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Experts Recommend How to Deal With Artificial Earthquakes

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Induced and natural earthqaukes in Calif
A typical sample of daily earthquakes in California is a mixture of natural events and artificial events. In Northern California, geothermal power plants at The Geysers and the Coso Geothermal Field produce continual small quakes plus a few events large enough to be felt. (USGS)

The ongoing rash of earthquakes in Oklahoma is a notorious side-effect of the oil and gas industry, but similar earthquake problems affect other states too.

A new paper from government geologists calls for a response to the growing threat of induced earthquakes by strengthening the national effort to monitor quakes of all kinds. It also calls for the industries involved to make their activities public.

By now, most people in Oklahoma know that the oil and gas industry has caused hundreds of earthquakes in a state where they once were rare. Some other states are reaching that stage, too. People often incorrectly blame the quakes on fracking, the hydraulic fracturing technique recently developed to retrieve oil and gas from shaly (clay-rich) rocks that couldn’t be tapped before.

In 2013 a federal agency, the U.S. Geological Survey, launched a working group at its cutting-edge John Wesley Powell Center for Analysis and Synthesis to tackle the problem of industrial earthquakes in an integrated way. Twelve members of that working group, led by Arthur McGarr, address the topic today in a “policy perspective” article in the journal Science.

Five different industrial practices are known to induce earthquakes—deep waste injection, extending production from old oil wells, fracking, storing carbon dioxide underground and collecting geothermal energy. The first of these, pumping industrial waste into deep rocks, is the most widespread.


Local geology matters. Deep waste injection wells are used across America, tens of thousands of them, but they are inducing earthquakes only in Oklahoma, Colorado, Kansas, Texas, Arkansas and Ohio.

Fracking, despite hundreds of thousands of wells using it, has been linked only to a few seismic events large enough to feel in Ohio. Extended oil production and geothermal energy extraction cause similar amounts of disturbance, and carbon dioxide storage is only an experimental technology.

These practices are used in different places, with different results. Scientifically, what they all have in common is that they inject fluids under high pressure deep into the ground. The earthquakes they induce are rarely large enough to feel. Nevertheless, induced earthquakes are a growing problem and they should be prevented, if we can learn how.

In the Science paper, McGarr’s team notes two factors that are important for deep injection wells in earthquake-prone areas. First, fluids are injected into a “crystalline basement.” This means hard, very old rocks that may react to the unexpected lubrication by releasing ancient stresses.

Second, wells inject large volumes of fluid that may migrate where an existing crack—a fault—is ready to move once the conditions change enough. We can’t always tell beforehand where such a fault may lurk.

Every place is different. In California, for instance, neither factor applies because the geology simply isn’t right. Here, only geothermal energy production creates any noticeable earthquakes, and those are very localized (for instance at The Geysers). Oklahoma is the opposite, and today it’s America’s poster child for induced quakes.

For planning purposes across the country, the Geological Survey has mapped the nationwide risk of earthquakes. This assessment could include the risk of induced earthquakes too, if we had a way to tell natural and artificial quakes apart. That’s still beyond our reach, according to McGarr’s team.

The more we know about induced quakes, the more we need to know. Government agencies, companies and citizens all have an interest in avoiding unwanted earthquakes, but different costs and benefits. Industry has forged ahead without a full understanding of the science, and government must undertake the research we now need with whatever speed it can muster.

To make progress, McGarr’s team argues, “the importance of seismic monitoring cannot be overstated.” They advise improving networks of seismometers to catch the tiniest earthquakes. These may detect warning signs as part of the “traffic light” systems used in some places (like Weld County, Colorado) to regulate the pace of wastewater pumping. Well fields might also be denied permits or relocated where they won’t affect people.

Next, the authors recommend that these seismic networks make their data public in real time. They urge industry to do the same with its data, “such as daily injection rates, wellhead pressures, depth of the injection interval, and properties of the target formation.” Having all the relevant data openly shared would give everyone a better shot at minimizing the problems we’ve created.

Every state has its own mix of geology and industry, so a nationwide policy can’t cover everything. But it could go far, because almost the whole nation is prone to natural earthquakes—major ones struck Boston in 1755, the Midwest in 1811-12 and South Carolina in 1886. The most widely felt earthquake in American history damaged the Washington Monument in 2011. Not to mention California. And I’ve never heard a seismologist say that we have enough seismometers.

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