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'{{Short description|Different atoms of the same element}} {{About|the atomic variants of chemical elements|other uses|Isotope (disambiguation)}} {{pp-move-indef}} {{Nuclear physics|cTopic=Nuclides' classification}} [[File:Hydrogen Deuterium Tritium Nuclei Schmatic-en.svg|thumb|300px|The three naturally occurring [[isotopes of hydrogen]]. The fact that each isotope has one proton makes them all variants of [[hydrogen]]: the identity of the isotope is given by the number of protons and neutrons. From left to right, the isotopes are [[hydrogen|protium]] (¹H) with zero neutrons, [[deuterium]] (²H) with one neutron, and [[tritium]] (³H) with two neutrons.]] '''Isotopes''' are two or more types of atoms that have the same [[atomic number]] (number of [[protons]] in their [[Atomic nucleus|nuclei]]) and position in the [[periodic table]] (and hence belong to the same [[chemical element]]), and that differ in [[nucleon]] numbers ([[mass number]]s) due to different numbers of [[neutron]]s in their nuclei. While all isotopes of a given element have almost the same chemical properties, they have different atomic masses and physical properties.<ref>{{cite web | title = Isotope | publisher = Encyclopedia Britannica | url = https://www.britannica.com/science/isotope|first = Gregory F. |last = Herzog|date = 2 June 2020}}</ref> The term isotope is formed from the Greek roots isos ([[wikt:ἴσος|ἴσος]] "equal") and topos ([[wikt:τόπος|τόπος]] "place"), meaning "the same place"; thus, the meaning behind the name is that different isotopes of a single element occupy the same position on the [[periodic table]].<ref>{{cite web |url=https://www.nobelprize.org/uploads/2018/06/soddy-lecture.pdf |title=The origins of the conceptions of isotopes |last=Soddy |first=Frederick |date=12 December 1922 |website=Nobelprize.org |page=393 |access-date=9 January 2019 |quote=Thus the chemically identical elements - or isotopes, as I called them for the first time in this letter to Nature, because they occupy the same place in the Periodic Table ...}}</ref> It was coined by Scottish doctor and writer [[Margaret Todd (doctor)|Margaret Todd]] in 1913 in a suggestion to the British chemist [[Frederick Soddy]].<ref>{{Cite web|title=isotope—Origin and meaning|url=https://www.etymonline.com/word/isotope|url-status=live|access-date=21 October 2021|website=www.etymonline.com|language=en}}</ref> The number of protons within the [[atomic nucleus|atom's nucleus]] is called its [[atomic number]] and is equal to the number of [[electron]]s in the neutral (non-ionized) atom. Each atomic number identifies a specific element, but not the isotope; an atom of a given element may have a wide range in its number of [[neutron]]s. The number of [[nucleon]]s (both protons and neutrons) in the nucleus is the atom's [[mass number]], and each isotope of a given element has a different mass number. For example, [[carbon-12]], [[carbon-13]], and [[carbon-14]] are three isotopes of the element [[carbon]] with mass numbers 12, 13, and 14, respectively. The atomic number of carbon is 6, which means that every carbon atom has 6 protons so that the neutron numbers of these isotopes are 6, 7, and 8 respectively. == Isotope vs. nuclide == A [[nuclide]] is a species of an atom with a specific number of protons and neutrons in the nucleus, for example carbon-13 with 6 protons and 7 neutrons. The ''nuclide'' concept (referring to individual nuclear species) emphasizes nuclear properties over chemical properties, whereas the ''isotope'' concept (grouping all atoms of each element) emphasizes [[chemistry|chemical]] over nuclear. The neutron number has large effects on nuclear properties, but its effect on chemical properties is negligible for most elements. Even for the lightest elements, whose ratio of neutron number to atomic number varies the most between isotopes, it usually has only a small effect although it matters in some circumstances (for hydrogen, the lightest element, the isotope effect is large enough to affect biology strongly). The term ''isotopes'' (originally also ''isotopic elements'',<ref>{{cite journal|author=Soddy, Frederick |year=1913|url=http://www.nature.com/physics/looking-back/soddy/index.html |title=Intra-atomic charge|journal=Nature|volume=92|pages=399–400|doi=10.1038/092399c0|issue=2301|bibcode = 1913Natur..92..399S |s2cid=3965303}}</ref> now sometimes ''isotopic nuclides''<ref>{{Cite web |url=http://iupap.org/wp-content/uploads/2014/05/A4.pdf |title=IUPAP Red Book |access-date=2018-01-06 |archive-date=2015-03-18 |archive-url=https://web.archive.org/web/20150318052346/http://iupap.org/wp-content/uploads/2014/05/A4.pdf |url-status=dead }}</ref>) is intended to imply comparison (like ''[[synonym]]s'' or ''[[isomer]]s''). For example, the nuclides {{nuclide|C|12}}, {{nuclide|C|13}}, {{nuclide|C|14}} are isotopes (nuclides with the same atomic number but different mass numbers<ref>[http://goldbook.iupac.org/html/I/I03331.html IUPAC Gold Book]</ref>), but {{nuclide|Ar|40}}, {{nuclide|K|40}}, {{nuclide|Ca|40}} are [[isobar (nuclide)|isobars]] (nuclides with the same mass number<ref>[http://goldbook.iupac.org/html/I/I03263.html IUPAC Gold Book]</ref>). However, ''isotope'' is the older term and so is better known than ''nuclide'' and is still sometimes used in contexts in which ''nuclide'' might be more appropriate, such as [[nuclear technology]] and [[nuclear medicine]]. == Notation == An isotope and/or nuclide is specified by the name of the particular element (this indicates the atomic number) followed by a hyphen and the mass number (e.g. [[helium-3]], [[helium-4]], [[carbon-12]], [[carbon-14]], [[uranium-235]] and [[uranium-239]]).