View source for Abundance of the chemical elements

{{short description|Measure of the relative occurrences of chemical elements in a given context}}
The '''abundance of the chemical elements''' is a measure of the [[Type–token distinction#Occurrences|occurrences]] of the [[chemical element]]s relative to all other elements in a given environment. Abundance is measured in one of three ways: by [[mass fraction (chemistry)|''mass fraction'']] (in commercial contexts often called ''weight fraction''), by ''[[mole fraction]]'' (fraction of atoms by numerical count, or sometimes fraction of molecules in gases), or by ''[[volume fraction]]''. Volume fraction is a common abundance measure in mixed gases such as planetary atmospheres, and is similar in value to molecular mole fraction for gas mixtures at relatively low densities and pressures, and [[ideal gas]] mixtures. Most abundance values in this article are given as mass fractions.

The abundance of chemical elements in the universe is dominated by the large amounts of hydrogen and helium which were produced during [[Big Bang nucleosynthesis]]. Remaining elements, making up only about 2% of the universe, were largely produced by [[supernova nucleosynthesis]]. Elements with [[even atomic numbers]] are generally more common than their neighbors in the [[periodic table]], due to their favorable energetics of formation, described by the [[Oddo–Harkins rule]].

The abundance of elements in the Sun and outer planets is similar to that in the universe. Due to solar heating, the elements of Earth and the inner rocky planets of the Solar System have undergone an additional depletion of [[volatile (chemistry)|volatile]] hydrogen, helium, neon, nitrogen, and carbon (which volatilizes as [[methane]]). The crust, mantle, and core of the Earth show evidence of chemical segregation plus some sequestration by density. Lighter silicates of aluminium are found in the crust, with more magnesium silicate in the mantle, while metallic iron and nickel compose the core. The abundance of elements in specialized environments, such as atmospheres, oceans, or the human body, are primarily a product of chemical interactions with the medium in which they reside.

== Abundance values ==
Abundance of each element is expressed as a relative number. Astronomy uses a [[Log scale|logarithmic]] scale for abundance <math>\epsilon_X</math> of element X relative to Hydrogen, defined by
<math display="block">\epsilon_X \equiv \log(N_X/N_H) + 12.00 </math>
for number density <math>N</math>; <math>\epsilon_H = 12.00</math> on this scale.<ref>{{Cite book |author1=N. Grevesse |author2=A. J. Sauva |editor=P. Murdin |date=2005 |title=Encyclopedia of Astronomy & Astrophysics |chapter=Solar Abundances |publisher=IOP Publishing |isbn=0333750888 |url=http://astro.uni-tuebingen.de/~rauch/TMAP/grevessesauval2001.pdf |access-date=2024-11-18 |via=astro.uni-tuebingen.de}}</ref> Another scale is [[Mass fraction (chemistry)|mass fraction]] or, equivalently, percent by mass.<ref>{{Cite web |publisher=[[International Union of Pure and Applied Chemistry]] (IUPAC)|title=IUPAC - mass fraction (M03722) |url=https://goldbook.iupac.org/terms/view/M03722 |access-date=2024-05-29 |website=goldbook.iupac.org}}</ref>

For example, the abundance of [[oxygen]] in [[pure water]] can be measured in two ways: the ''mass fraction'' is about 89%, because that is the fraction of water's mass which is oxygen. However, the ''[[mole fraction]]'' is about 33% because only 1 [[atom]] of 3 in water, H<sub>2</sub>O, is oxygen. As another example, looking at the ''mass fraction'' abundance of hydrogen and helium in both the [[universe]] as a whole and in the [[atmosphere]]s of [[gas-giant planet]]s such as [[Jupiter]], it is 74% for [[hydrogen]] and 23–25% for [[helium]]; while the ''(atomic) mole fraction'' for hydrogen is 92%, and for helium is 8%, in these environments. Changing the given environment to [[Jupiter's outer atmosphere]], where hydrogen is [[diatomic]] while helium is not, changes the ''molecular'' mole fraction (fraction of total gas molecules), as well as the fraction of atmosphere by volume, of hydrogen to about 86%, and of helium to 13%. Below Jupiter's outer atmosphere, volume fractions are significantly different from mole fractions due to high temperatures ([[ionization]] and [[disproportionation]]) and high density, where the [[ideal gas law]] is inapplicable.

== Universe ==
{{anchor|Universe}}
{{see also|Nucleosynthesis|Cosmochemistry|Astrochemistry}}

{| class="wikitable sortable" style="float:right; margin-left:1em;"
|+ Ten most common elements in the [[Milky Way Galaxy]] estimated spectroscopically<ref name="croswell">{{cite book | last = Croswell | first = Ken | title = Alchemy of the Heavens | publisher = Anchor | date = February 1996 | url = http://kencroswell.com/alchemy.html | isbn = 0-385-47214-5 | url-status = live | archive-url = https://web.archive.org/web/20110513233910/http://www.kencroswell.com/alchemy.html | archive-date = 2011-05-13 }}</ref>
|-
! [[Atomic number|Z]] !! Element !! Mass fraction<br/> (ppm)
|-
| 1  || [[Hydrogen]]  ||{{right}} 739,000
|-
| 2  || [[Helium]]    ||{{right}} 240,000
|-
| 8  || [[Oxygen]]    ||{{right}} 10,400
|-
| 6  || [[Carbon]]    ||{{right}} 4,600
|-
| 10 || [[Neon]]      ||{{right}} 1,340
|-
| 26 || [[Iron]]      ||{{right}} 1,090
|-
| 7  || [[Nitrogen]]  ||{{right}}   960
|-
| 14 || [[Silicon]]   ||{{right}}   650
|-
| 12 || [[Magnesium]] ||{{right}}   580
|-
| 16 || [[Sulfur]]    ||{{right}}   440
|-
|    || Total         ||{{right}} 999,060
|}

