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Inge Lehmann

Inge Lehmann is a physics 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 Inge Lehmann rather than just read about it. In short: Inge Lehmann (13 May 1888 – 21 February 1993) was a Danish seismologist and geophysicist who is known for her discovery in 1936 of the solid inner core that exists within the molten outer core of the Earth. She also discovered the seismic discontinuity in the speed of seismic waves at depths between 190 km (120 mi) and 250 km (160 mi), which is named the Lehmann discontinuity after her.

Inge Lehmann — main illustration
Inge Lehmann — illustration

Key takeaways

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

Reference excerpt

Inge Lehmann (13 May 1888 – 21 February 1993) was a Danish seismologist and geophysicist who is known for her discovery in 1936 of the solid inner core that exists within the molten outer core of the Earth. She also discovered the seismic discontinuity in the speed of seismic waves at depths between 190 km (120 mi) and 250 km (160 mi), which is named the Lehmann discontinuity after her. Lehmann is considered to be a pioneer among women and scientists in seismology research.

Early life, family and education Inge Lehmann was born on 13 May 1888 and raised in Østerbro, a part of Copenhagen, Denmark. Her father was experimental psychologist Alfred Georg Ludvik Lehmann (1858–1921), a pioneer in the study of experimental psychology in Denmark. Her mother Ida Sophie Tørsleff was a housewife. The Lehmann family had its roots in Bohemia; the Danish branch included barristers, politicians and engineers. Inge Lehmann's paternal grandfather laid out the first Danish telegraph line (1854). Her great-grandfather was Governor of the National Bank. Her mother's father, Hans Jakob Torsleff, was from an old Danish family with a priest in every generation. Members of the Tørsleff family were well-known public leaders and activists in the women's rights movement. Inge's cousins were the Minister of Trade, the chair of the Danish Women's Society, and the leader of the Danish Girl Scouts. Her younger sister Signe, a single mother, rose to popularity as a school superintendent. Lehmann's parents enrolled both their two daughters at Fællesskolen in 1904, a liberal and progressive school that offered the same curriculum to both boys and girls — a practice uncommon at the time. Most schools of this time separated boys' and girls' education. The principles of isolation by sex went much deeper for girls who were education-oriented. It was thought to be damaging to expose girls to mental exhaustion throughout puberty. Males were believed to be more biologically adapted for such activities and therefore, allowed to take the high school entrance exam and start upper-secondary education (high school) at 15 years old, whereas females were prohibited. This policy remained in effect until 1903. This school was led by Hanna Adler, Niels Bohr's aunt, a pioneering woman scholar and firm believer in equality of the sexes. A year after earning her degree, Adler launched her school, inspired by innovative teaching practices in the US. Many of her female co-graduates, who were ineligible for many of the positions accessible to their male peers, were hired by Adler to teach. Women were prohibited from working in universities at the time, and the vast majority of female college graduates searched for employment as elementary schoolteachers despite obtaining degrees that allowed them to teach at the upper-secondary (high school) level. Lehmann credited her father and Hanna Adler as the most significant influences on her intellectual development. At age 18, Lehmann achieved a first rank mark in the entrance exam for University of Copenhagen. In 1907, she started her studies in mathematics, chemistry and physics at the University of Copenhagen. She continued her studies of mathematics at Newnham College, Cambridge, from 1910 to 1911. Lehmann faced sex-based adversities there, not being allowed to fully participate in her studies, nor to achieve higher positions of education. As a result, Lehmann had a mental breakdown during her first year in 1911. She returned to Denmark in 1912. She served as an actuarial assistant until 1918 without attending school. She developed her computational skills in the actuary office until she resumed her studies at Copenhagen University in 1918. She completed the candidata magisterii degree in physical science and mathematics in two years, graduating in 1920. This was significant, since this degree was mostly given to male students. After a short period of time, studying mathematics at the University of Hamburg, in 1923 she accepted a position at University of Copenhagen as an assistant to J.F. Steffensen, the professor of actuarial science. Lehmann's younger sister, Harriet, became an actress. Inge lived alone as an adult. She ended an engagement in March 1917 and decided to remain unmarried in order to pursue an academic career, which was not an unusual choice at the time. Lehmann once complained to her nephew Niels Groes about the incompetence of her male colleagues, writing, "You should know how many incompetent men I had to compete with — in vain."

