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{{chembox |
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| verifiedrevid = 443541125 |
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|verifiedrevid = 443542677 |
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| ImageFile = Kristallstruktur Chalkosin.png |
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|ImageFile = Kristallstruktur Chalkosin.png |
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| ImageSize = |
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| IUPACName = Copper(I) sulfide |
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|IUPACName = Copper(I) sulfide |
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| OtherNames = Cuprous sulfide<br/>]<br/>Copper glance |
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|OtherNames = Cuprous sulfide<br/>]<br/>Copper glance |
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| Section1 = {{Chembox Identifiers |
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|Section1={{Chembox Identifiers |
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| ChemSpiderID_Ref = {{chemspidercite|correct|chemspider}} |
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|ChemSpiderID_Ref = {{chemspidercite|correct|chemspider}} |
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| ChemSpiderID = 8305611 |
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|ChemSpiderID = 8305611 |
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| InChI = 1/2Cu.S/q2*+1;-2 |
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|InChI = 1/2Cu.S/q2*+1;-2 |
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| ChEBI_Ref = {{ebicite|correct|EBI}} |
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|ChEBI_Ref = {{ebicite|correct|EBI}} |
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| ChEBI = 51114 |
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|ChEBI = 51114 |
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| SMILES = .. |
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|SMILES = .. |
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| InChIKey = AQMRBJNRFUQADD-UHFFFAOYAN |
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|InChIKey = AQMRBJNRFUQADD-UHFFFAOYAN |
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| StdInChI_Ref = {{stdinchicite|correct|chemspider}} |
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|StdInChI_Ref = {{stdinchicite|correct|chemspider}} |
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| StdInChI = 1S/2Cu.S/q2*+1;-2 |
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|StdInChI = 1S/2Cu.S/q2*+1;-2 |
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| StdInChIKey_Ref = {{stdinchicite|correct|chemspider}} |
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|StdInChIKey_Ref = {{stdinchicite|correct|chemspider}} |
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| StdInChIKey = AQMRBJNRFUQADD-UHFFFAOYSA-N |
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|StdInChIKey = AQMRBJNRFUQADD-UHFFFAOYSA-N |
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| CASNo = 22205-45-4 |
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|CASNo = 22205-45-4 |
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| CASNo_Ref = {{cascite|correct|CAS}} |
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|CASNo_Ref = {{cascite|correct|CAS}} |
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|UNII_Ref = {{fdacite|correct|FDA}} |
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| PubChem = 62755 |
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|UNII = 349M3C1RS1 |
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| RTECS = GL8910000 |
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|PubChem = 62755 |
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|RTECS = GL8910000 |
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| Section2 = {{Chembox Properties |
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| Formula = Cu<sub>2</sub>S |
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|Section2={{Chembox Properties |
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| MolarMass = 159.16 g/mol |
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|Formula = Cu<sub>2</sub>S |
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| Appearance = |
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|MolarMass = 159.16 g/mol |
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| Density = 5.6 g/cm<sup>3</sup> <ref>Pradyot Patnaik. ''Handbook of Inorganic Chemicals''. McGraw-Hill, 2002, ISBN 0070494398</ref> |
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|Density = 5.6 g/cm<sup>3</sup> <ref>Patnaik, Pradyot (2002). ''Handbook of Inorganic Chemicals''. McGraw-Hill, {{ISBN|0-07-049439-8}}</ref> |
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| MeltingPt = 1130 °C<ref name ="Greenwood">{{Greenwood&Earnshaw1st|page=1373}}</ref> |
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| BoilingPt = |
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|MeltingPtC = 1130 |
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|MeltingPt_ref = <ref name ="Greenwood">{{Greenwood&Earnshaw1st|page=1373}}</ref> |