The abundance of chemical elements in the universe is dominated by the large amounts of hydrogen and helium which were produced during [[Big Bang nucleosynthesis]]. Remaining elements, making up only about 2% of the universe, were largely produced by [[supernova]]e and certain [[red giant stars]]. [[Lithium]], [[beryllium]], and [[boron]], despite their low atomic number, are rare because, although they are produced by nuclear fusion, they are destroyed by other reactions in the stars.<ref name="LiBeB Story">{{cite book|last1=Vangioni-Flam|first1=Elisabeth|last2=Cassé|first2=Michel|editor1-last=Spite|editor1-first=Monique|title=Galaxy Evolution: Connecting the Distant Universe with the Local Fossil Record|date=2012|publisher=[[Springer Science & Business Media]]|pages=77–86|isbn=978-9401142137}}</ref><ref name="Trimble">{{cite book|last1=Trimble|first1=Virginia|editor1-last=Malkan|editor1-first=Matthew A.|editor2-last=Zuckerman|editor2-first=Ben|title=The origin and evolution of the universe|date=1996|publisher=[[Jones and Bartlett Publishers]]|location=Sudbury, Mass.|isbn=0-7637-0030-4|page=101|chapter=The Origin and Evolution of the Chemical Elements}}</ref> Their natural occurrence is the result of [[cosmic ray spallation]] of carbon, nitrogen and oxygen in a type of nuclear fission reaction. The elements from carbon to iron are relatively more abundant in the universe because of the ease of making them in [[supernova nucleosynthesis]]. Elements of higher atomic numbers than iron (element 26) become progressively rarer in the universe, because they increasingly absorb stellar energy in their production. Also, elements with [[even and odd atomic nuclei|even atomic numbers]] are generally more common than their neighbors in the [[periodic table]], due to favorable energetics of formation (see [[Oddo–Harkins rule]]), and among the lightest nuclides helium through sulfur the most abundant isotopes of equal number of protons and neutrons.

[[Hydrogen]] is the most abundant element in the Universe; [[helium]] is second. All others are orders of magnitude less common. After this, the rank of abundance does not continue to correspond to the [[atomic number]]. [[Oxygen]] has abundance rank 3, but atomic number 8. 
[[File:Isotopic Abundance bubble chart.png|thumb|300x300px|alt=refer to text|'''The most abundant isotopes -'''Isotopes with equal numbers of protons and neutrons are unusually abundant. Relative abundance is proportional to the area. '''<chem>^{1}H</chem>''' (large blue circle) comprises 74% of the ordinary matter of the universe. Color corresponds to nucleosynthetic process: Blue: Big Bang; Green: dying low-mass stars; Yellow: exploding massive stars.]]

There are 80 known [[stable elements]], and the lightest 16 comprise 99.9% of the ordinary matter of the universe. These same 16 elements, hydrogen through sulfur, fall on the initial linear portion of the [[table of nuclides]] (also called ''the'' ''Segrè plot''), a plot of the proton versus neutron numbers of all matter both ordinary and exotic, containing hundreds of stable isotopes and thousands more that are unstable. The Segrè plot is initially linear because (aside from hydrogen) the vast majority of ordinary matter (99.4% in the Solar System<ref name="Arnett">{{cite book |first=David |last=Arnett |date=1996 |title=Supernovae and Nucleosynthesis |edition=First |publisher=[[Princeton University Press]] |location=Princeton, New Jersey |isbn=0-691-01147-8 |oclc=33162440|page=11}}</ref>) contains an equal number of protons and neutrons (Z=N).

The abundance of the lightest elements is well predicted by the [[standard cosmological model]], since they were mostly produced shortly (i.e., within a few hundred seconds) after the Big Bang, in a process known as [[Big Bang nucleosynthesis]]. Heavier elements were mostly produced much later, in [[stellar nucleosynthesis]].

Hydrogen and helium are estimated to make up roughly 74% and 24% of all baryonic matter in the universe respectively. Despite comprising only a very small fraction of the universe, the remaining "heavy elements" can greatly influence astronomical phenomena. Only about 2% (by mass) of the [[Milky Way galaxy]]'s disk is composed of heavy elements.

These other elements are generated by stellar processes.<ref>{{cite journal |doi=10.1103/RevModPhys.28.53 |title=Abundances of the Elements |date=1956 |last1=Suess |first1=Hans |last2=Urey |first2=Harold |journal=Reviews of Modern Physics |volume=28 |issue=1 |page=53 |bibcode=1956RvMP...28...53S}}</ref><ref>{{cite journal |doi=10.1007/BF00172440 |title=Abundances of the elements in the solar system |date=1973 |last1=Cameron |first1=A. G. W. |journal=Space Science Reviews |volume=15 |issue=1 |pages=121 |bibcode=1973SSRv...15..121C |s2cid=120201972}}</ref><ref>{{cite journal |doi=10.1016/0016-7037(82)90208-3 |title=Solar-system abundances of the elements |date=1982 |last1=Anders |first1=E. |last2=Ebihara |first2=M. |journal=Geochimica et Cosmochimica Acta |volume=46 |page=2363 |bibcode = 1982GeCoA..46.2363A |issue=11 }}</ref> In astronomy, a "[[Metal (astronomy)|metal]]" is any element other than hydrogen or helium. This distinction is significant because hydrogen and helium are the only elements that were produced in significant quantities in the Big Bang. Thus, the [[metallicity]] of a [[galaxy]] or other object is an indication of stellar activity after the Big Bang.