<ref>[[IUPAC]] (Connelly, N. G.; Damhus, T.; Hartshorn, R. M.; and Hutton, A. T.), [http://old.iupac.org/publications/books/rbook/Red_Book_2005.pdf ''Nomenclature of Inorganic Chemistry – IUPAC Recommendations 2005''], The Royal Society of Chemistry, 2005; IUPAC (McCleverty, J. A.; and Connelly, N. G.), ''Nomenclature of Inorganic Chemistry II. Recommendations 2000'', The Royal Society of Chemistry, 2001; IUPAC (Leigh, G. J.), ''Nomenclature of Inorganic Chemistry (recommendations 1990)'', Blackwell Science, 1990; IUPAC, [http://pac.iupac.org/publications/pac/pdf/1971/pdf/2801x0001.pdf ''Nomenclature of Inorganic Chemistry, Second Edition''], 1970; probably in the 1958 first edition as well</ref> When a [[chemical symbol]] is used, e.g. "C" for carbon, standard notation (now known as "AZE notation" because ''A'' is the [[mass number]], ''Z'' the [[atomic number]], and E for [[chemical element|element]]) is to indicate the mass number (number of nucleons) with a [[superscript]] at the upper left of the chemical symbol and to indicate the atomic number with a [[subscript]] at the lower left (e.g. {{nuclide|He|3}}, {{nuclide|He|4}}, {{nuclide|C|12}}, {{nuclide|C|14}}, {{nuclide|U|235}}, and {{nuclide|U|239}}).<ref>This notation seems to have been introduced in the second half of the 1930s. Before that, various notations were used, such as [https://books.google.com/books?id=jkMcAQAAIAAJ&q=isotope Ne(22) for neon-22 (1934)], [https://books.google.com/books?id=7KQOAAAAIAAJ&q=neon-22+Ne22 Ne²² for neon-22 (1935)], or even [https://books.google.com/books?id=HD7OAAAAMAAJ&q=isotope Pb₂₁₀ for lead-210 (1933)].</ref> Because the atomic number is given by the element symbol, it is common to state only the mass number in the superscript and leave out the atomic number subscript (e.g. {{SimpleNuclide|He|3}}, {{SimpleNuclide|He|4}}, {{SimpleNuclide|C|12}}, {{SimpleNuclide|C|14}}, {{SimpleNuclide|U|235}}, and {{SimpleNuclide|U|239}}). The letter ''m'' is sometimes appended after the mass number to indicate a [[nuclear isomer]], a [[metastable]] or energetically excited nuclear state (as opposed to the lowest-energy [[ground state]]), for example {{nuclide|Tantalum|180|m}} ([[tantalum-180m]]). The common pronunciation of the AZE notation is different from how it is written: {{nuclide|He|4}} is commonly pronounced as helium-four instead of four-two-helium, and {{nuclide|U|235}} as uranium two-thirty-five (American English) or uranium-two-three-five (British) instead of 235-92-uranium. == Radioactive, primordial, and stable isotopes == Some isotopes/nuclides are [[radioactive]], and are therefore referred to as radioisotopes or [[radionuclide]]s, whereas others have never been observed to decay radioactively and are referred to as stable isotopes or [[stable nuclide]]s. For example, {{SimpleNuclide|C|14}} is a radioactive form of carbon, whereas {{SimpleNuclide|C|12}} and {{SimpleNuclide|C|13}} are stable isotopes. There are about 339 naturally i fucking horny right now help me daddy ////ah/aoccurring nuclides on Earth,<ref name="lindsay">{{cite web|url=http://www.don-lindsay-archive.org/creation/isotope_list.html|title=Radioactives Missing From The Earth}}</ref> of which 286 are [[primordial nuclide]]s, meaning that they have existed since the [[Solar System]]'s formation. Primordial nuclides include 35 nuclides with very long [[Half-life|half-lives]] (over 100&nbsp;million years) and 251 that are formally considered as "[[stable nuclide]]s",<ref name="lindsay" /> because they have not been observed to decay. In most cases, for obvious reasons, if an element has stable isotopes, those isotopes predominate in the elemental abundance found on Earth and in the Solar System. However, in the cases of three elements ([[tellurium]], [[indium]], and [[rhenium]]) the most abundant isotope found in nature is actually one (or two) extremely long-lived radioisotope(s) of the element, despite these elements having one or more stable isotopes. Theory predicts that many apparently "stable" isotopes/nuclides are radioactive, with extremely long half-lives (discounting the possibility of [[proton decay]], which would make all nuclides ultimately unstable). Some stable nuclides are in theory energetically susceptible to other known forms of decay, such as alpha decay or double beta decay, but no decay products have yet been observed, and so these isotopes are said to be "observationally stable". The predicted half-lives for these nuclides often greatly exceed the estimated age of the universe, and in fact, there are also 31 known radionuclides (see [[primordial nuclide]]) with half-lives longer than the age of the universe. Adding in the radioactive nuclides that have been created artificially, there are [[List of nuclides|3,339 currently known nuclides]].<ref>{{cite web|url=http://www.nndc.bnl.gov/nudat2/help/index.jsp|title=NuDat 2 Description|access-date=2 January 2016}}</ref> These include 905 nuclides that are either stable or have half-lives longer than 60 minutes. See [[list of nuclides]] for details. == History == === Radioactive isotopes === The existence of isotopes was first suggested in 1913 by the [[radiochemistry|radiochemist]] [[Frederick Soddy]], based on studies of radioactive [[decay chain]]s that indicated about 40 different species referred to as ''radioelements'' (i.e. radioactive elements) between uranium and lead, although the periodic table only allowed for 11 elements between lead and uranium inclusive.<ref>Choppin, G.; Liljenzin, J. O. and Rydberg, J.　（1995） ''Radiochemistry and Nuclear Chemistry'' (2nd ed.) Butterworth-Heinemann, pp. 3–5</ref><ref>Others had also suggested the possibility of isotopes; for example: * Strömholm, Daniel and Svedberg, Theodor (1909) "Untersuchungen über die Chemie der radioactiven Grundstoffe II." (Investigations into the chemistry of the radioactive elements, part 2), ''Zeitschrift für anorganischen Chemie'', '''63''': 197–206; see especially page 206. * Alexander Thomas Cameron, ''Radiochemistry'' (London, England: J. M. Dent & Sons, 1910), p. 141. (Cameron also anticipated the displacement law.)