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Copper @ Periodic Table of Chemical Elements

12345678 910111213141516 1718
IIIIIIbIVb VbVIbVIIbVIIIbIb IIbIIIIVVVI VIIVIII
1H
1.0079
2He
4.0026
3Li
6.9412
4Be
9.0121
5B
10.811
6C
12.010
7N
14.006
8O
15.999
9F
18.998
10Ne
20.179
11Na
22.989
12Mg
24.305
13Al
26.981
14Si
28.085
15P
30.973
16S
32.065
17Cl
35.453
18Ar
39.948
19K
39.098
20Ca
40.078
21Sc
44.955
22Ti
47.867
23V
50.941
24Cr
51.996
25Mn
54.938
26Fe
55.845
27Co
58.933
28Ni
58.693
29Cu
63.546
30Zn
65.409
31Ga
69.723
32Ge
72.641
33As
74.921
34Se
78.963
35Br
79.904
36Kr
83.798
37Rb
85.467
38Sr
87.621
39Y
88.905
40Zr
91.224
41Nb
92.906
42Mo
95.942
43Tc
98.906
44Ru
101.07
45Rh
102.90
46Pd
106.42
47Ag
107.86
48Cd
112.41
49In
114.81
50Sn
118.71
51Sb
121.76
52Te
127.60
53I
126.90
54Xe
131.29
55Cs
132.90
56Ba
137.32
57La
138.90
72Hf
178.49
73Ta
180.94
74W
183.84
75Re
186.20
76Os
190.23
77Ir
192.21
78Pt
195.08
79Au
196.96
80Hg
200.59
81Tl
204.38
82Pb
207.21
83Bi
208.98
84Po
208.98
85At
209.98
86Rn
222.01
87Fr
223.01
88Ra
226.02
89Ac
227.02
104Rf
261.10
105Db
262.11
106Sg
266.12
107Bh
264.12
108Hs
269
109Mt
278
110Ds
281
111Rg
282
112Cn
285
113Nh
286
114Fl
289
115Mc
290
116Lv
293
117Ts
294
118Og
294
Lanthanoids58Ce
140.11
59Pr
140.90
60Nd
144.24
61Pm
146.91
62Sm
150.36
63Eu
151.96
64Gd
157.25
65Tb
158.92
66Dy
162.50
67Ho
164.93
68Er
167.25
69Tm
168.93
70Yb
173.04
71Lu
174.96
Actinoids90Th
232.03
91Pa
231.03
92U
238.02
93Np
237.04
94Pu
244.06
95Am
243.06
96Cm
247.07
97Bk
247.07
98Cf
251.07
99Es
252.08
100Fm
257.09
101Md
258.09
102No
259.10
103Lr
260.10
Alkali metals Alkali earth metals Transition metals Other metals Metaloids Non-metals Halogens Noble gases
Element

29

Cu

Copper

63.5463

2
8
18
1
Copper photo
Basic properties
Atomic number29
Atomic weight63.5463 amu
Element familyTransition metals
Period4
Group1
Blocks-block
Discovery year9000 BC
Isotope distribution
63Cu
69.17%
65Cu
30.83%
63Cu: 69.17%65Cu: 30.83%
63Cu (69.17%)
65Cu (30.83%)
Physical properties
Density 8.933 g/cm3 (STP)
Atomic hydrogen (H) 8.988E-5
Meitnerium (Mt) 28
Melting1084.6 °C
Helium (He) -272.2
Carbon (C) 3675
Boiling2595 °C
Helium (He) -268.9
Tungsten (W) 5927
Chemical properties
Oxidation states
(less common)
+2
(-2, -1, 0, +1, +3, +4)
First ionization potential 7.726 eV
Cesium (Cs) 3.894
Helium (He) 24.587
Electron affinity 1.236 eV
Nobelium (No) -2.33
Atomic chlorine (Cl) 3.612725
Electronegativity1.9
Cesium (Cs) 0.79
Atomic fluorine (F) 3.98
Atomic radius
Covalent radius 1.12 Å
Atomic hydrogen (H) 0.32
Francium (Fr) 2.6
Van der Waals radius 1.4 Å
Atomic hydrogen (H) 1.2
Francium (Fr) 3.48
Metallic radius 1.28 Å
Beryllium (Be) 1.12
Cesium (Cs) 2.65
29CuWebQC.OrgCovalentMetallicVan der Waals
Compounds
FormulaNameOxidation state
Cu2OCopper(i) oxide+1
CuClCopper(i) chloride+1
Cu2SCopper(i) sulfide+1
CuICopper(i) iodide+1
CuCNCopper(I) cyanide+1
CuBrCopper(i) bromide+1
CuSO4Copper(II) sulfate+2
CuCl2Copper(II) chloride+2
Cu(NO3)2Copper(II) nitrate+2
CuOCopper(II) oxide+2
Cu(OH)2Copper(II) hydroxide+2
Cs2CuF6Caesium hexafluorocuprate(IV)+4
Electronic properties
Electrons per shell2, 8, 18, 1
Electronic configuration[Ar] 3d104s1
Bohr atom model
Bohr atom model
Orbital box diagram
Orbital box diagram
Valence electrons11
Lewis dot structure Copper Lewis dot structure
Orbital Visualization
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Electrons-

