Group 12 element
|Group 12 in the periodic table|
30 Transition metal
48 Transition metal
80 Transition metal
112 Transition metal
Group 12, by modern IUPAC numbering, is a group of chemical elements in the periodic table. It includes zinc (Zn), cadmium (Cd) and mercury (Hg). The further inclusion of copernicium (Cn) in group 12 is supported by recent experiments on individual copernicium atoms. Group 12 is also known as the volatile metals, although this can also more generally refer to any metal (which need not be in group 12) that has high volatility, such as polonium or flerovium. Formerly this group was named IIB (pronounced as "group two B", as the "II" is a Roman numeral) by CAS and old IUPAC system.
The three group 12 elements that occur naturally are zinc, cadmium and mercury. They are all widely used in electric and electronic applications, as well as in various alloys. The first two members of the group share similar properties as they are solid metals under standard conditions. Mercury is the only metal that is a liquid at room temperature. While zinc is very important in the biochemistry of living organisms, cadmium and mercury are both highly toxic. As copernicium does not occur in nature, it has to be synthesized in the laboratory.
- 1 Physical and atomic properties
- 2 Chemistry
- 3 Extensions
- 4 History
- 5 Occurrence
- 6 Production
- 7 Applications
- 8 Biological role and toxicity
- 9 Notes
- 10 References
- 11 Bibliography
Physical and atomic properties
|Z||Element||No. of electrons/shell|
|30||zinc||2, 8, 18, 2|
|48||cadmium||2, 8, 18, 18, 2|
|80||mercury||2, 8, 18, 32, 18, 2|
|112||copernicium||2, 8, 18, 32, 32, 18, 2 (predicted)|
Group 12 elements are all soft, diamagnetic, divalent metals. They have the lowest melting points among all transition metals. Zinc is bluish-white and lustrous, though most common commercial grades of the metal have a dull finish. Zinc is also referred to in nonscientific contexts as spelter. Cadmium is soft, malleable, ductile, and with a bluish-white color. Mercury is a liquid, heavy, silvery-white metal. It is the only common liquid metal at ordinary temperatures, and as compared to other metals, it is a poor conductor of heat, but a fair conductor of electricity.
The table below is a summary of the key physical properties of the group 12 elements. Very little is known about copernicium, and none of its physical properties have been confirmed except for its boiling point (tentative).
|Melting point||693 K (420 °C)||594 K (321 °C)||234 K (−39 °C)||?|
|Boiling point||1180 K (907 °C)||1040 K (767 °C)||630 K (357 °C)||357+112
−108 K (84+112
|Density||7.14 g·cm−3||8.65 g·cm−3||13.534 g·cm−3||? 23.7 g·cm−3|
|Appearance||silvery bluish-gray metallic||silver-gray||silvery||?|
|Atomic radius||135 pm||155 pm||150 pm||? 147 pm|
Zinc is somewhat less dense than iron and has a hexagonal crystal structure. The metal is hard and brittle at most temperatures but becomes malleable between 100 and 150 °C. Above 210 °C, the metal becomes brittle again and can be pulverized by beating. Zinc is a fair conductor of electricity. For a metal, zinc has relatively low melting (419.5 °C, 787.1 F) and boiling points (907 °C). Cadmium is similar in many respects to zinc but forms complex compounds. Unlike other metals, cadmium is resistant to corrosion and as a result it is used as a protective layer when deposited on other metals. As a bulk metal, cadmium is insoluble in water and is not flammable; however, in its powdered form it may burn and release toxic fumes. Mercury has an exceptionally low melting temperature for a d-block metal. A complete explanation of this fact requires a deep excursion into quantum physics, but it can be summarized as follows: mercury has a unique electronic configuration where electrons fill up all the available 1s, 2s, 2p, 3s, 3p, 3d, 4s, 4p, 4d, 4f, 5s, 5p, 5d and 6s subshells. As such configuration strongly resists removal of an electron, mercury behaves similarly to noble gas elements, which form weak bonds and thus easily melting solids. The stability of the 6s shell is due to the presence of a filled 4f shell. An f shell poorly screens the nuclear charge that increases the attractive Coulomb interaction of the 6s shell and the nucleus (see lanthanide contraction). The absence of a filled inner f shell is the reason for the somewhat higher melting temperature of cadmium and zinc, although both these metals still melt easily and, in addition, have unusually low boiling points. Gold has atoms with one less 6s electron than mercury. Those electrons are more easily removed and are shared between the gold atoms forming relatively strong metallic bonds.
Zinc, cadmium and mercury form a large range of alloys. Among the zinc containing ones, brass is an alloy of zinc and copper. Other metals long known to form binary alloys with zinc are aluminium, antimony, bismuth, gold, iron, lead, mercury, silver, tin, magnesium, cobalt, nickel, tellurium and sodium. While neither zinc nor zirconium are ferromagnetic, their alloy ZrZn
2 exhibits ferromagnetism below 35 K. Cadmium is used in many kinds of solder and bearing alloys, due to a low coefficient of friction and fatigue resistance. It is also found in some of the lowest-melting alloys, such as Wood's metal. Because it is a liquid, mercury dissolves other metals and the alloys that are formed are called amalgams. For example, such amalgams are known with gold, zinc, sodium, and many other metals. Because iron is an exception, iron flasks have been traditionally used to trade mercury. Other metals that do not form amalgams with mercury include tantalum, tungsten and platinum. Sodium amalgam is a common reducing agent in organic synthesis, and is also used in high-pressure sodium lamps. Mercury readily combines with aluminium to form a mercury-aluminium amalgam when the two pure metals come into contact. Since the amalgam reacts with air to give aluminium oxide, small amounts of mercury corrode aluminium. For this reason, mercury is not allowed aboard an aircraft under most circumstances because of the risk of it forming an amalgam with exposed aluminium parts in the aircraft.
Most of the chemistry has been observed only for the first three members of the group 12. The chemistry of copernicium is not well established and therefore the rest of the section deals only with zinc, cadmium and mercury.
All elements in this group are metals. The similarity of the metallic radii of cadmium and mercury is an effect of the lanthanide contraction. So, the trend in this group is unlike the trend in group 2, the alkaline earths, where metallic radius increases smoothly from top to bottom of the group. All three metals have relatively low melting and boiling points, indicating that the metallic bond is relatively weak, with relatively little overlap between the valence band and the conduction band. Thus, zinc is close to the boundary between metallic and metalloid elements, which is usually placed between gallium and germanium, though gallium participates in semi-conductors such as gallium arsenide.
