Group 12 element

Last updated

Group 12 in the periodic table
Hydrogen Helium
Lithium Beryllium Boron Carbon Nitrogen Oxygen Fluorine Neon
Sodium Magnesium Aluminium Silicon Phosphorus Sulfur Chlorine Argon
Potassium Calcium Scandium Titanium Vanadium Chromium Manganese Iron Cobalt Nickel Copper Zinc Gallium Germanium Arsenic Selenium Bromine Krypton
Rubidium Strontium Yttrium Zirconium Niobium Molybdenum Technetium Ruthenium Rhodium Palladium Silver Cadmium Indium Tin Antimony Tellurium Iodine Xenon
Caesium Barium Lanthanum Cerium Praseodymium Neodymium Promethium Samarium Europium Gadolinium Terbium Dysprosium Holmium Erbium Thulium Ytterbium Lutetium Hafnium Tantalum Tungsten Rhenium Osmium Iridium Platinum Gold Mercury (element) Thallium Lead Bismuth Polonium Astatine Radon
Francium Radium Actinium Thorium Protactinium Uranium Neptunium Plutonium Americium Curium Berkelium Californium Einsteinium Fermium Mendelevium Nobelium Lawrencium Rutherfordium Dubnium Seaborgium Bohrium Hassium Meitnerium Darmstadtium Roentgenium Copernicium Nihonium Flerovium Moscovium Livermorium Tennessine Oganesson
group 11    boron group
IUPAC group number 12
Name by elementzinc group
CAS group number
(US, pattern A-B-A)
IIB
old IUPAC number
(Europe, pattern A-B)
IIB

  Period
4
Zinc fragment sublimed and 1cm3 cube.jpg
Zinc (Zn)
30 Transition metal
5
Cadmium-crystal bar.jpg
Cadmium (Cd)
48 Transition metal
6
Pouring liquid mercury bionerd.jpg
Mercury (Hg)
80 Transition metal
7 Copernicium (Cn)
112transition metal

Legend

primordial element
synthetic element

Group 12, by modern IUPAC numbering, [1] is a group of chemical elements in the periodic table. It includes zinc (Zn), cadmium (Cd), mercury (Hg), [2] [3] [4] and copernicium (Cn). [5] Formerly this group was named IIB (pronounced as "group two B", as the "II" is a Roman numeral) by CAS and old IUPAC system. [note 1]

Contents

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 known to be a liquid at room temperature – as copernicium's boiling point has not yet been measured accurately enough, [note 2] it is not yet known whether it is a liquid or a gas under standard conditions. 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.

Physical and atomic properties

Like other groups of the periodic table, the members of group 12 show patterns in its electron configuration, especially the outermost shells, which result in trends in their chemical behavior:

Z Element No. of electrons/shell
30zinc2, 8, 18, 2
48cadmium2, 8, 18, 18, 2
80mercury2, 8, 18, 32, 18, 2
112copernicium2, 8, 18, 32, 32, 18, 2 (predicted)

The group 12 elements are all soft, diamagnetic, divalent metals. They have the lowest melting points among all transition metals. [8] Zinc is bluish-white and lustrous, [9] though most common commercial grades of the metal have a dull finish. [10] Zinc is also referred to in nonscientific contexts as spelter . [11] 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. [12]

The table below is a summary of the key physical properties of the group 12 elements. The data for copernicium is based on relativistic density-functional theory simulations. [13]

Properties of the group 12 elements
NameZincCadmiumMercuryCopernicium
Melting point 693 K (420 °C)594 K (321 °C)234 K (−39 °C)283±11 K [13] (10 °C)
Boiling point 1180 K (907 °C)1040 K (767 °C)630 K (357 °C)340±10 K [13] (60 °C)
Density 7.14 g·cm−38.65 g·cm−313.534 g·cm−314.0 g·cm−3 [13]
Appearancesilvery bluish-graysilver-graysilvery ?
Atomic radius 135 pm155 pm150 pm ? 147 pm

Zinc is somewhat less dense than iron and has a hexagonal crystal structure. [14] The metal is hard and brittle at most temperatures but becomes malleable between 100 and 150 °C (212 and 302 °F). [9] [10] Above 210 °C (410 °F), the metal becomes brittle again and can be pulverized by beating. [15] Zinc is a fair conductor of electricity. [9] For a metal, zinc has relatively low melting (419.5 °C, 787.1 °F) and boiling points (907 °C, 1,665 °F). [8] Cadmium is similar in many respects to zinc but forms complex compounds. [16] 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. [17] 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. [18] [19]

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. [11] While neither zinc nor zirconium are ferromagnetic, their alloy ZrZn
2
exhibits ferromagnetism below 35  K. [9] Cadmium is used in many kinds of solder and bearing alloys, due to a low coefficient of friction and fatigue resistance. [20] It is also found in some of the lowest-melting alloys, such as Wood's metal. [21] 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. [22]

Chemistry

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. [23] 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. [23] 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. [24] 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 mostly in the gas phase, in such compounds as linear Zn2Cl2, analogous to calomel. In the solid phase, the rather exotic compound decamethyldizincocene (Cp*Zn–ZnCp*) is known.