In general, elements up to [[iron]] are made by large stars in the process of becoming [[supernova]]e, or by smaller stars in the process of dying. [[Iron-56]] is particularly common, since it is the most stable nuclide (in that it has the highest nuclear binding energy per nucleon) and can easily be "built up" from [[alpha particles]] (being a product of decay of radioactive [[nickel-56]], ultimately made from 14 helium nuclei). Elements heavier than iron are made in energy-absorbing processes in large stars, and their abundance in the universe (and on Earth) generally decreases with increasing atomic number.

The table shows the ten most common elements in our galaxy (estimated [[spectroscopically]]), as measured in parts per million, by mass.<ref name="croswell"/>
Nearby galaxies that have evolved along similar lines have a corresponding enrichment of elements heavier than hydrogen and helium. The more distant galaxies are being viewed as they [[Cosmic redshift|appeared in the past]], so their abundances of elements appear closer to the primordial mixture. Since physical laws and processes are apparently uniform throughout the universe, however, it is expected that these galaxies will likewise have evolved similar abundances of elements.

As shown in the [[periodic table]], the abundance of elements is in keeping with their origin. Very abundant hydrogen and helium are products of the Big Bang. The next three elements in the periodic table ([[lithium]], [[beryllium]], and [[boron]]) are rare, despite their low atomic number. They had little time to form in the Big Bang. They are produced in small quantities by nuclear fusion in dying stars or by breakup of heavier elements in interstellar dust, caused by [[cosmic ray spallation]]. In [[supernova]] stars, they are produced by nuclear fusion, but then destroyed by other reactions.<ref name="LiBeB Story" />
{{Wide image|Nucleosynthesis periodic table.svg|512px|Periodic table showing the cosmological origin of each element|dir=rtl}}

Heavier elements, beginning with [[carbon]], have been produced in dying or supernova stars by buildup from [[alpha particle]]s (helium nuclei), contributing to an alternatingly larger abundance of elements with even atomic numbers (these are also more stable). The effect of odd-numbered chemical elements generally being more rare in the universe was empirically noticed in 1914, and is known as the [[Oddo–Harkins rule]].

The following graph ([[log scale]]) shows abundance of elements in the [[Solar System]].
<div class="skin-invert-image">{{Wide image|Elements_abundance-bars.svg|1000px|Estimated abundances of the chemical elements in the Solar System (logarithmic scale)}}</div>

{| class="wikitable sortable mw-collapsible" style="float:right; margin-left:1em;"
|+ Most abundant nuclides<br/> in the [[Solar System]]<ref name=Arnett/>
! [[Nuclide]]
! [[Mass number|A]]
!width="1"|<!-- Make column as narrow as possible --> Mass fraction in parts per million
!width="1"|<!-- Make column as narrow as possible --> Atom fraction in parts per million
|-
| [[Hydrogen-1]] ||1||style="text-align:right"|705,700 ||style="text-align:right"| 909,964
|-
| [[Helium-4]] ||4||style="text-align:right"|275,200 ||style="text-align:right"| 88,714
|-
| [[Oxygen-16]] ||16||style="text-align:right"|9,592 || style="text-align:right" | 774
|-
| [[Carbon-12]] ||12||style="text-align:right"|3,032 ||style="text-align:right"| 326
|-
| [[Nitrogen-14]] ||14||style="text-align:right"|1,105 ||style="text-align:right"| 102
|-
| [[Neon-20]] ||20||style="text-align:right"|1,548 ||style="text-align:right"| 100
|-
| colspan="4" | [[Image:spacer.gif|1px]]
|-
| colspan="2" | '''''Other nuclides:''''' ||style="text-align:right"|3,616 ||style="text-align:right"| 172
|-
| [[Silicon-28]] ||28||style="text-align:right"|653 ||style="text-align:right"| 30
|-
| [[Magnesium-24]] ||24||style="text-align:right"|513 ||style="text-align:right"| 28
|-
| [[Iron-56]] ||56||style="text-align:right"|1,169 ||style="text-align:right"| 27
|-
| [[Sulfur-32]] ||32||style="text-align:right"|396 ||style="text-align:right"| 16
|-
| [[Helium-3]] ||3||style="text-align:right"|35 ||style="text-align:right"| 15
|-
| [[Hydrogen-2]] ||2||style="text-align:right"|23 ||style="text-align:right"| 15
|-
| [[Neon-22]] ||22||style="text-align:right"|208 ||style="text-align:right"| 12
|-
| [[Magnesium-26]] ||26||style="text-align:right"|79 ||style="text-align:right"| 4
|-
| [[Carbon-13]] ||13||style="text-align:right"|37 ||style="text-align:right"| 4
|-
| [[Magnesium-25]] ||25||style="text-align:right"|69 ||style="text-align:right"| 4
|-
| [[Aluminium-27]] ||27||style="text-align:right"|58 ||style="text-align:right"| 3
|-
| [[Argon-36]] ||36||style="text-align:right"|77 ||style="text-align:right"| 3
|-
| [[Calcium-40]] ||40||style="text-align:right"|60 ||style="text-align:right"| 2
|-
| [[Sodium-23]] ||23||style="text-align:right"|33 ||style="text-align:right"| 2
|-
| [[Iron-54]] ||54||style="text-align:right"|72 ||style="text-align:right"| 2
|-
| [[Silicon-29]] ||29||style="text-align:right"|34 ||style="text-align:right"| 2
|-
| [[Nickel-58]] ||58||style="text-align:right"|49 ||style="text-align:right"| 1
|-
| [[Silicon-30]] ||30||style="text-align:right"|23 ||style="text-align:right"| 1
|-
| [[Iron-57]] ||57||style="text-align:right"|28 ||style="text-align:right"| 1
|}

