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Tenorite
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| Tenorite | |
|---|---|
 | |
| General | |
| Category | Oxide mineral |
| Formula | CuO |
| IMA symbol | Tnr[1] |
| Strunz classification | 4.AB.10 |
| Crystal system | Monoclinic |
| Crystal class | Prismatic (2/m) (same H-M symbol) |
| Space group | C2/c |
| Unit cell | a = 4.6837(5) Å b = 3.4226(5) Å c = 5.1288(6) Å; β = 99.47°; Z = 4 |
| Identification | |
| Color | Steel-gray, iron-gray, black |
| Crystal habit | Lathlike crystals, curved, scaly, dendritic; commonly pulverulent, earthy, massive |
| Twinning | Common on {011}, forming stellate groups; lamellar |
| Cleavage | Poor to indistinct |
| Fracture | Conchoidal to uneven |
| Tenacity | Brittle; flexible and elastic in thin scales |
| Mohs scale hardness | 3.5–4 |
| Luster | Metallic to earthy |
| Streak | Black |
| Diaphaneity | Opaque, thin flakes transparent |
| Specific gravity | 6.5 |
| Optical properties | Biaxial (+) |
| Pleochroism | Distinct; light to dark brown |
| References | [2][3][4] |
Tenorite, sometimes also called Black Copper, is a copper oxide mineral with the chemical formula CuO. The chemical name is Copper(II) oxide or cupric oxide.
Occurrence
[edit]_mit_Azurit_-_Nischne_Tagilsk,_Ural.jpg)
Tenorite occurs in the weathered or oxidized zone associated with deeper primary copper sulfide orebodies. Tenorite commonly occurs with chrysocolla and the copper carbonates, azurite and malachite. The dull grey-black color of tenorite contrasts sharply with the often intergrown blue chrysocolla. Cuprite, native copper and Fe–Mn oxides also occur in this environment.[2]
In addition to the hydrothermal, tenorite also occurs as a volcanic sublimate from Vesuvius, Campania, and Etna, Sicily, Italy. As a sublimate it occurs with copper chlorides, alkali chlorides and cotunnite.[2] The Vesuvian sublimate occurrence was originally named melaconise or melaconite by F. S. Beudant in 1832.[5]
Tenorite was named in 1841 after the Italian botanist Michele Tenore (1780–1861).[4]
See also
[edit]References
[edit]- ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- ^ a b c Handbook of Mineralogy
- ^ Webmineral data
- ^ a b Mindat
- ^ Chisholm, Hugh, ed. (1911). Encyclopædia Britannica (11th ed.). Cambridge University Press
Tenorite
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Nomenclature and History
Etymology
The mineral tenorite was named in 1841 by Italian mineralogist Giovanni Semmola in honor of Michele Tenore (1780–1861), a prominent Italian botanist and professor at the University of Naples who advanced studies in natural history.[6] Prior to this designation, the mineral was known as melaconite, a term introduced in 1832 by French mineralogist François Sulpice Beudant, derived from the Greek words melas (black) and konos (powder), alluding to its characteristic black, powdery appearance.[8][9] In modern mineral classification, tenorite has been assigned the International Mineralogical Association (IMA) symbol "Tnr," reflecting its standardized nomenclature since the IMA's unanimous adoption of the name in 1962 over the older synonym.[1][10]Discovery and Historical Context
Tenorite was initially recognized in 1832 by French mineralogist François Sulpice Beudant, who described a black, powdery copper oxide sublimate from volcanic fumaroles as melaconite, a term reflecting its dusty, dark appearance in such environments.[11] This early identification occurred in the context of Beudant's systematic mineral classification, where he noted its occurrence as a secondary product in volcanic settings.[11] Early samples of the mineral, then known under the melaconite name, were primarily sourced from Italian volcanoes, including Mount Vesuvius near Naples, where it formed as a sublimate in copper-rich fumarolic deposits.[1] These specimens linked tenorite to broader 19th-century investigations of volcanic copper minerals and sublimation processes, highlighting its role in understanding ore alteration in active volcanic systems.[12] In 1841, Italian mineralogist Giovanni Semmola provided the first formal description of the crystallized form from Vesuvius, naming it tenorite to honor botanist Michele Tenore and distinguishing it as a specific copper(II) oxide species.[1] Semmola's work, published in Opere minori, marked a key advancement in its characterization beyond the earlier descriptive label. Throughout the 19th century, tenorite evolved from a loosely defined volcanic sublimate or variety of black copper oxide to a formally accepted mineral in European classification systems, integrating it into the growing body of knowledge on oxide minerals.[12] This period saw increasing documentation of its occurrences beyond Italy, cementing its place in mineralogical literature.[1]Crystal Structure
Unit Cell Parameters