Zinc and cadmium are electropositive while mercury is not. As a result, zinc and cadmium metal are good reducing agents. The elements of group 12 have an oxidation state of +2 in which the ions have the rather stable d10 electronic configuration, with a full sub-shell. However, mercury can easily be reduced to the +1 oxidation state; usually, as in the ion Hg2+
2, two mercury(I) ions come together to form a metal-metal bond and a diamagnetic species. Cadmium can also form species such as [Cd2Cl6]4− in which the metal's oxidation state is +1. Just as with mercury, the formation of a metal-metal bond results in a diamagnetic compound in which there are no unpaired electrons; thus, making the species very reactive. Zinc(I) is known only in the gas phase, in such compounds as linear Zn2Cl2, analogous to calomel.
The elements in group 12 are usually considered to be d-block elements, but not transition elements as the d-shell is full. Some authors classify these elements as main-group elements because the valence electrons are in ns2 orbitals. Nevertheless, they share many characteristics with the neighboring group 11 elements on the periodic table, which are almost universally considered to be transition elements. For example, zinc shares many characteristics with the neighboring transition metal, copper. Zinc complexes merit inclusion in the Irving-Williams series as zinc forms many complexes with the same stoichiometry as complexes of copper(II), albeit with smaller stability constants. There is little similarity between cadmium and silver as compounds of silver(II) are rare and those that do exist are very strong oxidizing agents. Likewise the common oxidation state for gold is +3, which precludes there being much common chemistry between mercury and gold, though there are similarities between mercury(I) and gold(I) such as the formation of linear dicyano complexes, [M(CN)2]−. According to IUPAC's definition of transition metal as an element whose atom has an incomplete d sub-shell, or which can give rise to cations with an incomplete d sub-shell, zinc and cadmium are not transition metals, while mercury is. This is because only mercury is known to have a compound where its oxidation state is higher than +2, in mercury(IV) fluoride. However, this classification is based on one highly atypical compound seen at non-equilibrium conditions and is at odds to mercury's more typical chemistry, and Jensen has suggested that it would be better to regard mercury as not being a transition metal.
Relationship with the alkaline earth metals
Although group 12 lies in the d-block of the modern 18-column periodic table, the d electrons of zinc, cadmium, and (almost always) mercury behave as core electrons and do not take part in bonding. This behavior is similar to that of the main-group elements, but is in stark contrast to that of the neighboring group 11 elements (copper, silver, and gold), which also have filled d-subshells in their ground-state electron configuration but behave chemically as transition metals. For example, the bonding in chromium(II) sulfide (CrS) involves mainly the 3d electrons; that in iron(II) sulfide (FeS) involves both the 3d and 4s electrons; but that of zinc sulfide (ZnS) involves only the 4s electrons and the 3d electrons behave as core electrons. Indeed, useful comparison can be made between their properties and the first two members of group 2, beryllium and magnesium, and in earlier short-form periodic table layouts, this relationship is illustrated more clearly. For instance, zinc and cadmium are similar to beryllium and magnesium in their atomic radii, ionic radii, electronegativities, and also in the structure of their binary compounds and their ability to form complex ions with many nitrogen and oxygen ligands, such as complex hydrides and amines. However, beryllium and magnesium are small atoms, unlike the heavier alkaline earth metals and like the group 12 elements (which have a greater nuclear charge but the same number of valence electrons), and the periodic trends down group 2 from beryllium to radium (similar to that of the alkali metals) are not as smooth when going down from beryllium to mercury (which is more similar to that of the p-block main groups) due to the d-block and lanthanide contractions. It is also the d-block and lanthanide contractions that give mercury many of its distinctive properties.
|Valence electron configuration||2s2||3s2||4s2||5s2||6s2||7s2|
|Core electron configuration||[He]||[Ne]||[Ar]||[Kr]||[Xe]||[Rn]|
|Oxidation states[note 1]||+2, +1||+2, +1||+2, +1||+2, +1||+2||+2|
|Melting point||1560 K (1287 °C)||923 K (650 °C)||1115 K (842 °C)||1050 K (777 °C)||1000 K (727 °C)||973 K (700 °C)|
|Boiling point||2742 K (2469 °C)||1363 K (1090 °C)||1757 K (1484 °C)||1655 K (1382 °C)||2170 K (1897 °C)||2010 K (1737 °C)|
|Appearance||white-gray metallic||shiny gray metallic||dull silver-gray||silvery white metallic||silvery gray||silvery white metallic|
|Density||1.85 g·cm−3||1.738 g·cm−3||1.55 g·cm−3||2.64 g·cm−3||3.51 g·cm−3||5.5 g·cm−3|
|Atomic radius||105 pm||150 pm||180 pm||200 pm||215 pm||215 pm|
|Crystal ionic radius||59 pm||86 pm||114 pm||132 pm||149 pm||162 pm|
|Flame test color||white||brilliant white||brick-red||crimson||apple green||crimson red[note 2]|
|Organometallic chemistry||good||good||poor||very poor||very poor||extremely poor|
|Hydroxide||amphoteric||basic||basic||strongly basic||strongly basic||strongly basic|
|Oxide||amphoteric||strongly basic||strongly basic||strongly basic||strongly basic||strongly basic|
|Valence electron configuration||2s2||3s2||4s2||5s2||6s2||? 7s2|
|Core electron configuration||[He]||[Ne]||[Ar]3d10||[Kr]4d10||[Xe]4f145d10||? [Rn]5f146d10|
|Oxidation states[note 1]||+2, +1||+2, +1||+2, +1||+2, +1||+4, +2, +1||? +4, +2, +1, 0|
|Melting point||1560 K (1287 °C)||923 K (650 °C)||693 K (420 °C)||594 K (321 °C)||234 K (−39 °C)||?|
|Boiling point||2742 K (2469 °C)||1363 K (1090 °C)||1180 K (907 °C)||1040 K (767 °C)||630 K (357 °C)||357+112
−108 K (84+112
|Appearance||white-gray metallic||shiny gray metallic||silvery bluish-gray metallic||silver-gray||silvery||?|
|Density||1.85 g·cm−3||1.738 g·cm−3||7.14 g·cm−3||8.65 g·cm−3||13.534 g·cm−3||? 23.7 g·cm−3|
|Atomic radius||105 pm||150 pm||135 pm||155 pm||150 pm||? 147 pm|
|Crystal ionic radius||59 pm||86 pm||88 pm||109 pm||116 pm||? 75 pm|
|Flame test color||white||brilliant white||bluish-green[note 3]||?||?||?|
|Oxide||amphoteric||strongly basic||amphoteric||mildly basic||mildly basic||?|
All three metal ions form many tetrahedral species, such as MCl2−
4. Both zinc and cadmium can also form octahedral complexes such as the aqua ions [M(H2O)6]2+ which are present in aqueous solutions of salts of these metals. Covalent character is achieved by using the s and possibly p orbitals. Mercury, however, rarely exceeds a coordination number of four. Coordination numbers of 2, 3, 5, 7 and 8 are also known.