===Relation to nuclear binding energy===
Loose correlations have been observed between estimated elemental abundances in the universe and the [[nuclear binding energy curve]] (also called the ''binding energy per nucleon''). Roughly speaking, the relative stability of various atomic nuclides in withstanding the extremely energetic conditions of [[Big Bang nucleosynthesis]] (BBN) has exerted a strong influence on the relative abundance of elements formed in the Big Bang, and during the development of the universe thereafter.<ref name=Bell01>{{cite book|last=Bell|first=Jerry A.|title=Chemistry: a project of the American Chemical Society|date=2005|publisher=Freeman|location=New York [u.a.]|isbn=978-0-7167-3126-9|pages=191–193|author2=GenChem Editorial/Writing Team|chapter=Chapter 3: Origin of Atoms|quote=Correlations between abundance and nuclear binding energy [Subsection title]}}</ref>
See the article about [[nucleosynthesis]] for an explanation of how certain [[nuclear fusion]] processes in stars (such as [[carbon-burning process|carbon burning]], etc.) create the elements heavier than hydrogen and helium.

[[File:SolarSystemAbundances.svg|class=skin-invert|frameless|alt=refer to text|600px]]

A further observed peculiarity is the jagged alternation between relative abundance and scarcity of adjacent atomic numbers in the estimated abundances of the chemical elements in which the relative abundance of even atomic numbers is roughly 2 orders of magnitude greater than the relative abundance of odd atomic numbers ([[Oddo–Harkins rule]]). A similar alternation between even and odd atomic numbers can be observed in the [[nuclear binding energy curve]] in the neighborhood of carbon and oxygen, but here the loose correlation between relative abundance and binding energy ends. The binding energy for beryllium (an even atomic number), for example, is ''less'' than the binding energy for boron (an odd atomic number), as illustrated in the nuclear binding energy curve. Additionally, the alternation in the nuclear binding energy between even and odd atomic numbers resolves above oxygen as the graph increases steadily up to its peak at iron. The [[semi-empirical mass formula]] (SEMF), also called ''Weizsäcker's formula'' or the ''Bethe-Weizsäcker mass formula'', gives a theoretical explanation of the overall shape of the curve of nuclear binding energy.<ref name=Bailey>{{cite web |last=Bailey |first=David |title=Semi-empirical Nuclear Mass Formula |url=http://www.upscale.utoronto.ca/GeneralInterest/DBailey/SubAtomic/Lectures/LectF25/Lect25.htm|work=PHY357: Strings & Binding Energy |publisher=[[University of Toronto]]|access-date=2011-03-31 |url-status=live|archive-url=https://web.archive.org/web/20110724042945/http://www.upscale.utoronto.ca/GeneralInterest/DBailey/SubAtomic/Lectures/LectF25/Lect25.htm |archive-date=2011-07-24}}</ref>

[[File:Binding energy curve - common isotopes.svg|class=skin-invert|500px|alt=refer to text|Binding energy per nucleon for a selection of nuclides. The nuclide with the highest value, {{simple nuclide|Ni|62}}, does not appear. The horizontal lines are at 8 and 8.5 [[MeV]].]]

== Sun ==
Modern astronomy relies on understanding the abundance of elements in the Sun as part of cosmological models. Abundance values are difficult to obtain: even photospheric or observational abundances depend upon models of solar atmospherics and radiation coupling.<ref name="Asplund2020Review">{{Cite journal |last=Asplund |first=M. |last2=Amarsi |first2=A. M. |last3=Grevesse |first3=N. |date=2021-09-01 |title=The chemical make-up of the Sun: A 2020 vision |url=https://www.aanda.org/articles/aa/abs/2021/09/aa40445-21/aa40445-21.html |journal=Astronomy & Astrophysics |language=en |volume=653 |pages=A141 |arxiv=2105.01661 |doi=10.1051/0004-6361/202140445 |issn=0004-6361}}</ref> These [[#Abundance_values| astronomical abundance values]] are reported as logarithms of the ratio with hydrogen. Hydrogen is set to an abundance of 12 on this scale.

The Sun's [[photosphere]] consists mostly of hydrogen and helium; the helium abundance varies between about 10.3 and 10.5 depending on the phase of the [[solar cycle]];<ref>{{Cite journal |last1=Alterman |first1=Benjamin L. |last2=Kasper |first2=Justin C. |last3=Leamon |first3=Robert J. |last4=McIntosh |first4=Scott W. |date=April 2021 |title=Solar wind helium abundance heralds solar cycle onset |journal=Solar Physics |volume=296 |issue=4 |pages=67 |arxiv=2006.04669 |bibcode=2021SoPh..296...67A |doi=10.1007/s11207-021-01801-9 |s2cid=233738140}}</ref> carbon is 8.47, neon is 8.29, oxygen is 7.69<ref>{{Cite journal |last1=Pietrow |first1=A. G. M. |last2=Hoppe |first2=R. |last3=Bergemann |first3=M. |last4=Calvo |first4=F. |year=2023 |title=Solar oxygen abundance using SST/CRISP center-to-limb observations of the O I 7772 Å line |journal=Astronomy & Astrophysics |volume=672 |issue=4 |pages=L6 |arxiv=2304.01048 |bibcode=2023A&A...672L...6P |doi=10.1051/0004-6361/202346387 |s2cid=257912497}}</ref> and iron is estimated at 7.62.<ref>{{cite web |title=Abundance Ratios and Galactic Chemical Evolution - Andrew McWilliam |url=https://ned.ipac.caltech.edu/level5/March03/McWilliam/McWilliam2.html |website=ned.ipac.caltech.edu |access-date=24 May 2024}}</ref>

== Earth ==
[[File:element_abundance_earth_ppm_chart.svg|thumb|alt=refer to text|[[Parts-per-million]] cube of relative abundance by mass of elements of the entire Earth down to around 1 ppm]]
{{see also|Earth#Chemical composition}}

The [[Earth]] formed from the [[protosolar nebula|same cloud of matter]] that formed the Sun, but the planets acquired different compositions during the [[formation and evolution of the Solar System]]. In turn, the [[history of Earth]] led to parts of the planet having differing concentrations of the elements.

