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Ullmannite

Ullmannite is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Ullmannite rather than just read about it. In short: Ullmannite or Nickel glance (trivial name) is a nickel antimony sulfide mineral with formula: NiSbS. Considerable substitution occurs with cobalt and iron in the nickel site along with bismuth and arsenic in the antimony site.

Ullmannite — main illustration
Ullmannite — illustration

Key takeaways

  • Ullmannite belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Ullmannite to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Ullmannite from memory before moving on to harder problems.

Reference excerpt

Ullmannite or Nickel glance (trivial name) is a nickel antimony sulfide mineral with formula: NiSbS. Considerable substitution occurs with cobalt and iron in the nickel site along with bismuth and arsenic in the antimony site. A solid solution series exists with the high cobalt willyamite.

Physical properties Ullmannite is steel-gray to tin white in color with a metallic luster, has a Mohs hardness of 5 to 5.5 and a specific gravity of 6.65. Initially thought to be of two species, tetrahedral and cubic, it was later confirmed that both samples conformed to the 23 point group of the isometric crystal class and typically exhibits cubic, octahedral, or pyritohedral forms although euhedral crystals are rare. Variance in its chemical composition has been shown to be responsible for loss of symmetry and variations in striation patterns. Ullmannite crystals are usually less than 2 mm, however larger have been identified in especially antimony rich environments. Ullmannite commonly displays interpenetration twins as well as enantiomorphic twinning along [110].

Occurrence

It is a member of the cobaltite group and forms a series with willyamite ((Co,Ni)SbS). It occurs with nickeline, gersdorffite, pentlandite, chalcopyrite, pyrrhotite, galena, tetrahedrite and dyscrasite in hydrothermal deposits. Principal localities are in Germany, it is also found in Austria, Australia, France, England, and Wales. It was first described in 1843 for an occurrence in the Storch und Schöneberg Mine, North Rhine-Westphalia, Germany. Specimens of ullmannite were found at Sarrabus, Sardinia, Italy in 1887. The crystals of the specimens from Sarrabus were described as hemihedral with parallel faces, whereas specimens from Lölling in present-day Austria were hemihedral with inclined faces.

Origin of name Ullmannite was named for German chemist and mineralogist, Johann Christoph Ullmann (1771–1821), one of the fathers of systematic mineralogy. Ullmann established a mineral collection (now the basis for the internationally renowned Museum of Mineralogy in Marburg) and authored Ein Systematisch-Tabellarische Übersicht der Mineralogisch einfachen Fossilien, one of the first attempts to provide a structured organization to the observed minerals of the day.

See also List of minerals List of minerals named after people

References

Palache, C., H. Berman, and C. Frondel (1944) Dana’s system of mineralogy, (7th edition), v. I, 301–302.

Illustrations

Ullmannite illustration
Ullmannite: Ullmannite crystals from the Masaloni Mine, San Vito, Cagliari Province, Sardinia, Italy (size: 5.4 × 3.3 × 2.1 cm)
Ullmannite crystals from the Masaloni Mine, San Vito, Cagliari Province, Sardinia, Italy (size: 5.4 × 3.3 × 2.1 cm)

Worked examples

Example 1 — a first encounter with Ullmannite

Start with the simplest possible case. Write down what Ullmannite claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Ullmannite before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Ullmannite ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Ullmannite

In research
Ullmannite appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Ullmannite in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Ullmannite is common in secondary-school and first-year university syllabi. It links to neighbouring topics Antimonide minerals, Cubic minerals, Glances, so understanding it makes those chapters shorter.
In everyday life
Look for Ullmannite outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Ullmannite in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Ullmannite means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Ullmannite out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Ullmannite in simple terms?

Ullmannite or Nickel glance (trivial name) is a nickel antimony sulfide mineral with formula: NiSbS. Considerable substitution occurs with cobalt and iron in the nickel site along with bismuth and arsenic in the antimony site.

Why does Ullmannite matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Ullmannite?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Ullmannite.

Tags

  • Antimonide minerals
  • Cubic minerals
  • Glances
  • Minerals described in 1843
  • Minerals in space group 198
  • Nickel minerals
  • Sulfide minerals

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