jmh77
Civil/Environmental
- Apr 17, 2012
- 3
I am overseeing a 6' deep trench for the purpose of laying a 6" fire water line. Ingress will be required for the pipe layers to perform their connections. This project is in the Pacific Northwest where our groundwater table is approximately 5' below ground surface.
The soil strata consists of a thin layer ~1' of non-cohesive fill followed by native clayey material which has not be characterized in a lab.
Visual and manual observation of the native material gives our engineers strong confidence that the material is atleast deserving of a Type 'B' classification. In preparation for ingress, we have benched the excavation according to OSHA requirements for Type 'B' soil and the formation is stiff under foot and seemingly very reliable.
Despite the type 'B' qualities of the soil, the bottom of the excavation is just below the water table and we are seeing slow but steady seepage of water into the trench bottom.
According to OSHA, the soil must be declassified to Type C if "water is freely seeping through the sides of the excavation".
My question is, how should I interpret the meaning of "freely seeping". Is the presence of slowly flowing groundwater at the bottom of our trench immediate grounds for declassification from Type B to Type C conditions?
The soil is clearly very stiff outside of the seepage zone and meeting Class C excavation requirements is burdensome (for various site specific reasons),however, we want to adhere to the intent of OSHA's requirements and be conservative above all else.
The soil strata consists of a thin layer ~1' of non-cohesive fill followed by native clayey material which has not be characterized in a lab.
Visual and manual observation of the native material gives our engineers strong confidence that the material is atleast deserving of a Type 'B' classification. In preparation for ingress, we have benched the excavation according to OSHA requirements for Type 'B' soil and the formation is stiff under foot and seemingly very reliable.
Despite the type 'B' qualities of the soil, the bottom of the excavation is just below the water table and we are seeing slow but steady seepage of water into the trench bottom.
According to OSHA, the soil must be declassified to Type C if "water is freely seeping through the sides of the excavation".
My question is, how should I interpret the meaning of "freely seeping". Is the presence of slowly flowing groundwater at the bottom of our trench immediate grounds for declassification from Type B to Type C conditions?
The soil is clearly very stiff outside of the seepage zone and meeting Class C excavation requirements is burdensome (for various site specific reasons),however, we want to adhere to the intent of OSHA's requirements and be conservative above all else.