Classification

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. [25] 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, [26] 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 (though its existence is disputed, as later experiments trying to confirm its synthesis could not find evidence of HgF4). [27] [28] 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. [29]

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. [29]

Comparison of the properties of the alkaline earth metals and the group 12 elements (predictions for copernicium) [29]
NameBerylliumMagnesiumCalciumStrontiumBariumRadium
Valence electron configuration2s23s24s25s26s27s2
Core electron configuration[ He ][ Ne ][ Ar ][ Kr ][ Xe ][ Rn ]
Oxidation states [note 3] +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)
Appearancewhite-gray metallicshiny gray metallicdull silver-graysilvery white metallicsilvery graysilvery white metallic
Density 1.85 g·cm−31.738 g·cm−31.55 g·cm−32.64 g·cm−33.51 g·cm−35.5 g·cm−3
Pauling electronegativity 1.571.311.000.950.890.9
Atomic radius 105 pm150 pm180 pm200 pm215 pm215 pm
Crystal ionic radius 59 pm86 pm114 pm132 pm149 pm162 pm
Flame test colorwhite [29] brilliant white [30] brick-red [30] crimson [30] apple green [30] crimson red [note 4]
Organometallic chemistry goodgoodpoorvery poorvery poorextremely poor
Hydroxide amphoteric basic basicstrongly basicstrongly basicstrongly basic
Oxide amphotericstrongly basicstrongly basicstrongly basicstrongly basicstrongly basic
NameBerylliumMagnesiumZincCadmiumMercuryCopernicium
Valence electron configuration2s23s24s25s26s2 ? 7s2
Core electron configuration[He][Ne][Ar]3d10[Kr]4d10[Xe]4f145d10 ? [Rn]5f146d10
Oxidation states [note 3] +2, +1+2, +1+2, +1+2, +1+2, +1 ? +4, +2, +1, 0 [32] [33] [34]
Melting point1560 K (1287 °C)923 K (650 °C)693 K (420 °C)594 K (321 °C)234 K (−39 °C)283±11 K (10 °C)
Boiling point2742 K (2469 °C)1363 K (1090 °C)1180 K (907 °C)1040 K (767 °C)630 K (357 °C)340±10 K (60 °C)
Appearancewhite-gray metallicshiny gray metallicsilvery bluish-gray metallicsilver-graysilvery ?
Density1.85 g·cm−31.738 g·cm−37.14 g·cm−38.65 g·cm−313.534 g·cm−314.0 g·cm−3
Pauling electronegativity1.571.311.651.692.00 ?
Atomic radius105 pm150 pm135 pm155 pm150 pm ? 147 pm [33]
Crystal ionic radius59 pm86 pm88 pm109 pm116 pm ? 75 pm [33]
Flame test colorwhitebrilliant whitebluish-green [note 5]  ? ? ?
Organometallic chemistrygoodgoodgoodgoodgood ?
Hydroxideamphotericbasicamphotericweakly basic ? ?
Oxideamphotericstrongly basicamphotericmildly basicmildly basic ?

Compounds

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. [35] Covalent character is achieved by using the s and p orbitals. Mercury, however, rarely exceeds a coordination number of four. Coordination numbers of 2, 3, 5, 7 and 8 are also known.

History

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

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. [36] [37] Zinc was distinctly recognized as a metal under the designation of Fasada in the medical Lexicon ascribed to the Hindu king Madanapala (of Taka dynasty) and written about the year 1374. [38] The metal was also of use to alchemists. [39] The name of the metal was first documented in the 16th century, [40] [41] and is probably derived from the German zinke for the needle-like appearance of metallic crystals. [42]

Alchemical symbol for the element zinc Zinc symbol (fixed width).svg
Alchemical symbol for the element zinc

The isolation of metallic zinc in the West may have been achieved independently by several people in the 17th century. [43] 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. [44] 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. [45] [46] In 1799, Galvani's friend, Alessandro Volta, invented the Voltaic pile. [45] 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. [47]

Cadmium

In 1817, cadmium was discovered in Germany as an impurity in zinc carbonate minerals (calamine) by Friedrich Stromeyer and Karl Samuel Leberecht Hermann. [48] 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. [49] Stromeyer eventually isolated cadmium metal by roasting and reduction of the sulfide. [50] [51] [52]

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). [53] 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, [54] 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. [55]

Mercury

The symbol for the planet Mercury () has been used since ancient times to represent the element. Mercury symbol.svg
The symbol for the planet Mercury (☿) has been used since ancient times to represent the element.

Mercury has been found in Egyptian tombs which have been dated back to 1500 BC, [56] where mercury was used in cosmetics. It was also used by the ancient Chinese who believed it would improve and prolong health. [57] By 500 BC mercury was used to make amalgams (Medieval Latin amalgama, "alloy of mercury") with other metals. [58] 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. [59]

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. [60] Mercury is the only metal for which the alchemical planetary name became the common name. [59]

Copernicium

The heaviest known group 12 element, copernicium, was first created on February 9, 1996, at the Gesellschaft für Schwerionenforschung (GSI) in Darmstadt, Germany, by Sigurd Hofmann, Victor Ninov et al. [61] It was then officially named by the International Union of Pure and Applied Chemistry (IUPAC) after Nicolaus Copernicus on February 19, 2010, the 537th anniversary of Copernicus' birth. [62]

Occurrence

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. [63] Copernicium, as a synthetic element with a half-life of a few minutes, may only be present in the laboratories where it was produced.