Copper (Cu): Periodic Table Element

Scientific Review Article | Chemistry Reference Series

Abstract

Copper exhibits exceptional electrical and thermal conductivity properties that establish its significance as an industrial metal and chemical element. The element demonstrates characteristic d10 electronic configuration, resulting in distinct physical and chemical behaviors including diamagnetic properties and variable oxidation states. Copper manifests in crystalline face-centered cubic structure with atomic number 29 and atomic weight 63.546 u. The metal exhibits two primary oxidation states, +1 and +2, with cupric compounds displaying characteristic blue-green coloration. Natural occurrence includes native metallic copper and various sulfide, oxide, and carbonate mineral forms. Industrial applications exploit copper's conductivity, corrosion resistance, and alloy-forming capabilities across electrical, construction, and manufacturing sectors. Archaeological evidence indicates continuous human utilization for over 10,000 years, representing one of humanity's earliest metallurgical achievements.

Introduction

Copper occupies position 29 in the periodic table as the first element of the fourth period d-block transition metals. The element belongs to group 11 alongside silver and gold, characterized by completely filled d-orbitals and single s-orbital valence electrons. This electronic arrangement produces unique physical properties including exceptional electrical conductivity, thermal conductivity, and malleable mechanical characteristics. Copper represents the prototype coinage metal, demonstrating resistance to atmospheric corrosion while maintaining workability essential for technological applications.

Discovery of native copper deposits enabled early metallurgical development, with archaeological evidence documenting systematic copper utilization beginning approximately 8000 BC. The element's natural occurrence in unalloyed metallic form facilitated immediate technological adoption without requiring sophisticated extraction techniques. Subsequent development of copper smelting from sulfide ores around 5000 BC established copper as the foundation for Bronze Age metallurgy and technological advancement.

Physical Properties and Atomic Structure

Fundamental Atomic Parameters

Copper possesses atomic number 29 with electron configuration [Ar] 3d10 4s1, demonstrating complete d-orbital filling characteristic of group 11 elements. The atomic structure exhibits effective nuclear charge of approximately 6.1 for the 4s electron, resulting from nuclear charge shielding by inner electron shells. Atomic radius measures 128 pm in metallic coordination, while ionic radii vary with oxidation state: Cu+ exhibits 77 pm radius and Cu2+ demonstrates 73 pm radius in octahedral coordination.

Comparative analysis with neighboring elements reveals systematic trends in atomic properties. The d10 configuration produces diamagnetic behavior with magnetic susceptibility of -9.63×10-6 cm³/mol. Electronic structure governs chemical reactivity through availability of d-orbitals for coordination bonding and variable oxidation state stabilization.

Macroscopic Physical Characteristics

Copper exhibits distinctive reddish-orange metallic appearance in freshly exposed surfaces, attributed to characteristic optical absorption properties. The metal crystallizes in face-centered cubic structure with space group Fm3̄m and lattice parameter a = 361.49 pm. Crystal coordination demonstrates twelve nearest neighbors at equal distances, producing close-packed metallic bonding arrangement.

Thermodynamic phase behavior includes melting point 1084.62°C (1357.77 K) and boiling point 2562°C (2835 K). Heat of fusion measures 13.26 kJ/mol while heat of vaporization reaches 300.4 kJ/mol. Specific heat capacity equals 24.440 J/(mol·K) at standard conditions. Density at room temperature equals 8.96 g/cm³, placing copper among moderately dense transition metals. Thermal expansion coefficient measures 16.5 μm/(m·K) at 25°C, indicating moderate dimensional stability under temperature variation.

