Trouser
Structural
- Jan 31, 2011
- 19
I am the geotechnical designer for a county bridge replacement over a canal. Spread footings are to be placed within the dense embankment fill. The subsurface profile is attached.
The canal flows seasonally and the subsurface exploration took place approximately two weeks after the canal went dry for the year. Moisture contents in the embankment fill were in the realm of 20-30%, the Tephra (30% Fines) had moisture contents of ~65%, the fine alluvium deposits moisture contents were in the 10-15%, and the flow breccia's moisture content was near 5%. The boring terminated well into a basalt bedrock unit at 70' bgs and no water table was encountered. One hole was placed within 5' of the proposed bent locations and within 10' of the canal (two holes total).
I am assuming that the embankment fill, tephra, and fine alluvial deposits are saturated during canal flow. This is based on the relative moisture contents present in the soil samples after a two week dry canal period. The drainage path is downward towards the breccia. The relative moisture conents would suggest that the Tephra has the lowest hydraulic conductivity and serves as an aquitard (the underlying alluvium has a lower moisture content). The Tephra acts as somewhat of a barrier and keeps the breccia relatively dry.
When calculating effective stresses I intend to use the buyant unit weight of soils down to the base of the fine alluvium deposit; however, below this point the soils are no longer saturated/submerged and will feel the full weight of the soils plus the water. In essence, the breccia will be unsaturated and will have vertical effective stresses calculated using the submerged unit weight of the overlying soils without subtracting the pore water pressure. Is this correct?
Are there other considerations that need to be taken into account for the construction of spread footings on soils with such high moisture contents? Are these values indicative of compressible soils?
The canal flows seasonally and the subsurface exploration took place approximately two weeks after the canal went dry for the year. Moisture contents in the embankment fill were in the realm of 20-30%, the Tephra (30% Fines) had moisture contents of ~65%, the fine alluvium deposits moisture contents were in the 10-15%, and the flow breccia's moisture content was near 5%. The boring terminated well into a basalt bedrock unit at 70' bgs and no water table was encountered. One hole was placed within 5' of the proposed bent locations and within 10' of the canal (two holes total).
I am assuming that the embankment fill, tephra, and fine alluvial deposits are saturated during canal flow. This is based on the relative moisture contents present in the soil samples after a two week dry canal period. The drainage path is downward towards the breccia. The relative moisture conents would suggest that the Tephra has the lowest hydraulic conductivity and serves as an aquitard (the underlying alluvium has a lower moisture content). The Tephra acts as somewhat of a barrier and keeps the breccia relatively dry.
When calculating effective stresses I intend to use the buyant unit weight of soils down to the base of the fine alluvium deposit; however, below this point the soils are no longer saturated/submerged and will feel the full weight of the soils plus the water. In essence, the breccia will be unsaturated and will have vertical effective stresses calculated using the submerged unit weight of the overlying soils without subtracting the pore water pressure. Is this correct?
Are there other considerations that need to be taken into account for the construction of spread footings on soils with such high moisture contents? Are these values indicative of compressible soils?