Although copernicium is the heaviest known group 12 element, there has been some theoretical work regarding possible heavier group 12 elements. Although a simple extrapolation of the periodic table would put element 162, unhexbium (Uhb), under copernicium, relativistic Dirac-Fock calculations predict that the next group 12 element after copernicium should actually be element 164, unhexquadium (Uhq), which is predicted to have an electron configuration of [Uuo] 5g18 6f14 7d10 8s2 8p1/22. The 8s and 8p1/2 orbitals are predicted to be so strongly stabilized relativistically that they become core electrons and do not participate in chemical reactions, unlike the earlier group 12 elements where the s electrons behave as valence electrons. However, the 9s and 9p1/2 levels are expected to be readily available for hybridization and bonding, so that unhexquadium should still behave chemically like a normal transition metal. Calculations predict that the 7d electrons of unhexquadium should participate very readily in chemical reactions, so that unhexquadium should be able to show stable +6 and +4 oxidation states in addition to the normal +2 state in aqueous solutions with strong ligands. Unhexquadium should thus be able to form compounds like Uhq(CO)4, Uhq(PF3)4 (both tetrahedral), and Uhq(CN)2−
2 (linear), which is very different behavior from that of lead, which unhexquadium would be a heavier homologue of if not for relativistic effects. Nevertheless, the divalent state would be the main one in aqueous solution, and unhexquadium(II) should behave more similarly to lead than unhexquadium(IV) and unhexquadium(VI).
Unhexquadium should be a soft metal like mercury, and metallic unhexquadium should have a high melting point as it is predicted to bond covalently. It is also expected to be a soft Lewis acid and have Ahrlands softness parameter close to 4 eV. It should also have some similarities to ununoctium as well as to the other group 12 elements. Unhexquadium should be at most moderately reactive, having a first ionization energy that should be around 685 kJ/mol, comparable to that of molybdenum. Due to the lanthanide, actinide, and superactinide contractions, unhexquadium should have a metallic radius of only 158 pm, very close to that of the much lighter magnesium, despite its being expected to have an atomic weight of around 474 u, about 19.5 times as much as that of magnesium. This small radius and high weight cause it to be expected to have an extremely high density of around 46 g·cm−3, over twice that of osmium, currently the most dense element known, at 22.61 g·cm−3; unhexquadium should be the second most dense element in the first 9 periods of the periodic table, with only its neighbour unhextrium (element 163) being more dense (at 47 g·cm−3). Metallic unhexquadium should be quite stable, as the 8s and 8p1/2 electrons are very deeply buried in the electron core and only the 7d electrons are available for bonding. Metallic unhexquadium should have a very large cohesive energy due to its covalent bonds, most probably resulting in a high melting point.
Theoretical interest in the chemistry of unhexquadium is largely motivated by theoretical predictions that it, especially the isotope 482Uhq (with 164 protons and 318 neutrons), would be at the center of a hypothetical second island of stability (the first being centered around 306Ubb, with 122 protons and 184 neutrons).
The elements of group 12 have been found throughout history, being used since ancient times to being discovered in laboratories. The group itself has not acquired a trivial name, but it has been called group IIB in the past.
Zinc has been found being used in impure forms in ancient times as well as in alloys such as brass that have been found to be over 2000 years old. Zinc was distinctly recognized as a metal under the designation of Fasada in the medical Lexicon ascribed to the Hindu king Madanapala and written about the year 1374. The metal was also of use to alchemists. The name of the metal was first documented in the 16th century, and is probably derived from the German zinke for the needle-like appearance of metallic crystals.
The isolation of metallic zinc in the West may have been achieved independently by several people in the 17th century. German chemist Andreas Marggraf is usually given credit for discovering pure metallic zinc in a 1746 experiment by heating a mixture of calamine and charcoal in a closed vessel without copper to obtain a metal. Experiments on frogs by the Italian doctor Luigi Galvani in 1780 with brass paved the way for the discovery of electrical batteries, galvanization and cathodic protection. In 1880, Galvani's friend, Alessandro Volta, invented the Voltaic pile. The biological importance of zinc was not discovered until 1940 when carbonic anhydrase, an enzyme that scrubs carbon dioxide from blood, was shown to have zinc in its active site.
In 1817, cadmium was discovered in Germany as an impurity in zinc carbonate minerals (calamine) by Friedrich Stromeyer and Karl Samuel Leberecht Hermann. It was named after the Latin cadmia for "calamine", a cadmium-bearing mixture of minerals, which was in turn named after the Greek mythological character, Κάδμος Cadmus, the founder of Thebes. Stromeyer eventually isolated cadmium metal by roasting and reduction of the sulfide.
In 1927, the International Conference on Weights and Measures redefined the meter in terms of a red cadmium spectral line (1 m = 1,553,164.13 wavelengths). This definition has since been changed (see krypton). At the same time, the International Prototype Meter was used as standard for the length of a meter until 1960, when at the General Conference on Weights and Measures the meter was defined in terms of the orange-red emission line in the electromagnetic spectrum of the krypton-86 atom in vacuum.
Mercury has been found in Egyptian tombs which have been dated back to 1500 BC, where mercury was used in cosmetics. It was also used by the ancient Chinese who believed it would improve and prolong health. By 500 BC mercury was used to make amalgams (Medieval Latin amalgama, "alloy of mercury") with other metals. Alchemists thought of mercury as the First Matter from which all metals were formed. They believed that different metals could be produced by varying the quality and quantity of sulfur contained within the mercury. The purest of these was gold, and mercury was called for in attempts at the transmutation of base (or impure) metals into gold, which was the goal of many alchemists.
Hg is the modern chemical symbol for mercury. It comes from hydrargyrum, a Latinized form of the Greek word Ύδραργυρος (hydrargyros), which is a compound word meaning "water-silver" (hydr- = water, argyros = silver) — since it is liquid like water and shiny like silver. The element was named after the Roman god Mercury, known for speed and mobility. It is associated with the planet Mercury; the astrological symbol for the planet is also one of the alchemical symbols for the metal. Mercury is the only metal for which the alchemical planetary name became the common name.
The heaviest known group 12 element, copernicium, was first created on February 9, 1996, at the Gesellschaft für Schwerionenforschung (GSI) located in Darmstadt, Germany by Sigurd Hofmann, Victor Ninov et al. It was then officially named by the International Union of Pure and Applied Chemistry after Nicolaus Copernicus on February 19, 2010, the 537th anniversary of Copernicus' birth.
Like in most other d-block groups, the abundance in Earth's crust of group 12 elements decreases with higher atomic number. Zinc is with 65 parts per million (ppm) the most abundant in the group while cadmium with 0.1 ppm and mercury with 0.08 ppm are orders of magnitude less abundant. Copernicium, as a synthetic element with a half-life of a few minutes, may only be present in the laboratories where it was produced.