Chemical Properties and Reactivity

Electronic Structure and Bonding Behavior

Chemical reactivity derives from d10 electronic configuration enabling facile electron loss from 4s and 3d orbitals. Common oxidation states include +1 (cuprous) and +2 (cupric), with +3 and +4 states accessible under specific conditions. The Cu+ state demonstrates d10 configuration exhibiting stability in coordination complexes and solid compounds. Cupric Cu2+ state possesses d9 configuration producing characteristic Jahn-Teller distortion in octahedral coordination environments.

Coordination chemistry encompasses diverse ligand interactions with coordination numbers ranging from 2 to 6. Linear coordination characterizes Cu+ complexes, while Cu2+ typically adopts square planar or octahedral geometries with distortion. Bond formation involves d-orbital participation through crystal field stabilization and covalent character contribution. Copper-ligand bond lengths vary systematically with coordination environment: Cu-O bonds measure approximately 1.9-2.1 Å while Cu-N bonds range from 2.0-2.3 Å depending on ligand field strength.

Electrochemical and Thermodynamic Properties

Electronegativity measures 1.90 on the Pauling scale, positioning copper between transition metal extremes and indicating moderate electron-attracting capability. Successive ionization energies demonstrate increasing energy requirements: first ionization energy equals 745.5 kJ/mol, second ionization energy reaches 1957.9 kJ/mol, and third ionization energy requires 3555 kJ/mol. These values reflect electronic structure changes accompanying progressive electron removal.

Standard reduction potentials establish thermodynamic stability relationships for copper species. The Cu2+/Cu couple exhibits potential +0.337 V, while Cu+/Cu demonstrates +0.521 V versus standard hydrogen electrode. The Cu2+/Cu+ couple shows +0.153 V, indicating thermodynamic instability of Cu+ in aqueous solution through disproportionation: 2Cu+ → Cu2+ + Cu. Redox behavior varies significantly in different chemical environments, with complexation and pH effects modifying thermodynamic relationships.

Chemical Compounds and Complex Formation

Binary and Ternary Compounds

Copper forms extensive series of binary compounds across multiple anion types. Oxide formation produces Cu₂O (cuprous oxide) and CuO (cupric oxide) as principal species. Cuprous oxide adopts cubic crystal structure with Cu+ in linear coordination, while cupric oxide crystallizes in monoclinic structure with square planar copper coordination. Halide compounds include CuCl, CuBr, CuI for Cu+ state and CuCl₂, CuBr₂ for Cu2+ state.

Sulfide compounds demonstrate significant mineral importance with chalcocite Cu₂S and covellite CuS representing primary copper ore minerals. Formation mechanisms involve hydrothermal processes with temperature-dependent stability fields. Ternary compounds encompass sulfosalt minerals including chalcopyrite CuFeS₂ and bornite Cu₅FeS₄, demonstrating complex structural arrangements and mixed oxidation states.

Coordination Chemistry and Organometallic Compounds

Coordination complexes exhibit diverse geometric arrangements determined by d-electron count and ligand field effects. Cu+ complexes favor linear and tetrahedral coordination with d10 configuration providing kinetic lability. Cu2+ complexes adopt square planar, square pyramidal, or distorted octahedral geometries reflecting Jahn-Teller stabilization. Common ligands include ammonia, ethylenediamine, phenanthroline, and acetylacetonate with characteristic absorption spectra and magnetic properties.

Organometallic chemistry involves copper-carbon bond formation in various oxidation states. Cuprate reagents demonstrate synthetic utility in organic synthesis through conjugate addition and cross-coupling reactions. Copper-catalyzed reactions include alkyne coupling, amination, and etherification processes exploiting redox cycling between Cu+ and Cu3+ states. Bond characteristics include polarized Cu-C bonds with significant ionic character and moderate thermal stability.

Natural Occurrence and Isotopic Analysis

Geochemical Distribution and Abundance

Crustal abundance measures approximately 50 parts per million by weight, establishing copper as moderately abundant among transition metals. Geochemical behavior involves concentration through hydrothermal processes, producing economic deposits in porphyry, skarn, and volcanogenic massive sulfide environments. Copper exhibits chalcophile character, concentrating in sulfide phases during magmatic differentiation processes.

