Pages that link to "Item:Q4366491"
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The following pages link to Continuum mechanical modelling of the dissipative processes in the sediment-water layer below glaciers (Q4366491):
Displaying 13 items.
- A damage constitutive model for sliding friction coupled to wear (Q304164) (← links)
- Numerical evidence for the approximation of dissipative systems by gyroscopically coupled oscillator chains (Q2111905) (← links)
- Free-boundary models of a meltwater conduit (Q3193300) (← links)
- Paradoxes and problems with the longitudinal stress approximation used in glacier mechanics (Q3442906) (← links)
- A sliding law for glaciers of constant viscosity in the presence of subglacial cavitation (Q3771838) (← links)
- What are the dominant thermomechanical processes in the basal sediment layer of large ice sheets? (Q4223955) (← links)
- Temperature profile in a liquid–vapour interface near the critical point (Q4644835) (← links)
- On the role of mechanical interactions in the steady-state gravity flow of a two-constituent mixture down an inclined plane (Q4716835) (← links)
- Variations of porosity in a sheared pressurized layer of saturated soil induced by vertical drainage of water (Q4719855) (← links)
- A damaged non-homogeneous Timoshenko beam model for a dam subjected to aging effects (Q4992816) (← links)
- To Francesco dell’Isola (Q5048069) (← links)
- Maestro and his pupils: History of a scientific production (Q5048070) (← links)
- Cavitation on Deformable Glacier Beds (Q5432378) (← links)
