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M. King Hubbert

M. King Hubbert 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 M. King Hubbert rather than just read about it. In short: Marion King Hubbert (October 5, 1903 – October 11, 1989) was an American geologist and geophysicist. He worked at the Shell research lab in Houston, Texas.

M. King Hubbert — main illustration
M. King Hubbert — illustration

Key takeaways

  • M. King Hubbert 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 M. King Hubbert to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of M. King Hubbert from memory before moving on to harder problems.

Reference excerpt

Marion King Hubbert (October 5, 1903 – October 11, 1989) was an American geologist and geophysicist. He worked at the Shell research lab in Houston, Texas. He made several important contributions to geology, geophysics, and petroleum geology, most notably the Hubbert curve and Hubbert peak theory (a basic component of peak oil), with important political ramifications. He was often referred to as "M. King Hubbert" or "King Hubbert".

Biography Hubbert was born in San Saba, Texas. He attended the University of Chicago, where he received a Bachelor of Science in 1926, a Master of Science in 1928, and a Doctor of Philosophy in 1937, studying geology, mathematics, and physics. He worked as an assistant geologist for the Amerada Petroleum Company for two years while pursuing the PhD, additionally teaching geophysics at Columbia University. He also served as a senior analyst at the Board of Economic Warfare. He joined the Shell Oil Company in 1943, retiring from that firm in 1964. After he retired from Shell, he became a senior research geophysicist for the United States Geological Survey until his retirement in 1976. He also held positions as a professor of geology and geophysics at Stanford University from 1963 to 1968, and as a professor at UC Berkeley from 1973 to 1976. Hubbert was an avid technocrat. He co-founded Technocracy Incorporated with Howard Scott. Hubbert wrote a study course that was published without attribution called the Technocracy Study Course, which advocates a non-market economics form of energy accounting, in contrast to the current price system method. Hubbert was a member of the board of governors, and served as secretary of education in that organization. Hubbert died on October 11, 1989, at the age of 86 while receiving treatment for pulmonary embolism.

Research

Hubbert made several contributions to geophysics, including a mathematical demonstration that rock in the Earth's crust, because it is under immense pressure in large areas, should exhibit plasticity, similar to clay. This demonstration explained the observed results that the Earth's crust deforms over time. He also studied the flow of underground fluids. Based on theoretical arguments, Hubbert (1940) proposed a constitutive equation K abs = N D 2 {\displaystyle K_{\text{abs}}=ND^{2}} for absolute permeability K abs {\displaystyle K_{\text{abs}}} of an underground water or oil reservoir where D {\displaystyle D} is the average grain diameter and N {\displaystyle N} is a dimensionless proportionality constant. However, Kozeny (1927) proposed a constitutive equation for absolute permeability which contains Hubbert's proposal as a factor. Hubbert (1940, 1956) also presented a force potential, denoted Φ {\displaystyle \Phi } or Φ h {\displaystyle \Phi _{h}} , that bears his name:

Φ = ∫ Pref P d P ρ ( P ) − g z ⟹ ∇ Φ h = 1 ρ ∇ P − g ∇ z {\displaystyle \Phi =\int _{\text{Pref}}^{P}{\frac {dP}{\rho (P)}}-gz\implies \nabla \Phi _{h}={\frac {1}{\rho }}\,\nabla P-g\,\nabla z}

Some years later Hubbert (1956) showed that Darcy's law can be derived from the Navier–Stokes equation of motion of a viscous fluid. Hubbert is best known for his studies on the size of oil fields and natural gas reserves, and the limits these impose on rates of oil and gas production. He predicted that for any oil-producing area, whether a province, a nation, or the planet as a whole, the rate of petroleum production of the reserve over time would resemble a bell curve. Based on his theory, he presented a paper to the 1956 meeting of the American Petroleum Institute in San Antonio, Texas, which predicted that overall petroleum production would peak in the United States between 1965, which he considered most likely, and 1970, which he considered an upper bound. At first his prediction received much criticism, for the most part because many other predictions of oil capacity had been made over the preceding half century, but these had usually been based on the reserves-to-production ratio, had not taken into account future discoveries, and had proven false. Hubbert became famous when U.S. oil production hit a peak in 1970 and began to decline, as he had predicted. In 1974, Hubbert projected that global oil production would peak in 1995 "if current trends continue". Various subsequent predictions have been made by others as trends have fluctuated in the intervening years. Hubbert believed that solar power would be a practical renewable energy replacement for fossil fuels, and that nuclear energy in breeder reactors would be able to sustain humanity for centuries. He also states that "provided world population can somehow be brought under control, we may at last have found an energy supply (uranium) adequate for our needs for at least the next few centuries of the 'foreseeable future'."

Contributions Hubbert's contributions to science have been summarized as follows:

Mathematical demonstration that rock in the Earth's crust is plastic, and that the Earth's crust deforms over time. Prediction of migration paths of hydrocarbons. Predictions of peak rates of oil and gas mining, based on a consistent mathematical model which ties reserves, discovery rates, and production rates. His model remains highly influential, and has been widely applied to other finite resources.

… excerpt ends here. Continue reading the full article.

Illustrations

M. King Hubbert illustration
M. King Hubbert: A bell-shaped production curve, as originally suggested by M. King Hubbert in 1956
A bell-shaped production curve, as originally suggested by M. King Hubbert in 1956

Worked examples

Example 1 — a first encounter with M. King Hubbert

Start with the simplest possible case. Write down what M. King Hubbert 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 M. King Hubbert 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 M. King Hubbert 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 M. King Hubbert

In research
M. King Hubbert 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 M. King Hubbert 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
M. King Hubbert is common in secondary-school and first-year university syllabi. It links to neighbouring topics 1903 births, 1989 deaths, 20th-century American geologists, so understanding it makes those chapters shorter.
In everyday life
Look for M. King Hubbert 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 M. King Hubbert in 20 minutes

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

Frequently asked questions

What is M. King Hubbert in simple terms?

Marion King Hubbert (October 5, 1903 – October 11, 1989) was an American geologist and geophysicist. He worked at the Shell research lab in Houston, Texas.

Why does M. King Hubbert 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 M. King Hubbert?

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 M. King Hubbert.

Tags

  • 1903 births
  • 1989 deaths
  • 20th-century American geologists
  • 20th-century American physicists
  • American geophysicists
  • American petroleum geologists
  • Deaths from pulmonary embolism
  • Penrose Medal winners
  • People from San Saba, Texas
  • Presidents of the Geological Society of America
  • Scientists from Houston
  • Shell plc people

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