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Research Report
  • Language: en
  • Pages: 406

Research Report

  • Type: Book
  • -
  • Published: 1960
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  • Publisher: Unknown

None

Hearings and Reports on Atomic Energy
  • Language: en
  • Pages: 632

Hearings and Reports on Atomic Energy

  • Type: Book
  • -
  • Published: 1965
  • -
  • Publisher: Unknown

None

Engineering with Nuclear Explosives
  • Language: en
  • Pages: 408

Engineering with Nuclear Explosives

  • Type: Book
  • -
  • Published: 1964
  • -
  • Publisher: Unknown

None

Hearings
  • Language: en
  • Pages: 2416

Hearings

  • Type: Book
  • -
  • Published: 1965
  • -
  • Publisher: Unknown

None

Nuclear Science Abstracts
  • Language: en
  • Pages: 1310

Nuclear Science Abstracts

  • Type: Book
  • -
  • Published: 1971
  • -
  • Publisher: Unknown

None

When the Ice Is Gone: What a Greenland Ice Core Reveals About Earth's Tumultuous History and Perilous Future
  • Language: en
  • Pages: 179

When the Ice Is Gone: What a Greenland Ice Core Reveals About Earth's Tumultuous History and Perilous Future

Paul Bierman’s realization that Greenland’s ice sheet melted when Earth was no warmer than today sounds an alarm for our planet. In 2018, lumps of frozen soil, collected from the bottom of the world’s first deep ice core and lost for decades, reappeared in Denmark. When geologist Paul Bierman and his team first melted a piece of this unique material, they were shocked to find perfectly preserved leaves, twigs, and moss. That observation led them to a startling discovery: Greenland’s ice sheet had melted naturally before, about 400,000 years ago. The remote island’s ice was far more fragile than scientists had realized—unstable even without human interference. In When the Ice Is G...

Reports Received by Division of Technical Information Extension
  • Language: en
  • Pages: 914
Ice Tunnel Closure Phenomena
  • Language: en
  • Pages: 56

Ice Tunnel Closure Phenomena

  • Type: Book
  • -
  • Published: 1961
  • -
  • Publisher: Unknown

The mechanics of closure, exhibited by ice tunnels, can be understood by considering the ice as a viscous solid. The viscous solid will flow, when subjected to a force, at a rate dependent on the magnitude of the force, the area of relief open for flow, and the apparent viscosity of the viscous solid. In the case of the ice tunnels, the force inducing the flow is the weight of the overburden; the area of relief open for flow is the tunnel opening; and apparent viscosity is the resistance to flow exhibited by the ice. The closure of a rectangular opening made in ice was measured. Maximum closure occurs at the center of unsupported roof, wall, or floor spans. The vertical closure rate decrease...

TID.
  • Language: en
  • Pages: 410

TID.

  • Type: Book
  • -
  • Published: 19??
  • -
  • Publisher: Unknown

None