The mass of the Earth is approximately 5.97{{e|24}}&nbsp;kg. By mass, it is composed mostly of [[iron]] (32.1%), [[oxygen]] (30.1%), [[silicon]] (15.1%), [[magnesium]] (13.9%), [[sulfur]] (2.9%), [[nickel]] (1.8%), [[calcium]] (1.5%), and [[aluminium]] (1.4%); with the remaining 1.2% consisting of trace amounts of other elements.<ref name=pnas71_12_6973>{{cite journal | author=Morgan, J. W. | author2=Anders, E. | title=Chemical composition of Earth, Venus, and Mercury | journal=Proceedings of the National Academy of Sciences | date=1980 | volume=77 | issue=12 | pages=6973–6977 | doi=10.1073/pnas.77.12.6973 | pmid=16592930 | pmc=350422 |bibcode = 1980PNAS...77.6973M | doi-access=free }}</ref>

The bulk composition of the Earth by elemental mass is roughly similar to the gross composition of the solar system, with the major differences being that Earth is missing a great deal of the [[volatile element]]s hydrogen, helium, neon, and nitrogen, as well as carbon which has been lost as volatile [[hydrocarbons]].

The remaining elemental composition is roughly typical of the "rocky" [[inner planets]], which formed "inside" the "[[frost line (astronomy)|frost line]]" close to the Sun, where the young Sun's heat and [[stellar wind]] drove off volatile compounds into space.

The Earth retains oxygen as the second-largest component of its mass (and largest atomic fraction), mainly due to oxygen's high reactivity; this caused it to bond into [[silicate minerals]] which have a high melting point and low vapor pressure.
{| class="wikitable sortable collapsible collapsed" style="width: 90%; float:center; margin-right: 0; margin-left:1em; text-align:right"
|+ style="text-align: left;" |Estimated abundances of chemical elements in the Earth.<ref name="mit1">William F McDonough [https://web.archive.org/web/20110928074153/http://quake.mit.edu/hilstgroup/CoreMantle/EarthCompo.pdf The composition of the Earth]. quake.mit.edu, archived by the Internet Archive Wayback Machine.</ref> The right two columns give the fraction of the mass in [[parts per million]] (ppm) and the fraction by number of atoms in parts per billion (ppb).
|-
! Atomic number
! Name
! Symbol
! Mass fraction (ppm)<ref name="mit1"/>
! Atomic fraction (ppb)
|-
|8  ||  oxygen  ||  O  || 297,000 || 482,000,000
|-
|12  ||  magnesium  ||  Mg  || 154,000 || 164,000,000
|-
|14  ||  silicon  ||  Si  || 161,000 || 150,000,000
|-
|26  ||  iron  ||  Fe  || 319,000 || 148,000,000
|-
|13  ||  aluminium  ||  Al  || 15,900 || 15,300,000
|-
|20  ||  calcium  ||  Ca  || 17,100 || 11,100,000
|-
|28  ||  nickel  ||  Ni  || 18,220 || 8,010,000
|-
|1  ||  hydrogen  ||  H  || 260 || 6,700,000
|-
|16  ||  sulfur  ||  S  || 6,350 || 5,150,000
|-
|24  ||  chromium  ||  Cr  || 4,700 || 2,300,000
|-
|11  ||  sodium  ||  Na  || 1,800 || 2,000,000
|-
|6  ||  carbon  ||  C  || 730 || 1,600,000
|-
|15  ||  phosphorus  ||  P  || 1,210 || 1,020,000
|-
|25  ||  manganese  ||  Mn  || 1,700 || 800,000
|-
|22  ||  titanium  ||  Ti  || 810 || 440,000
|-
|27  ||  cobalt  ||  Co  || 880 || 390,000
|-
|19  ||  potassium  ||  K  || 160 || 110,000
|-
|17  ||  chlorine  ||  Cl  || 76 || 56,000
|-
|23  ||  vanadium  ||  V  || 105 || 53,600
|-
|7  ||  nitrogen  ||  N  || 25 || 46,000
|-
|29  ||  copper  ||  Cu  || 60 || 25,000
|-
|30  ||  zinc  ||  Zn  || 40 || 16,000
|-
|9  ||  fluorine  ||  F  || 10 || 14,000
|-
|21  ||  scandium  ||  Sc  || 11 || 6,300
|-
|3  ||  lithium  ||  Li  || 1.10 || 4,100
|-
|38  ||  strontium  ||  Sr  || 13 || 3,900
|-
|32  ||  germanium  ||  Ge  || 7.00 || 2,500
|-
|40  ||  zirconium  ||  Zr  || 7.10 || 2,000
|-
|31  ||  gallium  ||  Ga  || 3.00 || 1,000
|-
|34  ||  selenium  ||  Se  || 2.70 || 890
|-
|56  ||  barium  ||  Ba  || 4.50 || 850
|-
|39  ||  yttrium  ||  Y  || 2.90 || 850
|-
|33  ||  arsenic  ||  As  || 1.70 || 590
|-
|5  ||  boron  ||  B  || 0.20 || 480
|-
|42  ||  molybdenum  ||  Mo  || 1.70 || 460
|-
|44  ||  ruthenium  ||  Ru  || 1.30 || 330
|-
|78  ||  platinum  ||  Pt  || 1.90 || 250
|-
|46  ||  palladium  ||  Pd  || 1.00 || 240
|-
|58  ||  cerium  ||  Ce  || 1.13 || 210
|-
|60  ||  neodymium  ||  Nd  || 0.84 || 150
|-
|4  ||  beryllium  ||  Be  || 0.05 || 140
|-
|41  ||  niobium  ||  Nb  || 0.44 || 120
|-
|76  ||  osmium  ||  Os  || 0.90 || 120
|-
|77  ||  iridium  ||  Ir  || 0.90 || 120
|-
|37  ||  rubidium  ||  Rb  || 0.40 || 120
|-
|35  ||  bromine  ||  Br  || 0.30 || 97
|-
|57  ||  lanthanum  ||  La  || 0.44 || 82
|-
|66  ||  dysprosium  ||  Dy  || 0.46 || 74
|-
|64  ||  gadolinium  ||  Gd  || 0.37 || 61
|-
|52  ||  tellurium  ||  Te  || 0.30 || 61
|-
|45  ||  rhodium  ||  Rh  || 0.24 || 61
|-
|50  ||  tin  ||  Sn  || 0.25 || 55
|-
|62  ||  samarium  ||  Sm  || 0.27 || 47
|-
|68  ||  erbium  ||  Er  || 0.30 || 47
|-
|70  ||  ytterbium  ||  Yb  || 0.30 || 45
|-
|59  ||  praseodymium  ||  Pr  || 0.17 || 31
|-
|82  ||  lead  ||  Pb  || 0.23 || 29
|-
|72  ||  hafnium  ||  Hf  || 0.19 || 28
|-
|74  ||  tungsten  ||  W  || 0.17 || 24
|-
|79  ||  gold  ||  Au  || 0.16 || 21
|-
|48  ||  cadmium  ||  Cd  || 0.08 || 18
|-
|63  ||  europium  ||  Eu  || 0.10 || 17
|-
|67  ||  holmium  ||  Ho  || 0.10 || 16
|-
|47  ||  silver  ||  Ag  || 0.05 || 12
|-
|65  ||  terbium  ||  Tb  || 0.07 || 11
|-
|51  ||  antimony  ||  Sb  || 0.05 || 11
|-
|75  ||  rhenium  ||  Re  || 0.08 || 10
|-
|53  ||  iodine  ||  I  || 0.05 || 10
|-
|69  ||  thulium  ||  Tm  || 0.05 || 7
|-
|55  ||  caesium  ||  Cs  || 0.04 || 7
|-
|71  ||  lutetium  ||  Lu  || 0.05 || 7
|-
|90  ||  thorium  ||  Th  || 0.06 || 6
|-
|73  ||  tantalum  ||  Ta  || 0.03 || 4
|-
|80  ||  mercury  ||  Hg  || 0.02 || 3
|-
|92  ||  uranium  ||  U  || 0.02 || 2
|-
|49  ||  indium  ||  In  || 0.01 || 2
|-
|81  ||  thallium  ||  Tl  || 0.01 || 2
|-
|83  ||  bismuth  ||  Bi  || 0.01 || 1
|}

