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Meteorite Watch Rhodium plated full meteorite case + dial Miyota waterproof 5ATM
Estimated price for orientation: 4 500 $
Category: Meteorites and Tektites
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Description Brand: Muonionalusta Meteorite Watch Case Finish: Rhodium plated hardened glass MPN: Does Not Apply Face Color: Rhodium Features: 44 hour gear reserve and date Band Material: Genuine Leather Movement: Automatic Miyota Japan 44 hours gear reserve Band Color: Black, Multi-Color Water Resistance Rating: 50 m (5 ATM) Case Size: 40mm Display: Analog Year of Manufacture: 2010-Now Watch Shape: Round Country/Region of Manufacture: Germany Case Material: Etched Meteorite Metal Case Meteorite Watch: Muoninalusta Meteorite etched dial rhodium plated Case Color: Rhodium UPC: Does not apply
Meteorite cross-section, showing Widmanstätten patterns. The 60° angle between the sets of lamellae indicates this plate was cut approximately parallel to the form of the structure.Widmanstätten patterns, also called Thomson structures, are historically figures of long - crystals, found in the and some. They consist of a fine interleaving of and bands or ribbons called . Commonly, in gaps between the lamellae, a fine-grained mixture of and called can be found. Widmanstätten patterns describe features in modern steels, titanium and zirconium alloys.Discovery[]Widmanstätten pattern in the Staunton meteoriteIn 1808, these figures were named after , the director of the Imperial Porcelain works in . While flame heating ,Widmanstätten noticed color and zone differentiation as the various iron alloys oxidized at different rates. He did not publish his findings, claiming them only via oral communication with his colleagues. The discovery was acknowledged by , director of the Vienna Mineral and Zoology Cabinet, who named the structure after Widmanstätten.However, it is now believed that full credit for the discovery should actually be assigned to as he published the same findings four years earlier.Working in Naples in 1804, treated a with in an effort to remove the dull patina caused by oxidation. Shortly after the acid made contact with the metal, strange figures appeared on the surface, which he detailed as described above. Civil wars and political instability in southern Italy made it difficult for Thomson to maintain contact with his colleagues in England. This was demonstrated in his loss of important correspondence when its carrier was murdered. As a result, in 1804, his findings were only published in French in the Bibliothèque Britannique. At the beginning of 1806, invaded the and Thomson was forced to flee to and in November of that year, he died in at the age of 46. In 1808, Thomson's work was again published posthumously in Italian (translated from the original English manuscript) in Atti dell'Accademia Delle Scienze di Siena. The obstructed Thomson's contacts with the scientific community and his peregrinations across Europe, in addition to his early death, obscured his contributions for many years.The most common names for these figures are Widmanstätten pattern and Widmanstätten structure, however there are some spelling variations:Moreover, due the discover priority of , several authors suggested to call these figures Thomson structure or Thomson-Widmanstätten structure.Lamellae formation mechanismPhase diagram explaining how the pattern forms. First is exclusively composed of taenite. When cooling off it passes a phase boundary where is exsolved from taenite. with less than about 6 % Nickel () is completely changed to kamacite.Widmanstätten pattern, metallographic polished section and form at temperatures below the ; these alloys are . At temperatures below 900 to 600 °C (depending on the Ni content), two alloys with different nickel content are stable: kamacite with lower Ni-content (5 to 15% Ni) and taenite with high Ni (up to 50%). have a nickel content intermediate between the norm for and ; this leads under slow cooling conditions to the precipitation of kamacite and growth of kamacite plates along certain in the taenite crystal lattice.The formation of Ni-poor kamacite proceeds by diffusion of Ni in the solid alloy at temperatures between 700 and 450 °C, and can only take place during very slow cooling, about 100 to 10,000 °C/Myr, with total cooling times of 10 Myr or less. This explains why this structure cannot be reproduced in the laboratory.The patterns become visible when the meteorites are cut, polished, and acid etched, because is more resistant to the acid. In the picture shown, the broad white bars are kamacite (dimensions in the mm-range), and the thin line-like ribbons are taenite. The dark mottled areas are called plessite.The dimension of lamellae ranges from coarsest to finest (upon their size) as the nickel content increases. This classification is called .UseSince nickel-iron crystals grow to lengths of some centimetres only when the solid metal cools down at an exceptionally slow rate (over several million years), the presence of these patterns is the proof of the origin of the material and can be used to easily determine if a piece of comes from a .PreparationThe methods used to reveal the Widmanstätten pattern on iron meteorites vary. Most commonly, the slice is ground and polished first, then cleaned to remove any remaining polish