Sphalerite (ZnS), an important zinc ore Sphalerite4.jpg
Sphalerite (ZnS), an important zinc ore

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. [64] The commercially most important minerals of group 12 elements are sulfide minerals. [23] Sphalerite, which is a form of zinc sulfide, is the most heavily mined zinc-containing ore because its concentrate contains 60–62% zinc. [14] 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. [65] [66] One place where metallic cadmium can be found is the Vilyuy River basin in Siberia. [67] Although mercury is an extremely rare element in the Earth's crust, [68] 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. [69]

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. [70] Large deposits are in Australia, Canada and the United States with the largest reserves in Iran. [64] [71] [72] At the current rate of consumption, these reserves are estimated to be depleted sometime between 2027 and 2055. [73] [74] 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. [75] In 2005, China was the top producer of mercury with almost two-thirds global share followed by Kyrgyzstan. [76] 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. [77]

Production

Zinc is the fourth most common metal in use, trailing only iron, aluminium, and copper with an annual production of about 10 million tonnes. [78] 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. [79] Roasting converts the zinc sulfide concentrate produced during processing to zinc oxide. [80] 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. [81] The zinc vapor is collected in a condenser. [80] Electrowinning processing leaches zinc from the ore concentrate by sulfuric acid. [82] After this step electrolysis is used to produce zinc metal. [80]

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. [83] 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. [84]

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. [85] Mercury is extracted by heating cinnabar in a current of air and condensing the vapor. [86]

Superheavy 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. [87] The first fusion reaction to produce copernicium was performed by GSI in 1996, who reported the detection of two decay chains of copernicium-277 (though one was later retracted, as it had been based on data fabricated by Victor Ninov): [61]

208
82
Pb
+ 70
30
Zn
277
112
Cn
+
n

Applications

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 [2] as they will attract all local oxidation until they completely corrode. [88] These protective coatings can be applied to other metals by hot-dip galvanizing a substance into the molten form of the metal, [89] or through the process of electroplating which may be passivated by the use of chromate salts. [90] 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. [91]

In the US, zinc is used predominantly for galvanizing (55%) and for brass, bronze and other alloys (37%). [92] 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. [93] Zinc acts as the anode (negative terminus) by slowly corroding away as it passes electric current to the steel pipeline. [93] [note 6] Zinc is used to cathodically protect metals that are exposed to sea water from corrosion. [94] [95] Zinc is used as an anode material for batteries such as in zinc–carbon batteries [96] [97] or zinc–air battery/fuel cells. [98] [99] [100] 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. [93] Brass is generally more ductile and stronger than copper and has superior corrosion resistance. [93] These properties make it useful in communication equipment, hardware, musical instruments, and water valves. [93] Other widely used alloys that contain zinc include nickel silver, typewriter metal, soft and aluminium solder, and commercial bronze. [9] 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. [9] These alloys are marketed under the name Zamak. [101] 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. [92]

Cadmium has many common industrial uses as it is a key component in battery production, is present in cadmium pigments, [102] coatings, [90] and is commonly used in electroplating. [20] 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%. [103] 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. [20]

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, [104] while most of the other applications are slowly phased out due to health and safety regulations, [105] and is in some applications replaced with less toxic but considerably more expensive Galinstan alloy. [106] 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. [107] It is still used as an ingredient in dental amalgams. In the late 20th century the largest use of mercury [108] [109] was in the mercury cell process (also called the Castner-Kellner process) in the production of chlorine and caustic soda. [110]

Copernicium has no use other than research due to its very high radioactivity.

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, [111] animals, [112] and microorganisms. [113] 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. [111] There are 2–4 grams of zinc [114] distributed throughout the human body, [115] and it plays "ubiquitous biological roles". [116] A 2006 study estimated that about 10% of human proteins (2800) potentially bind zinc, in addition to hundreds which transport and traffic zinc. [111] In the U.S., the Recommended Dietary Allowance (RDA) is 8 mg/day for women and 11 mg/day for men. [117] Harmful excessive supplementation may be a problem and should probably not exceed 20 mg/day in healthy people, [118] although the U.S. National Research Council set a Tolerable Upper Intake of 40 mg/day. [119]

Mercury and cadmium are toxic and may cause environmental damage if they enter rivers or rain water. This may result in contaminated crops [120] as well as the bioaccumulation of mercury in a food chain leading to an increase in illnesses caused by mercury and cadmium poisoning. [121]

Notes

  1. The name volatile metals for group 12 has occasionally been used, [6] although this much more commonly refers to any metal having a high volatility.
  2. 340±10 K predicted, 357+112
    −108
     K
    experimentally [7]
  3. 1 2 See list of oxidation states of the elements. Oxidation states in bold are common.
  4. 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. [31]
  5. Sometimes reported as white. [29]
  6. Electric current will naturally flow between zinc and steel but in some circumstances inert anodes are used with an external DC source.

Related Research Articles

<span class="mw-page-title-main">Cadmium</span> Chemical element with atomic number 48 (Cd)

Cadmium is a chemical element; it has symbol Cd and atomic number 48. This soft, silvery-white metal is chemically similar to the two other stable metals in group 12, zinc and mercury. Like zinc, it demonstrates oxidation state +2 in most of its compounds, and like mercury, it has a lower melting point than the transition metals in groups 3 through 11. Cadmium and its congeners in group 12 are often not considered transition metals, in that they do not have partly filled d or f electron shells in the elemental or common oxidation states. The average concentration of cadmium in Earth's crust is between 0.1 and 0.5 parts per million (ppm). It was discovered in 1817 simultaneously by Stromeyer and Hermann, both in Germany, as an impurity in zinc carbonate.