=== Crust ===
{{main|Abundance of elements in Earth's crust}}

[[File:Elemental abundances.svg|thumb|400px|right|alt=refer to text|Abundance ([[atom fraction]]) of the elements in Earth's upper continental crust as a function of atomic number. The rarest elements in the crust (shown in yellow) are rare due to multiple factors: all but one are the densest [[siderophile]]s (iron-loving) elements in the [[Goldschmidt classification]], meaning they mix well with metallic iron, depleting them by relocating them deeper into Earth's core. Their abundance in [[meteoroid]]s is higher. Tellurium has also been depleted by preaccretional sorting in the nebula via formation of volatile [[hydrogen telluride]].<ref name="Chemical"/>]]

The mass-abundance of the nine most abundant elements in the Earth's crust is roughly: oxygen 46%, silicon 28%, aluminium 8.3%, iron 5.6%, calcium 4.2%, sodium 2.5%, magnesium 2.4%, potassium 2.0%, and titanium 0.61%. Other elements occur at less than 0.15%. For a full list, see [[abundance of elements in Earth's crust]].

The graph at right illustrates the relative atomic-abundance of the chemical elements in Earth's upper continental crust—the part that is relatively accessible for measurements and estimation.

Many of the elements shown in the graph are classified into (partially overlapping) categories:

#  rock-forming elements (major elements in green field, and minor elements in light green field);
#  [[rare earth element]]s (lanthanides (La–Lu), Sc, and Y; labeled in blue);
#  major industrial metals (global production >~3×10{{sup|7}} kg/year; labeled in red);
#  [[precious metal]]s (labeled in purple);
#  the nine rarest "metals" – the six [[platinum group]] elements plus [[Gold|Au]], [[Rhenium|Re]], and [[Tellurium|Te]] (a metalloid) – in the yellow field. These are rare in the crust from being soluble in iron and thus concentrated in Earth's core. Tellurium is the single most depleted element in the silicate Earth relative to cosmic abundance, because in addition to being concentrated as dense chalcogenides in the core it was severely depleted by preaccretional sorting in the nebula as volatile [[hydrogen telluride]].<ref name="Chemical"/>

There are two breaks where the unstable elements [[technetium]] (atomic number 43) and [[promethium]] (number 61) would be. These elements are surrounded by stable elements, yet their most stable isotopes have relatively short half lives (~4 million years and ~18 years respectively). These are thus extremely rare, since any primordial amounts of these elements have long since decayed. These two elements are now only produced naturally through [[spontaneous fission]] of very heavy [[radioactive]] elements (such as [[uranium]], [[thorium]], or the trace amounts of [[plutonium]] that exist in uranium ores), or by the interaction of certain other elements with [[cosmic ray]]s. Both technetium and promethium have been identified spectroscopically in the atmospheres of stars, where they are produced by ongoing nucleosynthetic processes.

