NNSS seismic tests can assist in detecting nuclear explosions

The Nevada National Security Site improves the nation’s ability to detect nuclear tests by continuously monitoring the recent Nevada earthquake.

In the aftermath of a 6.5-magnitude earthquake that struck central Nevada on May 15, NNSS deployed 48 seismic stations. The event, which struck the Monte Cristo mountain range, was Nevada’s largest earthquake in 66 years.

In 2018, NNSS received a new capacity to experiment with dry silt geology in the form of 500 portable seismic stations. These stations can be deployed in a short period of time and can collect data up to 30 days.

NNSS scientist, PhD, Cleat Zeiler, responded safely to the event after coordinating with the US Geological Survey and University of Nevada, Reno to position the sensors along the fault optimally. With the help of facility personnel, Zeller programmed and prepared 48 systems, weighing a total of 1,000 pounds, to deploy across the fault in central Nevada. While preparing the post, Zeller felt a 3.0-degree aftershock and heard the sound of rocks breaking.

“This experience alone made my tired, sore body regenerate,” Zeller said. “Putting the whole group in perspective. I’m going to collect a unique data set.”

Within 24 hours of the main shock, all 48 stations were operational. Typically, this level of effort could take several weeks to deploy, but the new capability provides a unique opportunity to respond quickly and effectively.

While most seismic sequences finish in a month, this sequence has been active for three months because earthquake stations only last 25 to 30 days, student interns Michel Dunn and Ryan Jensen Zeller helped switch devices and perform seismic risk assessments during the period. Active. Dan also uses the data to determine the seismic hazard associated with the region.

The main reason for collecting data from this earthquake is the shallow nature of the aftershocks. Most of the events are 8 to 10 kilometers deep; This sequence had events ranging from 1 to 20 km. This information will allow the NNSS to understand how to determine whether shallow aftershocks are explosions or earthquakes, since the depth of aftershock is usually the best indicator.

Using this set of data, the NNSS will be able to demonstrate a set of earthquake signatures and enhance the nation’s ability to detect nuclear tests.

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