<span class="mw-page-title-main">Gallium</span> Chemical element with atomic number 31 (Ga)

Gallium is a chemical element; it has the symbol Ga and atomic number 31. Discovered by the French chemist Paul-Émile Lecoq de Boisbaudran in 1875, gallium is in group 13 of the periodic table and is similar to the other metals of the group.

<span class="mw-page-title-main">Indium</span> Chemical element with atomic number 49 (In)

Indium is a chemical element; it has symbol In and atomic number 49. It is a silvery-white post-transition metal and one of the softest elements. Chemically, indium is similar to gallium and thallium, and its properties are largely intermediate between the two. It was discovered in 1863 by Ferdinand Reich and Hieronymous Theodor Richter by spectroscopic methods and named for the indigo blue line in its spectrum.

<span class="mw-page-title-main">Metal</span> Type of material

A metal is a material that, when polished or fractured, shows a lustrous appearance, and conducts electricity and heat relatively well. These properties are all associated with having electrons available at the Fermi level, as against nonmetallic materials which do not. Metals are typically ductile and malleable.

<span class="mw-page-title-main">Nickel</span> Chemical element with atomic number 28 (Ni)

Nickel is a chemical element; it has symbol Ni and atomic number 28. It is a silvery-white lustrous metal with a slight golden tinge. Nickel is a hard and ductile transition metal. Pure nickel is chemically reactive, but large pieces are slow to react with air under standard conditions because a passivation layer of nickel oxide forms on the surface that prevents further corrosion. Even so, pure native nickel is found in Earth's crust only in tiny amounts, usually in ultramafic rocks, and in the interiors of larger nickel–iron meteorites that were not exposed to oxygen when outside Earth's atmosphere.

<span class="mw-page-title-main">Silver</span> Chemical element with atomic number 47 (Ag)

Silver is a chemical element; it has symbol Ag and atomic number 47. A soft, white, lustrous transition metal, it exhibits the highest electrical conductivity, thermal conductivity, and reflectivity of any metal. Silver is found in the Earth's crust in the pure, free elemental form, as an alloy with gold and other metals, and in minerals such as argentite and chlorargyrite. Most silver is produced as a byproduct of copper, gold, lead, and zinc refining.

<span class="mw-page-title-main">Smelting</span> Use of heat and a reducing agent to extract metal from ore

Smelting is a process of applying heat and a chemical reducing agent to an ore to extract a desired base metal product. It is a form of extractive metallurgy that is used to obtain many metals such as iron, copper, silver, tin, lead and zinc. Smelting uses heat and a chemical reducing agent to decompose the ore, driving off other elements as gases or slag and leaving the metal behind. The reducing agent is commonly a fossil-fuel source of carbon, such as carbon monoxide from incomplete combustion of coke—or, in earlier times, of charcoal. The oxygen in the ore binds to carbon at high temperatures, as the chemical potential energy of the bonds in carbon dioxide is lower than that of the bonds in the ore.

<span class="mw-page-title-main">Tin</span> Chemical element with atomic number 50 (Sn)

Tin is a chemical element; it has symbol Sn and atomic number 50. A silvery-colored metal, tin is soft enough to be cut with little force, and a bar of tin can be bent by hand with little effort. When bent, the so-called "tin cry" can be heard as a result of twinning in tin crystals.

<span class="mw-page-title-main">Thallium</span> Chemical element with atomic number 81 (Tl)

Thallium is a chemical element; it has symbol Tl and atomic number 81. It is a gray post-transition metal that is not found free in nature. When isolated, thallium resembles tin, but discolors when exposed to air. Chemists William Crookes and Claude-Auguste Lamy discovered thallium independently in 1861, in residues of sulfuric acid production. Both used the newly developed method of flame spectroscopy, in which thallium produces a notable green spectral line. Thallium, from Greek θαλλός, thallós, meaning "green shoot" or "twig", was named by Crookes. It was isolated by both Lamy and Crookes in 1862; Lamy by electrolysis, and Crookes by precipitation and melting of the resultant powder. Crookes exhibited it as a powder precipitated by zinc at the international exhibition, which opened on 1 May that year.

In chemistry, a transition metal is a chemical element in the d-block of the periodic table, though the elements of group 12 are sometimes excluded. The lanthanide and actinide elements are called inner transition metals and are sometimes considered to be transition metals as well.

<span class="mw-page-title-main">Zinc</span> Chemical element with atomic number 30 (Zn)

Zinc is a chemical element with the symbol Zn and atomic number 30. It is a slightly brittle metal at room temperature and has a shiny-greyish appearance when oxidation is removed. It is the first element in group 12 (IIB) of the periodic table. In some respects, zinc is chemically similar to magnesium: both elements exhibit only one normal oxidation state (+2), and the Zn2+ and Mg2+ ions are of similar size. Zinc is the 24th most abundant element in Earth's crust and has five stable isotopes. The most common zinc ore is sphalerite (zinc blende), a zinc sulfide mineral. The largest workable lodes are in Australia, Asia, and the United States. Zinc is refined by froth flotation of the ore, roasting, and final extraction using electricity (electrowinning).

