<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>W.B. Durham</dc:contributor>
  <dc:contributor>L.A. Stern</dc:contributor>
  <dc:contributor>S. H. Kirby</dc:contributor>
  <dc:creator>T. Kubo</dc:creator>
  <dc:date>2006</dc:date>
  <dc:description>Rheological experiments on fine-grained water ice II at low strain rates reveal a creep mechanism that dominates at conditions of low stress. Using cryogenic scanning electron microscopy, we observed that a change in stress exponent from 5 to 2.5 correlates strongly with a decrease in grain size from about 40 to 6 micrometers. The grain size-sensitive creep of ice II demonstrated here plausibly dominates plastic strain at the low-stress conditions in the interior of medium- to large-sized icy moons of the outer solar system.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.1121296</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Grain size-sensitive creep in ice II</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>