Mccoy
Geotechnical
- Nov 9, 2000
- 907
Dear colleauges,
this issue has being gnawing at the background of my mind for a while now, and it's about time to submit it to your valuable attention.
We know that elastic and shear moduli decrease their value with an increase in strain deformation. Tangent moduli, Eo and Go, may be 10 times the value of secant moduli at large deformations. The adjustment tangent-to-secant may be done in various ways, some of such are called 'degradation schemes', as per the articles by Fahey et al. 1994, advertised by Paul Mayne 1999 and herein attached (chapter 3). It is based upon the determination of the mobilized shear strenght under the foundations and the application of a suitable hyperbolic law. References are contained in the attached Pdf.
Dynamic degradation takes place during earthquakes and in presence of intense vibratory motions. the degradation procedure is usually based on degradation curves, different for each material, where the deformation value is estimated or calculated with numerical methods of local seismic response. There are also tables though, like in the Eurocode 8, where the degradation is in function of the ground acceleration (with an uncertainty band which can be used to adjust for the soil type).
Now, I regularly apply these schemes. One thing makes me wander though. We have for instance a building foundation which mobilizes one third of the available shear strenght. According to Mayne this is the same thing as saying that the actual load is one third the soil bearing capacity. We'll degrade the modul accordingly. Using Fahey et al. procedure, with this degree of strain the modulus becomes 40% of its original value at zero deformation.
Now comes the earthquake though, since we've built in a higly seismic area. Now we have a seismic deformation field (with an alternate sign) which overlaps the static deformation field.
A typical value in my area in medium dense soil is 0.36.
Here I'm lost, since I found no literature which explains how the twine shall compose, a simple summation? about 0.8 in my case? It may be unlikely since the resulting settlement in many cases would be excessive but it doesn't in real life. Alternatively, it may be that the building practice actually mobilizes less soil capacity than what we think.
What are your thoughts on the combination of static and dynamic degradation? Are you aware of any references in the literature?
this issue has being gnawing at the background of my mind for a while now, and it's about time to submit it to your valuable attention.
We know that elastic and shear moduli decrease their value with an increase in strain deformation. Tangent moduli, Eo and Go, may be 10 times the value of secant moduli at large deformations. The adjustment tangent-to-secant may be done in various ways, some of such are called 'degradation schemes', as per the articles by Fahey et al. 1994, advertised by Paul Mayne 1999 and herein attached (chapter 3). It is based upon the determination of the mobilized shear strenght under the foundations and the application of a suitable hyperbolic law. References are contained in the attached Pdf.
Dynamic degradation takes place during earthquakes and in presence of intense vibratory motions. the degradation procedure is usually based on degradation curves, different for each material, where the deformation value is estimated or calculated with numerical methods of local seismic response. There are also tables though, like in the Eurocode 8, where the degradation is in function of the ground acceleration (with an uncertainty band which can be used to adjust for the soil type).
Now, I regularly apply these schemes. One thing makes me wander though. We have for instance a building foundation which mobilizes one third of the available shear strenght. According to Mayne this is the same thing as saying that the actual load is one third the soil bearing capacity. We'll degrade the modul accordingly. Using Fahey et al. procedure, with this degree of strain the modulus becomes 40% of its original value at zero deformation.
Now comes the earthquake though, since we've built in a higly seismic area. Now we have a seismic deformation field (with an alternate sign) which overlaps the static deformation field.
A typical value in my area in medium dense soil is 0.36.
Here I'm lost, since I found no literature which explains how the twine shall compose, a simple summation? about 0.8 in my case? It may be unlikely since the resulting settlement in many cases would be excessive but it doesn't in real life. Alternatively, it may be that the building practice actually mobilizes less soil capacity than what we think.
What are your thoughts on the combination of static and dynamic degradation? Are you aware of any references in the literature?