Group 12 metals are chalcophiles, meaning the elements have low affinities for oxides and prefer to bond with sulfides. Chalcophiles formed as the crust solidified under the reducing conditions of the early Earth's atmosphere. The commercially most important minerals of group 12 elements are sulfide minerals. Sphalerite, which is a form of zinc sulfide, is the most heavily mined zinc-containing ore because its concentrate contains 60–62% zinc. No significant deposits of cadmium-containing ores are known. Greenockite (CdS), the only cadmium mineral of importance, is nearly always associated with sphalerite (ZnS). This association is caused by the geochemical similarity between zinc and cadmium which makes geological separation unlikely. As a consequence, cadmium is produced mainly as a byproduct from mining, smelting, and refining sulfidic ores of zinc, and, to a lesser degree, lead and copper. One place where metallic cadmium can be found is the Vilyuy River basin in Siberia. Although mercury is an extremely rare element in the Earth's crust, because it does not blend geochemically with those elements that constitute the majority of the crustal mass, mercury ores can be highly concentrated considering the element's abundance in ordinary rock. The richest mercury ores contain up to 2.5% mercury by mass, and even the leanest concentrated deposits are at least 0.1% mercury (12,000 times average crustal abundance). It is found either as a native metal (rare) or in cinnabar (HgS), corderoite, livingstonite and other minerals, with cinnabar being the most common ore.
While mercury and zinc minerals are found in large enough quantities to be mined, cadmium is too similar to zinc and therefore is always present in small quantities in zinc ores from where it is recovered. Identified world zinc resources total about 1.9 billion tonnes. Large deposits are in Australia, Canada and the United States with the largest reserves in Iran. At the current rate of consumption, these reserves are estimated to be depleted sometime between 2027 and 2055. About 346 million tonnes have been extracted throughout history to 2002, and one estimate found that about 109 million tonnes of that remains in use. In 2005, China was the top producer of mercury with almost two-thirds global share followed by Kyrgyzstan. Several other countries are believed to have unrecorded production of mercury from copper electrowinning processes and by recovery from effluents. Because of the high toxicity of mercury, both the mining of cinnabar and refining for mercury are hazardous and historic causes of mercury poisoning.
Zinc is the fourth most common metal in use, trailing only iron, aluminium, and copper with an annual production of about 10 million tonnes. Worldwide, 95% of the zinc is mined from sulfidic ore deposits, in which sphalerite (ZnS) is nearly always mixed with the sulfides of copper, lead and iron. Zinc metal is produced using extractive metallurgy. Roasting converts the zinc sulfide concentrate produced during processing to zinc oxide: For further processing two basic methods are used: pyrometallurgy or electrowinning. Pyrometallurgy processing reduces zinc oxide with carbon or carbon monoxide at 950 °C (1,740 °F) into the metal, which is distilled as zinc vapor. The zinc vapor is collected in a condenser. Electrowinning processing leaches zinc from the ore concentrate by sulfuric acid: After this step electrolysis is used to produce zinc metal.
Cadmium is a common impurity in zinc ores, and it is most isolated during the production of zinc. Some zinc ores concentrates from sulfidic zinc ores contain up to 1.4% of cadmium. Cadmium is isolated from the zinc produced from the flue dust by vacuum distillation if the zinc is smelted, or cadmium sulfate is precipitated out of the electrolysis solution.
The richest mercury ores contain up to 2.5% mercury by mass, and even the leanest concentrated deposits are at least 0.1% mercury, with cinnabar (HgS) being the most common ore in the deposits. Mercury is extracted by heating cinnabar in a current of air and condensing the vapor.
Super-heavy elements such as copernicium are produced by bombarding lighter elements in particle accelerators that induces fusion reactions. Whereas most of the isotopes of copernicium can be synthesized directly this way, some heavier ones have only been observed as decay products of elements with higher atomic numbers. The first fusion reaction to produce copernicium was performed by GSI in 1996, who reported the detection of two decay chains of copernicium-277.
In total, approximately 75 atoms of copernicium have been prepared using various nuclear reactions.
Due to the physical similarities which they share, the group 12 elements can be found in many common situations. Zinc and cadmium are commonly used as anti-corrosion (galvanization) agents as they will attract all local oxidation until they completely corrode. These protective coatings can be applied to other metals through by hot-dip galvanizing a substance into the molten form of the metal, or through the process of electroplating which may be passivated by the use of chromate salts. Group 12 elements are also used in electrochemistry as they may act as an alternative to the standard hydrogen electrode in addition to being a secondary reference electrode.
In the US, zinc is used predominantly for galvanizing (55%) and for brass, bronze and other alloys (37%). The relative reactivity of zinc and its ability to attract oxidation to itself makes it an efficient sacrificial anode in cathodic protection (CP). For example, cathodic protection of a buried pipeline can be achieved by connecting anodes made from zinc to the pipe. Zinc acts as the anode (negative terminus) by slowly corroding away as it passes electric current to the steel pipeline.[note 4] Zinc is also used to cathodically protect metals that are exposed to sea water from corrosion. Zinc is also used as an anode material for batteries such as in zinc–carbon batteries or zinc-air battery/fuel cells. A widely used alloy which contains zinc is brass, in which copper is alloyed with anywhere from 3% to 45% zinc, depending upon the type of brass. Brass is generally more ductile and stronger than copper and has superior corrosion resistance. These properties make it useful in communication equipment, hardware, musical instruments, and water valves. Other widely used alloys that contain zinc include nickel silver, typewriter metal, soft and aluminium solder, and commercial bronze. Alloys of primarily zinc with small amounts of copper, aluminium, and magnesium are useful in die casting as well as spin casting, especially in the automotive, electrical, and hardware industries. These alloys are marketed under the name Zamak. Roughly one quarter of all zinc output, in the United States (2009), is consumed in the form of zinc compounds, a variety of which are used industrially.
Cadmium has many common industrial uses as it is a key component in battery production, is present in cadmium pigments, coatings, and is commonly used in electroplating. In 2009, 86% of cadmium was used in batteries, predominantly in rechargeable nickel-cadmium batteries. The European Union banned the use of cadmium in electronics in 2004 with several exceptions but reduced the allowed content of cadmium in electronics to 0.002%. Cadmium electroplating, consuming 6% of the global production, can be found in the aircraft industry due to the ability to resist corrosion when applied to steel components.
Mercury is used primarily for the manufacture of industrial chemicals or for electrical and electronic applications. It is used in some thermometers, especially ones which are used to measure high temperatures. A still increasing amount is used as gaseous mercury in fluorescent lamps, while most of the other applications are slowly phased out due to health and safety regulations, and is in some applications replaced with less toxic but considerably more expensive Galinstan alloy. Mercury and its compounds have been used in medicine, although they are much less common today than they once were, now that the toxic effects of mercury and its compounds are more widely understood. It is still used as an ingredient in dental amalgams. In the late 20th century the largest use of mercury was in the mercury cell process (also called the Castner-Kellner process) in the production of chlorine and caustic soda.
