Mccoy
Geotechnical
- Nov 9, 2000
- 907
A colleague of mine asked my opinion for a practical case he is examining:
we have a NC clay with very low permeability, a shallow water table and an excavation with a face a few metres high. Everything into the same low-permeability formation, no conspicuos silty or sandy layers. Just after excavation, the unloading causes a state of negative pore pressures in soil within and around the active wedge. We verify excavation stability in terms of Su. The Mohr circle construction makes it evident that a total stress analysis is more favourable (less conservative) than one based upon effective stresses, but it governs the calcs in the short term, some time after the cut has been completed.
Yet, beyond end of construction stage, after a wall or wathever has been built to contain the face (or even after face has been left unconfined), a swelling phenomenon (the reverse of consolidation) is triggered, due to a water influx toward the active wedge region which tends to equalize pore pressure.
The question, at last, is the following: How long does it take to reach such a degree of swelling that effective stresses analysis will govern the excavation stability?
It is the reverse of the question: "how long before a NC clay layer underneath a foundation will consolidate enough to allow us to reason in terms of effective stresses, in this instance (this is a loading problem) more conservative than a total stress analysis?".
The foundation example of course has well defined boundary conditions, which is not usually the case for the excavation problem. Tomlinson reports cases in London brown clay where excavations of similar geometry took 1 to 6 months prior to collapse. If we construe collapse as reaching the effective stress state, that could be an answer. My only doubt is that our clay has a very low permeability. I would expect YEARS to reach pore pressure equalization. Can that time in the real world routinely be shortened by ubiquitous permeable and almost invisible layers? Or by (micro)cracks in the active wedge caused by unloading stresses?
Am I missing some relevant point?
What's your opinion (based on literature or hard evidence) about the time necessary to reach the effective stress state in the example situation?
we have a NC clay with very low permeability, a shallow water table and an excavation with a face a few metres high. Everything into the same low-permeability formation, no conspicuos silty or sandy layers. Just after excavation, the unloading causes a state of negative pore pressures in soil within and around the active wedge. We verify excavation stability in terms of Su. The Mohr circle construction makes it evident that a total stress analysis is more favourable (less conservative) than one based upon effective stresses, but it governs the calcs in the short term, some time after the cut has been completed.
Yet, beyond end of construction stage, after a wall or wathever has been built to contain the face (or even after face has been left unconfined), a swelling phenomenon (the reverse of consolidation) is triggered, due to a water influx toward the active wedge region which tends to equalize pore pressure.
The question, at last, is the following: How long does it take to reach such a degree of swelling that effective stresses analysis will govern the excavation stability?
It is the reverse of the question: "how long before a NC clay layer underneath a foundation will consolidate enough to allow us to reason in terms of effective stresses, in this instance (this is a loading problem) more conservative than a total stress analysis?".
The foundation example of course has well defined boundary conditions, which is not usually the case for the excavation problem. Tomlinson reports cases in London brown clay where excavations of similar geometry took 1 to 6 months prior to collapse. If we construe collapse as reaching the effective stress state, that could be an answer. My only doubt is that our clay has a very low permeability. I would expect YEARS to reach pore pressure equalization. Can that time in the real world routinely be shortened by ubiquitous permeable and almost invisible layers? Or by (micro)cracks in the active wedge caused by unloading stresses?
Am I missing some relevant point?
What's your opinion (based on literature or hard evidence) about the time necessary to reach the effective stress state in the example situation?