</ref><ref name="ley196610">{{Cite magazine |last=Ley |first=Willy |date=October 1966 |title=The Delayed Discovery |department=For Your Information |url=https://archive.org/stream/Galaxy_v25n01_1966-10#page/n115/mode/2up |magazine=Galaxy Science Fiction |pages=116–127 }}</ref> Several attempts to separate these new radioelements chemically had failed.<ref name=Scerri>Scerri, Eric R. (2007) ''The Periodic Table'' Oxford University Press, pp. 176–179 {{ISBN|0-19-530573-6}}</ref> For example, Soddy had shown in 1910 that [[mesothorium]] (later shown to be ²²⁸Ra), [[radium]] (²²⁶Ra, the longest-lived isotope), and [[isotopes of radium|thorium X]] (²²⁴Ra) are impossible to separate.<ref name=Nagel /> Attempts to place the radioelements in the periodic table led Soddy and [[Kazimierz Fajans]] independently to propose their [[Radioactive displacement law of Fajans and Soddy|radioactive displacement law]] in 1913, to the effect that [[alpha decay]] produced an element two places to the left in the periodic table, whereas [[beta decay]] emission produced an element one place to the right.<ref>Kasimir Fajans (1913) "Über eine Beziehung zwischen der Art einer radioaktiven Umwandlung und dem elektrochemischen Verhalten der betreffenden Radioelemente" (On a relation between the type of radioactive transformation and the electrochemical behavior of the relevant radioactive elements), ''Physikalische Zeitschrift'', '''14''': 131–136.</ref><ref>Soddy announced his "displacement law" in: {{cite journal|doi=10.1038/091057a0|title=The Radio-Elements and the Periodic Law|year=1913|last1=Soddy|first1=Frederick|journal=Nature|volume=91|issue=2264|pages=57–58|bibcode = 1913Natur..91...57S |s2cid=3975657|url=https://zenodo.org/record/1429562}}.</ref><ref>Soddy elaborated his displacement law in: Soddy, Frederick (1913) "Radioactivity," ''Chemical Society Annual Report'', '''10''': 262–288.</ref><ref>Alexander Smith Russell (1888–1972) also published a displacement law: Russell, Alexander S. (1913) "The periodic system and the radio-elements," ''Chemical News and Journal of Industrial Science'', '''107''': 49–52.</ref> Soddy recognized that emission of an alpha particle followed by two beta particles led to the formation of an element chemically identical to the initial element but with a mass four units lighter and with different radioactive properties. Soddy proposed that several types of atoms (differing in radioactive properties) could occupy the same place in the table.{{r|ley196610}} For example, the alpha-decay of uranium-235 forms thorium-231, whereas the beta decay of actinium-230 forms thorium-230.<ref name=Scerri /> The term "isotope", Greek for "at the same place",{{r|ley196610}} was suggested to Soddy by [[Margaret Todd (doctor)|Margaret Todd]], a Scottish physician and family friend, during a conversation in which he explained his ideas to her.<ref name=Nagel>{{cite journal|author=Nagel, Miriam C.|title=Frederick Soddy: From Alchemy to Isotopes|journal=Journal of Chemical Education|year=1982|volume=59|pages=739–740|doi=10.1021/ed059p739|issue=9|bibcode = 1982JChEd..59..739N }}</ref><ref>Soddy first used the word "isotope" in: {{cite journal|author=Soddy, Frederick |year=1913|url=http://www.nature.com/physics/looking-back/soddy/index.html |title=Intra-atomic charge|journal=Nature|volume=92|pages=399–400|doi=10.1038/092399c0|issue=2301|bibcode = 1913Natur..92..399S |s2cid=3965303}}</ref><ref>{{cite journal|author=Fleck, Alexander |year=1957|title=Frederick Soddy|journal=Biographical Memoirs of Fellows of the Royal Society|volume=3|pages=203–216|quote=p. 208: Up to 1913 we used the phrase 'radio elements chemically non-separable' and at that time the word isotope was suggested in a drawing-room discussion with Dr. Margaret Todd in the home of Soddy's father-in-law, Sir [[George Beilby]].|doi=10.1098/rsbm.1957.0014|doi-access=free}}</ref><ref name="pmid16134128">{{cite journal |vauthors=Budzikiewicz H, Grigsby RD|title=Mass spectrometry and isotopes: a century of research and discussion |journal=Mass Spectrometry Reviews |volume=25 |issue=1 |pages=146–57 |year=2006 |pmid=16134128 |doi=10.1002/mas.20061|bibcode=2006MSRv...25..146B }}</ref><ref>Scerri, Eric R. (2007) ''The Periodic Table'', Oxford University Press, {{ISBN|0-19-530573-6}}, Ch. 6, note 44 (p. 312) citing [[Alexander Fleck]], described as a former student of Soddy's.</ref><ref>In his 1893 book, William T. Preyer also used the word "isotope" to denote similarities among elements. From [https://books.google.com/books?id=8zDsAAAAMAAJ&pg=PA9 p. 9] of William T. Preyer, ''Das genetische System der chemischen Elemente'' [The genetic system of the chemical elements] (Berlin, Germany: R. Friedländer & Sohn, 1893): "Die ersteren habe ich der Kürze wegen isotope Elemente genannt, weil sie in jedem der sieben Stämmme der gleichen Ort, nämlich dieselbe Stuffe, einnehmen." (For the sake of brevity, I have named the former "isotopic" elements, because they occupy the same place in each of the seven families [i.e., columns of the periodic table], namely the same step [i.e., row of the periodic table].)</ref> He received the 1921 [[Nobel Prize in Chemistry]] in part for his work on isotopes.{{r|soddynobel}} [[File:Discovery of neon isotopes.JPG|frame|right|In the bottom right corner of [[J. J. Thomson]]'s photographic plate are the separate impact marks for the two isotopes of [[neon]]: neon-20 and neon-22.]] In 1914 [[Theodore William Richards|T. W. Richards]] found variations between the atomic weight of lead from different mineral sources, attributable to variations in isotopic composition due to different radioactive origins.<ref name=Scerri /><ref name=soddynobel>[https://www.nobelprize.org/nobel_prizes/chemistry/laureates/1921/soddy-lecture.html The origins of the conceptions of isotopes] Frederick Soddy, Nobel prize lecture</ref> === Stable isotopes === The first evidence for multiple isotopes of a stable (non-radioactive) element was found by [[J. J. Thomson]] in 1912 as part of his exploration into the composition of [[canal rays]] (positive ions).