Biological role and toxicity
The group 12 elements have multiple effects on biological organisms as cadmium and mercury are toxic while zinc is required by most plants and animals in trace amounts.
Zinc is an essential trace element, necessary for plants, animals, and microorganisms. It is "typically the second most abundant transition metal in organisms" after iron and it is the only metal which appears in all enzyme classes. There are 2–4 grams of zinc distributed throughout the human body, and it plays "ubiquitous biological roles". A 2006 study estimated that about 10% of human proteins (2800) potentially bind zinc, in addition to hundreds which transport and traffic zinc. In the U.S., the Recommended Dietary Allowance (RDA) is 8 mg/day for women and 11 mg/day for men. Harmful excessive supplementation may be a problem and should probably not exceed 20 mg/day in healthy people, although the U.S. National Research Council set a Tolerable Upper Intake of 40 mg/day.
Mercury and cadmium are toxic and may cause environmental damage if they enter rivers or rain water. This may result in contaminated crops as well as the bioaccumulation of mercury in a food chain leading to an increase in illnesses caused by mercury and cadmium poisoning.
- See list of oxidation states of the elements. Oxidation states in bold are common.
- The color of the flame test of pure radium has never been observed; the crimson red color is an extrapolation from the flame test color of its compounds.
- Sometimes reported as white.
- Electric current will naturally flow between zinc and steel but in some circumstances inert anodes are used with an external DC source.
- Fluck, E. (1988). "New Notations in the Periodic Table" (PDF). Pure Appl. Chem. (IUPAC) 60 (3): 431–436. doi:10.1351/pac198860030431. Retrieved 24 March 2012.
- Greenwood, Norman N.; Earnshaw, Alan (1997). Chemistry of the Elements (2nd ed.). Butterworth-Heinemann. ISBN 0-08-037941-9.
- Cotton, F. Albert; Wilkinson, Geoffrey; Murillo, Carlos A.; Bochmann, Manfred (1999), Advanced Inorganic Chemistry (6th ed.), New York: Wiley-Interscience, ISBN 0-471-19957-5
- Housecroft, C. E.; Sharpe, A. G. (2008). Inorganic Chemistry (3rd ed.). Prentice Hall. ISBN 978-0131755536.
- Eichler, R.; Aksenov, N.V.; Belozerov, A.V.; Bozhikov, G.A.; Chepigin, V.I.; Dmitriev, S.N.; Dressler, R.; Gäggeler, H.W.; Gorshkov, V.A.; N.N., F.; et al. (2007). "Chemical Characterization of Element 112". Nature 447 (7140): 72–75. Bibcode:2007Natur.447...72E. doi:10.1038/nature05761. PMID 17476264.
- Wąs, Bogdan; Misiak, Ryszard; Bartyzel, Mirosław; Petelenz, Barbara (2006). "Thermochromatographic Separation of 206,208Po from a Bismuth Target Bombardet with Protons" (PDF). Nukleonica 51 (Suppl. 2): s3–s5.
- Kratz, Jens Volker (2012). "The impact of the properties of the heaviest elements on the chemical and physical sciences". Radiochimica Acta 100 (8–9): 569–578. doi:10.1524/ract.2012.1963.
- "Zinc Metal Properties". American Galvanizers Association. 2008. Archived from the original on February 21, 2009. Retrieved 2009-02-15.
- CRC 2006, p. 4–41
- Heiserman 1992, p. 123
- Hammond, C. R The Elements in Lide, D. R., ed. (2005). CRC Handbook of Chemistry and Physics (86th ed.). Boca Raton (FL): CRC Press. ISBN 0-8493-0486-5.
- Eichler, R.; Aksenov, N. V.; Belozerov, A. V.; Bozhikov, G. A.; Chepigin, V. I.; Dmitriev, S. N.; Dressler, R.; Gäggeler, H. W.; et al. (2008). "Thermochemical and physical properties of element 112". Angewandte Chemie 47 (17): 3262–6. doi:10.1002/anie.200705019. Retrieved 5 November 2013.
- Lehto 1968, p. 826
- Scoffern, John (1861). The Useful Metals and Their Alloys. Houlston and Wright. pp. 591–603. Retrieved 2009-04-06.
- Holleman, Arnold F.; Wiberg, Egon; Wiberg, Nils (1985). "Cadmium". Lehrbuch der Anorganischen Chemie (in German) (91–100 ed.). Walter de Gruyter. pp. 1056–1057. ISBN 3-11-007511-3.
- "Case Studies in Environmental Medicine (CSEM) Cadmium". Agency for Toxic Substances and Disease Registry. Archived from the original on February 3, 2011. Retrieved May 30, 2011.
- Norrby, L.J. (1991). "Why is mercury liquid? Or, why do relativistic effects not get into chemistry textbooks?". Journal of Chemical Education 68 (2): 110. Bibcode:1991JChEd..68..110N. doi:10.1021/ed068p110.
- "Why is mercury a liquid at STP?". Retrieved 2009-07-07.
- Ingalls, Walter Renton (1902). Production and Properties of Zinc: A Treatise on the Occurrence and Distribution of Zinc Ore, the Commercial and Technical Conditions Affecting the Production of the Spelter, Its Chemical and Physical Properties and Uses in the Arts, Together with a Historical and Statistical Review of the Industry. The Engineering and Mining Journal. pp. 142–6.
- Scoullos, Michael J.; Vonkeman, Gerrit H.; Thornton, Iain; Makuch, Zen (2001). Mercury, Cadmium, Lead: Handbook for Sustainable Heavy Metals Policy and Regulation. Springer. ISBN 978-1-4020-0224-3.
- Brady, George Stuart; Brady, George S.; Clauser, Henry R.; Vaccari, John A. (2002). Materials handbook: an encyclopedia for managers, technical professionals, purchasing and production managers, technicians, and supervisors. McGraw-Hill Professional. p. 425. ISBN 978-0-07-136076-0.
- Vargel, C.; Jacques, M.; Schmidt, M. P. (2004). Corrosion of Aluminium. Elsevier. p. 158. ISBN 978-0-08-044495-6.
- Moss, Alex (2003). "Descriptive P-block Notes" (PDF). Alchemyst Online. Retrieved June 2, 2011.
- Lindberg, S.E.; Stratton, W.J. (1998). "Atmospheric Mercury Speciation: Concentrations and Behavior of Reactive Gaseous Mercury in Ambient Air". Environmental Science and Technology (American Chemical Society) 32 (1): 49–57. Bibcode:1998EnST...32...49L. doi:10.1021/es970546u.