Tenorite crystallizes in the monoclinic system with space group C2/c (No. 15) and belongs to the prismatic crystal class 2/m.[13][14] The unit cell dimensions are a = 4.6837(5) Å, b = 3.4226(5) Å, c = 5.1288(6) Å, and β = 99.54°, yielding a cell volume of approximately 81.0 ų with Z = 4 formula units per cell.[14][13] This structure represents a distorted rock-salt type, where copper atoms adopt square-planar coordination to four oxygen atoms at an average distance of 1.96 Å, forming chains along the and [-110] directions.[13][14] X-ray diffraction studies confirm these parameters, with the strongest reflection corresponding to a d-spacing of 2.53 Å for the (-111) plane.[15][16]Crystal Habit and Morphology
Tenorite most commonly occurs in massive form, consisting of uniformly indistinguishable crystals that form large, compact aggregates, often appearing as earthy or powdery masses.[12] This habit predominates in natural specimens, giving the mineral a dull to earthy texture, though it can also develop as scaly coatings resembling fish scales or thin, shining, flexible plates.[12] Well-formed crystals are rare for tenorite, but when present, they exhibit prismatic or lath-like habits, with elongated forms up to several millimeters, often striated parallel to the direction on {100} faces.[1] These crystals may appear as paper-thin aggregates or curved plates, particularly in volcanic sublimates like those from Vesuvius, where they elongate along and parallel to {100}.[1] Microscopically, tenorite can form thin plates or needle-like crystals within vugs, contributing to dendritic or feather-like patterns in aggregates. Twinning is common in tenorite, primarily on the {011} contact plane, producing dovetail reentrants, stellate groups, and lamellar structures that enhance its dendritic morphology.[1] Possible twinning on {100} has also been observed, though less frequently.[1] The mineral displays poor to indistinct cleavage in zones along and [01̄1], with flexible and elastic behavior in thin scales.[1] Its fracture is typically irregular to uneven, often conchoidal, reflecting the mineral's brittle nature in larger masses.[1] In its monoclinic crystal system, tenorite's habits are influenced by growth conditions in oxidized copper deposits, where massive and earthy forms dominate due to rapid crystallization, while rarer prismatic crystals develop in cavities or sublimate environments.[1]Physical and Optical Properties
Mechanical and Density Properties
Tenorite exhibits a Mohs hardness of 3.5 to 4, which means it can be scratched by a copper coin but resists scratching from a steel knife.[17][12] This moderate hardness reflects its position among softer oxide minerals, making it susceptible to abrasion in handling or geological processing.[1] The mineral's specific gravity ranges from 6.45 to 6.50, indicating a high density that renders tenorite specimens notably heavy relative to their volume compared to common rocks. This property arises from its copper oxide composition and compact crystal structure, contributing to its accumulation in oxidized copper deposits where gravitational settling may influence distribution.[12] Tenorite is brittle in bulk form, though thin scales display flexibility and elasticity, leading to a conchoidal to uneven fracture when broken.[17] These mechanical behaviors make it prone to fragmentation under stress, often resulting in earthy or pulverulent masses in natural occurrences rather than intact crystals.[1] In terms of diaphaneity, tenorite is opaque, with transparency limited to the thinnest scales under transmitted light.[17] This opacity stems from its metallic luster and dark coloration, obscuring internal structure in typical hand samples.[12]Appearance and Optical Features
Tenorite typically exhibits a steel-gray to iron-black color in massive form, appearing brownish in transmitted light when examined in thin sections.[17] This coloration arises from its copper oxide composition, contributing to its distinctive visual identity in mineral assemblages.[1] The mineral's luster ranges from metallic on fresh crystal surfaces to dull earthy in massive or altered specimens, with iridescence often observed as a golden tint in reflected light on unaltered faces.[17] Its streak is black and non-powdery, providing a reliable diagnostic trait during identification.[1] In reflected light, tenorite appears light gray with a golden tint and exhibits weak pleochroism from light to dark brown, along with strong bireflectance and anisotropism (blue to gray).[1] Reflectivity ranges from 19.3% to 30.8% (400–700 nm).[1] These optical features make tenorite distinctive under reflected light microscopy.Chemical Composition
Molecular Formula and Structure
Tenorite has the chemical formula CuO, corresponding to copper(II) oxide in which the copper cation exhibits the +2 oxidation state (Cu²⁺).[12][19] The ideal stoichiometric composition of tenorite is 79.89% copper and 20.11% oxygen by weight, calculated from the molecular weight of 79.55 g/mol.[12] Natural occurrences of the mineral are typically nearly pure CuO, though minor impurities of elements such as iron or manganese may be present in specimens due to inclusions or substitutions from associated phases.[17] The bonding in tenorite combines ionic and covalent characteristics, with the ionic component dominated by the electrostatic attraction between Cu²⁺ and O²⁻ ions, while covalent contributions arise from d-p orbital overlap between copper and oxygen.[20][21] Structurally, each copper atom is coordinated by six oxygen atoms in a distorted octahedral arrangement, featuring four shorter equatorial Cu-O bonds (approximately 1.95 Å) and two longer axial bonds (approximately 2.75 Å) due to Jahn-Teller distortion typical of d⁹ Cu²⁺ centers.[22] This coordination motif links into a three-dimensional framework, consistent with the monoclinic crystal system described elsewhere.[21]Stability and Reactivity