and dirt. The slice is then placed into a solution or, more usually, solution. Since the content of each meteorite varies, the time of etch also varies; 30 to 60 seconds is typical. Once the meteorite has been etched, it is usually neutralized in an such as solution to remove any remaining acid and then washed and dried; application of a light gun oil helps resist corrosion.Shape and orientationCutting the meteorite along different planes affects the shape and direction of Widmanstätten figures because kamacite lamellae in octahedrites are precisely arranged. Octahedrites derive their name from the crystal structure paralleling an . Opposite faces are parallel so, although an octahedron has 8 faces, there are only 4 sets of plates. Iron and nickel-iron form crystals with an external octahedral structure only very rarely, but these orientations are still plainly detectable crystallographically without the external habit. Cutting an octahedrite meteorite along different planes (or any other material with octahedral symmetry, which is a sub-class of cubic symmetry) will result in one of these cases:perpendicular cut to one of the three (cubic) axes: two sets of bands at right angles each otherparallel cut to one of the octahedron faces (cutting all 3 cubic axes at the same distance from the crystallographic centre) : three sets of bands running at 60° angles each otherany other angle: four sets of bands with different angles of intersectionStructures in non-meteoritic materialsThe term "Widmanstätten structure" is also used on non-meteoritic material to indicate a structure with a geometrical pattern resulting from the formation of a new along certain of the parent phase, such as the basketweave structure in some . The Widmanstatten structures form due to the growth of new phases within the grain boundaries of the parent metals, generally increasing the hardness and brittleness of the metal. The structures form due to the precipitation of a single crystal-phase into two separate phases. In this way, the Widmanstatten transformation differs from other transformations, such as a or ferrite transformation. The structures form at very precise angles, which may vary depending on the arrangement of the crystal lattices. These are usually very small structures that must be viewed through a microscope, because a very long cooling rate is generally needed to produce structures visible to the naked eye. However, they usually have a great and often an undesirable effect on the properties of the alloy.Widmanstatten structures tend to form within a certain temperature range, growing larger over time. In , for example, Widmanstatten structures form during if the steel is held within a range around 500 °F (260 °C) for long periods of time. These structures form as needle or plate-like growths of within the crystal boundaries of the martensite. This increases the brittleness of the steel in a way that can only be relieved by recrystallizing. Widmanstatten structures made from sometimes occur in carbon steel, if the carbon content is below but near the composition (~ 0.8% carbon). This occurs as long needles of ferrite within the .Widmanstatten structures form in many other metals as well. They will form in brass, especially if the alloy has a very high zinc content, becoming needles of zinc in the copper matrix. The needles will usually form when the brass cools from the recrystallization temperature, and will become very coarse if the brass is annealed to 1,112 °F (600 °C) for long periods of time. , which is an iron-nickel alloy very similar to meteorites, also displays very coarse Widmanstatten structures. Telluric iron is metallic iron, rather than an ore (in which iron is usually found), and it originated from the Earth rather than from space. Telluric iron is an extremely rare metal, found only in a few place in the world. Like meteorites, the very coarse Widmanstatten structures most likely develop through very slow cooling, except that the cooling occurred in the Earth's mantle and crust rather than in the vacuum of space.However, the appearance, the composition and the formation process of these terrestrial Widmanstatten structures are different from the characteristic structure of iron meteorites. steels such as also bear patterns, but they are easily discernible from any Widmanstätten pattern.Widmanstätten pattern observed in 4, βZr grain boundaries are still visible even though βZr has been transformed to Widmanstätten. Micrograph of the previous probeSee also
Description
| Brand: | Muonionalusta Meteorite Watch | Case Finish: | Rhodium plated hardened glass |
| MPN: | Does Not Apply | Face Color: | Rhodium |
| Features: | 44 hour gear reserve and date | Band Material: | Genuine Leather |
| Movement: | Automatic Miyota Japan 44 hours gear reserve | Band Color: | Black, Multi-Color |
| Water Resistance Rating: | 50 m (5 ATM) | Case Size: | 40mm |
| Display: | Analog | Year of Manufacture: | 2010-Now |
| Watch Shape: | Round | Country/Region of Manufacture: | Germany |
| Case Material: | Etched Meteorite Metal Case | Meteorite Watch: | Muoninalusta Meteorite etched dial rhodium plated |
| Case Color: | Rhodium | UPC: | Does not apply |
Meteorite cross-section, showing Widmanstätten patterns. The 60° angle between the sets of lamellae indicates this plate was cut approximately parallel to the form of the structure.