<ref>{{cite journal|doi=10.1080/14786440808637325|title=XIX. Further experiments on positive rays|year=1912|last1=Thomson|first1=J. J.|journal=Philosophical Magazine |series=Series 6|volume=24|issue=140|pages=209–253|url=https://zenodo.org/record/1430842}}</ref><ref>{{cite journal|doi=10.1080/14786441008636962|url=https://archive.org/details/RaysOfPositiveElectricity|title=LXXXIII. Rays of positive electricity|year=1910|last1=Thomson|first1=J. J.|journal=Philosophical Magazine |series=Series 6|volume=20|issue=118|pages=752–767}}</ref> Thomson channelled streams of [[neon]] ions through parallel magnetic and electric fields, measured their deflection by placing a photographic plate in their path, and computed their mass to charge ratio using a method that became known as the Thomson's parabola method. Each stream created a glowing patch on the plate at the point it struck. Thomson observed two separate parabolic patches of light on the photographic plate (see image), which suggested two species of nuclei with different mass to charge ratios. [[Francis William Aston|F. W. Aston]] subsequently discovered multiple stable isotopes for numerous elements using a [[mass spectrograph]]. In 1919 Aston studied neon with sufficient [[Resolution (mass spectrometry)|resolution]] to show that the two isotopic masses are very close to the integers 20 and 22 and that neither is equal to the known molar mass (20.2) of neon gas. This is an example of Aston's [[whole number rule]] for isotopic masses, which states that large deviations of elemental molar masses from integers are primarily due to the fact that the element is a mixture of isotopes. Aston similarly showed in 1920 that the molar mass of [[chlorine]] (35.45) is a weighted average of the almost integral masses for the two isotopes ³⁵Cl and ³⁷Cl.<ref>{{cite journal |doi=10.1038/105617a0 |title=Isotopes and Atomic Weights |year=1920 |last1=Aston |first1=F. W. |journal=Nature |volume=105 |issue=2646 |pages=617–619 |s2cid=4267919 |url=https://zenodo.org/record/1531300 }}</ref><ref>[https://www.nobelprize.org/nobel_prizes/chemistry/laureates/1922/aston-lecture.html Mass spectra and isotopes] Francis W. Aston, Nobel prize lecture 1922</ref> == Variation in properties between isotopes == === Chemical and molecular properties === A neutral atom has the same number of electrons as protons. Thus different isotopes of a given element all have the same number of electrons and share a similar electronic structure. Because the chemical behavior of an atom is largely determined by its electronic structure, different isotopes exhibit nearly identical chemical behavior. The main exception to this is the [[kinetic isotope effect]]: due to their larger masses, heavier isotopes tend to react somewhat more slowly than lighter isotopes of the same element. This is most pronounced by far for [[hydrogen-1|protium]] ({{SimpleNuclide|H|1}}), [[deuterium]] ({{SimpleNuclide|H|2}}), and [[tritium]] ({{SimpleNuclide|H|3}}), because deuterium has twice the mass of protium and tritium has three times the mass of protium.<ref>{{Cite book |last=Laidler |first=Keith |title=Chemical Kinetics |publisher=Pearson Education |year=1987 |isbn=978-81-317-0972-6 |edition=3rd |location=India |pages=427 |language=English}}</ref> These mass differences also affect the behavior of their respective chemical bonds, by changing the center of gravity ([[reduced mass]]) of the atomic systems. However, for heavier elements, the relative mass difference between isotopes is much less so that the mass-difference effects on chemistry are usually negligible. (Heavy elements also have relatively more neutrons than lighter elements, so the ratio of the nuclear mass to the collective electronic mass is slightly greater.) There is also an [[Equilibrium constant#Effect of isotopic substitution|equilibrium isotope effect]]. [[File:Isotopes and half-life.svg|right|thumb|Isotope half-lives. ''Z'' = number of protons. ''N'' = number of neutrons. The plot for stable isotopes diverges from the line ''Z'' = ''N'' as the element number ''Z'' becomes larger|346x346px]] Similarly, two [[molecules]] that differ only in the isotopes of their atoms ([[isotopologue]]s) have identical electronic structures, and therefore almost indistinguishable physical and chemical properties (again with deuterium and tritium being the primary exceptions). The ''vibrational modes'' of a molecule are determined by its shape and by the masses of its constituent atoms; so different isotopologues have different sets of vibrational modes. Because vibrational modes allow a molecule to absorb [[photon]]s of corresponding energies, isotopologues have different optical properties in the [[infrared]] range. === Nuclear properties and stability === {{See also|Stable nuclide|Stable isotope ratio|List of nuclides|List of elements by stability of isotopes}} Atomic nuclei consist of protons and neutrons bound together by the [[residual strong force]]. Because protons are positively charged, they repel each other. Neutrons, which are electrically neutral, stabilize the nucleus in two ways. Their copresence pushes protons slightly apart, reducing the electrostatic repulsion between the protons, and they exert the attractive nuclear force on each other and on protons. For this reason, one or more neutrons are necessary for two or more protons to bind into a nucleus. As the number of protons increases, so does the ratio of neutrons to protons necessary to ensure a stable nucleus (see graph at right). For example, although the neutron:proton ratio of {{nuclide|He|3|link=yes}} is 1:2, the neutron:proton ratio of {{nuclide|U|238}} is greater than 3:2. A number of lighter elements have stable nuclides with the ratio 1:1 (''Z'' = ''N''). The nuclide {{nuclide|Ca|40}} (calcium-40) is