Tenorite, with the chemical formula CuO, exhibits high thermal stability under standard conditions but undergoes decomposition at elevated temperatures. Above approximately 800°C, particularly in the range of 850–1000°C, it decomposes into cuprous oxide (Cu₂O) and oxygen gas (½O₂) via the reversible reaction 2CuO → Cu₂O + ½O₂, a process that has been characterized through kinetic studies and is utilized in thermogravimetric analysis (TGA) to assess its phase transformation and mass loss behavior.[23] This decomposition is endothermic and oxygen-dependent, with the equilibrium shifting toward CuO in oxygen-rich atmospheres, making it relevant for applications in high-temperature thermochemical storage.[24] In terms of solubility, tenorite is insoluble in water at ambient conditions, reflecting its low solubility product and stability as an oxide mineral. However, it readily dissolves in acids such as hydrochloric acid (HCl), reacting to form copper(II) chloride (CuCl₂) and water according to the equation CuO + 2HCl → CuCl₂ + H₂O, which proceeds via protonation of the oxide surface.[19] This reactivity underscores its behavior in acidic environments, where it acts as a base to liberate Cu²⁺ ions. Tenorite often forms through the further oxidation of cuprite (Cu₂O) in oxidizing conditions, such as those encountered in the weathering zones of copper deposits, where descending meteoric waters facilitate the transformation Cu₂O + ½O₂ → 2CuO.[25] Synthetically, tenorite can be produced via precipitation from Cu²⁺ solutions, typically by adding a base like sodium hydroxide to form copper(II) hydroxide (Cu(OH)₂) as an intermediate, followed by calcination at 300–500°C to yield CuO. Alternatively, it is synthesized through thermal decomposition of copper salts, such as basic copper sulfates or nitrates, at temperatures around 750°C, enabling control over particle size and morphology for industrial applications.[26][27]Geological Occurrence
Formation Environments
Tenorite primarily forms in the supergene oxidation zones of copper sulfide deposits, where it develops as a secondary mineral through the weathering and oxidation of primary sulfides under near-surface conditions. In these environments, descending groundwater introduces oxygen, facilitating the breakdown of sulfides and the precipitation of copper oxides in the upper leached and enriched zones of ore bodies. This process is particularly prominent in porphyry copper systems with low pyrite content and reactive host rocks, such as those containing silicates or mafic minerals, which maintain neutral to alkaline pH and limit copper mobility to tens of meters.[28] Additionally, tenorite occurs as a sublimate or reaction product in volcanic settings, particularly on lava flows associated with fumaroles at active volcanoes. It crystallizes in high-temperature fumaroles, typically above 400 °C, through the vapor-phase transport of volatile copper chlorides reacting with water vapor, such as CuCl₂ + H₂O → CuO + 2HCl, in oxidizing conditions. Examples include fumarolic deposits at Vesuvius, where it forms early in the paragenesis alongside other copper oxides. Similar occurrences are noted at Etna, highlighting its role in sublimate assemblages from volcanic gases.[29] Tenorite also occurs in the oxidized zones of hydrothermal copper deposits, often within veins, where supergene alteration by oxygenated groundwater at near-surface temperatures (below 200 °C) converts primary sulfides and other copper-bearing phases. Its paragenesis typically involves the oxidation of primary sulfides like chalcopyrite, leading to tenorite as a stable end-product in supergene contexts overlying hydrothermal systems.[17][28]Associated Minerals and Localities
Tenorite commonly occurs in association with other secondary copper minerals in oxidized zones of copper deposits, including chrysocolla, malachite, azurite, cuprite, and native copper, as well as iron oxides such as goethite and hematite.[17] These associations reflect tenorite's formation as a product of copper oxidation, often appearing as black coatings or masses contrasting with the vibrant colors of its companions.[1] The type locality for tenorite is Mount Vesuvius, Campania, Italy, where it forms as a volcanic sublimate in fumaroles.[1] Here, it is found alongside copper chlorides and other sublimate minerals in the high-temperature volcanic environment.[17] Notable occurrences include the Keweenaw Peninsula in Michigan, USA, where tenorite coats native copper specimens from historic mines like the Phoenix and Ojibway.[5] In Arizona, USA, it appears in oxidized copper ores at the Morenci Mine, Greenlee County, often with malachite and azurite.[30] At the Angélica Mine near Tocopilla, Antofagasta Province, Chile, tenorite is part of advanced oxidation assemblages in arid coastal deposits.[31] In France, it occurs at the Chessy copper mines, Rhône, associated with azurite and malachite pseudomorphs after cuprite.[32] Tenorite has been reported from over 1,600 localities worldwide, predominantly in arid copper belts of the southwestern United States, northern Chile, and Australia, where supergene enrichment processes favor its development.[1]Applications and Significance
