paramontroseite

The name paramontroseite is derived from the Greek παρα (para), meaning near, and {{ill|montroseite|uk|Монтрозеїт}}, a related mineral.{{sfn|Barthelmy|loc=General Paramontroseite Information}}

The name was chosen due to the mineral's paramorphic relationship to the host mineral montroseite.{{sfn|Evans|Mrose|1955|p=862}}

Montroseite is named after Montrose County, Colorado, USA, where it was first found.{{sfn|Barthelmy (b)}}{{efn|Montrose County takes its name from the county seat, Montrose, which is named after the historical novel by Sir Walter Scott, A Legend of Montrose.{{sfn|Heim|2007|p=165}}

Montrose, in Forfarshire, Scotland, is a corruption of the Gailic monadh-rois, meaning the hill of the ravine.{{sfn|Smythe Palmer|1882|p=545}} }}

Names in other languages include Paramontroseit (German), paramontroseita (Spanish), парамонтрозеит (Russian) and 副黑钒矿 副黑铁钒矿 (Chinese).{{sfn|Paramontroseite – Mindat|loc=Other Language Names}}

Synonyms are Inorganic Crystal Structure Database (ICSD) 22303 and Powder Diffraction File (PDF) 25-1003.{{sfn|Barthelmy|loc=General Paramontroseite Information}}

Paramontroseite is associated with montroseite and {{ill|corvusite|ca|Corvusita}}.

It is found in relatively unoxidized Colorado Plateau-type uranium–vanadium ores in sandstones.{{sfn|Paramontroseite – Handbook of Mineralogy|loc=Occurrence}}

The type locality is Bitter Creek Mine, Paradox Valley, Uravan District, Montrose County, Colorado, USA.{{sfn|Paramontroseite – Mindat|loc=Type Occurrence}}

In the USA it is found in Montrose County, Colorado, San Miguel County, Colorado, Mesa County, Colorado, Emery County, Utah, Apache County, Arizona, McKinley County, New Mexico and Fall River County, South Dakota.{{sfn|Paramontroseite – Handbook of Mineralogy|loc=Distribution}}

It has also been reported from locations in the Czech Republic, Mendoza Province, Argentina and the Mounana uranium mine near Franceville, Gabon.{{sfn|Paramontroseite – Handbook of Mineralogy|loc=Distribution}}

Paramontrosite has also been found in an outcrop on the Van Irvine Ranch in the Pumpkin Buttes area of Wyoming, USA, associated with sulfides in red sandstone.{{sfn|Sharp|McKay|McKeown|White|1949|p=605}}

It is found in a zone where the sandstone changes color from red to gray.

The black paramontroseite cements grains of sand into nodular masses that enclose smaller pyrite masses.{{sfn|Sharp|McKay|McKeown|White|1949|p=606}}

The irregular concretionary masses are up to {{convert|1|ft}} across.{{sfn|Sharp|McKay|McKeown|White|1949|p=575}}

Vanadium salts have given a greenish coating to the exposed surfaces of these masses.

The masses are anomalously radioactive and the surrounding sandstone is weakly radioactive.

The radioactivity is mostly caused by tiny specks of coffinite in the paramontroseite.{{sfn|Sharp|McKay|McKeown|White|1949|p=606}}

When a section is polished the paramontroseite completely fills the gaps between the grains of sand.

It is very soft and has a gray color that is slightly lighter than quartz gray.

There is strong anisotrophism and many bright multi-colored internal reflections.{{sfn|Sharp|McKay|McKeown|White|1949|p=575}}

Deposits of montroseite (V,Fe)OOH and paramontroseite VO₂ have been found in the Saltwash Sandstone Member of the Upper Jurassic Morrison Formation in the Colorado Plateau.

From the diffraction characteristics of the paramontroseite there seem to be two distinct generations: a primary paramontroseite with good crystalline structure and a product of montroseite oxidation with poor crystalline structure.{{sfn|Wanty|Fitzpatrick|Goldhaber|1986|p=72}}

The paramontroseite found in this region is among the neutral minerals in the mid-range of vanadium valence (+4) above the primary ore of montroseite (+3) but below minerals such as carnotite (+5) and pascoite (+5).{{sfn|Wanty|Fitzpatrick|Goldhaber|1986|p=20}}

Paramontroseite is a metastable form of vanadium dioxide (VO₂) that results from oxidation of montroseite.{{sfn|Evans|Mrose|1955|p=861}}

It is formed by dehydrogenation of montroseite.{{sfn|Paramontroseite – Handbook of Mineralogy|loc=Occurrence}}

Paramontroseite seems to be the most common initial product of oxidation of montroseite.{{sfn|Garrels|Pommer|1987|pp=158−159}}

The primary difference between the crystal structures of the two minerals is that the oxygen–oxygen distance increases from 2.63Å in montroseite to 3.87Å in paramontroseite due to the loss of hydrogen in the latter.{{sfn|Evans|Mrose|1955|p=861}}

The vanadium–oxygen distances are also somewhat shorter in paramontroseite than in montroseite, as would be expected when the vanadium is oxidized from +3 to +4 when the hydrogen is removed.{{sfn|Evans|Mrose|1955|pp=870–872}}

The montroseite, VO(OH), is deposited in crystalline masses in a sandstone matrix by some unknown process.

Usually iron occurs in place of some of the vanadium.