observationally the heaviest stable nuclide with the same number of neutrons and protons. All stable nuclides heavier than calcium-40 contain more neutrons than protons. === Numbers of isotopes per element === Of the 80 elements with a stable isotope, the largest number of stable isotopes observed for any element is ten (for the element [[tin]]). No element has nine or eight stable isotopes. Five elements have seven stable isotopes, eight have six stable isotopes, ten have five stable isotopes, nine have four stable isotopes, five have three stable isotopes, 16 have two stable isotopes (counting {{nuclide|Ta|180|m|link=yes}} as stable), and 26 elements have only a single stable isotope (of these, 19 are so-called [[mononuclidic element]]s, having a single primordial stable isotope that dominates and fixes the atomic weight of the natural element to high precision; 3 radioactive mononuclidic elements occur as well).<ref name=nuclidetable>{{cite web|url=http://www.nndc.bnl.gov/chart/|title=Interactive Chart of Nuclides|publisher=Brookhaven National Laboratory|author=Sonzogni, Alejandro|location=National Nuclear Data Center|year=2008|access-date=2013-05-03|archive-date=2018-10-10|archive-url=https://web.archive.org/web/20181010070007/http://www.nndc.bnl.gov/chart/|url-status=dead}}</ref> In total, there are 251 nuclides that have not been observed to decay. For the 80 elements that have one or more stable isotopes, the average number of stable isotopes is 251/80&nbsp;≈&nbsp;3.14 isotopes per element. === Even and odd nucleon numbers === {{Main|Even and odd atomic nuclei}} {| class="wikitable" style="float:right; text-align:right; margin-left:1em;" |+ Even/odd ''Z'', ''N'' ([[parity of zero|{{simpleNuclide|H|1}} as OE]]) ! p, n !! EE !! OO !! EO !! OE !! Total |- | Stable || 145 || 5 || 53 || 48 || 251 |- | Long-lived || 23 || 4 || 3 || 5 || 35 |- | All primordial || 168 || 9 || 56 || 53 || 286 |} The proton:neutron ratio is not the only factor affecting nuclear stability. It depends also on evenness or oddness of its atomic number ''Z'', neutron number ''N'' and, consequently, of their sum, the mass number ''A''. Oddness of both ''Z'' and ''N'' tends to lower the [[nuclear binding energy]], making odd nuclei, generally, less stable. This remarkable difference of nuclear binding energy between neighbouring nuclei, especially of odd-''A'' [[isobar (nuclide)|isobars]], has important consequences: unstable isotopes with a nonoptimal number of neutrons or protons decay by [[beta decay]] (including [[positron emission]]), [[electron capture]], or other less common decay modes such as [[spontaneous fission]] and [[cluster decay]]. The majority of stable nuclides are even-proton-even-neutron, where all numbers ''Z'', ''N'', and ''A'' are even. The odd-''A'' stable nuclides are divided (roughly evenly) into odd-proton-even-neutron, and even-proton-odd-neutron nuclides. Stable odd-proton-odd-neutron nuclei are the least common. ==== Even atomic number ==== The 146 even-proton, even-neutron (EE) nuclides comprise ~58% of all stable nuclides and all have [[spin (physics)|spin]] 0 because of pairing. There are also 24 primordial long-lived even-even nuclides. As a result, each of the 41 even-numbered elements from 2 to 82 has [[List of elements by stability of isotopes|at least one stable isotope]], and most of these elements have ''several'' primordial isotopes. Half of these even-numbered elements have six or more stable isotopes. The extreme stability of [[helium-4]] due to a double [[semi-empirical mass formula#Pairing term|pairing]] of 2 protons and 2 neutrons prevents ''any'' nuclides containing five ({{nuclide|Helium|5|link=yes}}, {{nuclide|Lithium|5|link=yes}}) or eight ({{nuclide|Beryllium|8|link=yes}}) nucleons from existing for long enough to serve as platforms for the buildup of heavier elements via [[nuclear fusion]] in stars (see [[triple alpha process]]). {| class="wikitable" style="float:right; margin-left:1em;" |+ Even-odd long-lived ! !! [[Decay mode|Decay]] !! [[Half-life]] |- | {{nuclide|Cadmium|113|link=yes}} || [[beta decay|beta]] | style="text-align:right;" | 7.7{{e|15}} [[annum|a]] |- | {{nuclide|Samarium|147|link=yes}} || [[alpha decay|alpha]] | style="text-align:right;" | 1.06{{e|11}} [[annum|a]] |- | {{nuclide|Uranium|235|link=yes}} || [[alpha decay|alpha]] | style="text-align:right;" | 7.04{{e|8}} [[annum|a]] |} 53 stable nuclides have an even number of protons and an odd number of neutrons. They are a minority in comparison to the even-even isotopes, which are about 3 times as numerous. Among the 41 even-''Z'' elements that have a stable nuclide, only two elements (argon and cerium) have no even-odd stable nuclides. One element (tin) has three. There are 24 elements that have one even-odd nuclide and 13 that have two odd-even nuclides. Of 35 primordial radionuclides there exist four even-odd nuclides (see table at right), including the [[fissile]] {{nuclide|Uranium|235|link=yes}}. Because of their odd neutron numbers, the even-odd nuclides tend to have large [[neutron capture]] cross-sections, due to the energy that results from neutron-pairing effects. These stable even-proton odd-neutron nuclides tend to be uncommon by abundance in nature, generally because, to form and enter into primordial abundance, they must have escaped capturing neutrons to form yet other stable even-even isotopes, during both the [[s-process]] and [[r-process]] of neutron capture, during [[stellar nucleosynthesis|nucleosynthesis in stars]]. For this reason, only {{nuclide|Platinum|195|link=yes}} and {{nuclide|Beryllium|9|link=yes}} are the most naturally abundant isotopes of their element. ==== Odd atomic number ==== Forty-eight stable odd-proton-even-neutron nuclides, stabilized by their paired neutrons, form most of the stable isotopes of the odd-numbered elements; the very few odd-proton-odd-neutron nuclides comprise the others. There