Abstract
Experimental evidence for the saturation dependence of the nonlinear behavior of Berea sandstone has been analyzed using the Preisach-Mayergoyz space (P-M space) model in terms of classical and non-classical mesoscopic entities. The analysis suggests the introduction of two macroscopic solid-fluid interaction pressures, which link the moisture influence to characteristic populations of the material composition.
| Original language | English |
|---|---|
| Article number | 48 |
| Number of pages | 4 |
| Journal | Geophysical Research Letters |
| Volume | 29 |
| Issue number | 7 |
| DOIs | |
| Publication status | Published - 2002 |
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