geotech_ben
Geotechnical
- Jan 10, 2017
- 6
Hello World -
First time question, long time reader. Big, big fan of all the helpful information on this forum
Here is my situation:
We have a 7' swimming pool being constructed in 17' of loose(bpf of 4-7) silty sand to sandy silt (borderline, a typical wash indicates 52% sand) of low unit weight (moist 89 pcf) overlying a dense sandy gravel. We performed consolidation testing on what we believe were undisturbed shelby samples. (Good recovery, care, but they were shipped very well packaged FEDEX next day) We added water to one sample at around 6.7 ksf stress and had a drop of 4.8 percent strain. The other sample showed 0.9 percent strain at 3.4 ksf. Collapse anyone?
The geology maps indicate predominately lacustrine deposits but we may have aeolian (loess) deposits in some depressions. From what I have read in Peck Hanson and Thorburn, 1974, an aeolian transitional material between sand dunes and loess consists of a silty sand. This material will have a very low density and has a potential for collapse.
We are preparing to perform additional consolidation testing where our loading increments are lower and the water is added at a lower stress value to mimic our site conditions. Good idea? Is consolidation testing the best idea? Our total strain for the our expected loads is around 4 percent. Does this seem reasonable?
Thanks!
First time question, long time reader. Big, big fan of all the helpful information on this forum
![[bigsmile] [bigsmile] [bigsmile]](/data/assets/smilies/bigsmile.gif)
We have a 7' swimming pool being constructed in 17' of loose(bpf of 4-7) silty sand to sandy silt (borderline, a typical wash indicates 52% sand) of low unit weight (moist 89 pcf) overlying a dense sandy gravel. We performed consolidation testing on what we believe were undisturbed shelby samples. (Good recovery, care, but they were shipped very well packaged FEDEX next day) We added water to one sample at around 6.7 ksf stress and had a drop of 4.8 percent strain. The other sample showed 0.9 percent strain at 3.4 ksf. Collapse anyone?
The geology maps indicate predominately lacustrine deposits but we may have aeolian (loess) deposits in some depressions. From what I have read in Peck Hanson and Thorburn, 1974, an aeolian transitional material between sand dunes and loess consists of a silty sand. This material will have a very low density and has a potential for collapse.
We are preparing to perform additional consolidation testing where our loading increments are lower and the water is added at a lower stress value to mimic our site conditions. Good idea? Is consolidation testing the best idea? Our total strain for the our expected loads is around 4 percent. Does this seem reasonable?
Thanks!