A period 5 element is one of the chemical elements in the fifth row of the periodic table of the chemical elements. The periodic table is laid out in rows to illustrate recurring (periodic) trends in the chemical behaviour of the elements as their atomic number increases: a new row is begun when chemical behaviour begins to repeat, meaning that elements with similar behaviour fall into the same vertical columns. The fifth period contains 18 elements, beginning with rubidium and ending with xenon. As a rule, period 5 elements fill their 5s shells first, then their 4d, and 5p shells, in that order; however, there are exceptions, such as rhodium.

<span class="mw-page-title-main">Noble metal</span> Metallic elements that are nearly chemically inert

A noble metal is ordinarily regarded as a metallic element that is generally resistant to corrosion and is usually found in nature in its raw form. Gold, platinum, and the other platinum group metals are most often so classified. Silver, copper, and mercury are sometimes included as noble metals, but each of these usually occurs in nature combined with sulfur.

<span class="mw-page-title-main">Sphalerite</span> Zinc-iron sulfide mineral

Sphalerite is a sulfide mineral with the chemical formula (Zn, Fe)S. It is the most important ore of zinc. Sphalerite is found in a variety of deposit types, but it is primarily in sedimentary exhalative, Mississippi-Valley type, and volcanogenic massive sulfide deposits. It is found in association with galena, chalcopyrite, pyrite, calcite, dolomite, quartz, rhodochrosite, and fluorite.

Sulfide (also sulphide in British English ) is an inorganic anion of sulfur with the chemical formula S2− or a compound containing one or more S2− ions. Solutions of sulfide salts are corrosive. Sulfide also refers to large families of inorganic and organic compounds, e.g. lead sulfide and dimethyl sulfide. Hydrogen sulfide (H2S) and bisulfide (SH) are the conjugate acids of sulfide.

A selenide is a chemical compound containing a selenium with oxidation number of −2. Similar to sulfide, selenides occur both as inorganic compounds and as organic derivatives, which are called organoselenium compound.

<span class="mw-page-title-main">Chalcogenide</span>

A chalcogenide is a chemical compound consisting of at least one chalcogen anion and at least one more electropositive element. Although all group 16 elements of the periodic table are defined as chalcogens, the term chalcogenide is more commonly reserved for sulfides, selenides, tellurides, and polonides, rather than oxides. Many metal ores exist as chalcogenides. Photoconductive chalcogenide glasses are used in xerography. Some pigments and catalysts are also based on chalcogenides. The metal dichalcogenide MoS2 is a common solid lubricant.

<span class="mw-page-title-main">Silver compounds</span> Chemical compounds containing silver

Silver is a relatively unreactive metal, although it can form several compounds. The common oxidation states of silver are (in order of commonness): +1 (the most stable state; for example, silver nitrate, AgNO3); +2 (highly oxidising; for example, silver(II) fluoride, AgF2); and even very rarely +3 (extreme oxidising; for example, potassium tetrafluoroargentate(III), KAgF4). The +3 state requires very strong oxidising agents to attain, such as fluorine or peroxodisulfate, and some silver(III) compounds react with atmospheric moisture and attack glass. Indeed, silver(III) fluoride is usually obtained by reacting silver or silver monofluoride with the strongest known oxidizing agent, krypton difluoride.

<span class="mw-page-title-main">Amalgam (chemistry)</span> Alloy of mercury with another metal

An amalgam is an alloy of mercury with another metal. It may be a liquid, a soft paste or a solid, depending upon the proportion of mercury. These alloys are formed through metallic bonding, with the electrostatic attractive force of the conduction electrons working to bind all the positively charged metal ions together into a crystal lattice structure. Almost all metals can form amalgams with mercury, the notable exceptions being iron, platinum, tungsten, and tantalum. Silver-mercury amalgams are important in dentistry, and gold-mercury amalgam is used in the extraction of gold from ore. Dentistry has used alloys of mercury with metals such as silver, copper, indium, tin and zinc.

<span class="mw-page-title-main">Post-transition metal</span> Category of metallic elements

The metallic elements in the periodic table located between the transition metals to their left and the chemically weak nonmetallic metalloids to their right have received many names in the literature, such as post-transition metals, poor metals, other metals, p-block metals and chemically weak metals. The most common name, post-transition metals, is generally used in this article.

