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Induced seismicity in Basel

Induced seismicity in Basel 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 Induced seismicity in Basel rather than just read about it. In short: Induced seismicity in Basel led to suspension of its hot dry rock (HDR) enhanced geothermal systems project. A seismic-hazard evaluation was then conducted, resulting in the cancellation of the project in December 2009.

Key takeaways

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

Reference excerpt

Induced seismicity in Basel led to suspension of its hot dry rock (HDR) enhanced geothermal systems project. A seismic-hazard evaluation was then conducted, resulting in the cancellation of the project in December 2009. Basel, Switzerland sits atop a historically active fault and most of the city was destroyed in a magnitude 6.5 earthquake in 1356. But the Basel project, although it had established an operational approach for addressing induced earthquakes, had not performed a thorough seismic risk assessment before starting geothermal stimulation. Seismic events in Basel reached the trip point of Richter Magnitude ML 2.9 six days after the main stimulation was started on December 2, despite precautionary reduction of the injection rate earlier that same day upon reaching earlier "soft" thresholds. However, further tremors exceeding magnitude 3 were recorded on 6 January (measuring 3.1), 16 January 2007 (3.2), and 2 February 2007 (3.2). In all, between December 2006 and March 2007, the six borehole seismometers installed near the Basel injection well recorded more than 13,500 potential events connected with the geothermal project. The 200 largest were between magnitudes 0.7 and 3.4. Nine of these events had an ML of 2.5 or larger. The remainder were too small to be observed or felt at the surface. Between December 2 and January 24, 168 seismic events with magnitude greater than 0.6 occurred within 1 km of the wellbore, at depths of 4–5 km, near the well bottom. On 8 December 2006, only 6 days after the main stimulation started on 2 December, the HDR project in Basel was suspended when an earthquake tripped a 4-level "traffic light" scheme established for halting operations in the event of unacceptable induced earthquake occurrences. Trip points of Richter magnitudeML 2.9 and a peak ground velocity of 5 millimeters per second were established by the project as independent criteria for a "red alert" that entailed halting fluid injection and bleeding-off to minimum wellhead pressure. Lesser operational curtailments were triggered for lower magnitude and peak ground velocity thresholds. Earlier that day, a "yellow alert"—the second level—was called at 03:06 local time after a 2.6 ML event with peak ground velocity of 0.55 mm/s, which exceeded the "soft" 2.3 ML and 0.5 mm/s thresholds. As a precaution, the injection rate was reduced at 04:04. Following further events that were larger than 2.0ML, a level-three "orange alert" was declared—the injection was stopped at 11:34 and the well shut-in, maintaining the pressure. However, a 2.7 ML event occurred at 15:46, followed by a 3.4 ML event at 16:48, and so in accordance with the response strategy, the well was bled off as soon as practicable. The largest event prompted concern from local residents. The six borehole seismometers installed near the Basel injection well to monitor the natural background seismicity and the geothermal stimulation recorded more than 13,500 potential events connected with the geothermal project, from which 3,124 were of sufficient quality to permit [hypocenter] determinations in the period 2–12 December 2006, which spanned the main stimulation and the decline in the event rate. During the post-stimulation period from 13 December 2006 onward, a further 350 locatable events were detected up to 2 May 2007, by which time events were occurring sporadically at around one per day. In all, locations for more than 3,500 events were determined. Of these more than 3,500 events, only the 200 largest (magnitudes between 0.7 and 3.4) were also observed by the earthquake networks of the Swiss Seismological Service and the Seismological Service of Baden-Wuerttemberg, The remainder were too small to be observed or felt at the surface. For the period through 24 January 2007, there were 168 earthquakes with magnitudes > 0.6, 15 with ML > 2, and three with ML > 3. All of these were within 1 km of the wellbore, and at depths between 4 and 5 km, near the well bottom. There were only 9 events with an ML of 2.5 or larger in the borehole vicinity for the period through 2007. Five occurred in December 2006, two in January 2007, and one each February and March. Damage claims arose from the largest of the events. Eventually, some 2,700 claims were processed by the project's insurer for an estimated 7 million – 9 million Swiss francs (about 6.5 million to 8.3 million U.S dollars) Following a three-year study, the Basel HDR project canceled in December 2009. The study predicted that the town would have continued to experience small earthquakes a few times a year over the 30-year lifetime of the project. The USA soon reacted with new regulations on deep geothermal energy projects.

See also Energy in Switzerland Electricity sector in Switzerland

References

Worked examples

Example 1 — a first encounter with Induced seismicity in Basel

Start with the simplest possible case. Write down what Induced seismicity in Basel 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 Induced seismicity in Basel 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 Induced seismicity in Basel 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 Induced seismicity in Basel

In research
Induced seismicity in Basel 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 Induced seismicity in Basel 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
Induced seismicity in Basel is common in secondary-school and first-year university syllabi. It links to neighbouring topics Basel, Renewable energy in Switzerland, so understanding it makes those chapters shorter.
In everyday life
Look for Induced seismicity in Basel 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 Induced seismicity in Basel in 20 minutes

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

Frequently asked questions

What is Induced seismicity in Basel in simple terms?

Induced seismicity in Basel led to suspension of its hot dry rock (HDR) enhanced geothermal systems project. A seismic-hazard evaluation was then conducted, resulting in the cancellation of the project in December 2009.

Why does Induced seismicity in Basel 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 Induced seismicity in Basel?

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 Induced seismicity in Basel.

Tags

  • Basel
  • Renewable energy in Switzerland

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