- Al-Niaimi, N.S.; Hamid, H.A. (1976). "Stabilities of nickel(II), copper(II), zinc(II) and dioxouranium(II) complexes of some β-diketones". Journal of Inorganic and Nuclear Chemistry (Elsevier Ltd.) 3 (5): 849–852. doi:10.1016/0022-1902(77)80167-X.
- Transition element according IUPAC. Compendium of Chemical Terminology, 2nd ed. (the "Gold Book"). Compiled by A. D. McNaught and A. Wilkinson. Blackwell Scientific Publications, Oxford (1997). XML on-line corrected version: http://goldbook.iupac.org (2006–) created by M. Nic, J. Jirat, B. Kosata; updates compiled by A. Jenkins. ISBN 0-9678550-9-8
- Elusive Hg(IV) species has been synthesized under cryogenic conditions
- Wang, Xuefang; Andrews, Lester; Riedel, Sebastian; Kaupp, Martin (2007). "Mercury is a Transition Metal: The First Experimental Evidence for HgF4". Angewandte Chemie 119 (44): 8523–8527. doi:10.1002/ange.200703710.
- Jensen, William B. (2003). "The Place of Zinc, Cadmium, and Mercury in the Periodic Table" (PDF). Journal of Chemical Education (American Chemical Society) 80 (8): 952–961. Bibcode:2003JChEd..80..952J. doi:10.1021/ed080p952. Retrieved 2012-05-06.
- Royal Society of Chemistry. "Visual Elements: Group 2–The Alkaline Earth Metals". Visual Elements. Royal Society of Chemistry. Retrieved 13 January 2012.
- Kirby, H. W; Salutsky, Murrell L (1964). The Radiochemistry of Radium. National Academies Press.
- H. W. Gäggeler (2007). "Gas Phase Chemistry of Superheavy Elements" (PDF). Paul Scherrer Institute. pp. 26–28.
- Haire, Richard G. (2006). "Transactinides and the future elements". In Morss; Edelstein, Norman M.; Fuger, Jean. The Chemistry of the Actinide and Transactinide Elements (3rd ed.). Dordrecht, The Netherlands: Springer Science+Business Media. p. 1675. ISBN 1-4020-3555-1.
- Fricke, Burkhard (1975). "Superheavy elements: a prediction of their chemical and physical properties". Recent Impact of Physics on Inorganic Chemistry 21: 89–144. doi:10.1007/BFb0116498. Retrieved 4 October 2013.
- Richens, David T. (September 1997). The Chemistry of Aqua Ions. J. Wiley. ISBN 0-471-97058-1.
- Pyykkö, Pekka (2011). "A suggested periodic table up to Z ≤ 172, based on Dirac–Fock calculations on atoms and ions". Physical Chemistry Chemical Physics 13 (1): 161–8. Bibcode:2011PCCP...13..161P. doi:10.1039/c0cp01575j. PMID 20967377.
- Fricke, B.; Greiner, W.; Waber, J. T. (1971). "The continuation of the periodic table up to Z = 172. The chemistry of superheavy elements". Theoretica chimica acta (Springer-Verlag) 21 (3): 235–260. doi:10.1007/BF01172015. Retrieved 28 November 2012.
- Kratz, J. V. (5 September 2011). The Impact of Superheavy Elements on the Chemical and Physical Sciences (PDF). 4th International Conference on the Chemistry and Physics of the Transactinide Elements. Retrieved 27 August 2013.
- "Investigation of the stability of superheavy nuclei aroundZ=114 andZ=164". Zeitschrift f�r Physik 228: 371–386. doi:10.1007/BF01406719. replacement character in
|journal=at position 14 (help)
- Weeks, Mary Elvira (1933). III. Some Eighteenth-Century Metals. Easton, PA: Journal of Chemical Education. p. 20. ISBN 0-7661-3872-0.
- Greenwood 1997, p. 1201
- Ray, Prafulla Chandra (1903). A History of Hindu Chemistry from the Earliest Times to the Middle of the Sixteenth Century, A.D.: With Sanskrit Texts, Variants, Translation and Illustrations 1 (2nd ed.). The Bengal Chemical & Pharmaceutical Works, Ltd. pp. 157–158. (public domain text)
- Arny, Henry Vinecome (1917). Principles of Pharmacy (2nd ed.). W. B. Saunders company. p. 483.
- Habashi, Fathi. "Discovering the 8th Metal" (PDF). International Zinc Association (IZA). Retrieved 2008-12-13.
- Hoover, Herbert Clark (2003). Georgius Agricola de Re Metallica. Kessinger Publishing. p. 409. ISBN 0-7661-3197-1.
- Gerhartz, Wolfgang (1996). Ullmann's Encyclopedia of Industrial Chemistry (5th ed.). VHC. p. 509. ISBN 3-527-20100-9.
- Emsley 2001, p. 502
- Weeks 1933, p. 21
- Warren, Neville G. (2000). Excel Preliminary Physics. Pascal Press. p. 47. ISBN 1-74020-085-3.
- "Galvanic Cell". The New International Encyclopaedia. Dodd, Mead and Company. 1903. p. 80.
- Cotton 1999, p. 626
- "Cadmium". Kirk-Othmer Encyclopedia of Chemical Technology 5 (4th ed.). New York: John Wiley & Sons. 1994.
- Hermann (1818). "Noch ein schreiben über das neue Metall (Another letter about the new metal)". Annalen der Physik 59 (5): 113–116. Bibcode:1818AnP....59..113H. doi:10.1002/andp.18180590511.
- Waterston, William; Burton, J. H (1844). Cyclopædia of commerce, mercantile law, finance, commercial geography and navigation. p. 122.
- Rowbotham, Thomas Leeson (1850). The art of landscape painting in water colours, by T. and T. L. Rowbotham. p. 10.
- Ayres, Robert U.; Ayres, Leslie; Råde, Ingrid (2003). The life cycle of copper, its co-products and byproducts. pp. 135–141. ISBN 978-1-4020-1552-6.
- Burdun, G. D. (1958). "On the new determination of the meter" (pdf). Measurement Techniques 1 (3): 259–264. doi:10.1007/BF00974680.
- Beers & Penzes 1992
- Marion, Jerry B. (1982). Physics For Science and Engineering. CBS College Publishing. p. 3. ISBN 4-8337-0098-0.
- "Mercury and the environment — Basic facts". Environment Canada, Federal Government of Canada. 2004. Retrieved 2008-03-27.
- Wright, David Curtis (2001). The History of China. Greenwood Publishing Group. p. 49. ISBN 0-313-30940-X.
- Hesse R W (2007). Jewelrymaking through history. Greenwood Publishing Group. p. 120. ISBN 0-313-33507-9.