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| Solubility = Insoluble |
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|Solubility = insoluble |
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| SolubleOther = slightly soluble in ]; soluble in ]; dissolves in ]; decomposes in ], ] |
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|SolubleOther = slightly soluble in ]; soluble in ]; dissolves in ]; decomposes in ], ] |
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| Section7 = {{Chembox Hazards |
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|Section3={{Chembox Hazards |
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| EUIndex = Not listed |
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| FlashPt = Non-flammable |
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|FlashPt = Nonflammable |
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|PEL = TWA 1 mg/m<sup>3</sup> (as Cu)<ref name=PGCH>{{PGCH|0150}}</ref> |
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|REL = TWA 1 mg/m<sup>3</sup> (as Cu)<ref name=PGCH/> |
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| Section8 = {{Chembox Related |
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|IDLH = TWA 100 mg/m<sup>3</sup> (as Cu)<ref name=PGCH/> |
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| OtherAnions = ]<br/>] |
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| OtherCations = ]<br/>]<br/>] |
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|Section4={{Chembox Related |
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|OtherAnions = ]<br/>] |
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|OtherCations = ]<br/>]<br/>] |
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'''Copper(I) sulfide''' is a ], a chemical compound of ] and ]. It has the chemical compound Cu<sub>2</sub>S. It is found in nature as the mineral ]. It has a narrow range of stoichiometry ranging from Cu<sub>1.997</sub>S to Cu<sub>2.000</sub>S<ref>An electrochemical investigation of the system copper-sulfur, R. W. Potter, Economic Geology; 1977; 72;. 8; 1524-1542</ref>. |
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'''Copper(I) sulfide''' is a ], a chemical compound of ] and ]. It has the chemical compound Cu<sub>2</sub>S. It is found in nature as the mineral ]. It has a narrow range of stoichiometry ranging from Cu<sub>1.997</sub>S to Cu<sub>2.000</sub>S.<ref>{{cite journal|title=An electrochemical investigation of the system copper-sulfur|author=Potter, R. W. |journal=Economic Geology|year=1977|volume=72 |issue=8|pages= 1524–1542|doi=10.2113/gsecongeo.72.8.1524|bibcode=1977EcGeo..72.1524P }}</ref> Samples are typically black. |
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==Preparation and Reactions== |
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==Preparation and reactions== |
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Cu<sub>2</sub>S can be prepared by heating copper strongly in sulfur vapour or H<sub>2</sub>S<ref name ="Greenwood"/>. The reaction of copper powder in molten sulfur rapidly produces Cu<sub>2</sub>S, whereas pellets of copper require much higher temperature<ref> |
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Cu<sub>2</sub>S can be prepared by treating copper with sulfur or H<sub>2</sub>S.<ref name ="Greenwood"/> The rate depends on the particle size and temperature.<ref>{{cite journal|title=The formation of Cu<sub>2</sub>S from the elements I. Copper used in form of powders|author= Blachnik R., Müller A.|doi=10.1016/S0040-6031(00)00545-1|year=2000|journal=Thermochimica Acta|volume=361|pages=31}}</ref> |
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Cu<sub>2</sub>S reacts with oxygen to form SO<sub>2</sub>:<ref name = "Wiberg&Holleman">Wiberg, Egon and Holleman, Arnold Frederick (2001) ''Inorganic Chemistry'', Elsevier {{ISBN|0-12-352651-5}}</ref> |
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The formation of Cu2S from the elements I. Copper used in form of powders, Blachnik R., Müller A., Thermochimica Acta, 361, 1-2, (2000), 31-52, {{doi|10.1016/S0040-6031(00)00545-1}}</ref> |
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:{{chem2|2 Cu2S + 3 O2 -> 2 Cu2O + 2 SO2}} |
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Cu<sub>2</sub>S reacts with oxygen to form SO<sub>2</sub>:<ref name = "Wiberg&Holleman">Egon Wiberg, Arnold Frederick Holleman (2001) ''Inorganic Chemistry'', Elsevier ISBN 0123526515</ref> |
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:2Cu<sub>2</sub>S + 3O<sub>2</sub> → 2Cu<sub>2</sub>O + 2SO<sub>2</sub> |
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In the production of copper two thirds of the molten copper sulfide is oxidised as above, and the Cu<sub>2</sub>O reacts with unoxidised Cu<sub>2</sub>S to give Cu metal:<ref name = "Wiberg&Holleman"/> |
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The production of copper from chalcocite is a typical process in extracting the metal from ores. Usually, the conversion involves roasting, to give Cu<sub>2</sub>O and sulfur dioxide:<ref name = "Wiberg&Holleman"/> |
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:{{chem2|Cu2S + O2 -> 2 Cu + SO2}} |
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: Cu<sub>2</sub>S + 2Cu<sub>2</sub>O → 6Cu + SO<sub>2</sub> |