References

  1. Fluck, E. (1988). "New Notations in the Periodic Table" (PDF). Pure Appl. Chem. 60 (3): 431–436. doi:10.1351/pac198860030431. S2CID   96704008 . Retrieved 24 March 2012.
  2. 1 2 Greenwood & Earnshaw 1997.
  3. Cotton et al. 1999.
  4. Housecroft, C. E.; Sharpe, A. G. (2008). Inorganic Chemistry (3rd ed.). Prentice Hall. ISBN   978-0-13-175553-6.
  5. 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.; Haenssler, F.; et al. (2007). "Chemical Characterization of Element 112". Nature . 447 (7140): 72–75. Bibcode:2007Natur.447...72E. doi:10.1038/nature05761. PMID   17476264. S2CID   4347419.
  6. Simmons, L. M. (December 1947). "A modification of the periodic table". Journal of Chemical Education. 24 (12): 588. Bibcode:1947JChEd..24..588S. doi:10.1021/ed024p588.
  7. Mewes, J.-M.; Smits, O. R.; Kresse, G.; Schwerdtfeger, P. (2019). "Copernicium is a Relativistic Noble Liquid". Angewandte Chemie International Edition. 58 (50): 17964–17968. doi:10.1002/anie.201906966. PMC   6916354 . PMID   31596013.
  8. 1 2 "Zinc Metal Properties". American Galvanizers Association. 2008. Archived from the original on February 21, 2009. Retrieved 2009-02-15.
  9. 1 2 3 4 5 6 David R. Lide, ed. (2006). Handbook of Chemistry and Physics (87th ed.). Boca Raton, Florida: CRC Press, Taylor & Francis Group. p. 4-41. ISBN   978-0-8493-0487-3.
  10. 1 2 Heiserman, David L. (1992). "Element 30: Zinc". Exploring Chemical Elements and their Compounds. New York: TAB Books. p. 123. ISBN   978-0-8306-3018-9.
  11. 1 2 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.
  12. 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.
  13. 1 2 3 4 Mewes, Jan-Michael; Smits, Odile R.; Kresse, Georg; Schwerdtfeger, Peter (2019). "Copernicium: A Relativistic Noble Liquid". Angewandte Chemie. 131 (50): 18132–18136. Bibcode:2019AngCh.13118132M. doi: 10.1002/ange.201906966 . ISSN   1521-3757.
  14. 1 2 Lehto 1968, p. 826.
  15. Scoffern, John (1861). The Useful Metals and Their Alloys. Houlston and Wright. pp.  591–603. Retrieved 2009-04-06.
  16. 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   978-3-11-007511-3.
  17. "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.
  18. 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.
  19. "Why is mercury a liquid at STP?" . Retrieved 2009-07-07.
  20. 1 2 3 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.
  21. 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.
  22. Vargel, C.; Jacques, M.; Schmidt, M. P. (2004). Corrosion of Aluminium. Elsevier. p. 158. ISBN   978-0-08-044495-6.
  23. 1 2 3 Moss, Alex (2003). "Descriptive P-block Notes" (PDF). Alchemyst Online. Retrieved June 2, 2011.
  24. Lindberg, S. E.; Stratton, W. J. (1998). "Atmospheric Mercury Speciation: Concentrations and Behavior of Reactive Gaseous Mercury in Ambient Air". Environmental Science and Technology. 32 (1): 49–57. Bibcode:1998EnST...32...49L. doi:10.1021/es970546u.
  25. 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. 3 (5): 849–852. doi:10.1016/0022-1902(77)80167-X.
  26. IUPAC , Compendium of Chemical Terminology , 2nd ed. (the "Gold Book") (1997). Online corrected version: (2006) " transition element ". doi : 10.1351/goldbook.T06456
  27. Elusive Hg(IV) species has been synthesized under cryogenic conditions
  28. 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. Bibcode:2007AngCh.119.8523W. doi:10.1002/ange.200703710.
  29. 1 2 3 4 5 Jensen, William B. (2003). "The Place of Zinc, Cadmium, and Mercury in the Periodic Table" (PDF). Journal of Chemical Education. 80 (8): 952–961. Bibcode:2003JChEd..80..952J. doi:10.1021/ed080p952. Archived from the original (PDF) on 2010-06-11. Retrieved 2012-05-06.
  30. 1 2 3 4 Royal Society of Chemistry. "Visual Elements: Group 2–The Alkaline Earth Metals". Visual Elements. Royal Society of Chemistry. Retrieved 13 January 2012.
  31. Kirby, H. W.; Salutsky, Murrell L. (1964). The Radiochemistry of Radium. National Academies Press.[ permanent dead link ]
  32. H. W. Gäggeler (2007). "Gas Phase Chemistry of Superheavy Elements" (PDF). Paul Scherrer Institute. pp. 26–28. Archived from the original (PDF) on 2012-02-20.
  33. 1 2 3 Haire, Richard G. (2006). "Transactinides and the future elements". In Morss; Edelstein, Norman M.; Fuger, Jean (eds.). The Chemistry of the Actinide and Transactinide Elements (3rd ed.). Dordrecht, The Netherlands: Springer Science+Business Media. p. 1675. ISBN   978-1-4020-3555-5.
  34. Fricke, Burkhard (1975). Superheavy elements: a prediction of their chemical and physical properties. Structure and Bonding. Vol. 21. pp.  89–144. doi:10.1007/BFb0116498. ISBN   978-3-540-07109-9 . Retrieved 4 October 2013.{{cite book}}: |journal= ignored (help)
  35. Richens, David T. (September 1997). The Chemistry of Aqua Ions. J. Wiley. ISBN   978-0-471-97058-3.
  36. Weeks 1933, p. 20.
  37. Greenwood & Earnshaw 1997, p. 1201.
