000 ♠ 1.35 ( 24 ) × 10 s 2 + 11 Li 8 7001110437980000000 ♠ 11.043 798 ( 21 ) 6997875000000000000 ♠ 8.75 ( 14 ) ms β, n ( 84.9 % ) 10 Be 3 / 2 − β ( 8.07 % ) 11 Be β, 2n ( 4.1 % ) 9 Be β, 3n ( 1.9 % ) 8 Be β, α ( 1.0 % ) 7 He, 4 He β, fission (. 014 % ) 8 Li, 3 β, fission (. 013 % ) 9 Li, 2 12 Li 9 7001120537800000000 ♠ 12.053 78 ( 107 ) # < 6992100000000000000 ♠ 10 ns n 11 Li Jump up ^ The other two are deuterium and nitrogen - 14. Jump up ^ Bold for stable isotopes Jump up ^ One of the few stable odd - odd nuclei Jump up ^ Produced in Big Bang nucleosynthesis and by cosmic ray spallation Jump up ^ Immediately decays into two He atoms for a net reaction of Li → 2 He + e Jump up ^ Immediately decays into two He atoms for a net reaction of Li → 2 He + n + e Jump up ^ Has 2 halo neutrons Jump up ^ Immediately decays into two He atoms for a net reaction of Li → 2 He + 3 n + e Notes The precision of the abundance of isotopes of lithium and the overall atomic weight is limited through variations. The given ranges should be applicable to any normal terrestrial material. Exceptional samples of lithium from geology are known in which the isotopic composition lies outside the reported range. The uncertainty in the atomic mass might exceed the stated value for such samples. Commercially available samples of lithium may have been subjected to the undisclosed or inadvertent separation of the isotopes. Substantial deviations from the given atomic mass and isotopic composition can be found. In depleted lithium ( with the Li removed ), the relative abundance of lithium - 6 can be reduced to as little as 20 percent of its normal value, giving the measured atomic mass ranging from 6.94 Da to 7.00 Da. The values marked with # are not purely from experimental data, but they are partly or totally estimated from the general trends. The values of spin with weak assignment arguments are enclosed in parentheses. Uncertainties are given in concise form in parentheses after the corresponding last digits. Uncertainty values denote one standard deviation from the norm, except for the isotopic compositions and standard atomic masses from the IUPAC that use larger uncertainties. The unusual isotope lithium - 11 has a nuclear halo of two weakly linked neutrons that explains the important difference in its nuclear radius. Nuclide masses are given by IUPAP Commission on Symbols, Units, Nomenclature, Atomic Masses and Fundamental Constants ( SUNAMCO ). Isotope abundances are given by IUPAC Commission on Isotopic Abundances and Atomic Weights ( CIAAW ). Decay chains While β decay into isotopes of beryllium ( often combined with single - or multiple - neutron emission ) is predominant over heavier isotopes of lithium, Li and Li decay via neutron emission into Li and Li respectively due to their positions above the neutron drip line. Lithium - 11 has also been observed to decay via multiple forms of fission. Lighter isotopes of lithium ( < Li ) are only known to decay by proton emission. The decay modes of the two isomers of Li are unknown. 3 4 L i → 91 y s 2 3 H e + 1 1 H ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 4 ) Li ( \xrightarrow ( 91 ~ ys ) ) ( ) _ ( 2 ) ^ ( 3 ) He+ ( ) _ ( 1 ) ^ ( 1 ) H ) ) 3 5 L i → 370 y s 2 4 H e + 1 1 H ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 5 ) Li ( \xrightarrow ( 370 ~ ys ) ) ( ) _ ( 2 ) ^ ( 4 ) He+ ( ) _ ( 1 ) ^ ( 1 ) H ) ) 3 8 L i → 840.3 m s 4 8 B e + e − ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 8 ) Li ( \xrightarrow ( 840.3 ~ ms ) ) ( ) _ ( 4 ) ^ ( 8 ) Be + e ( ) _ ( ) ^ ( - ) ) ) 3 9 L i → 178.3 m s 4 8 B e + 0 1 n + e − ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 9 ) Li ( \xrightarrow ( 178.3 ~ ms ) ) ( ) _ ( 4 ) ^ ( 8 ) Be+ ( ) _ ( 0 ) ^ ( 1 ) n + e ( ) _ ( ) ^ ( - ) ) ) 3 9 L i → 178.3 m s 4 9 B e + e − ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 9 ) Li ( \xrightarrow ( 178.3 ~ ms ) ) ( ) _ ( 4 ) ^ ( 9 ) Be + e ( ) _ ( ) ^ ( - ) ) ) 3 10 L i → 2 z s 3 9 L i + 0 1 n ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 10 ) Li ( \xrightarrow ( 2 ~ zs ) ) ( ) _ ( 3 ) ^ ( 9 ) Li+ ( ) _ ( 0 ) ^ ( 1 ) n ) ) 3 11 L i → 8.75 m s 4 10 B e + 0 1 n + e − ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 11 ) Li ( \xrightarrow ( 8.75 ~ ms ) ) ( ) _ ( 4 ) ^ ( 10 ) Be+ ( ) _ ( 0 ) ^ ( 1 ) n + e ( ) _ ( ) ^ ( - ) ) ) 3 11 L i → 8.75 m s 4 11 B e + e − ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 11 ) Li ( \xrightarrow ( 8.75 ~ ms ) ) ( ) _ ( 4 ) ^ ( 11 ) Be + e ( ) _ ( ) ^ ( - ) ) ) 3 11 L i → 8.75 m s 4 9 B e + 2 0 1 n + e − ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 11 ) Li ( \xrightarrow ( 8.75 ~ ms ) ) ( ) _ ( 4 ) ^ ( 9 ) Be + 2 ( ) _ ( 0 ) ^ ( 1 ) n + e ( ) _ ( ) ^ ( - ) ) ) 3 11 L i → 8.75 m s 4 8 B e + 3 0 1 n + e − ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 11 ) Li ( \xrightarrow ( 8.75 ~ ms ) ) ( ) _ ( 4 ) ^ ( 8 ) Be + 3 ( ) _ ( 0 ) ^ ( 1 ) n + e ( ) _ ( ) ^ ( - ) ) ) 3 11 L i → 8.75 m s 4 7 H e + 2 4 H e + e − ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 11 ) Li ( \xrightarrow ( 8.75 ~ ms ) ) ( ) _ ( 4 ) ^ ( 7 ) He+ ( ) _ ( 2 ) ^ ( 4 ) He + e ( ) _ ( ) ^ ( - ) ) ) 3 11 L i → 8.75 m s 3 8 L i + 1 3 H + e − ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 11 ) Li ( \xrightarrow ( 8.75 ~ ms ) ) ( ) _ ( 3 ) ^ ( 8 ) Li+ ( ) _ ( 1 ) ^ ( 3 ) H + e ( ) _ ( ) ^ ( - ) ) ) 3 11 L i → 8.75 m s 3 9 L i + 1 2 H + e − ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 11 ) Li ( \xrightarrow ( 8.75 ~ ms ) ) ( ) _ ( 3 ) ^ ( 9 ) Li+ ( ) _ ( 1 ) ^ ( 2 ) H + e ( ) _ ( ) ^ ( - ) ) ) 3 12 L i → < 10 n s 3 11 L i + 0 1 n ( displaystyle mathrm ( ( ) _ ( 3 ) ^ ( 12 ) Li ( \xrightarrow ( < 10 ~ ns ) ) ( ) _ ( 3 ) ^ ( 11 ) Li+ ( ) _ ( 0 ) ^ ( 1 ) n ) ) See also COLEX process ( isotopic separation ) References Jump up ^ Meija, J. ; et al. ( 2016 ). `` Atomic weights of the elements 2013 ( IUPAC Technical Report ) ''. Pure Appl. Chem. 88 ( 3 ) : 265 -- 91. doi : 10.1515 / pac - 2015 - 0305. Jump up ^ BD Fields `` The Primordial Lithium Problem '', Annual Reviews of Nuclear and Particle Science 2011 Jump up ^ `` Isotopes of Lithium ''. Retrieved 20 October 2013. Jump up ^ Chandrakumar, N. ( 2012 ). Spin - 1 NMR. Springer Science & Business Media. p. 5. ISBN 9783642610899. Jump up ^ T.B. Coplen, J.A. Hopple, J.K. Böhlke, H.S. Peiser, S.E. Rieder, H.R. Krouse, K.J.R. Rosman, T. Ding, R.D. Vocke, Jr., K.M. Révész, A. Lamberty, P. Taylor, P. De Bièvre. `` Compilation of minimum and maximum isotope ratios of selected elements in naturally occurring terrestrial materials and reagents '', U.S. Geological Survey Water - Resources Investigations Report 01 - 4222 ( 2002 ). As quoted in T.B. Coplen ; et al. ( 2002 ). `` Isotope - Abundance Variations of Selected Elements ( IUPAC technical report ) '' ( PDF ). Pure and Applied Chemistry. 74 ( 10 ) : 1987 -- 2017. doi : 10.1351 / pac200274101987. Jump up ^ Holden, Norman E. ( January -- February 2010 ). `` The Impact of Depleted Li on the Standard Atomic Weight of Lithium ''. International Union of Pure and Applied Chemistry. Retrieved 6 May 2014. Jump up ^ Managing Critical Isotopes : Stewardship of Lithium - 7 Is Needed to Ensure a Stable Supply, GAO - 13 - 716 / / U.S. Government Accountability Office, 19 September 2013 ; pdf Jump up ^ Emsley, John ( 2001 ). Nature 's Building Blocks : An A-Z Guide to the Elements. Oxford University Press. pp. 234 -- 239. ISBN 978 - 0 - 19 - 850340 - 8. Jump up ^ Brumfiel, Geoff ( 1 March 2001 ). `` The Incredible Shrinking Nucleus ''. Physical Review Focus. 