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Influence of the fluid-dynamic and rheological properties of sediments on the process of viscoelastic compaction at different rates of sedimentation

✍ Scribed by E. I. Suetnova


Book ID
111457714
Publisher
International Academic Publishing Co (Nauka/Interperiodica)
Year
2010
Tongue
English
Weight
189 KB
Volume
46
Category
Article
ISSN
1069-3513

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The transient and steady-state influence
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The transient and steady-state solution of the linear heat Iransfcr equation considering the rate of compaction of sediments and the vertical migration of interstitial water are obtained, respectively, for a single layer and a multi-layer model of unconsolidated sediments. At steady state the temper