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Washington, D.C., 5 February 2015— A team of Geophysical Laboratory scientists have found “beautifully preserved” 15 million-year-old thin protein sheets in fossil shells from southern Maryland.

Washington, D.C., 28 January 2015— New findings from a team including Geophysical Laboratory's Ronald Cohen and Peng Zhang shows that a missing piece of the traditional theory explaining why metals become less conductive when they are heated was needed to complete the puzzle that explains Earth's field-generating process.

The AGU Fall Meeting 2014 will take place in San Francisco, CA from December 14-21.  Many staff members and postdoctoral associates from the Geophysical Laboratory will attend this year.  Check here daily for live updates on each day's science presentations.

Please join in on the AGU conversation by following our live Twitter feed, and including #AGU14 on any relevant tweets!

Washington, D.C., 10 December 2014—New work from the Geophysical Laboratory's Ivan Naumov and Russell Hemley delves into the chemistry underlying some surprising recent observations about hydrogen and reveals remarkable parallel between hydrogen and graphene under extreme pressures.

Washington, D.C., 17 November 2014— A team led by the Geophysical Laboratory's Timothy Strobel has synthesized an entirely new form of silicon, one that promises even greater future applications. Although silicon is incredibly common in today's technology, its so-called indirect band gap semiconducting properties prevent it from being considered for next-generation, high-efficiency applications. Strobel's silicon has a quasi-direct band gap that falls within the desired range for solar absorption, something that has never before been achieved.

Washington, D.C., 12 November 2014 —Data have suggested that deep, hot, fluid magma oceans of melted silicates, a major Earth material, may reside above the core-mantle boundary. The Geophysical Laboratory's Alex Goncharov has found, using high-pressure experiments with a proxy material, that the deep Earth materials conduct far less heat under increasing pressure than previously thought.

Washington, D.C., 27 October 2014—In a new paper in Nature Geoscience, the Geophysical Laboratory’s Sami Mikhail and Dimitri Sverjensky outline a compelling model for nitrogen accumulation in Earth’s atmosphere, suggesting subduction, and subsequent degassing at arc volcanoes, is key.

Washington, D.C., 21 October 2014— At extreme pressures hydrogen has four known solid phases. Now scientists, including the Geophysical Laboratory's Alexander Goncharov, have combined hydrogen with its heavier sibling deuterium and created a novel, disordered, “Phase IV”-material, where the molecules interact differently than have been observed before.

The Geophysical Laboratory's Andrew Steele joins the Rosetta team as a Co-Investigator working on the COSAC instrument aboard the Philae lander, which will be deployed to land on the comet in November.

Washington, D.C., 25 September 2014—Natural semiconducting and photon-absorbing ability of GaAs requires some tuning in order to make it more desirable for use in manufacturing products such as solar cells and optoelectronics. New work from a team led by the Geophysical Laboratory’s Alexander Goncharov explores a novel approach to such tuning.

Washington, D.C., 25 September 2014— A team including the Geophysical Laboratory’s Malcolm Guthrie and George Cody has, for the first time, discovered how to produce ultra-thin "diamond nanothreads" that promise extraordinary properties, including strength and stiffness greater than that of today's strongest nanotubes and polymer fibers. 

In celebration of National Postdoc Appreciation Week, the Geophysical Laboratory and DTM held an ice cream social on Wednesday, 17 September 2014 in Tuve Hall. 

Washington, D.C., 31 July 2014—New work from a team including several Geophysical Laboratory scientists reveals that molybdenum disulfide becomes metallic under intense pressure. 

Torredu, India---Geophysical Laboratory research scientist Maddury Somayazulu visited Torredu, India this month and gave a talk to the children of the village in telugu (a South-Central Dravidian language) about how science impacts society.

The high water storage capacity of minerals in Earth’s mantle transition zone (410- to 660-kilometer depth) implies the possibility of a deep H2O reservoir, which could cause dehydration melting of vertically flowing mantle.