7. doi : 10.1103 / PhysRevFocus. 7.11. Jump up ^ `` Universal Nuclide Chart ''. Nucleonica. Retrieved 2012 - 09 - 27. ( Registration required ( help ) ). Isotope masses from : G. Audi ; A.H. Wapstra ; C. Thibault ; J. Blachot ; O. Bersillon ( 2003 ). `` The NUBASE evaluation of nuclear and decay properties '' ( PDF ). Nuclear Physics A. 729 : 3 -- 128. Bibcode : 2003NuPhA. 729... 3A. doi : 10.1016 / j. nuclphysa. 2003.11. 001. Archived from the original ( PDF ) on 23 September 2008. Isotopic compositions and standard atomic masses from : J.R. de Laeter ; J.K. Böhlke ; P. De Bièvre ; H. Hidaka ; H.S. Peiser ; K.J.R. Rosman ; P.D.P. Taylor ( 2003 ). `` Atomic weights of the elements. Review 2000 ( IUPAC Technical Report ) ''. Pure and Applied Chemistry. 75 ( 6 ) : 683 -- 800. doi : 10.1351 / pac200375060683. M.E. Wieser ( 2006 ). `` Atomic weights of the elements 2005 ( IUPAC Technical Report ) ''. Pure and Applied Chemistry. 78 ( 11 ) : 2051 -- 2066. doi : 10.1351 / pac200678112051. Lay summary. Half - life, spin, and isomer data selected from the following sources. See editing notes on this article 's talk page. G. Audi ; A.H. Wapstra ; C. Thibault ; J. Blachot ; O. Bersillon ( 2003 ). `` The NUBASE evaluation of nuclear and decay properties '' ( PDF ). Nuclear Physics A. 729 : 3 -- 128. Bibcode : 2003NuPhA. 729... 3A. doi : 10.1016 / j. nuclphysa. 2003.11. 001. Archived from the original ( PDF ) on 23 September 2008. National Nuclear Data Center. `` NuDat 2.1 database ''. Brookhaven National Laboratory. Retrieved 23 February 2017. N.E. Holden ( 2004 ). `` Table of the Isotopes ''. In D.R. Lide. CRC Handbook of Chemistry and Physics ( 85th ed. ). CRC Press. Section 11. ISBN 978 - 0 - 8493 - 0485 - 9. External links Lewis, G.N. ; MacDonald, R.T. ( 1936 ). `` The Separation of Lithium Isotopes ''. Journal of the American Chemical Society. 58 ( 12 ) : 2519 -- 2524. doi : 10.1021 / ja01303a045. Isotopes of helium Isotopes of lithium Isotopes of beryllium Table of nuclides Isotopes of the chemical elements He Li Be 5 6 7 8 9 10 Ne 11 Na 12 Mg 13 Al 14 Si 15 16 17 Cl 18 Ar 19 20 Ca 21 Sc 22 Ti 23 V 24 Cr 25 Mn 26 Fe 27 Co 28 Ni 29 Cu 30 Zn 31 Ga 32 Ge 33 As 34 Se 35 Br 36 Kr 37 Rb 38 Sr 39 Y 40 Zr 41 Nb 42 Mo 43 Tc 44 Ru 45 Rh 46 Pd 47 Ag 48 Cd 49 In 50 Sn 51 Sb 52 Te 53 54 Xe 55 Cs 56 Ba 57 La 72 Hf 73 Ta 74 75 Re 76 Os 77 Ir 78 Pt 79 Au 80 Hg 81 Tl 82 Pb 83 Bi 84 Po 85 At 86 Rn 87 Fr 88 Ra 89 Ac 104 Rf 105 Db 106 Sg 107 Bh 108 Hs 109 Mt 110 Ds 111 Rg 112 Cn 113 Nh 114 Fl 115 Mc 116 Lv 117 Ts 118 Og 58 Ce 59 Pr 60 Nd 61 Pm 62 Sm 63 Eu 64 Gd 65 Tb 66 Dy 67 Ho 68 Er 69 Tm 70 Yb 71 Lu 90 Th 91 Pa 92 U 93 Np 94 Pu 95 Am 96 Cm 97 Bk 98 Cf 99 Es 100 Fm 101 Md 102 No 103 Lr Table of nuclides Categories : Isotopes Tables of nuclides Metastable isotopes Isotopes by element Retrieved from `` https://en.wikipedia.org/w/index.php?title=Isotopes_of_lithium&oldid=815100556 '' Categories : Lithium Isotopes of lithium Lists of isotopes by element Hidden categories : Pages with login required references or sources Use dmy dates from August 2013 Wikipedia articles needing clarification from November 2013 Talk Contents About Wikipedia Català Чӑвашла Čeština Español Esperanto فارسی Français 한국어 Italiano Magyar Nederlands 日本 語 Русский Svenska Українська Tiếng Việt 粵語 中文 Edit links This page was last edited on 12 December 2017, at 19 : 45. 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Question: how many protons are in a lithium nucleus
Answer: three