- Stillman, J. M. (2003). Story of Alchemy and Early Chemistry. Kessinger Publishing. pp. 7–9. ISBN 978-0-7661-3230-6.
- Cox, R (1997). The Pillar of Celestial Fire. 1st World Publishing. p. 260. ISBN 1-887472-30-4.
- S. Hofmann; et al. (1996). "The new element 112". Zeitschrift für Physik A 354 (1): 229–230. doi:10.1007/BF02769517.
- Barber, Robert C.; Gäggeler, Heinz W.; Karol, Paul J.; Nakahara, Hiromichi; Vardaci, Emanuele; Vogt, Erich. "Element 112 is Named Copernicium". Pure and Applied Chemistry (iupac.org) 81 (7): 1331–1343. doi:10.1351/PAC-REP-08-03-05. Archived from the original on February 24, 2010. Retrieved 2010-04-05.
- Wedepohl, K. Hans (1995). "The composition of the continental crust". Geochimica et Cosmochimica Acta 59 (7): 1217–1232. Bibcode:1995GeCoA..59.1217W. doi:10.1016/0016-7037(95)00038-2.
- Greenwood 1997, p. 1202
- Plachy, Jozef. "Annual Average Cadmium Price" (PDF). USGS. Retrieved June 16, 2010.
- Fthenakis, V (2004). "Life cycle impact analysis of cadmium in CdTe PV production". Renewable and Sustainable Energy Reviews 8 (4): 303–334. doi:10.1016/j.rser.2003.12.001.
- Fleischer, Michael (1980). "New Mineral Names" (PDF). American Mineralogist 65: 1065–1070.
- Ehrlich, H. L.; Newman D. K. (2008). Geomicrobiology. CRC Press. p. 265. ISBN 978-0-8493-7906-2.
- Rytuba, James J. "Mercury from mineral deposits and potential environmental impact". Environmental Geology 43 (3): 326–338. doi:10.1007/s00254-002-0629-5.
- Tolcin, A. C. (2011). "Mineral Commodity Summaries 2009: Zinc" (PDF). United States Geological Survey. Retrieved 2011-06-06.
- "Country Partnership Strategy—Iran: 2011–12". ECO Trade and development bank. Retrieved 2011-06-06.
- "IRAN – a growing market with enormous potential". IMRG. July 5, 2010. Retrieved 2010-03-03.
- Cohen, David (2007). "Earth audit". New Scientist 194 (2605): 8. doi:10.1016/S0262-4079(07)61315-3.
- "Augsberg University Calculate When Our Materials Run Out". IDTechEx. 2007-06-04. Retrieved 2008-12-09.
- Gordon, R. B.; Bertram, M.; Graedel, T. E. (2006). "Metal stocks and sustainability". Proceedings of the National Academy of Sciences 103 (5): 1209–14. Bibcode:2006PNAS..103.1209G. doi:10.1073/pnas.0509498103. PMC 1360560. PMID 16432205.
- World Mineral Production. London: British Geological Survey, NERC. May 2001. Check date values in:
|year= / |date= mismatch(help)
- About the Mercury Rule
- "Zinc: World Mine Production (zinc content of concentrate) by Country" (PDF). 2006 Minerals Yearbook: Zinc (Washington, D.C.: United States Geological Survey): Table 15. February 2008. Retrieved 2009-01-19.
- Rosenqvist, Terkel (1922). Principles of Extractive Metallurgy (2 ed.). Tapir Academic Press. pp. 7, 16, 186. ISBN 82-519-1922-3.
- Porter, Frank C. (1991). Zinc Handbook. CRC Press. ISBN 978-0-8247-8340-2.
- Bodsworth, Colin (1994). The Extraction and Refining of Metals. CRC Press. p. 148. ISBN 0-8493-4433-6.
- Gupta, C. K.; Mukherjee, T. K. (1990). Hydrometallurgy in Extraction Processes. CRC Press. p. 62. ISBN 0-8493-6804-9.
- National Research Council (U.S.), Panel on Cadmium, Committee on Technical Aspects of Critical and Strategic Material (1969). Trends in Usage of Cadmium: Report. National Research Council, National Academy of Sciences-National Academy of Engineering. pp. 1–3.
- Scoullos, Michael J (2001-12-31). Mercury, cadmium, lead: handbook for sustainable heavy metals policy and regulation. pp. 104–116. ISBN 978-1-4020-0224-3.
- Rytuba, James J. (2003). "Mercury from mineral deposits and potential environmental impact". Environmental Geology 43 (3): 326–338. doi:10.1007/s00254-002-0629-5.
- Vallero, Daniel A (2008). Fundamentals of air pollution. pp. 865–866. ISBN 978-0-12-373615-4.
- Barber, Robert C.; Gäggeler, Heinz W.; Karol, Paul J.; Nakahara, Hiromichi; Vardaci, Emanuele; Vogt, Erich (2009). "Discovery of the element with atomic number 112 (IUPAC Technical Report)". Pure and Applied Chemistry 81 (7): 1331. doi:10.1351/PAC-REP-08-03-05.
- Stwertka, Albert (1998). "Zinc". Guide to the Elements (Revised ed.). Oxford University Press. ISBN 0-19-508083-1.
- Emsley, John (2001). "Zinc". Nature's Building Blocks: An A-Z Guide to the Elements. Oxford, England, UK: Oxford University Press. pp. 499–505. ISBN 0-19-850340-7.
- Smith C.J.E.; Higgs M.S.; Baldwin K.R. (April 20, 1999). "Advances to Protective Coatings and their Application to Ageing Aircraft" (PDF). RTO MP-25. Retrieved May 29, 2011.
- Newman, John (2004). Electrochemical Systems. New Jersey: John Wiley & Sons. ISBN 0-471-47756-7.
- "Zinc: World Mine Production (zinc content of concentrate) by Country" (PDF). 2009 Minerals Yearbook: Zinc. Washington, D.C.: United States Geological Survey. February 2010. Retrieved 2010-06-06.
- Lehto 1968, p. 829
- Bounoughaz, M.; Salhi, E.; Benzine, K.; Ghali, E.; Dalard, F. (2003). "A comparative study of the electrochemical behaviour of Algerian zinc and a zinc from a commercial sacrificial anode". Journal of Materials Science 38 (6): 1139–1145. Bibcode:2003JMatS..38.1139B. doi:10.1023/A:1022824813564.
- Stwertka 1998, p. 99
- Besenhard, Jürgen O. (1999). Handbook of Battery Materials (PDF). Wiley-VCH. ISBN 3-527-29469-4. Retrieved 2008-10-08.
- Wiaux, J.-P.; Waefler, J.-P. (1995). "Recycling zinc batteries: an economical challenge in consumer waste management". Journal of Power Sources 57 (1–2): 61–65. doi:10.1016/0378-7753(95)02242-2.