are 41 odd-numbered elements with ''Z'' = 1 through 81, of which 39 have stable isotopes (the elements [[technetium]] ({{PhysicsParticle|Tc|BL=43}}) and [[promethium]] ({{PhysicsParticle|Pm|BL=61}}) have no stable isotopes). Of these 39 odd ''Z'' elements, 30 elements (including hydrogen-1 where 0 neutrons is [[parity of zero|even]]) have one stable odd-even isotope, and nine elements: [[chlorine]] ({{PhysicsParticle|Cl|BL=17}}), [[potassium]] ({{PhysicsParticle|K|BL=19}}), [[copper]] ({{PhysicsParticle|Cu|BL=29}}), [[gallium]] ({{PhysicsParticle|Ga|BL=31}}), [[bromine]] ({{PhysicsParticle|Br|BL=35}}), [[silver]] ({{PhysicsParticle|Ag|BL=47}}), [[antimony]] ({{PhysicsParticle|Sb|BL=51}}), [[iridium]] ({{PhysicsParticle|Ir|BL=77}}), and [[thallium]] ({{PhysicsParticle|Tl|BL=81}}), have two odd-even stable isotopes each. This makes a total {{nobr|30 + 2(9) {{=}} 48}} stable odd-even isotopes. There are also five primordial long-lived radioactive odd-even isotopes, {{nuclide|Rubidium|87|link=yes}}, {{nuclide|Indium|115|link=yes}}, {{nuclide|Rhenium|187|link=yes}}, {{nuclide|Europium|151|link=yes}}, and {{nuclide|Bismuth|209|link=yes}}. The last two were only recently found to decay, with half-lives greater than 10¹⁸ years. Only five stable nuclides contain both an odd number of protons ''and'' an odd number of neutrons. The first four "odd-odd" nuclides occur in low mass nuclides, for which changing a proton to a neutron or vice versa would lead to a very lopsided [[proton-neutron ratio]] ({{nuclide|Hydrogen|2|link=yes}}, {{nuclide|Lithium|6|link=yes}}, {{nuclide|Boron|10|link=yes}}, and {{nuclide|Nitrogen|14|link=yes}}; spins 1, 1, 3, 1). The only other entirely "stable" odd-odd nuclide, {{nuclide|Tantalum|180|m|link=yes}} (spin 9), is thought to be the rarest of the 251 stable nuclides, and is the only primordial [[nuclear isomer]], which has not yet been observed to decay despite experimental attempts.<ref>{{cite journal |doi=10.1016/j.apradiso.2009.01.057 |title=Search for the radioactivity of 180mTa using an underground HPGe sandwich spectrometer |year=2009 |last1=Hult |first1=Mikael |last2=Wieslander |first2=J. S. |last3=Marissens |first3=Gerd |last4=Gasparro |first4=Joël |last5=Wätjen |first5=Uwe |last6=Misiaszek |first6=Marcin |journal=Applied Radiation and Isotopes |volume=67 |issue=5 |pages=918–21 |pmid=19246206}}</ref> Many odd-odd radionuclides (such as the ground state of tantalum-180) with comparatively short half-lives are known. Usually, they beta-decay to their nearby even-even [[isobar (nuclide)|isobars]] that have paired protons and paired neutrons. Of the nine primordial odd-odd nuclides (five stable and four radioactive with long half-lives), only {{nuclide|Nitrogen|14|link=yes}} is the most common isotope of a common element. This is the case because it is a part of the [[CNO cycle]]. The nuclides {{nuclide|Lithium|6|link=yes}} and {{nuclide|Boron|10|link=yes}} are minority isotopes of elements that are themselves rare compared to other light elements, whereas the other six isotopes make up only a tiny percentage of the natural abundance of their elements. ==== Odd neutron number ==== {| class="wikitable" style="float:right; margin-left:1em" |+ Neutron number [[parity (mathematics)|parity]] ([[parity of zero|{{simpleNuclide|H|1}} as even]]) ! N !! Even !! Odd |- | Stable || 194 || 58 |- | Long-lived || 27 || 7 |- | All primordial || 221 || 65 |} [[Actinide]]s with odd neutron number are generally [[fissile]] (with [[thermal neutron]]s), whereas those with even neutron number are generally not, though they are [[fissionable]] with [[fast neutron]]s. All observationally stable odd-odd nuclides have nonzero integer spin. This is because the single unpaired neutron and unpaired proton have a larger [[nuclear force]] attraction to each other if their spins are aligned (producing a total spin of at least 1 unit), instead of anti-aligned. See [[deuterium]] for the simplest case of this nuclear behavior. Only {{nuclide|Platinum|195}}, {{nuclide|Beryllium|9}}, and {{nuclide|Nitrogen|14}} have odd neutron number and are the most naturally abundant isotope of their element. == Occurrence in nature == {{See also|Abundance of the chemical elements}} Elements are composed either of one nuclide ([[mononuclidic element]]s), or of more than one naturally occurring isotopes. The unstable (radioactive) isotopes are either [[primordial nuclide|primordial]] or postprimordial. Primordial isotopes were a product of [[stellar nucleosynthesis]] or another type of nucleosynthesis such as [[cosmic ray spallation]], and have persisted down to the present because their rate of decay is so slow (e.g. [[uranium-238]] and [[potassium-40]]). Post-primordial isotopes were created by [[cosmic ray]] bombardment as [[cosmogenic nuclide]]s (e.g., [[tritium]], [[carbon-14]]), or by the decay of a radioactive primordial isotope to a radioactive [[radiogenic nuclide]] daughter (e.g. [[uranium]] to [[radium]]). A few isotopes are naturally synthesized as [[nucleogenic]] nuclides, by some other natural [[nuclear reaction]], such as when neutrons from natural [[nuclear fission]] are absorbed by another atom. As discussed above, only 80 elements have any stable isotopes, and 26 of these have only one stable isotope. Thus, about two-thirds of stable elements occur naturally on Earth in multiple stable isotopes, with the largest number of stable isotopes for an element being ten, for [[tin]] ({{PhysicsParticle|Sn|BL=50}}). There are about 94 elements found naturally on Earth (up to [[plutonium]] inclusive), though some are detected only in very tiny amounts, such as [[plutonium-244]]. Scientists estimate that the elements that occur naturally on Earth (some only as radioisotopes) occur as 339 isotopes ([[nuclide]]s) in total.