Career

In 1925, Lehmann was assigned to be the assistant of seismologist Niels Erik Nørlund. She took an interest in his field, and she began studying it on her own. She was chosen as a delegate for Denmark to attend the International Union of Geodesy and Geophysics in 1927—a role she filled another eight times over the next forty years. By 1928, Lehmann obtained a magister scientiarum in seismology, and she was appointed head of the Geodætisk Institut's seismological department the same year. In this position, she was responsible for overseeing the operation of three seismographic observatories, two of which were in Greenland. She personally operated the one in Copenhagen, producing reports based on its readings. Though it was not part of her job, Lehmann also engaged in research at the facility. In 1929, Lehmann studied the Murchison earthquake which struck on the South Island of New Zealand. She analysed the seismic data from the earthquake and noticed that there were waves of significant amplitude recorded in the Russian cities of Sverdlovsk and Irkutsk, both unexpected locations. Lehmann noticed after reviewing the data from the earthquakes that there were waves emanating from the earthquakes, which were called seismic waves. They were unexpected locations due to the theory that S-waves and some P-waves are deflected by the core creating a shadow area in which waves are not able to pass through. The waves seemed to pass through that area to reach Russia. This led to her discovering that there is a spherical core of solid material at the Earth's centre.

… excerpt ends here. Continue reading the full article.

Illustrations

Inge Lehmann illustration
Inge Lehmann: A modern understanding of the Lehmann discontinuity: velocity of seismic S-waves in the Earth near the surface in three tectonic provinces: TNA = Tectonic North America SNA = Shield North America and ATL = North Atlantic.[14]
A modern understanding of the Lehmann discontinuity: velocity of seismic S-waves in the Earth near the surface in three tectonic provinces: TNA = Tectonic North America SNA = Shield North America and ATL = North Atlantic.[14]
Inge Lehmann: Schematic view of Earth's interior structure. .mw-parser-output .legend{page-break-inside:avoid;break-inside:avoid-column}.mw-parser-output .legend-color{display:inline-block;min-width:1.25em;height:1.25em;line-height:1.25;margin:1px 0;text-align:center;border:1px solid black;background-color:transparent;color:black}.mw-parser-output .legend-text{}  continental crust  oceanic crust  upper mantle  lower mantle  outer core  inner core — discovered by LehmannMohorovičić discontinuitycore–mantle boundaryouter core–inner core boundary
Schematic view of Earth's interior structure. .mw-parser-output .legend{page-break-inside:avoid;break-inside:avoid-column}.mw-parser-output .legend-color{display:inline-block;min-width:1.25em;height:1.25em;line-height:1.25;margin:1px 0;text-align:center;border:1px solid black;background-color:transparent;color:black}.mw-parser-output .legend-text{}  continental crust  oceanic crust  upper mantle  lower mantle  outer core  inner core — discovered by LehmannMohorovičić discontinuitycore–mantle boundaryouter core–inner core boundary

Worked examples

Example 1 — a first encounter with Inge Lehmann

Start with the simplest possible case. Write down what Inge Lehmann claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In physics, 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 Inge Lehmann 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 Inge Lehmann 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 Inge Lehmann

In research
Inge Lehmann appears in physics 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 Inge Lehmann 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
Inge Lehmann is common in secondary-school and first-year university syllabi. It links to neighbouring topics 1888 births, 1993 deaths, 20th-century Danish physicists, so understanding it makes those chapters shorter.
In everyday life
Look for Inge Lehmann 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 Inge Lehmann in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Inge Lehmann 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 Inge Lehmann out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Inge Lehmann in simple terms?

Inge Lehmann (13 May 1888 – 21 February 1993) was a Danish seismologist and geophysicist who is known for her discovery in 1936 of the solid inner core that exists within the molten outer core of the Earth. She also discovered the seismic discontinuity in the speed of seismic waves at depths betwee…

Why does Inge Lehmann matter?

Because it connects several physics 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 Inge Lehmann?

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 Inge Lehmann.

Tags

  • 1888 births
  • 1993 deaths
  • 20th-century Danish physicists
  • 20th-century Danish women scientists
  • 20th-century women physicists
  • Alumni of Newnham College, Cambridge
  • Danish geophysicists
  • Danish women centenarians
  • Danish women geologists
  • Foreign members of the Royal Society
  • Scientists from Copenhagen
  • Seismologists

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