- Culter, T. (1996). "A design guide for rechargeable zinc-air battery technology". Southcon/96. Conference Record: 616. doi:10.1109/SOUTHC.1996.535134. ISBN 0-7803-3268-7.
- Whartman, Jonathan; Brown, Ian. "Zinc Air Battery-Battery Hybrid for Powering Electric Scooters and Electric Buses" (PDF). The 15th International Electric Vehicle Symposium. Retrieved 2008-10-08.
- Cooper, J. F; Fleming, 2D.; Hargrove, D.; Koopman; R.; Peterman, K. "A refuelable zinc/air battery for fleet electric vehicle propulsion". Society of Automotive Engineers future transportation technology conference and exposition. Retrieved 2008-10-08.
- Eastern Alloys contributors. "Diecasting Alloys". Maybrook, NY: Eastern Alloys. Retrieved 2009-01-19.
- Buxbaum, Gunter; Pfaff, Gerhard (2005). "Cadmium Pigments". Industrial inorganic pigments. Wiley-VCH. pp. 121–123. ISBN 978-3-527-30363-2.
- "Battery collection; recycling, nature protected". European Union. Retrieved November 4, 2008.
- Hopkinson, G. R.; Goodman, T. M.; Prince, S. R. (2004). A guide to the use and calibration of detector array equipment. SPIE Press. p. 125. ISBN 0-8194-5532-6.
- "Mercury Reduction Act of 2003". United States. Congress. Senate. Committee on Environment and Public Works. Retrieved 2009-06-06.
- Surmann, P; Zeyat, H (Nov 2005). "Voltammetric analysis using a self-renewable non-mercury electrode". Analytical and Bioanalytical Chemistry 383 (6): 1009–13. doi:10.1007/s00216-005-0069-7. PMID 16228199.
- FDA. "Thimerosal in Vaccines". Retrieved October 25, 2006.
- The CRB Commodity Yearbook (annual). 2000. p. 173. ISSN 1076-2906.
- Leopold, B. R. (2002). "Chapter 3: Manufacturing Processes Involving Mercury. Use and Release of Mercury in the United States" (PDF). National Risk Management Research Laboratory, Office of Research and Development, U.S. Environmental Protection Agency, Cincinnati, Ohio. Archived from the original (PDF) on June 21, 2007. Retrieved May 1, 2007.
- "Chlorine Online Diagram of mercury cell process". Euro Chlor. Archived from the original on September 18, 2011. Retrieved 2012-04-09.
- Broadley, M. R.; White, P. J.; Hammond, J. P.; Zelko, I.; Lux, A. (2007). "Zinc in plants". New Phytologist 173 (4): 677–702. doi:10.1111/j.1469-8137.2007.01996.x. PMID 17286818.
- Prasad A. S. (2008). "Zinc in Human Health: Effect of Zinc on Immune Cells". Mol. Med. 14 (5–6): 353–7. doi:10.2119/2008-00033.Prasad. PMC 2277319. PMID 18385818.
- Zinc's role in microorganisms is particularly reviewed in: Sugarman B (1983). "Zinc and infection". Review of Infectious Diseases 5 (1): 137–47. doi:10.1093/clinids/5.1.137. PMID 6338570.
- Rink, L.; Gabriel, P. (2000). "Zinc and the immune system". Proc Nutr Soc 59 (4): 541–52. doi:10.1017/S0029665100000781. PMID 11115789.
- Wapnir, Raul A. (1990). Protein Nutrition and Mineral Absorption. Boca Raton, Florida: CRC Press. ISBN 0-8493-5227-4.
- Hambidge, K. M.; Krebs, N. F. (2007). "Zinc deficiency: a special challenge". J. Nutr. 137 (4): 1101–5. PMID 17374687.
- Connie W. Bales; Christine Seel Ritchie (21 May 2009). Handbook of Clinical Nutrition and Aging. Springer. pp. 151–. ISBN 978-1-60327-384-8. Retrieved 23 June 2011.
- Maret, W.; Sandstead, H. H. (2006). "Zinc requirements and the risks and benefits of zinc supplementation". Journal of Trace Elements in Medicine and Biology 20 (1): 3–18. doi:10.1016/j.jtemb.2006.01.006. PMID 16632171.
- "Zinc – Summary". Dietary Reference Intakes for Vitamin A, Vitamin K, Arsenic, Boron, Chromium, Copper, Iodine, Iron, Manganese, Molybdenum, Nickel, Silicon, Vanadium, and Zinc (2001). Institute of Medicine, Food and Nutrition Board. Retrieved 2010-03-30.
- Nogawa, Koji; Kobayashi, E; Okubo, Y; Suwazono, Y (2004). "Environmental cadmium exposure, adverse effects, and preventative measures in Japan". Biometals 17 (5): 581–587. doi:10.1023/B:BIOM.0000045742.81440.9c. PMID 15688869.
- Mozaffarian D, Rimm EB (2006). "Fish intake, contaminants, and human health: evaluating the risks and the benefits". JAMA 296 (15): 1885–99. doi:10.1001/jama.296.15.1885. PMID 17047219.
- CRC contributors (2006). David R. Lide, ed. Handbook of Chemistry and Physics (87th ed.). Boca Raton, Florida: CRC Press, Taylor & Francis Group. ISBN 0-8493-0487-3.
- Cotton, F. Albert; Wilkinson, Geoffrey; Murillo, Carlos A.; Bochmann, Manfred (1999). Advanced Inorganic Chemistry (6th ed.). New York: John Wiley & Sons, Inc. ISBN 0-471-19957-5.
- Emsley, John (2001). "Zinc". Nature's Building Blocks: An A-Z Guide to the Elements. Oxford, England, UK: Oxford University Press. pp. 499–505. ISBN 0-19-850340-7.
- Greenwood, N. N.; Earnshaw, A. (1997). Chemistry of the Elements (2nd ed.). Oxford: Butterworth-Heinemann. ISBN 0-7506-3365-4.
- Heiserman, David L. (1992). "Element 30: Zinc". Exploring Chemical Elements and their Compounds. New York: TAB Books. ISBN 0-8306-3018-X.
- Lehto, R. S. (1968). "Zinc". In Clifford A. Hampel. The Encyclopedia of the Chemical Elements. New York: Reinhold Book Corporation. pp. 822–830. ISBN 0-442-15598-0. LCCN 68-29938.
- Stwertka, Albert (1998). "Zinc". Guide to the Elements (Revised ed.). Oxford University Press. ISBN 0-19-508083-1.
- Weeks, Mary Elvira (1933). "III. Some Eighteenth-Century Metals". The Discovery of the Elements. Easton, PA: Journal of Chemical Education. ISBN 0-7661-3872-0.
|Periodic table (Large cells)|