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Cuprous oxide readily converts to copper metal upon heating. |
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==Structure== |
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==Structure== |
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There are two forms of Cu<sub>2</sub>S a low temperature monoclinic form ("low-chalcocite") which has a complex structure with 96 copper atoms in the unit cell<ref name=evans>H. T. Evans "Djurleite (Cu1.94S) and Low Chalcocite (Cu2S): New Crystal Structure Studies" </ref> and a hexagonal form stable above 104°C.<ref name = "Wells"> Wells A.F. (1984) ''Structural Inorganic Chemistry'' 5th edition Oxford Science Publications ISBN 0-19-855370-6 </ref> In this structure there are 24 crystallographically distinct Cu atoms and the structure has been described as approximating to a hexagonal close packed array of sulfur atoms with Cu atoms in planar 3 coordination. This structure was initially assigned an orthorhombic cell due to the twinning of the sample crystal. |
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=== Stoichiometric === |
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Two forms (]) of Cu<sub>2</sub>S are known. The so-called low temperature ] ("low-chalcocite") has a complex structure with 96 copper atoms in the unit cell.<ref name=evans>{{cite journal|doi=10.1126/science.203.4378.356|title=Djurleite (Cu<sub>1.94</sub>S) and Low Chalcocite (Cu<sub>2</sub>S): New Crystal Structure Studies|year=1979|last1=Evans|first1=H. T.|journal=Science|volume=203|issue=4378|pages=356–8|pmid=17772445|bibcode=1979Sci...203..356E |s2cid=6132717 }}</ref> The hexagonal form, stable above 104 °C,<ref name = "Wells">Wells A.F. (1984) ''Structural Inorganic Chemistry'', 5th ed., Oxford Science Publications, {{ISBN|0-19-855370-6}}</ref> has 24 crystallographically distinct Cu atoms. Its structure has been described as approximating to a ] array of sulfur atoms with Cu atoms in planar 3 coordination. This structure was initially assigned an orthorhombic cell due to the twinning of the sample crystal. |
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=== Non-stoichiometric === |
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As illustrated by the mineral ], a cuprous sulfide is also known. With the approximate formula Cu<sub>1.96</sub>S, this material is ] (range Cu<sub>1.934</sub>S-Cu<sub>1.965</sub>S) and has a monoclinic structure with 248 copper and 128 sulfur atoms in the unit cell.<ref name=evans/> Cu<sub>2</sub>S and Cu<sub>1.96</sub>S are similar in appearance and hard to distinguish one from another.<ref>{{cite journal|url=http://www.minsocam.org/ammin/AM66/AM66_807.pdf|title=Copper coordination in low chalcocite and djurleite and other copper-rich sulfides|author= Evans H.T.|journal=American Mineralogist|year=1981|volume= 66|issue= 7–8|pages=807–818}}</ref> |
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== Phase transition == |
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There is also a crystallographically-distinct phase (the mineral ]) with stoichiometry Cu<sub>1.96</sub>S which is ] (range Cu<sub>1.934</sub>S-Cu<sub>1.965</sub>S) and has a monoclinic structure with 248 copper and 128 sulfur atoms in the unit cell <ref name=evans/>. Cu<sub>2</sub>S and Cu<sub>1.96</sub>S are similar in appearance and hard to distinguish one from another.<ref>Copper coordination in low chalcocite and djurleite and other copper-rich sulfides, Evans H.T., American Mineralogist; August 1981, 66, 7-8, 807-818</ref> |
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The ] increases abruptly at the phase transition point around 104 °C, with the precise temperature depending on the stoichiometry.<ref>{{Cite journal |last=Garisto |first=Dan |date=2023-08-16 |title=LK-99 isn't a superconductor — how science sleuths solved the mystery |url=https://www.nature.com/articles/d41586-023-02585-7 |journal=Nature |volume=620 |issue=7975 |pages=705–706 |language=en |doi=10.1038/d41586-023-02585-7|pmid=37587284 |bibcode=2023Natur.620..705G |s2cid=260955242 }}</ref><ref>Jain, Prashant K. "]." ''arXiv preprint arXiv:2308.05222'' (2023).</ref> |
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==See also== |
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==See also== |
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*] for an overview of all copper sulfide phases |
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*] for an overview of all copper sulfide phases |
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*], CuS |
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*], CuS |
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*] - compound evaluated in 2023 for possible superconductivity |
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==References== |
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==References== |
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{{Copper compounds}} |
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{{Copper compounds}} |
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{{Sulfides}} |
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