Industrial and Economic Uses
Tenorite, the mineral form of cupric oxide (CuO), functions as a minor copper ore in the oxidized zones of porphyry and other secondary copper deposits, where it is smelted alongside more abundant minerals to recover metallic copper. However, its low concentration and limited occurrence make it rarely viable as a standalone economic resource, contributing only marginally to global copper supply.[33][34] Although CuO, of which tenorite is the mineral form, is used in ceramics as a colorant in glazes and enamels to produce shades of blue, green, red, and occasionally black, industrial CuO is typically synthetic rather than derived from the rare mineral tenorite.[35][36] Similarly, CuO provides stable black tones in pigments for industrial applications, including paints and coatings.[37] CuO also finds application in battery production, particularly as an additive in nickel-cadmium (Ni-Cd) electrodes to enhance performance and prevent swelling during charge-discharge cycles, but again, from synthetic sources.[38][39] Historically, CuO has been used in glass coloring to create black glazes, a practice dating back to traditional ceramic and glassmaking techniques.[40] Synthetic CuO also serves as a catalyst in organic synthesis reactions, such as dehydrogenation.[19] Recent studies have explored sulfidization-free flotation methods using collectors like potassium amyl xanthate for tenorite recovery, potentially improving efficiency in processing oxidized copper ores.[41] Extraction of tenorite typically occurs as a byproduct during the mining of richer copper sulfides such as chalcopyrite, with its global production remaining negligible relative to primary sulfide ores that dominate the copper industry.[34][33]Collectibility and Research Value
Tenorite is popular among mineral collectors for its distinctive massive or earthy black forms, often occurring as botryoidal aggregates or thin coatings on native copper or associated with vibrant green chrysocolla, particularly from classic localities in the Keweenaw Peninsula of Michigan, USA, such as the Phoenix Mine and Indiana Mine.[42][1] Specimens from Chilean copper districts, including Chuquicamata and Collahuasi, are also sought after for their association with large-scale porphyry deposits, though less commonly available than Michigan material.[1] The mineral's metallic luster and occasional iridescent tarnish on copper hosts enhance its aesthetic appeal, making well-preserved examples desirable for display collections.[43] Well-formed crystals of tenorite are rare, typically appearing as thin, flexible scales or laths rather than robust euhedral forms, which significantly boosts the value of exceptional pieces.[1] As of 2023, market prices for collector specimens typically range from $10 to $500, depending on size, quality, and provenance; for instance, small cabinet-sized pieces from Michigan mines with copper inclusions often sell in the $50–200 range, while rarer crystal groups or those with multiple associated minerals command higher prices.[44][43] Due to its role as a secondary mineral, tenorite serves significant educational value in illustrating oxidation and supergene processes in copper deposits, with fine examples housed in major institutions such as the Smithsonian National Museum of Natural History and the Natural History Museum in London.[45][46] In scientific research, tenorite (CuO) acts as a key model for studying oxide mineral weathering in copper ore systems, where it forms through the oxidation of primary sulfides like chalcopyrite, providing insights into supergene enrichment zones.[47] Its presence in weathered profiles helps trace copper mobility in environmental geochemistry, as tenorite's stability under near-surface conditions influences the dispersion and precipitation of Cu in soils and groundwater.[47] Additionally, synthetic tenorite is integral to studies of high-temperature superconductivity, serving as the structural basis for cuprate materials like YBa₂Cu₃O₇, where CuO layers enable electron pairing at elevated temperatures.[48] These applications underscore tenorite's value in advancing understanding of mineral alteration, geochemical cycling, and advanced materials science.[48]References
- https://www.[mindat.org](/page/Mindat.org)/min-3912.html
- https://rruff.geo.[arizona](/page/Arizona).edu/doclib/hom/tenorite.pdf