<ref>{{cite web|url=http://www.don-lindsay-archive.org/creation/isotope_list.html |title=Radioactives Missing From The Earth |access-date=2012-06-16}}</ref> Only 251 of these naturally occurring nuclides are stable, in the sense of never having been observed to decay as of the present time. An additional 35 [[primordial nuclide]]s (to a total of 286 primordial nuclides), are radioactive with known half-lives, but have half-lives longer than 100&nbsp;million years, allowing them to exist from the beginning of the Solar System. See [[list of nuclides]] for details. All the known [[stable nuclide]]s occur naturally on Earth; the other naturally occurring nuclides are radioactive but occur on Earth due to their relatively long half-lives, or else due to other means of ongoing natural production. These include the afore-mentioned [[cosmogenic nuclide]]s, the [[nucleogenic]] nuclides, and any [[radiogenic]] nuclides formed by ongoing decay of a primordial radioactive nuclide, such as [[radon]] and [[radium]] from uranium. An additional ~3000 radioactive nuclides not found in nature have been created in nuclear reactors and in particle accelerators. Many short-lived nuclides not found naturally on Earth have also been observed by spectroscopic analysis, being naturally created in stars or [[supernova]]e. An example is [[aluminium-26]], which is not naturally found on Earth but is found in abundance on an astronomical scale. The tabulated atomic masses of elements are averages that account for the presence of multiple isotopes with different masses. Before the discovery of isotopes, empirically determined noninteger values of atomic mass confounded scientists. For example, a sample of [[chlorine]] contains 75.8% [[chlorine-35]] and 24.2% [[chlorine-37]], giving an average atomic mass of 35.5 [[atomic mass unit]]s. According to generally accepted [[physical cosmology|cosmology theory]], only isotopes of hydrogen and helium, traces of some isotopes of lithium and beryllium, and perhaps some boron, were created at the [[Big Bang]], while all other nuclides were synthesized later, in stars and supernovae, and in interactions between energetic particles such as cosmic rays, and previously produced nuclides. (See [[nucleosynthesis]] for details of the various processes thought responsible for isotope production.) The respective abundances of isotopes on Earth result from the quantities formed by these processes, their spread through the galaxy, and the rates of decay for isotopes that are unstable. After the initial coalescence of the [[Solar System]], isotopes were redistributed according to mass, and the isotopic composition of elements varies slightly from planet to planet. This sometimes makes it possible to trace the origin of [[meteorite]]s. == Atomic mass of isotopes == The [[atomic mass]] (''m''_r) of an isotope (nuclide) is determined mainly by its [[mass number]] (i.e. number of [[nucleon]]s in its nucleus). Small corrections are due to the [[binding energy]] of the nucleus (see [[mass defect]]), the slight difference in mass between proton and neutron, and the mass of the electrons associated with the atom, the latter because the electron:nucleon ratio differs among isotopes. The mass number is a [[dimensionless quantity]]. The atomic mass, on the other hand, is measured using the [[atomic mass unit]] based on the mass of the carbon-12 atom. It is denoted with symbols "u" (for unified atomic mass unit) or "Da" (for [[John Dalton|dalton]]). The atomic masses of naturally occurring isotopes of an element determine the [[standard atomic weight]] of the element. When the element contains ''N'' isotopes, the expression below is applied for the average atomic mass <math>\overline m_a</math>: <math> \overline m_a = m_1 x_1+m_2 x_2+...+m_Nx_N</math> where ''m''₁, ''m''₂, ..., ''m''_''N'' are the atomic masses of each individual isotope, and ''x''₁, ..., ''x''_''N'' are the relative abundances of these isotopes. == Applications of isotopes == === Purification of isotopes === {{Main|isotope separation}} Several applications exist that capitalize on the properties of the various isotopes of a given element. [[Isotope separation]] is a significant technological challenge, particularly with heavy elements such as uranium or plutonium. Lighter elements such as lithium, carbon, nitrogen, and oxygen are commonly separated by gas diffusion of their compounds such as CO and NO. The separation of hydrogen and deuterium is unusual because it is based on chemical rather than physical properties, for example in the [[Girdler sulfide process]]. Uranium isotopes have been separated in bulk by gas diffusion, gas centrifugation, laser ionization separation, and (in the [[Manhattan Project]]) by a type of production [[mass spectrometry]]. === Use of chemical and biological properties === {{Main|isotope geochemistry|cosmochemistry|paleoclimatology}} * [[Isotope analysis]] is the determination of [[isotopic signature]], the relative abundances of isotopes of a given element in a particular sample. Isotope analysis is frequently done by [[isotope ratio mass spectrometry]]. For [[biogenic substance]]s in particular, significant variations of isotopes of C, N, and O can occur. Analysis of such variations has a wide range of applications, such as the detection of adulteration in food products<ref name=Jamin>{{cite journal|last1=Jamin|first1=Eric|last2=Guérin|first2=Régis|last3=Rétif|first3=Mélinda|last4=Lees|first4=Michèle|last5=Martin|first5=Gérard J. |title=Improved Detection of Added Water in Orange Juice by Simultaneous Determination of the Oxygen-18/Oxygen-16 Isotope Ratios of Water and Ethanol Derived from Sugars |journal=[[J. Agric. Food Chem.]]|volume= 51|year=2003|doi=10.1021/jf030167m|pmid=12926859|issue=18|pages=5202–6}}</ref> or the geographic origins of products using [[isoscapes]]. The identification of [[Mars meteorite|certain meteorites]] as having originated on [[Mars]] is based in part upon the isotopic signature of trace gases contained in them.