There are also breaks in the abundance graph where the six [[noble gas]]es would be, since they are not chemically bound in the Earth's crust, and so their crustal abundance is not well-defined.

The eight naturally occurring very rare, highly radioactive elements ([[polonium]], [[astatine]], [[francium]], [[radium]], [[actinium]], [[protactinium]], [[neptunium]], and [[plutonium]]) are not included, since any of these elements that were present at the formation of the Earth have decayed eons ago, and their quantity today is negligible and is only produced from [[radioactive decay]] of uranium and thorium.

[[Oxygen]] and [[silicon]] are the most common elements in the crust. On Earth and rocky planets in general, silicon and oxygen are far more common than their cosmic abundance. The reason is that they combine with each other to form [[silicate mineral]]s.<ref name="Chemical">Anderson, Don L.; ‘Chemical Composition of the Mantle’ in ''Theory of the Earth'', pp. 147–175 {{ISBN|0865421234}}</ref> Other cosmically common elements such as [[hydrogen]], [[carbon]] and [[nitrogen]] form volatile compounds such as [[ammonia]] and [[methane]] that easily boil away into space from the heat of planetary formation and/or the Sun's light.

==== Rare-earth elements ====
"Rare" earth elements is a historical misnomer. The persistence of the term reflects unfamiliarity rather than true rarity. The more abundant [[rare earth element]]s are similarly concentrated in the crust compared to commonplace industrial metals such as chromium, nickel, copper, zinc, molybdenum, tin, tungsten, or lead. The two least abundant stable rare earth elements ([[thulium]] and [[lutetium]]) are nearly 200 times more common than [[gold]]. However, in contrast to the ordinary base and precious metals, rare earth elements have very little tendency to become concentrated in exploitable ore deposits. Consequently, most of the world's supply of rare earth elements comes from only a handful of sources. Furthermore, the rare earth metals are all quite chemically similar to each other, and they are thus quite difficult to separate into quantities of the pure elements.

Differences in abundances of individual rare earth elements in the upper continental crust of the Earth represent the superposition of two effects, one nuclear and one geochemical. First, the rare earth elements with even atomic numbers (<sub>58</sub>Ce, <sub>60</sub>Nd, ...) have greater cosmic and terrestrial abundances than the adjacent rare earth elements with odd atomic numbers (<sub>57</sub>La, <sub>59</sub>Pr, ...). Second, the lighter rare earth elements are more incompatible (because they have larger ionic radii) and therefore more strongly concentrated in the continental crust than the heavier rare earth elements. In most rare earth ore deposits, the first four rare earth elements – [[lanthanum]], [[cerium]], [[praseodymium]], and [[neodymium]] – constitute 80% to 99% of the total amount of rare earth metal that can be found in the ore.
{{Clear}}

=== Mantle ===
{{main|Earth's mantle}}

The mass-abundance of the seven most abundant elements in the Earth's mantle is approximately: oxygen 44.3%, magnesium 22.3%, silicon 21.3%, iron 6.32%, calcium 2.48%, aluminium 2.29%, nickel 0.19%.<ref>{{Cite journal |last1=Wang |first1=Haiyang S. |last2=Lineweaver |first2=Charles H. |last3=Ireland |first3=Trevor R. |date=2018-01-01 |title=The elemental abundances (with uncertainties) of the most Earth-like planet |url=https://www.sciencedirect.com/science/article/pii/S0019103517302221 |journal=Icarus |language=en |volume=299 |pages=460–474 |doi=10.1016/j.icarus.2017.08.024 |hdl=1885/139094 |s2cid=119434532 |issn=0019-1035|hdl-access=free }}</ref>

=== Core ===
{{see also|Structure of Earth#Core}}

Due to [[Planetary differentiation#Gravitational separation|mass segregation]], the core of the Earth is believed to be primarily composed of iron (88.8%), with smaller amounts of nickel (5.8%), sulfur (4.5%), and less than 1% trace elements.<ref name="Arnett"/>

=== Ocean ===
{{for|a complete list|Abundances of the elements (data page)#Sea water}}
{{see also|Seawater#Chemical composition}}

The most abundant elements in the ocean by proportion of mass in percent are oxygen (85.84%), hydrogen (10.82%), chlorine (1.94%), sodium (1.08%), magnesium (0.13%), sulfur (0.09%), calcium (0.04%), potassium (0.04%), bromine (0.007%), carbon (0.003%), and boron (0.0004%).

=== Atmosphere ===
{{see also|Atmosphere of Earth#Composition}}

The order of elements by volume fraction (which is approximately molecular mole fraction) in the [[Earth's atmosphere|atmosphere]] is [[nitrogen]] (78.1%), [[oxygen]] (20.9%),<ref name="NYT-20131003">{{cite news |last=Zimmer |first=Carl |author-link=Carl Zimmer |title=Earth's Oxygen: A Mystery Easy to Take for Granted |url=https://www.nytimes.com/2013/10/03/science/earths-oxygen-a-mystery-easy-to-take-for-granted.html |date=3 October 2013 |work=[[The New York Times]] |access-date=3 October 2013 |url-status=live |archive-url=https://web.archive.org/web/20131003185748/http://www.nytimes.com/2013/10/03/science/earths-oxygen-a-mystery-easy-to-take-for-granted.html |archive-date=3 October 2013 }}</ref> [[argon]] (0.96%), followed by (in uncertain order) carbon and hydrogen because water vapor and carbon dioxide, which represent most of these two elements in the air, are variable components. Sulfur, phosphorus, and all other elements are present in significantly lower proportions.

