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{{chembox
{{chembox
|Watchedfields = changed
| verifiedrevid = 443541125
|verifiedrevid = 443542677
| ImageFile = Kristallstruktur Chalkosin.png
|ImageFile = Kristallstruktur Chalkosin.png
| ImageSize =
| IUPACName = Copper(I) sulfide
|IUPACName = Copper(I) sulfide
| OtherNames = Cuprous sulfide<br/>[[Chalcocite]]<br/>Copper glance
|OtherNames = Cuprous sulfide<br/>[[Chalcocite]]<br/>Copper glance
| Section1 = {{Chembox Identifiers
|Section1={{Chembox Identifiers
| ChemSpiderID_Ref = {{chemspidercite|correct|chemspider}}
|ChemSpiderID_Ref = {{chemspidercite|correct|chemspider}}
| ChemSpiderID = 8305611
|ChemSpiderID = 8305611
| InChI = 1/2Cu.S/q2*+1;-2
|InChI = 1/2Cu.S/q2*+1;-2
| ChEBI_Ref = {{ebicite|correct|EBI}}
|ChEBI_Ref = {{ebicite|correct|EBI}}
| ChEBI = 51114
|ChEBI = 51114
| SMILES = [Cu+].[Cu+].[S-2]
|SMILES = [Cu+].[Cu+].[S-2]
| InChIKey = AQMRBJNRFUQADD-UHFFFAOYAN
|InChIKey = AQMRBJNRFUQADD-UHFFFAOYAN
| StdInChI_Ref = {{stdinchicite|correct|chemspider}}
|StdInChI_Ref = {{stdinchicite|correct|chemspider}}
| StdInChI = 1S/2Cu.S/q2*+1;-2
|StdInChI = 1S/2Cu.S/q2*+1;-2
| StdInChIKey_Ref = {{stdinchicite|correct|chemspider}}
|StdInChIKey_Ref = {{stdinchicite|correct|chemspider}}
| StdInChIKey = AQMRBJNRFUQADD-UHFFFAOYSA-N
|StdInChIKey = AQMRBJNRFUQADD-UHFFFAOYSA-N
| CASNo = 22205-45-4
|CASNo = 22205-45-4
| CASNo_Ref = {{cascite|correct|CAS}}
|CASNo_Ref = {{cascite|correct|CAS}}
|UNII_Ref = {{fdacite|correct|FDA}}
| PubChem = 62755
|UNII = 349M3C1RS1
| RTECS = GL8910000
|PubChem = 62755
}}
|RTECS = GL8910000
| Section2 = {{Chembox Properties
}}
| Formula = Cu<sub>2</sub>S
|Section2={{Chembox Properties
| MolarMass = 159.16 g/mol
|Formula = Cu<sub>2</sub>S
| Appearance =
|MolarMass = 159.16 g/mol
| Density = 5.6 g/cm<sup>3</sup> <ref>Pradyot Patnaik. ''Handbook of Inorganic Chemicals''. McGraw-Hill, 2002, ISBN 0070494398</ref>
|Density = 5.6 g/cm<sup>3</sup> <ref>Patnaik, Pradyot (2002). ''Handbook of Inorganic Chemicals''. McGraw-Hill, {{ISBN|0-07-049439-8}}</ref>
| MeltingPt = 1130 °C<ref name ="Greenwood">{{Greenwood&Earnshaw1st|page=1373}}</ref>
| BoilingPt =
|MeltingPtC = 1130
|MeltingPt_ref = <ref name ="Greenwood">{{Greenwood&Earnshaw1st|page=1373}}</ref>
| Solubility = Insoluble
|Solubility = insoluble
| 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>]]
|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>]]
}}
}}
| Section7 = {{Chembox Hazards
|Section3={{Chembox Hazards
| EUIndex = Not listed
| FlashPt = Non-flammable
|FlashPt = Nonflammable
|PEL = TWA 1 mg/m<sup>3</sup> (as Cu)<ref name=PGCH>{{PGCH|0150}}</ref>
}}
|REL = TWA 1 mg/m<sup>3</sup> (as Cu)<ref name=PGCH/>
| Section8 = {{Chembox Related
|IDLH = TWA 100 mg/m<sup>3</sup> (as Cu)<ref name=PGCH/>
| OtherAnions = [[Copper(I) oxide]]<br/>[[Copper(I) selenide]]
}}
| OtherCations = [[Nickel(II) sulfide]]<br/>[[Copper(II) sulfide]]<br/>[[Zinc sulfide]]
|Section4={{Chembox Related
}}
|OtherAnions = [[Copper(I) oxide]]<br/>[[Copper(I) selenide]]
|OtherCations = [[Nickel(II) sulfide]]<br/>[[Copper(II) sulfide]]<br/>[[Zinc sulfide]]
}}
}}
}}


'''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. Potter, Economic Geology; 1977; 72;. 8; 1524-1542</ref>.
'''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.


==Preparation and Reactions==
==Preparation and reactions==
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>
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>
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>
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>
:{{chem2|2 Cu2S + 3 O2 -> 2 Cu2O + 2 SO2}}
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>

:2Cu<sub>2</sub>S + 3O<sub>2</sub> → 2Cu<sub>2</sub>O + 2SO<sub>2</sub>
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"/>
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"/>
:{{chem2|Cu2S + O2 -> 2 Cu + SO2}}
: Cu<sub>2</sub>S + 2Cu<sub>2</sub>O → 6Cu + SO<sub>2</sub>
Cuprous oxide readily converts to copper metal upon heating.


==Structure==
==Structure==
[[File:Chalcocite-139819.jpg|thumb|left|Crystals of chalcocite (mineral form of Cu<sub>2</sub>S).]]
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" [http://dx.doi.org/10.1126/science.203.4378.356 Science 203 (1979) 356]</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.

=== Stoichiometric ===
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&nbsp;°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.

=== Non-stoichiometric ===
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>


== Phase transition ==
There is also a crystallographically-distinct phase (the mineral [[djurleite]]) with stoichiometry Cu<sub>1.96</sub>S which 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>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>
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>


==See also==
==See also==
*[[copper sulfide]] for an overview of all copper sulfide phases
*[[Copper sulfide]] for an overview of all copper sulfide phases
*[[copper monosulfide]], CuS
*[[Copper monosulfide]], CuS
*[[Chalcocite]]
*[[Chalcocite]]
*[[Djurleite]]
*[[Djurleite]]
*[[LK-99]] - compound evaluated in 2023 for possible superconductivity


==References==
==References==
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{{Copper compounds}}
{{Copper compounds}}
{{Sulfides}}


[[Category:Sulfide minerals]]
[[Category:Sulfide minerals]]
[[Category:Sulfides]]
[[Category:Sulfides]]
[[Category:Copper compounds]]
[[Category:Copper(I) compounds]]
[[Category:Non-stoichiometric compounds]]
[[Category:Non-stoichiometric compounds]]


[[ca:Sulfur de coure]]
[[de:Kupfer(I)-sulfid]]
[[fa:مس(۱) سولفید]]
[[ja:硫化銅]]
[[ja:硫化銅]]
[[pl:Siarczek miedzi(I)]]
[[tr:Bakır(I) sülfür]]
[[ru:Сульфид меди(I)]]