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Microtremor

Microtremor is a 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 Microtremor rather than just read about it. In short: Microtremor is a low amplitude (in the order of micrometres) ambient vibration of the ground caused by man-made or atmospheric disturbances. The term Ambient Vibrations is now preferred to talk about this phenomenon.

Key takeaways

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

Reference excerpt

Microtremor is a low amplitude (in the order of micrometres) ambient vibration of the ground caused by man-made or atmospheric disturbances. The term Ambient Vibrations is now preferred to talk about this phenomenon. Observation of microtremors can give useful information on dynamic properties of the site such as predominant period and amplitude. Microtremor observations are easy to perform, inexpensive and can be applied to places with low seismicity as well, hence, microtremor measurements can be used conveniently for seismic microzonation. More detailed information on the shear wave velocity profile of the site can be obtained from microtremor array observation.

History After the pioneering work by Kannai and Tanaka, many researchers have investigated the applicability and reliability of the microtremor method. The major drawback of the method proposed by Kannai and Tanaka was that they considered the Fourier spectra of observed horizontal motions to reflect the transfer function of the surface. It has now been established that the horizontal microtremor spectra often show the characteristics of the source rather than the transfer function of a site. Yukta Nakamura in 1989, modified microtremor analysis by proposing a new technique, generally referred to as the H/V method. In this technique, it was shown that the source effect can be minimized by normalizing the horizontal spectral amplitude with the vertical spectral amplitude. Assuming that the shear wave dominates the microtremor, Nakamura indicated that the horizontal-to-vertical (H/V) spectral ratio of microtremors at a site roughly equals the S wave transfer function between the ground surface and bedrock at a site. This means that the H/V peak period and peak value itself correspond to the natural site period and amplification factor respectively. This method does not require any boreholes and is, hence, more convenient and inexpensive compared to the traditional borehole method. This method is now widely used for microtremor observation although it lacks a clear theoretical background. Lermo and Chavez-Garcia showed the applicability of Nakamura's method of microtremor in site effect prediction. However, it was found true only for the fundamental resonance peak of the transfer function. The results supported the idea that Nakamura's technique effectively compensated for the site effects. Another technique which known as refraction microtremor is also widely used in earth sciences today.

References

Worked examples

Example 1 — a first encounter with Microtremor

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

In research
Microtremor appears in 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 Microtremor 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
Microtremor is common in secondary-school and first-year university syllabi. It links to neighbouring topics Seismology, so understanding it makes those chapters shorter.
In everyday life
Look for Microtremor 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 Microtremor in 20 minutes

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

Frequently asked questions

What is Microtremor in simple terms?

Microtremor is a low amplitude (in the order of micrometres) ambient vibration of the ground caused by man-made or atmospheric disturbances. The term Ambient Vibrations is now preferred to talk about this phenomenon.

Why does Microtremor matter?

Because it connects several 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 Microtremor?

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 Microtremor.

Tags

  • Seismology

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