Copper(I) sulfide: Difference between revisions
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|verifiedrevid = 443542677 |
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|ImageFile = Kristallstruktur Chalkosin.png |
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|IUPACName = Copper(I) sulfide |
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|OtherNames = Cuprous sulfide<br/>[[Chalcocite]]<br/>Copper glance |
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|Section1={{Chembox Identifiers |
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|ChemSpiderID_Ref = {{chemspidercite|correct|chemspider}} |
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|ChemSpiderID = 8305611 |
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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 = 51114 |
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|SMILES = [Cu+].[Cu+].[S-2] |
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|InChIKey = AQMRBJNRFUQADD-UHFFFAOYAN |
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|StdInChI_Ref = {{stdinchicite|correct|chemspider}} |
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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 = AQMRBJNRFUQADD-UHFFFAOYSA-N |
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|CASNo = 22205-45-4 |
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|CASNo_Ref = {{cascite|correct|CAS}} |
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|UNII_Ref = {{fdacite|correct|FDA}} |
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|UNII = 349M3C1RS1 |
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| Appearance = |
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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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|MeltingPtC = 1130 |
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|Solubility = insoluble |
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|SolubleOther = slightly soluble in [[hydrochloric acid|HCl]]; soluble in [[ammonium hydroxide|NH<sub>4</sub>OH]]; dissolves in [[potassium cyanide|KCN]]; decomposes in [[nitric acid|HNO<sub>3</sub>]], [[sulfuric acid|H<sub>2</sub>SO<sub>4</sub>]] |
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|Section3={{Chembox Hazards |
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| EUIndex = Not listed |
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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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|IDLH = TWA 100 mg/m<sup>3</sup> (as Cu)<ref name=PGCH/> |
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'''Copper(I) sulfide''' is a [[copper sulfide]], a chemical compound of [[copper]] and [[sulfur]]. It has the chemical compound Cu<sub>2</sub>S. It is found in nature as the mineral [[chalcocite]]. 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. |
'''Copper(I) sulfide''' is a [[copper sulfide]], a chemical compound of [[copper]] and [[sulfur]]. It has the chemical compound Cu<sub>2</sub>S. It is found in nature as the mineral [[chalcocite]]. 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 |
==Preparation and reactions== |
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Cu<sub>2</sub>S can be prepared by |
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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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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:2Cu<sub>2</sub>S + 3O<sub>2</sub> → 2Cu<sub>2</sub>O + 2SO<sub>2</sub> |
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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== |
==Structure== |
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[[File:Chalcocite-139819.jpg|thumb|left|Crystals of chalcocite (mineral form of Cu<sub>2</sub>S).]] |
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=== Stoichiometric === |
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⚫ | Two forms ([[Polymorphism (materials science)|a dimorphism]]) of Cu<sub>2</sub>S are known. The so-called low temperature [[Monoclinic crystal system|monoclinic form]] ("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 [[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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=== Non-stoichiometric === |
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⚫ | As illustrated by the mineral [[djurleite]], a cuprous sulfide is also known. With the approximate formula Cu<sub>1.96</sub>S, this material is [[non-stoichiometric]] (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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The [[electrical resistivity]] 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:2308.05222|Phase transition of copper (I) sulfide and its implication for purported superconductivity of LK-99]]." ''arXiv preprint arXiv:2308.05222'' (2023).</ref> |
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==See also== |
==See also== |
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*[[ |
*[[Copper sulfide]] for an overview of all copper sulfide phases |
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*[[ |
*[[Copper monosulfide]], CuS |
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*[[Chalcocite]] |
*[[Chalcocite]] |
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*[[Djurleite]] |
*[[Djurleite]] |
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*[[LK-99]] - compound evaluated in 2023 for possible superconductivity |
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==References== |
==References== |
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{{Copper compounds}} |
{{Copper compounds}} |
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{{Sulfides}} |
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[[Category:Sulfide minerals]] |
[[Category:Sulfide minerals]] |
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[[Category:Sulfides]] |
[[Category:Sulfides]] |
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[[Category:Copper compounds]] |
[[Category:Copper(I) compounds]] |
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[[Category:Non-stoichiometric compounds]] |
[[Category:Non-stoichiometric compounds]] |
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[[ca:Sulfur de coure]] |
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[[de:Kupfer(I)-sulfid]] |
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[[fa:مس(۱) سولفید]] |
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[[ja:硫化銅]] |
[[ja:硫化銅]] |
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[[tr:Bakır(I) sülfür]] |
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[[ru:Сульфид меди(I)]] |