According to the abundance curve graph, argon, a significant if not major component of the atmosphere, does not appear in the crust at all. This is because the atmosphere has a far smaller mass than the crust, so argon remaining in the crust contributes little to mass fraction there, while at the same time buildup of argon in the atmosphere has become large enough to be significant. <!--it's not that argon can't stay in the crust due to being inert. Helium stays in the crust well enough! And there is argon trapped in rocks or K-Ar dating would not work. Instead, the reason is the one given.-->
{{Clear}}

=== Urban soils ===
''For a complete list of the abundance of elements in urban soils, see [[Abundances of the elements (data page)#Urban soils]].''
{{see also|Soil#Chemistry}}

== Human body ==
{{main|Composition of the human body}}
{| class="wikitable collapsible collapsed"  style="float:right;"
|+ Elemental abundance in the human body
|-
! Element !! Proportion (by mass)
|-
| [[Oxygen]]    || 65
|-
| [[Carbon]]    || 18
|-
| [[Hydrogen]]  || 10
|-
| [[Nitrogen]]  ||  3
|-
| [[Calcium]]   || 1.5
|-
| [[Phosphorus]]|| 1.2
|-
| [[Potassium]] || 0.2
|-
| [[Sulfur]]    || 0.2
|-
| [[Chlorine]]  || 0.2
|-
| [[Sodium]]    || 0.1
|-
| [[Magnesium]] || 0.05
|-
| [[Iron]]      || &lt; 0.05
|-
| [[Cobalt]]    || &lt; 0.05
|-
| [[Copper]]    || &lt; 0.05
|-
| [[Zinc]]      || &lt; 0.05
|-
| [[Iodine]]    || &lt; 0.05
|-
| [[Selenium]]  || &lt; 0.01
|}
[[File:element_abundance_human_body_ppm_chart.svg|thumb|[[Parts-per-million]] cube of relative abundance by mass of elements in an average adult human down to 1 ppm]]
By mass, human cells consist of 65–90% water (H<sub>2</sub>O), and a significant portion of the remainder is composed of carbon-containing organic molecules. Oxygen therefore contributes a majority of a human body's mass, followed by carbon. Almost 99% of the mass of the human body is made up of six elements: [[hydrogen]] (H), [[carbon]] (C), [[nitrogen]] (N), [[oxygen]] (O), [[calcium]] (Ca), and [[phosphorus]] (P) . The next 0.75% is made up of the next five elements: [[potassium]] (K), [[sulfur]] (S), [[chlorine]] (Cl), [[sodium]] (Na), and [[magnesium]] (Mg). Only 17 elements are known for certain to be necessary to human life, with one additional element (fluorine) thought to be helpful for tooth enamel strength. A few more [[trace element]]s may play some role in the health of mammals. [[Boron]] and [[silicon]] are notably necessary for plants but have uncertain roles in animals. The elements aluminium and silicon, although very common in the earth's crust, are conspicuously rare in the human body.<ref>Table data from {{cite book
  | last = Chang
  | first = Raymond
  | title = Chemistry
  | edition = Ninth
  | publisher = [[McGraw-Hill]]
  | date = 2007
  | page = 52
  | isbn = 978-0-07-110595-8 }}
</ref>

Below is a periodic table highlighting nutritional elements.<ref>{{cite book |chapter=Ultratrace minerals |last=Nielsen |first=Forrest H. |title=Modern nutrition in health and disease |editor=Maurice E. Shils |editor2=James A. Olsen |editor3=Moshe Shine |editor4=A. Catharine Ross |location=Baltimore |publisher=Lippincott Williams & Wilkins |year=1999 |pages=283–303 |hdl=10113/46493 |hdl-access=free |isbn=978-0683307696}}</ref>

{{Periodic table (nutritional elements)}}

== See also ==
* {{Annotated link|Abundances of the elements (data page)}}
* {{Annotated link|Abundance of elements in Earth's crust}}
* [[Natural abundance]] – isotopic abundance
* {{Annotated link|Goldschmidt classification}}
* {{Annotated link|Primordial nuclide}}
* {{Annotated link|Radiative levitation}}
* [[List of data references for chemical elements]]

==References==

===Footnotes===
{{reflist}}

===Notes===

{{reflist|group=Note}}

===Notations===
* {{Cite web|title=Rare Earth Elements—Critical Resources for High Technology {{!}} USGS Fact Sheet 087-02|url=http://geopubs.wr.usgs.gov/fact-sheet/fs087-02/|website=geopubs.wr.usgs.gov}}
* {{Cite web|title=Imagine the Universe! Dictionary |url=http://imagine.gsfc.nasa.gov:80/docs/dict_ei.html |archive-url=https://web.archive.org/web/20031203202925/http://imagine.gsfc.nasa.gov/docs/dict_ei.html |url-status=dead |archive-date=3 December 2003 |date=3 December 2003 }}

== External links ==
* [https://www.science.co.il/elements/?s=Earth List of elements in order of abundance in the Earth's crust] (only correct for the twenty most common elements)
* [https://web.archive.org/web/20060901133923/http://www.astro.wesleyan.edu/~bill/courses/astr231/wes_only/element_abundances.pdf Cosmic abundance of the elements and nucleosynthesis]
* [https://web.archive.org/web/20160303223016/http://www.webelements.com/periodicity/ WebElements.com] Lists of elemental abundances for the Universe, Sun, meteorites, Earth, ocean, streamwater, etc.

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