Widmanstätten pattern in the Staunton meteorite
Phase diagram explaining how the pattern forms. First is exclusively composed of taenite. When cooling off it passes a phase boundary where is exsolved from taenite. with less than about 6 % Nickel () is completely changed to kamacite.
Widmanstätten pattern, metallographic polished section
The dimension of lamellae ranges from coarsest to finest (upon their size) as the nickel content increases. This classification is called .UseSince nickel-iron crystals grow to lengths of some centimetres only when the solid metal cools down at an exceptionally slow rate (over several million years), the presence of these patterns is the proof of the origin of the material and can be used to easily determine if a piece of comes from a .PreparationThe methods used to reveal the Widmanstätten pattern on iron meteorites vary. Most commonly, the slice is ground and polished first, then cleaned to remove any remaining polish and dirt. The slice is then placed into a solution or, more usually, solution. Since the content of each meteorite varies, the time of etch also varies; 30 to 60 seconds is typical. Once the meteorite has been etched, it is usually neutralized in an such as solution to remove any remaining acid and then washed and dried; application of a light gun oil helps resist corrosion.Shape and orientationCutting the meteorite along different planes affects the shape and direction of Widmanstätten figures because kamacite lamellae in octahedrites are precisely arranged. Octahedrites derive their name from the crystal structure paralleling an . Opposite faces are parallel so, although an octahedron has 8 faces, there are only 4 sets of plates. Iron and nickel-iron form crystals with an external octahedral structure only very rarely, but these orientations are still plainly detectable crystallographically without the external habit. Cutting an octahedrite meteorite along different planes (or any other material with octahedral symmetry, which is a sub-class of cubic symmetry) will result in one of these cases:perpendicular cut to one of the three (cubic) axes: two sets of bands at right angles each otherparallel cut to one of the octahedron faces (cutting all 3 cubic axes at the same distance from the crystallographic centre) : three sets of bands running at 60° angles each otherany other angle: four sets of bands with different angles of intersectionStructures in non-meteoritic materialsThe term "Widmanstätten structure" is also used on non-meteoritic material to indicate a structure with a geometrical pattern resulting from the formation of a new along certain of the parent phase, such as the basketweave structure in some . The Widmanstatten structures form due to the growth of new phases within the grain boundaries of the parent metals, generally increasing the hardness and brittleness of the metal. The structures form due to the precipitation of a single crystal-phase into two separate phases. In this way, the Widmanstatten transformation differs from other transformations, such as a or ferrite transformation. The structures form at very precise angles, which may vary depending on the arrangement of the crystal lattices. These are usually very small structures that must be viewed through a microscope, because a very long cooling rate is generally needed to produce structures visible to the naked eye. However, they usually have a great and often an undesirable effect on the properties of the alloy.Widmanstatten structures tend to form within a certain temperature range, growing larger over time. In , for example, Widmanstatten structures form during if the steel is held within a range around 500 °F (260 °C) for long periods of time. These structures form as needle or plate-like growths of within the crystal boundaries of the martensite. This increases the brittleness of the steel in a way that can only be relieved by recrystallizing. Widmanstatten structures made from sometimes occur in carbon steel, if the carbon content is below but near the composition (~ 0.8% carbon). This occurs as long needles of ferrite within the .Widmanstatten structures form in many other metals as well. They will form in brass, especially if the alloy has a very high zinc content, becoming needles of zinc in the copper matrix. The needles will usually form when the brass cools from the recrystallization temperature, and will become very coarse if the brass is annealed to 1,112 °F (600 °C) for long periods of time. , which is an iron-nickel alloy very similar to meteorites, also displays very coarse Widmanstatten structures. Telluric iron is metallic iron, rather than an ore (in which iron is usually found), and it originated from the Earth rather than from space. Telluric iron is an extremely rare metal, found only in a few place in the world. Like meteorites, the very coarse Widmanstatten structures most likely develop through very slow cooling, except that the cooling occurred in the Earth's mantle and crust rather than in the vacuum of space.However, the appearance, the composition and the formation process of these terrestrial Widmanstatten structures are different from the characteristic structure of iron meteorites. steels such as also bear patterns, but they are easily discernible from any Widmanstätten pattern.
Widmanstätten pattern observed in 4, βZr grain boundaries are still visible even though βZr has been transformed to Widmanstätten.
Micrograph of the previous probe