<ref name=Treiman>{{cite journal|author1=Treiman, A. H. |author2=Gleason, J. D. |author3=Bogard, D. D. |title=The SNC meteorites are from Mars |journal=[[Planet. Space Sci.]]|volume= 48|page=1213|year=2000| doi=10.1016/S0032-0633(00)00105-7 |bibcode=2000P&SS...48.1213T|issue=12–14}}</ref> * Isotopic substitution can be used to determine the mechanism of a [[chemical reaction]] via the [[kinetic isotope effect]]. * Another common application is [[isotopic labeling]], the use of unusual isotopes as tracers or markers in chemical reactions.<ref>{{Cite journal|last1=Deegan|first1=Frances M.|last2=Troll|first2=Valentin R.|last3=Whitehouse|first3=Martin J.|last4=Jolis|first4=Ester M.|last5=Freda|first5=Carmela|date=2016-08-04|title=Boron isotope fractionation in magma via crustal carbonate dissolution|journal=Scientific Reports|language=en|volume=6|issue=1|pages=30774|doi=10.1038/srep30774|pmid=27488228|issn=2045-2322|pmc=4973271|bibcode=2016NatSR...630774D}}</ref> Normally, atoms of a given element are indistinguishable from each other. However, by using isotopes of different masses, even different nonradioactive [[stable isotope]]s can be distinguished by [[mass spectrometry]] or [[infrared spectroscopy]]. For example, in 'stable isotope labeling with amino acids in cell culture ([[SILAC]])' stable isotopes are used to quantify [[protein]]s. If radioactive isotopes are used, they can be detected by the radiation they emit (this is called ''radioisotopic labeling''). * Isotopes are commonly used to determine the concentration of various elements or substances using the [[isotope dilution]] method, whereby known amounts of isotopically substituted compounds are mixed with the samples and the isotopic signatures of the resulting mixtures are determined with [[mass spectrometry]]. === Use of nuclear properties === * A technique similar to radioisotopic labeling is [[radiometric dating]]: using the known [[half-life]] of an unstable element, one can calculate the amount of time that has elapsed since a known concentration of isotope existed. The most widely known example is [[radiocarbon dating]] used to determine the age of carbonaceous materials. * Several forms of spectroscopy rely on the unique nuclear properties of specific isotopes, both radioactive and stable. For example, [[nuclear magnetic resonance]] (NMR) spectroscopy can be used only for isotopes with a nonzero nuclear spin. The most common nuclides used with NMR spectroscopy are ¹H, ²D, ¹⁵N, ¹³C, and ³¹P. * [[Mössbauer spectroscopy]] also relies on the nuclear transitions of specific isotopes, such as ⁵⁷Fe. * [[Radionuclide]]s also have important uses. [[Nuclear power]] and [[nuclear weapon]]s development require relatively large quantities of specific isotopes. [[Nuclear medicine]] and [[radiation oncology]] utilize radioisotopes respectively for medical diagnosis and treatment. == See also == * [[Abundance of the chemical elements]] * [[Bainbridge mass spectrometer]] * [[Geotraces]] * [[Isotopomer]] * [[List of nuclides]] * [[List of particles]] * [[Mass spectrometry]] * [[Reference Materials for Stable Isotope Analysis|Reference materials for stable isotope analysis]] * [[Table of nuclides]] == References == {{reflist|35em}} == External links == * [http://www.nucleonica.com/ The Nuclear Science web portal Nucleonica] * [http://www.nucleonica.com/wiki/index.php?title=Category%3AKNC The Karlsruhe Nuclide Chart] * [http://www.nndc.bnl.gov/ National Nuclear Data Center] Portal to large repository of free data and analysis programs from NNDC * [http://isotopes.gov/ National Isotope Development Center] Coordination and management of the production, availability, and distribution of isotopes, and reference information for the isotope community * [http://science.energy.gov/np/research/idpra/ Isotope Development & Production for Research and Applications (IDPRA)] U.S. Department of Energy program for isotope production and production research and development * [http://www.iaea.org/ International Atomic Energy Agency] Homepage of [[International Atomic Energy Agency]] (IAEA), an Agency of the [[United Nations]] (UN) * [http://physics.nist.gov/cgi-bin/Compositions/stand_alone.pl?ele=&ascii=html&isotype=some Atomic Weights and Isotopic Compositions for All Elements] Static table, from NIST ([[National Institute of Standards and Technology]]) * [https://web.archive.org/web/20070121042708/http://atom.kaeri.re.kr/ Atomgewichte, Zerfallsenergien und Halbwertszeiten aller Isotope] * [https://web.archive.org/web/20061205022425/http://ie.lbl.gov/education/isotopes.htm Exploring the Table of the Isotopes] at the [[LBNL]] * [https://web.archive.org/web/20141217141609/http://isotope.info/ Current isotope research and information] isotope.info * [https://web.archive.org/web/20070825124014/http://www.bt.cdc.gov/radiation/isotopes/ Emergency Preparedness and Response: Radioactive Isotopes] by the CDC ([[Centers for Disease Control and Prevention]]) * [http://www.nndc.bnl.gov/chart/ Chart of Nuclides] {{Webarchive|url=https://web.archive.org/web/20181010070007/http://www.nndc.bnl.gov/chart/ |date=2018-10-10 }} Interactive Chart of Nuclides (National Nuclear Data Center) * [http://www.yoix.org/elements.html Interactive Chart of the nuclides, isotopes and Periodic Table] * [http://www-nds.iaea.org/livechart The LIVEChart of Nuclides – IAEA] with isotope data. * [https://web.archive.org/web/20120330123733/http://alsos.wlu.edu/adv_rst.aspx?keyword=isotope&creator=&title=&media=all&genre=all&disc=all&level=all&sortby=relevance&results=10&period=15 Annotated bibliography for isotopes] from the Alsos Digital Library for Nuclear Issues * [https://www.youtube.com/watch?v=UTOp_2ZVZmM&t=192 The Valley of Stability (video)] – a virtual "flight" through 3D representation of the nuclide chart, by [[French Alternative Energies and Atomic Energy Commission|CEA]] (France) {{Isotope index}} {{Authority control}} [[Category:Isotopes| ]] [[Category:Nuclear physics]]'