  38. 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. Vol. 1 (2nd ed.). The Bengal Chemical & Pharmaceutical Works. pp. 157–158. (public domain text)
  39. Arny, Henry Vinecome (1917). Principles of Pharmacy (2nd ed.). W. B. Saunders company. p.  483.
  40. Habashi, Fathi. "Discovering the 8th Metal" (PDF). International Zinc Association (IZA). Archived from the original (PDF) on 2009-03-04. Retrieved 2008-12-13.
  41. Hoover, Herbert Clark (2003). Georgius Agricola de Re Metallica. Kessinger Publishing. p. 409. ISBN   978-0-7661-3197-2.
  42. Gerhartz, Wolfgang (1996). Ullmann's Encyclopedia of Industrial Chemistry (5th ed.). VHC. p. 509. ISBN   978-3-527-20100-6.
  43. Emsley 2001, p. 502.
  44. Weeks 1933, p. 21.
  45. 1 2 Warren, Neville G. (2000). Excel Preliminary Physics. Pascal Press. p. 47. ISBN   978-1-74020-085-1.
  46. "Galvanic Cell". The New International Encyclopaedia. Dodd, Mead and Company. 1903. p. 80.
  47. Cotton et al. 1999, p. 626.
  48. "Cadmium". Kirk-Othmer Encyclopedia of Chemical Technology. Vol. 5 (4th ed.). New York: John Wiley & Sons. 1994.
  49. 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.
  50. Waterston, William; Burton, J. H (1844). Cyclopædia of commerce, mercantile law, finance, commercial geography and navigation. p. 122.
  51. Rowbotham, Thomas Leeson (1850). The art of landscape painting in water colours, by T. and T. L. Rowbotham. p. 10.
  52. Ayres, Robert U.; Ayres, Leslie; Råde, Ingrid (2003). The life cycle of copper, its co-products and byproducts. Springer. pp. 135–141. ISBN   978-1-4020-1552-6.
  53. Burdun, G. D. (1958). "On the new determination of the meter". Measurement Techniques. 1 (3): 259–264. doi:10.1007/BF00974680. S2CID   121450003.
  54. Beers, John S.; Penzes, William B. (May–June 1999). "The NIST Length Scale Interferometer" (PDF). Journal of Research of the National Institute of Standards and Technology. 104 (3): 226. doi:10.6028/jres.104.017. S2CID   2981956.
  55. Marion, Jerry B. (1982). Physics For Science and Engineering. CBS College Publishing. p. 3. ISBN   978-4-8337-0098-6.
  56. "Mercury and the environment — Basic facts". Environment Canada, Federal Government of Canada. 2004. Archived from the original on 2007-01-15. Retrieved 2008-03-27.
  57. Wright, David Curtis (2001). The History of China. Greenwood Publishing Group. p.  49. ISBN   978-0-313-30940-3.
  58. Hesse, R. W. (2007). Jewelrymaking through history. Greenwood Publishing Group. p. 120. ISBN   978-0-313-33507-5.
  59. 1 2 Stillman, J. M. (2003). Story of Alchemy and Early Chemistry. Kessinger Publishing. pp. 7–9. ISBN   978-0-7661-3230-6.[ permanent dead link ]
  60. Cox, R. (1997). The Pillar of Celestial Fire. 1st World Publishing. p. 260. ISBN   978-1-887472-30-2.
  61. 1 2 Hofmann, S.; et al. (1996). "The new element 112". Zeitschrift für Physik A . 354 (1): 229–230. Bibcode:1996ZPhyA.354..229H. doi:10.1007/BF02769517. S2CID   119975957.
  62. Barber, Robert C.; Gäggeler, Heinz W.; Karol, Paul J.; Nakahara, Hiromichi; Vardaci, Emanuele; Vogt, Erich (2009). "Element 112 is Named Copernicium". Pure and Applied Chemistry. 81 (7): 1331–1343. doi: 10.1351/PAC-REP-08-03-05 .
  63. 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.
  64. 1 2 Greenwood & Earnshaw 1997, p. 1202.
  65. Plachy, Jozef. "Annual Average Cadmium Price" (PDF). USGS. Retrieved June 16, 2010.
  66. 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.
  67. Fleischer, Michael (1980). "New Mineral Names" (PDF). American Mineralogist. 65: 1065–1070.
  68. Ehrlich, H. L.; Newman D. K. (2008). Geomicrobiology. CRC Press. p. 265. ISBN   978-0-8493-7906-2.
  69. 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. S2CID   127179672.
  70. Tolcin, A. C. (2011). "Mineral Commodity Summaries 2009: Zinc" (PDF). United States Geological Survey . Retrieved 2011-06-06.
  71. "Country Partnership Strategy—Iran: 2011–12". ECO Trade and development bank. Archived from the original on 2011-10-26. Retrieved 2011-06-06.
  72. "IRAN – a growing market with enormous potential". IMRG. July 5, 2010. Archived from the original on 2013-02-17. Retrieved 2010-03-03.
  73. Cohen, David (2007). "Earth audit". New Scientist. 194 (2605): 8. doi:10.1016/S0262-4079(07)61315-3.
  74. "Augsberg University Calculate When Our Materials Run Out". IDTechEx. 2007-06-04. Retrieved 2008-12-09.
  75. 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.
  76. World Mineral Production (Report). London: British Geological Survey, NERC. 2007.
  77. About the Mercury Rule Archived 2012-05-01 at the Wayback Machine
  78. "Zinc: World Mine Production (zinc content of concentrate) by Country" (PDF). 2006 Minerals Yearbook: Zinc: Table 15. February 2008. Retrieved 2009-01-19.
  79. Rosenqvist, Terkel (1922). Principles of Extractive Metallurgy (2 ed.). Tapir Academic Press. pp. 7, 16, 186. ISBN   978-82-519-1922-7.
