كبريتيد النحاس الأحادي

كبريتيد النحاس الأحادي
Kristallstruktur Chalkosin.png
الأسماء
اسم أيوپاك
Copper(I) sulfide
أسماء أخرى
Cuprous sulfide
Chalcocite
Copper glance
المُعرِّفات
رقم CAS
3D model (JSmol)
ChEBI
ChemSpider
ECHA InfoCard 100.040.751 Edit this at Wikidata
رقم RTECS
  • GL8910000
UNII
الخصائص
الصيغة الجزيئية Cu
2
S
كتلة مولية 159.16 g/mol
الكثافة 5.6 g/cm3[1][صفحة مطلوبة]
نقطة الانصهار
قابلية الذوبان في الماء insoluble[بحاجة لمصدر]
قابلية الذوبان في hydrochloric acid slightly soluble[بحاجة لمصدر][كمية]
قابلية الذوبان في ammonium hydroxide soluble[بحاجة لمصدر][كمية]
المخاطر[3]
صفحة بيانات السلامة Sigma-Aldrich[2]
NFPA 704 (معيـَّن النار)
Flammability code 0: لن يشتعل. مثل الماءHealth code 0: التعرض تحت ظروف النار لن يشكل خطراً أكثر من مادة عادية قابلة للاشتعال. مثل كلوريد الصوديومReactivity (yellow): no hazard codeSpecial hazards (white): no codeNFPA 704 four-colored diamond
0
0
نقطة الوميض Nonflammable
حدود التعرض الصحية بالولايات المتحدة (NIOSH):[4]
PEL (المسموح)
TWA 1 mg/m3 (as Cu)
REL (الموصى به)
TWA 1 mg/m3 (as Cu)
IDLH (خطر عاجل)
TWA 100 mg/m3 (as Cu)
مركبات ذا علاقة
ما لم يُذكر غير ذلك، البيانات المعطاة للمواد في حالاتهم العيارية (عند 25 °س [77 °ف]، 100 kPa).
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مراجع الجدول

Copper(I) sulfide is a copper sulfide, a chemical compound of copper and sulfur. It has the chemical formula of Cu
2
S
. It is found in nature as the mineral chalcocite. It has a narrow range of stoichiometry ranging from Cu
1.997
S
to Cu
2.000
S
.[5] Samples are typically black.[بحاجة لمصدر]

التحضير والتفاعلات

Cu
2
S
can be prepared by treating copper with sulfur or H
2
S
.[6] The rate depends on the particle size and temperature.[7] Cu
2
S
reacts with oxygen to form SO
2
:[8][صفحة مطلوبة]

2 Cu
2
S + 3 O
2
→ 2 Cu
2
O + 2 SO
2

The production of copper from chalcocite is a typical process in extracting the metal from ores. Usually, the conversion involves roasting, to give Cu
2
O
as an intermediate which is further reduced to the metal, and sulfur dioxide:[8][صفحة مطلوبة]

Cu
2
S + O
2
→ 2 Cu + SO
2

Copper(I) oxide readily converts to copper(II) oxide when heated in the presence of oxygen, and to copper metal upon heating in a reducing environment. (cf. Carbothermic reduction)

البنية

Crystals of chalcocite (mineral form of Cu2S).

اتحادية العناصر

Two forms (a dimorphism) of Cu
2
S
are known. The so-called low temperature monoclinic form ("low-chalcocite") has a complex structure with 96 copper atoms in the unit cell.[9] The hexagonal form, stable above 104 °C (219 °F),[10][صفحة مطلوبة] 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.

عدم اتحادية العناصر

As illustrated by the mineral djurleite, a cuprous sulfide is also known.[مطلوب توضيح] With the approximate formula Cu
1.96
S
, this material is non-stoichiometric (range Cu
1.934
S
-Cu
1.965
S
and has a monoclinic structure with 248 copper and 128 sulfur atoms in the unit cell.[9] Cu
2
S
and Cu
1.96
S
are similar in appearance and hard to distinguish one from another.[11]

الانتقال بين الأطوار

The electrical resistivity increases abruptly at the phase transition point around 104 °C (219 °F), with the precise temperature depending on the stoichiometry.[12][13]

انظر أيضاً

المراجع

  1. ^ Patnaik, Pradyot (2003). Handbook of inorganic chemicals. New York: McGraw-Hill. ISBN 0-07-049439-8.
  2. ^ "Copper (I) sulfite, SDS". Sigma-Aldrich. Retrieved 18 July 2025.
  3. ^ Sigma-Aldrich Co., Copper(I) sulfide. Retrieved on 18-07-2025.
  4. ^ "NIOSH Pocket Guide to Chemical Hazards".
  5. ^ Potter, R. W. (1977). "An electrochemical investigation of the system copper-sulfur". Economic Geology. 72 (8): 1524–1542. Bibcode:1977EcGeo..72.1524P. doi:10.2113/gsecongeo.72.8.1524.
  6. ^ خطأ استشهاد: وسم <ref> غير صحيح؛ لا نص تم توفيره للمراجع المسماة Greenwood
  7. ^ Blachnik R., Müller A. (2000). "The formation of Cu2S from the elements I. Copper used in form of powders". Thermochimica Acta. 361: 31. doi:10.1016/S0040-6031(00)00545-1.
  8. ^ أ ب Wiberg, Egon; Wiberg, Nils; Holleman, A. F. (2001). Inorganic chemistry (1st English ed.). San Diego : Berlin ; New York: Academic Press ; De Gruyter. ISBN 0-12-352651-5.
  9. ^ أ ب Evans, H. T. (1979). "Djurleite (Cu1.94S) and Low Chalcocite (Cu2S): New Crystal Structure Studies". Science. 203 (4378): 356–8. Bibcode:1979Sci...203..356E. doi:10.1126/science.203.4378.356. PMID 17772445. S2CID 6132717.
  10. ^ Wells, A. F. (1984). Structural inorganic chemistry (5th ed.). Oxford [Oxfordshire] : New York: Clarendon Press ; Oxford University Press. ISBN 0-19-855370-6.
  11. ^ Evans H.T. (1981). "Copper coordination in low chalcocite and djurleite and other copper-rich sulfides" (PDF). American Mineralogist. 66 (7–8): 807–818.
  12. ^ Garisto, Dan (2023-08-16). "LK-99 isn't a superconductor — how science sleuths solved the mystery". Nature (in الإنجليزية). 620 (7975): 705–706. Bibcode:2023Natur.620..705G. doi:10.1038/d41586-023-02585-7. PMID 37587284. S2CID 260955242.
  13. ^ Jain, Prashant K. "Phase transition of copper (I) sulfide and its implication for purported superconductivity of LK-99." arXiv preprint arXiv:2308.05222 (2023).