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Home : Our Work : Areas of Research : Plasma Physics

    Plasma Physics

Phone: (202) 767-5635

 

Overview

The Plasma Physics Division conducts broad theoretical and experimental programs of basic and applied research in plasma physics, laboratory discharge, and space plasmas, intense electron and ion beams and photon sources, atomic physics, pulsed power sources, laser physics, advanced spectral diagnostics, and nonlinear systems. 

The effort of the Division is concentrated on a few closely coordinated theoretical and experimental programs. Considerable emphasis is placed on large-scale numerical simulations related to plasma dynamics; ionospheric, magnetospheric, and atmospheric dynamics; nuclear weapons effects; inertial confinement fusion; atomic physics; plasma processing; nonlinear dynamics and chaos; free electron lasers and other advanced radiation sources; advanced accelerator concepts; and atmospheric laser propagation.

Core Capabilities 

  • Radiation Hydrodynamics - The principal emphasis is in the development and application of theoretical models and state-of-the-art numerical simulations combining magnetohydrodynamics, high energy density physics, atomic and radiation physics, and spectroscopy.
  • Laser Plasma - Primary areas of research include physics underpinnings of laser fusion, high-energy-gain laser-inertial- fusion target designs, experiments and simulations of laser-matter interactions at high intensity, advancing the science and technologies of high-energy krypton fluoride and argon fluoride lasers, advancing the technologies of durable high-repetition-rate pulse power and electron-beam diodes for laser pumping and other applications, laser fusion as a power source.
  • Space and Laboratory Plasmas - Space research includes theoretical, numerical, and laboratory and space experimental investigations of the dynamic behavior of the near-Earth space plasmas and radiation belts, and the modification of space plasmas for strategic effects on HF communications, satellite navigation, over-the-horizon radar, and UHF satellite communications.  Applications-oriented plasma research is performed in the production, characterization, and use of low-temperature plasmas and related technology for applications to advance capabilities across the Navy and DOD.  Pulsed-power investigations include electromagnetic launch science and technology and research on directed energy systems for the U.S. Navy.
  • Pulsed Power Physics - Experimental and theoretical research is performed to advance pulsed power driven accelerator technology in areas relevant to defense applications. Research concerns the production, transport, characterization, and modeling of pulsed plasmas and intense high-power, charged particle beams using terawatt-class hundred-kilojoule pulsed power systems that employ capacitive or inductive energy storage and advanced switching. 
  • Directed Energy Physics - Research encompasses the integration of theoretical/computational and experimental research relevant to DOD, ONR, DARPA, and DoE in the areas of ultra-high field laser physics, atmospheric propagation of intense lasers, advanced radiation and accelerator physics, laser-generated plasma-microwave interactions, and dynamics of nonlinear systems. 

Facilities Fact Sheets

  • Electra Experimental Lab Facility - Electron beam pumped laser.  [ Download PDF]
  • NIKE KrF Laser Target Facility.  [Download PDF]
  • Space Plasma Simulation Chamber.  [Download PDF]

Plasma Physics News

NEWS | Sept. 20, 2021

NRL Scientist in the Right Place, Right Time to Record Historical Earthquake

By Kevin McAndrews, U.S. Naval Research Laboratory Corporate Communications

U.S. Naval Research Laboratory (NRL) researcher Ben Phrampus recorded the largest U.S. earthquake in nearly half a century when it hit recently off the coast of southern Alaska. The 8.2-magnitude earthquake went mostly unnoticed since it was almost 20 miles below the ocean floor. It briefly, however, sparked evacuations, tsunami warnings in the region, and two aftershocks of 6.2 and 5.6, respectively.

Phrampus, a research physicist in NRL’s geology and geophysics section, was in the right place at the right time while on watch aboard a research vessel when the earthquake hit July 29, and the crew’s instruments recorded the event.

The United States academic community’s national seismic research facility Marcus G. Langseth, operated by Lamont-Doherty Earth Observatory’s Office of Marine Operations at Columbia University, sat west of an island chain called, Haida Gwaii, off the northern Pacific coast of Canada. An acoustic receiver, known as a hydrophone streamer, recorded the noise while it was in the water at the time and showed a massive spike.

“Seeing it live on the data stream was particularly exciting,” Phrampus said. “We were actually seeing the earthquake’s acoustic waves on our instruments in near real time, which is just awesome.”
The earthquake happened near Perryville, Alaska, a small community on the Alaskan Peninsula about 500 miles southwest of Anchorage.

“I was standing watch (on duty) looking at incoming data to make sure everything looked good,” Phrampus said. “I happened to look at the streamer data at the right time to catch the event as it happened.”

The technicians onboard were initially concerned about what they were seeing.
“We wanted to be sure there wasn’t an issue with the equipment,” he said. “We quickly recognized it was not an equipment issue. This led to our curiosity to find the source.”

Some quick checking revealed it was an earthquake. They confirmed their findings after viewing the U.S. Geological Survey’s website, which reported the 8.2-magnitude quake.

After the tsunami warnings went off, coastal residents scrambled to higher ground and-or evacuated. The earthquake was the most powerful in North America since a 9.2-magnitude earthquake in Alaska in 1964. Known as the “Great Alaskan earthquake,” it spread across south-central Alaska, ground fissures, collapsing structures, and tsunamis. More than 130 died in the most powerful earthquake recorded in North America. This was the second largest earthquake ever recorded on Earth.

The most recent earthquake may have caused light to moderate damage and moderate shaking, according to preliminary seismic data. The U.S. National Tsunami Warning Center canceled a tsunami warning issued for parts of Alaska after waves of less than one foot arrived onshore. Tremors extended throughout the Alaska Peninsula and Kodiak.

Phrampus said a rupture offshore went all the way to the seafloor along the continental slope. This produced seismic energy that interacted with the sound fixing and ranging channel, or SOFAR, which is an ocean channel that allows sound to carry great distances, according to the National Ocean Service. The ocean consists of many zones, and sound can travel through a zone for hundreds, sometimes thousands of miles. Interacting with the SOFAR converted the energy into acoustic waves, a process called downslope conversion, Phrampus said.

This interaction trapped the acoustic waves in the water column and helped spread them across the Pacific Ocean. Just 20 minutes later, the hydrophone streamer recorded the event, Phrampus said, both surprising and exhilarating the crew.

The research team is assessing tectonics and seismic hazards of earthquakes and tsunamis along the Queen Charlotte Fault, which has produced large earthquakes in the past. Though the recent event was exciting enough, there is still a great deal to learn about the most recent earthquake and the fault itself, he said.

“We’ve only done preliminary analysis to verify that the 8.2 quake is what we are seeing on our equipment,” he said. “We will be diving into this more in the coming months.”
The research cruise ended Aug. 24. Results will be presented at the American Geophysical Union in New Orleans in December.


About the U.S. Naval Research Laboratory 

NRL is a scientific and engineering command dedicated to research that drives innovative advances for the U.S. Navy and Marine Corps from the seafloor to space and in the information domain. NRL is located in Washington, D.C. with major field sites in Stennis Space Center, Mississippi; Key West, Florida; Monterey, California, and employs approximately 2,500 civilian scientists, engineers and support personnel.

For more information, contact NRL Corporate Communications at (202) 480-3746 or nrlpao@nrl.navy.mil.