  80. 1 2 3 Porter, Frank C. (1991). Zinc Handbook. CRC Press. ISBN   978-0-8247-8340-2.
  81. Bodsworth, Colin (1994). The Extraction and Refining of Metals. CRC Press. p. 148. ISBN   978-0-8493-4433-6.
  82. Gupta, C. K.; Mukherjee, T. K. (1990). Hydrometallurgy in Extraction Processes. CRC Press. p. 62. ISBN   978-0-8493-6804-2.
  83. National Research Council, 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.
  84. Scoullos, Michael J (2001-12-31). Mercury, cadmium, lead: handbook for sustainable heavy metals policy and regulation. Springer. pp. 104–116. ISBN   978-1-4020-0224-3.
  85. 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. S2CID   127179672.
  86. Vallero, Daniel A. (2008). Fundamentals of air pollution. Elsevier. pp. 865–866. ISBN   978-0-12-373615-4.
  87. 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)" (PDF). Pure and Applied Chemistry. 81 (7): 1331. doi:10.1351/PAC-REP-08-03-05. S2CID   95703833.
  88. Stwertka 1998, p. [ page needed ].
  89. Emsley 2001, pp. 499–505.
  90. 1 2 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. Archived from the original (PDF) on March 4, 2016. Retrieved May 29, 2011.
  91. Newman, John (2004). Electrochemical Systems. New Jersey: John Wiley & Sons. ISBN   978-0-471-47756-3.
  92. 1 2 "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.
  93. 1 2 3 4 5 Lehto 1968, p. 829.
  94. 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. S2CID   135744939.
  95. Stwertka 1998, p. 99.
  96. Besenhard, Jürgen O. (1999). Handbook of Battery Materials (PDF). Wiley-VCH. Bibcode:1999hbm..book.....B. ISBN   978-3-527-29469-5 . Retrieved 2008-10-08.
  97. 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. Bibcode:1995JPS....57...61W. doi:10.1016/0378-7753(95)02242-2.
  98. Culter, T. (1996). "A design guide for rechargeable zinc-air battery technology". Southcon/96 Conference Record. p. 616. doi:10.1109/SOUTHC.1996.535134. ISBN   978-0-7803-3268-3. S2CID   106826667.
  99. Whartman, Jonathan; Brown, Ian. "Zinc Air Battery-Battery Hybrid for Powering Electric Scooters and Electric Buses" (PDF). The 15th International Electric Vehicle Symposium. Archived from the original (PDF) on 2006-03-12. Retrieved 2008-10-08.
  100. Cooper, J. F.; Fleming, D.; Hargrove, D.; Koopman; R.; Peterman, K. (1995). "A refuelable zinc/air battery for fleet electric vehicle propulsion". NASA Sti/Recon Technical Report N. 96. Society of Automotive Engineers future transportation technology conference and exposition: 11394. Bibcode:1995STIN...9611394C. OSTI   82465.
  101. "Diecasting Alloys". Maybrook, NY: Eastern Alloys. Retrieved 2009-01-19.
  102. Buxbaum, Gunter; Pfaff, Gerhard (2005). "Cadmium Pigments". Industrial inorganic pigments. Wiley-VCH. pp. 121–123. ISBN   978-3-527-30363-2.[ permanent dead link ]
  103. "Battery collection; recycling, nature protected". European Union . Retrieved November 4, 2008.
  104. 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. Bibcode:2004gucd.book.....H. ISBN   978-0-8194-5532-1.
  105. "Mercury Reduction Act of 2003". United States. Congress. Senate. Committee on Environment and Public Works. Retrieved 2009-06-06.
  106. 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. S2CID   22732411.
  107. FDA. "Thimerosal in Vaccines". Food and Drug Administration . Retrieved October 25, 2006.
  108. "The CRB Commodity Yearbook (annual)". The CRB Commodity Yearbook: 173. 2000. ISSN   1076-2906.
  109. 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.
  110. "Chlorine Online Diagram of mercury cell process". Euro Chlor. Archived from the original on September 18, 2011. Retrieved 2012-04-09.
  111. 1 2 3 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.
  112. 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.
  113. Zinc's role in microorganisms is particularly reviewed in: Sugarman, B. (1983). "Zinc and infection". Reviews of Infectious Diseases. 5 (1): 137–47. doi:10.1093/clinids/5.1.137. PMID   6338570.
  114. Rink, L.; Gabriel, P. (2000). "Zinc and the immune system". Proc Nutr Soc. 59 (4): 541–52. doi: 10.1017/S0029665100000781 . PMID   11115789.
  115. Wapnir, Raul A. (1990). Protein Nutrition and Mineral Absorption. Boca Raton, Florida: CRC Press. ISBN   978-0-8493-5227-0.
  116. Hambidge, K. M.; Krebs, N. F. (2007). "Zinc deficiency: a special challenge". J. Nutr. 137 (4): 1101–5. doi: 10.1093/jn/137.4.1101 . PMID   17374687.
  117. 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.
  118. 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.
  119. Institute of Medicine (US) Panel on Micronutrients (2001). Zinc – Summary. Institute of Medicine, Food and Nutrition Board. doi:10.17226/10026. ISBN   978-0-309-07279-3. PMID   25057538 . Retrieved 2010-03-30.{{cite book}}: |work= ignored (help)
  120. 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. S2CID   8053594.
  121. 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.

Bibliography