Oxygen in the air or groundwater then oxidizes the crystallised montroseite at temperatures under 50 °C through the reaction:

:2VO(OH) + {{1/2}}O₂ → 2VO₂ + H₂O

During the solid state alteration process the hydrogen atoms migrate through the crystal structure to the surface, where they combine with oxygen.

In the process there is a slight shift in the crystal structure, but the structure remains intact.{{sfn|Evans|Mrose|1955|p=872}}

The vanadium-oxygen bonds have not been broken and the hexagonal close-packed oxygen framework has not been disrupted.{{sfn|Evans|1987|p=94}}

In some cases there may be an intermediate "diffuse A" phase.{{sfn|Evans|Mrose|1955|p=872}}

The process by which montroseite is altered to paramontroseite seems analogous to the magnetite → maghemite, lepidocrocite → maghemite, and goethite → hematite processes.{{sfn|Evans|Mrose|1955|p=874}}

Paramontroseite is not stable and is destroyed by weathering, replaced by minerals of the corvusite type.{{sfn|Evans|Mrose|1955|p=872}}

The paramontroseite reacts under neutral or acid conditions to form many compounds such as vanadyl vanadate and metal vanadates such as hewettite, hummerite, pascoite and rossite.{{sfn|Garrels|Pommer|1987|p=159}}

Paramontroseite may dissolve in slightly alkaline conditions, then combine with Ca⁺⁺ to form {{ill|simplotite|ca|Simplotita}}:{{sfn|Garrels|Pommer|1987|p=158}}

:4VO₂ + 2OH⁻ + Ca⁺⁺ → CaV₄O₉ + H₂O

Autophagy is a process of cellular degradation that is essential in preserving homeostasis of cells.

It is often thought that when autophagosomes encapsulate and trap inorganic nanoparticles they may be unable to degrade them and the cell's well-being may be threatened.

However, experiments have shown that nanocrystals of paramontroseite induce cyto-protective autophagy in cultured HeLa cells.

It is possible that this may have value in therapies.{{sfn|Zhou|Miao|Zhang |Liu |2013}}

Montroseite and paramontroseite microspheres have been synthesized by hydrothermal carbonization of sucrose and calcinated to form V₂O₃-VO₂-C core-shell microspheres.

These have been used experimentally as cathode materials for a lithium-ion battery.{{sfn|Hailong|Xiaokun|Mingdeng|Kemei|2011|p=2049}}

Y. Xu and colleagues of the University of Science and Technology of China have shown that synthetic montroseite VOOH hollow structures can convert topochemically to paramontroseite without altering the size and appearance of the structures.

Both forms appear to have potential in lithium-ion batteries as anode materials.{{sfn|Xu|2012|p=1815}}

Monoclinic vanadium dioxide VO₂(M) is potentially of great value for applications such as intelligent temperature sensors and smart windows.

The classic solid state transformation from vanadium precursors to rutile VO₂(R) is slow and costly.

A transformation from goethite VOOH to synthetic "paramontroseite" VO₂ to the desired monoclinic VO₂(M) promises to greatly reduce cost and time.{{sfn|Changzheng|Feng|Jun|Jun|2011 |page=791}}

Paramontroseite was first described before 1959.

It is a member of the Ramsdellite Group.{{sfn|Paramontroseite – Mindat|loc=Relationship ... to other Species}}

It is classified as follows:{{sfn|Paramontroseite – Mindat|loc=Classification}}

• Strunz 8th edition: 4/F.08-30.
• Nickel-Strunz 10th edition: 4.DB.15a
• Dana 8th edition: 4.4.11.1
• Hey's CIM Reference: 7.12.3

Physical properties of Paramontroseite include

:

The X-ray powder diffraction pattern for a Bitter Creek mine sample is 3.39 (100), 2.645 (50), 4.35 (35), 2.213 (35), 1.426 (35), 2.479 (25), 2.179 (25).

In this sample the chemistry was:{{sfn|Paramontroseite – Handbook of Mineralogy|loc=X-ray Powder Pattern}}

:

A sample from Matchless mine, Colorado, USA had chemistry:{{sfn|Paramontroseite – Handbook of Mineralogy|loc=Chemistry}}

:

The measured chemistry of a microprobe fragment in the gray phase by the RRUFF project gave metals in the ratio:

V⁴⁺ (82%), Fe³⁺ (9%), U⁶⁺ (4%) and Al (2%), with one metal atom per two oxygen atoms.

The lightest phase was uranophane.{{sfn|Armbruster|Danisi}}

Paramontroseite is opaque and black to grayish black in color.{{sfn|Paramontroseite – Handbook of Mineralogy|loc=Optical Properties}}{{efn|Some sources simply give the color as "black".{{sfn|Barthelmy|loc=Physical Properties}}{{sfn|Paramontroseite – Mindat}} }}

Its optical class is biaxial.{{sfn|Paramontroseite – Handbook of Mineralogy|loc=Optical Properties}}

It has a sub-metallic luster and a black streak.

From the Gladstone–Dale relation (KC = 0.393), the NCalc is 2.61 where Ncalc=Dcalc*KC+1, or 2.57 where Ncalc=Dmeas*KC+1.{{sfn|Barthelmy|loc=Optical Properties}}

Paramontroseite crystal properties include:

:

{{notes}}

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{{wiktionary|paramontroseite}}

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Category:Vanadium minerals

Category:Orthorhombic minerals

Category:Minerals in space group 62

Category:Oxide minerals