Distribution patterns reflect geological processes including metamorphic grade, weathering intensity, and secondary mineral formation. Supergene enrichment processes concentrate copper through oxidation and leaching mechanisms, producing secondary copper minerals including azurite Cu₃(CO₃)₂(OH)₂ and malachite Cu₂CO₃(OH)₂ in oxidized zones. Marine environments demonstrate low copper concentrations averaging 0.5 μg/L in seawater, while freshwater systems contain approximately 2 μg/L copper concentration.

Nuclear Properties and Isotopic Composition

Natural isotopic composition comprises two stable isotopes: 63Cu (69.15% abundance) and 65Cu (30.85% abundance). Both isotopes possess nuclear spin 3/2 with magnetic moments +2.2273 μN and +2.3817 μN respectively. Nuclear stability derives from favorable neutron-to-proton ratios within the valley of beta stability.

Radioisotopic species include 64Cu with 12.7-hour half-life exhibiting both β+ and β- decay modes. 67Cu demonstrates 2.58-day half-life through β- decay exclusively. These isotopes find applications in medical imaging and radiopharmaceutical research. Nuclear cross-sections for thermal neutron interactions measure 3.78 barns for 63Cu and 2.17 barns for 65Cu, enabling isotopic analysis through neutron activation techniques.

Industrial Production and Technological Applications

Extraction and Purification Methodologies

Industrial extraction predominantly utilizes sulfide ore processing through concentration and pyrometallurgical treatment. Froth flotation concentrates copper sulfides from gangue minerals, achieving typical concentrates containing 20-30% copper content. Flash smelting processes operate at temperatures exceeding 1200°C, converting concentrated sulfides to copper matte through controlled oxidation reactions.

Pyrometallurgical refining involves converting operations transforming copper matte to blister copper containing 98-99% purity. Electrorefining achieves final purification producing cathode copper with 99.99% purity through electrochemical deposition. Production statistics indicate annual global output approaching 23 million metric tons, with Chile, Peru, and China representing primary producing regions. Environmental considerations include sulfur dioxide emission control and acid mine drainage mitigation in extraction operations.

Technological Applications and Future Prospects

Electrical applications exploit copper's conductivity measuring 5.96×107 S/m, second only to silver among pure metals. Wire and cable manufacturing consumes approximately 60% of copper production, supporting power transmission and electronic device connectivity. Thermal conductivity of 401 W/(m·K) enables heat exchanger and cooling system applications in automotive, industrial, and residential sectors.

Alloy formation produces bronze, brass, and specialized compositions for marine, architectural, and precision instrument applications. Antimicrobial properties support healthcare and food processing uses through bacteriostatic mechanisms. Emerging technologies include renewable energy infrastructure, electric vehicle components, and advanced electronic systems requiring high-performance conductive materials. Economic significance reflects commodity market dynamics with pricing sensitivity to global supply-demand fluctuations and technological demand growth.

Historical Development and Discovery

Archaeological evidence documents copper utilization beginning approximately 8000 BC in Anatolia and the Middle East, representing humanity's earliest systematic metallurgy. Native copper deposits provided directly usable metal without requiring chemical reduction processes, enabling immediate technological adoption. The Chalcolithic period (Copper Age) demonstrates transitional phase between stone and bronze technologies, with copper tools and ornaments appearing throughout Mediterranean and Near Eastern civilizations.

Smelting technology development around 5000 BC enabled processing of copper sulfide ores, dramatically expanding available copper sources beyond native deposits. Casting techniques evolved around 4000 BC, allowing complex shape fabrication through molten metal manipulation. Bronze production beginning approximately 3500 BC represented first intentional alloy creation, combining copper with tin to produce superior mechanical properties. These metallurgical advances established copper as fundamental to technological progress through ancient, medieval, and modern periods.

Scientific understanding progressed through systematic investigation of copper chemistry during 18th and 19th centuries. Identification of cupric and cuprous oxidation states, crystal structure determination, and electronic theory development provided theoretical foundation for modern copper science. Contemporary research focuses on nanostructured copper materials, catalytic applications, and sustainable extraction technologies addressing environmental and resource sustainability challenges.

Conclusion

Copper maintains unique position among transition metals through combination of filled d-orbital electronic structure, exceptional transport properties, and diverse chemical reactivity. The element's significance extends across modern technological applications including renewable energy systems, electronic communications, and materials science innovations. Fundamental research continues investigating quantum effects in copper nanostructures, catalytic mechanisms in organic synthesis, and advanced alloy development. Future technological advancement will likely exploit copper's established properties while developing novel applications in emerging fields including quantum computing, energy storage, and sustainable materials engineering.

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